ie * 4 ‘i CAS VANS) hoe oa pe See en eta. War Raa Whe FRB PPR ed iat ane eRe a! . wie Hh e i a ae Ny aS y\ Haris - TRS : Pekan bea S “ ’ we S h : - ne wee we wa ie SUR Re J MURMUR ee PAPAL A res Sa Be ‘SWS OS a's a THE LONDON, EDINBURGH, axp DUBLIN PHILOSOPHICAL MAGAZINE AND JOURNAL OF SCIENCE. Beer Gan BY LORD KELVIN, LL.D. P.R.S. &e. GEORGE FRANCIS FITZGERALD, M.A. Sc.D. F.B.S. AND WILLIAM FRANCIS, Pu.D. F.L.S. F.R.A.S. F.C.S. ‘¢ Nec aranearum sane textus ideo melior quia ex se fila gignunt, nec noster vilior quia ex alienis libamus ut apes.” Just. Lips. Polit. lib. i. cap. 1. Not. VOL. XXXV.—FIFTH SERIES. JANUARY—JUNE 1893. LONDON: TAYLOR AND FRANCIS, RED LION COURT, FLEET STREET. SOLD BY SIMPKIN, MARSHALL, HAMILTON, KENT, AND CO., LD.; WHITTAKER AND CO. ; AND BY ADAM AND CHARUES BLACK ;—T. AND T. CLARK, EDINBURGH ; SMITIT AND SON, GLASGOW ;--HODGRES, FIGGIS, AND CO., DUBLIN ;— PUTNAM, NEW YORE ;—-~VEUVE J. BOYVEAU, PARIS ;— AND ASHER AND CO., BERLIN, “Meditationis est perscrutari occulta; contemplationis est admirari perspicua.... Admiratio generat queestionem, queestio investigationem, investigatio inventionem.”—Hugo de S. Victore. “Cur spirent venti, cur terra dehiscat, Cur mare turgescat, pelago cur tantus amaror, Cur caput obscura Phoebus ferrugine condat, Quid toties diros cogat flagrare cometas, Quid pariat nubes, veniant cur fulmina ccelo, Quo micet igne Iris, superos quis conciat orbes Tam vario motu.” J. B. Pinelli ad Mazonium. CONTENTS OF VOL. XXXV. (FIFTH SERIES). NUMBER CCXIL—JANUARY 1893. Prof. R. Threlfall on the Electrical Properties of Pure Sub- stances.—Part I. The Preparation of Pure Nitrogen and mitempes to Condense it... (Plate d.) 1. ele os td die oe ys Messrs. Heinrich Rubens and Benj. W. Snow on the Refrac- tion of Rays of Great Wave-length in Rock-salt, Sylvite, amr ALONE). bola, soctasbheds oid. wyaiw is wi escel ol ote’ oo 0% Mr. Walter Baily on the Construction of a Colour Map . Mr. R. H. M. Bosanquet on Mountain-Sickness ; ; and Power MEME ERODE MCE oe 3 or 260s =. oh ois.'n, 3; mopiyas cayijeoe Masveuds AER Dr. William Pole: Further Data on Colour-blindness.— Prof. F. Y. Edgeworth « on a New Method of treating Corre- Ee SCS) IN Artis hui a bat miyhre Fi Swicki slew Foesens Mr. Fernando Sanford on a necessary Modification of Ohm’s emmy Ae oo Sra ce ik, te eke ge oe nS tees anoles Messrs. Rimington and Wythe Smith on Experiments in Electric and Magnetic Fields, Constant and Varying. Ephedra) eR Ses 2p crus C etme, whic « tate see WBN Y welnias pos ae NS Notices respecting New Books :-— Mid esawers Odorographiag.'.). .0\4a%. 0 ss eee oes « Proceedings of the Geological Society :— Prof. M. E. Wadsworth on the Geology of the Iron, _ Gold, and Copper Districts of Michigan............ Mr. H. M. Becher on the Gold-quartz Deposits of aban (vialay Peninsula) iter. cease ea ols esis Mr. F. D. Power on the Pambula Gold-deposits ...... An Electrolytic Theory of Dielectrics, by A. P. Chattock On a Chemical Actinometer, by H. Rigollot Bh Aen ae ae On the Attraction of two Plates separated by a Dielectric, eevee silicon Mereynes eg Wa Ses eee ck ee ee ees Investigation of the Properties of Amorphous Boron, by Be VOUSSAI \. Suny ae es sek ee vs 5 MS OES Se area ane Page 1V CONTENTS OF VOL. XXXV.——FIFTH SERIES. NUMBER CCXIII.—FEBRUARY. Page Dr. W. E. Sumpner on the Diffusion of Light ............ 81 Dr. G. Gore on the Relation of Volta Electromotive Force to Pressure &. 2. ces es oe ee 5s te, rr 97 iB] Galitzine on Radiant Hnergy ........-... .5: 3 eee 113 Mr. 8. U. Pickering on the Diffusion of Substances in Nolution ..6. 2 Si. se eee kee aed oo er 127 Prof. J. G. MacGregor on Contact-Action and the Conserva- tion Of Hnerey oo... tea ee sos ee 134 Mr. A. A. Campbell Swinton’s Experiments with Ze Frequency Electric Discharges .. 52. ..2.. 3c 142 Notices respecting New Books :— Mr. J. F. Blake’s Annals of British Geology, 1891 . 145 Proceedings of the Geological Society :— Prof, E. Hull’s Outline of the Geological Features of Arabia: Petrea and -Palestine.-...... 2.0. «s..05eeee eee 146 Rev. A. Irving on the Base of the Keuper Formation in Devon’ 2-0. A IC a err 147 Mr. J. H. Cooke on the Marls and Clays of the Maltese Tslamds: asco oe oaceia oie Wie caleta: «ate eer 148 Prof. T. G. Bonney on the Nufenen-Stock (Lepontine AN 0) :) A EO EEE 5 148 Prof. T. G. Bonney on some Schistose ‘‘ Greenstones ” and allied Hornblendic Schists from the Pennine Alps, as illustrative of the Effects of Pressure-Metamor- PHISMs © see ee eee oe eee ese ete he 149 Prof. T. G. Bonney on a Secondary Development of - Biotite and of Hornblende in Crystalline Schists from the: Binnenthal-......-. i... 8.04 one 150 Mr. J. H. Collins’s Geological Notes on the Bridgewater : District in Eastern Ontario. . 5. ~°" 120 eee 150 Visible Representation of the By polsde Lines in Plates traversed by Currents; explanation of Hall’s Phenomenon, by ©. Hommel... 0.0.5.4. 3 2. oe. 2a er 151 On the Action of Light upon Electrical Discharges m.various Gases, by I. Breissig..00. 0.0... 2 | 0 151 Notice of a Meteoric Stone seen to fall at Bath, South Dakota, by A. FE: Foote... 0.0.00 152 NUMBER CCXIV.—MARCH. Prof. Ludwig Boltzmann on the Equilibrium of Vis Viva-— Wart WT os fas i. oa wee S's 2 ak es er 153 Mr. Carl Barus on the Fusion Constants of Igneous Rock.— Part II. The Contraction of Molten Igneous Rock on Passing from Liquid to Solid: (Plate V.) 2... .... >) ase 173 Dr. J. R. Rydberg on a certain Asymmetry in Prof. Rowland’s Concave:Gratings.. 00... ah aa ca errr CONTENTS OF VOL. XXXV.-—FIFTH SERIES. v Page Mr. EH. C. C. Baly on the Separation and Striation of Rarefied Gases under the Influence of the Electric Discharge...... 200 Dr. J. H. Gladstone on some Recent Determinations of Molecular Refraction and Dispersion ...............+.. 204 Mr. Frederick J. Smith on High Resistances used in con- nexion with the D’Arsonval Galvanometer ............ 210 Mr. William Sutherland on the Laws of Molecular Force .. 211 Mr. Carl Barus on the Fusion Constants of Igneous Rock.— Part III. The Thermal Capacity of Igneous Rock, con- sidered in its Bearing on the Relation of Melting-point to fpeetemcoy. CelatooVil.)*! M5. seiko Aye wie Se Sg ke Ph 296 Notices respecting New Books :— Mr. P. Alexander’s Treatise on Thermodynamics ...... 307 Dr. Carl Barus’s Die physikalische Behandlung und die Messung hoher Temperaturen.............. 0.00% 310 Dr. Ad. Heydweiller’s Hiilfsbuch fiir die Ausfihrung elekerischer Messumgemi. hh .ckiad la sean ss eee dll Proceedings of the Geological Society :— Herr Victor Madsen on Scandinavian Boulders at Cromer 312 Miss C. A. Raisin on the Variolite of the Lleyn, and assecidted Volcanic Rocks. 2 as . we.) aw ts aay cians wa = 312 Mr. H. Emmons on the Petrography of the Island of CANDIED Fh che Se euoag Re Cnn Ge Nar ae eatag ge em eer 313 On a New Electrical PRES. by M. Henri Moissan ...... 313 On the Daily Variations of Gravity, by M. Mascart........ 314 Preliminary Note on the Colours of Cloudy Condensation, by MO eA TSU Speer ck Sh reg oie dS ev andeav's ypale Gh ae basen oe ahem 315 NUMBER CCXV.—APRIL. Dr. Charles V. Burton on Plane and Spherical Sound-Waves Sra tmmie; AMPLE Or... sc ths ei sre ip wie ede oe orig, vob or oe 8 = 317 Prof. J. D. Everett on a new and handy Focometer........ 333 Mr. G. H. Bryan on a Hydrodynamical Proof of the Equations of Motion of a Perforated Solid, with Applications to the Motion of a Fine Rigid Framework in Circulating Liquid . 338 Prof. G. M. Minchin on the Magnetic Field of a Circular CTUETRSTAUE "5 Ss scene Oar en ao CG 304 Dr. John Shields on Hydrolysis in Aqueous Salt-Solutions.. 365 Dr. G. Johnstone Stoney: Suggestion as to a possible Source of the Energy required for the Life of Bacilli, and as to the DP iicey Ok Ue is IMA WE SIZ whence y c1sis cyeuy m. shnisl sh sini oun #5 sues © 389 On the Magnetization of Iron Rings slit in a Radial Direction, lose Jak Mie loeiies anil seein te ere rae ne ne ae ee cn 392 Je ORAS UBT RANE ee! Sor Rea ng ean arco ee RIA re AY CEE eens 393 On the Official Testing of Thermometers, by I]. F. Wiebe .. 395 vi CONTENTS OF VOL. XXXV.—FIFTH SERIES. NUMBER CCXVI.—MAY. Page Prof. H. A. Rowland on Gratings in Theory and Practice .. 397 Mr. T. H. Blakesley on the Differential Equation of Electrical WG Wee OE a ee |e 419 K. Tsuruta on: the Heat of Vaporization of Liquid Hydro- chleric"Acid™ >. 2200.3 oe ES er vos SO M. P. Rudski on the Flow of Water ina Straight Pipe .... 439 Prof. J. Perry (assisted by Messrs. J. Graham and C. W. Heath) on Liquid Fmetion.. (Plate ViT.) ~.2: ..2 2 ee 44] Miss A. G. Earp-on the Effect of the Replacement of Oxy- gen by Sulphur on the Boiling- and Melting-points of Compounds’*30. 27202. 0 oD Pe 458 Notices respecting New Books :— Mr. R. Lachlan’s Elementary Treatise on Modern Pure Geometry 220i. se PS 462 Revue Semestrielle des Publications Mathématiques ré- digée sous les auspices de la Société Mathématique d’ Amsterdam... ..)..2y2 2s. 0 to. 2 463 Proceedings of the Geological Society :— Prof. J. W. Judd on Inclusions of Tertiary Granite in the Gabbro of the Cuilin Hills, Skye ; and on the Pro- ducts resulting from the Partial Fusion of the Acid ‘by the Basic Rock... 00. 5 SA er 464 Mr. W. 8. Gresley on Anthracite and Bituminous Coal- beds) cis i os oo tad ee 465 Messrs. Fox-and Teall. on some Coast-Seetions at the Lizard; and on a Radiolarian Chert from Mullion island seo. 3 ne EE 466 Mr. T. Roberts on the Geology of the District west of CaerinaribeMlc .. se. ices = 2's 4530 ie 467 Lieut. G. C. Frederick’s Geological Remarks on certain Islands in the’ New Hebridés °..-........ - eee 467 Mr. H. W. Monckton on the Occurrence of Boulders and Pebbles from the Glacial Drift in Gravels south of the Thames. 2. ....5 2260s... 150s 468 Mr. O. A. Shrubsole on the Plateau-Gravel south of Meade... dae ees se es a ee ee 468 Mr. Clement Reid on a Fossiliferous Pleistocene Deposit at Stone, on the Hampshire Coast ...............- 469 On Villari’s Critical Point in Nickel, by Prof. Heydweiller .. 469 On the Interference-Bands of Grating-Spectra on Geiatine, by DUE ON A. oe sis oes ova aie Bo hd ss Vale Un a 471 CONTENTS OF VOL. XXXV.—FIFTH SERIES. Vil NUMBER CCXVII.—JUNE. Page Lieut. G. Owen Squier on the Electrochemical Effects due : SMMC IAAT ON Gacy fa tot on Fests a wd vq ieiaas od eieleehei co od vee 473 Dr. ©. V. Burton on the Applicability of Lagrange’s Hqua- tions of Motion in a General Class of Problems; with especial reference to the Motion of a Perforated Solid in a MRE Mere ay os aN) oe VR ois 8 ages aQabte foe wats die d= 490 Mr. A. B. Basset on the Finite Bending of Thin Shells .... 496 Prof. Angstrém on Bolometric Investigations on the Inten- sity of Radiation by Rarefied Gases under the Influence <5 Flag rer DISIGI or ae rae a 502 Mr. E. C. Rimington on Luminous Discharges in Electrodeless WEE TIE ELLEN ecg ne eins Can ere ee Sa 506 Mr. M. S. Pembrey’s Comparative Experiments with the Dry- and Wet-Bulb Psychrometer and an improved Chemical TEV EIST TED ESC RG e e eg e wes d e RR Deer 525 Mr. R. E. Hughes on Water as a Catalyst...............- 531 Notices respecting New Books :— Drs. Bedell and Crehore’s Alternating Currents . .... 534 Prof. 8. W. Holman’s Discussion of the Precision of Measurements, with Hxamples taken mainly from Physics and Electrical Engineering................ 535 On the Disengagement of Heat occurring when Electrical Vibrations are transmitted through Wires, by Dr. I. Riis cer gas poke. LIS. Sthekoe Wie ahice ie 537 On the Potential of Electrical Discharge, by Prof. Heyd- NER PE Cotes aad bas bn (Ss alten Wo pease aden a WRRe 62 Da wees 538 On a Property of the Anodes of Geissler’s Tubes, by E. Sead SEM Tete sis, = Dae lav ain oahawel PH Viv SF ROE VL ee dW ae 538 PLATES. _ I. Illustrative of Prof. Threlfall’s Paper on the Electrical Properties of Pure Nitrogen. : ) II. Illustrative of Messrs. Rubens and Snow’s Paper on the Refraction of Rays of Great Wave-length in Rock-Salt, Syivite, and Fluorite. IIT. Illustrative of Mr. F. Sanford’s Paper on a necessary Modification of Ohm’s Law. IV. Illustrative of Messrs. Rimington and Wythe Smith’s Paper on Experiments in. Electric. and Magnetic Fields, Constant and Varying. V. & VI. Illustrative of Dr. Carl Barus’s Papers on the Fusion Con- stants of Igneous Rock. . VIL. Illustrative of Prof. J. Perry’s Paper on Liquid Friction, THE LONDON, EDINBURGH, axn DUBLIN PHILOSOPHICAL MAGAZINE AND JOURNAL OF SCIENCE. SSS eT SSS [FIFTH SERIES.] JANUARY 1893. I. The Electrical Properties of Pure Substances.—Part I. The Preparation of Pure Nitrogen and attempts to Condense it. By Professor R. THRELFALL”. [Plate I.] a 1886 a paper was published in the Proceedings of the Royal Society by Professor J. J. Thomson and myself, “On an Effect produced by the passage of an Electric Dis- charge through Pure Nitrogen.” The effect in question was briefly as follows :—When a nitrogen tube provided with a small mercury or sulphuric-acid gauge is exhausted to a pres- sure of about 8 millim. of mercury and then sparked with a discharge too small to heat the tube in a sensible manner, a diminution of the elastic force of the enclosed gas is observed. This diminution was found to be independent of the size or material of the electrodes, of the volume of the tube or the extent of its surface, but to depend on the kind of discharge employed, and its duration ; on the temperature and pressure of the gas in the tube during the process of sparking and afterwards. Arguing by exclusion, we attributed the diminu- tion of pressure to a condensation of nitrogen molecules, similar to the condensation which oxygen undergoes when converted into ozone. This property of nitrogen, if established, would be of un- doubted interest, and consequently in 1889 I undertook a * Communicated by the Author. Phil. Mag. 8.5. Vol. 35. No. 212. Jan. 1893. B I FO a Ot NL A TG I Ry NS A TN NT yee My mm 2 Prof. R. Threlfall on the Electrical repetition of the experiments with a view to testing our con- clusions by an extended examination of the phenomena in question. This investigation has proved a most laborious task; and it was not until December 1891 that I finally satisfied myself that the effect was due to the combination of nitrogen with the mercury of the pressure-gauge under the influence of the electric discharge, and in the presence, as I think, of a minute trace of some other substance whose nature I have not been able to determine. The experiments to be described leave little doubt that pure nitrogen at ordinary temperatures does not condense in the same way that oxygen condenses, whether the discharge be by means of external electrodes or by means of wires fused into the tube. Since these experiments form the starting- point of other researches, I will begin by an account of a method by which pure nitrogen may be most advantageously prepared. Singularly enough this apparently simple chemical problem has not, so far as I know, been solved hitherto. Sias, in his researches, makes the remark that nitrogen is easily obtained pure (Bulletin de ? Académie Royale des Sciences de Belgique, 1860, sér. 2, t. x. p. 254); and this remark may very possibly have produced misunderstanding—everything depends on what is meant by the word pure. ‘lhe fundamental principles in all processes of purification are :—Ilst, that reagents used to remove any impurity must really keep the impurity when they have got it, and not liberate it or its equivalent through any instability of the compounds formed ; and 2nd, that the reagents themselves must not give rise to impurities. As an example of a common violation of the first principle, I will mention the absorption of sulphuretted hydro- gen, sulphur dioxide, or the oxides of nitrogen, by potash or soda ; and of the second, the use of imperfectly prepared phos- phorus pentoxide. Trouble arising from layers of air or other gases condensed on the surfaces of glass vessels can only be relieved by arranging the method of production of the gas required in such a way that the glass surfaces may remain for weeks or months in contact with the gas under experiment, otherwise completely purified. If mercury be in contact with glass in any part of the apparatus, then, as I believe, it is impossible by ordinary means to be sure that the glass is ever completely denuded of its primitive layers of gas. I append a list of some of the varicus ways in which nitrogen has been prepared for careful work, and shall, I think, be able to show that all these processes are open to objection, at all events where a continuous supply of gas is necessary. The list is short, because nearly all experimenters simply state that Properties of Pure Substances : Nitrogen. 3 they used pure nitrogen without giving details of its method of preparation. Name. Moor otas,... Neuman Olzewski .... re blew Et: Lupton H. Deslandres. W. Gibbs.... N. W. Fisher, Regnault .... Wullner Huggins Warburg .... Reference. Bull del Acad, de Belgique, vol. x. p. 204. J, fiir prk. Chemie, [2] xxxvil. p. 342. Wien. Anzerger, March 1884. C. &. xeviii. p. 982. Cas: J. 18763 Chem. News, XXxiil. p. 90. CR. ci, p. 1256. Ber. x. p. 1887. Poge. Ann. xvii. . 187 Pp : COR} t. xx..p. 975. Pogg. Ann. cxlvil. p. 325. Phil. Trans. 1860. Ann, der Chem. und der Phys. 1887, p. 048. Method. By passing purified air over hot copper turnings and gauze, which are previously reduced by hydrogen. Copper oxide at end of tube (?); ordinary ab- sorbent reagents to help purify the gas after leaving the hot copper. From chloride-of-lime cubes (made by Winkler’s method) and aqueous ammonia (see C, 8S. J. 1887, p. 442). Hot copper and air. Hot copper and air. Air and ammonia over hot copper ; claims to get pure N with a short tube. Hot copper and air; no precaution mentioned. Sodium nitrite, ammonium sul- phate, and potassium dichro- mate in excess. If there is a trace of chloride present, im- purities are introduced. Uses cuprous chloride as an ab- sorber of oxygen from air. Hot copper and air. Burning phosphorus in air over mercury and removing traces of oxygen by incandescent iron wire. Purified air over hot reduced copper. Hittorf’s method. Dust-free air over hot white phosphorus, then over potassium permanganate, solid potash, and phosphorus pentoxide. Special drying in some cases followed by exposure (Wied. Ann. xl. p. 1) to nascent sodium obtained by the electro- lysis of glass. It is clear that the most popular way of making nitrogen is to absorb the oxygen from air by means of red-hot copper. There are a great many objections to this method, however, even when precautions are taken against the possibility of the formation of oxides of nitrogen. In the first place, a satis- factory method of making connexion to the porcelain tube is unknown to me; indiarubber stoppers are undesirable in any ~ 4. Prof. R. Threlfall on the Electrical case, and particularly in places where they can become hot. One never feels certain, moreover, that a red-hot tube, even of glazed porcelain, is absolutely ‘impermeable to furnace- gases. If one uses a bath of magnesia this difficulty may perhaps be overcome, but there remains the difficulty of making proper connexions. If hard glass be employed instead a porcelain, then there is insecurity i in the joints between it and the glass used for the remainder of the apparatus. Metal tubes present similar difficulties with regard to the junctions, and are besides more or less porous at high temperatures. Another grave dis- advantage is that, whether porcelain or glass tubes be used, there is “always a chance of a crack occurring, and perhaps escaping notice. The reduction ef the copper also presents great difficulty: it is more difficult to get a strong stream of really pure hydrogen or carbon monoxide than to get the nitrogen ; and any sulphur absorbed by the copper is a permanent disadvantage ; for, as metallurgists know, copper contain- ing sulphur may be oxidized and reduced many times and yet at each oxidation some sulphur will burn out. The reason is, of course, that sulphide of copper heated in air forms some sulphate of copper as well as sulphur dioxide. On the next reduction sulphide of copper is re-formed, and then, on passing air over the mixture, the process of incom- plete oxidation is repeated. Judging by a discussion which took place in Section A of the British Association not long ago, these simple facts are not as widely known as might have been expected. I know of no reagent which will absorb sulphur dioxide so as to form an absolutely stable compound, and which is itself easy to prepare in a state of sufficient purity to be above suspicion of giving off foreign matters to the nitrogen. Of course it may be argued that a large number of vessels containing, say, a solution of caustic potash might be used, the second retaining the sulphur dioxide given off from the first, and so on; but this device is obviously unsuited for a continuous process, where the reagents must be untouched for weeks or months. Finally, I gave the process a careful trial, and found it unsatisfactory “from the causes mentioned ; and, as a matter of fact, the trouble of preparing hydrogen or carbon monoxide in a sufficient state of purity to reduce the copper without contaminating it with sulphur or chlorine is at least as great as the trouble of preparing nitrogen itself. With regard to the method of passing air over melted white phosphor us, the manipulation of phosphorus i is always Properties of Pure Substances: Nitrogen. 5 troublesome, and I have not been able to find any information as to whether phosphorus absorbs gases which might be given off during the process of the removal of oxygen from. air. Warburg used a solution of potassium permanganate to absorb the vapour of phosphorus; but I have not been able to obtain information as to whether such a solution is to be relied on, in the first place to remove all the phosphorus, and in the second to give off nothing else during the process. I understand, from the paper im Wied. Ann. vol. xl. TSOOF peele that Warbur ‘o, in his later experiments, did not succeed to his satisfaction in remov ing the last trace of oxygen by this method, but had to electrolyse the glass of his vacnum-tubes so as to liberate the sodium in presence of the nitrogen, in order to get rid of the last traces of oxygen and hydrogen. This method appears satisfactory if one has at one’s disposal a sufficient electromotive force, suitable glass, and an infinite time : the hydrogen appears to be absorbed as by palladium. Another method over which I spent six months of fruitless labour is based on the decomposition of ammonium bichromate by heat. This method is convenient, because if the bichro- mate could be got to deliver nitrogen of suitable quality, small quantities of the salt could be decomposed in bulbs fused on to the vacuum-tubes along with suitable purifying reagents. Ordinary ammonium bichromate (i. e. that sold as pure) gives off a good deal of ammonia and oxides of nitrogen as well as nitrogen itself and water-vapour. This means the use of a good many purifying reagents, so that the method loses its advantages of simplicity ; and in addition the oxides of nitrogen cannot be fixed satisfactorily by any suitable reagent ‘known to me. I thought, however, that possibly very pure ammonium bichromate might decompose in a simpler manner, and consequently went to great trouble to procure a pure sample, For this purpose I purified a large quantity of ammonium chloride and sulphate by the method described by Stas (Bull. de ? Académie Royale de Belgique, 2nd ser. t. x. p. 283), repeating the boiling with nitric acid more often than Stas found requisite. The purified samples were used to generate gaseous ammonia (under the influence of specially prepared marble-lime), which after copious wash- ing was absorbed by chromic acid. Some samples of this ammonia were passed over red-hot platinized asbestos with sufficient pure oxyg gen* to destroy three quarters of the ammonia, 4NH;+3 ))= 6H, O+2N,, with a view to destroy- ing any traces of organic ammonium compounds; but the * The method of procuring pure oxygen will be described in another connexion. eis Prof. R. Threlfall on the Electrical resulting bichromate of ammonium coming from the small quantity of ammonia which was not destroyed by the oxygen did not differ in behaviour from the other samples. It may be noted here that Stas found (loc. cit.) that purified ammonia has a much less unpleasant smell than ordinary ammonia : careful trial, however, failed to enable me to detect any differ- ence between the smell of my purest ammonia and that obtained by boiling so-called pure solution of ammonia obtained from the dealers. I conclude that the “ pure ammonia” of commerce is much purer now-a-days than it was thirty years ago. The chromic acid was made from repeatedly crystallized bichromate of potash, bought as pure, and the sulphuric acid which is sold for analytical purposes. The resulting chromic acid was washed free from sulphuric acid by strong nitric acid, distilled for the purpose. I found incidentally that the addition of a little chromic acid to the mixture of nitric and sulphuric acid in the retort appeared to have a good effect in diminish- ing the quantity of nitrous acid which generally accompanies “fuming” nitric acid. The washed chromic acid was dried on tiles in the usual way, and heated with great care and continual stirring until it partly melted ; but even so it was slightly decomposed. Of course the greater portion of the nitric acid had been previously got rid of by heating the chromic acid on a water-bath in a partly exhausted retort with ground-on condenser, the latter containing some sticks of potash. The chromic acid being partially decomposed gave a solution, which had to be filtered through glass-wool before it was used to absorb the ammonia. This solution was tested by distilling, the distillate being tested for nitrites both before and after reduction with sodium amalgam. The result of these tests was to show that either the solution contained no nitro-compounds, or, if so, not more than are contained in the same quantity of platinum distilled water. The bichromate of ammonia made from this was recrystallized three times from platinum distilled water. Some small samples were crystallized up to six times, but did not differ from the results of the third crystallization. All these samples, when heated either in air or in vacuo, gave off nitrous compounds, and did not behave in any way differently to the sample which had been bought as pure. I therefore conclude that the normal decomposition of ammonium bichromate is complex, and that it is not a good substance to use as a source of nitrogen. I will now describe a method of procuring nitrogen which has not been mentioned hitherto, which lends itself remark- ably well to a continuous process, and which is almost, but not Properties of Pure Substances : Nitrogen. 7 quite, free from objection. I refer to the copper-ammonia and chromous-chloride method of Berthelot and Recoura (‘ Watts’ Dictionary, new edition, and Ann. de Phys. et de Chim. s. 6, vol. x. p. 5). When air is exposed to a large sur- face of copper wet with strong ammonia, the oxygen is for the most part absorbed. In my experience with the arrange- ments about to be described, there is only about three per cent. of oxygen left after the reagents have acted for half an hour, and only one per cent. after three hours. Since in practice with my apparatus the air often stands over the copper for a day or even a week, the absorption is probably nearly complete. The last traces of oxygen are absorbed by a strong solution of chromous chloride, which perhaps exer- cises a stronger absorptive power on oxygen than any other liquid, and is for this purpose quite easily prepared. As the method is not so well known as it deserves to be, I give the following description from Recoura’s paper :— A large flask is taken, and in it are placed 250 to 300 grammes of granulated redistilled zine with 50 grammes powdered crystals of potassium bichromate. The bichromate must be finely powdered ; it should be pounded till it looks bright yellow. Three hundred cubic centimetres of pure hydrochloric acid are mixed in a beaker with two hundred cubic centim. of water, and I have found it advantageous to heat the mixture almost to boiling. The contents of the beaker are then poured as quickly as possible into the flask, and a violent evolution cf hydrogen and steam at once com- mences. If the flask is too small, some of the liquid will of course be projected from it. Under the powerfully reducing influence of the zine and hydrochloric acid, the chromium is rapidly reduced to the state of green oxide, which then redissolves to a beautiful blue solution. The whole reaction only takes about ten minutes or a quarter of an hour. If the bichromate is not sufficiently finely powdered, a further quantity of hydrochloric acid may have to be added to com- plete the reaction, or the mixture may be left (excluding air) for a few hours. The blue solution contains chromous chlo- ride, chlorides of zinc and potassium, and possibly various impurities. The slightest trace of oxygen destroys the perfect colour of the chromous chloride by converting it into the green or grey substances investigated by Recoura. On standing over zinc for some time, however, if not too much oxidized and slightly acid, the chromium compounds become again reduced and the fine blue colour reappears. The colour is as clear and bright and almost exactly of the same shade as the colour of an ammoniacal solution of cupric hydrate. Recoura states that a stream of gas containing free oxygen 8 Prof. R. Threlfall on the Electrical can be completely deprived of the latter by allowing it to bubble once through a flask containing the blue liquid. To test this I placed two flasks in series, both containing a few hundred centimetres of the solution, and fitted with tubes allowing air to be sucked through both, one after the other. Though I allowed the air to pass much more briskly than if I had been actually using the process (say three times faster than one ordinarily allows the oxygen to pass in an organic analysis), I did not observe any change in the second flask till the first had long been quite opaque and had become more than warm, and then suddenly the contents of the second flask became attacked. In manipulating the chromous- chloride solution, it is useful to have a flask of the blue liquid permanently at hand to purify the carbonic acid or nitrogen which must be used in the subsequent operations. In many cases it does not matter whether the gas has a trace of hy- drogen in it or not; but for my purpose I was not willing to run any risk of having hydrogen about, and consequently I never allowed the purifying flask to contain zine. Having satisfied myself as to the reliability of the chromous chloride as an absorber of oxygen, I undertook a number of experiments with the object of discovering, Ist, the most suitable form in which to use it; 2nd, whether in the process of absorption any other gas was given off, or any vapour which could not be safely absorbed. In these experiments large vessels containing copper and ammonia (arranged in a manner to be presently explained), and capable of furnishing a continuous steam of nitrogen mixed with oxygen in pro- portions which could be varied at will, were used throughout. The ammonia was removed from the nitrogen by strong sul- phuric acid that had been heated to boiling and cooled in a vacuous desiccator. With regard to the best way of using the chromous chloride, I began with the impression that tubes filled with the dry salt would be the most convenient, espe- cially as Recoura shows that small crystals of dry chromous chloride have an affinity for oxygen which surpasses that of the solution. I therefore prepared large quantities of the blue solution, and obtained the crystals from it by the method recommended by Recoura, which is briefly as follows :—The blue liquid is mixed with a saturated solution of sodium acetate, which precipitates echromous acetate in the form of a dark red powder. This powder is then dissolved in dilute hydrochloric acid, and the chromous chloride precipitated from the solution by passing in gaseous hydrochloric acid so as to gradually increase the strength of the hydrochloric-acid solution Properties of Pure Substances: Nitrogen. 9 The crystals are repeatedly washed with strong hydro- ehloric acid and dried by pressing them into tubes with Kieselguhr. All these operations require to be performed in an atmosphere free from oxygen, and consequently are troublesome. The crystals are of a fine sky-blue colour, and have a really extraordinary affinity for oxygen. For my purpose, however, I disliked the use of the sodium acetate, because I never felt quite sure that I had washed all the resulting acetic acid out of the crystals. I have no reason to believe that, even if acetic acid were present during the absorption of oxygen, any organic compound would be libe- rated, but in the absence of any information I thought it better not to run the risk. I therefore turned my attention to the criginal blue solution. This of course contains chlorides of zinc and potassium, free hydrochloric acid, hydrogen in solution, and possibly traces of sulphur compounds coming from impurity in the potassium dichromate. It is a question, then, whether during the absorption of oxygen we may not have chlorine or sulphur compounds liberated. Both the acid and zine were free from arsenic and antimony, so that I had no uneasiness about these substances. I first satisfied myself that chlorine was not given off, by allowing nitrogen with 3 per cent. of oxygen to pass through two flasks of chromous chloride, and then through copper sulphate to retain traces of hydrochloric acid, and finally over paper dipped in a solution of iodide of potassium and starch. Though ten litres of gas were passed through, I could detect no change in the starch- paper. Sulphuric acid, when added to the blue liquid, is partly reduced and hydrogen sulphide is given off; conse- quently, since potassium bichromate is generally contaminated with potassium sulphate, which is hard to remove, I had to test whether any sulphur compounds were evolved. For this purpose, and with the arrangement of the last experiment, I passed nitrogen through the liquid and then over filter-paper, saturated with a slightly acid solution of nitrate of silver, but no change of colour could be detected. It remained for me to make sure that in the liquid I intended to use there could be no volatile impurity (the traces of hydrochloric acid itself need not be considered, because hydrochloric acid can be stopped readily by potassium hydrate). Before discussmg this I must explain my method of pre- paring the blue liquid, which was as follows :—About ten litres of the raw product were prepared in several operations and drawn into one large vessel through a filtering-tube. This tube contained a length of four inches of compressed glass- wool, and was closed at its lower end by a perforated platinum 10 - Prof. R. Threlfall on the Electrical plate whose edges were fused into the tube. The blue liquid was forced through the plug by a pressure of carbonic acid made from marble, which had been boiled for a good many hours at reduced pressure in water before being placed in the Kipp’s apparatus. This carbonic acid always passed through a wash-bottle of blue litmus purified in the way to be described by a preliminary experiment. ‘The filter acted so perfectly that the liquid passing through it was brilliantly clear and free from zinc-dust, which I greatly feared. In these preli- minary operations I was practically forced to make use of some rubber-stoppers, and this 1s the worst fauit of the method. How- ever, all the stoppers used were well coated with pure paraffin; and though they might have given oft some hydrocarbons, still I was unable to detect any trace of them in the nitrogen finally obtained. Some rubber-tubing was also employed to make joints, but the same precautions were taken with it, and in all cases the sulphur was well cleaned off. The filtered liquid was finaily got into a retort with a ground-on con- denser, and was concentrated to one third of its original volume in a brisk current of carbonic acid. © Towards the end of the operation the stream of carbonic acid was stopped, and a partial vacuum was created in the retort and condenser by a water-pump, so that the final con- centration took place under reduced pressure. These pre- cautions were considered sufficient to remove the hydrogen dissolved in the liquid as well as any traces of volatile sulphur compounds resulting from supposed impurities in the potas- sium bichromate. The resulting liquid was a clear blue syrup, and was transferred at once to the absorption-apparatus. Before going into any details as to other precauticns, I will describe the arrangements adopted for the continuous pre- paration of the nitrogen by this process. These arrange- ments will be most easily understood by a reference to the diagram (PI. I.), though taps and clips are exaggerated for clearness. g is a pipe projecting through the window of the laboratory, and terminating close to the wall at a height of about three metres from the ground. The University paddock separates the laboratory by nearly a quarter of a mile from the nearest road on this side, but the road on the other side lies within 150 yards. The elevation of the laboratory is 120 feet above sea-level. Consequently the composition of the air is probably move nearly that of typical “country air” than of town air. H is a U-tube with paraffin (M.P. 51° C.) covered cork stoppers, and is tightly packed with cotton-wool, from which the dust was blown before the tube was mounted. F is a two-way tap, Properties of Pure Substances: Nitrogen. it enabling the large glass vessel to be placed in communication either with the external air through H, or with the system of purifying tubes. The large vessel with tap KH is filled with copper gauze and strip, and communicates by a tube having a rubber-joint and clip D and tap C with another large vessel placed 2°4 metres above it (measured from bottom to bottom). The upper vessel can be put in communication with a water-pump by a pipe passing through B and having atapat A. This upper vessel contains strong liquid am- monia. It will be readily understood that by. working the taps &e. the ammonia may be drawn into the upper vessel while air is being admitted to the lower, and may then be allowed to descend by gravity, and furnish the requisite head to force the gas through the remainder of the apparatus when the two-way “tap F is ‘suitably turned. G is an auxiliary tap for allowing samples of the gas to be drawn off and tested for oxygen in an ordinary Hempel’s gas-analysis apparatus, not shown in the diagram. The air, from which the greater part of the oxygen has been sbsonbed by the copper and ammonia, now passes into a horizontal tube I about half filled with strong sulphuric acid, where the greater portion of the ammonia is absorbed. The management of this tube requires care or the entrance soon gets stopped up by the formation of ammonium sulphate. After two years’ work this tube was replaced by a large glass wash-bottle with ground-in stopper. J isa tube containing strong sulphuric acid through which the gas bubbles; / is merely a drawn-out end for facilitating the acon of the joints of the glass tubes. At K are two “double ” wash-bottles containing the chromous chloride Sys and L represents a U-tube with ground-in tap-stoppers filled with glass beads, and likewise containing chromous chloride. The stoppers of L and K are weighted with lead weights to enable them to stand the pressure, and mercury cups are arranged round the stoppers. M is a tube contain- ing a solution of caustic potash. N contains nitrate of silver together with a little silver hydroxide and potassium nitrate, O contains more potash, and P contains strong sulphuric acid. @ is half filled with potash in lumps, and half with soda-lime. KR is a tube into which phosphorus pentoxide has been distilled so as to present a large surface. 8,a Win- chester bottle with ground-in stopper, and the wide tube U both contain phosphorus pentoxide. Originally there was a mercury-gauge at V, and though this was dispensed with, the apparatus for eliminating mereury vapour was allowed to remain because one or two ‘drops of mercury had got into the tube near V. W is a specially fine tap protected with 12 Prof. R. Threlfall on the Electrical mercury ; and X is a little phosphorus-pentoxide tube re- quired to protect the tap, which is lubricated with phosphorus pentoxide, and which of course requires to be kept at the proper degree of concentration. Y is a sulphur tube, and at Z are silver and copper tubes. Beyond Z is seen a tube and gauge of the type used in experimenting on the nitrogen at low temperatures. & is a small phosphoric-acid guard-tube, Wis a sulphur tube, and © and ©® are silver and copper tubes separated from each other by long tubes of capillary bore. This system divides at 6, so that it may be put in communication with a water-pump wd d, a, and e, or a Geissler pump through 7, where there is another tap not shown. ‘The taps at F, W, d, and / are fine samples of the diagonal taps made by the successors of Geissler, of Bonn ; they have all been reground with ‘ optical” precision, and are all lubricated (except I) with phosphorus pentoxide and protected with mercury. ‘lhe weak point in the system is at the stoppers of L and K, which had to be lubricated with tallow. In order to satisfy myself of the nature of the tallow I began by purifying it with animal charcoal, and finally by keeping it melted for eight hours in a vacuum. After this the smell was almost gone and the tallow was applied to the stoppers mentioned. The tap F was lubricated with vaseline and beeswax also long melted zn vacuo. I feared that I should introduce hydrocarbons at these points, but the convenience of using the tallow caused me to try it, and undertake an examination of the gas in a vacuum-tube in order to find whether any hydrocarbons were present or not. The result was that no trace of the ‘ three” bands could be found, so that the enormous complications which would have been required in the other event were happily unnecessary. The stoppers of the large ammonia vessels were of paraffin-coated rubber. It will be noticed that all the points where tallow or rubber were used are to the right of the main purifying system, which includes strong sul- phuric acid, and the grinding of all the stoppers was so ac- curate that an almost inappreciable film of tallow was all that was necessary. It remains to describe the precautions taken with the various reagents, beginning on the right. Ammonia.—The examination of the ammonia sold as “ pure liquid ammonia”’ which I made in connexion with the am- monium bichromate experiments showed that nothing was to be gained for the purpose of the main experiment by attempt- ing any further purification. Copper.—At different times sheet gauze, wire, and turn- ings were employed. The purity of the copper does not Properties of Pure Substances: Nitrogen. 13 seem to be of importance, but it is necessary to get rid of grease. This must be done in such a way as not to waste too much copper. In order tu clean the turnings and gauze they were soldered into a copper tube, and a considerable quantity of shale benzine was distilled and allowed to condense among them. This secures that every part shall be wetted. The process was then continued by gasoline. The gasoline was distilled over the copper to avoid residues, and was finally dried out at about 120° for twelve hours, a good stream of filtered air being drawn over the copper by means of an air- pump. The same process was gone through with alcohol, and finally water. The copper was then washed with dilute chromic acid and digested with strong ammonia for half an hour. All this trouble was gone to, to avoid wastirg the turnings, which one has to cut oneself in order to get them in nice long curls, so that they will stand in the bottle and not break up at once and go to the bottom. After about a year’s work it was found necessary to renew the copper and ammonia—the former having almost disappeared in a yellow red mud (cuprous oxide ?) which was not further examined— and the ammonia solution had also partially lost its blue colour. Copper strip about 1 millim. thick was now used to replace the gauze and turnings and wire, and was of course strong enough to stand dipping in nitric and sulphuric acid. It is, on the whole, more convenient to use copper in strip than any other form. Sulphuric Acid.—This was bought as pure for analysis, and was heated with pure ammonium sulphate for some time before being used. Its purity was, however, of no great moment, except in the case of the final drying-tube P. Chromous Chloride—Already discussed. Potassium Hydrate-—During the experiments on the de- composition of ammonium bichromate, I incidentally noticed that all the samples of petash and soda in my possession yielded traces of nitrites, either on simple solution or when distilled with strong sulphuric acid (which was itself free from this impurity) and the distillate reduced by sodium amaleam. The samples of potash which were said to have been purified by solution in alcohol were the worst in this respect, while some rough lumps of commercial caustic potash were nearly free from the impurity in question. I found considerable quantities of nitrites also in samples of potash procured by exposing clean potassium to moist air. I did not try with dry air. After a good deal of trouble I was re- duced to using a solution of a sample of potash in sticks not specially purified, but which only gave the reaction very Ae Prof. R. Threlfall on the Electrical slightly, and was boiled under diminished pressure for two or three hours before use. The solution still gave a distillate with sulphuric acid which reacted with starch and iodine, but after a time so long that it was possible that the exposure to air during the experiment had been sufficient to supply the nitrite discovered. In fact a control experiment made with some ammonia, known to be free from nitrites or nitrates, yielded a distillate which coloured to nearly the same extent on standing. ‘The solution was made up to the strength re- commended for use in organic analysis. Silver Nitrate.—Crystals of silver nitrate bought as pure were dissolved in platinum distilled water to make a ten-per- cent. solution ; to this, when in the tube, a little of the potash solution was added—so as to form a little silver hydroxide. This hydroxide darkened gradually in the bright light to which it was exposed. It was not considered necessary to investigate the solution for traces of free nitrous compounds, as the gas on leaving it passed through another potash-tube. Solid Potash and Potash-Lime.—The above-mentioned stick potash was used, and the potash-lime was made by adding a little of the solution to some marble-lime prepared in the laboratory ; the drying process was carried out in a clean iron dish. Phosphorus Pentowide.—This, being the last reagent tra- versed by the nitrogen, requires to be exceptionally carefully treated. I began by acting on a hint obtained in 1889 from Prof. Josiah P. Cook, of Harvard, and endeavoured to pre- pare a pure sample of the pentoxide by burning phosphorus in a very strong draught of air, rather than by attempting to purify the ordinary commercial reagent. For this purpose an elaborate sheet-iron cylindrical chamber, measuring 3 feet by 2 feet, was prepared and fitted with suitable contrivances for carrying out the combustion of several pounds of phos- phorus. ‘The air-blast was obtained from a Root’s blower worked by a gas-engine, and the filtered air travelled through a tin tube about 4 feet long and 7 inches in diameter, filled with calcium chloride in the state usually described as “ rough dried.” After many attempts a large quantity of excellent pentoxide was obtained, which, however, though indefinitely better than the commercial product, still retained traces of phosphorus. The tests | employed for the purpose of dis- covering whether the pentoxide contained free phosphorus or not were the following :—(1) Dissolving 10 or 15 grammes weight of the pentoxide in clear distilled water and observing (a) whether anything remains undissolved, (@) whether, at the moment of throwing the phosphorus pentoxide on the Properties of Pure Substances: Nitrogen. 15 water any smell of phosphorus can be detected. (8) is a good deal more delicate than (a), for I clearly discerned the smell of phosphorus after the pentoxide had become pure enough to yield no perceptible particles when thrown into water. (2) A small porcelain crucible was filled with the pentoxide to be tested, the lid was replaced, and the crucible rapidly raised to a dull red heat, or till the pentoxide just began to distil off. The room in which the operation was conducted was quite dark except for the fickle light emitted by the Bunsen flame used in heating the crucible. As soon as the proper moment arrived the observer adjusted the cru- cible tongs with one hand and turned out the Bunsen with the other. The cover of the crucible was then removed. and by turning on a tap ready to hand a jet of oxygen was caused to impinge on the phosphorus pentoxide in the crucible: if any phosphorus is present “ sparkles’? are seen on the sur- face of the pentoxide ; and if the room is dark and the eyes of the observer sensitive this is a very good test, but not quite so good as that by the smell caused by throwing a large quantity of the pentoxide on water. (3) A few drops of a solution of chloride of gold in ether were mixed with about 500 cub. centim. of water, so as to make a very dilute solution. This solution was divided into two parts and occupied two similar cylinders. To one portion the solution obtained by throwing about 1 gramme of the pentoxide into 100 cub. centim. of water was added, and to the other an equal quan- tity of pure water. The observation, lasting for several days, consisted in watching the cylinders and noting the reduction of gold that took place, as evidenced by the rosy purple colour which the solution assumed. This test is not so deli- cate as the others, and is valueless unless a control experiment is made in the manner here described. As tested by these tests, the phosphorus pentoxide prepared by myself was never quite free from phosphorus, and I was therefore obliged to undertake the distillation of the raw product in a stream of oxygen. ‘This of course involved the making of the oxygen in a sufficient state of purity. For- tunately the presence of nitrogen in oxygen used for this purpose is of no consequence so jong as the amount is not large, the impurities to be dreaded are hydrocarbons and chlorine. The oxygen was consequently prepared from po- tassium chlorate with the usual precautions as for an organic analysis, being passed through several potash-tubes and wash- bottles on its way to the gas-holder—a large copper one free from grease on the taps. J'rom the gas-holder the oxygen passed through the following system: 16 Prof. R. Threlfall on the Electrical (1) Solution of potassium hydrate in tube 4 feet long. *(2) Tube 18 in. long, first half filled with metallic anti- mony, second half filled with clean silver foil. (3) U-tube 12 x1 in., solution of silver nitrate. (4) U-tube 12 x1 in., solid potash. (5) 2 ditto, salphuric-acid beads. (6) 1 bottle, phosphorus pentoxide. (7) 2 U-tubes, ditto. All the connexions were of glass throughout, but it was found convenient to use several rubber stoppers coated with hard paraffin. The distillation of the pentoxide was carried on in a porcelain tube 2 centimetres in diameter and nearly a metre long, the connexions being made with glass tubes pushed into the ends of the porcelain tube, and packed with glass-wool and some pentoxide. This packing is very firm and good. The first three quarters of the porcelain tube were nearly filled with pentoxide, the last quarter contained platinized porcelain and asbestos, the latter most carefully purified by boiling in hydrochloric acid and strong heating. The distillation was carried on in some cases so as to cause the pentoxide to condense in the tubes and vessels in which it was to be used, and a considerable quantity was also collected in a bottle. The final product passed all the tests I have enumerated, and was used throughout the nitrogen apparatus, even for drying the pump, lubricating the taps, &e. Of course a good many tubes full of pentoxide were distilled, and nearly three months were consumed in obtaining the final product. If I had not had the assistance of Mr. J. A. Pollock in this work, I have an impression that I might be at it still. The com- mercial pentoxide was used in this work, for the substance we prepared ourselves was probably good enough for most purposes as it was. I have sometimes wondered whether ex- perimenters who have of late used so much pentoxide for critical work on gases have recognized the necessity of testing the product obtained by distilling the pentoxide in oxygen. In my experience, unless the oxygen stream be very strong it is quite possible to fail to remove the last traces of free phosphorus. Sulphur t.—I happened to have some very pure sulphur which had been prepared for another purpose. It will be * It was found as the result of several preliminary experiments that metallic antimony is a rather good absorber of chlorine, and keeps what it absorbs. t+ An account of the experiments with sulphur will form a chapter of this monograph. Properties of Pure Substances: Nitrogen. li sufficient here to say that the sulphur was originally precipi- tated from calcium polysulphides by hydrochloric acid ; it was laboriously ground and washed, and distilled five times, and care was taken not to let it take fire. The degree of purity attained was tested by burning off large quantities in a burnished platinum dish, and continuing the process till the residue had disappeared. This product was rather precious, consequently it was made the most of in the present case by using it to coat glass beads ; some in powder was also employed near the entrance of the purifying tubes. Copper and Silver.—Both bought as pure and deprived of grease by dipping in appropriate acid solutions. General Remarks.— During the two years the apparatus has been in use various accidents, such as the breaking of pumps &e., have at ditterent times caused some of the re- agents to get mixed up, and the apparatus has been taken down and set up again some three or four times; the first bottles of chromous chloride have also required to be refilled. The phosphorus pentoxide has never required to be touched. I wish to draw attention to a remark of Hittorf’s as to the importance of using tubing free from air-bubbles. On several occasions I have been much troubled by the minute leaks which such imperfect tubes give rise to at the joints, and I have in my possession at least two tubes leaking from this cause, but so minutely that even when the leak was localized to within six or seven inches it was impossible to say exactly where it was. In work of this kind the cleaning of the tubes is of course of great importance. If the work is to be done rapidly the great secret is to clean the tube with alcohol before the jointing or general glass-blowing opera- tions are carried out on it. ‘The dirty places are almost always near where the blowpipe-flame has been applied, and after trying all and every means of cleaning, I have finally come back to aqua regia caused to boil at the dirty place and left in the tube for at least ten hours. Certainty of cleaning and jointing has led me to employ English flint glass ex- clusively in this work, and I always use the clean flame of an oxygen-gas blowpipe, which saves time so as to far more than repay the cost of the oxygen. All the blowing required in jointing the tubes is done through a compact but efficient establishment of filtering and phosphoric-acid tubes. The glass springs so extensively used throughout allow of con- siderable latitude in the relative movements of parts of the apparatus, and I have had no cases of spontaneous breaking. The whole of the glass work has been done by myself, as L can get no assistance of a suitable kind in Sydney. Phil. Mag. 8. 5. Vol. 35. No. 212. Jan. 1893. C os 18 - Prof, R. Threlfall on the Electrical ~ It may possibly be objected that some of the precautions taken are finnicking, and that (as in the manufacture of the oxygen) an unnecessary variety of absorptive materials are used. The reply I should make to such a criticism is that the complete operation of any one reagent is always to some small extent hypothetical, and I consider that by varying the reagents one helps to get rid of the chance of the persistence of impurities so small in amount as to be beyond the range of ordinary analysis, 2.e. beyond the point up to which we are certain of the action of the reagents. Testing the Gas for Hydrocarbons and Hydrogen. _ In order to avoid the impurities introduced by the presence of internal electrodes, a tube was prepared with external electrodes. It was about 35 centim. long, of which length 20 centim. were made of capillary tube. In order to fill this with the pure gas, the apparatus was exhausted three times, as far as the chromous chloride U-tube, each exhaustion re- quiring seven or eight hours’ work with the Geissler pump, after a good water-pump had got rid of the greater part of the gas. The pressure of the remaining gas was imperceptible by inspection of the pump-gauge (of which a description will be given), but the pump continued on each occasion to show a just appreciable bubble of gas when the mercury flowed into the barometer-tube. The pumping was done at times separated from each other by three or four days in order to give the residual gas from the walls of the vessel time to come off ; of course this gas was removed as it appeared. he pressure I should judge was, on each occasion, about of the order of -01 millim. Several bottles of gas were also forced through the apparatus at the ordinary pressure. Finally, on Feb. 19, 1891, the tube together with another for experimental purposes were fused off—the former at about *1 millim, pressure (the latter will be dealt with later). The tube had previously been heated till the glass began to soften and the walls to fall in, and the gas admitted had been for several days in contact with the phosphorus pentoxide. The only objection to the external electrode tube is that I have hitherto failed to produce a line-discharge in it—though of course Prof. J. J. Thomson’s method (Phil. Mag. vol. xxxii. 1891) would give it in an endless tube without electrodes, and if the method had been known at the time I should have employed it. However, I got a bright bluish-white discharge in the narrow tube (the larger ends being golden), and this Properties of Pure Substances: Nitrogen. uy) yielded a fine band-spectrum which has been described often enough, showing well both in the more and less refrangible ends. I took as my authority on the typical hydrocarbon bands those mentioned in the B.A. Report for 1880, p. 226. Observer. Wave-length. Angstrom and Thalén . . 5633 at least refran- gible end. Pi ges ee ty a p WOOL L Angstrém and Thalén . . 5164 Peaks fe herby Sf ae} lei’ err, HOLOD Angstrém and? Thalén elo 2 4736 Weise eet ai ear So Professors Liveing and Dewar (Proc. Roy. Soc. vol. xxx.) say that the characteristic spectrum of hydrocarbons is com- posed (among others) of four bands in the orange, yellow, green, and olive. ‘These were well seen by me in an olefiant- gas tube prepared for the purpose without any pretensions to purity. The cone of a Bunsen flame was also examined, and I saw the lines (according to my map) a at 5637 instead of 5634 [Seas (Salat A, 5165 (strongest) y ,, 4736 ms 4738 1 had a number of commercial tubes and examined these as a check ; the following is the result : @ turned up in petroleum and alcohol but not in olefiant gas, where there was a band at 5197 to 5198. This last band was strong and was seen in CO,, H, O, turpentine, petroleum, and eoal-gas, as well as in the clefiant gas. I do not know what this band is due to, but it did not appear in the nitrogen. The nitrogen was examined side by side with an alcohol tube showing « and 8 well; but the former did not show these bands or any trace of them. The nearest band was at 5240, and quite too far away for there to be any mistake. The experiment was also tried with a similar tube and nitrogen at 10 millim. pressure, with a like result. Finally the examina- tion was repeated at the lowest pressure at which I could get a brilliant discharge, which was of course far beyond the limit of discrimination of my pressure-gauge. The result was the same as before. The red and blue hydrogen lines were never seen in any of my tubes showing banded spectra. This analysis is of course dependent partly on the accuracy of our map, though when once the typical lines were picked up, their coincidence or not could be determined by direct expe- C2 20 Prof, R. Threlfall on the Electrical riment. It was necessary, therefore, to make a map of the spectrum to suit my spectroscope. The latter was an instrument with a 5-in. Trouton and Sims circle, and was made by Hilliott Bros. ; one fine heavy glass prism was used throughout, and the map refers to it; 1t was always in the position of minimum deviation for each line observed. The mapping of the spec- trum was done for me by Mr. J. H. D. Brearley (a student in the laboratory), who also assisted at this time in all the spectroscopic work and to whom my thanks are due. The map was made by a selection of 33 lines drawn from all sorts of sources, and verified in all sorts of ways, the tables used being those in the B.A. Reports for 1884, 1885, 1886 ; Row- land’s map (got in 1889) ; and Rowland’s table, Phil. Mag. 1889. Schellen was also found of some use. Hach line was set upon ten times; and the prism was adjusted ten times. Intermediate lines were now well picked up off Rowland’s map. Our limit of discrimination was about 2 in the fourth significant figure of the wave-length, 7. e. I could not decide with certainty that a line 1 made out to be at, say, 5165 was not at 5163. I append a list of the lines used in mapping the spectrum, not because it is in any way to be regarded as a model selec- tion, but because I, as a beginner at spectroscopy, should have been very glad of such a list at the time, had I been able to find one. I also note the means adopted by us for the iden- tification of the lines, as it may interest other beginners in spectroscopy. The lines are not given in the order in which they were examined, but in order of wave-length. 1.—B. Sun, 6867°796-6867-462. Rowland, Phil. Mag. June, 1889. Recognized by being near both to a large iron and to a potassium line. 2.—Li,, 6705°4. From lithium chloride in a Bunsen flame. Wave-length from B.A. Report, 1884; given by Mascart, Liveing and Dewar, and Thalen. 3.—C, Sun (hydrogen). Good line recognized by com- parison with a tube-spectrum of H,O. A=6563°042. Rowland, Phil. Mag. 1889. 4,—Sun, 6400°2. A good line picked up when the map was nearly finished from Rowland’s map. 5.—Sun, 6191°7. Same as number 4. 6.—Li,;, 6102. Authority, Mascart. 3.—Iron line, 5930°4. Rowland’s map verified by com- parison with spark-spectrum of iron. B.A. Report. Cornu gives 5929-3. Properties of Pure Substances : Nitrogen. At 8.—D. Halfway between the two lines. Mean, A=5893. Rowland, Phil. Mag. 1889. Compared with sodium flame. 9.—Picked up from Chart. A=5709°8. 10.—Barium (vy). From flame-spectrum of Ba (NO3)p. B.A. Report, 1884. Liveing and Dewar. %=5534:3. A bright line. ; i1.— Magnesium, A=5528. Rowland’s map and_ spark- spectrum. 12.—Thallium (2), \=5349. B.A. Report, 1885. Liveing and Dewar, and de Boisbaudran. Got from flame- spectrum. 13.—Iron, 5328:°2. Rowland’s map verified by spark-spec- trum. A good line. 14.—H. A=5270. Rowland’s map, a big double. Picked up at first because it was found from Schellen’s map that it was between two cobalt lines and near an iron line. These lines were seen in their proper relative places in the spark-discharge from iron and cobalt. This was one of the first lines identified. 15.—b,, 5183°798. Rowland, Phil. Mag. Verified by mag- nesium-spectrum. One of the first lines got. 16.—A=5041-5042. Picked up from Rowland’s map. Veri- fied by finding from B.A. Report that it was an iron line and then confirming by spark-spectrum. 17.—vA=4957°6. Picked up and verified as in the last case. 18.—rA=4920°6. Ditto. 19.—F. 2X7=4861:492-4859-929. Rowland’s map confirmed by vacuum-tube. 20.—Bismuth. »=4752. B.A. Report, Thalen, and Huggins. From spark-spectrum. Not very good. lHvidence as to identification, its general relation and appearance. 21.—Bismuth. XA=4724°5. ee we ee a a a a ee ea me A 3X | MERCURY LEVEL 3cer l Vv Inside diameter of main tube 1:5 cm. ; thickness of walls 15 cm, slightly changed conditions, so that new facts might present themselves and the previous results be controlled. I decided to make a tube of such a kind that I could begin by sparking it so that the sparks only passed through nitrogen, and then, after a sufficient interval of time and at any convenient opportunity, introduce mercury with a view to observing the modified action. In order to vary the conditions, the whole drying apparatus up to the sulphuric-acid tube was pumped out afresh and filled with gas, which passed through the reagents very slowly. This precess occupied two days, one day and a half it took to exhaust the vessels, and half a day t 30 Prof. R. Threlfall on the Hlectrical (5 hours) for the gas to flow in. It will be convenient here to describe the tube employed, though the dimensions given are taken from a later experiment, which was supposed to be a repetition of the one in question ; the dimensions of this tube may therefore be in error by a few per cent., but the actual dimensions are not of muchimportance. The ends of the tube dip down into mercury cups (not shown) so as to protect the part where the wires enter from leakage. The mercury pocket in the tube which forms the subject of the diagram (fig. 2) is attached to the spark-tube by means of a capillary tube 14 centim. long. This capillary tube was the finest piece of thermometer tubing I actually happened to have by me, and was, as I should imagine, about*1 millim.indiameter*. In preparing the tube after the final filling, the inlet at A is fused off, and when the proper pressure is reached the pump connexion at B is sealed, and afterwards, in two or three hours’ time, the con- necting tube of the mercury gauge. September 10-19. These days were spent in abortive attempts to get tubes of the pattern described to submit to having their electrodes white-hot for two or three hours without fracturing the glass. September 19. Tube 5, as described, sealed off at 87 millim,. The mercury was put in hot through a side-tube, but was not boiled zn setu in order to avoid getting vapour into the spark-tube. In order to avoid the presence of air- bubbles between the mercury and the glass, the tube at C was at first about 8 centim. long, and was drawn down to a fine point, where it was fused off. The apparatus was then filled with nitrogen and well heated when containing a nitrogen vacuum, especial care being devoted to the mercury pecket. Nitrogen was then admitted at more than atmospheric pressure, and finally the end of the tube was broken off near © and the mercury run in as quickly as possible from a fine funnel reaching to the bottom of the pocket. The tube at C was then sealed, and the mercury warmed again to perhaps 100° C. and the visible bubbles displaced, the tube being of course vacuous. Sept. 21. The mercury in the gauge was accurately at the same height in both limbs. Sparked for five hours with the best kind of sparks ; no effect. Sept. 22. Sparked four hours with an air-break in cireuit just sufficient to stop the spark but not the brush-discharge across the air-break. It was noticed that luminosity went * This capillary tube was part of the later arrangements. In the tube under discussion its place was taken by a tube 2 millim. in diameter and only about 6 centim. long. Properties of Pure Substances : Nitrogen. al down the tube to the mercury, and was much increased by touching the outside of the tube near the mercury. This dis- charge, ‘of course, was small compared with the discharge in the main tube. There was no effect on the gauge. Sept. 23. Sparked with rather large sparks 6} hours. No effect. ; Sept. 24. Sparked strongly, so as to make the tube warm, for 64 hours. No effect. Sept. 25. The mercury boiled up into tube. This led to the gauge showing a real increase of pressure of a little less than *1 millim.; T attribute this to gas from the sides of the tube between it and the mercury. Sparked strongly for 52 hours; when all was cold the pressure excess had grown to about *2 millim., i.e. in a direction contrary to the one expected. Sept. 26. Discharge on for 64 hours fairly strong, so as to warm tube perceptibly. The gauge then showed the same pressure on each side. Sept. 27. A wet paper band round that part of the tube where the mercury was most thickly condensed. Sparked four hours (?). No effect. Sept. 28. Ditto 3 hours. No effect. Sept. 29. Faint sparks for 5 hours ; wet paper band, as before. No effect. Oct. 1. Temperature being more rigorously equal, and gauge carefully tapped, there isa shrinkage of about *1 millim. | Sparked six hours with faint sparks and wet paper round tube. No effect Oct. 2. Strong current on 6 hours. Looking the next day (Uctober 3rd), a faint yellow tinge was observed round the mercury drops, and the gauge showed ‘8 millim. difference of pressure. Sparked hard 6 hours; the mercury was now obviously attacked, and when examined on October 8rd it was found that the pressure difference amounted to 3°2 millim. Sparked 3 hours with full discharge ; this increased the effect to 6 millim., and in another 44 hours the discharge had become splendidly golden, the resistance in the tube small, and the tube was fluorescing strongly (a sign of mercury vapour). Effect increased to about 7 millim. The experiment was then inter- rupted by the cracking of the tube. No opportunity for examining the deposit occurred till November 16th, z.e. for more than a month. The tube was then cut into bits, and it was observed that the deposit had become partly incrusted with some whitish incrustation. On trying to produce an explosion the experiment failed, and it was obvious that the film had quite decomposed. It is to be noted that the mercury was only attacked with difficulty. oo Prof. R. Threlfall on the Electrical Tube 6.—Dec. 5, 1891. This is the tube shown in fig. 2. All drying apparatus exhausted twice; tube prepared by a steady discharge during December 11th; left till 14th to test for leaks, when it was found that the whole apparatus was air-tight. Tube again sparked hard all December 14th with best pump-vacuum attainable. Electrodes at a bright red heat for 15 hours ; mercury separated by long tube and boiled in pocket. Sealed off at about 6 millim. pressure on December 15th. Dec. 16. Sparked 2 hours through capillary water resist- ance ; tube slightly warm. No effect. Dec. 17. Sparked so as to produce a yellow glow for 3 hours and by small blue sparks for 1 hour. No effect. Dec. 18. Sparked with fairly strong discharge for 8 hours. Tube too warm to read: so left till December 3]st, when it was found that the tube pressure had diminished by *2 millim. This led to an examination of the tube by hoiding a sheet of white paper behind it; and it was found that a bronze-coloured film had formed where mercury had condensed near the top of the capillary tube. ‘The mercury within the sphere of action was only the most minute trace. Sparked 3 hours and on. Dec. 22. Effect about :3 millim. Sparked for about an hour, and then on careful examination it was found that the glow was actually passing down the tube to the mercury. It was clearly of no use to go on with the experiment in this way, and consequently the mercury was boiled into the tube and the spark turned on. ‘The effect diminished during the boiling from °35 millim. to ‘3 millim. Sparked then for 5 hours ; effect increased to 1°2 millim. Dec. 26. Sparked 4 hours. Effect 2-4 millim. Dec. 27. Ditto 3 hours. Hffect 4°3 millim. Dec. 28. Sparked for one hour, when it was noticed that the tube-resistance had increased and the gauge showed 5°38 millim. of effect ; hence the tube is nearly empty. On first turning on the spark, the illumination began by being strong - for about one minute. The strize were well marked, and the mercury spectrum prominent. After about one minute the luminosity diminished to that corresponding to faint blue sparks. In twenty minutes the tube was again hot and fairly luminous, and continued with luminous sparks and rising tem- perature for 35 minutes: the gauge showed that the rise of temperature (?) was producing an increase of pressure. Tube cooled for one hour, when it was found that the excessive sparking had at last cracked the tube near the platinum wire, and that some mercury had been drawn in. The tube was then cut into bits, and one was heated in a test-tube in a Properties of Pure Substances: Nitrogen. 33 glycerine bath with the same precautions exactly as one uses in taking a melting-point. I extract the following account from my note~book verbatim:—“ I could not detect any change till about 230° C., at which temperavure quiet decomposition set in, and was complete and the tube clean at 235°. A con- siderable portion of the thermometer stem was outside the bath, though it did not begin to register till above 110°. Making all allowances, the temperatures might on this account have been anything less than 5° above those given. The tem- perature rose very slowly, and the glycerine was kept well stirred by a crescent-shaped stirrer of zinc. Hxperiments on other bits of the tube were made by heating them in the bare flame. In two of these (out of about four) there was a distinct crepitation, but I did not note any flash, though that the decomposition when once started ran very rapidly over the whole mirror was well seen in all the experiments. The deposit suddenly brightered with a puff of vapour. I could detect no nitrous smell. The temperature must heve been 200° C. in all eases. The platinum deposits were enormous, and the elec- trodes torn up in all directions as described by Hdison.” These experiments may be considered to settle the question of the cause of the effect observed by Professor Thomson and myself in 1885 and 1886. No trace of the effect was ever found unless the mercury was attacked ; and, contrariwise, the mercury was never seen to be attacked without the “ effect” making its appearance. It is curious to note the difference in the readiness with which the action can be brought about, even when all the circumstances of the experiments appear to be identical. It is for this reason that I imagine that the reaction requires the intervention of minute traces of some third sub- stance, and the actual amount of these traces differs in different experiments. When the reaction once commences it goes on with increasing rapidity till near the end, and apparently faster the more powerful the discharge. One experiment appears to indicate that even after the trimercuramine (?) is decomposed its constituents are in a state of “labile”’ equi- librium with respect to one another, and combine slightly or separate according to some set of circumstances which I cannot assign. It is curious, too, that the dissociation should be so irreversible. Unless the mercury vapour continually liberated is removed from the sphere of action—by combination with the platinum deposit, for instance—I cannot understand the effect of repeated heating ; and, indeed, I consider that the suggestion just made is very possibly the true explanation. The condensation of nitrogen, therefore, at ordinary tem- peratures has not been observed ; but it is possible that it may Phil. Mag. 8. 5. Vol. 35. No. 212. Jan. 1893. D b4 On the Electrical Properties of Pure Substances. occur at low temperatures. Jor this purpose | prepared Tube 7, which is figured in the Plate in the position it occupied before it was sealed off. This tube was prepared with even more than the usual care. Thus, the cleaning of the tube occupied two days and the final rinsing was accomplished by means of some thrice-distilled water from the platinum and gold still. This water ran into the tube direct from the still. The electrodes were prepared by sparking during five hours witha discharge sufficient to make them red- hot, during which time the tube was thrice filled and exhausted. The next day the tube was heated twice, and on each occasion about 500 cub. centim. of gas were passed through it; after which it was exhausted as far as possible (in an hour), and then the final charge was allowed to enter. The tube was sealed off at 8°7 millim. pressure, and then put in salt and pounded ice and kept at —14° C. by means of frequent stirring and the aadition of fresh ice and salt. Sparked 2 hours with effective sparks: no effect. (The effect was looked for the next day, when the temperatures were equalized, but was not observed.) | Jan. 2. Sparked for 2 hours at about —10° C., all kinds of sparks. No effect. The filamentary tube was then replaced by a wider one, as it was observed that the gauge only acted very slowly owing to the extreme fineness of the filamentary tube. The spark- tube then required to be pumped out and prepared afresh, except for the heating of the electrodes, which, however, inci- dentally took place. Jan. 4. Sparked 13 hours at —10°C. No effect. Jan.6. Sparked 7 hours ata mean temperature of — 8° C various sparks. No effect. Jan. 7. Observed again, at very uniform temperatures. Still no effect. Jan. 12. Ditto. The conclusion is that no effect is produced on nitrogen, so far as condensation goes, by sparking it at a temperature of about —10°C. and at a pressure of 8:2 millim. s ce) Summary of Results. 1. Nitrogen can be prepared by a continuous process in a state of great purity. 2. Nitrogen so prepared cannot be caused to condense by any available kind of spark down toa temperature of —10° C and a pressure of about 8 millim. 3. When mercury is presen:, a compound of mercury and Refraction of Rays of Great Wave-length. 35 nitrogen is formed. This compound is probably identical » with the nitride obtained by Plantamour. 4, The rate of formation of this nitride, other things being the same, is so irregular as to suggest that its formation is due to the interaction of an otherwise inappreciable trace of some other substance. 5. This compound is dissociable ; but under the circum- stances of the experiment the dissociation process is not entirely reversible, since sufficient heating will permanently destroy the compound. 6, There are changes in the appearance of the discharge in nitrogen which can be brought about by very slight variations of temperature, and possibly of electromotive force, for which, so far as I know, no explanation is at present forthcoming. Sydney, August 5, 1892. II. On the Refraction of Rays of Great Wave-length in Rock-salt, Sylvite, and Fluorite. By Heinrich RuBens and Bens. W. Snow™*. [Plate IL] N volume xl. of Wiedemann’s Annalen one of the present authors recently described a method whereby a know- ledge of the dispersion of rays in the infra-red may be easily obtained. With the aid of this device the dependence of the index of refraction upon the wave-length was determined for sixteen materials ; viz. for nine different samples of glass, for water, carbon disulphide, xylol, benzol, quartz, rock-salt, and fluorite. Inasmuch as in this paper is given a minute de- scription of the methods employed, it will suffice here briefly to refer to the main features of the method of procedure followed in the present determination. The rays from the zirconia burner of Linnemann, after being reflected from the front and the rear surfaces of a thin plate of air, enclosed between two parallel glass planes, were then concentrated upon the slit of a spectrometer, by which means two beams of light were produced, capable of mutual interference, so that the otherwise continuous spectrum of the incandescent zirconia plate was crossed by a series of vertical interference-bands. The wave-length » of each such dark band, multiplied by a certain whole number m, always equals the product of twice the thickness d of the layer of air and the cosine of the angle of incidence? of the rays. With the aid * Communicated by the Authors. D 2 36 HH. Rubens and B. W. Snow on the Refraction of of the Fraunhofer lines the wave-lengths of the interference- bands were determined for the visible portion of the spectrum, and from these data were calculated the order m of each dark band and the product K=2dcosi. The knowledge of these two constants proved, then, sufficient to determine also the wave-lengths of the interference-bands in the infra-red. The positions of these latter were obtained by allowing the sensitive filament of a linear bolometer to wander through the spectrum, and plotting the observed galvanometer-deflexions as a function of the angular deviation. ‘The interference- bands are then recognized as minima or maxima in the curve. In this way, for a series of angular deviations may be deter- mined the corresponding indices of refraction; that is, a number of points in the n—2 plane determined, which, when joined by a smooth curve, give the curve of dispersion for the material examined. In the majority of the bodies thus investigated, the limit of the region in the infra-red capable of being explored was prescribed by the absorption, which increases rapidly with increasing waye-lengths. In two cases alone, viz. when working with rock-salt and with fluorite, were the investiga- tions discontinued at wave-lengths ~X=5°7m and A=d'3yu respectively, before the region of strong absorption was reached. This was rendered necessary by the fact that the apparatus employed proved to be insufficiently sensitive to measure the exceedingly feeble energy found in the spectrum of the zirconia burner at these long waye-lengths. As a means of continuing the investigation beyond this point two ways of improvement suggested themselves. At first we thought it possible to increase the energy of the source of light, but all endeavours to attain this end proved of no avail. The use of the electric arc for this purpose was, after a short but thorough trial, discontinued. Even are lamps of unusually good regulation, when supplied by the almost per- fectly constant current of the Berlin Central Station, gave a radiation too fluctuating to be used in place of the zirconia light. The regulation of the are by hand was also tried, but also without success. The use, moreover, of a zirconia burner of nearly double the dimensions of the former resulted in only a feeble increase in the energy, while a series of new diffi- culties was thereby introduced, such as the melting of the latinum cell, a greater consumption of gas, &. We con- cluded, therefore, for the further investigation, to retain the source of light in its original form, and to make better use of the energy here at hand by increasing as far as possible the sensitiveness of the measuring apparatus. — Rays of Great Wave-length in Rock-salt, Sylvite, §e. 37 The first change toward the accomplishment of this end was efiected in the substitution of two plane surfaces of larger dimensions in place of the reflecting plates formerly used. For this purpose the optical firm of Carl Zeis, of Jena, most generously provided us with two plates with plane surfaces, 4 centim. square and 1 centim. thick, one of crown glass and the other of fluorite. The plates were set in metal frames, and the distance between them regulated by a system of screws, as in the former case. With the exception of the extreme edges both plates were ground to a truly plane sur- face. A rectangular opening in a diaphragm, placed in the path of the rays, allowed only light to enter the slit of the spectroscope which had been reflected from the central portion of the plates. The interference-bands thus produced were unusually sharp, as can be seen from the pronounced minima of the curves in figs. 1, 2, and 3 (Plate I1.), which represent the three different energy-spectra. Hardly need it be men- tioned that in the following experiments the entire optical system consisted wholly of rock-salt and fluorite. The delicacy of the bolometer was increased chiefly by using a galvanometer of the highest degree of sensitiveness which one of us had constructed, and which will be described in detail in a forthcoming paper. The coils of the galvanometer in series measured 140 ohms resistance. When the period of the needle was reduced for the single swing to 10 seconds, one millimetre deflexion on the scale indicated a current of 1:3x10-" ampere. With this degree of astaticism the zero- point of the needle was perfectly constant. The bolometer with which the following determinations were made is described as No. 2 in the previous paper. It consisted of two strips of platinum, 12 millim. long and 0:05 millim. wide, each having about 80 ohms resistance, only one of them being exposed to radiation. With the aid of the new galvanometer we were able to trace a sensitiveness of 0:000003° C. per millimetre deflexion. A standard candle one metre distant produced a deflexion of 400 milli. With the exception of the changes here mentioned all pieces of apparatus were identical with those formerly de- scribed. The relative positions, moreover, of the instrument, as well as the manner and the order in which the operations were performed, were retained unchanged. We can therefore pass at once to the results of our observations. Measurements were made upon the three materials so well known for their diathermanous properties—rock-salt, sylvite, and fluorite. 38 H. Rubens and B. W. Snow on the Refraction o7 I. Rock-salt. We had at our disposal a prism of this mineral having a triangular base 34} centim. on each side and 43 centim. in height. Before being used the prism was freshly polished and its refracting angle redetermined. ‘The observations with the bolometer gave the energy spectrum represented in fig. 1, Pl. Il. The positions of the maxima and minima were corrected, as in the paper cited above, with the aid of the enveloping curve, whereby the points of contact of the two curves were used without further modification as the characieristic points in question. As the theory shows, this method givesa closer approximation to the quantities required than the method by construction given in the former paper. But little weight, however, is to be attached to the superiority of this modification, as both methods lead to results which are identical to the fourth decimal place. Inasmuch as the present investigation was undertaken ex- pressly for the purpose of extending measurements as far as possible into the infra-red, we were compelled to use a com- paratively thick layer of air for reflecting the interfering beams of light, which brought the interference-bands in the spectrum very near together. It was quickly found, how- ever, that even the narrow width of the bolometer and the impurity of the spectrum, caused by the aberration of the lenses, placed a limit beyond which the further reduction of the breadth of the interference-bands could not be carried. With the feeble dispersion of the materials used, this limit was practically reached when the visible spectrum was crossed by seven or eight interference-bands, which gave a value to the constant K=2d cosz of about 8-54. According to this, the minimum of the first order, which is the farthest possible attainable point in the infra-red, has a wave-length A=8-5p. Then follow the maximum of the second order and the corre- sponding minimum, which have wave-lengths A=5°7p and A==4°3u respectively. Although the curvature of the curve of dispersion in this region is slight, it seems to us, neverthe- less, desirable to add, for greater accuracy in our measure- ments, other possible points to the small number already obtained. In order to attain this end, we found it advan- tageous to use not only the corrected positions of the maxima and minima and their corresponding wave-lengths for plotting the curve of dispersion, but also the points of intersection of the energy curve G=/(a) (see fig. 1) with the curve of mean energy R=/(«), since the wave-lengths corresponding to the abscissee of these points are easily calculated. This Rays of Great Wave-length in Rock-salt, Sylvite, §c. 39 latter curve might have been observed directly, had the distance between the plates enclosing the reflecting layer of air been sufficiently increased. This curve R=/f(a), which represents the distribution of energy when no interference is present, can be constructed, however, with sufficient accuracy, when at each point an ordinate is erected equal to the mean of the ordinates of the corresponding points of the enveloper, Pand Q. If the curve G=/(a) is intersected at any point by the curve R=/(a), then the amplitude for the abscissa of this point must have the same magnitude which it would have attained had a superposition of the energy of the two beams taken place without interference. The vibratory motion of the two beams whose amplitude and period are A and T' respectively, may be represented > the equations ; a y=Asin Qa 7 x) Ie =e Ygz= A sin 2a ( 2 gw i They unite to form the ray (K+ postr ect ca fyiN e an Tg e 1 a a Bee ETO T x ra a =2A sin™© sin 2 (4-2), It follows from what has been said above that, for the abscissa of the point of intersection of the two curves R and G, the amplitude of the beam Y, viz. 2A sin a must equal +A V2. dis accordingly determined from the equation sin as =+35 V2, wmK w 389 Sm (Qn+1)7 ee ee ae 2 where n is any whole number. The wave-length, therefore, of each point of intersection is given by the equation _ 4K ~ Qn+1: A knowledge of the order of the adjacent maxima and minima gives at once an interpretation to the quantity x. If 40 H. Rubens and B. W. Snow on the Refraction of the point of intersection in question lies in such a way that the adjacent minimum (mth order) lies on the side of the longer wave-lengths, and the adjacent maximum on the side of the shorter wave-lengths, then »=2m. - The introduction of these points in the calculation of the curve of dispersion made it possible for us to conduct the observations with interference-bands as broad aswerenecessary, and at the same time to obtain a sufficiently great number of points to enable us to ascertain the character of the curve of dispersion with nearly the same degree of accuracy as in those ee of the spectrum lying but little beyond the reach of the eye. At this point mention should be made of a peculiarity of the energy-curve, which may be observed in the drawing (fig. 1). The deflexions of the galvanometer, at the point of the last minimum a,,, not only sink to zero, but even assume negative values. The cause of this singularity, which also appears to a smaller degree in the energy-curve of fluorite, is to be found in the fact that the second unilluminated arm of the bolometer, which was placed in the apparatus within a casing of hard-rubber, notwithstanding this covering received upon its surface a greater amount of energy than the first arm, which was exposed to the direct radiation. The plausi- bility of this explanation is increased when we remember that the covered resistance is then at a portion of the spectrum in which the mean energy is 50 times greater than in the neighbourhood of the minimum ay, and that ebonite is not opaque to thermal radiation of great wave-length. In the following Table are found the results of the observed indices of refraction and wave-lengths. The first column, entitled “ Name,” gives the quality of the characteristic point in question, as Fraunhofer line, minimum (a), maximum (5), ‘or point of intersection (c) of the curves G and R; the second column contains the angle of deviation « as measured on tue graduated circle ; the third contains the index of refraction n, calculated from the refracting angle @ and the angle of deviation « according to the formula eee 2 =—$—=— - ing the fourth column contains finally the wave-length which is calculated from the order m of the interference-band and the constant K=2dcos?. The curve of dispersion plotted from the data of this Table is found in fig. 4,a. Rays of Great Wave-length in Rock-salt, Sylvite, Sc. 41 TABLE I. Refracting Angle of the Rock-salt Prism, 6=60° 2’. K=8°307p ; a, is 11th Order. Name. at, Ne Xr. titan 4 p. ae @ 37 15607 0-434 pe a 5g 15531 0-485 eee... | 7 15441 0-589 7 a 40 47 15404 0:656 a... 29 15370 0-755 a 222 15358 0-790 we. 164 15347 0-831 ER A... 114 15337 0:876 po... 7 15329 0-923 ts oe oe 4 15321 0-978 (a 39 58 15313 1-035 eile. n: 544 15305 1107 oe... al 15299 1186 Lao ATR 15293 1-277 sine A4 15286 1:384 ae Al 15280 1511 oe... 38 15275 1-660 (cee 35 15270 1-845 7 32 15264 2-076 Dee i. 28 15257 2:372 Annas Selesinciste-r's 223 1:5247 PATA oe . 18 15239 3-022 eee 133 15230 3:320 oie oe 7 15217 3:690 (ag ee 2 15208 4:150 a... 38 56 . 15197 A745 i ee 49 15184 5-540 Des... 373 15163 | 6-647 cn 4 15138 | 8:307 It is well known that Professor Langley*, by a method wholly different from the one here described, was able to follow the dispersion in rock-salt to a wave-length A=5-du. He found, in these experiments, that the curve of dispersion from about X=2yp on followed very nearly a straight line. Owing to the fact that even with the elaborate means at hand he was unable to extend measurements by his method farther than this in the direction of the long wave-lengths, he concluded to extend this straight line throughout the still more distant region of the infra-red in which his observations were taken. Many theoretical objections are at once suggested by so extensive an exterpolation. Among these criticisms may be * Ann. de Chim. et de Phys. [6] ix. p., 483 (1886). 42 HH. Rubens and B. W. Snow on the Refraction of mentioned one in particular, that, from a definite wave- length on, the indices of refraction would assume negative values, which points to an utter impossibility. There re- mained, however, the possibility that within the limits of Professor Langley’s measurements of energy, the straight line exterpolation gave results which were at least a first approxi- mation to the true value. A glance at the curve (fig. 4, a) shows, on the other hand, that in reality this is not the case. Indeed it is true that our own curve of dispersion tends toward a straight line until a point is reached almost as distant as A=5u; but at \=5y the curve begins gradually to lessen its inclination to the horizontal axis of wave-lengths ; and at N= 8yu the effect of this curvature is so considerable that a straight line exterpolation carried from A=5u on to this point would introduce an error in the determination of wave- length not less than lp. es In the following Table a comparison is made- between our results and those of Professor Langley. It is to be noticed that his curve, as far as this is plotted from his observations, agrees fairly well with our own, but that his values given by exterpolation differ widely from those observed by us, and that their difference increases as the wave-lengths become longer. There are also added here for completeness the data obtained from the previous paper. That an easier com- parison may be made with Langley’s figures, the wave-lengths selected increase by multiples of Ap>=0°589u. TaseE If, 3 : 7 i) ube a zs Wave-length. cancion (uuiene: i rane pret ey Be 1, X,,=0°589 | 15442 | 1:5441 1-5441 00001 2 — tie) Lbebl | 1-5300 1°5301 0 Se ion 1 O22 1:5269 15272 1) 4. d,=2856 | 15254 | @|° 1-253 15256 —0:0002 5. A, = 2945 | 15248 \ gs 15241 1-5240 +6°0003 6. ,=8'5384 | 15227 Sy 1°5227 15226 1 ke tla)» Sl -ozi5 |” 15214 1-5212 3 8. A,=4712 | 15201 1-5202 1°5200 1 SNe oS0l-: 1 5186 ) 1:5189 1:5188 —0:0002 10. 4,=5°890 | 151724 3 ie 15177 5 11. 4,=6-480 | 15158 | ¢ 1:5166 8 12. Ap=7070 | 15144 \'S 15157 18 13. Ap = 7°66 15129 | 2 15148 ten 14. ’p=S25.- | 15115 J > 1:5138 28 a i Rays of Great Wave-length in Rock-salt, Sylvite, §c. 43 The values, therefore, attributed by Professor Langley* to the wave-lengths in that region of the spectrum lying be- tween A=( and A=5y are undoubtedly correct. Beyond this limit, however, at least as far as X=8r3y, the values assumed are too small, but it is not impossible that when still greater wave-lengths are reached the sign of the error may change. ‘The results, nevertheless, of his observations remain of the greatest interest, since it will be easily possible to apply a correction to the wave-lengths as soon as the dispersion in rock-salt can be followed to sufficiently small indices of refraction. Sylvite. The behaviour of rock-salt is in every respect similar to that of the mineral sylvite, to which it stands in close chemical relation. There was placed at our disposal a prism of this material, 14 millim. at the base and 20 millim. in height. The surfaces of this prism were so well polished that the refracting angle could be determined to within 0°5 minute. In fig. 2 the observed galvanometer-defiexions are plotted as functions of the angular deviation of the arm of the bolo- meter. Hrom this curve is computed the table of dispersion in the manner described above. Corresponding to this is plotted the curve of dispersion (fig. 4, b). Tasxe IIT. Refracting Angle of the Prism of Sylvite, 6=59° 54’. K=8:022 3 a, is 10th Order. | Name. | a. N. r. Name. a n. r. J ae ee REY 2 | URE aE aS ore S| | pe Oh jul : Q 4 “& Hy ...| 387 30 1:5048 0:434 OR phe a1) 14766 1:458 a es ee 36 55 14981 0:486 UR xacase 23 | 14761 1:603 eee ste 133] 1:4800 0589 Dig asec 34 594) 1:4755 1-781 Crees 35 57 | 14868 | 0-656 Ge terae 564| 1:4749 | 2-005 Gy icles ol 1:4829 0:802 Greta ss 53 1:4742 2°291 Dips ac 32 14819 0°845 Gi Nitec 48 1-473: 2-673 Gi. Zi 1:4809 0°893 Op Seas 43 14722 3°209 (Di Seem 234 | 1:4802 0:944 CML 404} 14717 3561 Di donniss 20 1:4795 1:003 Gigineee sn 38 1:4712 4011 ee 164| 14789 | 1-070 || c, ...... 362) 1:-4708.| 4577 Oks winis«' 13 14782 1:145 ORR gi 32 14701 5345 Orettens 10 1:4776 1:234 Che tee 28 1-4693 6:412 ae 73| 14771 | 1387 || a, ..| 22 | 14681] 8022 * Langley, Sill. Journ. [8] xxxi. pp. 1-22, 1886; further [3] cai pp. 88-106, 1886, and [3] xxxviil. pp. 421-440; Phil. Mag. xxvi. p. 505, 1888. The same is true of t he paper of Angstrém, Ofversigt af Kongl. Vet.-Akad, Forhandl. ix. p. 549, 1889, and vii. p. 851, 1890, and W. Hi. Julius, Are? Néert, i, pp. 310-384, 1888. 44 H. Rubens and B. W. Snow on the Refraction of A study of this curve shows that the dispersion in sylvite, which in the visible spectrum is only slightly inferior to that in rock-salt, decreases in a similar manner but far more rapidly than in the latter mineral, so that at wave-length A=8y the dispersion is only about one third of the corresponding dispersion in rock-salt. Notwithstanding the great durability of this material, and its permanence in moist air as well as its almost perfect trans- parency to thermal radiations, the exceedingly rapid decrease in the dispersive power of sylvite renders this substance not so well adapted for experiments involving the use of prisms as rock-salt, whose surfaces are only with difficulty kept perfect. In the construction of condensing lenses this difficulty does not occur. Fluorite. The prism here examined is the same one which was used in the former investigation. The value of the refracting angle was redetermined and was found to agree very closely with the observations previously made. For a long time we tried in vain to measure beyond wave- length X=3'5 pw, the energy-spectrum produced by the fluorite prism. The results of the previous observations show the cause of our failure to be due to the fact that, after a region of comparatively feeble dispersion, the dispersive power of fluorite increases and the energy in this portion of the spec- trum becomes proportionally weaker. In order to make further advances, we were finally compelled to open wider the slit of the spectrometer at those places where the radiant energy sank below a measurable quantity. The repetition of this device enabled us to reach a wave-length in the infra-red greater than X=8y. In the curve shown in fig. 3, which represents the observed distribution of energy produced by the fluorite prism, the slit was twice opened ; the first time from 0:1 millim. to 0°4 millim. when the arm of the bolometer was at a deviation «=380° 10’, and a second time from 0:4 millim. to 1:0 millim. at an angle of deviation «=28° 50’. By this means the deflexions of the galvanometer were increased fourfold and tenfold respectively. Owing to the greatly increased dispersion and the corresponding increase in the breadth of the mterference-bands, this change in the width of the slit did not materially interfere with the sharp- ness of the bands in this region of the spectrum. Inasmuch as only one side of the slit was movable, a correction had to be applied to the reading of the arm of the bolometer when the slit was opened. : The distribution of energy, as shown in fig. 3, gives a curve whose character is wholly different from the representation of Rays of Great Wave-length in Rock-salt, Sylvite, §c. 45 the energy-spectra produced by rock-salt or sylvite, given in figs. 1 and 2. While in these latter the breadth of the interference-bands increases only slowly as the extreme infra- red is reached, amounting finally to hardly more than double the smallest value, the breadth of these bands varies in the energy-spectrum, as given by the fluorite prism, from 5 minutes to more than 24 degrees. Corresponding to this peculiar characteristic in the energy-spectrum of fluorite, the quality of the dispersion in this mineral is quite different from that of the materials previously considered. In the following Table, which contains these data, the indices of refraction are given only to three decimal places. As a result of the very considerable breadth of the interference- bands, it is impossible to locate the position of the cha- racteristic points with the precision attainable in other cases. TABLE LY. Refracting Angle of the Fluorite Prism, 6=59° 593’. K=8:070,; a, is 10th Order. Name. a. Ne Ar. Name. a nN. d. ay) ‘ie Qt le? Bly ees!) 32-5 1:43898 0:434. Getenne: 30 59 1:4267 1-466 de ered ol 52 1:43872 | 0°485 CU ass 554 | 1:4260 1613 Dee Be 36 1:4340 0-589 Oe 51 1:4250 1-792 Cie. 29 1:4325 0:656 Ca 46 1:4240 2-019 Cerin. 19 1:4307 0:807 OF ee 33 14224 | 2-303 Dats. iW 1:4303 O;850) iP aiicess: 29 1:4205 2°689 Open iia 142; 1:4299 0-896 Oana ire 14174 | 3:225 On ese 12 1:4294 0:950 Cie cee 29 46 14117 4°035 Ga easis 10 1:4290 1:009 Ouran 29 1-408 4°62 i ee 8 1:4286 1-076 Oh eipons 4 1:403 5°38 Grosses-| 6 14281 L152 OR ihe 28 30 1°396 6:46 Bit ate 4 14277 AO RE ae 8 eel oe 1:378 8:07 Gros 2 14272 | 1:345 | The curve of dispersion, shown in fig. 4, ¢, exhibits more graphically than this table the peculiar character of the dis- persion. From this it is seen that the dispersive power of fivorite decreases as far as A=2 w and then gradually increases, reaching at X=8y a value only slightly inferior to the value of the dispersion in the red. Compared with rock-salt and syivite, the dispersion of fluorite in the visible spectrum is exceedingly small and unusually great in the infra-red; so that this material is peculiarly well adapted to the production of prismatic heat- spectra, an advantage which is still further increased by the ease with which it can be worked and by the permanence of its surface in the air. Physical Laboratory, University of Berlin, June 1892, lia a ILI. Notes on the Construction of a Colour Map. By WAuTER Batty, M.A.* iL is my paper on this subject, read before the Physical Society on April 8 last}, in discussing the method of plotting out the curve giving the mixtures of two spectrum colours, I stated that points in the curve lying in the ab- normal or imaginary regions could not be determined by experiment. This I now find is a mistake. Let 8, and 8, be spectrum colours, of which the mixtures are to be represented by points on the curve. The part of the curve lying in the imaginary and abnormal regions is obtained by subtracting light of one colour from light of the other colour, and equating the resulting colour to the mixture (if I may use the expression) obtained by subtracting white from some other spectrum colour 8S. We have MS, —mS.=S—aw. This equation does not represent any possible physical ex- periment, but it may be transformed, without altering the value of any of the quantities, into S) + Ngo = Ri + aw. This last equation means :—Make a colour-patch of 8 and S,, and a colour-patch of 8; and W, and vary the quantities of 8), S:, and W until the two patches are similar in colour, and then measure the quantity of white. A line drawn to the left from the position of 8, and proportional in length to the quantity of white, will define the position of the required point in the curve. 2. In the map the region on the right of the line of spec- trum colours is occupied by all the colours obtained by mixing spectrum colours and white. I suggest that this should be called the Spectral Region. The equation. for determining points on the mixture curves in the Spectral Region is nS + NoSo= S +auW. The region to the left of the abnormal and imaginary regions is occupied by colours complementary to those in the Spectral Region. I suggest that this should be called the Complementary Region. The equation for determining points * Communicated by the Physical Society: read October 28, 1892. t+ Phil. Mag. June 1892, p. 496. Mountain-Sickness ; and Power and Endurance. AZ on the mixture curves in the Complementary Region is Ss =e nS, + Noe =cW. The equation for determining points on the mixture curves in the Imaginary and Abnormal! Regions has just been shown to be (for one part of the curve) s + Nye = N94 + aW, and it is obvious that for the other part it will be S -- nS, Vise + aW. 8. In defining a colour as compounded of a spectrum colour and white, we have to determine both quality and quantity of the white light. A colour may be defined by three spectrum colours by means of the equation 29; + Ngdo=nz383+aW, or of the equation N94 + Nee + N33 =avW. The colour is that obtained when a patch formed in ac- cordance with one side of the equation is made identical with a patch formed in accordance with the other. In this case quantity of white need not be defined, but quality must be defined. If a colour be defined by four spectrum colours the defini- tion is independent of any convention as to the quality of white light. Let 8,, S:, 83, 8, be four spectrum colours whose waye-lengths are in oer of magnitude, then the equation 19, +7393 = Ngdeot+ 484 defines a certain colour, which can be obtained by making a patch of S, and $3 identical in colour with one of S, and 8, TV. Mountain-Sickness ; and Power and Endurance. By R. H. M. Bosanquet, /.A.S.* HE account of mountain-sickness at great altitudes, given in Mr. Whymper’s work, ‘Travels amongst the Great Andes of the Equator,’ is of great interest. On reading it, it appeared to me to suggest a simple explanation of the occurrence of mountain-sickness under the circumstances * Communicated by the Author, 48 Mr. R. H. M. Bosanquet on Mountain-Sickness ; narrated, an explanation consistent with all the facts, inclu- ding the immunity enjoyed by Mr. Perring (p.51). Ithought the matter too plain for publication. But the appearance of Mr. Dent’s article in the ‘ Nineteenth Century’ (Oct. 1892), “Can Mount Everest be ascended?” shows that my point of view has escaped notice. This appears at once from the remark at p. 611: “ Men of large vital capacity, with large bones and full-blooded, are the best suited [for the ascent of the highest mountains].’? So far as mountain-sickness of the great-altitude type is concerned, this is certainly not true without qualification : the case of Mr. Perring above alluded to is in point. The body may be compared to a steam-engine and boiler, the food-arrangements being paralleled by a mechanical stoker, such that the supply of fuel can be fed into the reservoir of the stoker in lump quantities, as food is fed into the stomach at meals. The digestion and other internal arrangements, which we may speak of as the “internal feed,” pass this on into the place of combustion just as a mechanical stoker does fuel. When food is regularly taken, the internal feed will supply the combustion within the body at a more or less con- stant rate, not depending on any voluntary action at the moment, but depending on the constitution, on the average amount of food taken at meals, and probably on the efficiency or wastefulness of the internal feed. The rate of the internal feed must vary enormously in different persons. In men “of large vital capacity, ...and full-blooded,” it will generally be very much larger than in persons of small vital capacity. Now we can easily suppose an internal feed so copious as to approach, in its requirement of oxygen for its proper combustion, the possible supply afforded by the breathing mechanism. And my suggestion is simply that in eases of great-altitude mountain-sickness, such as Mr. Whymper relates, the diminution of the air-supply reaches a point at which there is not enough oxygen for the consumption of the fuel continually brought forward by the internal feed. Of course, so long as this is the case, disturbance of the system is to be expected from the accumulation of the reducing (oxygen-devouring) substances furnished by the internal feed to the blood. Under these circumstances, food would probably not be taken for a time; the internal feed would after a time be reduced ; and an equilibrium of the system set up again founded on a reduced food consumption. And this is precisely wuat happened, according to Mr. Whymper’s account. ‘and Power and Endurance. 49 On the other hand, Mr. Perring, “rather a debilitated man, and distinctly less robust than ourselves” (p. 51), escaped the sickness. According to my view, the food-supply his system was dealing with was not in excess of what could easily be consumed by the air he breathed, even at the reduced density. According to this view, while the artificial supply of oxygen advocated by some investigators should be able to give relief, if the oxygen could be got to its work, yet the obvious course is to attack the other element; and by a judicious preliminary course of moderate starvation, combined with light work, to endeavour to bring the system into the required condition of reduced fuel consumption—in fact into the condition at which it arrived in Mr. Whymper’s case, through the painful path of the attack of mountain-sickness. So far I have spoken of what may be ealled “ great-alti- tude ” mountain-sickness. As to the more ordinary form, I am sorry to say I was at one time a sufferer. Hxperience enabled me to overcome it by adopting a slow uniform mea- sured pace. But, after the disappearance of the agility of youth, for some seasons I always suffered in my first expedi- tions, even at quite moderate elevations. And I have no doubt whatever that it was due to the system being over- tasked ; that is to say, when I was endeavouring to do some- thing like, say, ;4; of a horse-power for a time far longer than I was capable of, I collapsed, probably not being capable of doing more than, say, 3!, of a horse-power for any con- siderable time, at all events when out of training. So far I have avoided going into numerical details, as they are not necessary for the general explanation, and they open up an exceedingly wide subject. But I propose now to deal shortly with certain relations of the external work which can be performed by men; this is conveniently reckoned in terms of ‘ horse-power.”’ One “‘horse-power” is commonly defined as 550 footpounds per second, without qualification. When recently horses were replaced by electric motors on certain tramways, it was gene- rally considered a surprise that motors of about 35 H.P., as above defined, were required to replace the horses. ‘The explanation is that the 550 footpounds per second definition was based on the average effort that horses could exert for a considerable time. ‘The output of power of a horse on such occas’ons as drawing a load up a sharp hill must be quite ten times a nominal horse-power. And the machine is required to be able to replace the greatest effort of which, say, 3 horses are capable. Phil. Mag. 8. 5. Vol. 35. No. 212. Jan. 1893. K 50 Mr. R. H. M. Bosanquet on Mountain-Sickness ; Similarly, consider a man weighing 12 stone. According to a well-known mountaineering datum, he may lift his wel ght 1000 feet per hour for many hours. Under. these cireum- stances he is doing about +4, of a nominal horse-power. Certain experiments on the treadmill gave § horse-power external work, maintained: for 34 hours. soe But any ordinary person can do-a whole horse-power, if the time of the effort be short enough. Take a man weighing 12 stone=168 lb. If he raise his weight a little over 3 feet per second, he is doing a horse-power of work. (For 550/168 = 3°27, or a little more than 34.) Now any ordinary person who can run upstairs two steps at a time can do this easily for a few seconds, and an active person for longer, but the duration of the effort will not easily exceed a certain fraction of a minute. Further, active people can do 2 horse-power, running upstairs at the rate of 64 feet of ascent per second, for a very few seconds. It appears, therefore, that the power a man is capable of exerting depends on the duration of the effort. The following (p. 51) are a few data I have selected as the basis for a numerical law. The law adopted is that the time of duration of effort (or the “ endurance’’) varies inversely as the cube of the power exerted, supposed uniform. Or, conversely, that the power which can be exerted for a given time varies inversely as the cube root of the time (or of the “ endurance’’). Of course the numbers here given can only be rough approximations to an average; and we need not be surprised if we find wide divergences in isolated cases. While the correspondence of the calculated times with the estimates is not in all cases close, the discrepancies are in opposite directions. Further, any considerable change in the assumed law would tend to make the calculated numbers impossible in the one direction or the other. Thus, if we took the fourth power instead of the cube, it would make the tasks at the bottom easier, and that at the top impossible or nearly so, and vice versa if we took the square instead of the cube. The treadmill datum has been taken as the starting-point, the calculated endurances of the other cases being derived by multiplying 34 hours by the cubes of the inverse ratios of H.P. It must be noted that we do not know the average weight of Leslie Stephen’s party. I have assumed that this was 12 stone. If not, a correction will be required. It will be seen that their actual endurance appears greatly to exceed oe and Power and Endurance. ae ae . | on | Estimated © . Nature of Data. Exact. H.P. ae Cee | ieee sich Sut eras. a | | | Mountaineer’s rule of 1000 feet per hour. Esti- | | O85 We | 1]h gm 10h mated endurance, say 10 hours ....... Seas 4 | Leslie Stephen : Dom from Randa. 10,000 feet 105 ce 5h 54s | Sh NOL co), LKOTTNTS a ( Jem ess Beet 0 oie ole yea ane a be: a Datum from treadmill, quoted from Smith by | | = Frankland (Chem. Journ. 1868, p. “a = + 33> (datum). 35° Reduced by me to English units ........ | 1 H.P. exerted by ascending at rate of 3:27 feet 1 9456 _ Fraction of per second fo some fraction of a minute ee | minute. 2 H.P. exerted by mena at rate of 64 feet 9 28.8 Few seconds. per second for few seconds.............. iG hows | ie ee iy eae NS 2 is nae Vink eer teem bei ie ia ee kes Pe, cea Ie hale eS aly Ae ee 52 Dr. W. Pole on Colour-Blindness. that indicated by the law for the power developed. If the average weight were much less the discrepancy would be lessened. But I think I remember seeing Leslie Stephen described somewhere as “the fleetest-footed of all the Alpine brotherhood ;” so that probably his party might be expected to show an endurance in excess of the average, at a high speed of ascent. The bearing of these considerations on the use of such an expression as “horse-power ” is important. However con- venient it may be asa short name for 550 ft.lbs. per sec., it is clear that no specification of ft.lbs. per sec. can really repre- sent the work of any animal, unless the endurance, or the time for which that power can be maintained, is also specified, and the law connecting the two is known. V. Further Data on Colour-blindness.—No. ILI. By Dr. Wiuttam Poe, F.R.S.* Professor von Hetmuoutz’s Handbook of Physiological Optics. F all the names that could be mentioned as authorities on the subject. of colour-blindness, probably that of von Helmholtz stands the highest, not only from the asso- ciation of his name with that of Young in the most popular theory of colour-vision, but more especially on account of his monumental Handbuch der Phystologischen Optik, which has acquired a classical celebrity. This work appeared at inter- vals from 1856 to 1866 ; but scientific knowledge advances much in a quarter of a century, and the learned author is conferring a great boon on the public by giving them a new edition, thoroughly revised and brought up to date. To make it more accessible it is published in separate “ Liefer- ungen,” of which seven have appeared, comprising 560 closely printed large octavo pages. I have been surprised to find how little this new edition is known in Hngland ; and as the part treating of colour- blindness is already out, it would be culpable, in offering data on this subject, to omit reference to it, particularly as one of the special objects of this Magazine has always been to call the attention of the English-reading scientific world to important foreign publications. The subject mentioned forms, indeed, but a minute item in the whole treatise ; but * Communicated by the Author. Dr. W. Pole on ColourBlindness. oe “ex. pede Herculem,’ and I may claim a more extensive discipleship under the great master in another branch of his labours. . The description of colour-blindness which Helmholtz gave in the old edition is so well known that it is only necessary to reter to a few passages bearing on our comparisons with the new one. The author stated (p. 294) that the patients saw in the spectrum only two colours, which they for the most part called blue and yellow, and he mentioned experi- ments on a patient tried by himself, which proved that for this person’s eyesight all colours could be compounded by mixtures of yellow and blue. He then explained how, on Grassmann’s principles of colour mixtures, ‘‘ for an eye which acknowledges trichromic matches, but which confuses red with green, it follows that all the hues which it especially distinguishes may be compounded of two other colours some- thing like (etwa) yellow and blue.” . | The author, however, in further explanation, pointed out why he believed that yellow and blue might not. be the colour-sensations really experienced. He said, p. 297 :— In the Young hypothesis the colour invisible to the colour- blind eye could naturally be only one of the fundamental colours, Red-blindness would thus be explained on Young’s hypo- thesis by a paralysis of the red-perceiving nerves ..... and it follows from this that the red-blind perceive only green, violet, and their mixture, blue. He also (p. 299) mentioned another class, in regard to whom “it might be conjectured (kann man vermuthen) that their defect lay in an insensitiveness of the green-perceiving nerves.” These passages, it will be seen, contain the essence of the original application of Young’s theory to dichromic vision, which became so popular. We now turn to the new edition; and as it is matter of common knowledge that, in the interval of time since the previous publication, the applicability of the hypothesis re- ferred to has been seriously questioned, we look with interest to what is said now on the matter. We may take it up at page 362, where we find a mathe- matical investigation by geometry and algebra, to show that if two colours, R and G, appear alike to the colour-blind, there may be found another colour which, though visible to the normal eye, is invisible to them. All this is just as it stands in the old edition ; but now we come to the first change of importance. The author, at the end of the investi- gation, adds a new passage as follows : 54 Dr. W. Pole on Colour-Blindness. But it is not hereby excluded that this wanting colour might -also be wanting to. the normal eye, and its weight = 0. That would mean that two of the fundamental sensations of the normal eye would, to the colour-blind person, be excited to equal strength by all exciting causes. In fact, it has recently become probable that the solution of the enigma is to be sought in this direction. The older attempts to explain colour-blindness proceeded from the first-named assumption, that one of the fundamental sensa- tions was wanting to dichromic eyes. I myself have adopted this in the first edition of this hand-book*. ins} _ As Helmholtz is not a person to use language incon- siderately in such a case as this, we may gather much information from this short passage. In the first place he makes it clear that the original hypothesis was not in- tended as a positive and definite explanation. It was only an “attempt to explain,” and it is now characterized as “alt ” (old), a word which, as I understand it, does not here mean simply early in time, but carries with it the idea of “aged,” “ancient,” “antique,” ‘stale,’ something superseded by “new.” The expression often recurs with clearly this meaning. Then the explanation of colour-blindness is called an “enigma’”’ ; it is still obscure, and wanting “ solution.” _And thirdly, the passage states that in consequence of some recent events a new solution has become probable in a certain direction. The recent events alluded to have been clearly the more complete evidence acquired as to the facts of dichromic vision ; and the new solution, which indeed is already indicated, will be better explained by and by. _ It is difficult to construe all this otherwise than as intimating that the author does not now attach much weight to the former explanation, and we shall find, farther on, abundant confirmation of this interpretation. He, however, thinks it right to reprint the part which -contains the “ tilteren Hrklirungsversuche,” but he adds now the following new saving clause (p. 366). | Nevertheless (¢mmerhin), as it appears doubtful what sensations of the normal eye correspond to the two colour sensations of the dichromic patients, Donders has recommended that, according to * The important original passages are as follows :— “Das wurde heissen, dass zwei der Grundempfindungen des normalen Auges dem Farbenblinden durch alle Reizmittel gleich stark erregt wurden. In der That ist es neuerdings wahrscheinlich geworden, dass in dieser Richtung die Lésung des Riithsels zu suchen ist. “ Die alteren Erklirungsversuche der Farbenblindheit gingen von der erstgenannten Annahme aus, dass den dichromatischen Augen eine der Grundempfindungen fehlte. Ich habe dies in der ersten Auflage dieses Handbuchs selbst angenommen,” . Dr. W. Pole on Colour-Blindness. Da the customary expression of painters, the colour corresponding to the red or less retrangible halt of the spectrum should be called the warm colour, and that of the blue half the cold colour; and we will do so in what follows. At pages 367-8 he remarks on the distinction of the classes of “ red-blind ” and “ green-blind,” but more positive opinions are given later. At pages 368 and 369 we come upon the “ new ”’ explana- tion of colour-blindness already alluded to. The idea of this appears to have arisen with Helmholtz himself at a very early period. In 1860 Edmund Rose pointed out the diffi- culty of Young’s original explanation, stating that after eareful examination of 59 colour-blind patients, he found it irreconcilable with the facts observed. In 1867, when the last portions of Helmholtz’s work appeared, he noticed Rose’s experiments, admitting as an alternative suggestion (p. 848), that “in the case of the congenital colour-blind it might well be imagined that the activity of the nerve-fibres might not be removed, but that the intensity curves of the three kinds of light-sensitive elements might change, whereby a much greater variability in the effect of objective colours on the eye might enter” *, Leber, in 1873, expanded the idea and put it into a practical form. The great difficulty had been the continually increasing evidence that the warm sensation of the colour-blind corre- sponded with the normal yellow, and not with red or green as the Young explanation would require ; and Leber pointed out that if, instead of abolishing the red or the green element, the two were assumed, by changes in their intensity curves, to coincide, forming yellow, the whole difficulty would vanish. This explanation was afterwards repeated by . Fick, and at a later time, 1886, reproduced by Konig in his communication to the British Association. Helmholtz takes this up in his new edition apparently with approval, and much matter will be found bearing on it in pages 368 and following, and again at page 376. He thinks that if the green curve has gone over to the red, it will produce the sensations of the “ green-blind”; but if the red curve has gone over to the green, it will produce those of the “ red-blind,” there being, however, less frequent inter- mediate degrees between the two extremes. In pages 372 to 374 he applies the same explanation (as Fick had done) to the colour phenomena of the normal * The new explanation is always ascribed to Leber; this clear antici- pation of it by Helmholtz seems hitherto to have escaped attention, even by Dr. Konig, 56 Dr. W. Pole on Colour-Blindness. retina, and alludes to the analogy between these and colour- blindness. . : - Helmholtz thinks it right to devote considerable space (pages 376 to 382) to the discussion of the theory of Hering. He considers it a modification of Young’s theory, giving a long description of it, illustrated by mathematical formule, and he says it will explain the facts of colour combinations as well as, but not better than, Young’s theory. Then follows much controversial, matter, founded on arguments and state- ments by Hering, but very little of which affects the question of colour-blindness. The most important novelty in Helmholtz’s second edition is contained in section 21, on The Intensity of the Sensation of Light. This section is a long one, extending over nearly 100 pages ; and a large portion of it, 2. e. from pages 401 to 473, is entirely new. It contains a most elaborate essay on “ Helligkeit,’ a word for which we have no perfect equi- valent, but which is generally rendered hy “brightness” or “luminosity.” The matter is principally devoted to the relations between “ Helligkeit”’ and colour, which appear to be exceedingly complicated and difficult ; so much so, indeed, that Helmholtz, with the modesty that so often accompanies great knowledge, expresses distrust of his power to. deal satisfactorily with them. 3 _ Fortunately, however, we have no occasion to speak of these relations, further than as they are connected with an entirely new determination of the three fundamental colowr-sensations, by a method in which “ Helligkeit” (which for this purpose I translate as “luminosity”’) takes a part. This investigation may be said to begin on page 444, with a dissertation, “On the relations between Sensitiveness to Colour and Sensitive- ness to Luminosity.” The author raises the question how far observations on the spectral colours, having these elements in view, will bear on the nature of the three physiological colour- sensations, and having satisfied himself on this point he undertakes the investigation. I can only give (and it would not be right to do more) the barest outline of this interesting but difficult and complicated problem. It adopts in the first place the view of the funda- mental sensations applied shortly before by Kénig and Die- tericl in attempting a similar inquiry. They had analysed the spectral hues by a great mass of experiments, using three “ Hlemental colours” R, G, V, taken from the two ends and the middle of the spectrum, by combinations of which every other spectral hue could be produced. These, on the Dr. W. Pole on Colour-Blindness. 57 old plan, would have been called the primary colours ; but here they were only considered as preliminary elements ; the new fundamental colours, say w, y, and z, being dependent on them and connected with them by linear equations : thus e=a,.R+b,.G4+¢.V, y=a,.R+b,.G+¢, .V, , z=a3;.R+b;.G+e;.V. The nine coefficients having to be hereafter determined, making, in each line, at+tb+e=l1. To arrive at these constants appears the cruz of the problem, it being necessary for this purpose to enter into the investi- gation regarding the colour and luminosity relations before referred to. ‘The quantities dH,, dE, and dH; are taken to represent the magnitudes of the differential perceptions for the elementary observations, and dE is the magnitude of the difference in the colour resulting therefrom. This latter quantity had to be expressed in terms of x, y, and z, and for this purpose the following formula was arrived at (p. 453) :— oh a/( ak wy +(2 dy = =) Lic eld ae ko V3 ean Vy GN) Xd aN 2 aN ee aan) , where \ = wave-length, 6\ = a certain mean error, and ka constant found by multiplied observations. This equation has to do with the sensitiveness to colour. With the aid of the constants, having given an observation of the values of R, G, and V, at any wave-length, the values of #2, y, and z may also be found, and the constants must be such that dH, determined by the above equation, shall be equal, or nearly so, at all points of the spectrum. Having got this constant value of dH, it has then to be compared with the equation for dH arrived at in a different way, from dH,, dy, and ds, viz. Qi hi nel A/ a where ¢ is a certain very small fraction, also arrived at by observation. This second value of dE has to do with the sensitiveness to luminosity. And if the two values are equal or nearly so, the calculation may be considered justified. ines uns ih 2 . * Probably this is a misprint for—. The book unfortunately contains several typographical errors, 58 Dr. W. Pole on Colour-Blindness. The most suitable constants were found to be, in round numbers, | x=0°'80.R—0°35 .G+0°55 .V, y=0°26.R+035 .G+0°39 .V, 2=0:25.R+0:125.G+0°625. VY, where R, G, and V represent the quantities of each elemental colour in a given spectral hue. _ To carry out the calculations, an immense number of obser- vations were collected on the various spectral colours (some 50 on each hue), determining the proportions of R, G, and V in each colour. For example: at w.l. 520, the green hue was found to be made up of A:62 of R+8:45 of G+1°:10 of V; then, applying the above equations to these figures, the pro- portions of the three fundamental colours contained in this hue of the spectrum were found to be 1:37 of #+4°51 of y+2°90 of 2. Or in 100 parts of the green, | 15 of #+51 of y+ 384 of <. This being done for many points along the spectrum, and the comparisons being satisfactory, the fundamental colours can be laid down in a triangle, and their relations with the spectrum shown in a geometrical form. The results will be found in the tables on pages 454 and 455 and in the diagram on page 457, The three newly-found fundamental colours are, generally speaking, red, green, and blue; but all very much more highly saturated than anything in the spectrum. : The Red, x, is a highly saturated carmine-red, more tending to blue than the extreme red of the spectrum. The Green, y, is a yellow-green about w.l. 560, somewhat greener than the complement to violet, and nearly corre- sponding to the green of vegetation. The Blue, z, is about w.l. 482, corresponding to ultra- marine. The author states that the fundamental red and blue cor- respond with Hering’s anticipations (Vermuthungen) ; and I may be allowed to say that the former agrees with my deter- mination of my own wanting colour in 1856, before any one suspected the existence of an extra-spectral fundamental. The following short table, which I have made out from the diagrams, tables, and formulee, will show, in a simple manner, Dr. W. Pole on Celour-Blindness. - 59 the percentages of the “ Urfarben,” 2, y, and z, contained in some of the chief hues of the spectrum. Wave- ‘lengths. ce y: i ee i ends «hi 61 6) A Se MOAN PE e005. .6s e052: eee OOO a Ve Ete 00) 28 kee eee 580 36 30 thle hoo Shida) | 22 2h eemRee ee 520 i) D1 34 ln. 480 31 29 40 RA OICUMER aac. av aec tenner: end. 539) 25 40 Tits a re aio 830 ul nae If we apply to these quantities the principle that a mixture of equal proportions of the three fundamental colours will make white, we may form an idea of the enormous vrade of saturation of the ideal fundamental colours, compared with that of the spectral hues. For example, spectral red will contain 42 parts of w, 1 part of y, and 57 of white; spectral yellow will contain 11 parts of w, 14 of y, and 75 of white; spectral blue will contain 2 parts of a, 11 parts of z, and 87 parts of white. This is a somewhat astounding idea; but a glance at the diagram on page 407 will show it is what the author intends. The author points out that all simple colours excite the three nerve-elements simultaneously, and with only moderate distinctions of intensity ; facts for which there are analogous phenomena in the known photochemical effects of photo- graphy. This brief account gives a very vague idea of the skill and labour that has been embodied in the work referred to; and, considering the entire novelty and difficulty of the attempt, the acuteness of the logical reasoning required, and the complicated nature of the relations involved, I should venture to say it may be pointed to as one of the most striking examples of the application of high mathematics to physio- logical research. — But it may be asked, What immediate connexion has this with Colour-blindness ? . The author has himself answered the 60 - Dr. W. Pole on Colour-Blindness. question by immediately going on, page 408, to a further investigation, entitled “ Comparison with Dichromic Eyes.” He begins with the remark that the fundamental colours he has found do not coincide with those which K6nig and Dieterici had deduced from the comparison of colour-blind eyes with normal ones, and which he had himself quoted in former parts of this work. They had arrived at pretty nearly the same hues of red and blue, but their third fundamental, green, differed materially, and the intensities were very different in all. Helmholtz takes some pains to explain and comment on ihis, showing that the discrepancy is due to the attempt made by Konig and Dieterici to apply the “old” assumption that dichromic vision was simply caused by the absence of one of the fundamental excitements of the trichromie eye. He mentions that this assumption originated with Young, and was, at an earlier period, accepted by most of the adapters of the theory, including himself and Hering, as well as Konig and Dieterici, and he thereby gives a good defence for their zealous endeavours, but at the same time he leaves no doubt that this assumption has vitiated their results. As a further proof of this he cites (p. 461) the determina- tion by Konig and Dieterici of the colours wanting to the red and green blind respectively, according to the funda- mental colours chosen by them ; and he shows that when the newly found fundamentals are substituted, such a determina- tion leads to irrational results, giving negative values ; whereas (p. 460) Young’s hypothesis only allows positive values of the physiologically possible colours. Considering therefore, apparently, the old assumption as now proved intractable, he goes on to explain that a more general hypothesis respecting the existence of dichromatism may be found, in which the necessity ceases that the missing colour should be one of the fundamentals *. * The following are the original words :—‘‘ Die hier gefundenen Grund- farben stimmen nicht mit denen iiberein, welche die Hrn. A. Kénig und C. Dieterici aus der Vergleichung farbenblinder Augen mit normal- sichtigen hergeleitet haben. Nur die besondere, von Th. Young ausge- gwangene und von den meisten Bearbeitern der Theorie, auch von mir selbst, von E. Hering, A. Konig, und C. Dieterici friher angenommene Erklarungsweise, dass bei den Dichromaten einfach eine der Grund- erregungen des trichromatischen Auges nicht zu Stande komme, tritt in Widerspruch mit dem bezeichneten Ergebniss. “ Aber es ist eine allgemeinere Hypothese tiber das Wesen der Dichro- masie moglich, bei welcher die Nothwendigkeit aufhort, dass die fehlende Farbe eine der Grundfarben sei, und doch die Regel festgehalten wird dass alle Farbenpaare, welche fur das normale trichromatische Auge gleich aussehen, auch fiir das dichromatische gleich aussehend bleiben.” Dr. W. Pole on Colour-Blindness. 61 He first shows the possibility of this by a simple example. Suppose, he says, that the rays which ordinarily excite the green sensation do not excite the green sensitive nerves, but do continue to excite the red and blue ones. The eye would become dichromie, and according to the old explanation would see only red and blue. But these two sensations will not be the same as the trichromic red and blue, in which the green element forms part; and further, it is possible that the green nerves, though not excited by the green rays, might retain their former excitability by the red and blue ones,—in which case the dichromic colours would be a certain kind of yellow and blue. The author then explains (pages 458 to 461) his “Adlge- meinere Form der Dichronvasie.” First, by algebraical reasoning. If 2, y, and z represent the three fundamental colour-sensations in the normal eye, and X, Y, Z the three in the dichromic eve, then, as all matches for the former are also good for the latter, X, Y, Z must be linear functions of w, y, z, and the following equations are arrived at, namely :-— O=aX+BY+yZ. Xp U + poy + p32. Y= qe t+ Qey + 932 L=aX+bY. The result being that the whole colour value of the dichromic eye appears as a mixture, in variable proportion, of two definite compound colours, X and Y. Another explanation is given by geometry, in which the author uses a more comprehensive mode than the ordinary plane diagrams. He adopts Lambert’s plan of geomecry of three dimensions. ‘The values of the three trichromic funda- mentals wv, y, z, are used as rectangular coordinates, by which may be formed an imaginary parallelopipedon (like a brick whose three dimensions 9 x 44 x 3 will represent w, y, and z respectively) : then the extreme corner most distant from the origin of the coordinates will represent the place of the com- pounded colour ; the length of the diagonal line drawn _be- tween these two points will represent the quantity of the colour, and its direction will represent the hue. Planes may be also drawn intersecting the figure, which will represent the ordi- nary plane colour-diagrams, and will serve as the bases of ‘Lambert pyramids,” containing all the colours physiologi- cally possible. It is shown that, under the conditions of dichromatism, the resulting planes will each be uniformly 62 Dr. W. Pole on Colour-Blindness. coloured, and the trichromic variety of hues will no longer exist. This more general theory of dichromatism appears, so far as I can understand it, to amount to the view that while the two dichromic hues must be in some way derived from the three fundamental colours of normal vision, there is no necessary condition as to the manner of their derivation, or as to what they shall be*. The author, further, in regard to his new theory, calls attention to a point of considerable importance. One of the greatest stones of stumbling for years past has been the division, consequent on the “old” explanation, of dichromic patients into the two theoretically distinct classes of “ red- blind”? and “ green-blind.” It is obvious that this division naturally disappears when the old explanation is abandoned ; but Helmholtz takes pains to show geometrically that his new theory gives no place for such a division. And he, moreover, expresses the opinion that such a division does not seem to have been fully justified by observation. He adds, ‘‘ By this it is also shown that the want of corre- spondence between the absent colour of the dichromic system and one of the fundamental colours found by us, does not in- volve any insoluble contradiction f. It is not my business to offer any comments on the views I have endeavoured (imperfectly I fear) to call attention to ; I have only to repeat the reference to the original for fuller information regarding them. But even though there should be differences of opinion on minor points, there can be none as to the character of the work or the position of its author among the great men of the age. Atheneum Club, $.W., December, 1892. * Only it would seem that as the dichromic eye now loses nothing, but uses the whole of the three fundamentals and no more, and as their sum makes normal white, then the total sum of the dichromic vision must make normal white also, and the two hues, X and Y, will be complementary.—W. P. t On account of the great importance of these two expressions of opinion, I subjoin Helmholtz’s own words (page 461) :—“In unseren Betrachtungen ist keinerlei Beschrankung fiir die Lage der Schnitt- punktes gegeben. Daher fallt bei dieser Verallgemeinerung der Theorie der Dichromasie auch die Trennung in zwei scharf getrennte Klassen, Griinblinde und Rothblinde, weg, welche ja auch den Beobachtungen gegentiber nicht ganz gesichert erscheint. “Damit ist auch nachgewiesen, dass der Mangel an Ueberstimmung zwischen der fehlenden Farbe der dichromatischen Systeme und je einer der von aus gefundenen Grundfarben keinen unléslichen Widerspruch einschliesst.” : . E 63oc VI. A New Method of treating Correlated Averages. By Professor F. Y. Epcuworta, M.A., D.C.L.* oo following is a simpler method of solving one of the problems treated in a former paper relating to correlated averagest. Taking the case of three variables for conve- nience of enunciation, let us put for the exponent (of the expression for the probability that any particular values of the variables will be associated) R= aa? + by? + cz" + 2fyz + 2gaz + 2hay. And let it be required to determine the coefficients a, b, ¢, &e. The most probable values of y and z corresponding to any assigned value of x, say w’, are deduced from the equations by +fethe’ =0, : Lezt+fy+tgu =0. The values of y and z determined from these equations may indeed diverge widely from the particular values corresponding in any one specimen to vw’. But if we take a number of specimens, it becomes more true ft that bSy+fSz+hda’=0, eSze +/Sy + 9a’ =0. Dividing each equation by the sum of the assigned values +2’, we have ee +/Pi3 +4=0, CPs t+fpitg=0 5 where pj2, p13 Mean (as in the former paper) the coefficients of correlation pertaining to each couple of organs (Mr. Galton’s 7). By similarly assegneng values of y and of z, and observing the associated values of the other variables, we obtain six (in general n(n—1)) equations for the sought coefficients a, b,...g, 4; which, being rearranged, are as follows :— Prttp3g+t h=0, pitt g+po3h=0 ; 230+ baa sh — protpaft h=0; puctprft g=9, poset ftppg=0. * Communicated by the Author. Tt Phil. Mag. August 1892. } Cf loc. cit, p. 191 et seg. 64 A New Method of Treating Correlated Averages. A solution of this system is afforded by putting a, b, ¢ each proportional to one of the principal minors, and f, q, h each to a certain one of the other three minors, of the following determinant :— JL P12) P3is | P12) 1 P235 r+] P3i P2395 1, : For call the three minors formed by omitting successively each constituent in the first row a, h, g. By a well-known theorem ™*, if each of these minors is multiplied by the corre- sponding constituent in the rows other than the first, the sum of these products=0. That is Pritt h+ po23g¢=0 P31 + po3h + g=0 Thus the first two of the above-written six equations are satisfied. By parity of reasoning, if we put, for 0, the princi- pal minor b, for c, ec, and, for 7, the minor f, obtained by omitting the row and column containing (either) p3, the remaining four equations are satisfied. ‘The proposed system of proportional values is therefore a solution. And since the equations are simple, it is the solution. We have thus obtained by a simpler method than before the solution of the problemy: given the values of some of the variables, what are the most probable values of the other variables? For the proportionate values of the coefficients a, b,...g, h having been ascertained, we have only to sub- stitute in R the given values of one or more variables, e. g. z'; and for the most probable values of the remaining vari- ables we have the equations erage, But we have not obtained a solution of the second problem f: given the values of some of the variables, what is the law of dispersion for the remaining ones? For in order to solve this problem we require the absolute values of the coefficients. I do not see how to obtain these, except by the method before adopted, viz., obtaining the integrals of the expression J ea? + by? + cz? + Bfyz+ 2gxz+ 2hary) with respect to all but two, and all but one, of the variables. Balliol College, Oxford. * Salmon, ‘ Higher ‘Algebra,’ lesson iv. article 27. + Generalizing the statement given in the former paper, p. 190. { Generalizing the statement given in the former paper, p. 190. [El _ VII. A necessary Modification of Ohim’s Law. By FERNANDO SANFORD*. [Plate III] URING the past year I have been engaged in some investigations which seem to call in question the validity of Ohm’s law, by showing that the resistance of a metallic conductor varies with the nature of the dielectric in its field of force. For the purpose of determining if this be the case, I have made a large number of measurements of the resistance of a copper wire in various dielectrics, and have found that in several cases the change of resistance, both in liquid and gaseous dielectrics, is very marked. The apparatus used consists of a copper tube about four feet long and one inch in internal diameter, closed with copper plates at the end, and having a copper wire 1 miilim. in diameter stretched through its centre and fastened by means of a binding-screw to the centre of one end plate, while it passes through an insulating-plug in the centre of the other end plate. The tube is provided with stopcocks at the ends for filling and emptying, and with an opening in the side for inserting a thermometer. The current, which was always between the extremes of five and eight milliamperes, was passed one way through the tube and back through the wire, so that the whole dielectric in its field could be changed at will. The measurements were made by means of a Wheat- stone’s bridge with arms of i : 1000, and a sensitive galvano- meter. A change of resistance of 0°1 ohm in the box, which corresponded to ‘0001 ohm in the tube and wire, produced a very noticeable deflexion of the galvanometer-needle. The measurements were accordingly estimated with a fair degree of accuracy to ‘00001 ohm. The resistance of the tube and wire was measured in air at different temperatures through a range of about ten degrees Centigrade, and a curve was plotted, using the temperatures as abscissee and the resistances as ordinates. This curve did not depart appreciably from a straight line. The dielectric to be tested was then poured into the tube, a set of measure- ments was made in it through the same range of temperatures, the dielectric drawn out, the tube cleaned and dried, and a new set of measurements made in air. This was repeated several times, until it was certain that after each change of dielectrics the resistance returned to the same value which it had previously shown in the same dielectric. In the case of air and petroleum this comparison was carried on for a month, the dielectrics in the meantime being changed five times, and * Communicated by the Author. Phil. Mag. 8. 5. Vol. 35. No. 212. Jan. 1893. K 66 Mr. F. Sanford on a necessary the apparatus being allowed to stand untouched for two weeks to make sure that none of the constants were changing, and in the whole series not a single measurement in either dielec- tric fell upon or beyond the curve made for the other dielectric (see Pl. III. fig. 1). The resistance of the wire in petroleum was shown to be about ‘00006 ohm less than in air; and as the whole resistance of the tube and wire averaged about °0335 ohm, this difference corresponded to about ‘18 of one per cent. of the whole resistance. Regarding the conductivity of the wire in air as unity, its conductivity in the liquid dielectrics tested was as follows :— Petroleum . a 5 al OES Mixture of carbon bisulphide and turpentine > 10009 Carbon bisulphide, uncertain, apparently . . I+ Wood alcohol "9998 Benzine. 5. fk ws ce oe ot Wood alcohol and benzine ... . . . «sumeeo Absolute aleohol . .. .-.. %. + « «oe Wood alcohol and petroleum . . .. =. . ‘9973 Distilled water, uncertain, apparently . . . I— It will be seen that when two dielectrics which do not seem to mix with each other were used together the resistance of the wire was greatly increased, as in the case of wood alcohol and benzine, and wood alcohol and petroleum. That these liquids do diffuse into each other was shown by measuring the index of refraction of the two components before and after they had stood in contact with each other, and in every case a change was observed. A similar change of resistance was noticed when the tube contained different gaseous dielectrics. This was first observed when the burning gas used in the laboratory was allowed to enter the tube. This gas was made from gasoline by a machine on the ground, and consisted of the vapour of gaso- line mixed with air. of chloride, iodide, or bromide of sodium. One of the plates is exposed to the rays of light, the other is protected from the~action either by surrounding it with parchment or paper, or by placing it directly behind the first plate at a distance of about a millimetre. The action of the light is instantaneous and disappears when the illumination is destroyed. The sensitiveness of an element decreases rapidly at first and then becomes virtually constant. The electromotive force of a given actinometer varies with the colour of the light which acts upon it. M. RigolJot has investigated the electromotive force in the different parts of the spectrum, and gives the curves obtained by taking as abscissee the lengths of waves, and as ordinates the divisions read off on the galvanometer-scale. These curves show that the actinometer with copper plates is most sensitive in the red portion of the spectrum, that is in the region most luminous for the eye. In this respect it differs from actinometers with silver compounds, which are more especially sensitive to the most refrangible rays. If, after having traversed the spectrum from red to violet, the sysvem of plates is again exposed in all parts of the spectrum but proceeding from violet to red, the curves retain the same form, and the increase of sensitiveness for red rays observed by M. Becquerel (Lumiere, vol. ii, page 188) for iodized plates which 78 Intelligence and Miscellaneous Articles. have been previously exposed to the most refrangible rays, does not seem here to take place. M. Rigollot used his actinometer to investigate the light diffused by the northern region of the sky at different times of the day. He gives the curve obtained on September 17, 1889, on the terrace of the Physical Laboratory of the Faculty of Science at Lyons with a clear sky. This shows a maximum illumination towards half-past twelve; the curve is virtually symmetrical with respect to this maximum for different times of day. The author has investigated if, as M. Egoroff has found for iodized plates, the intensity of the current is inversely proportional to the square of the distance from the source to the apparatus. _ This law holds approximately with Drummond’s light as source, that is to say with a feeble light, but with sunlight the intensity increases nore rapidly than the intensity of the current. As the indications of the instrument are proportional to the illumination for faint light, it may be used with advantage in certain cases, such as examining the luminosity of the sky in diffused light.—Journal de Physique, November 1892; from Annales de Chimie et Physique, vol. xxii. p. 567, 1891. ON THE ATTRACTION OF TWO PLATES SEPARATED BY A DIELECTRIC. BY M. JULIEN LEFEVRE. I have measured the attraction of two electrified plates sepa- rated by a dielectric not in close contact with them, and have verified that it is al by the following formula :— rio where Fis the attraction of the i plates at the distance e+e’ in air; F the attraction at the same distance when a plane insulating plate of thickness ¢ has been placed between the plates; ¢' is then the suin of the thicknesses of air on either side of this plate; & is the dielectric constant of the plate. I used two horizontal plates, and a sensitive balance to the beam of which was hung at one end a scale-pan; the movable plate of the electrical apparatus, which is 12 centim. in diameter, is suspended at the other end by an insulating stem. This plate is surrounded by a guard-ring provided with a kind of cover, which is only perforated by a hole to allow the rod to pass. The fixed plate, which is 19 centim. in diameter, is placed below the former and rests on an insulating support with levelling- screws, so that the distance e+e’ can be varied. Three insulating rods pass through this plate and support the dielectric. On either side of this are layers of air as thin as possible; it must, however, be possible for the movable plate to make small oscillations. The source of electricity is a Ruhmkorft’s coil worked by six Bunsen’s elements. One of the poles communicates with the fixed plate, and with the inner coating of a jar the capacity of Intelligence and Miscellaneous Artzcles. 79 which is, according to circumstances, 70 to 150 times greater than that of the condenser formed by the two plates. The other pole, the external armature of the jar, the movable plate, and the beam of the balance are put to earth. The whole apparatus except the scale-pan is placed in a cage the air of which is dried. The plates of sulphur and of paraffin are obtained by melting in a mould, the bottom of which is carefully levelled. The thick- ness of the plate is measured by a two-ended screw and a catheto- meter. The distance between the two plates is also measured by a cathetometer. The dielectric is placed in the cage some days befove the experi- ment so as to get rid of all traces of electricity. The balance being somewhat too lightly tared, and all parts being put to earth, I counterpoise by a weight p. I then electrify the fixed plate, and counterbalance again with a weight P. I put this plate to earth and counterpoise again by a weight p’: then tap (ae. F=P—*3. The attraction EF’ is determined in like manner by three operations. I work in the same way with liquids, measuring FE’ first, and then F so as to avoid evaporation. The thickness of air e’ undergoes in this case a slight correction, which consists in replacing the thick- ness of the layer of air forming the bottom of the vessel containing the liquid by the equivalent thickness of air. In each experiment I calculate the ratio a and then the cor- rected ratio Re # (1S i 1 Gaee From (1) we should have pip, The following table, in which e and ¢’ are expressed in centi- metres, F and F i in milligrammes, shows that the values of VR agree with the values of 4 which I have obtained by means of Coulomb’s balance (Comptes Rendus, Nov. 16, 1891). The formula (1) is therefore correct ; and particularly in the case in which ¢’ can be disregarded, we have r = - | Dielectric. é. e', E 1 = R VR. | & Paraffin, No.1 ......) 2°20 | 0-70 | 39°5 | 17:25] 2:29 | 353] 1:88 | 2 ~ Spiny a eobies ) 0-66 | 40°5 | 14 2°89 | 438 | 2:09 | ,, 5 No. 2c 3°37 | 061 | 805 | 9 3:39 | 4:51 | 2:12] ,, eines 9 OOS 2S8De) i2ol eee eee 210.1. Sulphur Eeiaanaaccine | 356 | 0°54 | 485 | 9°75) 4:97 | 7:27 | 2-70 | 26 IONMIGON, S5.,c0iccn desis 2:04 | 0°32 | 72°75| 18°75} 3:88 | 5:39 | 232 | 23 Carbon bisulphide...) 2°60 | 1:09 | 22 oe | 28 | er) Le | Oil of turpentine .... 2°77 | 0-79 | 26:25) 18 2:02 | 249] 1:58 | 15] | Petroleum ............ 2-98 | 071] 1950) 8 | 243] 388] 1:84 | 1:91 | | 80 Intelligence and Miscellaneous Articles. i may, in conclusion, observe that the attraction of two plates lends itself perfectly to the measurement of dielectric constants ; it is simple, rapid, and only requires a sensitive balance, and is preferable to all methods now in use.—Journal de Physique, June 1892. INVESTIGATION OF THE PROPERTIES OF AMORPHOUS RORON. BY H. MOISSAN. Pure amorphous boron, obtained by reducing borie anhydride by means of magnesium, is a bright chestnut-brown dirty powder, of specific gravity 2-45. ven in the electric arc it cannot be melted ; heated for a long time to 1500° it agglomerates, but not to any great extent. The electrical conductivity is small; the specific resistance ~=801 megohms. Heated in the air, amorphous boron takes fire at 700°, and burns with production of sparks. It burns in oxygen with a brilliant lustre; with sulphur also it unites at 610°, with incandescence, boron sulphide being formed: Borcn takes fire in chlorine at 410°; it burns with bright incandescence, forming chloride; bromine acts in an analogous manner. Amorphous boron combines with metalloids more readily than with metals. At a high temperature it combines, however, with magnesium, iron, and aluminium, and more readily still with silver and platinum. Very concentrated nitric acid readily acts on amorphous boron and with ignition. Sulphuric acid is reduced to sulphurous ; phosphorus is separated from phosphoric acid at 800°, arsenic from arsenic acid, and iodine from iodic acid. Boron is a powerful reducing agent, exceeding carbon and silicon in this respect, for at a red heat it can withdraw oxygen from carbonic oxide and from silica. it can readily reduce a number of metallic oxides; CuO, SnO, PbO, SbO,, and 5i,0,, even on moderate heating, part with their oxygen to boron, with incandescence. Lead peroxide detonates violently when rubbed with boron in a mortar; and a mixture of sulphur, nitre, and boron detonates under a red heat like gunpowder. Amorphcas boron also has a reducing action on a great number of salts; the sulphates of potassium and sodium, as well as those of calcium and barium, are reduced by boron to sulphides as by carbon. Silver is separated in beautiful crystals from solutions of silver nitrate; and from solutions of palladium, platinum, and gold the corresponding metals. Boron unites directly with nitrogen only at very high tempe-. ratures. . Amorphous boron shows thus in its chemical relations remark- able analogies with carbon.— Comptes Rendus, vol. exiy. p. 607. THE LONDON, EDINBURGH, ann DUBLIN PHILOSOPHICAL MAGAZINE AND JOURNAL OF SCIENCE. [FIFTH SERIES.] FEBRUARY 1898. XII. The Diffusion of Light. By W. EH. Sumpnur, D.Se.* | ee information appears te have been published about the diffusing power of unpolished surfaces. The sub- ject has been studied by optical measurements by Zollner and others, chiefly for astronomical purposes ; and the radiation from such surfaces has also been investigated with appa- ratus designed for measuring radiant heat. But the in- fluence of such diffusion in increasing the illumination of rooms and open spaces, although well known, does not appear to be appreciated to the extent that its importance deserves 3 and a few numerical determinations of the coefficients of reflexion, absorption, and transmission of diffusing surfaces may prove of interest. Terms in light are used vaguely, and it will not be deemed out of place to define those which will be here needed. By the reflecting power of a surface is meant the ratio of the amount of light reflected by it to the total amount of light incident upon it. The zddwmenation of a surface is the amount of incident light per unit area of the surface. The unit quantity of light is the flux of radiation per second across a unit area of a sphere of unit radius at whose centre a unit light (of one candle) is placed. The amount of light radiated by a source of & candle-power, within a solid angle Q, is kQ, and the total quantity of light emitted by it is Ark. The brightness of a diffusing surface is its candle-power per unit * Communicated by the Physical Society: read Dec. 9, 1892. Phil. Mag. 8. 5. Vol. 35. No. 213. Feb. 1893. G 82 Dr. W. E. Sumpner on the Diffusion of Light. area in the direction normal to the surface. The illumination produced at a point by a surface of brightness B, subtending a (small) solid angle Q at the point, is BO, and if a surface, containing this point, have its normal inclined at an angle ¢ to the axis of Q, the illumination of this second surface due to the first is BO cos ¢. If B is the brightness of a surface rendered luminous by reflexion, if 7 is its (diffused) reflecting-power, and if I is the illumination of the surface, then cB=7l. 2. This relation follows from the assumption of the law of cosines, viz. that the candle-power (per unit area) of a bright surface is Bcos ¢ in a direction making an angle ¢@ with the normal. The right-hand member of (1) is by definition equal to the whole light reflected from unit area of the sur- face, and must be equal to the integral of B cos ¢ dQ for all directions on one side of the surface. The value of the integral is easily seen to be 7B. The brightness of a body, as just defined, is directly pro- portional to the illumination of the image of the body on the retina of the eye, and the word may thus be quite justly used in the ordinary physiological sense of the term. Similarly the law of cosines, just alluded to, is merely another way of expressing the fact that the sensation of the brightness of a diffusing surface is the same from whatever direction this surface may be viewed. For the amount of hght received by the eye, and concentrated on the image on the retina, is simply the product of the area of the pupil of the eye and the illumination at the surface of the eye due to the bright object. Tbe former tactor is constant for different directions of view, and the latter must vary as the solid angle subtended by the object at the eye, since the area of the image on the retina is a measure of this solid angle. The illumination at a point at which a surface of brightness B subtends a solid angle © is not necessarily BO for all inclinations of © to the surface, unless the law of cosines is fulfilled; and, if this law is fulfilled, it follows that the illumination of the image of this surface on the retina of the eye is constant at all dis- tances and inclinations. The eye is a good judge, and is indeed the only judge, of quick variations in brightness, and the cosine law is always applicable to diffusing surfaces, the appearance of which does not alter as the eye moves past them. Any divergence from this law is negligible so far as its influence on illumination is concerned. 7 If @ is the quantity of light radiated per second by the Dr. W. E. Sumpner on the Diffusion of Tight. 83 light-sources within a room, and if Q’ is the total amount of light falling on the walls, OO ee 2) For of the quantity Q’, a portion 7Q’ must be reflected, and the rest absorbed, and the rate at which light is absorbed by the walls must be equal to the rate at which it is produced. The average illumination I! of the walls of the room must hence be related to I, the i/lumination due to the direct action of the lights, by the equation Bes aS ee ee et) eee — 9) 101 and 1 4="90).1/=2 I, so that the illumination due to the walls of the room may become far more important than that caused by the direct rays of the hghts. The truth of this relation may be also seen as follows :— The light Q falling on the walls is partially reflected, and a quantity 7(@ is sent back into the room. This light falls on the walls again and a portion 7 xQ is reflected a second time. The total quantity of light Q! falling on the walls owing to successive reflexions is given by the equation* , OO AO ae =. =7 2. Or, again, as the illumination I,’ of the walls at any point P is made up of a portion I, due to the direct rays of the lights, together with a part caused by radiation from the walls, we have L/ =I, + | Bos dQ, eh Sond nara as where B is the brightness of the walls, and @ is the inclina- tion of the solid angle dO, to the normal to the surface at the point P. Assuming that the brightness is the same all over the bounding surtace of the room, the value of the integral is readily seen to be mB, and this, as already shown, is equal to nl’, where I’ is the average illumination of the walls. When the bounding surface of a room or enclosure consists of portions whose reflective powers are different, the average reflective power may be taken as 1, = De iieest &e. S00 Ue ‘ . (5) * Since writing this paper I have discovered that this relation has been already pointed out by Mascart [see Palaz, Trazté de Photométrie Industrielle, p. 268). G 2 84 Dr. W. E. Sumpner on the Diffusion of Light. where A is the total area of the bounding surface, of which a portion A, has a reflective power equal to 7;, and a second portion A, a reflective power 7, &e. This relation is very approximately true for ordinary rooms, and may be shown to be quite accurate for a spherical enclosure. For let P and Q be any two points of a sphere of centre C and radius 7 (fig. 1). Then PQ=2r cos ¢, where ¢ is the angle which the chord makes with the radius through either P or Q. Also, with the same notation as before, we have dA cos¢@ PIP? y where dA is an element of area at Q of brightness B, and subtending a solid angle dA cos¢/PQ? at P. Now PQ’=4?r? cos*$ and tB=71’, where I’ is the illumination of the area dA: hence os 1 I, =I,+gasindA=1,+ 7 )IndA, . ©) iby = if + | Beos¢ A being the total area of the spherical surface. The integral is constant whatever the position of the point P, and what- ever the character of the reflecting surface of the sphere. Thus if any complete [or if any portion of a] spherical sur- face be illuminated in any manner I, by the direct rays of a combination of light sources, the actual illumination I,’ will exceed I, by a constant amount all over the sphere, owing to the reflective action of the surface. Also, if the original dis- tribution be uniform all over the sphere, I,=I, a constant, I,’ will also be constant, =I’, and / : =I +5 Jad = I+ tal’, where : ndA 13 (7) Dr. W. E. Sumpner on the Diffusion of Light. 85 Taking as an average case for rooms a reflecting power of 70 per cent. for the ceiling, 40 per cent. for the walls, and 20 per cent. for the floor, the average value of 9 is a little over 40 per cent., and the increase of illumination by re- flexion becomes as much as 70 per cent. If the walls and ceiling of a room be well whitewashed, the average reflecting power will not fall far short of 80 per cent.; and in such ceases the illumination due to diffused reflexion is four times as important as that caused by the direct action of the lights in the room. A further great advantage, resulting from the use of good diffusing surfaces, arises from the fact that the illumination they cause is, in most cases, very approximately constant all over the room, and does not cast shadows. Tt is to be noted that when a reflecting surface is coloured, its average reflecting power does not properly represent the character of the increase of illumination caused by it. A room whose walls are covered with red paper whose average reflecting power is 40 per cent., may quite possibly have the red light in the room increased five times owing to the action of the walls. Suppose, for instance, that the reflective power of the paper for red light is 80 per cent., and for other kinds of light only 10 per cent., the average reflecting power will not exceed 40 per cent., yet the red light will be increased five times, while other kinds of light will not be increased to any perceptible extent. Measurements of [eflective Power. The surface, whose reflective power was required, was attached to a Jarge screen of black velvet placed at one end O of a 3-metre photometer-bench OL (see fig. 2), so as to Fig. 2, be perpendicular to its length. Two lights were used, one being a Methven two- candle. gas standard, placed at L, and 86 Dr. W. E. Sumpner on the Diffusion of Light. the other a glow-lamp run generally at about 20 candle- power, placed at P,;. A Lummer-Brodhun photometer was slid along the bench to a point P, at which the illumination due to reflexion from the surface OR was equal to that due to the Methven standard at L. At first the lamp P, was permanently situated a little to one side of the bench, and the rays from it in the direction of the photometer P, were screened off. Subsequently the points P, and P, were made to coincide, the lamp being fixed to the same slider as the photometer and suitably screened from it and from the eyes of the observer. In some experiments the distance OL was kept fixed and the position of balance OP was determined for each surface tested. In other cases both OP and OL were varied. Let :— A = area of diffusing surface on screen OR (centre at O). D,, O, = solid angles subtended by A at P,, P. respectively. 21, #2 = distances OP,, OP, respectively. y = distance P.L. K = candle-power of the glow-lamp at Pj. k = candle-power of Methven standard at L. Then :-— The quantity of light falling on the area A is KQ,, the average illumination of A is KQ,/A, the average brightness is n7KO,,/7-A, by (1), the illumination at P, is 7KO,0,/7A, © and also the illumination at P, is k/y? ; whence ey ie eee Se 10,07 K Af?? — provided the dimensions of A are small compared with «, or 2. When this is not the case, the equation (8) is not suffi- ciently correct, and a more accurate formula may be obtained as follows, by taking note of the inclination of the rays to the surfaces. The illumination of the surface at the point R due to the lamp at P, can be easily shown to be K cos? ¢,/2,2, where ¢, is the angle between RP, and OL, the line of centres of the bench. The bmghtness B of the surface at R is therefore nK cos*d,/72z,? by equation (1). An element of area dA at R subtends at P, a solid angle dO, equal to cos*¢.dA/z,2, and the illumination at P, due to this element is BdO,= 7K cos’ $; cos*p2dA/7#?22" on any area placed perpendicular to RP.. As the photometer screen is perpendicular to the Dr. W. E. Sumpner on the Diffusion of Light. 87 bench and not to RP., we must multiply this expression by cos, to get the effective illumination due to the element dA. Finally we have for the total illumination the integral :— = al CORO COSMO Ly i. see (9) in which the angles ¢,, ¢ are related by the equation xv tan ¢;=2, tan do. When the area A is circular, with O as its centre, this integral reduces to I= = COs® Hid S107 O55)... 4. , CLO) 1 The value of this integral can be readily evaluated, but it does not lead to a convenient formula, and as it was found prac- tically preferable to fix the lamp to the same slider as the photometer, and at the same distance from the screen OR, we may put $1 = b2= 9; and (10) then reduces te KZ , l=n-3 zL1 —cos’¢ |, e ° ° 2 SS) (11) in which ¢ is the semiangle of the cone with base A and height x. This expression is rendered more convenient for purposes of calculation by taking advantage of the fact that A/zx’, or tan’d, is a small quantity. By neglecting tan*d compared with unity we obtain 2 iL 5 [1—cos’] = x’ where i Hi TH X= +1°754+ 413— 3, bag. 3) SBR ee EE) and in most cases it will be found that the third term in this expression is negligibly small compared with the sum of the other two. The value of I found in (11) may be equated to k/y? when the photometer is in the position of balance, and on doing so, we find for 7 the value cnikes faa IK x which reduces to (8) when 2 is large. ee te Pete a tS) 88 Dr. W. E. Sumpner on the Diffusion of Light. This equation was used for the great majority of the re- flexion tests. With feebly diffusing surfaces such as black cloth, the distance z had to be so much reduced that the area A subtended a greater angle at the photometer screen than the aperture of the photometer itself. In such cases the angle @ in (11) was calculated from the solid angle sub- tended by the aperture of the photometer at the centre of the photometer screen. With diffusing surfaces which appeared to shine slightly under the action of light the effect of regular reflexion had to be separated from that of diffused reflexion, by experiments made with the same surface for different values of x In such cases, which will be alluded to subsequently, the true reflecting-power is not given by formula (13). The areas A of the reflecting surfaces used in the experiments were never circular, as assumed in the above proof, but as they were always ap- proximately square, with the central portion at O (fig. 2), any error in (12) and (13) arising in this way must be quite negligible. The ratio £/K of the two lights was frequently tested in the course of the experiments and was found very constant during every set of tests. The results obtained are given in the accompanying table. In the majority of cases the numbers given are approximate only, as there seemed no object in aiming at great accuracy. The first four surfaces referred to in the table, viz., thick white blotting-paper, white (rough) cartridge-paper, tracing- paper, and tracing-cloth, were, however, carefully tested, and the numbers obtained represent the mean of many observations. TasLeE J.—Reflecting- Powers. per cent. per cent. White blotting-paper_......... 82 Plane deal (clean) ......... 40 to 50 White cartridge-paper ......... 80 (dirty) <2yecseseeneee 20 PDracing-ClOb j..t.2+-6 260 ocuases 30 Yellow cardboard <2-2222-5--ae 30 Dracins- paper. so-<1.-s-4.” ky — ke Sa ak gee ar ol) and the true absorption coefficient « is given by ky—k a=(l—4)—, - spice pana eee (UD) 0 where 7 is the previously found reflexion coefficient. When an inner envelope is used to produce a light which radiates equally well in all directions, it is necessary for the outer envelope to be large compared with it, since otherwise the formula for the increase of illumination due to internal reflexion cannot be applied. The following table gives the values of the absorbing coefficients, expressed as percentages, for the four substances at the head of Table I., from which the corresponding values of m used in applying (15) have been taken. TABLE II, Apparent Absorption. Real Absorption. White Blotting-paper ......... 77 per cent. 13°8 per cent. White Cartridge-paper ...... 61 Mi 12:2 (, Mraeine—Clobla i202 .-je.. foe ee sae 23 - 15:0 - RACINE =PAPCL ciaecveneeeeveees 9 70 Three large glass globes, made for arc-lamps, were also tested. As the reflective powers of the globes could not easily be found, only the apparent absorption was measured. One globe was of opal glass (almost transparent), and the ratio of apparent absorption was 15 per cent. A second globe was of ground glass and absorbed 42 per cent. The remaining one was of opal glass, too opaque to allow any bright object placed within it to be distinguished. This absorbed 39 per cent. Measurements of Transmitting-Power. The amount of light transmitted through the surfaces above mentioned was measured in a very similar manner to that in which their reflective powers were determined ; the 92 Dr. W. EB. Sumpner on the Diffusion of Laght. only difference being that the glow-lamp at P, (see fig. 2) was moved to the opposite side of the surface as in fig. 3. OR represents the screen of paper, pinned on a wooden frame, and placed perpendicular to the optical bench P;L. The Fig. 5. OR —OP — itz lia glow-lamp was at P,, the photometer at P,, and the Methven standard at L. The distances OP,, OP, were arranged to be equal, and balance obtained by moving L along the bench. On referring to equations (8) to (13) and the arguments used in establishing them, it will be seen that they are all applicable to the case now considered if only we substitute 7, the transmitting-power, for 7. When, however, tests were made with the paper surfaces already referred to, it was soon found that the numbers calculated from expression (13), X=Y,. 0 were not constant for the same substance. They differed from each other far more than could be accounted for by errors of experiment; thus, the values found for 7 by this formula were too high, and frequently exceeded 100 per cent. For any given surface the values were found to increase pro- gressively with the value of « used in the tests. The reason for this is easily seen when it is remembered that equations (8) to (13) are only true on the assumption that the surfaces considered are purely diffusive, and do not alter in appearance as the eye changes its point of view. When light is trans- mitted through a semitransparent substance such as tracing- paper, or tracing-cloth, the brightest part of the surface is always on the line joining the eye to the light, and visibly moves over the surface as the point of view ischanged. The set Ne Dr. W. EH. Sumpner on the Diffusion of Light. 93 easiest way to represent these facts is to assume that, of the light transmitted, a portion 7, passes through without change of direction, Paul that the rest 7, is diffused in accordance with the cosine law. The case is analogous with a reflecting surface such as white enamelled iron, which reflects a portion m, of the incident light in accordance with the regular law of reflexion, and diffuses another portion 7, according to the law of cosines. On referring to equations (8) to (11) it will be noticed that they are still true for the illumination due to diffusion if we substitute for 7 either tT. or n, (according as we are considering transmission (fig. 3) or reflexion (fig. 2) respectively). The additional illumination at the photometer due to regular, z. e. direct, transmission (transparency) is K Ui Qa)” : (17) and a similar expression holds for regular reflexion if we substitute 7, for 7}. The whole illumination must, as before, be equal to k/y?, and by (11), (12), and (17) we have K Kees tk Tae Te 0 = 5 ° ° (18) whence the value of Y in (16) is equal to Y=7,+ eee: aoheeco ual soence 19) and a similar expression holds for reflexion if we replace 7, and 7, by , and 7, respectively. The true values for the transmitting and reflecting coefficients are rantt, | 20 n=m™+, |’ oy and the reason the values found for Y were too high, and became greater and greater as x increased, was simply that the values used for X (see 12) were always greater than 4, and increased rapidly with «. By plotting the numbers found for Y with the corresponding values of X, a straight line is obtained from which the values represented by the symbols in (20) can all be determined. The straightness of these lines, and the verification of the fundamental formula nt+atT=l1, 94 Dr. W. E. Sumpner on the Diffusion of Light. affords a good criterion of the extent to which the principles and the formule, referred to in this paper, can be relied upon. "The following Tables IIT., [V., and V. contain the results of three sets of tests on the transmitting-jower of blotting- paper and tracing-cloth, and on the reflecting-power of tracing-cloth. The values of Y,,. are calculated with the aid of (12) and (16) from the observed valnesof «andy. All the dimensions are given in centimetre-units. In the accom- panying sheet of curves the values of Y,,, are plotted as ordinates, with the corresponding values of X as abscisse. From the straight line most nearly representing the connexion between the points the values of Y,,,, have been obtained, and are given in the tables. From this straight line also the true value of the transmitting (or reflective) power can be found by finding the value of the ordinate when X=4. The intercept on the axis of Y shows the portion of the light which is diffused. Tasie L1].—Transmitting-Power of Blotting-paper. A=980, K=26. £=2 r=92. Y,.1,=650527R/* Pesos es | 60 50 40 45 AD 60 yi Were neal: ge tO 84. 1046 187. 154 | X Bee | 136 9-8 70 weer; ee | ibd . 182 - 112. 19-0... (142s av wae Os | 157° 481-979" yea 4 ae TaBLE 1V.—Transmitting-Power of Tracing-cloth. A=980, K=931. s=2 r=544. Yi). =410+418-4X/4. haces S028 cnow .) WOW 894. 105:6°> 953. 17 eae 46-1 | SORE | 6 ose 50M NS6 Pra" 22°30 19-4- > 15 ee 8°25 BUOY bs Oe tere SO a7. OGSHIG 107 915 Sli -ias os Gta Sion 5 60'6 40-9272 AS 106 940-- 7802 sa ide) Qn Dr. W. EB. Sumpner on the Diffusion of Light. Taste V.—Reflecting-Power of Tracing-cloth (shiny side). A=1300. K=12. £=2. 9=85°7. Yate, =80°9+4'8X/4. J Pee 56 55 623 598 475 445 ee OLA | 977, 1202. 85. 755 BO ii! ee S10 Ae tO4y 7-22 655 ee... Wee Set lee AS 2) 896 S86 Me eresates: | 408 «418 4k 484896 88-7 200 150 100, 0 5 10 15 20 Several sets of tests were taken. Some of these are repre- sented by the sheet of curves shown in fig. 4. Y is the percentage of the incident light which the surface apparently reflects or transmits, assuming that it is all diffused, and is calculated from equation (16). The true values ef the co- efficients are obtained from the curves by applying equations (19) and (20). The numerical details of the observations are of no special interest, and the essential results may be sum- marized as follows :— 96 Dr. W. E. Sumpner on the Diffusion of Light. TasLe V1I.—Reflective Powers. Regular. Diffased. Total. 7): No: 1). ——— —— ———_____ |, ——__—_ ee a oeeemae Blottme=paperzts.c.0.se22 34sec | 0 per cent.| 82 percent. | 82 per cent. if Cartridge-paper ~.2..----.5.25- 8) S SO 2 80 = | Tracing-cloth (shiny side) .... 48 ,, | RO case fee | » (cough side)...| 2-7 ,, B168 | BY ay cial Tracing-paper .............06... D2. ss 19:3. | DEO TasBLeE VIi.—Transmissive Powers. Direct. | Diffused. Totaly: Tae Tix ze Blotime-papetices...0-------- 2-7 per cent. | 6:5 per cent. | 92 per cent. Cartridge-paper .........0. a ee 87, a | racine =e Opies: cece aneaner | 13°4 5 41-0 % | Sas oe | Tracimeopapetesc:-..0--.267- | 29°8 os 46:2 A 76:0 3 We may now collect the coeflicients 7, a, 7, determined by the foregoing independent methods, and compare their sum with unity. TABLE VIII 0. a. T. nt+eatr. Blutting-paper ...... 82 per cent. | 13°8 per cent.| 9:2 per cent.| 105-0 per cent. Cartridge-paper ...| 80 ___,, 22a. | CU ee 1034.5, Tracing-cloth ...... Sper, | 150 3 54:4 te 1044 — ,, Tracing-paper ...... v7 aaa (fe TOD a 1050 ae The numbers in the last column differ from the true value of 100 per cent. to a greater extent than can fairly be accounted for by the limits of experimental error. They are all over 100; and this was the case, not only for the tests here given, but also for every one of many sets of tests taken. The small dis- crepancy would be accounted for by assuming that the law of cosines is not exactly fulfilled. A very slight departure from this law would be amply sufficient to expiain the results. Suppose the candle-power of a unit area of a diffusing surface in the direction of the normal is B, and in any Relation of Volta Electromotive Force to Pressure $c. 97 direction ¢ is B (cos )!+«, It is then easy to show that the total amount of light given out per unit area is equal to Bia - (es +9 In all the above experiments the actual measurements have referred to the light receding from the diffusing substance at inclinations all practically normal to its surface. The quantity B has been measured, the total light has been calculated as a B, and has been overestimated in the ratio 1 +5: Ie To account for an error of 5 per cent., the quantity e« need only be 0-1. The brightness of the surface (in the physio- logical sense) would, when viewed at an inclination @¢, be proportional to B (cos g)'t*/cos f, or B (cos d)*. This quantity is practically constant (if e=0°1) until @ becomes very large. Its value is ‘994 for 6=20° and :974 for @¢=40°, and the change in the brightness of the surface would hardly be perceptible to the eye. This correction applies to the coefficients 7, and T.; it does not affect the values of 7, #, or tT, In some of the first tests of reflecting-power the inclination of the light-rays to the surface was considerably less than 90 degrees, and the values of 7 obtained were less than those given above. ‘These tests confirm the idea that the cosine law is not strictly fulfilled, but they were not accurate enough to be conclusive. The above measurements were all made in the Optical Laboratory of the Central Institution, and the writer has had the benefit of the assistance of some of the students of that College in re-testing and confirming the results given in the foregoing tables. XM. Relation of Volta Hlectromotive Force to Pressure §e. By Dr. G. Gore, P.A.S.* aan years ago I made several experimental attempts to discover a difference of molecular state of the upper and lower ends of a vertical column of solution of cupric sulphate:—I1st. By suddenly reversing the ends of a utta-percha tube, about 6 feet high and 6 inches diameter, filled with the liquid, by swinging the tube in a vertical * Communicated by the Author. Note. Compare Wild’s experiment (Wiedemann’s Galvanismus, 1872, vol. i.p. 776; Pogg. Ann. 1865, vol. exxv. p. 119). Phil. Mag. 8. 5. Vol. 35. No. 213. Feb. 1898. H 98 Dr. G. Gore on the Relation of Volta plane upon a transverse horizontal axis at its centre, the ends of the tube being formed of two similar plates of electrolytic copper connected with a galvanometer ; and 2nd, by simul- taneously raising and lowering two similar disks of copper 1m a tall column of such solution, the disks being attached to the galvanometer and suspended from the two ends of a cord passed over a pulley. These attempts, however, were not successful owing to disturbing influences at the surfaces of the plates, and to the employment of an insufficiently sensitive galvanometer. Recently I have renewed the experiments in a somewhat different form, and have succeeded in obtaining de- finite though small effects; only minute ones were anticipated. The arrangement usually employed was as Fig. 1. follows:—A single glass tube (or several), about 3 metres long and 1 centim. bore, securely fixed upon a board, was fitted with corks and two wire electrodes of the same kind of metal at its two ends, and filled within *5 centim. with an electrolyte (see fig. 1). It was then placed horizontal, so that the bubkle of air receded into the branch of the tube; the two elec- trodes were then connected with a Thomson’s reflecting-galvanometer of 3040 ohms resist- ance, and the tube allowed to remain undis- turbed until all sign of current or of variation of current ceased. It was then placed vertical, and as soon as a steady permanent deflexion occurred its direction and amount was noted ; the tube was then placed either horizontal until all current ceased, or at once placed vertical with its ends reversed, and the amount of maximum steady deflexion again recorded. In many cases five such tubes were fixed upou the board and connected in series, the upper electrode of one to the lower of the next one, in order to multiply the effect, and as many of them charged with an electrolyte and connected with the galvanometer as was desired. The electrodes were fixed in the corks by means of melted shellac, and the corks were saturated with melted paraffin. By employing suitable metals and electrolytes, making each pair of electrodes of metal cut from imme- diately contiguous parts of the same piece, and including in each instance a wire coil of 50,000 ohms resistance in the circuit, the fluctuations Sag B TV VAIL EAMTATH ANU ROHOV UCT TH Wt ls Aaa cul Electromotive Force to Pressure §c. 99 of the current were reduced to a minimum, and the needles usually settled at or near zero in about 5 or 10 minutes after closing the circuit with the tubes in a horizontal position. No perceptible amount of interference was caused by the small difference of temperature, usually equal to about 1°°5 C. of the upper and lower parts of the experiment room. All the experiments were repeated two or three times in order to ensure reliable results. The solutions employed were all of them made with dis- tilled water, and were in nearly all cases dilute; the exact strength used, however, was not a matter of much importance. Those of the halogens usually contained about 3°29 grains of chlorine, 7°41 grains of bromine, or 11:25 grains of iodine in 18 ounces of water. Those of the acids contained about D9 grains of absolute acid in 40 ounces of water ; and those of neutral salts or of alkalies contained about 300 grains of the substance to that amount of water. The electrodes of cadmium, zinc, aluminium, tin, lead, and copper were formed of thick wire; and those of nickel, iron, silver, gold, and platinum were thin wires. The following Tables give the particulars and the results. TABLE I, Hffect of Varying the Hlectrolyte only. With Electrodes of Zn. aS Substances. Grains per oz. noe Saas 122 (3) Re eee 164 9) 8° A C135 ea Bi) f 0 3. CPCI ..22%.: 1848:°3 2 50° A 4, Br+KbBr ......... OT+ ,, . 28715 5. ST ed ed 62+ ., ” 12° ” 6. (CHE oO) > 4 sat. soln.+9°4 4 Ooh fee |, Br--K Bro i..5. 00. 6drops+ ,, i Very variable. (Sg pl Ges Ss (Ge 3 grains+ ,, 5 20° 4 9 | 5 (( ©) [gene
"|-AaneSO 7 > vies 49. AmSesquicarb. ... ie i baie Weta irl 2 ( See eee $3 DN | PAWL oe teccce 75 Livia lie 5: 3 age ARS ee - Diba sal geal ence be van ge S 54; -+| Ba2BrO, | .....222. sf BS: Th BaZN On| se... d8e. 5 Die MIE eres wceteae ra) Dc Hl EOIN coe. actos Me ie igae! Bi 041 0) ISS oe Sa T5 Sys es bal FO) a Se eae ae 795 GO. UM ESO Frees so 2: - TIGR E11 C1 a Ses Semen a 75 ad ar AEN 0. na ae 3. Cob Ars) Ces ae oes e 2 ee es DSS) eed eae 75 65. | Distilled water ...| 32 oz. Dr. G. Gore on the Relation of Volta Table I. (continued). No. of Tubes. Amount of Deflexion. TT —— ————————_ . wt Electromotive Force to Pressure &c. 101 TABLE II. Effect of Varying the Electrodes and Liquids. With Electrodes of various Metals. me. Substances. Grains per oz. eas Tiee 66. | Al with Cl+KCl.| d sat. soln. +94 4 20° A 67. » », Br+KBr.) 6 drops ota 3 302 a5 68. |CdwithC1+KCl.|4sat.som.494/ 4 | 20° 4 69. » » Br+KBr. 6drops’ + ,, Hs 202": 70. 3) os DEKE s..| 3igrains + ,, 302"; 71. | SnwithCl+KCl. | } sat. soln. +9-4 1 10° | 72. » » Br+KBr.| 6drops + ,, x 0° 73. | Pb with C1+KCL| d sat. soln. +9-4 1 oe 74. pec l|On.. 75 grains. 3 0° 75. | Fe with Cl+ KCl, 3 sat. soln. +9°4 1 20° A 76. Co ? 9) =F b} 9) =F 9? »” 35° bP) (Gk Ni 99 99 + 99 99 Te 39 59 50° oe) 78. Cu +) 99 + 99 99 ata 9 50° 99 79. » >» Br+KBr.| 6drops 4+ ,, et 0° 80. |Ag ,, Cl+KCl.| d sat. soln. + ,, 1 0° Oe &,, KC... .~. 1D 5 0° 82. |Au ,, Cl1+KCl.| § sat soln. +9-4 1 30° 83. Pt 99 39 == 9) >) i 9 19 99 ‘) 84. » » Br+KBr.| Gdrops + ,, 5 0° SPM 55,7 FOL orcas 16 4 i, Somming 1, KCIO, 75 2 - 87. ” ” KHSO, 99 5 ” &8. 9 9 KHO 9 ) ” TaseE ITI. Hiquivalent Solutions. No. of : No. of Amount of ae Substances. Grains per 02. Tales. Dereon: 89. | Cdwith Cl+KCl.| -18 gr. + 8° gr. 2 12° 90. ” ” Br+KBr.| °37 ein oy ” 28° 91. ” ” T+KI ...| 62 pe ies a 2 10° In experiments Nos. 17, 18, 20, 66, 67, and 70, evolution of gas and disturbances of the current occurred; and in Nos. 71, 72, and 73 the quantity of water employed was only 18 ounces. 102 Dr. G. Gore on the Relation of Volta In every case of production of current, provided the two electrodes were neutral whilst in the horizontal position, and were allowed to remain sufficiently long in each of the vertical ones, the two opposite currents produced were equal in amount. In all the cases in which a sudden change from the horizontal position (and a neutral state) to the vertical one was attended by production of a current, the maximum amount of deflexion of the needles usually occurred in about three minutes ; but if in any case, whilst the tube was vertical, its ends were suddenly reversed, the reversal of the deflexion required a longer period of time to attain its maximum. Degree of Permanence of the Currents. With the object of ascertaining whether the currents were temporary or permanent, two of the tubes were fitted with zinc electrodes and a solution of NaClOs of the usual strength (see exp. 389) made with distilled water, which had been deprived of air by boiling. After having become neutral in the horizontal position, they were placed vertical and gave the following results :— TABLE LV. Influence of Time. Laue Of | Minutes. Deflexions. |, Minutes.| Deflexions.|| Minutes.| Deflexions, experiment. fe) je) ° (\- Ast. 10 } 10th. 30 75th. 30 } | 2nd. 20 ,, 15th. se 90th. ae 92. die) Sd. 25, | webth: eile 105th. le | 4th. 30 ,, 45th, 25 ,, 120th. 7. \| 5th. shan | 60th. ee 16 hours. yA l By subsequently placing the tubes horizontal to become neutral, and then erecting them again, the deflexion was 25°}. The results show that the action was of a comparatively per- manent character, and that the currents were not due to dissolved air. Influence of Strength of Solution. In this case zine electrodes and two solutions of the same substance of different degrees of concentration were employed. Electromotive Force to Pressure Sc. 1038 The upper and lower ends of the tubes were wrapped in cotton-wool. The following are the particulars of the ex- periments :— Number of os: : Number of | Amount of experiment. SESE AGe, | CUES [De . Tubes. Deflexion. 93. KCW a. +0 2 8 94. 5 Ee 40:0 ” 12 ,, These results show that the amount of deflexion was in- creased fifty per cent. by employing a solution of ten times the degree of concentration (compare alsu experiments Nos. 3 and 5 with 6 and 8). The catton-wool had no apparent effect upon the amount of deflexion, thus showing that the unequal temperature of the upper and lower parts of the room had no perceptible effect. Period of Time required for Reversal. With zinc electrodes in the solution of KC1O; (exp. 24) and three tubes, the period required to attain the maximum effect after a complete reversal was 4°5 minutes, and was the same after standing vertical 15 hours. | With zinc electrodes in the solution of Na,SO, (exp. 41) and three tubes the time required to completely reverse was 10 minutes, and in the solution of KCl (exp. 21) it was 15 minutes. With cadmium in the same solution of KCl it was 13 minutes, and after standing vertical 18 hours it was again 13 minutes. The degree of fixity of the state produced varied, therefore, both with different liquids and with different metals, but not with lapse of time. Degree of Electromotive Force of the Current. This was measured by the method of balance with two thermoelectric couples of iron and German-silver wires, the junctions of which were immersed in melted paraftiin at 120° C., the outer ends of the wires being at 20°C. With zinc electrodes in two tubes and the solution of four grains of KCl per ounce of water, giving a deflexion of 8 degrees, as in exp. 93, the electromotive force was equal to ‘00072 volt. Wild (see note, ante) attempted to find the variation of 104 Dr. G. Gore on the Relation of Volta electromotive force of amalgamated zinc in a solution of zine sulphate by increase of pressure of about two thirds of an atmo- sphere, and observed that it was in any case less than one 400,000th of that of one Daniell’s cell, = about ‘0000028 volt (compare exp. 63). He apparently failed to discover the phenomenon of the current by not happening to select a suitable electrolyte. General Results. On examining Tables I., II., III., and IV. various facts may be observed :—Ist. Currents were produced by using a large variety of metals as electrodes, and by employing various kinds of electrolytes. 2nd. The results varied both with the kind of liquid and with that of metal. 3rd. In every one of the ceases in which the liquid employed was a diluted acid alone no current was observed, and the addition of a salt to the acid appeared to have no effect unless the salt alone gave a current (compare exps. 19, 20, 24, 45). 4th. Out. of 91 experi- ments 41 gave perceptible currents ; probably in many other cases currents were produced, but were too feeble to be detected. 5th. Out of the 41 cases in which a current occurred, in 39 it was in an upward direction and in 2 downward. 6th. The current continued many hours without sensible diminution. 7th. In every case the current was extremely small, and required a few minutes to attain its maximum amount. 8th. It was much smaller with a dilute solution than with a concentrated one. 9th. The largest current occurred with zinc in a solution of Cl and KCI, prob- ably in consequence of the great chemical energy of the combination and the small amount of resistance. 10th. By adding to a solution of Cl some KCl, or to one of Br some KBr, a larger current was obtained than with either liquid singly, probably in consequence of diminution of resistance. 11th. Sclutions of iodides frequently gave smaller currents than those of bromides, and bromides less than chlorides ; there are, however, numerous exceptions to this statement. And 12th. Vibration of the lower electrode by means of a tuning-fork had no apparent effect upon the maximum current. Influence of Equal Pressure at the two Electrodes. In order to ascertain whether the current was produced during the absence of any difference of pressure at the two electrodes, I employed one of the usual tubes, 3 metres high, having a porous biscuit-ware diaphragm ;% inch thick near Electromotive Force to Pressure &c. 105 its lower end, offering such a degree of Fig. 2. hindrance as to almost entirely prevent the flow of the liquid, whilst allowing the electric current to pass, and provided with a bent glass tube at its lower end to receive the lower electrode (see fig. 2). In order to prevent any diminution of pressure at the upper electrode an open branch-tube was provided, as shown ; and to obviate any increase of pressure at the lower one, a minute nick in the side of the lower cork allowed any of the liquid which had passed through to over- flow: only one drop of the liquid, how- ever, was forced through by the pressure in about one hour. Sufficient hindrance to the passage of the liquid was obtained by coating the whole of each end of the diaphragm with varnish, except a minute portion of the surface about 1 millim. diameter. A perfectly clean diaphragm was employed in each case, and it was soaked in the liquid previous to use. Only a single tube with zine electrodes was employed in each experiment. Two experiments were made, one with a solution of 18°7 grains of chlorate of potassium and the other with 18°7 grains of nitrate of strontium per ounce of pre- boiled water, and although the circuit was complete no current was produced by placing the tube vertical in either case (compare exps. 24 and 57). These results prove that the current was not produced during the absence of difference of pressure. este eee: VOU EE Ee et LUCA VELARDE UV CUT TEACUP TOU TT Ty a CULATED TUDE CETTE ETE EET EU eT li Influence of Difference of Pressure without Difference of Altitude. In order to test whether difference of pressure alone was sufficient to produce a current, the following arrangement was employed (see fig. 8). A, pressure-tube containing mercury ; B, very thick tube of indiarubber ; C, glass tube witha branch containing a zinc-wire electrode securely fixed in it by means of a cork and shellac ; D, porous-ware diaphragm 3 inch long and 4 inch diameter fixed inacork ; H, a second branch-tube containing the other similar electrode. The diaphragm was sufficiently impervious to allow not more than one drop of the 106 Dr. G. Gore on the Relation of Volta electrolyte to pass per hour whilst under the pressure of a vertical column of 380 inches of mercury. The electrolyte Fig. 3. XS G; was a solution of 18°7 grains of chlorate of sodium per ounce of water, and was allowed to completely saturate a perfectly clean diaphragm previous to the experiment being made. The entire arrangement was fixed upon a board. After placing the tube A horizontal until the two electrodes became neutral it was quickly raised to the vertical position: a current and deflexion of 10 degrees was gradually produced in about three minutes. This current was permanent, but gradually diminished to 6 degrees on removing the pressure. Several trials were made, and in each case the electrode which was under pressure was positive to the other. By repeating the experiments with a pressure of 52 inches height of mer- cury, a defiexion of 12 degrees was obtained. The experi- ments were repeated with the apparatus modified by haying a glass tube about 3 metres long fixed to the end H and filled with the electrolyte, with the second electrode transferred to its distant end: whether this glass tube was horizontal or vertical, the effects of varying the mercurial pressure were substantially the same as in the previous experiments. These results show that difference of pressure alone was sufficient to Electromotive Force to Pressure Sc. 107 produce the currents. In all these experiments, and in the previous ones in which a diaphragm was employed (see fig. 2), the latter manifestly diminished the amount of the current. Influence of Thernelectric Action. It might be supposed that the stronger pressure at the lower electrode, by giving rise to greater chemical heat, is attended by a thermoelectric current from that electrode to the electrolyte ; and this view is apparently supported by the circumstances :—Ist, where the chemical energy is greatest the current is usually the strongest ; 2nd, the full strength of the current is developed gradually ; and, 3rd, the current is a continuous one. But it does not agree with the fact, established by numerous and varied experiments, that whilst heat usually makes metals more electropositive in solutions of alkaline salts and alkalies, it makes them more negative in those of acid salts and acids (see “‘ The Thermoelectric Properties of Liquids,” Proc. Roy. Soc. 1878, vol. xxvii. p. 513). If heat therefore was the cause, downward currents would have occurred in the latter group of liquids, instead of which no currents occurred in dilute acids, and upward ones were pro- duced in solutions of acid salts. In order to finally settle this point, I made the following experiments :—Two vertical metal wires, 2 inches long, coated with shellac over about an inch of their length at about half an inch from their ends, were immersed three-fourths of an inch in two portions of the electrolyte contained in two small glass beakers placed about 3 inches asunder, the two portions of liquid being connected together by a piece of clean linen tape previously soaked in the solution and laid upon a strip of sheet-glass connecting the edges of the two vessels ; each beaker contained a thermometer, and the wires were connected with the usual galvanometer. After the needles of the gal- vanometer had settled at zero, heat was applied to one of the beakers until the temperature of the liquid had risen about 3 or 4 Centigrade degrees, and the effect was then noted. With zine and the solution of KHSO, of exp. 29, no per- ceptible current occurred, but in that of NaClO; of exp. 39 a deflexion of 20° was produced, the warm metal being nega- tive. With platinum in the KHSQ, solution, and in that of KHO, no current was perceptible (compare exps. 87, 88). These results together with those previously mentioned clearly prove that the currents obtained were not due to thermo- electric action. 108 Dr. G. Gore on the Relation of Volta General Remarks and Conclusions. The currents were manifestly occasioned by difference of pressure at the upper and lower electrodes, and apparently by that circumstance alone. They were not due to the unequal temperatures of the room or to heat evolved by the pressure at the lower electrode, nor to air or impurities dissolved in the water, nor to bubbles of gas &. adhering to the electrodes, nor to greater conduction resistance of the electrolyte in a downward than in an upward direction, nor to difference of altitude of the electrodes except so far as it affected the difference of pressure; nor were the deflexions caused by mechanical disturbances of the galvanometer or by any magnetic substance near it. They were also not produced by thermoelectric action due to greater chemical heat at the lower electrode. In all the cases in which a diaphragm was employed, the electric current due to pressure was not per- ceptibly affected by any current produced by flow of the electrolyte through the partition ; the considerable conduction resistance of the septum, however, largely reduced the quantity of the current due to pressure. The results of the experiments in general indicate that the upper and lower ends of a column of an electrolyte are not in ex- actly the same physical or chemical state ; that a fixed difference of condition of the liquid and metal was gradually produced when the tube was placed vertical, and that this condition re- quired several minutes in order to attain its maximum. ‘That both the metal and the liquid are altered by the pressure is shown, not only by the fact that a change of either affects the amount (and in some cases also the direction) of the current, but also by the circumstance that the period of time required to reverse the condition, and the current, by reversing the tube varies with a change of metal as well as of liquid. These cir- cumstances are interesting, and indicate the gradual produc- tion by pressure of a state of mechanical stress of the lower electrode and of the liquid near it; and as action and reaction are always equal and opposite, the state of stress of the metal must be attended by one of counter stress of the liquid. The same states of stress might of course be produced by means of a hydraulic press, a lever, &., or by centrifugal action during rapid whirling of the tube. As the increase of pressure and stress at the lower electrode was followed by the production of a permanent electric current, it must also have been followed by increased energy of chemical union of the metal and liquid a ” Ellectromotive Force to Pressure &c. 109 and an increase of electromotive force at that electrode ; the three kinds of pressure—mechanical, chemical, and electrical— varying directly together. The greater mechanical pressure at the lower electrode enabled the liquid and metal to chemically unite with greater energy, and thus permitted that electrode to become electropositive to the other. The fact that the strongest currents were usually obtained by the use of the most energetic chemical substances further support the view that the phenomenon is partly chemical, and it is well known that certain substances will only chemically combine whilst kept under pressure together. In all the cases in which the more positive metals, such as zine, were employed, both the electrodes were visibly corroded ; as, however, the electric current was excessively minute, only an extremely small proportion of this chemical action was inseparably associated with it; and as the currents were not due to ordinary chemical heat, any examination of the com- parative losses of weight of the two electrodes by corrosion would probably have been of but little value. The phenomena suggest some abstruse questions,— What is the most hidden cause of the current? Only a very funda- mental cause could have produced so large a proportion as 95 per cent. of currents in one uniform direction. The original cause must lie in some change of the potential motion of the molecules ; some kind of molecular energy must have been lost in order to produce the currents. The immediate cause was probably a small proportion of the potential energy of the motion of the superficial molecules which must have been transformed into current during chemical union of the metal and liquid, the other and far greater portion being directly changed into chemical heat. The questions why one portion is directly converted into electric current and another into heat, and why so largely into heat, I have not examined (compare Proc. Roy. Soc. 1884, vol. xxxvi. p- 8381; also M. B. Raoult, Ann. de Chim. et de Phys. 1867, pp. 137-193). We know that work is done during the act of putting on the pressure, and that this work may increase the energy of molecular motion; in addition to the energy communicated to the arrangement in this way, constant pressure may pro- duce constant current if there is a continual yielding of the molecules to it; but as only motion can produce motion, and as unchanging pressure isa purely statical phenomenon, if there is no such yielding unvarying pressure cannot be a real cause of continuous current. We know also that the properties of substances and the molecular motions to which those 110 Dr. G. Gore on the Relation of Volta properties are due vary with every change of mechanical pressure. If, therefore, pressure alters the direction or the velocity of molecular motion, it may act as a permitting con- dition so as to enable some of the unceasing motion of the molecules to expend itself in producing a permanent current, like such motion does in a voltaic cell; and this appears to be a reasonable explanation. Contraction of total volume by chemical union, being a yielding to pressure, may contribute to the result in the present case. As the production of current was conditional upon deference of pressure at the two electrodes, it must have been as much dependent upon the pressure and the state of molecular motion at one electrode as upon that at the other. And as we know that volta electromotive force is very intimately connected with velocity of the molecules, and that the two appear to vary directly together (see ‘“‘ A General Relation of Electro- motive Force to Equivalent Volume and Molecular Velocity,” Proc. Birm. Phil. Soc. 1892, vol. vil. pp. 63-188; The Electrical Review, vol. xxx. pp. 693, 722, 755, 786; and Phil. Mag. Sept. 1892, p. 307), it is probable that the greater degree of pressure at the lower electrode permits some of the molecules of liquid and metal to strike each other with greater velocity than at the upper one. It is worthy of notice that pres- sure has the same effect as dilution of the electrolyte, &e. upon volta electromotive force (zbzd.) ; as dilution and pressure each separately increases volta electromotive force, and as dilution is apparently attended by an increase of velocity of the mole- cules, it is reasonable to conclude that pressure is probably attended by a similar effect. It would be interesting to in- vestigate the relations of the current to the compressibility and elasticity of metals and electrolytes. The present results indicate that electromotive force may be due to unequal mole- cular pressure. Whatever may be the manner in which the molecular motions are affected by pressure, whether by altering their direction or their velocity, the experiments of this research show that they are influenced in essentially the same way in 39 out of 41 instances, and it is evident that only some very fundamental cause could produce such a uniform effect. The fact that nearly all the currents are in one direction suggests that the real cause of electromotive force itself can only be about one stage more fundamental than the cause of the currents. In all cases the currents obtained were results, not only of a difference of electromotive force between the lower metal and liquid and the upper ones, but primarily of the Electromotive Force to Pressure &e. Lie influence of pressure upon the electric potential of the metal alone and upon that of the liquid alone at each electrode. It is probable that an investigation of the effect of pressure upon the electric potential of the metal alone and upon that of the electrolyte alone would yield more uniform results than that of its effect upon the electromotive force of the two substances in mutual contact, because the conditions would then be more simple ; but as the effect upon the potential produced by a single compression would be extremely small, a series of compressions, with the effects of them accumulated by means of an electric condenser as in an influence machine, would be necessary in order to render the effect manifest. Such a research would probably show that pressure increases the positive potential of positive substances and the negative potential of negative ones. As pressure increases electro- motive force it must increase the two kinds of electric potential which constitute that force; thus in a case where a current occurs with a closed circuit, the two potentials are always pro- duced if the circuit is open. The facts also that the largest currents in the present research usually occurred with the most positive metals and the most negative electrolytes (see exps. 3 and 6), and the smallest frequently, though not in- variably, happened with the most positive electrolytes (see exps. 33, 34, 42, 43, 49, 50), support this hypothesis. Some of the cases in which no appreciable current was produced, or in which reverse ones occurred, might have been due to the pressure increasing the electropositive potential of the liquid as fast as, or faster than, that of the metal. Although some effect of the atomic or molecular weights of the substances employed upon the direction or magnitude of the currents must have occurred, none was observed (see Table III.) ; many additional experiments would probably be necessary to properly examine this question. I have not been able to suggest any explanation of the circumstance that diluted acids did not in any case produce a current ; nor have I been able to investigate in what manner the pressure may have affected the direction of motion of the molecules of the combining substances, but possibly some information might be obtained by examining the influence of pressure upon the thermal spectra of the substances and comparing the results with those obtained in this research. As the properties and molecular motions of substances vary with every change of temperature, it is probable that the electromotive force pro- duced by unequal mechanical pressure would vary with the temperature of the metal and electrolyte. 112 Relation of Volta Electromotive Force to Pressure §c. Liffect of Pressure upon Voltaic Couples. In all the foregoing experiments the investigation was limited to the influence of pressure upon the electromotive force generated by a single kind of metal and a single kind of liquid, and did not include its influence upon that of ordinary voltaic couples composed of pairs of metals or pairs of liquids ; it is evident, however, that the latter are only compound cases of the former. Gibault has already experimentally examined the effect of a pressure of 100 atmospheres on several kinds of voltaic cells, and obtained the following amounts of electro- motive force in volts :—Daniell’s cell (20 per cent. ZnSO,) +:0005 ; (27°56 per cent. ZnSO,)+°'0002 ; Warren De la Rue cells (1:0 per cent. ZnCl,)+°0007; (40°0 per cent. ZnCl.) —:0005 ; Volta’s cells —:06; Bunsen’s —-04; Gas battery +0°8 (Comptes Rendus, 1891, vol. cxiil. p. 465; The Hlectrician, 1891, vol. xxvii. p. 711). Owing to the greater complexity of the conditions in these experiments, the pro- portion of cases giving reverse effects was 30 per cent., or six times larger than in those with single metals in the present research. In all such experiments with voltaic cells, we have to con- sider not only the effect of pressure at the positive metal, but also that at the negative one. The results obtained in the present research show that the direction of the current which oceurs with zine and other positive metals is the same as that with gold and platinum ; so that the effect of pressure upon the negative metal of a voltaic couple would probably be in nearly all cases to produce a greater or less amount of counter electromotive force, which would either diminish or reverse the effect due to the positive one. The amount or balance of effect, therefore, obtained with a voltaic couple would usually be very much less than that with a single kind of metal ; this conclusion is confirmed by the results of Gibault’s experiments, in which the amounts of electromotive force obtained by a pressure of 100 atmospheres were very much less than those usually obtained in my experiments by a difference of pressure of only about 2 or 3 atmospheres. As the pressure alone attending the height of the liquid of a voltaic cell affects the electromotive force, it necessarily follows that the energy of such a cell is affected by gravity and varies with the altitude and geographical position of the cell. Pe Pts] XIV. On Radiant Energy. By B. GaLtrzine*. § 1. Introduction. TARTING with the far-reaching ideas of Faraday, Max- wellf has developed his theory of dielectrics, in which, by the identification of light with electrical vibrations, he comes to the conclusion that a ray of light must exert a certain pressure in the direction of its propagation, this pres- sure being numerically equal to the energy contained in each unit of its volume. One half of this energy is present in the electric, and the other half in electromagnetic, form. By an entirely different line of argument, derived from an application of the second law of thermodynamics, Bartoli t has arrived at the same result. His paper is extremely inter- esting, and the method by which he proves the eaistence of the pressure of light is free from objections, at any rate in the form given to it by Boltzmann§ in a more recent paper. But the process by which he calculates the numerical value of this pressure P appears to me to be wrong. Bartoli imagines a perfectly reflecting empty sphere of radius R, with a perfectly non-refleciing (black) sphere of very small radius yr atits centre. Let Q be the quantity of energy which falls on each unit of surface of the outer sphere in unit time. Then if the radius of this sphere be decreased by 6R, accord- ing to Bartoli the inner sphere receives an amount of heat g=2Q/V .47R?. dR, where V is the velocity of propagation of light. In this expression 2Q/V is the energy contained in unit of volume. Whether the energy can be expressed so simply or not, is not evident without further explanation. For the case of a cylinder, & times the energy which is v received by any normal section of the cylinder does noé repre- sent the energy contained in unit volume, as we shall see later. Boltzmann || has already pointed out that Bartoli does not appear to have considered the effect of rays with oblique incidence. Bartoli goes on to say that, since the inner sphere has increased its energy by an amount g, the work done * Translated from Wiedemann’s Annalen, vol. xlvii. pp. 479-495 (November 1892), by James L. Howard, D.Sc. + ‘Electricity and Magnetism,” vol. i. p. 144; vol. ii. p. 3983 (2nd edit.). t Sopra it movimenti prodotti dalla luce e dal calore e sopra i radio- metro di Crookes (Florence. Le Monnier, 1876). Also Nuov. Crm. [3] xv. pp. 193-202 (1884) ; Exner’s Repertoriwm, xxi. pp. 198-207 (1885). § Wied. Ann. xxii. p. 33 (1884). || Tom. ett. p. 35. Phil. Mag. 8. 5. Vol. 35. No. 213, Feb. 1893. I 114 B. Galitzine on Radiant Energy. against the pressure of light, viz. P .47R?. dR, must be equal to this, and hence 2Q a This conclusion appears to me to be wrong, although the - result obtained by a different method of reasoning differs from Bartoli’s formula only by a constant factor. Our system consists of the inner black sphere and the space between the two spheres, which also possesses a portion of the energy*. On reducing the outer sphere work is done ; not because the energy of the absolutely black body is thereby increased—for all the energy gained by the inner sphere is taken from the space between the spheres—but because the whole energy of the system passes from a lower to a higher temperature. Boltzmann f has also attacked the same question. Let H be the heat radiated from unit surface in unit time (Boltzmann denotes it by ¢(t)); then he finds for the pressure P of light against a perfectly reflecting wall the expression dE pa7 ft |r dt — EB], diy p=7 [r) ae av], T being the absolute temperature. He writes the constant of integration equal to zero. This formula enables us to caleu- late the pressure P numerically for any assumed law of radiation. The method by which Boltzmann obtains his formula is quite a legitimate one, but I differ from him as to the value of the numerical factor. The subject may be treated in a more simple manner, as I shall proceed to show. In conclusion | may draw attention to a paper by Lebedewf, who has made a very interesting application of the Maxwell- Bartoli theory, by comparing ‘the force of repulsion due to radiation with universal gravitation §. § 2. Deduction of the Formula for the Pressure of Light P. Imagine an empty cylinder AB, of length h, whose walls or * Cf. Thomson, Phil. Mag. ce p- 386 (1855). : Wied, Ann. xly. p-. 292 (1892 | Tomancit. § Cf. also Kolacek, Wied. Pies XXX1x. “Pp. 254 (1880). B. Galitzine on Radiant Energy. 115 and base B, are perfect reflectors, and in which B can be displaced after the manner of a piston. A is an absolutely h black body~ which may be re- placed, when necessary, by a . | perfectly reflecting wall. A te For simplicity, let the area of the cross section of the cylinder be unity. Let us denote by ¢ the emissivity of our black body, i. e. the quantity of heat which unit surface of it radiates out in a normal direction every second. In a direction making an angle @ with the normal to the surface the emissivity will be smaller, namely ecos¢. To obtain the total quantity of heat E radiated from a unit of surface each second we require to evaluate the following integral*:— 1/2 B=2me| COMM SING Adi me, 5 . «1 (i) 0 in which both e and E are functions of the absolute tempe- rature T only f. Now let us calculate the quantity of energy e in unit volume of our cylinder when the black surface A is at tempe- rature T. First of all imagine the cylinder to extend to infinity on the right, and let e denote the energy contained in unit volume in this case. We have obviously Ge Ee Sg OM ws oh ac atgye ev Cop) If the surface sent out all its energy EH in a normal direc- tion, we should have C= Vv’ or | oe 2H, . But in reality a quantity of heat 2aesindcosd¢dd is radiated at an angle lying between ¢ and ¢+d¢. The velocity Vg with which this energy is propagated in a direc- tion parallel to the axis of the cylinder is, according to the laws of reflexion, equal to Vcos¢. The amount of energy in unit volume will thus be greater, and we shall have, as soon as equilibrium is established, 72 sin b cos ie to 6. =2ire a ee gti) Te i ; \ Vo ¢ ND NE * Cf. Wiillner, Lehrbuch der Experimental-Physik, iii. p. 238 (4th edition, 1885). + Cf. Kirchhoff, Poge. Ann. cix. p. 275 (1860). ; 12 116 B. Galitzine on Radiant Energy. or, from (2), fe é= as 3 eo 5. «id ae c (3) e is likewise a function of T only (Kirchhoff). E denotes the amount of energy which crosses any section of the cylinder in a given direction during unit of time. In order, therefore, to obtain the amount of energy contained in unit of volume, we must multiply the quantity E, not by 2/V, but by 4/V. (CF. Introduction.) If P is the pressure exerted on the base B, we have TAvide P=1 7 pet é. First Proof. Let the piston B be in contact with A, and keep A at temperature T. Now let the piston B be moved as slowly as possible through a distance h. The amount of heat Q im- parted to the system, assuming the masses of A &c. to be infinitely small, is given by Q=eh+ Ph. All quantities of heat are expressed in mechanical units. If, now, we gradually reduce the temperature of A to zero, all the energy will be transferred from the cylinder to other bodies. When this has been done, let B be pushed back again to A without expenditure of work. The process is reversible, and as A’s mass is infinitely small the second law of thermo- dynamics gives us the following equation:— T T h de e+P Tagt T ={ T aT, (4) or pide pat|, ae, . ees which was to be proved. This formula differs, however, from that of Boltzmann by a constant factor. For, substituting for e¢ its value from (8), P=7[T| aan et-¥); ae 0 B. Galitzine on Radiant Energy. 117 whereas, according to Boltzmann, T Tl dH P=7(T) 7p l—E |. oe (64) 0 Second Proof. Start with B at a distance A from A, and let A have tem- perature T. Let us take T and / us independent variables. Consider, now, how much heat dQ must be given to the system when T increases by an amount dT, and i by dh. The work done in this case is Pdh, and dQ=d(he)+Pdh ; de dQ=(e+P)dh +h om aT. or The increase of entropy dS is therefore _ dQ _e+P h de It follows from this, since according to the second law dS must be a perfect differential, and since e is a function of T only, that Alb ee e ‘° e ° ° ® ° (7) This equation is an immediate consequence of equation (4), from which it may be obtained by differentiation. On integrating equation (7) we obtain P=1] 0 + | par], 0 P=1(G+ | pS a (8 = + | oa |-e. pe ee eri St) To make this formula agree with (5) we must put the con- stant C, equal to zero, which appears perfectly legitimate. We shall indeed see later that Pis proportional toe. If, then, for infinitely small values of T, e is proportional to any power of T, say e=AT”, the assumption C,=0 is clearly equivalent to the condition n>1. Third Proof—Yhis proof rests upon the consideration of a complicated cyclical process, which is the same in principle as that of Boltzmann. I have merely introduced a slight alteration, and drawn further conclusions from the equation which expresses the first law of thermodynamics. Suppose the piston B to be at A. Move B through a distance /,, the temperature of A being always kept at Ty. or 118 B. Galitzine on Radiant Energy. Let the heat required be Q;. Then, as in the first case, QO = = exh, + P Ay. e, and P, denote respectively the energy contained in unit volume, and the light or heat pressure, at temperature T). Now let A be replaced by a perfectly reflecting wall, and let the piston B be moved further away to a distance hg. In this process an amount of work + will be done, but as the operation is an adiabatic one the temperature must gradually decrease from T, to T>. hy “=| Pdh. . . 4 WE The principle of conservation of energy gives us ho aun —eaha= | Pdh; ... . ee hy or, for an infinitely small displacement, —d(ech)=P dh, . “o) Raa) This having been done, we can again replace the reflecting wall A by a perfectly black sur face, and either (1) oradually reduce this surface to zero temperature, and then, without doing any work, push the piston B back to A; or (2) keep the black surface at constant temperature T, and then bring back the piston B to A against the constant pressure P, (this latter being Boltzmann’s operation). The last process neces- sary to complete the cycle is the heating of A to temperature T,; this requires no energy, as its mass is infinitely small. In both cases the cycle of operations is reversible. Applying formula (4), the second law of thermodynamics gives us the following set of equations:— ée:+P, oe: “1 de éo+P, aah de . n=l pgp he=he| ee Li From these we obtain éo+P, ae ae aye €y hy— i —,—-h, =0, or e+P a( 7 h )=0, d(eh) + Pdh+hdP — fe (e+ P)dT=0; or, having regard to (10a), B. Galitzine on Radiant Energy. 119 de SAF) ior ls PAL thus leading us back to equation (7) again. Equation (10a) enables us to find a relation between T and h for adiabatic processes. As e, and therefore P, are functions of T alone, it follows from (10a) that 1° eae ae es uy Seca.» ix, 28 ne ley) or from (7), [de ee ree dT We can also obtain these formule: by a comparison of the two integrals in equation (11). These give Pinder, bo) {nf Tapa | =0, an)" Ee ea) 0 Td ak or AN Te Ner Le OT ae de dt In order to evaluate the expressions in equations (5) and (13), we should require to know the relation between radiating power and absolute temperature. But if a direct relation between P and e could be found by any means, it would enable us to obtain directly the unknown law of radiation by inte- erating equation (7). As I have said before, 1 do not consider Bartoli’s argument to be tenable. I have not succeeded in dis- covering a relation between P and e from purely mechanical considerations. Maxwell also, according to his own confession, was equally unsuccessful*. But the relation sought for may be deduced from the principles of the electr omagnetic theory of light, and indeed by a simple application ‘of Maxwell’s fundamental conceptions to our case, as Boltzmann} was the first to show. I should like to give a slightly different proof of Boltzmann’s relation, however. * Maxwell, ‘ Electricity and Magnetism,’ vol. i. p. 154 (2nd edit.). + Wied. Ann. xxii. p. 291 (1884). 120 B. Galitzine on Radiant Energy. We know that a ray of light exerts a certain pressure along its line of propagation, which is numerically equal to the quantity of energy contained in unit of volume of theray. If the beam is completely reflected the pressure is twice as great. A 5 (s4a Suppose for greater generality s is the area of the radiating surface A, and consider those rays which are emitted with inclination @ to its normal. According to the laws of re- flexion these will meet the other base B of our strazght cylinder at the same angle, as is diagrammatically represented in the figure. The quantity of energy radiated at the angle d is dH=27e sing cospdd s. We can assume all these rays to have the same direction. They exert on ab or a'l/, which are perpendicular to their direction of propagation, a certain pressure dp’, this being equal to dH/abV. As ab=s cos ¢, we have 277€ dp = ve sin d dd. To every element of a/b! there is a corresponding element of B, which is greater in the ratio of cos¢@ tol, and there- fore the force acting on each unit of surface of B is cos¢ times smaller than dp’. Besides this, the force acts in a direction making an angle @ with the normal to B. It follows that the pressure exerted on B is dp = dp! cos? $. If B is a perfect reflector we must double the above ex- pression in order to obtain the total pressure, and integrate for all values of @ between 0 and = Hence 72 (lr P= 2. vA, cos*¢ sin ddd, or, from (3), Pete. 6. re Formula (14) expresses the required relation. B. Galitzine on Radiant Energy. 121 We see, then, that P is proportional to e. If we substitute for P in formula (7), and then for e in equations (1) and (3), we find de __ 4e or di ay? Elias eames oo. ee Go) This is exactly Stefan’s* law of radiation, which is thus deduced directly from the principles of thermodynamics and the electromagnetic theory of light, as Boltzmann has already indicated. We have also Bee erah etree st) 4, OGD ERG) a formula of which further use will be made in the following sections. Hquation (14) makes it possible for us to establish a more simple relation between A and T. From (13) ,ot__t or Ah ae if Nes (Cy. ape ° e . ° ° ° ° (17) C, is determined by the initial conditions of the experiment. It will be observed, then, that in adiabatic and reversible processes, such as we have just considered, the temperature varies inversely as the cube root of the volume. § 3. The Meaning of Absolute Temperature. The energy contained in unit volume of our radiation- cylinder depends directly on the sum of all the electrical vibrations emitted at temperature T from the perfectly black surface, these being specified not by their wave-length, which is variable according to the nature of the external medium, but by their period or the number of vibrations per second, 2. If T=0 we must have alson=0. But ifT begins to increase new swings are constantly being added, and to every tem- perature there correspends a certain maximum rate of vibration Mmax, Which the black body is capable of emitting at that temperature. Plainly mmax 1s a function of T. FOCI. A icepah ARAM oD) Let us suppose we are dealing with only one ray (the whole energy in unit volume will be obtained by integration * Wien. Ber, Ixxix. p. 423 (1879). 122 _B. Galitzine on Radiant Energy. with respect to @). If we start with the general equations of the electromagnetic field the electric force F, at a point, which corresponds to any given time of swing, must be a periodic function of the time. Let the corresponding ampli- tude be a,. Ii the force were constant we should have for the energy contained in unit volume 1 = 3 AE, ° ° ° ° ° ° (19) k being the dielectric constant of the external medium. But in our case F is variable. To every F, there corre- sponds a particular dielectric constant k,, but the energy in unit volume for these particular swings is clearly proportional to a. Since k may be put equal to unity for all swings in vacuo, the total energy per unit volume (e) is obtained as a sum of the following form, e=const. 3 a?, the summation being extended to all vibrations which the body is capable of emitting at the temperature T. a? is a function of T and n. e@=fT,n). . 19.8 re) The function / depends directly on the distribution of energy in the normal spectrum, the term “spectrum” in- cluding all possible rates of vibration. If the energy is distributed in a continuous manner throughout the spectrum, the above summation becomes an integral. Let @(n)dn denote the probability of occurrence of waves whose rate of vibration lies between n and n+dn, then N»,=(T) e=eonst. | F(a, Dod@mdn. . eee For a perfectly black body which exercises no selective absorption, d(n) is constant, but we ay leave equation (21) in its more general form. From ( (15), (1), and (8) it follows that Dis const." Dd(n)dn: ) (eee 0 The expression under the integral sign is a quantity which is proportional to the square of the Pomnesipon tis electrical displacement. We thus obtain the following result. The absolute tem- B. Galitzine on Radiant Energy. 123 perature depends directly on the sum total of all electrical displacements, and the fourth power of the absolute tempera- ture is directly proportional to the sum of the squares of all the electrical displacements, these latter being calculated for vacuum. The equation (22) enables us to solve another problem. If we differentiate it with respect to T,, we have n,,=(T) Tt ; dw T? = const. [ | b(n)dri + f(%myL) b(n) ap: If the function f is known, that is if we know completely the distribution of energy in the spectrum, we are led to an equation of the form Sete Sr El, 7), from which the unknown function @ can be determined. The converse problem untortunately cannot be solved ; that is to say, a knowledge of the function o tells us nothing con- cerning the distribution of energy in the spectrum, because o/(n, T)/OT cannot be equated to zero*, § 4. Relation between the Radiating Power and the Surrounding Medium. Let us now imagine our radiation-cylinder to contain some * Cf. on this subject the following references :—Draprr, Phil. Mag. [3] xxx. p. 340 (1847): KnoBiaucu, Pogg. Ann. Ixx. pp. 205, 337 (1847) : Jaques, Inaugural Dissertation Johns Hopkins University (Baltimore, J. Wilson & Son, 1879); Bevrbl. ii. p. 865 (1879): Sreran, Wien. Ber. Ixxix. p. 423 (1879): Crova, Ann. de Chim. et de Phys. [5] xix. pp. 472-550 (1880): Laneiey, Comptes Rendus, xcii. p. 701 (1881); xcil. p. 140 (1881), and later papers: DEsains, Comptes Rendus, xciv. p- 1144 (1882); xcv. p. 485 (1882); xevil. pp. 689, 732 (1883): LrecuEr, Wied. Ann. xvi. p. 477 (1882): CHrIsTANSEN, Wied. Ann. xix. p. 267 (1883) : SCHLEIERMACHER, Wied. Ann. xxvi. p. 287 (1885): BorroMLEy, Beibl. x. p. 569 (1886): H. Weser, Wied. Ann. xxxil. p. 255 (1887) ; Math.-naturw. Mitth, aus den Sitzungsber. d. Berl. Akad. xxxix. pp. 933, 565 (1888); Berbl. xiv. p. 897 (1890): KovEstigerHy, Wied. Anz. xxx. p. 699 (1887); Ast. Nachr. Nr. 2805, p. 329 (1887) ; Abh. der ungar. Akad. der Wiss. xii. Ny. 11; Math. u. naturw. Ber. aus Unyarn, iv. p. 9 (1887) ; v. p. 20 (1887); vil. p. 24 (1889); Berd. xii. p. 346 (1888) ; xiv. p- 116 (1890): W. MicuEtson, Journ. d. russ. phys.-chem. Ges. |4] xix. p. 79 (1887); [6] xxi. p. 87 (1889) ; Journ. de Phys. [2] vi. p. 467 (1887) ; Beibl. xiv. p. 277 (1890): EmpEn, Wied. Ann. xxxvi. p. 214 (1889): GRaAETZ, Wied. Ann, xxxvi. p. 867 (1889): Lord Rayteicu, Phil. Mag. xxvii. p. 460 (1889): Ferrer, Sill. Journ, [8] xxxix. p. 187 (1890) ; BLeibl. xiv. p. 981 (1890): Epier, Wied. Ann. xl. p. 5381 (1890): Vioiie, Comptes Rendus, cxiv. p. 734 (1892) ; Journ. de Phys. [8] 1. p. 298 (1892). 124 B. Galitzine on Radiant Energy. diathermanous body whose dielectric constant for swings of frequency nis k, As the temperature remains the same, the range of frequencies is the same as before, namely, from n=0 ton, =o(T). Hquation (19) shows that the energy transferred across any section of the cylinder will be £, times greater than before, for swings of frequency n, because the external medium takes part in the vibratory movement. Also, since the velocity of propagation V, of these particular waves is smaller than in vacuum, the energy present in each unit of volume will be increased k,V/V,-fold ; and if e, is the total energy per unit volume we have, as in § 3, — é Ny»=aXT) a= const. | kaa fn, TYG (n) dn, . a ees} 0 n the constant having the same value as in equation (21), which may be looked upon as a special case of the more general equation (23). If we neglect the effect of dispersion of the different waves we can write down the mean values k and V; instead of kn and Vn, and we thus obtain or, having regard to equations (1) and (3), Are, V Arre from which , i ke. This is exactly Clausius’s law of radiation*, since, according to the electromagnetic theory of light, provided we neglect dispersion, we are perfectly justified in taking the square of the mean index of refraction as equal to the dielectric constant. Clausius’s law of radiation appears, then, to be a necessary consequence of Maxwell’s fundataental conceptions. § 5. Meaning of the Second Law of Thermodynamics. The above investigation of the radiant energy in a cylinder enables us to understand more clearly the meaning of the second law. In the course of the third proof of the formula * Clausius, ‘Mechanical Theory of Heat, p. 314, § 10 (Macmillan, 1879); Bartoli, N. Com. [8] vi. pp. 265-276 (1880); Bezbl. iv. p. 889 (1880). B. Galitzine on Radiant Energy. 125 for the pressure of light we arrived at equation (10a). In that case the operation considered was an adiabatic one, and consisted in giving to a new portion of space, or let us say a new volume of zether dh, a quantity of energy dq=e dh. This transfer of energy to a new mass of ether is accom- panied, as we have seen, by a certain expenditure of work Pdh. We have, then, two correlative phenomena, and in the limit, for infinitely small displacement, only 4 of the energy transferred can be converted into external work. We have, indeed, from (14), dt as dq ee The previous investigations enable us to calculate the same ratio. for adiabatic displacements of finite magnitude; and this ratio is only a function of the initial and finai temperatures. From the same equation (10a) it follows that, if we wish to concentrate a certain quantity of energy into a smaller mass of ether, this can only be done by the expenditure of external work, the first law being obeyed throughout the process. In this lies the closer explanation of the second law. From equations (10) and (9) we find, for finite displace- ments, eyhy —ehy=T= U,— Uz. ° ° ° ° . (24) is and U, denote the quantities of energy in the cylinder at the beginning and end of the operation. From equations (14), (16), and (17) it follows that N= SOC EI! me 2 AL (95) Insert this in equation (24) and note that 30C,3 may be determined from the initial conditions ; we have T= a 1 The available work is directly proportional to the fall in temperature (Second Law). Itis only in the case of T,=0, i.e. when the given quantity of energy U, is distributed over an infinitely great mass of ether (since according to (17) T=0 only when h=oo ), that the whole energy can be transformed into externa] work. In conclusion, let us compare the quantities of energy 126 B. Galitzine on Radiant Energy. present at the beginning and end of a reverséble adiabatic operation. These give ee Ue ah, Substituting from (25) and (17), 1 Ben i. Agus Who As fh represents the volume (v) of the sther over which the given quantity of energy is distributed, the above equa- tion may be written U “> = constant. This is a statement which is probably capable of further extension. It expresses the fact that in adiabatic and re- versible processes the quantity of disposible energy is inversely proportional to the cube root of the volume throughout which the energy is distributed. The statement does not involve the absolute temperature, but it really expresses the same principle as the second law of thermodynamics. § 6. Summary of Results. 1. Bartoli’s proof is not admissible in ail its details. 2. The application of the second law of thermodynamics enables us to calculate the pressure of light, as well as the changes of temperature in adiabatic and reversible operations (Boltzmann). 3. The fourth power of the absolute temperature is directly proportional to the sum of squares of all the electric dis- placements. 4. Clausius’ law of radiation is an immediate consequence of Maxwell’s fundamental conceptions. 5. The transfer of energy to new masses of ether is accom- panied by the expenditure of work in the case of reversible operations. 6. In the case of adiabatic and reversible processes the amount of disposible energy is inversely proportional to the cube root of the volume throughout which this energy is distributed. ae pereliay” i- XV. Some Experiments on the Diffusion of Substances in Solution. By SPENCER UMFREVILLE PickgRING, W.A., Os TEXHE following determinations of the comparative rates of diffusion of various non-electrolytes were intended to be preliminary to a more extended investigation, but, as I do not see my way at present to continue the work, I think it well to put on record those results which have so far been obtained. Osmotic pressure is held to be due simply to the gaseous impact of the dissolved substance, and is theretore proportional to the number of molcules per unit volume, the temperature being constant. Now, by Graham’s law, the rate of diffusion of a gas should be, ceteris paribus, inversely as the square root of its density, or of its molecular weight. Hence, at a given temperature and pressure the product of the molecular weight, m, by the square of the rate of diffusion, v, should be a constant. ‘lhe relative values for v in the case of different bodies might be determined by sunple diffusion-experiments if these could be conducted under perfect conditions: namely, the diffusing liquid remaining of a constant strength through- out, and the water into which diffusion is taking place remaining uncontaminated with the substance. ‘The present results seem to show, either that the above supposition as to osmotic pressure is incorrect, or that the conditions obtainable in diffusion-experiments are very far from obtaining to ideal perfection ; for the values deduced for mv? are by no means constant, even in those cases where the substances behave normally as to their osmotic pressure, i.e. where the solutions of equal molecular strength give the same osmotic pressure, this latter being measured by the depression exercised by them on the freezing-point of the water in which they are dissolved. The method adopted was that termed by Graham jar- diffusion. The solutions under examination were placed in an open jar inside a large vessel of water, and the amount of substance which had ditfused out of the former in a given time was ascertained by determining the strength of the remaining solution. The inner jars were beakers of a cylin- crical form with ground flanges: they were ground also on the bottom, and rested on inverted ground-glass saucers placed in the centre of the large outer glass jars. Before being filled, each jar was placed in position and adjusted so * Communicated by the Author. 128 Mr. 8. U. Pickering on the Diffusion that the mouth of the inner jar should be exactly level. The jars were marked so that they could be replaced in the proper position after being filled. When filled they were closed by glass plates with rods attached to them, and then lowered inside the larger jars which had previously been filled with water. The glass plates were then removed very slowly and earefully. At the end of the time allowed for diffusion the plates were replaced on the jars, the latter were removed from the water and the strength of their contents determined. Both the large and small jars were filled two days before the latter were placed inside the former, in order that the temperature of the cellar in which the determinations were made might be attained; and after the inner jars had been placed in position a further period of five hours was allowed before the glass plates were removed, so that any disturbance of temperature which had occurred in placing them in position might subsice. The capacity of the inner jars was 480 cubic centim., their internal diameter was 70 millim., and their internal height 125 millim. About three dozen of them were made, and of these the twelve which were found to be most uniform in size were used in the determinations. The extreme ditterence in the capacity of the largest and smallest of these twelve was 3°3 per cent., and the extreme difference of their superficies at the mouth was 3°8 per cent. ‘The outer jars contained 12,000 cubic centim. of water, or twenty-five times the volume of the inner jars. The mouths of the jars were about midway between the surface and bottom of the water in the inner Jars. The strength of the solutions remaining in the jars at the end of the experiments was determined by means of their freezing-points. ‘The solutions taken to start with were made up by weighing. The freezing-points of these, and also of weaker solutions obtained from them by dilution, were deter- mined, and from these results the strength of any solution having a given freezing-point could be calculated. In order to minimize any errors due to possible irregularities of the freezing-points when plotted against composition, the solutions of known strengths, of which the freezing-points were deter- mined, were selected so as to approach as nearly as possible to the strength of the solution left in the diffusion-jar. The strength of the solutions taken was, as a rule, about 0:3 molecule to every 100 molecules of water, showing a depression of the freezing-point of water amounting to about 0°:3 ; about one third of the dissolved substance had diffused out by the end of the determination, the decrease in the mR of Substances in Solution. 129 freezing-point measured being thus about 0° 1. The water into which the diffusion had taken place would at the end of the experiment contain only about 4 molecules of the sub- stance to every 100,000 H,O. ‘These proportions had neces- sarily to be modified in several instances, and in such cases it was assumed that, in accordance with Graham’s results (in upport of which some of the present results may also be adduced), the rate of diffusion varied directly as the number of molecules present in a given volume of solution, or, more roughly, in a given weight of water. The determinations were made in two separate series, marked (1) and (2) respectively in Table I., which contains the results. In the first series the temperature varied from 12°1 to 15°3, the time allowed being probably 18 days, the record of the exact time having been unfortunately lost : in the second series the temperature was 16°:0 to 18°:2, and the time was 25 days. Various steps were taken to estimate the magnitude of the probable errors. In the first place, the error due to any disturbance occurring in removing and replacing the glass plate from the inner jar was found to be inappreciable. A blank experiment in which these opera- tions were performed showed that the solution of cane-sugar which the inner jar contained gave exactly the same freezing- point before and after the operations, 2. e. within the estimation-figure of the thermometric reading, which was 0:05 millim. or 0°:0005. Secondly, in the first series dupli- cate determinations were made with each of the substances cane-sugar, acetic acid, and urea: the differences in the freezing- oints of the solutions obtained in each pair were ‘O01L1°, "0062°, and -0026° respectively, mean 0:00338°, or about 3 per cent. of the actual decrease measured, a quantity fully accounted for by the difference in size of the jars. Three per cent. in the actual decrease, however, represents only 1:24 per cent. in the proportional decrease (or actual decrease — mean freezing-point), which is the quantity which is taken to represent the rate of diffusion v; and an error of 1°24 per cent. here will represent an error of 2°4 per cent. on the values of the supposed constant mv’. Thirdly, glycerine solutions of the same strength were used in both series, and so also were cane-sugar solutions of nearly the same strength : the relative values for mz? in the two series were 1 ; 2°586 in the case of glycerine, and I : 2°567 in the case of cane-sugar, the difference between the two ratios amounting to only 0°3 per cent. The results of the diffusion-experiments are given in Phil. Mag. 8. 5. Vol. 85, No. 218, Feb. 1893. Ix 130 Mr. 8S. U. Pickering on the Diffusion Table I., the supplementary freezing-points necessary for the calculation of the strengths of the final solutions being given in Table Il. (In the case of cane-sugar and acetic acid the determinations used for this purpose have already been published, Berichte d. deutsch. chem. Gesell. xxiv. p. 3329.) The values in the table refer to the weight of anhydrous substance, the water of crystallization, whenever present, having been allowed for. This water, in the case of alloxan, was found to be 3H,O; whereas in the cases of gallic acid, tannin, and raffinose, 1, 2, and 5H,0 were taken as being respectively present. The proportional decrease of freezing- point or strength of the solution is the fraction which the actual decrease is of the mean freezing-point or strength. The molecular weight m’ is deduced from the freezing-points in accordance with van’t Hoff’s formula mean strength x 18°9 nm = mean f.-p. The values, it will be seen, agree fairly well in most cases with the theoretical molecular weights. The sugars as well as the tannin and dextrin were ob- tained from Messrs. Trommsdorf. The dextrin, however, was doubtless very far from being pure (indeed pure dextrin has never yet been obtained), and very little weight can be attached to the results obtained with it. The sample of amylodextrin I owe to the courtesy of Mr. Horace Brown: unfortunately, however, the solution used deposited some of the substance during the experiments in the insoluble form, and hence the results with it are very doubtful; for not only is the mean strength of the solution uncertain, but the amount which had diffused out is also uncertain; for this had to be estimated in the diffusate, a large quantity of it being evaporated to a small bulk so as to “obtain a depression of freezing-point sues for measurement ; while, to correct for solids dissolved from the dish by the liquid during its evaporation, a similar volume of water was evaporated in the same manner. The calculated molecular weight of the amylo- dextrin was obtained from the freezing-point of the initial solution, and of that entered in Table II. The values which these gave were 2519°4 and 2452°8 respectively. The resnlts with gallic acid are equally uncertain for a similar reason, the solution taken having been too strong, and having deposited crystals during the course of the expe riment, In the case of pyrogallol the liquid used to make the solu- of Substances in Solution. 131 tion, and also that into which it diffused, was a very weak solution of sulphuric acid of which the freezing-point was 0°-0441. This prevented all but a trace of oxidation of the pyrogallol. The tannin used was probably not pure; but the difference in the calcuiated molecular weights deduced from the determinations in the two series is due to the solutions used being of different strengths, and to the fact that the molecular depression of the freezing-point diminishes rapidly as the strength of the solution increases. The depressions, I may mention, appear to show some marked irregularity ; for when the four determinations (the two in Table I. at the initial strength, and the first two in Table II.) are plotted out, they do not all lie on any simple curve, either the detent: nation at 12 parts to 100 giving much too small a value, or that at 16 parts too large” a value. Another speciinen of tannin was examined as to the freezing-points, and the results, ~which are the last four given in Table II., show the same peculiarity. This sample, however, gave throughout smaller values than that used in the diffusion-experiments, and the three stronger solutions of it deposited some tannin as well as ice in the freezing-point determination. The first sample did not do so. In order to make the results of the first. series more easily comparable with those of the second, the values for mv? obtained in the former have been multiplied by 2°577(=2), in accordance with the results obtained with glycerine and cane-sugar, as mentioned above. The values for mv’ are, as will be seen, very far from being constant. They vary from 16-09 with pyrogallol (omitting the doubtful result with gallic acid) to 46°81 with the weakest solution of cane-sugar; a variation of some 200 per cent., which cannot be in any way explained by the purely experimental error, since this, as has been mentioned, does not exceed 2 to 38 per cent. When we take the molecular weight deduced from the osmotic pressure (freezing-point) itself, m’, instead of the theoretical molecular weight, the constancy is in most cases scarcely improved; and, indeed, in those three cases where these calculated mo- lecular weights do not agree with the simple theoretical weight, the values for m/v? are made much less nearly con- stant, and attain the enormous proportions of from 72 to 260. 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TI8- GPL G6TE- LION. | S8T&.— | SL0%.— 6698. — wade y i “‘oseex00p a te ie ae es “sasva.oop ies SS e Bae WOAT jeoy jeaoy |‘osvorooq | ‘uvop | ‘Teun | ‘penimy jeuoy |osvetooq | ‘uvoy | ‘yeung | ‘Teyy poyepnoRg| -e100y], || -todorg -10dorg “qysio MA Le[NoaTOW AMEE *SUOIYNIOG 94} Jo squrod-surzo0A iT 1948 MA JO NOT OF S91Bq—'suOIyNTOg Jo yysueayg "SUOIJVULLUIO}O(T OY} JO S}[NSoyY—'] AIAVy, puoc os (2) scouLyesy mes (G) — asogTe Ty, reese (z) ‘“ seuss (gz) & roses (g) & esses (BZ) “ “ees (7) cedns-oueg reese (z) “s Hee (qT) uraUey, “* (z) ungxopopéury se eeee (Z) oer UlYyxo(q (Z) poe ore “"(T) plow OLLB4.U8 7, eveee (J) UCXO]LV (Z) joresoars Py) pouetd Hees (g) «s “"" (7) aura0dT49, meee CT) Peetal eaeeee (1) plow ooo yw ‘vouRysqng a | On the Diffusion of Substances in Solution. 133 Taste II.—Supplementary Freezing-point Determinations. Parts to Parts to Substance, 100 of F.-p. Substance. 100 of | F.-p. Water. Water. Tartaric acid...... 2152 | —-2966 | Dextrin oo... 97-484 | — -6208 2G) oe 1425 | —-2000 ASHEN va PEA AeE AAS, 47-943 | —1:1082 Glycerine ......... 1-453 | —-3023 || Tannin ............ 2557 | — 0440 GHOSE... scc0s 4-670 | —:2463 ih Deh Late ae 12°310 | -- -1221 Pyrogallol.......... 1603 | —°2228 say LIE Aiea SPE aves 15°804 | — ‘1110 Gallic acid... 0667 | —-0697 Fy MA ode es 10184 | — -O844 Sel isieis0 slenisic 07133 | —-0180 ah sete epee 4°983 | — -0542 Raflinose ......3.. 0-640 | —:2669 3h AK Cae: 2-473 | — -0342 Amylodextrin ...| 7940 | —-0609 The “molecular’’ depression, which, on the theory of osmotic pressure, will be proportional to mv’, must, when we take the molecular weights calculated from it (m’), be an absolute constant, whereas the values for this same quantity (m’v”), when deduced from the diffusion-experiments, and when these same molecular weights are used, are far from being constant; moreover, while the ‘theoretical’? mole. | cular weights give the values of mv’ in the diffusion expe- riments with dextrin, amylodextrin, and tannin as being similar to those with the other substances investigated, they will, when used for calculating the molecular depression, give values from 4 to ith only of thuse obtained with the other substances investigated. These values are given in the last column of the table: molec. dep. = (mean dep. x m) + (mean strength x 17:96). The fact that the results with dextrin, amylodextrin, and tannin are of doubtful accuracy must, it is true, weaken the strength of any conclusions based on them. But, on the other hand, the fact that they do not give exceptional values for mv” renders it probable that they are not very inaccurate ; and, moreover, the exceptional values which they give for mv are not out of harmony with the results with the other substances ; for the sugars, where the molecular weights are large, give values which are considerably larger than those given by the other substances examined. There seems indeed to be a general tendency for m/v? to increase with the mole- cular weight of the substance diffusing: thus, with the first seven substances entered in the table we have molecular 134 .Prof. J. G. MacGregor on Contact-Action weights from 60 to 150, and the value of mv" is generally about 20: with the last three substances in the. tabie, where the molecular weights are high, 314 to 430 (taking the calculated values mm’), m’v? is much larger, namely over 30; while dextrin, tannin, and amylodextrin show still larger, and, taken in their order, increasing molecular weights, and also larger and increasing values for m’‘v*. Thus it would appear that with higher molecular weights the rate of diffusion is abnormally large. The exceptionally large values for mv? in the case of the weakest solution of cane-sugar is remarkable, but in the absence of a duplicate determination it is well not to lay much stress upon it. XVI. Contact-Action and the Conservation of Energy. By Prof. J. G. MacGrecor, M..4., Se.D.* (EVERAL years ago Prof. O. J. Lodge, in a series of papers published in this Magazinet, proposed new definitions of work done and energy, and claimed (1) that by their aid he had deduced from the third law of motion and the hypothesis of universal contact-action alone, a law (which he called the law) of the conservation of energy ; (2) that the law thus deduced was an extension of, and fully as axiomatic as, the law ordinarily enunciated under the same name ; (3) that action ata distance might be shown to be incompatible with Newton’s third law, or the law of the con- servation of energy, or both; and (4) that energy cannot be transferred without being transformed, or transformed without being transferred. ‘These claims, though primd facie so extraordinary as necessarily to have drawn attention, have never, so far as | am aware, been seriously challenged, and it is, perhaps, somewhat late in the day to challenge them now; but the remarkable progress which has recently been made in the application of contact-action theories, seems to make it desirable that they should be subjected to examination. (1) Lhe Deduetion of the Conservation of Energy. In the first version of the argument by which this deduction is made t, Prof. Lodge seems to me (a) to assume the ordinary law of the conservation of energy in addition to the third law _ * Communicated by the Author. + Phil. Mag. [5] vols. viii. (1879) p. 277, xi. (1881) pp. 36 & 529, xix. (1885) p. 482. + Ibid. vol. viii, (1879) p. 278. and the Conservation of Energy. 1385 of motion and contact-action, and (0) to deduce, not a law of the conservation of energy, but of its conservation during transference merely. Paje T he unacknowledged assumption is made in the “ de- finition ” of energy :—‘ Whenever work is done upon a body, an effect is produced in it which is found to increase the working-power of that body (by an amount not greater than the work done) ; hence this effect is called energy, and it is measured by ‘he quantity of work done in producing it. Whenever work is done by a body, 27. e. anti-work done on it, its working-power is found to be diminished (to at least the extent of the work done), and it is said to have lost energy — the energy lost being measured, as before, by the anti-work done in destroying it.” ‘The words ‘‘is found ” indicate an appeal to experience. We may readily recognize what it is, if we note that the increment or decrement of w orking-power which is produced in a body on or by which work has been done, may be kinetic or potential, and that, as Prof. Lodge says*, “for a body to possess kinetic energy you must have not merely motion, you must have a guarantee of persistence of motion, the body must possess inertia,” and “ for a body to possess potential energy we must have two things—the exer- tion of a force, together with a guarantee that that force shall be exerted over a certain distance ; 2. e. a continuance of the force even after motion is permitted.” If, then, these two guarantees be expressed quantitatively, so as to ensure fh equality of the change of working-power to the work done, they will form a statement of the experience to which appeal is made. When so expressed, the former is seen to be Newton’s second law of motion, and the latter the axiom that the work done by the mutual forces between the parts of a material system during any change of its configuration de- pends only on the initial and final configurations. If these guarantees cannot be deduced from the third law and universal contact- -action, they are thus unacknowledged assumptions in the argument under consideration, We may assume that Prot. Lodge will not hold it to be possible to make this deduction in the case of the latter of the two assumptions mentioned. He does hold, however, that Newton’s second and third laws of motion are ditterent aspects of one law t, and he may therefore regard the first of the two guarantees mentioned above as not forming an addi- tional assumption in his argument. I have not access to ‘ The Engineer’ of 1885, in which he says his argument in support * Phil, Mag. [5] vol. xix. (1885) p. 4865. + Ibid. vol, xix. (1885) p, 488, 136 Prof. J. G. MacGregor on Contact-Action of this view is published. But in the edition of his book on Klementary Mechanics which bears the date 1892, he reaches this conclusion in the following way (p. 56) :—“ It [ Newton’s third law] is deducible from the first law of motion (see Max- well, ‘ Matter and Motion’), for if the forces exerted by two parts of the same body on each other were not equal and opposite, they would not be in equilibrium ; and consequently two parts of the same body might, by their mutual action, cause it to move with increasing velocity for ever, the possi- bility of which the first law denies. We have already shown that the first law is a special case of the second, and now we have deduced the third from the first; hence all are really included in the second, which is therefore excessively im- portant.” ‘That the first law is a special case of the second ts obvious ; but that the third is deducible from the first in the above way I have elsewhere * endeavoured to disprove. It is not necessary to repeat the discussion here ; for it will probably be sufficient to point out that the equality and oppo- sition of the action and reaction of two parts of the same body do not constitute the third law of motion, that law asserting the equality and opposition of the action and reaction between two bodies, to each of which the first law applies. That this criticism is sound becomes especially obvious if we reflect that the laws of motion, as fundamental hypotheses of dy- namics, must be held to apply to particles, not to extended bodies ; and the above argument is clearly inapplicable to a particle. The unacknowledged assumptions are thus not deducible, at least have not been deduced, from those admittedly used. Now the law of the conservation of energy, as ordinarily enunciated, may be deduced from these-two assumptions alone. Hence, in the argument under consideration, Prof. Lodge assumes the ordinary law of the conservation of energy in addition to the third law of motion and universal contact- action. (6) The following is the conclusion which he draws :— ““Trence the energy gained by the first body is equal to the energy lost by the second; or, on the whole, energy is neither produced nor destroyed, but is simply transferred from the second body to the first.” This states only that energy is conserved during transference, and says nothing as to its fate after transference to the first body, and during residence * In an Address on the fundamental hypotheses of Dynamics, read at the last Meeting of the Royal Society of Canada, and to be published in vol, x. of its Transactions. See abstract in ‘Science,’ vol. xx. (1892) page and the Conservation of Energy. 137 in it. The law deduced is thus not a law of the conservation, but of the transference of energy. Obviously, with the assumptions which seem to me to have been employed, the complete law of conservation might have been deduced. But the conservation of energy during residence in the body could not have been proved without the explicit employment of the two assumptions involved in the definition of energy. In a second yersion* of the above argument, Newton’s third law and contact-action are the only assumptions made ; but the conclusion drawn is not a law of the conservation of energy in the sense of working-power. The definition of energy in this argument is quite different from that of the earlier paper :— “ Hnergy is that which a body loses when it does work ; and it is to be measured as numerically equal to the work done.”” There is here no reference to working- power. loss of energy is simply a synonym for work done by, and gain of energy for work done on. The conservation of energy which Prof. Lodge claims to have deduced is there- fore the conservation of the work done on two bodies during mutual action, whichis of the same nature as the conservation of their momentum, and is quite consistent with the non- conservation of their working-power. (2) Generality and Axiomatic Character of Prof. Lodge’s Law. It will be obvious that, as Prof. Lodge’s definition of energy is different from the ordinary definition, his law of conserva- tion cannot be the same as that ordinarily enunciated under the same name. He says himself it is “ probably a slight (very slight) extension” of the ordinary law f. We have seen, however, that in deducing it he assumes the ordinary law, the third law ef motion and universal contact-action. It is therefore merely the form which the ordinary law takes in the particular case of contact-action with equal reaction. This conclusion is borne out by a consideration of the definition of energy quoted above. Work done and the working-power of a body having been so defined ¢ as to make * Phil. Mag. [5] vol. xix. (1885) p. 483. + Ibid. vol. xi. (1881) p. 533. t “ Whenever a body exerting a force moves in the sense of the force it exerts, it is said to do work; and whenever a body exerting a force moves in the sense opposite to that of the force it exerts, it is said to have work done upon it, or to do anti-work, the quantity of the work being measured in each case by the product of the force into the distance moved through in its own direction.” ‘The working-power of a body is mea- sured ‘by the average force it can exert, multiplied by the range or distance through which it can exert it.” Ibid. vol. viii. (1879) p. 278. 138 Prof. J. G. MacGregor on Contaet- Action their denotation identical with their ordinary denotation, pro- vided the third law of motion hold, energy is detined quali- tatively as being the working-power = a body, and quanti- tatively as being measured by “the work done in producing it. The ordinary definition of energy is working-power simply, whether that power be possessed by a body or a system, its measure being the work the body or system can do. Prof, Lodge’s energy will therefore be identical with energy in the ordinary sense only in cases in which his work done and his werking-power are identical with ordinary work done and ordinary working-power, and in which the working-power of a system is the sum of the working-powers of the bodies of which it consists. Now this latter condition requires that the actions between the bodies of the system shall occur only at constant distance. Tor if the actions might occur at variable distance, a part of the working-power of the system would be potential working-power which could not be said to be pos- sessed by the bodies singly. The former condition is satisfied if the third law of motion hold. Hence Prof. Lodge has so defined energy as to make its denotation identical with the ordinary denotation only in cases of action with equal reaction at constant distance. Prof. Lodge asserts also that his law is “ fully as axiomatic as’ the ordinary law*. Mere assertion, however, cannot make two propositions equally axiomatic. They must be proved to be so. And the test is very simple. If they are applicable with equal generality in the investigation of dyna- mical phenomena, they are equally axiomatic ; if not, they are not. Now, if there be actions in nature which are not actions “at constant distance, Prof. Lodge’s law is not applicable to them, while the ordinar y lawis. Even if it be admitted that all actions in nature are contact-actions, there are many groups of phenomena which, in the present state of our knowledge of them, cannot be investigated on the hypothesis of contact-action. The early staves. of their investigation must be conducted by the aid of the fiction of action at a distance ; and in such stages Prof. Lodge’s law is not applic- able, while the ordinary law is. Hence Prof. Lodge’s law is not so general in its applicability as the ordinary law. (3) Deduction of Contact-Action. In Prof. Lodge’s argument to prove the incompatibility of action at a distance with the third law of motion and the law of the conservation of energy 7, he seeems to me neither to * Phil. Mag. [5] vol. xi. (1881) p. 533. t Ibid. vol. x1. (1881) p. 36. and the Conservation of Energy. assume a law of the conservation of working-power. deduce contact-action. The energy of which he assumes the conservation is ( in the same way as in the second version of his deduction wu the law of conservation :—A body ‘is said”? to have lost or gained an amount of energy numerically equal to the work done by or on it respectively. There is no reference to working-power. What he assumes, therefore, is the conser- vation of the work done on two bodies during their mutual action. The conclusion drawn is that “ the two bodies must move over precisely the same distance in the same sense,” which is action at constant distance, not contact-action. Nor does the assertion that they are “practically ” the same make it contact-action. It is obvious, however, that if the conclusion reached above is sound, viz., that Prof. Lodge’s law of the conservation of energy is the ordinary law expressed for the particular case of action with equal reaction at constant distance, action at variable distance must be incompatible with it and the third law of motion. The argument to show action at a distance to be incom- patible with the law of the conservation of energy alone is as follows *:—“‘ If it were possible for two bodies exerting stress — on one another to move over unequal distances, then it would be possible to obtain work without the anti-work, and thus to get a new source of energy (technically called the per- etual motion) ; but, asa fact of experience, it is not possible.” Clearly, in the case supposed, there would be a new source of energy as defined by Prof. Lodge. But a new source of energy as thus defined does not imply the perpetual motion. For in such a case there would be working-power which could not be called energy according to the definition; and the ordinary law of the conservation of energy tells us that, provided the stress supposed to act were independent of the velocities of the bodies acted upon, the change produced during the motion in this portion of the working-power of the system would be such as to render the perpetual motion impossible. No attempt is made, in the papers cited above, to show action at a distance to be incompatible with Newton’s third law of motion alone, although it is asserted t that the incom- patibility may be proved. * Phil. Mag. [5] vol. viii. (1879) p. + Ibid. vol. Xi. (1881) p. 36. 140 Prof. J. G. MacGregor on Contact- Action (4) Transference and Transformation of Energy. Prof. Lodge’s argument to show that, on the assumption of contact-action, “‘energy cannot be transferred without being transformed,” is as follows *:—‘ When a body possess- ing potential energy does work, its ‘range’ f necessarily diminishes, while the motion of the body on which the work is done increases. Qn the other hand, when a moving body does work its motion diminishes, and the body which resists the motion, since it yields over a certain distance, gains po- tential energy.” It seems to me that these sentences would be equally accurate if we were to subject them to “ double decomposition,” after which process they would read thus :— When a body possessing potential energy does work its range necessarily diminishes, while the body on which work is done, since it yields over a certain distance, gains potential energy. On the other hand, when a moving body does work its motion diminishes, while the motion of the body on which the work is done increases.—A statement which would in general be more complete than either, would be obtained by combining the two. For if one body exert on another a certain force through a certain distance the same work is done on it, whether the former body lose kinetic or potential energy in doing the work; while the effect produced in the latter body will in general be a change both in its motion and its state of strain, z.e. both in its kinetic and its potential energy. Thus, whether the former lose kinetic or potential energy, or both, the latter will, in general, gain both, or transference of energy will, in general, involve partial but not complete transformation. Prof. Lodge cites the air-gun as an instance of the trans- formation of potential into kinetic energy during transference. If we extract the bullet and plug up the muzzle it will serve equally well as an instance of the transference of potential energy without transformation. For if we now pull the trigger, the compressed air will do work on the air in the barrel. The “range” of the former will diminish, that of the latter will increase. As an instance of the transformation of kinetic into potential energy during transference, he selects the case of a bullet fired against a spring and caught by it. But if the spring have inertia, the energy acquired by it through the work done by the bullet must be partly kinetie, and in such a case, therefore, the transformation is only partial. Such instances, however, must be defective as illus- * Phil. Mag. [5] vol. xix. (1885) p. 486. + That is ‘ the distance through which it can exert force.” and the Conservation. of Energy. 141 trations, because the air, the spring, the bullet, which are treated as simple bodies, must be regarded as complex systems between the parts of which transferences of energy are oc- curring. When we make a more intimate study of such instances from the point of view of contact-action, we must, as Prof. Lodge points out, regard bodies as consisting of particles connected by a medium possessing some property of the nature of elasticity. If we assume the particles to be rigid they can, of course, have kinetic energy only. If the medium be assumed to have no inertia, its elements can have potential energy only. Hence if both assumptions be made, transference of energy between the particles and the medium must involve complete transformation, while transference | from element to element of the medium must occur without transformation. If, however, both the particles and the medium be assumed to have both inertia and elasticity, the transference of energy will, in general, it seems to me, involve only partial transformation, whether it occur between the elements of the medium or between the particles and the medium. When, therefore, Prof. Lodge states that “a bullet fired upwards gradually transfers its undissipated energy to the gravitation medium, transforming it at the same time into potential,” he seems to me to assume that the bullet is rigid and that the medium is without inertia. Prof. Lodge states finally that “ energy cannot be trans- formed without being transferred,’ but he gives no demon- stration of this proposition. I find it difficult to reconcile with this statement one of his illustrations:—“ A perfectly elastic bounding hall has all its energy transformed into potential at the middle of every period of contact with the obstacle from which it rebounds.’ Immediately after con- tact has ceased all its energy is kinetic, for apparently vibra- tions are excluded by hypothesis. The energy has thus been completely transformed without transference from the ball. It may, of course, be held that the ball must be regarded as a system of particles connected by an elastic medium. But in that case, what has been said of the ball, as a whole, is true of the particles in contact with the obstacle, if they are as- sumed to be elastic, or, if not, of the elements of the medium in contact with them, provided the medium be assumed to have inertia. After the middle of the period of contact, they do work on the elements of the medium beyond them. No work is done on them. They, therefore, lose energy and gain none. Yet after contact is over they possess kinetic energy. Whence has it come, if not through transformation of their own potential energy ? That energy cannot be trans- 142 Mr. A. A. C. Swinton on formed without being transferred must, of course, be true if bodies consist of particles with inertia but without elasticity, and if the medium connecting them possess elasticity but notinertia. Indeed, on these assumptions we may go farther and say it cannot be transformed without being transferred either trom particles to medium, or from medium to particles. If, however, either or both be assumed to have both pro- perties, the proposition seems to me to be erroneous, and certainly requires proof. In concluding the discussion of this subject Prof. Lodge says:— All I have stated is that change of form is necessary and universal whenever energy is transferred.” If this is all the statements under discussion are to be taken to mean they may be admitted at once, on the assumption of contact-action. But this version of the statements quoted above seems to me to be a new statement altogether. or, expressed in terms of energy, it says merely that when one body does work on another through the exertion of contact-force the potential con) energies of both bodies in general undergo change. Dalhousie College, Halifax, N.S., Dec. 30th, 1892. XVII. Haperiments with High Frequency Electric Discharges. By A. A. CAMPBELL SWINTON *. ‘HE writer has succeeded in passing through his body from hand to hand sufficient electricity to bring the filament of an ordinary 5-candle power 100-volt incandescent lamp very nearly to full incandescence, or to bring the fila- ment of a 32-candle power 100-volt lamp to full redness. Practically no sensation was experienced. The apparatus employed consisted of a large “ Apps” induction-coil capable of giving 10-inch sparks, supplied with current through the ordinary vibrating contact-breaker, and a resistance consisting of eight 50-candle-power lamps in parallel, from a 105-volt continuous-current supply. The total energy in the primary, excluding what was lost in the resistance and contact-breaker, was about 3850 watts, or not far off half an electric horse-power. To the positive and negative terminals of the secondary of the induction-coil were connected respectively the inside and outside coatings of three half- gallon Leyden jars, connected in parallel. The disruptive discharge of these jars across an air-gap of about a quarter of an inch excited the primary of a simple form of high-fre- quency coil similar to those employed by Mr. Tesla and * Communicated by the Author. — High Frequency Electric Discharges. 143 Prof. Elihu Thompson. The secondary of this coil consisted of 500. turns of No. 26 S8.W.G. cotton-covered wire wound on a paper tube. Outside this paper tube was a glass tube, upon which the primary, consisting of 10 turns of three No. 16 guttapercha-covered wires, in parallel, was wound. The whole coil was immersed in resin oil contained in a wooden trough. ‘The ends of the secondary were connected through small glass tubes, also filled with oil, to brass balls. On approaching the hand to one of the balls forming the terminals of the oil-coil, sparks shot out from the brush dis- charge which surrounds it. Ifthe spark is taken on the skin a sharp prick is felt, but on approaching the terminal or touching it with a piece of metal grasped in the hand, or after grasping the terminal itself, practically no appreciable sensa- tion is felt. If the terminal is grasped in this manner with the right hand, sparks will shoot out from the left hand or indeed from any portion of the body, if brought into proxi- mity with another person, a piece of metal, the gas- or water- pipes, or any conducting body. In the experiment referred to the incandescent lamp was hung by one terminal on a wire connected to earth, and connexion was made between the other lamp terminal and the coil through the two arms and body by the right hand being brought into contact with one terminal of the oil-coil, and a piece of metal grasped in the left hand being approached to the free terminal of the lamp. At the first approach the bulb of the lamp became filled with phosphorescent light, but, on reducing the distance between the metal in the left hand and the free lamp ter- minal, sparks shot out between them and the filament at once became incandescent—the incandescence increasing very nearly to the full normal amount when the piece of metal and the lamp terminal were finally brought into contact. To produce a similar incandescence of the filament with continuous or alternating currents of ordmary frequency would require about one fifth of an ampere, and at first sight it would seem that this quantity of current must pass through the arms and body of the operator. It has been generally assumed that with high-frequency currents the current is rendered harmless by reason of the high frequency—in fact, that high frequency renders harmless to the human body currents of a strength that would be dangerous and painful, if not fatal, were the frequency lower. The writer is inclined to think that another explanation is possible, and that the true fact is, not that high frequency renders harmless a given strength of current that with ordinary frequency would be harmful, but that with high frequency it is possible to obtain effects with exceedingly small currents, 144. Keperiments with High Frequency Electric Discharges. that with continuous and ordinary alternating currents can only be obtained by the use of much larger currents. This hypothesis 1s probably applicable to many other high- frequency effects, but as applied to the above-mentioned experiment it is simply this:—The lamp-filament having a certain definite resistance, with continuous or ordinary alter- nating currents which pass uniformly or nearly so through the section of the filament, a certain amperage of current is necessary to produce the number of watts required to raise the filament to incandescence. With the high-frequency currents, on the other hand, as is well understood, the current travels chiefly on the outer surface of the filament, little or none passing through the central portion. The current is in fact merely skin-deep. The virtual resistance is therefore very high, as only an extremely small portion of the sectional area of the filament acts as a conductor. There is an ample sufficiency of volts, and though the current is very minute there is a sufficient expenditure of watts to raise the filament to incandescence. ‘The lamp, in fact, ceases to be a 100-volt lamp and becomes, it may well be, a 100,000-volt lamp. As confirming this hypothesis, it should be mentioned that while the filament was incandescent sparks passed between the lamp terminals, which were at some distance apart, this being evi- dence that there was a difference of potential amounting at least to thousands of volts between the two ends of the filament. Returning to the experiments, several other curious results were obtained. If, instead of connecting the lamp to the coil through the human frame, a wire was used, the filament became much brighter than in the previous experiment; in fact, it gave considerably more than its normal candle-power. From this it was evident that the human body offered con- siderable opposition of some description to the passage of the electricity. In order to form some idea of the amount of this opposition, the body was again inserted in the circuit between the coil and the lamp, as previously, and the thumbs of the two hands brought near together. Sparks about one quarter of an inch in Jengih were found to pass between them, evidencing that the two hands of the operator hada difference of potential between them apparently equal to some thousands of volts. When the sparks passed between the hands, or when the wrists were brought into contact, so as to short-circuit, as it were, to some extent the resistance of the arms and bedy, the filament became very appreciably brighter. It should be mentioned that when the sparks were allowed to pass be- tween the hands very perceptible shocks were felt in the wrists. Notices respecting New Books. 145 Another experiment was to connect one lamp terminal ‘by a wire to the coil, connect the other lamp terminal to earth, and short-circuit the lamp through the body by grasping the coil terminal with one hand and a piece of metal connected to earth with the other. The effect of so doing was to reduce the incandescence of the filament to rather less than one half its normal amount, half of the available current going appa- rently through the lamp, the other half through the body. With the lamp terminal connected to the coil, it was found unnecessary to connect the other lamp terminal to earth to produce incandescence, all that was necessary being to touch this lamp terminal with a piece of metal held in the hand. That the incandescence of the filament produced under these conditions was due to the electrostatic capacity of the operator and not to his forming a connexion to earth, was evidenced by the fact that it made no perceptible difference whether he stood on the floor or on an insulated stool. In all the above experiments the second terminal of the oil- coil was free and not counected to anything. It was, how- ever, found that the effect of a second operator touching this terminal, or of connecting it by wire to earth, was to diminish the incandescence of the lamp-filament. It was also found that the filament incandesced toa greater degree of brightness when connected as above between one terminal of the coil and earth, than when it was directly connected between the two terminals of the coil, but that, while the operator experienced practically no sensation when his body was inserted between one terminal and earth, the sensation was very severe—in fact, quite unbearable—when the body was inserted between the two terminals. The above seem to show that capacity has much to do with the results obtained, and that the phy- siological effects of electric currents are not necessarily _ proportional to their heating-power. It should also be mentioned that in some of the experiments there was a decided tendency for the filament to vibrate in unison with the contact-breaker of the induction-coil. In fact, in some cases the amplitude of vibration was sufficient to cause the end of the filament to beat against the glass of the lamp bulb. XVIII. Notices respecting New Books. Annals of British Geology, 1891. By J. F. Buaxs, M.4., F.GS, 8vo. Pages viii & 404. Dulau and Co., London, 1892. ie a review of the former volume (for 1890) in the Philosophical Magazine for March 1892, the plan of these “Annals ” was fully described. It has been followed in the present volume, except Phil. Mag. 8. 5. Vol. 35. No. 213. Feb, 1893. L 146 Geological Society :— that :—no notice is taken of papers merely read before Societies, but not published in the year concerned,—the abstracts and Prof. Blake’s notes thereon have been submitted to the authors, and those which have been received back are marked with anasterisk — and a new feature is “ the introduction of illustrations of all new British species, and of other important novelties.” On this last point we may observe that “the will may be taken for the deed”; but that, though inadequate in very many instances to define the characters of the intended fossils, the amateur out- lines may serve as useful indications, to some extent, where the descriptive memoirs cannot be got at. The two maps (pls. i. and ii.), though roughly executed, seem to be more available for their intended purpose. As the asterisk placed before the No. of an Article indicates that the abstract has been seen and corrected by the Author or Editor of its memoir, we may notice that fifteen articles are indi- cated in the Table of Corrections as being entitled to these asterisks, as well as the very many (the majority) of the abstracts standing in the text with those marks. Important corrections appear (from the List of Corrigenda) to have been fortunately made by the authors in some of these abstracts after the printing. The “ Personal Notes” of the former yolume are now limited to eritical footnotes. These are always suggestive, and not unfre- quently decidedly useful. Some of the articles are, relatively, of considerable length ; for instance no. 6 (Murray and Renard) has 17 pages; no. 324 (A. 5. Woodward) 7 pages; no. 334 (R. B. Newton) 9 pages. The *‘ Personal Items” about the Staff and Officers of the Societies and Institutions are discontinued. The two Indexes (of Authors and Periodicals) are given, and one of new names. If the geographical and the geological points were indexed, we think advantages would accrue; and we venture to suggest that the cost of the plates might be saved to that end in the next volume. The masterly Gf not also masterful) manner in which the numerous memoirs are treated is well sustained, and tends always to indicate their interest, and often to advance their usefulness. Evidently no pains have been spared by the enthusiastic author in earnestly carrying out his plan of diffusing a correct knowledge of current British Geology, and of the work of British Geologists, among all who are interested in the Science. XIX. Proceedings of Learned Societies. GEOLOGICAL SOCIETY. [ Continued from p. 76.] November 23rd, 1892.—W. H. Hudleston, Esq., M.A., F.R.S., President, in the Chair. (ye following communications were read :— . “Outline of the Geclogical Features of Arabia Petreea and Palestine.” By Prof. Edward Hull, LL.D., F.R.S., F.G.S. The region may be considered as physically divisible into five The Base of the Keuper Formation in Devon. 147 sections, viz. :—(i) The mountainous part of the Sinaitic Peninsula ; (ai) the table-land of Badiet-el-Tih and Central Palestine; (iii) the Jordan-Arabah valley ; (iv) the table-land of Edom, Moab, and the voleanic district of Jaulaén and Haurdan; and (v) the maritime plain bordering the Mediterranean. The most ancient rocks (of Archzean age) are found in the southern portion of the region; they consist of gneissose and schistose masses penetrated by numerous intrusive igneous rocks. They are succeeded by the Lower Carboniferous beds of the Sinaitic peninsula and Moabite table-land, consisting of bluish limestone with fossils, which have their counterparts chiefly in the Carboniferous Limestone of Belgium, and of a purple and reddish sandstone (called by the author ‘the Desert Sandstone,’ to distinguish it from the Nubian Sandstone of Cretaceous age), lying below the limestone. The Nubian Sandstone, separated from the Carboniferous by an enormous hiatus in the succession of the formations, is probably of Neocomian or Cenomanian age, and is succeeded by white and grey marls, and limestones with flint, with fossils of Turonian and Senonian ages. The Middle Eocene (Nummulitic Limestone) beds appear to follow on those of Cretaceous age without a discordance; but there is a real hiatus notwithstanding the apparent conformity, as shown by the complete change of fauna. In Philistia a calcareous sandstone in which no fossils have been observed is referred to the Upper Eocene; for the Miocene period was a continental one, when faulting and flexuring was taking place, and the main physical features were developed—e. g., the formation of the Jordan-Arabah depression is referable to this period. . In Pliocene times a general depression of land took place to about 200-300 feet below the present sea-level, and littoral deposits were formed on the coasts and in the valleys. To this period belong the higher terraces of the Jordan-Arabah valley. The Pliocene deposits consist of shelly gravels. Later terraces were formed at the epoch of the glaciation of the Lebanon Mountains, when the rainfall was excessive in Palestine and Arabia. | The volcanoes of the Jaulan, Hauran, and Arabian Desert are considered to have been in active operation during the Miocene, Pliocene, and Pluvial periods; but the date of their final extinction has not been satisfactorily determined. 2. “The Base of the Keuper Formation in Devon.” By the Rev. A. Irving, B.A., D.Sc., F.G.S. In a paper published in the February number of the volume of the Quarterly Journal for the current year, the author definitely accepted the breccia which is clearly marked on the left bank of the Sid at Sidmouth as the base of the Keuper, but he had not then satisfactory data for determining a similar basement-line in the country between the valleys of the Sid and Otter, where the Keuper is repeated by the great Chit-rock Fault. Since then he has received information from the Rev. Dr. Dixon of Aylesbeare, mentioning the occurrence of breccia at several points on the east side of the Otter, and has subsequently visited the district, and with 148 Geological Society :— Dr. Dixon traced the breccia (the true base of the Keuper) along the left bank of the Otter, which for many miles seems to mark the western limit of the Keuper in Devonshire. — - As results, (i) the paleontological difficulty which the occurrence of Hyperodapedon east of Ottermouth presented is now removed ; (ii) the statement made in the last paragraph on p. 71 of the author’s paper in the February number of the Quarterly Journal needs some modification ; (iii) the geological maps of the Devon area require considerable revision; (iv) data are furnished which enable us to estimate the thickness of the Upper Bunter at not more than about 100 feet; and (v) points of interest in the physio- graphy of the country are indicated. 3. “The Marls and Clays of the Maltese Islands.” By John H. Cooke, Esq., F.G.S. _ The following deposits (in ascending order) occur in the Maltese Islands :—I. Limestone, II. Globigerina-limestone, III. Clays, IV. Greensands, V. Upper Coralline Limestone. The Marls and Clays forming the subject of this communication are No. III. of this list. They lie conformably upon the Globigerina-limestone, and so obscure is the line of demarcation between the two, and so striking the similarity of their fossils, that the Clay may be considered as an argillaceous division of the formation upon which it rests. The upper part of the Globigerina-limestone is referred to the Horner- schichten of the Vienna basin, and the Clay to the Schlier. The separation between the clay and the greensands is sometimes, though not always, complete, and occasionally the greensands are absent, and the coralline limestone rests directly on the clay. The thick- ness assigned to the clay by Dr. Murray (20 feet) is probably not far wide of the mark. A description of the lithological characters of the deposits of the clay division, based on microscopic evidence, is given. They consist largely of tests of foraminifera and minute fragments of minerals, and contain nodules of ochreous clay. A list of fossils of the clays is appended, including an addition of 31 species of foraminifera to the 122 contained in Dr. Murray’s list. December 7th.—W. H. Hudleston, Esq., M.A., F.BS., President, in the Chair. The following communications were read :— - 1. “Note on the Nufenen-stock (Lepontine Alps).” By Prof. T. G. Bonney, D.Sc., LL.D., F.B.S., V.P.GS. In 1889 the author was obliged to leave some work incomplete in this rather out-of-the-way portion of the Lepontine Alps. In the summer of 1891 he returned thither in company with Mr. J. Eccles, F.G.S., and the present note is supplementary to the former paper. The Nufenen-stock was traversed from north to south, and a return section made roughly along the eastern bank of the Gries Glacier. Gneiss abounds on the north side of the Nufenen Pass, followed by rauchwacke and some Jurassic rock. On the flank of the mountain are small outcrops of rauchwacke and of the so-called ‘ Disthene- Schistose ‘Greenstones’ from the Pennine Alps. 149 schists’ (both badly exposed), followed by much Dark-mica schist, often centaining black garnets. Higher up is a considerable mass of Jurassic rock with the ‘knots’ and ‘ prisms’ which have been mis- taken for garnets and staurolites, but Dark-mica schists set in again before the summit is reached. They continue down the southern flank of the peak ; but rather north of the lowest part of the water- shed, between Switzerland and Italy, the ‘ Disthene-schist’ is again found, followed by a fair-sized mass of rauchwacke. The return section gave a similar association in reverse order ; and both confirmed the conclusions expressed by the author in 1890 as tothe absence of garnets and staurolites from Jurassic rocks (with belemnites &c.), and the great break between these or the under- lying rauchwacke (where it occurs) and the crystalline schists, in which garnets often abound, of the Lepontine Alps. The crystal- line schists and the Mesozoic rocks are thrown into a series of very sharp folds, which, locally, presents at first sight the appearance of interstratification. 2. “On some Schistose ‘ Greenstones’ and allied Hornblendic Schists from the Pennine Alps, as illustrative of the Effects of Pressure-Metamorphism.” By Prof. T. G. Bonney, D.Sc., LL.D., ehess, V ob.G.8. The author describes the results of study in the field and with the microscope of (a) some thin dykes in the cale-schist group, much modified by pressure ; (0) some larger masses of green schist which appear to be closely associated with the dykes; (c) some other pressure-modified greenstone dykes of greater thickness than the first. ‘he specimens were obtained, for the most part, either near Saas Fee or in the Binnenthal. These results, in his opinion, justified the following conclu- slons :— (1) That basic intrusive rocks, presumably once dolerites or basalts, can be converted into foliated, possibly even slightly banded, schists, in which no recognizable trace of the original structure remains. (2) That in an early (possibly the first) stage of the process the primary constituents of the rock-mass are crushed or sheared, and thus their fragments frequently assume a somewhat ‘streaky’ order; that is to say, the rock passes more or less into the ‘ mylonitic’ condition. (3) That next (probably owing to the action of water under great pressure) certain of the constituents are decomposed or dissolved. (4) That, in consequence of this, when the pressure is sufliciently diminished, a new group of minerals is formed (though in some cases original fragments may serve as nuclei), (5) That of the more important constituents hornblende is the first to form, closely followed, if not accompanied, by epidote; next comes biotite (the growth of which often suggests that by this time the pressure is ceasing tio be definite in direction), and lastly a water- clear mineral, probably a felspar, perhaps sometimes quartz. 150 Geological Society. (6) That in all these cases the hornblende occurs either in very elongated prisms or in actual needles. The author brings forward a number of other instances to show that this form of hornblende may be regarded as indicative of dynamometamorphism; so that rocks where that mineral is more granular in shape (cases where actinolite or tremolite appears as a mere fringe being excepted) have not been subjected to this process. 3. “On a Secondary Development of Biotite and of Hornblende in Crystalline Schists from the Binnenthal.” By Prof. T. G. Bonney, iSc., TiiD., FRS., Vales: Both the rocks described in this communication come from the Binnenthal, and were obtained by Mr. J. Kecles, F.G.8., in the summer of 1891. They belong to the Dark-mica schists described by the author in former papers, and have been greatly affected by pressure. In each a mineral above the usual size has been subse- quently developed. In the rock from near Binn this mineral is a biotite ; the dimensions of one crystal, irregular in outline and having its basal cleavage roughly perpendicular to the lines indica- tive of pressure, are about ‘175 x ‘03 inch. The other mineral, from the peak of the Hohsandhorn, is a rather irregularly formed horn- blende, the crystals (which lie in various directions) beng sometimes more than half an inch long. The exterior often is closely asso- ciated with little flakes of biotite. The author discusses the bearing of this fact, and the circumstances which may have favoured the formation of minerals, so far as his experience goes, of an exceptional size. Some remarks also are made on the relation of these structures developed in the Alpine schists to the various movements by which those rocks have been affected, and on the general question of pressure as an agent of metamorphism. 4, “ Geological Notes on the Bridgewater District in Eastern Ontario.” By J. H. Collins, Esq., F.G.S. The plateau of the Bridgewater district consists chiefly of gneiss and mica-schist, with subordinate beds of white marble, quartz- conglomerate and quartzite, and some veins of ‘ giant-granite.’ The general dip of the gneissose series is eastward. The author notes the effect of frost in splitting off flakes of the eneissose rocks and conglomerates, especially on the bare glaciated surfaces, and suggests that many of the smaller and shallower lakelets may have originated by this process. The conglomerates are described as gneisses and mica-schists, with subordinate pebble-beds. . The occurrence of gold in quartz-veins near Flinders and at Madoc is noted; and amongst other economic products are the micas of the eranites, asbestiform actinolite, and marble. The author discusses the mode of origin of the granite, marble, and actinolite-rock. ol | ~~ XX. Intelligence and Miscellaneous Articles. VISIBLE REPRESENTATION OF THE EQUIPOTENTIAL LINES IN PLATES TRAVERSED BY CURRENTS ; EXPLANATION OF HALL’S PHENOMENON. BY E. LOMMEL. (Preliminary Notice.) Moen consideration shows that the equipotential lines at right angles to the lines of flow in a plate are at the same time the magnetic lines of force belonging to the flow. If iron filings are strewed on the plate with a sufficiently strong current, they arrange themselves to form a beautiful image of the equipotential lines. If the plate is brought mto a magnetic field. these magnetic lines of force alter their position, and therefore also the lines of force which necessarily are at right angles to them. In this lies the simple explanation of Hall’s phenomenon.—Wiedemann’s Annalen, No. 12, 1892. ew ON THE ACTION OF LIGHT UPON ELECTRICAL DISCHARGES IN VARIOUS GASES. BY F. BREISSIG. As source of light the author used a gas-flame. As he had the intention of determining the influence of the visible rays in electrical discharges, he tried to find a gas in which this action is as great as possible, but he came to the conclusion that the difference between various gases in this respect is too small to lead to the preference of any one in particular. M. Breissig uses Hallwachs’ form of the luminous discharge with a somewhat different arrangement. Opposite the source of heht is placed an amalgamated zinc plate, and in front of it a wire gauze, also amalgamated, of galvanized iron, both being insulated. The zine plate was kept at constant potential by a Daniell’s battery of 80 elements, while the wire gauze was connected with one quadrant pair of an electrometer. ‘The potential was measured of the quantity of electricity passing from the zine plate to the wire gauze owing to illumination. A decrease of sensitiveness of the plate with the duration of the illumination was observed, as Hallwachs and Righi had also observed for other sources of light; moreover, an increase was observed in all the gases investigated as the pressure diminished. In opposition to the observations of others, the author found a feebler discharge in carbonic acid than in air; the deflexions are reduced to about one half: this phenomenon is due to the fact that in his experiments the rays of a spectral region are used differing from that of other observers, and the action of the various parts of the spectrum on many gases may be different. With cool gas a feebler action is observed if the gas has already been illuminated. ' The discharges in some vapours were stronger than in all the gases examined, especially in air half saturated with alcohol vapour. The following table gives in round numbers the results observed by the author. V2 Intelligence and Miscellaneous Articles. Discharge. ae es Normal Diminished pressure. pressure. Atmosphericair . . . . 10 18-22 — ORV CEM wn yebigelae® is. he 14 20 VOC CM gee seo sok eof 8 16 Carbonic acid Covey ie 6 14 Coal-gas . . ee a 12 Sulphuretted Hydrogen 3 3 Air containing vapour of ee Aleoholi:;').0 °°... «20° 80-40 | aon GCN cece, Mees Of hs) ea ok 20-30 sae a Marpembinte ss yo te et 6 BenzGles. nye eine 2 2'4 10-20 Petroleum spirit . ... 10 XV NON ae ee ca ee aN 6 In this the mean strength of the discharge in dry atmospheric air is taken at 10—Inaugural Dissertation, Bonn, 1881; Beeblatter der Physik, vol. xvii. p. 60. NOTICE OF A METEORIC STONE SEEN TO FALL AT BATH, SOUTH DAKOTA. BY A. EK. FOOTE. On the 29th day of August, 1892, about 4 o’clock in the afternoon, while Mr. Lawrence Freeman and his son were stacking upon his farm two miles south of Bath, they were alarmed by a series of heavy explosions. On looking up they saw a meteoric stone flying through the air followed by a cloud of smoke. Its course was easily traced to the point where it fell within about twenty rods from where they were standing. The stone penetrated the hardened prairie to a depth of about sixteen inches, and when reached it was found to be so warm that gloves had to be used in handling it. Three small pieces of an ounce or two each had apparently been blown off by the explosions, but the stone still weighed 462 lb. One of these small pieces was found by some men not fax distant, and was broken up and distributed among them. The explosions were plainly heard by a large number of people at Bath, two miles away, and at Aberdeen, nine miles away, it sounded like distant cannonading. The exterior of the stone presents the usual smooth black crust. The interior is quite close- grained, resembling in texture the stones from Mécs. The iron is abundantly disseminated through the mass ; and although the grains are small, they are easily distinguished and separated on pulverizing. Preliminary tests made by Mr. Amos P. Brown, of the Minera- logical Department of the University of Pennsylvania, prove the presence of nickel and cobalt in considerable quantity. Silliman’ 8 Journal, January 1893. a THE LONDON, EDINBURGH, axn DUBLIN PHILOSOPHICAL MAGAZINE AND JOURNAL OF SCIENCE. a [FIFTH SERIES.] MAR CH 1893. XX1. On the Equilibrium of Vis Viva.—Part III. By Prof. Lupwig BottzMann*. IT think that a problem of such primary importance in molecular science ought to be scrutinized and examined on every side, so that as many persons as possible may be enabled to follow the demonstration. Maxwell, Scientific Papers, il. p. 713. § 1. On the Variables which reduce the expression for the Vis Viva to a Sum of Squares. AXWELL? was the first to establish the formula for the distribution of vis viva among monatomic gas molecules, which he regarded as perfectly hard spheres of similar or dissimilar form (mass and radius). He also worked out the case in which the molecules are considered as rigid bodies with three different moments of inertia, and he found that for such a gas the ratio of specific heats must be 12. Since, however, this ratio has the value 1:4 for the best known simple gases, he concluded that the mechanical analogy is at variance with known facts on this subjectt. It is remarkable that Maxwell, who was successful in presenting the solution of the problem with such almost inconceivable * Communicated by the Author, from the Sitzwngsberichte der mathe- matisch-phystkalischen Classe der konighch-bayerischen Akademie der Wissenschaften (Munich), vol. xxii. part 3. Translated by James L. Howard, D.Sc. + “Illustrations of the Dynamical Theory of Gases,’ Phil. Mag. January and June 1860, Sci. Pap. i. p. 877. t Maxwell, Sci. Pap. 1. p. 409. Phil. Mag. 8. 5. Vol. 35. No. 214. March 1898. M 154 Prof. Ludwig Boltzmann on the ease, both in the case of spheres and of bodies which possess no axis of rotation, did not then think of considering the allied and almost similar case, namely that of the various perfectly smooth and rigid solids of revolution which differ from the spherical form. He would then have obtained exactly the desired value 1°4 for the ratio of specific heats. The proof which Maxwell gave at that time for his law of distribution of kinetic energy was afterwards shown by him- self to be insufficient ; and in a second paper* he gave an exact proof that the distribution of vis viva found previously was a possible one, 7. e. that when once set up among the molecules of the gas it would not be altered by their impact. This proof as well as Maxwell’s law itself is capable of considerable extension, and he pointed out its very close con- nexion with a far more general theorem which applies to any system in which any forces operatet. In the attempt to make this latter theorem still more general, however, Max- well{ committed an error in assuming that by choosing suitable coordinates the expression tor the ws viva could always be made to contain only the squares of the momenta, this assumption being, as Lord Kelvin has shown §, in general incorrect. But the mistake may be easily corrected by a slight modification of Maxwell’s conclusions. To demon- strate this let us turn to Maxwell’s paper just quoted above, and write with him (Sci. Pap. ii. p. 720) 6, b, b3...6, for generalized coordinates, and a, a)... d, as the corresponding momenta. We must then stop at Maxwell’s equation (42) (1. c. p. 724), and so write for the vis viva T=43[11]a,?+ [12 Ja, Ug.+e- All Maxwell’s conclusions as far as equation (29) inclusive are perfectly accurate. In order to correct the further con- clusions we might write the following deduction in place of that of Maxwell, from that point onward. Let us suppose « to be a linear function of the momentum a, and thus write k=n an= D CaM. p= Then we can always choose the coefficients ¢ so that (1) their * Phil. Mag. [4] vol. xxxv. (1868); Sci. Pap. ii. p. 26. + Boltzmann, Wienzr Sttzwngsberichte, vols. lviil., ixiii., Lxvi., Ixxii , Dexty., Lxxy, t “On Boltzmann’s Theorem on the Average Distribution of Energy,” Camb. Phil. Trans. xii. part 3 (1878); Sci. Pap. ii. p. 713. § ‘Nature,’ 15th August, 1891. Tquilebrium of Vis Viva. 155 determinant © is equal to unity, that is Cy C19 2 8 e@ and (2) the doubled kinetic energy takes the form TS eee i In this investigation the coefficients c and w are functions of the generalized coordinates b,...b, but the «’s cannot in general be regarded as momenta which belong to any system of generalized coordinates whatever. I will therefore call them “ momentoids” in order to prevent confusion. The angular velocities about the three principal axes of inertia of a solid in the most general case of rotation furnish an example. _ I shall denote by 4, that portion of the whole vis viva which belongs to the momentoid a, Since @=1, we have day, ddg...ddn=d,, dé,...de,. Jet us insert the variable T in place of a, on the jeft and of «, on the right, then il i 7 dT dag da3...da, = at Ue WER 45 ete da, da, Dividing by dT and observing that 2g ellie, dor aa, aie lyed? we obtain EZ day daz «.. Aa, = as daty das... day. 1 jemi From Maxwell’s equation (28) (/.c. p. 721) we find for the number of systems whose generalized coordinates lie between the limits 6, and 0,+db,...6, and b,+db,, and whose momentoids lie between # and #+da ....a, and a,+da, («, being determined from the equation of tis viva) the value NC palel If we now proceed with the integration exactly as Maxwell does, we arrive at his equation (45), which is thus perfectly correct. By calculating the probability that the ws viva dpm,¢,? M 2 AION ee clan ats Galen 156 Prof. Ludwig Boltzmann on the belonging to the momentoid a, lies between the values /, and k,+dk,, we again arrive exactly at Maxwell’s expression (51) (ae p. 425 ). The expressions (52) and (53) (Ul. ¢. p. 726) of Maxwell’s paper thus represent the mean and maximum values of the vis viva belonging to any momentoid. Instead of the law of Maxwell that the mean vis viva has the same value for every coordinate, we now obtain the law that the mean value of the vis viva belonging to all momentoids is the same. Since the number of momentoids is always the same as that of the degrees of freedom, the law given by Maxwell at the commencement of his paper (/. ¢. p. 716) still remains true, viz. that the mean kinetic energies of two given parts of the system are in the ratio of their respective degrees of freedom. The kinetic energy T; of any portion whatever may therefore contain the products of different »;’s, the terms p;, being the momenta of the general coordinates of that portion. But T;, must not contain the product of a term p; and another mo- mentum which is not included among the terms p;,. Asa special case, the law will apply without any moditication to so-called polyatomic molecules of a gas, whose condition is expressible by generalized coordinates. T - i=n ; As 2 o is equal to > a; eh in all cases, my proof of the 1=1 second law* will still be correct, provided that by g, we un- derstand, not the momenta belonging to the coordinates pz, but the momentoids. ON THE SPECIAL CASES SUGGESTED By Lorp KELVIN AS TEST-CASES. § 2. Motion of a Material Point in a Plane. I believe that with these modifications Maxwell’s proof of the laws enunciated in the previous paragraphs is a satisfactory one; but in addition I have already given another proof from a quite different point of viewf. I believe therefore that its truth as a law of analytical mechanics can hardly be called into question{. As I myself arrived at my theorem only * Borchard-Kronecker’s Jowrnail, vol. c. p. 201 (1885). 7+ “On the Equilibrium of Heat between Polyatomic Gas-molecules. Part I. Motion of the Atoms in the Molecules,” Wien. Sitz.-Ber. vol. iii. 9th March, 1871. “Some General Theorems on Equilibrium of Heat,” ebid. 13th April, 1871. In the latter paper J first made use of generalized coordinates. { It is an entirely different question, whether such systems present a suffidently close analogy with hot bodies. This question cannot be discussed here; cf, however, Beibi. v. p. 408 (1881). Equilibrium of Vis Viva. 157 after a laborious consideration of many special cases*, I can appreciate the value of continually testing general theorems by means of special examples, and will therefore take up one of the particular cases suggested as a test-case by Lord Kelvin, namely the one he mentions last ; because it is the simplest, and because I respect the sentence of De Morgan, quoted once by Prof. Tait, to the effect that “formule, if too long, are often not read.” | Let a material point of unit mass move in the plane of a, y. Let 2, y be its coordinates, qg its velocity, u,v the components of the velocity in the directions of the axes of coordinates, and @ the angle which the direction of motion makes with the positive direction of the axis of abscissa, the angle being counted from 0 to 27. Suppose the potential V to be any function of the coordinates. We assume that the motion neither becomes infinite nor asymptotically approaches a fixed limit ; and that all possible sets of values of a, y, and @ which are consistent with the equation of vs vera are obtained with any required degree of approximation, provided the motion continues for a sufficiently long time T. Let us take a ¢-coordinate perpendicular to the plane of x, y, and define any condition of the moving point by marking off as z-coordinate over the point where it happens to be, the angle @ which its velocity makes with the positive direction of abscisse. We shall call the point of space with the coordi- nates x, y, 9 the point which characterizes the condition of the moving body, or briefly the instantaneous condition-point. We can then define our assumption thus :—In the course of an interval of time T the condition-point occupies all positions in a finite cylinder (the condition-cylinder) which has a height 27 in the direction of the axis of z. The condition-point passes suddenly from the base to the summit of this cylinder, and vice versa ; with this exception its motion is continuous. Suppose the moving point to be at the point w, y at any time ¢, and let its velocity make an angle @ with the axis of abscissee and have the components wv, v. The condition-point at time ¢ will then be a point A of space with coordinates w, y, 0. After the lapse of a very short time 6¢, that is at time ¢+ 6¢, let the moving point be at w’,y’. Let @’ be the angle between the direction of motion and the axis of abscissee, and uw’, v’ the * “On the Equilibrium of Vis Viva,” Wren. Sitz.-Ber. vol. lviii. 8th October 1868.— ‘Solution of a Mechanical Problem,” ¢ded. 17th December, 1868.—“ Some General Theoren:s on Equilibrium of Heat” (end of part 2) (d. c.).-- Remarks on some Problems in the Mechanical Theory of Heat,” Wien. Sitz.-Ber, vol. lxxv. 11th January, 1877 (end of part 3). 158 Prof. Ludwig Boltzmann on the components of the velocity resolved along the coordinate AXES. We may denote the position of the condition-point at time t+8¢ by A’. A’ will be called the point corresponding to A. If we consider o¢ as constant, every point within the condition- cylinder will possess its corresponding point. Always, when at any time the condition-point has occupied any point of space, it will, after a time d¢ has elapsed, pass to the corre- sponding point ; and vice versd, the moving body can never reach the corresponding point except by having passed through the point to which it corresponds at a time 6o¢ previously. 7 We have then w=c+q cos @. dt, Me w=uté.dt, v'=v+7. 6, (1) in which €=— o 7=— = are the components of the force acting on the moving particle, and are therefore functions of aandy. Further, ru 6’ =arctg — uw which gives, on substituting the above values, 6’ =6+(n.cos 0—¢ sin @) - + = ee) Now let us construct an infinitely small rectangular parallelopiped dxdyd@, of which one edge is situated at the point A. Let the fraction of the whole time T during which the condition-point lies within the parallelopiped be dt. This is the time during which the three variables 2, y, 9 will be included between the values w and «+dz, y and y+dy, and 9 and 6+d@. We may then write in all cases dt=/(«,y,@)dzdyd0. -. -. 1 =) Samia} Now construct at each point of the parallelopiped dz dy d@ the corresponding point, and hence obtain the parallelopiped dx’ dy’ d@'. That fraction of the time T during which the condition-point les within dw’ dy’ dé’ is, according to equa- tion (3), dt! = f(a’, y', 0) da! dy! dé’. Sinee, however, according to our definition of the conditicn- point, every time it enters the parallelopiped dz dy d@ it must after an interval d¢ enter dz’ dy’ d@', and since the interyal Hquilibrium of Vis Viva. 159 between the exits from the two parallelopipeds is also exactly dt, it follows that the condition-point must enter both paral- lelopipeds the same number of times and must remain for the same time in each. This gives dt/=dt, or Ke, y’, &) da’ dy! d =f (x, y, 0) dx dy dé. But we have / / / dizi dy! dd = oY, Oy, OY dex dy dd. OF OF OF Ov Oy 00 As 6¢ is constant, and g?= const. —2V, equations (1) and (2) give / / , a = 148050." 80 —14qsind. 7 { OF == (Ecos 0+ sin a= If we neglect the terms of order 627, the functional deter- minant reduces to On OV) OO. OL nay SBOrH 2 da! dy’! dW’ = dx dy dé, from which also f(a’, y’, 0’)=/(a, y, 0). As wecan pass from the parallelopiped de a d@ to its corresponding one, and from this latter to its corresponding one, and so on, it follows that (&, y, 9) is always constant, and therefore that dt=C da dy dé. This result agrees perfectly with that found in my paper pre- viously quoted, on the ‘‘ Solution of a Mechanical Problem.” Lord Kelvin denotes by N d@ dr the number of times during the interval T that the moving particle traverses an element of surface, whose length in the direction of motion is ds and whose breadth perpendicular to this direction is dy, in such a manner that 0 lies between tlie values @ and 6+d0@. As the moving point always remains for a time ds/g in the element of surtace, the fraction of T during which the moving point is situated in drds and has at the same time a direction of motion between 0 and 0+ d@, is and consequently SN dr ds dé. q 160 Prof. Ludwig Boltzmann on the But we have just seen that. this time is C dr ds dé, from which it follows that N=Cg. WN is therefore quite independent of the angle 6, and not only Lord Kelvin’s coefficient A, but-also A, and all the coefficients following vanish. | I can hardly doubt that Lord Kelvin will be satisfied with this result of his test-case. § 3. On the Distribution of Kinetic Energy among Kelvin’s Doublets. The other cases suggested by Lord Kelvin relate to a theorem which is closely connected with the problem just considered, but not by any means identical with it, nor even a special case of it; namely, the question of the equilibrium of heat in the case of polyatomic gaseous molecules. It can easily be shown that in this problem there exists one particular distribution of vs viva which is not altered either by internal motion of the molecules or by impacts. Let 91, P2;-++*Pn be the generalized coordinates by which the positions of all constituents of a molecule are determined relatively to its centre of mass, the rotation of the molecule being included. Let 41, G2,--.n be the corresponding mo- menta, T the total vis viva of the molecule, V the potential- function of its internal forces, w, v, w the components of the velocity of its centre of mass, and finally A and & constants ; then the distribution of vis viva referred to is that in which the number of molecules per unit volume, for values of the variables uw, U, W, P15 Pay++*Pn> G1» Yay +++ Yn between the limits wu, and uj+duy,..+Gn and gn+dgn, is equal to eee Oy its 220 G as If there are several kinds of molecules present the constant «, but not A, must have the same value for each. The verification of this result in the special case imagined by Lord Kelvin is so simple that I shall not consider it here. But the other proof, that the distribution of kinetic energy given by the above formula is the only possible one, can only be established indirectly by the assumption that a certain particular function must, if altered, be necessarily increased by collisions. As this function is very closely connected on the one hand with the quantity designated by Clausius as entropy*, and on the other hand with the probability of occurrence of * Wien, Sitz.-Ber. Bd. lxxvi. (1877), Bd. Ixxviii. (1878). Equilibrium of Vis Viva. 161 the state referred to, the second law of thermodynamics appears from it te be purely a law of probability. It appears to me to be a matter of interest (wide Motto) to examine this latter proof for the case of the molecule provided with elastic springs as imagined by Lord Kelvin, and which, following his example, we shall call a “doublet.” By a doublet let us understand the combination of two material points with masses m and m’’, which attract each other with a force proportional to their distance apart. m’ (the nucleus) is never acted upon by any other force. The masses m (shells) of any two doublets impinge on each other like elastic spheres whenever they come within a distance D” of each other. Besides these, suppose simple atoms of mass m’ to be present, which collide with each other if they approach nearer than distance D’, and with the shells if they come within dis- tance D from them. We shall always write, for the sake of brevity, ‘ shell” instead of centre of the shell, and “‘ nucleus” instead of centre of the nucleus. Let 2, y, < be the coordi- nates of the nucleus of a doublet referred to « system of rect- angular coordinates the origin of which is at the centre of the shell and the axes of which have fixed directions ; let a’, v’”, w’’ be the absolute components of the velocity of the nucleus, and ul, v, 1 the same components taken relatively to the shell ; let g, h, k be the components of the velocity of the centre of gravity of the doublet, u, v, w those of the shell, and a, v4, w, those of a single atom. Finally, suppose y(a, y, 2, ut, v, W, g, h, k) dv...dk to be the number of doublets per unit of volume for values of the variables #...k at the time ¢ lying between the limits « and w+dw#...k and k+dk, and let T (uray Ury W1) Cu, dv, dw, be the Srna kes of single soe | in unit of volume whose velocity-components uj, 71, w, lie between the limits , u, and uj+du,, rv, and v,4+dv,, w, and w,+dwy. Then the expression the value of which can only be dimi- nished by impacts, and which for brevity we call the entropy, is es \xlog x da hin dk+\ flog f du, dv; dw), in which the integration extends over all possible values of the variables. The first term of the expression EH can be obtained in the following manner. We write down the value of log yx for ev ery claw alee contained in the unit of volume; 2. e. we insert in log y for all the variables those values w Teck it takes for the doublet under consideration. Then we add together all the values of logy so obtained. In order to 162 Prof. Ludwig Boltzmann on the express this symbolically we may denote the sum by > log x. In a similar manner the second term gives us } log /, the summation being extended to all the single atoms in a unit of volume. In order to prove that E can only diminish, let us first find the change produced in the value of {logy simply by the relative motion of nucleus and shell in the doublets, assuming no collisions to take place. In this case gy, h, and & would obviously remain constant. On the other hand, we should have at any time ¢, x=Asin(at+B), w=Aacos (at+B), and at time ¢=(, #=AsinB, t%t)=Aacos B. If we consider all doublets for which A and B are ineluded within specified infinitely close limits, then da di=da,dyj=AadAdb » 2 ie and similarly for the y- and z-axes, dy dv=dy) dv), dzdw=dza dw 20. 2) It can easily be shown that the equation dx dy dz dit dv dw = day dy dz dit dv, AW also holds good if the nucleus and shell have any other central motion whatever. (Cf. my investigation of the equilibrium of heat in the case of polyatomic gaseous molecules, previously referred to.) If no collisions were to take place the doublets, whose variables at time t=0 lay between the limits xz) and Xo t+dx...ky and ky +dky, would have their variables at time ¢ between the limits # and e+dza...k and k+dk. Let us therefore consider for a moment the variable ¢ as explicitly expressed in the function x, in order not to exclude the pos- sibility of a variation of y with time. We have then as the number of the former doublets, X(2-- Wo, g, h, k, O)day..dk=yy day... dk and of the latter Veh tide. cdie=wde «Ake. Hence we have Xo Axo erie dk=y dx a6 dk, and from (4) and (5) Xo =X; from which it follows that Xo log Xo, day)..dk =x logy dx..dk. — Equilibrium of Vis Viva. 163 The integration of this last equation over all possible values of the variables involved in it shows us at once that the quantity = log y suffers no alteration by internal motion of the doublets, and the same will be true, of course, for any central motion. All that now remains is to determine the effect of the collisions. Let us now introduce instead of u, v, Ww, 9, h, k, the absolute velocities a, v,w, uw’, wv”, w’. Since Malt (m +m!) g=mu +m usu! =u, it follows that. dg du=du du". If we write for the number of doublets in unit. volume, whose variables x, y, z, wu", v", w", u, v, w, lie between the limits xand e+da...wandw+dw, the value F (a, y, z, ul v", w", u, v, w) dx ...dw, where , mut nu’ \ F= (eget ee) x Ys%) m +m" JP then > logx=|F log F da...dw= log F, in which the summation again extends to all the doublets contained in the unit of volume. Now denote by 6,3 loy F the increase in & log F produced during time 6é by the impact of doublets on each other, by 6,2 log f the increase in & log f during the same time, produced by the impact of single atoms on each other, and by 6,,(3 log F+% log f) the corresponding increase of the quantity in brackets, produced by the impact of doublets and single molecules. To calculate 6,.(2 log F +2 log /f) we must sort out, from all the impacts between a shell and a single atom in unit volume during time o¢, those collisions for which the velocity- components of the shell at the moment of the collision (and likewise before) lie between the limits w and u+du, v and v+dv, w and w+duw, the velocity-components of the nucleus being between w!' and w" +-du!', vo" and vu" + dv", w!’ and w" + dw", the coordinates of the nucleus relatively to the shell being between w and «+d, y and y+dy,z and z+dz; further, the velocity-components of the common centre of gravity of the shell and the single atom are to lie botween p and p+dp, q¢ and g+dq,7r and r+ dr, and the direction of the line of centres of the impinging atoms at the moment of impact are to lie within an infinitely narrow cone placed in a definite direction in space and having an infinitely small angle dX. The velocity- components of the single atom at the instant when the impact 164 Prof. Ludwig Boltzmann on the begins are then _m+m— m m+tm =m .— — — 1 = — Vv 1 m! P mi? 1 mi q 73 I m+m m Wy, — ay — —U. e (6) VID m For the number of impacts which take place in unit volume during time 6t, under the conditions specified above, we find without difficulty the value dn=D?. F(a, y, z, ul", v", w", u, v, w) f (a, M1, U1) x Vedax... dw" du dv dw du, dv, dw, dr 6. In this expression V is the relative velocity of the two atoms at the moment of collision, and e the cosine of the acute angle between the line of motion and the line of centres. If we introduce instead of w, v,, w, the variables p, q, 7, from equation (6) we find 1) 3 dn=D* Ff, es Veda...dw!" du dv dw dp dq dr dn &E, in which the suffix 1 denotes that the values of the variables as given in equations (6) are to be substituted in the function. In each of the impacts just specified a shell loses velocity- components uw, v, w, and hence in all the dn impacts = log F will be diminished by dn log F. After each of the impacts considered let the velocity- components of the shell be between w! and u! +dw', vandv'+dv', wand w'+dw!. In order that shells may be formed with these new velocities {log F must be increased by dn log FE’, where the affix denotes that the variables 2... w", ul, v', w! are to be substituted in the function F. We assume that the collisions are instantaneous, in which case the variables z... aw"! are unaltered by the impacts. The total increase of Y log F by reason of the impacts considered is, therefore, dn (log F’—log F). In like manner we find that Slog 7 receives an increase dn (log fy’— log f;) during time 6é from the same impacts, the affix and suffix meaning that the following values of the velocity-components of the impinging single atom after impact are to be substi- tuted in the function /. Equilibrium of Vis Viva. 165 aoe mi Denier ; m+m! m u,!= — — 7) o/= ——v - pene ele E a all ! m+m m ! oo L——w. . 7 i an! m! @) The total increase of Slog F+ 2 log/ by all impacts of the type specified is, therefore, dn (log F’ + log /"; —logF —log f\). From this we shall obtain the total increase previously designated by 6,,(2log F+ log /) if we integrate over all values of the variables whose differentials are contained in dn*. This integration may be performed by means of a special device. In conjunction with the above terms which are furnished by the “ specified ” impacts, let us take the terms furnished by the “ opposite’ impacts, and thus divide the whole of the collisions into pairs. We shall consider an impact to be “ opposite” to any ‘“ specified ’’ one when the condition of the colliding atoms at the end of either is exactly the same as their condition at the commencement of the other one. ‘The centres of the colliding atoms must, however, be interchanged of course, since they approach each other before impact. The remaining variables a...w' will be included between the same limits for both impacts. In the accompanying figures the largest circle repre- sents a shell, the smallest a nucleus, and the intermediate one a single atom; the arrows drawn through their centres represent * If we assume that the second of the impinging atoms is not a single atom, but a shell, we arrive by exactly analogous reasoning at a similar equation 28,3 log F= \dn (log F’+log F,’—log F —log F,), in which “cia By SF (@, Yyy My Ma'', Py ') Wi") Uy M, W). BY SE y, yy 2 Uy") P15 W's Uy’, |, &')- U,V, Wy, and w,', v,',w,’ are the velocity-components of the second shell before and after the impact, and must be expressed by equations of similar form to (6) and (7). %4, Y%, %, %'', v,’, w,"' are the remaining quantities by which the position of the second doublet at the moment of the impact is determined. Finally, dn=D'? FF, Vedz... dw" du dv dw dx,... dw,'' dp dq dr dy &t. By similar processes of reasoning we should find 23,3 log f= {dn (log. f’+log f;'—log f— log /) dn=D"ff, Ve du dv dw dp dq dr ad &t. and The meanings of the quantities in these equations will be clear without further explanation. 166 Prof. Ludwig Boltzmann on the the velocities. Figs. 1 and 2 show the configurations before and after an impact respectively, while figs. 8 and 4 give the Fig. 1. Fig. 2. — Tr: 4 O° g. o.- tL 12. Fig. 3 2 4 a ones : configurations before and after the corresponding “‘ opposite ” impact respectively. Arrows numbered alike have always equal lengths and make the same angle with the line of centres. For all collisions which are “ opposite” to those previously considered, the velocity-components of the impinging shell at the commencement of the impact lie between the limits wand ul +du', v' and vo +d, w! and w! + dw! and at the end of the impact they le between wu and u+du, vand v+dv, w and w4 dw. The same holds good for the impinging single atom in which the motion of the centre of gravity, the magnitude of the relative velocity and its inclination to the line of centres have the same values for the opposite impact as for that originally considered. In each opposite impact a shell loses velocity-components w’, v’, w', and a single atom loses uy', vy!, w'; on the other hand, a shell gains u, v, w, and a single atom uy, %, wy. If dn! is the number of collisions per unit volume in time 6¢ which are opposite to those previously considered, the term = log F +2 log/ is increased by them to the extent of dn! (log F + log f; —log F’—log 7). The total increase in the value of this expression due to the specified and opposite impacts together is (log F + log f,—log F’—log f\!)(dn—dn’). If we integrate this expression for all values of the variables whose differentials are contained in dw and du, we obtain Equilibrium of Vis Viva. 167 261o(>% log F + % log tT); because we count every Impact twice ; once as a“ specified,” and the second time as an “ opposite,” impact. As V,e¢, and dd are not changed by the impact, we have Pes Oa a are Veda... du! du! du! dw! dp dq dr dv 6t. It can easily “ shown (most simply by a geometrical proof ) that du’ dv' dw'=du dv dw, and hence §,(S log F+ Z log f) = z { (log F’ + log f/ — log F—log f) 1\3 x (Ff, — F'7') ee VeD?du dv dw dp dq dr dz...du" dr. (8) Similarly it can be shown that §,3 log F = 281) (log F! + log F\!—log F —log F,)(FF,—F'Fy') x Ve D'?dz...dw"dx,... dw," du dv dw dp dq dr dn, 8,3 log f= 284\(log /' + log f,'—log f—log ft) (SAS) NeW dududwmdpagd: AN. 2 5.) . (9) in which the variables are the same as in the footnote on page 165. We shall confine our attention to the consideration of the stationary condition, in which F and / are at all times the same functions of the variables contained in them. In this case no causes except those already considered can effect changes in 2 log F and 2 log /; and the total change in H during the time 6¢ is therefore dH=6, (Slog F+ > log /)+6,2 log F+8, 3 log /. Since everything (and therefore EL) remains unaltered, 6H must be zero. But in the integrals of equations (8) and (9) the two factors in brackets have necessarily opposite signs, while the remaining quantities are essentially positive. The expression to be integrated is therefore necessarily negative, and the sum of the integrals of which 6H is composed can only vanish if at each impact eye Ee ——ay i «ss . CLO) Let us now consider the most simple case, namely, that in which the shelis always pass each other without i impinging, and similarly with the single atoms ; but between a shell and a single atom let there be “alw ays an impact if they approach within distance D of each other. We have then only the first of the equations (10), but it holds good for every possible 168 Prof. Ludwig Boltzmann on the impact. If we put the velocity of a single atom Vu +o +07 equal to ¢,, then /, is clearly a function of ¢, but F may be expressed as a function of the following six variables: —(1) the two velocities c and c” of shell and nucleus, (2) their distance apart p (measured from centre to centre), (3) the angles « and a'’ which the directions of c and c" make with the line p, the latter being supposed drawn from shell to nucleus, and (4) the angle 8 between the plane containing p and c and that con- taining p and c”. | . Now imagine a collision to take place, and denote the values of these variables at the moment immediately before the impact by letters without an affix, their values just after the impact being distinguished by the affix. We can so choose the direction of the line of centres at the moment of impact and the direction of cq, that c, «, and @ take any re- quired values c’, a’,and 8’, provided these latter furnish a real value c,' of the variable ¢, after impact. This value will be determined by the equation of vis viva me? +me?=m'e2 +me. The values of the variables c’, p, and x” will not be altered by the impact. The first of the equations (10) can therefore be written in the form Fc", a, p,c,e, B) - fala) =F, al, p, eya!, Sa xf, / (x /ot4 (ce) ) This equation must be satisfied by all possible values of the variables ¢c', a", p, c, a, 8, c, a, B', and ¢,; from which it follows easily that Filer) =A. e—K'ey? KF = AewKme?, in which A, and / are simple constants, while A may contain the variables ¢", p, and @”. It is therefore evident that the mean kinetic energies of a shell and a single atom are equal, and that Maxwell’s law of distribution of velocities between shells and single atoms is satisfied, without assuming the existence of impacts of shells on each other, or of single atoms on each other. These assumptions do not alter the distribution of vis vzva in the slightest degree, however, because the values of /; and F found above satisfy identically the other relations demanded by the equations (10). On the other hand, the condition that the nuclei should never - come into collisions of any kind does not prevent the law from Equlbrium of Vis Viva. 169 applying even to them ; but the proof of this is much more difficult. For, if such collisions existed, it would follow that F would depend upon c” in exactly the same manner as it depends upon ¢, and there we should be forced to stop. In this case we must consider more closely the internal motion of the doublet. We can next prove without difficulty that in the distribu- tion of velocities just found the values of c, a, 8 are altered on the average in exactly the same manner and degree by each impact as by its opposite one, for every set of values of c', p', and #". If, then, certain forms of central motion are suddenly destroyed by a collision, the same forms are pro- duced again elsewhere equally often by other collisions, and consequently the same law of distribution of central motions would exist even if all impacts were suddeniy to cease. It is remarkable that just for the simple case imagined by Lord Kelvin, in which the central force is taken proportional to p, the calculation is exceedingly long. In order not entirely to forget the sentence of De Morgan, previously quoted, I will b e e assume some other law, e.g. ap + o°? or, indeed, any one in which the angle between two consecutive apsidal lines bears no rational proportion to 7. The total energy of a doublet is Pe et, oe. (LL) where @ is the potential-function. The doubled velocity of the relative motion of shell and nucleus in the plane of their central motion is K=p V¢ sin? a +c” sin? a” —2cc" sin a sin a" cos B, . (12) and the velocity of the centre of gravity of the doublet mul- tiplied by m+m"' is G= V m2? + m!?d? + 2mm''ce"(cosacos a! + sin asin! cos 8) (18) and its component perpendicularly to the plane of central motion is 3 ce" sin a sin #" sin B (14) — We sin? até? sin? a! — Qc" sin asin a cos B The number of doublets in unit of volume for which K, L, G, H lie between the limits Kand K+dK, L and L+dL, G and G+dG, H and H+dH, Phil. Mag. 8. 5. Vol. 35. No. 214. March 1893. N 170 Prof. Ludwig Boltzmann on the may be written ®(K, L, G, H) dK dL dG dH. The number of these doublets for which p lies between p and p+dp is dp Podp dp ®,. dK dL dGdH .—+ —=Vdk dL dG .dH—, Oo Pl dt 1 a peri-centre to an apo-centre; this latter is, therefore, a given functionof K,L,G, H; andV=@ / ‘ = is likewise a function in which o= Sy , and |" ze is the time which elapses from p / 1 of these four variables. Let us limit our attention to those doublets for which (1) the last apsidal line of the central orbit makes an angle lying between ¢ and e+ de with a straight line drawn in the plane of the orbit parallel to a fixed plane; (2) two planes, one normal to the central orbit and including the direction of motion of the centre of gravity, and the other parallel to a fixed straight line , make angles between w and @+dw with each other; and (3) the direction of motion of the centre of gravity lies within a cone of given direction of axis and of infinitely small angie dA. We have then to multiply by de dw dd/167°, and the number of doublets in unit volume which fulfil.these conditions is 1 7 If we denote by g and g+dg, h and h+dh, k and k+dk, the limits between which the velocity-components of the centre of gravity of the doublets must lie (the coordinate axes being rectangular and fixed), then G?dG dx=dg dh dk. Now keep g, h, and & constant, and place at the centre of the shell a system cf rectangular coordinates whose z-axis is in the direction of G; denote the coordinates and velocity-com- ponents of the nucleus relatively to this system by 2, y, 2, Uy, Vj, W, respectively, and transform these six variables in , L, H, p, e,@. We then introduce a second system of co- ordinates, referred to which the coordinates and velocities of the shell are 2, Yo, 22, Ug, Ve, We, respectively. The z-axis of this second system is to be taken normal to the plane of the central motion, and its z-axis in the section of the plane of Equilibrium of Vis Viva. 171 central motion and the old zy-plane. We have then H=Gsin 08, 90—@ being the angle between the two axes of z; therefore, since G is constant, dH=G cos 6 dé. Winally, let us denote by the angle between the two w-axes, seeing that it only differs from the angle previously so designated by a quantity which we are at present regarding as constant. In this case sg=w, cos Osin w + y; cos 8 cos w + 2; Sin O, We =U, Cos Osin w + v, cos 8 cos @ + w, sin 8, and these two expressions must both vanish, inasmuch as the xy plane is that of the central motion. By means of these two equations we can introduce @ and @ in place of z, and w,, when #, 7; % and vy, are constants, and we thus obtain oy le de. dz, dw, = (yu — 20) — Further Xy= #1, COSM—Y; SIN @, Yo SInO=2,sin wo +4, COS @, with similar equations for 2, v2, u, v. From these it follows that YU — Ly = sin O (yyto— Xyvq) = K sin 9, and, if 0 and » are contants, day dy, sin @=da,dy,; dugdvsin 0=du, dv, from which : diy dy, dz, du, dv, dw,=K cos 8 daydys dug dv, dO dw. Now let us denote, as before, by o and 7 the component velocities of the relative motion of shell and nucleus in the direction of p and normal to this direction, respectively ; then for constant values of w, and y, do dr=duydvy K=pr, L=h a qn (0? +7”) + h(p) , 7 © 2(m+m') p nl! dKkdL= emit oe do dr, where [iy is the energy ‘ee anal of the centre of gravity, and 172 On the Equilibrium of Vis Viva. is now constant. Finally, let the angle between p and the last apsidal line be yr, then a=pcos(etp), Y2=p sin(e +), in which ¥ is a function of p, K, and L ; both the latter are now constant, and therefore pdpde= day dy2. Collecting all these equations ee find that da, dy, dz, du, dv, dw,= a ae isd ae dK dL dH dp do de ; and it will immediately “ seen ae if coordinates and velocities without suffix or affix refer ae any random set of fixed coordinate axes, we must have likewise dx dy dz du dv dw= ee dK dl dH dp dw de. Introducing this in equation an es remembering that for constant values of wu, v, and w, mils Lis oe dv" dw", we find (m+m 1 mt WW Jo Topol 167° (m+m")* KG, Kad dy dzdu dy dw du! dv’ dw for the number of doublets in unit of volume for which the variables w...w’” lie between z and x+dw...w" and w”+dw." But we have previously found for this number the expression F . dex dy dz du dv dw du! de! dw", and we then saw that F must be of the form Ae—*”, in which A is a function of ¢",p, and «” ouly. It follows then, if we write K= NB Ye IES PO) that B must be on the one hand a function of e”, p,and a” only, and on the otker hand a function of K, L, G,and H only. B must therefore be a function of these latter variables which i is quite independent of c, «, and 8, and only a function ore oranda < If we put B=/(K, L, G, H), then this function must be independent of ¢, «, and 8, for all values of c” and #”. Sub- stitute for the variables K, L, G, H their values from 11, 12, 13, and 14, and make c’=0 at first. Then K=pcesina, L=}mc’+¢(p), G=me, H=0. 2 B=/(posin 2,“ +$(p), me, 0). The Fusion Constants of Igneous Rock. 173 As this expression is independent of ¢ and & the function f does not contain the quantity K, and it only involves L and G in the form 2mL—G’. We can best express this by writing the function with variable 2mL—G?, instead of L, G, when it becomes B=/(2mL—G?,H). If we introduce again into this expression the general values given in equations 11 to 14, we see that the two variables in the function are quite independent of each other if c, a, 8 are to have all possible values. And since B is constant for all values of ¢, a, and £8, it is so for ail values of 2mlL—G? and H, and is therefore absolutely constant. The distribution of ws viva is therefore obtained. XXIL. The Fusion Constants of Igneous Rock.—Part II. The Contraction of Molten Igneous Rock* on Passing from Liquid to Solid. By Cart Barusf. [Plate V. | INTRODUCTORY. if. VPA TERIAL and Method.—The following volume- -’* measurements were made for Mr. Clarence King, on a typical sample of diabase which he furnished. The method of testing the volume-behaviour by allowing the rock to expand in a vertical tube provided with an index was suggested to Mr. King by Lord Kelvin. I therefore pre- ferred it to a method of my ownf, in which the behaviour in question is to be determined by high-temperature air-volumetry, with the rock enclosed in a glazed platinum bulb-and-stem arrangement. In place of the index or float I employed an electric micrometer, believing a probe of this kind to be more trustworthy (§ 13). Imay state here, that the fact that the con- traction of the magma in passing from liquid to solid can actually be measured by the simple burette method was to mea great surprise. After many trials I found, however, that by allowing the furnace to cool so slowly that the platinum vessel remained rigid relatively to the charge, the contraction of the latter could be followed even into the solid state. As a consequence of slow cooling, moreover, the magma was probably undercooled, and | thus obtained the whole volume- difference liquid-solid at a given temperature. The data are * Cf. note in American Journal, xli. p. 498 (1891). + Communicated by the Author. t Cf. Phil. Mag. July 1892, where this method is tentatively employed to measure the expansion of white-hot porcelain. 174 Mr. Carl Barus on the Fuszon sufficient to compute the corresponding contraction at other temperatures. 2. Literature—The question has elicited voluminous dis- cussion ; but literary comments are superfluous here, since ‘Prof. F. Niess*, of Hohenheim, not long ago made a careful survey of all that has been done on the subject. The reader desiring specific information is referred to this interesting pamphlet. ‘Hs ist ein durch Contraste buntes Bild,” says Prof. Niess (loc. cit. p. 36), “welches in der vorstehenden Citatenlese dem lLeser zu entrollen war, und aus dem Wirrwarr entgegengesetzter Ansichten heben sich nur zwei Korper: Wismuth und Hisen, heraus, iiber welche man wohl mit absoluter Sicherheit die Acten als geschlossen bezeichnen kann, und zwar in dem Sinne, dass fiir sie die Ausdehnung im Momente der Verfestigung als zweifellos bewiesen gelten kann. Die iibrigen Metalle stehen noch im Streit, und fiir sie gilt dasselbe was wir fiir die kiinstlichen Silicate zu fordern Hatten’. 52). 2 ” Now iron, in virtue of the occurrence of recalescence (Gore, Barrett), is scarcely a fair substance to operate upon; and it heightens the confusion to find that Prof. Niess, after weighing all the evidence in hand, is obliged to conclude that rocks expand on solidifying. The present experiments show beyond question, I think, that at least for diabase this is not true. I find that this rock not only contracts between 3°5 and 4 per cent. on solidi- fying, but that such solidification is sharply broken and only apparently continuous with temperature, and that the fusion- behaviour throughout is quite normal in character. Hence, with certain precautions which I shall adduce in the course of this paper ($ 21), the volume thermodynamic relations which I derived by acting on organic bodies may be applied to rock magmas. 3. Lifect of Fusion. Density—The rock after fusion is changed to a compact black obsidian, and quite loses its characteristic structure. It was therefore important to examine the volume-relations of this change, preliminarily. This is done in Table I., where the dersities obtained with lumps of the rock (mass M) at the temperature ¢ are given, A being the density before, A’ after fusion. * “ Ueber das Verhalten der Silicate ete.,” Programm zur 70, Jahresfeier d. k, Wirtemb. landw. Academie, Stuttgart, E. Koch, 1889. Cf. Niess u. Winkelmann, Wied. Ann, xiii. p. 43 (1881); xviii. p. 364 (1883). Constants of Igneous Rock. 175 TasLEe 1.—Density of Diabase before and after Fusion. Before Fusion. After Fusion. _ Sample M. | t. | ac Sample M. Z, ie ieee No | | No. a —- | | ie ec y I. | 228950, 25 | 30161 || *Z |699330] 21 |2-701é] -104 | Tf. | 45:3654| 21 | 30181 ‘II. |33-'7659 | 19 |2:7447] -090 Ill. | 547208) 21 | 30136 || +IIT. |29:9777 | 19 | 2°7045} -1038 IV. | 69-4940! 21 | 3-0935 The rock was fused both in clay and in platinum crucibles. In the latter case the density of the known mass of metal had been previcusly determined, and the glass was not removed from the crucible. In the other case the clay was broken away from the solid lump within, and its density then measured directly. A few small bubbles were visible on the fresh fracture of the glass, due, I presume, to the ejection of dis- solved gases on solidification. At some other time I will make vacuum-measurements of the density of powders both of the rock and the glass, but I do not believe the data of Table I. will be seriously changed by such a test. From Table I. it appears that the mean density of the original rock is 3°0178; that of the glass after fusion is only 2-717, indicating a volume increment of 10 per cent. as the effect of fusion. This remarkable behaviour is not isolated. Niess (J. c. p. 47), quoting from Zirkel’s Lehrbuch, adduces even more remarkable volume-increments of the same naturet; viz., in garnet 22 per cent., in vesuvianite 14 per cent., in orthoclase 12 per cent., in augite 13 per cent., &.: but I doubt whether the great importance of these facts has been sufficiently emphasized. Suffice it to indicate here that it makes an enormous difference into what product the magma is to be conceived as being solidified ; and that throughout this paper the molten rock solidifies into a homogeneous obsidian. I am only determining, therefore, those volume- * Fused in a clay crucible. Glass detached when cold. + Fused in a platinum crucible. Glass not detached. t Cf. Thoulet, Ztschr. f. Kryst. u. Mineralogie, v. p. 407 (1881); Bull, Soc. Min, de France, iii. p. 34 (1880). 176 Mr. Carl Barus on the Fusion changes which lie at the margin, as it were, of the more profound and chemically significant volume-changes (poly- meric passage from homogeneity to organized rock-structure), even though the latter may be conceived as producible by pressure alone, under conditions of nearly constant (high) temperature. I may add, in passing, that the magnitude of the chemical changes of volume makes it advisable to carry the work on the effect of pressure on the chemical equilibrium of solids and of liquids, and on the solution behaviour solid- liquid, into greater detail than I have thus far attempted*. APPARATUS. 4, Temperature Measurement.—In work of the present kind an apparatus for the accurate measurement of high tempera- tures is the fundamental consideration. I may, however, dismiss this subject here, since I discussed it in the intro- ductory papert. The temperature-measurements of this paper were made with a thermocouple of platinum and pla- tinum with 20 per cent. of iridium, which had been frequently compared with my re-entrant porcelain air-thermometer throughout an interval of 1100° C., and tested for freedom from anomalies beyond this interval. Inasmuch as the electric method consists in expressing thermoelectromotive force by aid of a zero method, in terms of a given Latimer- Clark standard cell, the temperature-apparatus is of the same order of constancy as to time as the standard cell. To find in how far my earlier data were trustworthy after the lapse of upwards four years, I made fresh check measure- ments of the boiling-points of mercury and of zine. The latter only need be instanced here. My original mean datum of the boiling-point of zinc, expressed as electromotive force for the couples under consideration, was (1887) e.=11,074 microvolts, the cold junction being at 20° C. The new expe- riments (1891) gave me data as follows :— Thermocouple No. 35, és) = 11,168 (microvolts), e No. 36, 5 hdl 2 5 No. 39, joe Tai = is No. 40, 72) aa a Means eis. 12d aliag = * American Journal, xxxvii. p. 339 (1889); ibid. xxxvyiii. p. 408 (1889) ; ibid. xl. p. 219 (1890); ibid. xli. p. 110 (1891) ; ibid. xlii. p. 46 et seg. (1891). Also Phil. Mag. [5] xxxi. p. 9 (1891), tT See this Magazine, July 1892, p. 1. Constants of Igneous Rock. 177 agreeing very closely with subsequent specially careful measurements, v1z.:— Thermocouple No. 86, é) = 11,131 (microvolts), Nor 30, ,, tlts4 i The difference of values, new and old, is 60 microvolts, only about 4 per cent. as regards electromotive force, and corre- sponding to about 4° at 1000°. In view of the excessive use and abuse to which the couples had been put in the lapse of time this result is gratifying. Endeavouring to ascertain where this discrepancy was to be sought, I also made new comparisons between the Clark cell and a normal Daniell of my own (Bull. 54, U.S. Geolog. Survey, p. 100), in which the cells are separate, and only joined during the time of use. Supposing the electromotive force of the former to have been e=1°435 throughout, the following succession of values obtained for the standard Daniell :— March SSO 20e Cr eee 38, mugust ~ 18871,.238° C., 1:139, September 1891, 27° C., 1:147. If, therefore, instead of regarding the Clark cell as constant I had attributed* this virtue to the standard Daniell, the small thermoelectric discrepancy equivalent to 4° at 1000° would be altogether wiped out. Now I made the Clark cells in question as far back as 1888, when less was known about details of construction than is now available. I conclude, therefore, that the discrepancy is very probably in the standard cells, and that the thermocouples have remained absolutely constant, a result which is borne out by my boiling-points of cadmium. , Apart from this, the new standardization with boiling zine fixes the scale relatively to the accepted value for this datum. 5. General disposition of Apparatus.—This is given in Plate V. on a scale of 1: 4, where figs. 1 and 3 are sectional elevations showing the parts chiefly with reference to their vertical height, and fig. 2 is a sectional plan, in which the parts are given with reference to the horizontal. The molten rock, Z Z, contained in a long cylindrical pla- tinum tube, largely surrounded by a tube of fire-clay, FF’, is fixed vertically in a tall cylindrical furnace, DD, LL. The heat is furnished by six burners, B, B,..., fed by gas and an * Our laboratory affords insuflicient facilities for the direct measure ment of electromotive force. 178 Mr. Car] Barus on the Fusion air-blast, laden, if need be, with oxygen. These burners are placed at equal intervals along the vertical, three on one side and three on the other (see fig. 2), and set like a force-couple, so as to surround the platinum tube with a whirlwind of flame. Suitable holes are cut in the walls of the furnace for the sym- metrical insertion of the insulated thermocouples, T, and also at S for fixing the sight-tubes, A, near the top and the bottom of the furnace. Parts of the envelope of the platinum tube are cut away, so that the upper and lower ends of the (red hot) platinum tube can be seen in the telescope of an external (screened) cathetometer. Thus the expansion of the platinum tube is measured directly. A vertical micrometer, Kkd (figs. 3 and 4), insulated so as to admit of electrical indica- tions of contact, furnishes a means of tracing the apparent expansion of the rock Z Z, within the fusion-tube. In principle, the excessively slow cooling of the furnace is to be so conducted that the magma may always remain much less viscous than the practically rigid platinum envelope (§§ 1, 18). The furnace stands on a massive iron base perforated by eight holes, into which vertical iron uprights are screwed, symmetrically surrounding the furnace and at a distance of 4 or 5 centim. from its circumference. Only one of these is indicated at QQ (fig. 8), the rest with other subsidiary parts being omitted to avoid confusing the figure. ‘T'wo of these uprights h hold the vertical micrometer, two hold the burners in place, and two subserve as buffers for the clay arms, H, H,... by which the fusion-tube is adjusted verti- cally. The sight-tubes are suitably clamped to the seventh and the insulators of the thermocouples to the eighth. All these uprights are hollow, and a swift current of water con- tinually circulates through them, issuing still cold to the touch. The same current also flows through the bent screen, X X, of the vertical micrometer, and through the vertical flat screen of the cathetometer. 6. Lhe Furnace-—The burners, B, are each fed with the same amount of gas and air by properly branching the large supply-tubes. A graduated stopcock is at hand for regulating the supply of gas to a micety. Hence the furnace is fed with a mixture of gas and air, and temperatures between 400° and 1500° are obtained by ‘simply making the influx poorer or richer in combustible gas. Oxygen ‘has not thus far been necessary”. - * Burners suitable for the above purpose are shown in Bee little shi on high temperatures (Leipzig, Barth, 1892). Constants of Igneous Rock. Ig The products of combustion are carried off by the two oblique tubes, E, H, in the lid LL (fig. 4). Nete that the water-screen bends around the vertical micrometer in such a way that flames issuing from E do no injury, and a perforated free plate, mm, closes the vertical hole in the lid L L. Two large size Fletcher-bellows, set like a duplex-pump and actuated by a gas-engine, furnished the air-blast. In order to insure greater constancy of temperature, and at the same time increase the high temperature efficiency of the furnace, it is essential to jacket both the latter and the lid heavily (1-2 centim.) with asbestos. 7. Fusion-tube-—The platinum tube holding the molten rock ZZ is 25 centim. long and about 1°5 centim. in dia- meter, drawn as accurately cylindrical as possible and provided with a flat bottom. To protect this tube from gases, to keep it from bulging in consequence of the fluid-rock pressure within, and to insure greater constancy and slower changes of temperature, the platinum tube is surrounded by the fire- clay tube F F (figs. 1 and 6) fitting loosely. Care must be taken to allow for shrinkage of the clay, which in a fresh tube, after some hours’ exposure to 1500°, exceeds 3 per cent. or more, and is permanent. After this the tube expands nor- mally. It rarely warps, and may therefore be fixed by fire- clay arms, H (figs. 1, 2, and 7), suitably clamped on the outside of the furnace. Near the bottom a perforated ring, CC (figs. 1 and 5), embraces both the tube FF and a pro- jection, G, in the furnace. 8. Thermocouples.—In addition to figs. 1 and 2, figs. 6 and 8 give a full account of the adjustment. The tube FF is laterally perforated with three pairs of fine holes, t, corre- sponding to the two canals of the insulator*, TT. The wires of the thermocouple are then threaded through ¢ and the insulator canals, in such a way that the respective junctions lie in small cavities at ¢, immediately in contact with the out- side of the platinum tube. Holes are left in FF and the furnace for this operation. _ The cold junctions of the thermocouples terminate in three pairs of mercury-troughs, insulated by hard rubber, and sub- merged in a bath of petroleum. With these troughs the terminals of the zero method are successively connected, and the temperatures of the top, the middle, and the bottom of the fusion-tube measured by § 4. * The method of making these is given in Bull. No. 54, U.S. Geolog. Survey, p. 95. 180 Mr. Carl Barus on the Fusion 9. Seght-tubes.—Grunow’s excellent cathetometer is placed on a pier, so that the prism of the instrument is only about 50 centim. oft from the fusion-tube. A tall, hollow screen, 30 centim. broad, 70 centim. long, and 1 centim. thick, fed with cold water, and movable on a slide, is interposed between furnace and cathetometer. Slots, cut through the screen and closed by plate glass, correspond to the two posi- tions of the telescope ; and the lines of sight pass through S, 8, near the top and the bottom of the furnace (see figs. 1 and 2). Thus the ends of the fusion-tube, one of which pro- jects above the clay tube F F, and the other is seen through the perforation O in © C (figs. 1 and 5), appear as sharp lines in the telescope, against the red-hot background of clay. It is necessary, however, to prevent the escape of flame and gas at S, and hence these holes are provided with porcelain tubes A (only one shown in the figure) about 15 centim. long, the outer end of which is ground off square and closed with a piece of plate glass b, by aid of a clamping device aa. 10. Vertical Micrometer. — Figures 3 and 4 give a full account of this instrument (also made by W. Grunow), both of which are sectional elevations at right angles to each other. The millimetre-screw plays easily through the massive block of brass, P P, and the fixed lock-nut gg. P P is bolted down to the rigid bridge of brass, NN, by means of screws, RR, and the counterplate U U. The ends of NN are provided with sleeves, p p, and a clamp-screw, M, whereby the whole micrometer may be moved up or down or fixed in any posi- tion along the uprights, QQ. To secure insulation of the screw K £, R, Rare surrounded by jackets n, n of hard rubber, and plates, 7,7, q of this material are suitably interposed be- tween PP, NN, U U, and other parts. Sufficiently wide slots are cut in the bridge, N N (see figures), whereby the plate may be shifted in any direction, and then clamped in position. In view of the heat which rises from the furnace, an N- shaped screen, X X, through which water rapidly circulates (entering and leaving at diagonally opposite points, V and Y, at the top), nearly envelopes the micrometer. The micro- meter-screw passes through a narrow tube in the bottom of XX; hence the screen must also be adjustable, and a way is shown in the figure. Thus the micrometer and its water- screen slide as a single piece, along the upright QQ. Q and Y are joined by a sufficient length of rubber hose, a connexion merely indicated in the figure. Constants of Igneous Rock. 181 Finally K & is prolonged by a straight cylindrical tube of platinum dd, which may be fixed to the steel rod & by the clamp ¢ in any position along the vertical. The tube fits the rod & singly, and a special steel rod is provided by which the tube may be straightened, should it become warped. The lower end of d is clearly visible in the telescope of the cathetometer, through the sight-tube A. On being screwed down, d enters the fusion-tube axially, supposing both tubes (d and Z Z) to have been properly fixed in position. In how far such adjustment has been made, can be seen by tempo- rarily removing one of the efflux tubes, H (fig. 4), when the parts concerned are visible to the eye. 11. Telephonic Registration—Since it is necessary to find the depth of the meniscus of the molten rock ZZ below the plane of the top of the fusion-tube, the moment of contact of ZZ and d is registered electrically. Above, say, 500° C., rock is a good conductor. Hence, if a current be passed into the screw K k, through the clamp-screw / (fig. 3), it will issue at the bottom at the clamp-screw c (fig. 1), provided ¢ be electric- ally connected (platinum wires) with the bottom of the fusion- tube, Z Z A telephone actuated by Kohlrausch’s small inductor is more conyenient for the present purpose than a galvanometer. Contact is then indicated by a loud roar, and the observer’s attention is not further distracted. Ifthe glass Z Z be sticky, the drawing out of a thread corresponds to a more or less gradual cessation of the noise, so that the character of the fusion can be pretty well indicated in this way. Care shouid be taken to insure a small sparking-distance. If the expansion of the rock be known, and the tube dd be sunk deeply into the mass, it is clear that the present method admits of a measurement of the relation of the electric resistance of the glass and temperature. JI mention this, believing that not only will a suitable method of temperature measurement be thus available, but that the volume diagrams, constructed below, may also be derived solely from measure- ments of electrolytic resistance *. Mertuop oF MEASUREMENT. 12. Consecutive Adjustments.—Thus far I have only studied rock-contraction. For this purpose, the graduated faucet, * Cf. Am, Journ. Sci. xlii. pp. 134-35 (1891), where I have already speculated on the character of electrolytic resistance referred to tem- perature. 182 Mr. Carl Barus on the Fuszon §§ 5, 6, is turned on in full, and the furnace fired as far as 1400° or 1500°, when the measurements may be commenced. The length of the fusion-tube is first accurately measured by cathetometer observations at the bottom and the top. The telescope is then left adjusted for the top, and the vertical micrometer (centrally fixed) screwed down until the image of its lowest point is in contact with the cross hairs. After this the micrometer is further screwed down, until the telephone indicates contact between the platinum micrometer-tube and the meniscus of molten rock. The difference of readings gives the depth of the latter below the top plane of the fusion- tube. I usually repeated these measurements three times. Hereupon. the temperature measurements were made by connecting the terminals of the zero method with the lower, the middle, and the upper thermocouple. Finally, the cathetometer and micrometer measurements were again repeated in full. Uniform heating presupposed, it was permissible to regard the two sets of length measure- ments as coincident with the intermediate temperature mea- surement. This done, 1 frequently waited 15 minutes or more, to make another complete measurement, under better conditions of constant temperature. The graduated stopcock was then partially closed by a proper fractional amount, and after waiting a sufficiently long time, the same series of measuring operations was gone over again. Thus I continued until the glass became sticky and solidification imminent, when longer waiting and more finely graded changes of temperature were essential. Fortunately the observer can infer the state of fusion very well, by noting the time necessary for the glass threads drawn out by the micrometer to break, § 11. Finally, the enamel on the end of the micrometer-tube becomes solid and ceases to change its form, simultaneously with which the marked contraction of the molten mass in the fusion-tube begins. Having waited long enough for the lowest position of the meniscus, temperature may be varied in larger steps again. When the furnace is dark, measurement is no longer pos- sible. I then allowed the whole arrangement to cool over night, and next morning determined both the depth of the solid meniscus and the length of the cold tube. The former was computed from bulk measurements (with water) as well as measured micrometrically. These are the normal or fiducial data to which all the other volumes were referred. Constants of Igneous Rock. 183 13. Computation.—Let the linear expansion of the platinum fusion-tube be given by /=h(1+/(é)), where / and J) are the lengths at ¢ degrees and at zero respectively. Let » and Ay be the depths of the meniscus below the plane of the top of the fusion-tube, and v and wv the volumes of the enclosed molten magma at ¢ and zero respectively. Then, if (1+/(¢) )’ is nearly enough 1+ 3/(é); if the expansion constants of the fusion-tube and of the micrometer-tube be the same, and if in consideration of the small motion of the latter and the high temperature in the furnace, the air temperature outside of it be nearly enough zero, since 0/0) = (g—A)(1 +/(t))?/(lo— Ao); (ve— v9) /Vp=3F (4) + Ap—A)(1L + 8/(4) (lo — Av)» «1D Here 3 /(¢) is directly given at each observation, or may be computed by some smoothing process from the data as a whole. The equation, therefore, gives the actual expansion of the rock, in terms of unit of volume of solid rock at zero Centi- gerade. If this be multiplied by the initial specific volume, the absolute expansion is obtained. An inspection of (1) shows that in the factor Ay»—A, the micrometer value of the length 2X is to be inserted in both cases, supposing the contour of the meniscus to remain similar to itself; whereas in /)—)A, the value of \y determined from bulk measurements of the space at the top of the cold tube is suitable, since the tube is flat-bottomed. I may add in passing that if 6H be the rise of a flat-bottomed cylindrical float of platinum, submerged to a depth A in a column of magma of height A, then nearly eee GROEN Nn vusule Cory (2) Since, therefore, the float shortens the efficient length of the fusion-tube and there is difficulty in determining A in this case, the above micrometric method is preferable quite aside from flotation errors due to viscosity and capillarity, to the easy welding of white hot platinum surfaces, to the tendency of gas bubbles to accumulate on the surface of the float, to the cessation of true flotation during the change from liquid to solid, &e. 14, Lrrors—The change of temperature from top to bottom of the fusion-tube is measured. The change of tem- perature from circumference to axis of the fusion-tube is nel 184 Mr. Carl Barus on the Fusion in proportion as the furnace cools slowly. The latter con- dition is met at least so long as glass is liquid, and data for the former are fully given below. ‘To avoid strains of dilata- tion it would be desirable to make the glass solidify from the bottom upward. This, however, my furnace as yet fails to do. Indeed, I have frequently noted lateral holes shaped like an inverted funnel and terminating in the otherwise smooth surface of the meniscus. This may indicate the occurrence of gas bubbles under the free surface or be a strain effect, § 3. The tendency of these nearly unavoidable difficulties is to make the solidification contraction too small; and I have therefore not been disturbed by them. Only at very high temperatures (above 1500°) did I obtain apparent evidence of the viscosity of platinum relatively to the pressure of the column of 25 centim. of molten rock, whereas the combined system of platinum and clay tube with- stood this pressure. There is also a slight deepening of the meniscus from day to day, and a similar decrease of the length of the platinum fusion-tube ; but, thus far, I have encountered no serious error due to the high temperature viscosity of the vessel, § 18. The assumption that the meniscus remains similar to itself in form at all temperatures cannot be quite true. At white heats, however, the glass wets platinum so thoroughly that convex forms of meniscus need never be apprehended. It is futile, however, to endeavour to make allowance for meniscus ; but data for the difference between the (cold) bulk and micro- metric measurements are given below. Although too much reliance must not be placed on the behaviour of the solid state, yet the values are redeemed from the character of mere estimates by the close coincidence of the expansion of pla- tinum and its solid glass core. Strains imposed on both the metal and the glass do not probably exceed the limits of elasticity of either, §§ 17,18. When cooling is conducted slowly enough, the experiments show that the platinum tube is not dragged along seriously by the solidifying magma; and the data thus retain a degree of trustworthiness greater than was anticipated, even in the solid state. At the same time dilatational strain is reduced to a minimum, and constancy of temperature throughout efficient parts of the furnace is promoted. One error much in my way thus far has been the allowance to be made for the expansion of the platinum probe dd (fig. 3). It is not merely the amount by which the probe is lowered that is subject to expansion, but a considerable length of the Constants of Igneous LItock. 185 metallic screw K kdd passes from a lower to an indeterminable higher temperature. I hope, however, in the future to obtain an estimate for this discrepancy, by measuring a given amount of thrust through the sight-tube with the cathetometer, and comparing this value with the corresponding value to be read off on the vertical micrometer. Hollow screws and water circulation would be exceedingly difficult to attach here. RESULTS. 15. Arrangement of the Tables.—In the following tables / and vp denote the length and radius of the (cold) fusion-tube, and A, the bulk value (water measurement) of the mean depth of the meniscus, these measurements being made on the day after the fusion experiments. ‘The temperatures at the bottom, the middle, and the top of the fusion-tube are given under 0, @2, 03, respectively. For each value of mean tempera- ture @, two data for the apparent expansion of the rock, for the volume-expansion of the fusion-tube, and for the actual volume-expansion, (v%—v)/vp= Ov/v,, of the rock are given, and they were obtained before and after the intermediate temperature measurement, respectively. Reference is thus made to unit of volume of solid rock at zero Centigrade, throughout. The data enclosed in parentheses show that for them, the value applied for the expansion of the fusion-tube is obtained as a mean result of all the measurements made, otherwise the value directly observed was directly applied. The chief constants are summarized at the end of each table. 16. Contraction of Diabase. Series 1. and I1.-——The results of these series, being of inferior accuracy and serving chiefly to substantiate the remarks of § 14, may be omitted here. They showed a liquid volume-expansion of 50/10° per degree, a solid expansion of 20/10° per degree, and a solidification contraction of about 3 per cent. only, owing to the occurrence of dilatational strain. 17. Contraction of Diabase. Series I1., Tables.—This work was done on October 20, 1891, and the data are given in Table II. Precautions for slow cooling were fully taken, and the solidification point is therefore sharply apparent. ‘The results will be discussed in connexion with the next series. Phil. Mag. 8. 5. Vol. 35. No. 214. March 1893. O 186 Mr. Carl Barus on the Fusion TABLE II.—Contraction of Diabase. {y= 25°466 centim., 03: 0,. | Mean G2. 0. a: oC: 1360 | 1886 1596 1403 1286 | 1300 1504 1311 1163 | 1166 1167 1168 1097 | 1093 1093 1089 1102 | 1095 1095 1088 929 | 896 897 863 461 | 468 453 510 20 | Rock, mean actual expansion, solid, 0°-1000° Apparent | Volume- volume- | expansion expansion of Rock. Sele 452 4D4 437 438 406 409 376 300 14 13 bo 33 39 of the tube. 8l Ov/ Up » x 104. 810 812 (808) (810) 77 ee (771) (772) 703 706 (706) (709) 646 603 (657) (614) 288 286 (296) (295) 211 (213) 0 Mean. 6v/Up. 0811 (-0809) ‘0079 0000 99 39 Series III. Time. Minutes. | Liquid. 0 23 86 hit 185 Ap=1'424 centim., 7>=°75 centim. Remarks. oT eT. Cd Liquid. Sticky. Very sticky. To be drawn out in threads. Eventually solidifying. Solid. Solid. Solid. Next day.| Cold. liquid, 1100°-1500° a contraction on solidification (1094°) Rock, mean apparent expansion, solid, 0° 1000° . : { a liquid, 1100°-1500° -0000205 Tube, mean v olume-expansion below 1000° above 1100° 99 99 29 29 -0000250 “0000470 °0390 "(000007 0000240 0000265 18. Contraction of Diabase. Series TV. Tables and Chart.— The data of the last series of experiments (made on October 21, 1891) are given in Table ILI. results correspond to each step of temperature. ‘wo complete sets of Constants of Igneous Rock. 187 TasBLe II1.—Contraction of Diabase. Series IV. () =25°447 centim., Ay’ =1:220 centim., ry=75 centim. se Ap parent Volume- ; ean.| volume- | expansion . Mean. , o> 8. | expansion Of the 8u/% ovjv ue. 3° of Rock. tube. 2G: oC: Sail: x 104. x 104. Minutes. 1374 | 1388 403 397 760 -0760 5 1394 404 (356) 761 (0760) 1395 | (759) (760) | 1415 | 1421 407 302 768 ‘0770 20 1431 409 (304) Tel (0771) 1417 (771) (773) #318 | 1319 | . 394 341 734 (0731) 50 1324 | i giicleyy (339) 727 (0730) 1315 (733) | (726) | 1304 | 1305 383 350 733 0736 65 1308 390 (335) 740 (0721) 1304 (718) (725) 1204 | 1190 307 316 673 "0672 90 1189 399 (305) 671 (0661) 1176 (662 ; (660) yg | 163 355 299 655 0652 105 1158 349 (299) 649 (0652) 1153 (655) (649) esse LV 339 286 625 “0628 128 1109 344 (286) 630 (0628) 1090 (625) (630) 1117 | 1092 200 275 475 "0475 151 1088 155 (280) 430 (0480) 1072 91 366 1109 | 1092 333) 282 315 0287 175 1081 5 (280) 287 (0285) 1086 946 914 13 213 226 0223 198 903 6 220 893 900 855 3 199 202 0202 210 827 3 202 837 20 0) 0 0) ‘0000 |Next day. a 5 a liquid, 1100°—1500° - conbenchion on solidification, at 1092° Rock, mean apparent expansion, 0%1000°. . . 6 ie . 1100°-1500° j Tube, mean volume-expansion below 1000° . . above LL0Q°... O2 xy mean actual expansion, solid, 0°—1000° . ( 9 39 39 °? Remarks. Liquid. ‘Liquid. Liquid. Liquid. Sticky. Very sticky. To be drawn out in threads. | Top en- crusted, Solidifying. | Solidifying, Solid. Solid. Cold. “QOV0250 ‘0000468 °0340 “QQOOQ005 “O0V0218 “Q000235 "O000260 188 Mr. Carl Barus on the Fusion ‘These data are given in the chart (fig. 10), temperatures in degrees C., as abscissee, volume- changes as ordinates. A ae of the same character may also be constructed from Table IL., but this is superfluous. In figure 10 the actual expansion of the rock is shown by the heavy line debef, and the numbers attached to the points of observation indicate the times at which they were made. ‘lhe apparent expansion of the rock is shown by the light line /kgh, where the ordi- nates of the solid contour are nearly zero. Finally the ex- pansion of the fusion-tube is represented by the dotted line deat. The amount of break at a, which is even smaller in Series ILI, indicates the amount of drag or a shortening of the length of the platinum tube by the solidifying rock within, and furnishes an estimate for the trustworthiness of the solid results. It is interesting to note that in both Series Il].and IV.the first length measurements of the tube are smaller than the second at the same temperature, showing ay the tube has to some extent recuperated from the strain, r that the amount of end thrust has diminished. It is Se auladle possible to note the sag as expressed by the cold lengths (25°49 centim. in Series II., 25:47 centim. in Series get ., and 25°45 centim. in Series IV.) of the plaiinum fusion- tube. Finally, the depth of the liquid meniscus at the outset of Series III: and IV. ., and at about the same temperature, was X=*5() centim. and A="62 centim., showing enlargement of the bulk of the tube. These changes, which are in part allowed for, show that viscosity introduces no serious dis- crepancy. Regarding the differences of A, and A, the remarks made in § 14 apply. An inspection of the curve dbef as a whole indicates the occurrence of sharply marked solidification at 1093°. This is sufficient evidence to prove that rock-fusion (diabase) is thoroughly normal in type. A method is thus given in which the solidifying-point is determined free from non- intrinsic tests. Finally, the contraction on solidification, 3°9 per cent. in Series ILI., and 3:4 per cent. in Series IV., is established, for diabase at least, beyond question. It is to be noted, more- over, that the smaller value (LV.) corresponds to a larger drag during solidification on the platinum tube (cf. Tables I. and IIl.). Hence the value 39 per cent. is the more probable. In general, temperatures (@,, 62, 63) are nearly alike so long as the glass is liquid. This ceases to be the case after solidification ; and since the top of the fusion-tube is apt to be colder than the bottom, some of the solid contraction expresses itself in dilatational strain, § 14. Constants of Igneous Rock. : 189 19. Flotation.—Naturally I made a few tests on the flota- tion of solid rock on the molten magma. Cf. § 3. To my surprise such flotation usually occurs, notwithstanding the fact that the original cold rock may be 8 per cent. + 10 per cent. more dense than the molten magma. The cause, how- ever, is crudely mechanical, since the rock, in virtue of its weight and temperature, hollows out a cavity and chills its surface simultaneously, forming a little boat in which it He on the very viscous liquid below. ‘This is indicated in fig. 9 where a is the body of rock, AA the molten magma, and bb the solidified skin. I also attempted to make Niess and Winkelmann’s “ Fundamentalversuch” (Niess, J. c. p. 16), by submerging the rock; but here, both on account of the intense white ‘elare of the furnace and the tendency to chill at the surface, I did not reach a definite point of view. INFERENCES. 20. Hysteresis-—In the above experiments I have only studied the solidifying magma. It does not appear, there- fore, whether solidification and fusion take place at identical temperatures, or whether they will comprehend a volume-lag. In other work, in which the rock of the fusion-tube was alternately fused ‘and solidified, the loci are oy clic in marked degree, covering considerably more than 50°. It so difficult, however, to discriminate between true hysteresis and the accompanying discrepancy due to insufficiently rapid heat conduction as compared with the insufficiently slow change of temperature, that experiments made with a tube which is not at quite the same temperature throughout its length are not unassailable. Having failed to perfect the experiments, I omit the data altogether. 21. Melting-point “and Pressure.—Since the fusion of rocks like diabase is thoroughly normal, it follows that melting- point must increase with pressure. It is well to examine tentatively into the nature of this relation, and for this pur- pose I have constructed certain unpublished results of mie for thymol, in the same scale as used for the rock, in fig. The curve mn'olp! shows the contraction of thymol at Fe melting-point (somewhat below 50°), where the substance is quid along o’p’ and solid along m'n'. The curve mnop similarly applies at O°C. It is seen, therefore, that here solidification contraction and thermal expansion (solid or liquid) decrease together. This is also true on passing from thymol to the rock. Could liquid thymol be cooled down as far as —25°, it would then show the same solidification con- traetion as fie silicate. 190 Dr. J. R. Rydberg on a certain Asymmetry Analogously the latter must show decidedly smaller com- pressibility than the organic body, and hence it follows that whereas the lower critical pressure (solid-liquid) of naphtha- lene, for instance, lies in the region of some 10,000 atmospheres in my experiments, the corresponding (critical) pressure of the rock magma will be indefinitely higher. From this, however, it is by no means to be inferred that the relation of melting-point to pressure (d@/dp) will be different in the silicate and in the carbon compound. In the latter case data for normal fusion are available for wax, paraffin, spermaceti, and naphthalene. These lie within a margin of ‘020 to ‘036. Taken into consideration with the difficulty of obtaining these data, the preliminary character of the experiments, the lack of crystalline definiteness in many of the compounds, and the fact that even for the same sub- stance* the coefficient may vary as much as ‘027 to -035, the said margin may reasonably be regarded as narrow. It appears to me probable, therefore, since fusion in the organic bodies and the silicate is alike in type, that the same factor d@/dp will correspond to both cases. Direct evidence in favour of this view will be adduced in my next paper. XXIII. On a certain Asymmetry in Prof. Rowland’s Concave Gratings. By Dr. J. R. RypBere, Docent of Physics at the University of Lund, Sweden f. I. i order more especially to obtain a series of observations fitted for a continuation of the studies on the spectra of the elements, of which the commencement has been pub- lished in my “ Recherches sur la constitution des spectres linéaires des éléments chimiques ”’ (K. Svenska Vetensk. Akad. Handl. Bd. xxiii. No. 11), a spectroscope with one of Prof. Rowland’s concave gratings (10,000 lines to the inch) was procured for the Physical Institution of the University of Lund. It was mounted in a most excellent manner by the Mechanician of the Physiological Institution, Hilding Sand- strém, according to the instructions of Prof. Rowland (see Ames, Johns Hopkins University Circulars, viii. No. 73, May 1889; Phil. Mag. [5] xxvii. p. 369), but with full freedom in the details of construction. The adjustments also were executed according to the same instructions, but * See my work for Naphthalene in American Journal, xlii. p. 144, el seg., 1891. + Communicated by the Author. rn Prof. Rowland’s Concave Gratings. 191 with greater precision in the special determinations with the intention to obtain by the exactness of the adjustment the same scale through the whole spectrum. However, when all adjustments were completed, no distinct image could be obtained in any part of the spectrum. In the visible spectrum of the first order the image was not very much out of focus, but the deviation increased gradually, so that it became necessary to displace the eyepiece several centimetres to obtain well-defined images of the spectra of higher orders. All details being executed with the same accuracy, there was nothing that could indicate the cause of the discrepancy, so that nothing remained but to make all the adjustments over again, determining at the same time the extreme limits of the errors. [or this purpose I have made use of new methods of adjustment, and I have ascer- tained by these researches :— 1. That the courses which the apex of the grating and the cross hairs of the eyepiece follow in their movement on the rails do not deviate in any point from straight lines by more than 0°2 millim. 2. That the angle formed by the average directions of the rails did not differ from a right angle by more than 15” (corresponding to an arc of 0°5 millim. at one of the ends of one of the rails), the difference probably not amounting to more than a third of this value. 3. That the middle of the slit could not be more than 0:2 millim. from the crossing-point of the lines that are described by the apex of the grating and the cross hairs of the eye- 1ece. A, That the apex of the grating and the cross hairs of the eyepiece were not more than Q'l millim. distant from the axes of the carriages. 5. That the distance peraean the centre of curvature of the grating and the axis of the carriage on which the eye- piece was placed, did not amount to 0°5 millim. during the whole movement. 6. That the lines of the grating and the direction of the slit were parallel and at right angles with the plane of the . That the grating was entirely free from all constraint a of spherical form, the j images in the centre of curvature being of excellent definition. 8. That the optical state of the slit was perfectly normal. With these results it was only in the grating itself that the cause of the displacement of the spectra could be looked for, either in some imperfection of the theory or in some 192 Dr.. J. R. Rydberg on a certain Asymmetry fault in the execution of the work, at least with regard to the special grating in question. Hitherto, I had not deemed it possible to make any of these assumptions, as it seemed that Prof. Rowland himself and other spectroscopists who have used the concave gratings ought to have recognized such an anomaly, if it existed. During all the adjustments the grating was left in the same position in its holder, so that I had made use only of the spectra on one side of the grating. Now it was removed from its holder and, after being reversed, it was adjusted in the same manner as before, with the intention of learning whether the focal curve that passes through the centre of curvature is symmetrical with respect to the principal axis of the concave mirror. ‘Then it was found that the distance between the grating and the eyepiece ought to be increased in order to get distinct images, while before it was necessary to diminish it. From this it was evident that the inaccuracy in the position of the images was due to the grating. II. First of all the question was to determine the true form of the focal curve that passes through the centre of curvature of the grating. According to Prof. Rowland’s theory this ought to be a circle, which should have as a diameter the straight line that unites the centre of curvature with the apex of the grating. Ifthe form of the curve differed perceptibly from a circle, it would not be possible with these gratings to obtain spectra of a uniform scale. Fig. 1. ay SS 0, 0) _ The form of the focal curve can be determined with the greatest facility, if the apparatus is altered in such a manner in Prof. Rowland’s Concave Gratings. 193 that the slit is made movable along the rail that carries the grating. Let G,G, (fig. 1) be the grating, C its apex, O its centre of curvature, CLOM the theoretical focal circle, ClL,O,; OM, the true focal curve that passes through O,L the slit in its original place at the point of the right angle which is formed by the rails LO and LO. Then, on displacing the slit along LC or its elongation to a certain point Ly, it will always be possible to obtain distinct images of the spectra, supposing in all cases that such can be given by the erating. This point L, belongs to the curve in question, whose polar coordinates will be determined by measuring the radius of curvature CO (p), the displacement LL, (d), and the angle LCO (w). For then, supposing d to be positive, when the slit is moved away from the mirror, the radius vector L,C=r=pcos w+d and the vectorial angle =p. Denoting the wave-length by A, the number of order of the spectrum by n, the distance between two adjacent lines of the grating by w, we should have, if the theory were exact, Si = Ee 2 is nv=— . LO, p ©) p To decide whether the same formula can be applied in the present case, it will be sufficient to displace the slit along the rail LC and to observe if any change is produced in the spectrum, viz., if the same value of mw always corresponds to the same value of 2» independently of the value of r. In reality small irregular variations were found, which did not seem to exceed one of Angstrém’s units, and which were doubtless due to imperfections in the rails and the adjust- ment, According to the theory of concave gratings a dif- ference of one Angstrom’ s unit in the spectrum corresponds to a lateral displacement of the slit varying in the spectra of different orders between 0°25 and 1 millim. Consequently the formula is exact within the limits of error of our experiments. It follows that the angle ¢ of the segment CL,O is determined by the equation Boo Nae LON p.nr In this formula d and nd being the only variables, we see Cone that it is sufficient that their quotient © be constant, in order that the angle e may be so too. III. The measurements were executed in such a way that the spectroscope was directed on some known line of the 194 Dr. J. R. Rydberg on a certain Asymmetry spectrum and the movable carriage that bears the slit dis- placed along the rail LC, until a distinct image was obtained in OQ. The position of an index, attached to the carriage, was read on a millimetre-seale fixed to the rail LC. Hach of the numbers given in the following table under a, and a, is the mean of 10 of these readings, the carriage being alter- nately brought near to and removed from the grating. The column a, corresponds to the spectra on one side of the grating, the cclumn a, to those on the other; a greater value denotes a greater distance from the grating. It was found that the slit could be displaced through the space of about one millimetre without it being possible to distinguish any variation in the definition of the image. The probable errors of the means amount in general to 0°2 millim., they never exceed 0°4 milliim. Using as a source of light some- times the sun, sometimes the yoltaic arc, I directed the spectroscope in the spectra of the first four orders to the weak lines between D,; and D, (A=5893) and to the double lines 6; and 6, of the solar spectrum or the strong doublets of the neighbouring band of carbon (A about 5165). | : Calcu- | iat Wave: | Observed. | lated. | ow lengih- fae al ies. 3(44+4,) od —. | 4. | ae I. ,.../1%5165| 1838] 1538 | - 1438 | —100| +100] 94 I. D...|1x5893| 183-4] 1556] 1445 | —104!/ 4118] 108 | IL. 8,...}2 X5165, 1232 | 1617 | 1425 | —206/ 4179] 139 | IL. D...| 2 x5893| 121-8 | 1652 |- 1435 | —220| 4214) Sip | IIL. 8,...|8x5165) 1158 | 1716 | 1437 | —280) +278] 283 | IIL. D...|3x5893| 1120 | 1757] 1438 | —318 | +319] 323 | IV. 2,....4X5165| 1060 | 1816] 1438 | —378| +378] 377 | IV. D...|4x5893| 1014 | 1876} 1445 | —424|) +438) 430 | Mean 143°8 The first column contains the number of order of the spec- trum and the line to which the spectroscope was directed ; the second the approximate wave-length. In the fifth column are the means of the values of a; and aj, which cor- respond to the same line in the spectra on the two opposite sides of the grating. These means approach, as we see, to a constant value 143°8, which corresponds evidently to the normal position of the slit at the vertex of the right angle formed by the rails. On determining by direct measure- ments this position, I have found 144°8+0°1. But the difference of one millimetre between the two numbers is zn Prof. Rowland’s Coneave Gratings. 195 perfectly explained through the uncertainty in the two adjustments of the centre of curvature of the mirror on the axis of the carriage of the eyepiece, first in the direction of the girder that unites the two carriages, and secondly, in the lateral direction. Of this I have convinced myself by another series of determinations. by displacing intentionally the centre of curvature. A fault of 0°5 millim. in the deter- mination of the radius of curvature is sufficient to explain the before-mentioned difference. Thus the point 143°8 is to be considered as the vertex of the right angle of the rails, through which passes in the present oO ease the theoretic focal circle of the grating, or rather a y) eurve which differs from it very slightly. Using this number (a) I have calculated the differences d,=a,;—dy and dy=d,—d,), which are found in the table under the heading “observed.” A glance at these numbers shows that they are at least very nearly proportional to the corresponding values of nd, which implies that the angle ¢ of the segment of the true focal curve is constant. To examine this more closely, we will insert in the preceding equation of ¢ p cot ¢ = Ww i) 5) and we will calculate by the method of least squares the exact value of w trom the 16 equations of the form i, which we obtain from the preceding table on using all the values d, and dg. In this way we find the value ee wo 18261 +80. The numerically equal values of d, and d,, which are obtained on making use of this value of x, are given under d in the last column of the table. The differences between these numbers and the observed values being confined within the limits of errors of observation, it must be considered as proved that the angle € in the segment of the focal curve ts a constant. A segment of which the angle is a constant belonging necessarily to a circle, we can express the result of our re- searches as follows :— The focal curve which passes through the centre of curvature of the mirror ts a circle, which, however, has not the radius of curvature in the apex of the grating as a deameter. 196 Dr. J. R. Rydberg on a certain Asymmetry Always supposing, as in the preceding, that this curve also passes through C, we see on fig. 1 where OO, is a diameter of the true focal circle, that the angle between CO and CO, is =b=5-«, even hee tan 6= cot c= 18261". The determination of the radius of curvature has given p=6484+41 millim. According to the statement engraved on the grating, a=0:0001 inch =0:00254 millim. From this we obtain 6=24’ 47” and the are OO,=p tan 6=18261 @ =46°4 millim. The difference between the diameters CO and CO, amounts to 0°17 millim. IV. Though there could be no doubt as to the obliquity of the grating, it was possible that we had to do with some accidental anomaly peculiar to our special grating. or that reason it was of great interest for me to find an opportunity to examine another grating of the same kind, and this has been made possible through the kindness of Dr. A. H. Andersson at Kristianstad, who has been good enough to place at my disposal a concave Rowland grating of exactly the same kind as the preceding. The measurements, which have been executed in the same order as before, follow here :— > >| : Calcu- Spectral | WWave- | | Observed. lated. Seon een: ay. Ce 3 (a+ 4,) 3 ‘|— | 107m2r. | aoa 4. d I. 6,...) 1 X5165| 180°3 | 155°6 143-0 —123 | +13°0 | 116 I. D...| 15893 | 129°2 | 158:5 143°9 —134 |} +159 13:2 TO, ses | 25¢ 5165 | 118735). 16456 141°5 —243 | +220 23°2 e512 5 mV? —t. +> he where V is velocity and R is force between two molecules at distance 7 apart. According to the law of the inverse fourth power, the double sum of the internal virial reduces to an expression varying inversely as the volume and independent of the tem- perature, as I have shown before (Phil. Mag. July 1887). If we integrate Amagat’s relation 0p/dOT=/(v), we get p=SOT +o); and as in the perfect gaseous state pv= RT, where v being the volume of unit mass and T reckoned as temperature C.+ 273°, R varies inversely as the molecular weight of the substance, we will-write our equation in the form pv= RTvf(v) + vd(v), where we see that rf(v) stands for the internal virial-term. If, then, according to the law of the inverse fourth power, the internal virial varies inversely as v, then v’f(v) ought to be constant. Now Ramsay and Young have carefully tabulated the values of R/(v) and ¢(v) for different values of v in the case of ethyl oxide ; so it is easy to tabulate Rv/(v) and v’(v), as we proceed to do in the following Table, where v is the volume of a gramme of ethyl oxide in cubic centimetres, and the metre of mercury is the unit of pressure. These units will be used throughout when we are dealing with experi- mental results involving pressures ; but when necessary, for theoretical convenience, we will convert to absolute units. Tasie [.—Hthyl Oxide. v. Rof(v). | voce). || Rof(v). | v?¢(v). | | Perfect gas. "842 | 33 1°758 2413 100 ‘912 5710 |) 3 1:865 | 2366 50 ‘973 5190 2°79 2013 | 23871 20 16029 4554 2-5 2°30 2487 15 1-201 4302 2-4 2°42 yay ks) 10 1327 3908 2°3 2°56 2550 | 8 1-409 3661 2:2 2°73 2589 6 1-525 3308 2-1 2°95 2646 5 1595 3047 || ~=2:0 3°19 2691 4 1654 2656 || 1:9 3°54 2771 37 1682 | 2534 Laws of Molecular Force. 215 The critical volume of ethyl oxide is between 5 and 4; so that if Qp/OT does become variable with temperature below the critical volume, the values of Rv/(v) and v’¢(v), calcu- lated for volumes below 5, on Ramsay and Young’s assump- tion that even below the critical volume 6p/OT is independent of temperature, will be affected with an error of more or less importance ; they may therefore be regarded as a first approxi- mation only and are added for comparison. The first point to notice in these numbers is that Ruf(v) increases steadily from its limiting value *842 in the perfect gas state to double that amount near the critical volume, while at the same time v’¢(v) diminishes from its limiting value in the gaseous state to the half of it near the critical volume. This result would seem at once to contradict the law of the inverse fourth power ; but we shall see in the sequei that, in compression down to the critical region, there is a process of pairing going on among the molecules and producing this de- parture from the requirements of the law of the inverse fourth power, uncomplicated by such a process. It is to be noted that the limiting value of v’¢(v) is diffi- cult to determine experimentally, because o(v), the quantity measured, tends to the limit zero. But while below volume 4, Rzj(v) increases with increasing rapidity, v’d(v) remains almost stationary, it dips a little and then increases; but remembering that its values count only as first approxima- tions, we may assume that v’f(v) attains near the critical volume a value which remains constant in the liquid state, and is about half of the limiting value for the gaseous state. Thus there is discontinuity in the passage from the region above the critical volume to that below (or, more briefly but less accurately, during liquefaction). We must note carefully that in the range of volume from 4 to 1°9, which is a large liquid range, v°¢(v) remains constant, as it should avcording to the law of the inverse fourth power, now that the process of pairing is completed. To represent Rvf(v) I found the form R{142k/(v+k)? to be efficient ; it gives the limit 2R to the function when v=:; and as ‘842 is the known value of R, each of the above tabulated values of Ref(v) yields a value of £, the mean value 4:066 having been adopted by me. ‘The other function, v’(v), proved no less amenable to simple representation, the form found to fit it being lv/(v-+&), which attains the value lj2 when v=k ; and as the value of & is known, we can calcu- late from each tabulated value of v’d(v) a value of J, and ayain adopt the mean value 5514. Hence down to near the 216 Mr. William Sutherland on the critical volume we have the behaviour of ethyl oxide repre- sented by the simple form of equation 2k l pe Roi ony with k=4°066 an ; involving only the two constants & and J peculiar to ethyl oxide. We will now compare a few values of the pressures, in metres of mercury, given by this equation with those found by Ramsay and Young. TaBsnn Ld. | Wolwine *22 2557522 100. 50 20 10 6 175° G. {| Pressure, experiment. | 3:500 6°620 13-88 fo" ’* 1) Pressure, calculated. | 3:5388 | 6634 | 13°78 | 195° C { _ Pressure, experiment. | 3°710 7020 1506 | 23:00} 27-00 _ Pressure, calculated. 3719 | 7021 14:90 | 22:99| 27-44 280° C Pressure; experiment. |. ic.c25-0" |. 0 easan 19°80 | 34:59] 49°62 Pressure: calculated: “|* ceces-uu |) scot 19°69 | 34:28} 49-00 The agreement is as close as can be looked for; because although Ramsay and Young measure volumes to within ‘01 centim., and pressures to within 2 centim. of mercury, the quantities measured cannot be considered known with that degree of accuracy; for the discrepancies between their mea- surements and those of Perot (Ann. de Chim. et de Phys. ser. 6, t. xill.), who made special determinations in a large globe of the saturation-volume of ethyl oxide at different temperatures, are greater than those in Table Il. Accord- ingly it would be useless to seek a better empirical represen- tation of Ramsay and Young’s results than the above ; and as we are chiefly interested in establishing our simple form of characteristic equation, we had better proceed at once to the consideration of Amagat’s experiments on carbonic dioxide, practically identical with Andrews’s, but more extensive. Amagat’s unit of volume is 334, of that occupied by the gas at 0° and 1 atmosphere ; taking the weight of a litre of the gas at 0° and 1 atmosphere as 1:°9777 gramme, we can convert Amagat’s data to the gramme and centim. as units. The following Table is arranged in the same way as Table [. :— Laws of Molecular Force. 217 TasLeE I1].—Carbonic Dioxide. v. Rof(v). | v?6(v). | v. Rof(v). | v?o(v). | Perfect gas. | 1-421 | 264 | 256 | 1661 7 3A 1:92 2159 || 2:35 2-64 | 1566 (7-00) (211) | (2500) | 2:05 | 277 | 1482 | 5:14 ise 207 ||, ot 2:86 | 1440 | (5:00) (237) | (2400) || 1-76 3:02 | 1430 3°67 2°31 1858 (The bracketed numbers are introduced from Andrews.) A glance at this Table shows the same facts to be in it as m Table I. The critical volume of CO, is somewhere about 2; and we notice that near this volume Rv/(v) tends to double the value 1°421 in the gaseous state, while at the same point v’h(v) approaches a constant value about the half of what must from inspection be estimated as the upper limit of it. Both functions are accurately represented by the same forms as in the case of ethyl oxide with 4=1:762 and /=2773. With these values the following pressures were calculated for comparison with experiment :— TABLE LV.—Carbonic Dioxide. Wolumenssi2.. 11°74.) 88. | 5:87. | 3:67. | 2°64. | 2:20. 100° C Pressure, experiment. | 39 49-8 | 69 | 968 | 124 | 143 § Pressure, calculated. | 39°4 | 50-4 | 70 99 £29) 137 roo Cc Pressure, experiment. | 34:5 | 43°7 | 588 | 79:5 | 95 | 105 2 ; Pressure, calculated. | 34°38 | 44:0 | 594) 80:0 | 94 | 100 35° C Pressure, experiment. | 29°7 | 36°5 | 46°4 | 55:8 61 63°6 0 “|| Pressure, calculated. | 295 | 365 | 47:0 | 57: Sey The agreement is quite satisfactory except at the lowest volume, which is near the critical ; and I have shown (Phil. Mag. August 1887) that near the critical point in capillary tubes the relation of pressure to volume becomes fickle, the measurements of Andrews and Amagat differing from one another as much as experiment and calculation in Table IV. To illustrate this at higher volumes I introduced into Table III. a couple of Andrews’s values of Rvf(v) and v’f(v), from values of Rf(v) and ¢(v) calculated by Ramsay and Young (Phil. Mag. 1887), after conversion of Andrews’s air-manometer indications to true metres of mercury. It will be seen that Phil. Mag. 8. 5. Vol. 35. No. 214. March 18938. Q 218 Mr. William Sutherland on the Andrews makes 0p/OT a little larger than Amagat ; and this being so, it is not worth while to seek for closer agreement than that in Table LV., at least at present. We have, however, a sensitive means of determining whether the form and the values of the constants adopted truly repre- sent the behaviour of CQ, closely enough at high volumes,— namely, Thomson and Joule’s and Regnault’s experiments on the cooling of CO, when it escapes through a porous plug from under pressure (Phil. Trans. 1854-1862; dém. de? Acad. xxxvil.). Natanson (Wied. Ann. xxxi.) has repeated the Joule and Thomson experiments on CO, under the more favourable conditions afforded by the commercial sale of the fluid in large quantity and great purity, so that he has been able to measure not only the cooling effect for a given pressure excess, but also its variation with pressure. Taking all these experi- ments together, we have a delicate test for the equation at high volumes. The most convenient expression for the cooling effect for our present purpose is K donde ape aeee: where 6 is the cooling effect, K,, is the specific heat at constant pressure, and @ is temperature on the absolute thermo- dynamic scale. In previcus papers I took from Joule and Thomson’s original investigation @=T+°7°, not then aware that Sir W. Thomson, in his article “ Heat” (Hncye. Brit.), had by a fuller discussion of all the experimental data proved 6=T, and so removed the difficulty that the term *7 opposed to the harmony of the thermodynamic and molecular kinetic conceptions of temperature. With our characteristic equation the cooling effect is, after the appropriate reductions, given by dé aaa = 2(I/RT—h) +p{4(/RT—k)(/RT—2h) —2k(l/ RT — 2h) —lk/RT RT. Within Joule and Thomson’s range of pressure this can be reduced to Kea, =2(1/RT—f) ; and dé can be made to stand for the integral cooling effect if dp stands for the integral excess of 2°54 metres of mercury, to which they reduced their results, The term in p will be Laws of Molecular Force. 219 taken account of when we come to Natanson’s results. From Regnault’s data we have, in dynamical measure K,=424(:187 + 000272). TABLE V. (Cooling effect of CO, escaping through a porous plug under a pressure excess of 2°04 metres of mercury.) Wemperature ©....) 7°42.) 8°o 11991. )35°°6.| 54°, | 91°°5.| 93°°5 | 97° 5 Th. and Joule ...| 4:4 42 3°9 3:4 | 2:9 Caleculated......... 4-4 4°4 4°] 3°7 | 3:4 2-7 Path 2°6 Temperature OC. |—25°| 3°. | 100°. Repnault ......... 6:3 4-1 26 Caleulated......... 55 4:5 2°6 The agreement is as good as possible if both sets of experi- ‘ments are taken into consideration. But Natanson’s result affords a more delicate test; he found that at 20° up to 25 atmospheres the cooling effect for a pressure excess of one atmosphere could be represented by dé Fp Fe 18 +°0126 p ; while the theoretical equation above gives a) : which is practically identical with Natanson’s. On account of the closeness of this agreement we obtain as an indirect conclusion, that the experimental work on CQ, taken as a whole makes the absolute thermodynamic zero —273°, the same result as Sir W. Thomson has obtained for air and H in the article “ Heat” (dincye. Brit.), while for CQ,, using only Regnault’s coefficient of expansion and Joule and his own cooling effects, he found —273°°9. Now that CQ, is seen to be in harmony with the other two more perfect gases, the number 273 may be accepted definitely as the absolute temperature of melting ice. The equation therefore applies accurately at high volumes, a fact which we can prove by another test, seeing that Amagat carried out a special research (Compt. Rend. xciii.) to determine the ratios of pv top'v! at different temperatures and up to values of p! about 8 atmospheres, v being double v’. Q 2 220 Mr. William Sutherland on the TaBLe VI. (Values of pv/p'v' at high volumes for CO,.) (p=5'T metres of mercury : v=20') Temperature C. ...... DO: KOO: 200°. 300°. AMA AL bo doedes ee eee 1:0145 1-0087 1-0040 1:0020 Calculated: -a.-es: es. 1:0156 10092 1-0026 10000 As the experiments are not free from liability to an error of 1 in 1000, the agreement is again close enough to prove the applicability of the equation at high volumes. | In the sequel it will be shown that this equation applies to the great majority of compounds, but meanwhile the only other experimental determinations similar to those already discussed for ethyl oxide and carbonic dioxide are Amagat’s for tH), O>, No, CH, and C,H; Roth’s for SO, and NH; (Wied. Ann. xi.) ; Janssen’s for N,O (Wied. Bedi. Fes and Ramsay and Young’s on methyl and ethyl alcohol (Phil. Mag. Aug. 1887). Our form of characteristic equation applies to SO., NH;, and NO successfully, but not to H,, O., No, and CH,, which require a still simpler type, the alcohols on the other hand requiring a less simple type. These are the values of & and / for SO,, NH3, and N,O :— SO,. NHL. N,0. kk yes £208 4°8 2°3 [oe AO 22040 3420 with which the following pressures have been calculated for comparison with the experimental data, the latter being taken direct from air or nitrogen amen rats without comceae for departure from Boyle’s Taw. TABLE VII. SO, at 99°-6. NH, at 99°-6. | N,O at 25°1. | | i v. pexp. | p calc, Veta PIeXD. a wprcallies U. pexp. | p cale. 41-9 9 80 4) 172 76 76 7:0 39:1 | 37-2 17-6 i rel| 17-0 85°7 14:8 14-7 5°36 426 | 42-4 | 136 21:2 20°8 65:4 13:8 18°9 3°78 43°9 | 46-7 9:9 26:0 26°2 40-0 28:6 29:1 At 183°, At 183°. At 43°°8, 182 ) 21-7 | 22-0 | 160 103. | 10-2 5:83 ) 49:4 ) 47-9 | L6 | 198 19-6 4-62 | 556 | 544 | 409 | 421 || 347 | 614 | 610 275 | 982 | 935 | 162 | 826 54 || 282 | 641 | 643 Laws of Molecular Force. 221 This comparison has been made only to show that the form is applicable to other bodies as well as to ethyl oxide and car- bonie dioxide ; full confirmation of the form will come later on, in the study of many of its applications. 2. Establishment of the Characteristic Equation for the Gaseous Hlements, with proof of continuity during liquefaction. —tThe simplest plan in the case of the gaseous elements will be to take nitrogen as typical and tabulate for it Ref (v) and v’d(v) from Amagat’s experiments up to 320 metres of mercury. Taste VILII.—Nitrogen. \ | { v. Ruf(v). | v?o(v). Vv Rof(v). v2). | Perfect gas 2-233 me ASD 3°20 1188 | 9:22 263 | | 3°69 3°40 1007 | | 6-91 aT eT, 3°46 3°44 982 5°76 peat? fie LooOu hk one 3°80 1250 4-61 i ee a SUSRe sh | The values of v*$(v) are unsteady, because the departures from Boyle’s law are so small that ¢(v) cannot be determined with accuracy ; but it is clear enough that v*d(v) does not tend to diminish within the range of volume available, not a wide enough one, however, to convince us that there is a radical difference between the course of this function in elements and compounds. But if we adopt from this Table as it stands the only pessibie conclusion that v’7d(v) is constant, we shall be able to justify it by its consequences. In contrast to the constancy of v?p(v) is the tendency of Rvf (v) at low volumes to double its perfect gas-value. In the case of H, and O, the two functions run a similar course to that for No, but it is a more unexpected fact that they also do the same for the soup bn methane, CHy, as is shown in Table LX. TabBLe [X.—Methane. v. Rof(v). v7o(v). || v. Ro/(v). v°o(v). Perfect gas. 3908 peta 5:24 6900 32:3 4°16 | 10:09 5:43 6400 28:2 4°30 5600 || 8:07 5°95 6500 24-2 4-39 6200. 0|| 7:27 6-47 7000 20-2 4-73 6900 6-46 6°80 6800 161 4°73 3200 || 6:05 673 6200 It is evident that we have here to do with v*f(v) asa constant, 229 Mr. William Sutherland on the that is with an internal virial varying inversely as the volume down to near the critical volume, and Rv/{v) tending some- where near that point to about double its value in the perfect gas state. The course of Rvf(v) in these four gases is repre- sented by the simple form nied (8) which attains the value 2R when v=k. Hence the charac- teristic equation down to v=; is 2 Peer 2 2 / a form which I had already adopted for air (Phil. Mag. Aug. 1887). The following are the values for & and 1 :— H. N.. O.. CH,. AGh geoe Heong > 20) 2°64 1°78 Dol 2°47[2°11] Die A100" Ao So 6460 1110[ 910] The values given in brackets for air are those previously found by me from Amagat’s data (Compt. Rend. xcix.), but as these data are not carried to such high pressures as those for N, and O,, I have calculated values for air by adding to four fifths of the values for N, one fifth of the values for Oy». This equation is almost identical with that of Van der Waals, but it is a little simpler. It gives the following pres- sures for comparison with Amagat’s experimental results :— l ” TABLE X. Hydrogen. Nitrogen. Oxygen. Atl7-7° C. PD IUCN = Oh At 14-727G: v pexp.| peale.| ». pexp. | p cale. v. p exp. | p cale. 166-9 575 56-9 || 13-83 46 45°7 5°73 88°9 89°7 100-1 99 99 6-91 92 91 3°58 | 141 142 60-1 | 176 176— || «461 145 142 2:58 | 201 203 46°7 | 238 241 | 3869 194 188 2°43 | 216 219 | 323 223 226 At 100° C. At 100 C. At 100° C. 1669 14-2 73°3 || 13°83 60 60°5 |} 5°73 123 124 100-1 -).129 123.) 1) OOL 125 124 3°58 204 204 60:1 | 230 229 4°61 200 199 2°58-| 300 301 AG fan ies lal 31 Lat | eS) 270 266 2°43 322 327 | 3-23 320 323 Laws of Molecular Force. 225 The experimental numbers for oxygen are taken from Amagat’s data-in the Comptes Rendus, xci. The most delicate test we can apply to our form at high volumes is, in the case of air, to compare the calculated with the experimental Thomson and Joule cooling effect. When I did this with the previous equation for air (e— 2b and {=910), 1 assumed the difference :7° to exist between the melting-point of ice on the thermodynamic and gas ther- mometers ; but, as already pointed out, Sir W. Thomson having proved this difference not to exist, there must have been a compensation of errors in the application of the previous equation. Thomson’s expression for the cooling effect, applied to our equation for air, becomes K,d8/dp = 21/RT—k/2, which gives the following calculated values :— Cooling effects of air escaping through a porous plug into the atmosphere under a pressure excess of 2°04 metres of mercury. | Pemiperature C............. (alls ae 3976. 92°'8. Experiment . . . °88 "86 Ue “oil: Calenlation= {9 2. 2°84 80 ‘ali “5D The agreement is the closest to be looked for and proves the accuracy of our equation for air at high volumes. At low volumes we can test the form for all the elementar y gases and CH, by applying it to the calculation of the critical volume, pressure, and temperature in each case. To do this at the present stage we must assume that our form can be trusted to hold not only to the critical volume but also a little past into the liquid region, a legitimate assumption for the elements, where we have seen the internal virial varying inversely as the volume, and so giving a guarantee of con- tinuity, but not legitimate for the compounds where dis- continuity occurs. Then, applying James Thomson’s idea of the passage from the gaseous to the liquid state, as pre- cisionized by Maxwell and Clausius, we have the critical point determined by the conditions Qp/Ov=0, 0?p/dv?=0 Along with the characteristic equation tees lead to the fol- ‘ih ring values:—critical volume ve= = 38k/2; critical temperature = = 161/27Rk; critical pressure p.= Al/27 12 ,---to compare with os experimental values found by Olszewski for O, and Ny (Compt. Rend. ¢.), by Wroblewski fer air, and by Dewar for CH, (Phil. Mag. 1884, xviii.). 224 Mr. William Sutherland on the TaBLe XI. | | H,,. N.. Ox CH,. | Air. | Critical { EXPO: kl ay eee 34 2°5 Wielumme.: {(\cal. sis] -wceeae 3°96 267 Critical EXperere | Geis. —146 | —119 | —995 —140 Temperature. {cale......) —229 —155 | —127 | —99 —149 Critical Sie dee 27 38 37 30 Pressure. Gales Les 25 40 | 32 | 27 The agreement is all that can be looked for in view of the difficulties of measuring these low critical temperatures and their associated pressures. With regard to hydrogen all we know is that Olszewski (Compt. Itend. ci.) has submitted it to a temperature estimated by him as —220° without a sign of liquefaction. If our equation is to be trusted, it would indi- cate that he would need to go some 10 degrees lower before the only unliquefied gas is conquered. Wroblewski has pub- lished data on the compressibility of 11, up to pressures of 70 atmospheres at temperatures of —103° and —182° (Journ. Chem. Soc. 1889), and with these our equation is in accord, but there is hardly need of tabulated proof. 3. Brief discussion of exceptional Compounds such as the Alcohols and Ethylene.—To complete our survey of the ex- perimental materia! on bodies above the critical region we have to consider Ramsay and Young’s observations on methyl and ethyl alcohol, and Amagat’s on ethylene. Ramsay and Young point out that at low volumes the values of Op/OT for the alcohols are not so reliable as for ethyl oxide, being deter- mined froma smaller temperature range ; hence our values of Ref (v) and v*f(vr) are not so reliable as before, but they suffice to show the exceptional nature of these bodies. Taste X1I.—Methyl Alcohol. | v. Ref(v). | v?d(v). OF | Rof(v). | 0d(2). —————— ee | eo. a’ ee | Perfect gas. | 1-950 25 3°50 24800 340 2-14 20 3:70 23060 40 2-32 45500 18 3-79 22000 20 2-40 48000 | 16 3:97 21700 i 2-46 46109 | 14 4-18 20900 135 2-56 43700 | 12 4-38 19900 100 2-70 41000 | 11 4-46 19600 70 3-04 42100 | 10 4-53 179v0 50 3:10 33500 | 9 4°58 16700 | 40 3:20 30200 | 8 4-5 15000 30 S37 26800 | 7 4:39 12900 Laws of Moleculur Force. . 225 Table XII. (continued) —Hthyl Alcohol. | v. Rof(v). | v?¢(v). v. Ref(v). | v?o(v). | Perfect gas. 1:35 8 343 11300 ee LOS 2 | 165 | 18000 6 334 8600 53-4 1°83 | 15000 4 3°37 6200 30 2°16 15000 3 ddl 5000 2671 \* isk 16000 | 2-4 3°93 4600 18-2 | 2:83 | 17000 2 4:87 4700 12 | 332 15000 18 5°83 4900 | 10 | 341 | 13500 16 7-06 4900 9 _ 3843 12500 1-4 881 4700 The numbers for methyl alcohol do not extend as far as the critical volume, while those for ethyl alcohol go considerably beyond it, lying as it does between 3 and 4; but we notice in both cases that Rv/(v) increases from the limiting gaseous value, but attains a practically constant value before the critical yolume is reached. In ethyl alcohol we may say that the value 3:4 is retained from volume 10 to volume 3, and moreover this 3°4 is not now double the initial 1°35, but about 2°5 times it. In methyl alcohol the value 4°5 may be said to be retained constant from volume 11 to 7, the lowest on the table ; so that it is probable that, as in the case of ethyl alcohol, this value will be retained down to the critical volume: here again, also, the 45 is more than double the initial 1-95, but is only 2°3, not 2°5, times it. Note that, in ethyl] alcohol, as soon as the critical volume is passed Rv/(v) begins again to increase rapidly, just as happened in the case of ethyl oxide. But for our present purpose more interest attaches to the course of v*p(v). In methyl alcohol at high volumes it seems to approach a limit which we may assign as 45,000, and then at volume 16, where Rvf(v) has risen to double its initial value, v*d(v) has fallen to almost half of 46,000, but as Rv/(v) continues to rise v?(v) continues to fall, and still continues to do so even when Rof(v) has become constant. In methyl alcohol we cannot follow the changes right down to the critical volume, but in ethyl alcohol we see that v*f(v) attains at the critical volume a value which is carried constant into the liquid state, this constant value being about one quarter of the apparent limiting value 20,000 at large volumes. The constancy of v°f(v) below the critical volume is in striking contrast to the rapid variation of Rvf(v). I have not sought to represent by formulas the course of the two functions for the alcohols, as I have doubts about 226 Mr. William Sutherland on the 0p/OT being independent of temperature in the case of the aleohols ; if it is variable then the values of our functions are affected with error. In any case we have seen that above the critical region the alcohols behave differently from our two typical compounds, ethyl oxide and carbonic dioxide ; in section 14 it will be seen that in the liquid region, on the other hand, the alcohols approach the regular compounds in many respects, but are still exceptional in others. There remains now only ethylene to consider as to its gaseous behaviour. Taste XIII].—Hthylene. v. Ruf(v). | v?9(v). | v, Ruf(v). | v?o(v). Perfect gas. | 2°22 4-61 4°15 4500 20°75 Ze 5800 415 4:45 4500 16°14 2°78 5320 3 69 4°81 4400 11°53 3°07 5500 322 571 4700 9-23 3°24 5300 | ATT 6-41 4400 6°92 3:58 5100 | 2°65 6°63 4200 576 3°83 4900 | 2°54 787 5000 According to Cailletet and Mathias (Compt. Rend. cii.), the critical volume of ethylene is about 4°5 ; so that again in the above table we see Rv/(v) near the critical volume attaining double its initial value and increasing rapidly thereafter. Once more, too, we see v’d(v) attaining near the critical volume a value which it retains constant below; but ethylene is excep- tional in that this value is not half the limit at high volumes. The facts in the above table may be summarized in the state- ments that Rvf(v) may be represented by the form R(1+4/v), and v’d(v) by the form vl/(v+a); so that the characteristic equation for ethylene is k l oes A a Fe with k=4°15, a=1°64, and 1=6270. The form for ethylene is intermediate in simplicity between that for the simple gases and that for compounds, except that it has an extra constant. It is also worth noting that the forms 5 | (5) k/v, and 2k/(v+h) are special cases of a general form nk/{v+(n—1)k}, with n=34, 1, and 2. Laws of Molecular Force. 227 A. Establishment of Characteristic Equation below the region of the Critical Volume.—Now that we have practically exhausted the available data of the gaseous state, we see that by themselves they do not give much scope for generalization ; but if we can secure an equation applicable from the critical volume down to the volumes of liquids in the ordinary state, then, with two equations covering almost the whole range of fluidity, we shall have a much larger experimental area laid under contribution for information on the characters of mole- cules. Already we have secured one important fact towards the acquisition of such an equation, namely that below the critical volume the internal virial term varies inversely as the volume ; and in the case of ethyl oxide we know its actual amount /2v with /=5514. We have therefore only to add to 1/2» Ramsay and Young’s values of pv at different temperatures for different volumes below the critical, and we obtain the values of the kinetic-energy term in the desired equation ; we can then proceed to study how this quantity depends on temperature and volume, and express the resulting conclusions in a formula. As to the form we have this clue, that it must join on con- tinuously with the previous one where that ceases to be appli- cable. Now the first fact to notice is that our form for compounds above the critical region cannot, like that for the elements, give a critical point by itself at all; for given p and JT it is not a cubic but a quadratic in v, and hence cannot give us the three equal roots which are adopted as charac- teristic of the critical point when we apply the conditions Op/dv =0, d2p/9v? = 0. This emphasizes the discontinuity in compounds as contrasted with elements. However, we know as an experimental fact that at the critical point 0p/dQv=0, which with the charac- teristic equation gives us only two relations between the critical temperature, pressure, and volume. As a third relation that would perfectly define these three quantities I was led to believe that the critical volume is proportional to k, and found cat critical volume v,=7k/6 is the relation which, with the two others, gives successfully the numerics of the critical state in agreement with ex- periment. As this will be proved subsequently (Section 10) for a large number of substances, I will not delay at present to give examples, except for those compounds for which we have already found k and J, 228 Mr. William Sutherland on the Taste XIY. Critical temperature, T,=120//409 R& ; critical pressure, p =86 1/409 FP’. (C,H,),0. | CO,. | “SO, Seas eee: Critical experon...| Wot 32 155 130 35 Temperature. | cale....... 199 52 | e125 96 36 Critical expetye| 20d. 800 60 87 57 Pressure. cale....... 293 | 786 56 84 57 The want of accuracy in the agreement in parts of this table is to be ascribed partly to inaccuracy in the ordinary determinations of the critical point, as I have already pointed out that capillary action must sometimes largely affect the numerics of the critical state when these are determined in capillary tubes (Phil. Mag. August 1887). Regnault, in his account of his experiments on the saturation-pressures of CO,, expressly declares that be had liquid CO, at 42°, which is 10° above the apparent critical temperature in capillary tubes ; and Cailletet and Colardeau (Compt. Rend. cviii.) have shown that although the meniscus between gas and liquid CO, disappears to the eye about 31° or 32°, yet cha- racteristic differences between liquid and gas can be proved to exist several degrees higher than this. Hence an error of at least 10° is possible in ordinary determinations of critical temperatures. On the other hand, an error of 5 per cent. in the value of an absolute temperature of about 40U° as given by our equation would amount to 20°. Table XIV. is to be taken in the light of these facts. We have now ascertained a second property that our equation for volumes below the critical is to possess : it must begin to apply when v=7k/6, as the other form cannot apply below this volume at the critical temperature. At this volume the kinetic-energy term in our form above the critical region becomes BC +12/13),- or 25RT/13- so that 25R/13 is the lower limit of the term which in the new equation is to take the same place as Rvf(v) hitherto. Hence for this term the form 25R(1+F(v))/18 naturally suggests itself, and as F(v) is to vanish when v=7k/6, we get (7k/6—v) /(v) as a suggestion for its form ; and it only 1emains from the data obtained, as I have said, by Laws of Molecular Force. 229 adding //2v to Ramsay and Young’s values of pu for voluines of ethyl oxide below &, to determine the form of the function W(v). This was found, after a rather tedious search, to come out in the simple form VT(v—£)/B ; so that finally we have the following as the equation for ethyl oxide below the volume kf: with the following values for oe Liane : fe 2 n/t eo. boob B= lh, R, k, and / as before. I propose to call this the infracritical equation. It is to be noticed that we have introduced only two additional constants ; so that, as regards number of constants, we could hardly look for a simpler form. Above the volume 7k/6 the appropriate form was proved to be 2k ae ees which I propose to call the supracritical equation. Between & and 7k/6 we have the circacritical form a/R ye les was ‘y—B otk This, then, gives the complete representation of ethyl oxide in the fluid state if we establish the sufficiency of the infra- critical form, as we now proceed to do. In the next table are compared the pressures found by Ramsay and Young and those given by the equation. py= RIT (14+ Taste XV.—Liquid Hthyl Oxide. aVolurnel. sce Reece 3-7. 2-75, | 2:25. 2. 16g - Eee! exper. .| 28 Boo 43 | ae c.f Tea tet ae 26 45 | - IPTESSUPey ex peters ee wanccnes || ace 19 43 oC: { sy: | as CHLOR Re Uc ate.6 | km seians 14 48 A IPMESSUPO,EXDGL hs tmaee Bik Rcvess fo) Rescues |! Seseue 19°5 ae SO able ie aade | SA aeost | Gige doe. 4 [hs Ree 20 230 Mr. William Sutherland on the For the proper appreciation of this table it must be borne in mind that as soon as we enter the liquid region the pv term of the characteristic equation becomes the small difference of two terms, a small percentage error in either of which becomes a large one in pv. The fact that the above table brings out is that from 150° to 195° the relation between volume and temperature given by the equation is so accurate as to make only the small errors in pressure in the above table. But to show this more directly, we will now compare the volumes of the liquid under a pressure of 9 metres of mercury between O° and 100°, as determined by Grimaldi (Wied. Bezbl. x.) and as given by the equation. The specific gravity of ethyl oxide at 0° and under one atmosphere is taken as °7366. Taste XVI. (p=19°5 metre.) Temperature ......... 0°. 50°. 100°. 150°. Volume, experiment......... 1355 1-469 1-630 19 ee eplewlated ss.g.42-:| 1 obe 1-467 1 6383 1-9 This, taken in conjunction with Table XV., shows that the equation represents with a high degree of accuracy the ex- pansion of liquid ethyl oxide right up to the critical volume. It is now to be tested as to its power to give compressibilities correctly. The next Table contains the calculated compressi- bilities of liquid ethyl oxide, and also the experimental as given by Amagat (Ann. de Chim. et de Phys. 5 sér. t. xi.), Avenarius (Wied. Seidl. 11.), and Grimaldi (Wied. Berdl. x.). Amagat’s values bad to be interpolated for comparison with the others. TaBLE XVII. Compressibilities with metre of mercury as pressure-unit. Temperature ......... oe 40°. 60°. 100°. Menaedios feos. oh: 000200 | 000309 | -v00380 | -000730 AGRE Te ene 000178 | -000817 | -000403 | -000654 Grin as 00207 | -000316 | -00e407 | -000682 at, eee 000183 | -0003G0 | -000392 | -000710 Laws of Molecular Force. Dek The agreement here is again satisfactory, and we have now seen that our form, with only two constants in addition to those characteristic of the gaseous state, can give both the expansion and compression of the liquid at low pressures ; but Amagat has measured these also at high pressures up to 2000 and 3000 atmos. (Compt. Rend. cil. and ev.), and the following Table compares first his values of the mean co- efficient of expansion between 0° and 50° at pressures from 76 up to 2280 metres with those given by the equation, and, second, his values of the mean compressibility at 17°4 and at pressures up to 1500 metres with those given by the equation. If v, and v, are the volumes at p, and po, then the mean com- pressibility is taken as (vj—v)/v,\(p2—p1). The apparent compressibilities given by Amagat are converted to true values by adding 000002, which he has since given as the com- pressibility of glass. TABLE XVIII. Mean Coefficient of Expansion at high pressures. pinmetres... ‘76. 380. 760. 1140. 1520. 1900. 2280. PATNAGAG oe ieee 0s 00170 +-00112 -00091 ‘00077 -00070 -00063 -00056 Hquation™:.:...... 700170 ‘00101 ‘00076 00066 -00056 -00050 -00047 Mean Compressibilities at high pressures. pin metres ... 76 to 114 to 866 to 654 to 933 to 1218 to 1500 | | | | | | Amagat ........0. ‘000208 -000143 -000112 -000086 -000070 -000062 Equation ......... 000197 -000128 -000085 -000060 -000046 -000037 As regards expansion the equation goes fairly near to the truth ; except at the lowest pressures, it gives coefficients somewhat smaller than the experimental, but it parallels closely the main phenomenon of the rapid diminution of the coefficient with rising pressure. But in the compressibilities there is an increasing divergence between experiment and equation with increasing pressure, although again the equation is true to the main fact of the rapid diminution of compres- sibility with increasing pressure. We may conclude from the last table that our equation holds within the limits of experi- mental accuracy up to 760 metres ; beyond that it begins to fail. A simple empirical modification would adapt the form to the whole of Amagat’s range, but as it stands it will be found good enough for our applications. We will now consider briefly how this form applies to car- bonic dioxide below the critical volume ; and the comparison 232 Mr. William Sutherland on the is interesting, as it relates to temperatures both above and below the critical. The values of the constants are B=54, TABLE XIX. Carbonic Dioxide below critical volume. V olumie nce. ye ees 1526; 23) | 1220s: 1-105: 1-027. Ei ° Pressure, ne 150 274 cy i 0.4 Wie lei 24 qipns266 or Pressure, exp....... 69 126 187 320 35° 0. { eh ag ae 120 184 320 180 G, { Pressure, exp...) cece | teens 99 200 5 -of CC A RR (am ere o7 208 | | The agreement is within the limit of experimental error at the high pressures. Cailletet and Mathias have determined (Compt. Rend. cii.) the density of liquid CO, at various tem- peratures under the pressure of saturation. Here is a com- parison with a couple of their results :— Temperature. . . —34°. | G2: Volume—Cailletet and Mathias . °946 1:087 ait SellQUAtiON Seka ae tli: sn eee 1:086 As far as compound gases are concerned, the applicability of the form for volumes below the critical has now been de- monstrated in two typical cases. The elementary gases have now to be considered as to their behaviour below the critical volume. The data are again those furnished by Amagat (Compt. Rend. evii. and Phil. Mag. Dec. 1888) on the com- pressibility of these gases between 760 and 2280 metres of mercury. Our study of these bodies above the critical volume has given us the knowledge that the internal virial term below k must be J/v, and the kinetic-energy term at the critical volume is 38RT/2, and with these guides the complete form required is soon found from the experimental numbers. It is 3k—~v y po = §RT(140% — C— with the following values for the additional constants B and b :— k. B. b. Enya rocen. tlh 2. ok? 43 "480 Nitrogen. =s = 2°64. “81 "420 Oxyoen OL eS “604 "4415 Methane .. . [5°51] EP59] > ee ~ Laws of Molecular Force. 233 The approximate equality of the values of the constant b is worth noting. I have also reproduced here the values of k at the side of those for @, in order to point out that @ is nearly k/3 in each case. Amagat has not published data for methane at volumes below the critical region, but the numbers given in brackets for methane were obtained indirectly as explained below. These relations of 8 and 0 give our equation such a degree of simplicity as largely to establish the soundness of its form. The next Table shows the degree of accuracy with which it represents the experimental facts. TABLE X X.—Oxygen at high pressures. MHOUUTIIG: “J cekceste esses 1277. | 1:097. | 1-008. 949, ‘905. | 150 ¢, { Prossure, exp....... 760 | 1140 | 1520 | 1900 | 2280 : eee 79 | lia | sipia | 1363") 2096 The agreement is quite as good for hydrogen and nitrogen. By means of this equation we can calculate the volumes of -a gramme of liquid nitrogen and oxygen at their boiling- points under a pressure of *76 metre, for comparison with Wroblewski and Olszewski’s determinations of the same (Compt. Rend. cii.; Wied. Bebl. x.; and ‘ Nature,’ April 1887). Oxygen. Nitrogen. ates Wroblewski. . °85 1:20 eae Olszewski . . °89 at — 108 Meuation:... (7; 20 1:26 The equation is seen to give the volumes of these two bodies at these low temperatures within the present limits of experi- mental accuracy, and accordingly it covers a range of 2000- metres pressure and almost the whole experimental range of temperature. In the case of methane, if we take Olszewski’s value 2°41 for its volume at —164°, and assume 0 is the mean of 6 for H,, Nz, and Oy, then we can calculate the value of 6 which is tabulated above. To ethylene above the critical region we had to assign a special form intermediate between that for ordinary compounds and that for elements ; so that we had better do likewise for its infracritical equation, which I have cast in the form Ty Ay l k Phil. Mag. 8. 5. Vol. 35. No. 214. March 1893. R 934. Mr. William Sutherland on the with B=56:5, 8=1°53. For the elements we had v,=dk/2, for ordinary compounds v,=7k/6 ; so that to make ethylene intermediate v, is taken as 5k/4, all these being of the general form (1+2n)/2n, with n=1, 2, 3. With the values of the constants B and 6 given above as derived from Amagat’s results at high pressures, we can determine the density of liquid ethylene; at —21° under saturation-pressure the density is ‘414, identical with the experimental value of Cailletet and Mathias (Compt. Rend. cli.). It will be as well at this stage to extract clear from among the argumentative detail the most important results so far obtained. First, in the elements the internal virial varies inversely as the volume over the whole experimental range. Second, in compounds there is mathematical discontinuity in the value of the internal virial at volume & ; from volume k& downwards the internal virial varies inversely as the volume : from the volume & upwards it tends towards variation inversely as the volume as the limiting law, the limiting constant being double that which holds below the volume & ; between the two limiting cases the internal virial of compounds varies inversely as (v+h). Third, a fact of the highest importance in connexion with the kinetic-energy or temperature term in the equation arrests our attention, namely, that the coefficient of T in it, or the apparent rate of variation of the translatory kinetic energy with temperature at constant volume, attains near the critical volume double its value in the gaseous state, and below the critical region increases rapidly with diminishing volume (see column Rvf(v) in Table I.), becoming at ordinary liquid volumes as much as ten times as large (see coefficient of 'T in infracritical equation). Now the specific heat of liquids at constant volume, which is the rate of variation of the total energy with temperature, is rarely much more than twice that for their vapours. Hence we must seriously consider the interpretation to be put on the different terms of our equations. 5. A short digression on the general interpretation of Clausius’s Equation of the Virial.—Returning to Clausius’s theorem of the virial, 2 pe = %gmV?—F.3 >> Ry, we see that strictly the kinetic-energy term includes not only the energy of the motion of the molecules as wholes, but also that of the motion of their parts, and at the same time the ~ Labs of Molecular Force. 235 internal virial includes the actions between the parts of the molecules as well as those between the molecules. Calling these actions the chemic force, we can write the theorem thus: 3 pv = the total kinetic energy—chemic virial—virial of molecular forces. Now in the usual treatment of the equation it is assumed that the chemic virial is equal to that part of the total kinetic energy which is due to the motion of the parts of the mole- cules relatively to their centres of mass, and neutralizes it in our equation, reducing it to 3 pv = translatory kinetic energy of molecules as wholes —virial of molecular forces. But if we retain the full equation, and assume that the virial term we have been finding for various bodies is the true virial of the molecular forces, and includes none of the chemice virial, then the term usually regarded as the translatory kinetic energy of the molecules as wholes is really the total kinetic energy minus the chemic virial. Let E be the total kinetic energy of unit mass, V the virial of the chemic forces, and P their potential energy ; then, above the critical volume, and +h which in the limiting gaseous state becomes 3R/2. Also 0 or the specific heat at constant volume. Below the critical volume, 9 eee VT ki—v E V=§R'T(1+ 4 =e) S(E-V)=gR (1+ =) API) IK 0 AY == Supy 9 Aa il ki —-y and, again, | 0 (H— —P)'=K.. R 2 or 236 Mr. William Sutherland on the Now we can calculate K, from the experimental values of K, by the relation Let us then make a comparison in the case of ethyl oxide, using E. Wiedemann’s value “3725 for K, for the vapour at 0°, and Regnault’s value ‘529 for the liquid at 0°; then, con- verting to ergs per degree C., we get Vapour at 0°. Liquid at 0°. fe) ree : 16 Fe 6 sq) = - I-65 5ca0 15°3 x 10°, Sauce S. (E—P) = 144 x10® 17-9 108, Thus we see that while in the liquid 6(H—V)/OT is nearly equal to O(E—P)/OT, there is a great difference in the vapour : 0(V—P)/d9T=12'7 for the vapour and only 2°6 for the liquid. Or, while K, is nearly the same in the two states, 6(H—V)/oT has in the liquid state increased to nine times its value in the vaporous. We have here, therefore, an interesting opening into the regions of chemic force ; but meanwhile we must restrict ourselves to the question of molecular force at present in hand, calling attention, however, to the fact that our energy term in its two forms for elements and its two forms for com- pounds is well worthy of the closest study. It summarizes a lot of information about the internal dynamics of molecules— perhaps about the relations of matter and ether; but these would need to be extracted by a special research on the term and its relation to our experimental knowledge of specific heat. It is worth mentioning here that Clausius’s equation of the virial, as usually applied to molecular physics, takes no account of the mutual action of matter and ether—an action which we know must exist, from the radiation of heat by gases as well as by liquids and solids. According to ordinary views of the eether this may be neglected, on account of the smallness of the mass and of the specific heat of the ether; but it is well to remember that we are neglecting it. 6. Consideration of Van der Waals’s generalization.—We are now in a position to consider how far Van der Waals’s generalization holds, namely :—If the volume, pressure, and temperature are measured for each substance in terms of the critical values as units, then one and the same aw holds for all substances. Laws of Molecular Force. Dad In the first place, we see from what has gone before that the same law cannot apply to both elements and compounds, nor can the alcohols and water follow the same law as regular compounds. “s In the case of the elements and methane we have the critical volume, pressure, and temperature given in terms of R, J, and k by three relations (see end of Section 2), 4 f 16 J v= 8k/2, Pe= 97 re T= 57 Rk Whence, in the supracritical equation replacing R, J, and & by their values in terms of v,, p,, T,, we get po 18 ee 1 nee 3 which shows that when the critical values are made the units in the measurements of the variables, one and the same law holds for the elements above the critical volume. Below the critical volume we have We have seen that 6 is nearly the same for these bodies and that 8/v, is approximately constant, so that below the critical volume the elements and methane all follow approximately the same law. In the case of compounds, we have (see Section 4, at the beginning) | 36 1 120 1 M= THC, P= 409 ~°= 409 BP with which, eliminating R,’, and / from the supracritical equation, we get —+1 foe wal) Ab 2 409 1 pe rob s/o ai ePbsot st ( U ) 6 v Prose le ee Hence, above the critical volume the compounds follow the same law among themselves. In the same way, below the critical volume we get for compounds :— 238 Mr. William Sutherland on the 7 es po 20 2 Ti Vt se age es Bu BR One and the same law holds for compounds below the eritical volume only if B varies as the square root of the critical temperature, and if 8 is proportional to the critical volume : in the elements we have found the latter condition to hold approximately, and so we are prepared to find it do so for compounds. The following Table compares B with /T, and 8 with k, which is 6v,/7 for the five compounds for which we haveas yet found &. The values of B and 8 for NH; and N.O were obtained from Andréeff’s data for the expansion of these bodies as liquids (Ann. Chem. Pharm. ex.) and for SO, from Jouk’s (Wied. Bezbl. vi.). TABLE X XI. | | he. | B. k/p. | B. | B/N Te. (CAPO 4066 | 111 | 37 | \@sqgiaess OO, 20 ce 176 | -69.| 40 | 54 7p SOe NS cat, ai 208 | ‘55 38. | 36 INET Schen Ms 4-8 1:22 | 39 70 36 NEOR Sate Lage 2:3 66 | 35 55 31 In these bodies we find a fair approximation to propor- tionality between @ and & on the one hand, and between B and /T, on the other; to the same degree of approxi- mation Van der Waals’s generalization can be applied to compounds below the critical volume (excluding of course such exceptional bodies as the-alcohols and water). The accurate statement of the generalization ought then to be as follows :—When the variables are expressed in terms of their critical values as units, then down to the critical point compound bodies with certain exceptions have all one and the same characteristic equation, but below the critical point they have closely similar but not identical equations, - It is a remarkable tact that Van der Waals should have been led to his valuable generalization by means of a form of equation which completely fails to apply to the substances which are the subject of the generalization. Asa point in the history of this branch of molecular physics, it calls for mention that Waterston, in the Phil. Mag. vol. xxxv. (1868), had prac- Laws of Molecular Force. 239 tically discovered the generalization, and expressed it in its most striking aspects by means of several diagrams for a number of bodies ; but the verbal expression of his results was so unsystematic, and withal so crabbed, that his work has been overlooked. 3 | There is one typical application of the generalization which’ is of special importance—to the relation between pressure and temperature of saturation. If with the aid of our equations we trace the complete isothermals for temperatures below the critical, we shall get curves with the James Thomson double- bend as shown in Ramsay and Young’s isothermals for ether (Phil. Mag. May 1887). According to Maxwell’s thermodynamical deduction, the pressure of saturation at a given temperature is that cor- responding to the line of constant pressure which cuts off equal areas in the two bends, a result which Ramsay and Young verified by actual measurement on their curves. Let v3 and v, be the volumes of saturated vapour and liquid at pressure P and temperature T; then Maxwell’s principle gives us that the pressure of saturation is defined by the three equations :— P(m—a)= | pate 2k l Py, = RI(1+— 5 Tose VT Lk—v ae, = 25 gees f LB) | ee Pu, = #RT(1+-4, — aa v3 is given in terms of P and T by a quadratic, and can therefore be eliminated from the integral when evaluated ; v, is given by a cubic, but as Pv, can for practical purposes be put 0, a very close approximation to v, can be obtained also from a quadratic. The resulting relation between P and T, which is the law of saturation, involves the constants R, &, J, B, and £. The actual evaluation of the integral would of course proceed in three stages, corresponding to the supra-, circa-, and infracritical equations. The law of the integral in the first stage from v3 to 7k/6, with critical values of the variables as units, would be the same for all compounds ; and we have seen that the integral in the other two stages will follow approximately the same lawin all cases. Hence if saturation pressures and temperatures are expressed in terms of the critical values, the law of their relation will be approximately the same for all regular compounds. If this were an absolutely accurate relation, the best means 240. Mr. William Sutherland on the of testing it would be to take Regnault’s formula, with one exponential term, | loot — atba*, and by a simple recalculation from his values for a, b, and «, to cast it in the form T/Te log p/p, = et+dy"”, proving that the constants e, d, and y are approximately the same for all compounds. But the objection to this plan soon becomes obvious on trial, as the formula owes its empirical convenience to tLe power of adjustment amongst the con- stants ; and the same difficulty would be experienced with any purely empirical equation. Accordingly, to test this matter, I have thought it best to compare the pressures of a number of bodies at temperatures which are constant fractions of their critical temperatures, such as ‘6T,,°7'T,, and so on. The ratio of the pressure of any substance to the corresponding pressure of ethyl oxide ought to be approximately the same for that substance at all values of the fraction. Great uncertainty attends the mea- surement of critical pressures: an error of 20° in the critical temperature is not a large fraction of its value measured from absolute zero, but it makes a large difference in a saturation- pressure, and the critical pressure is the limiting saturation- pressure. In the subjoined Table the critical-pressure ratios are given for what they are worth in the column T.,. TABLE XXII. Ratios of Saturation-Pressures at constant fractions of the critical temperature to the Saturation-Pressures of Ethy] Oxide at the same fractions of its critical temperature. | Fractions of Te. Te. 6. 65. otk ‘75. "3. OD: HilaasO: ACEEONE J24ec0-- 0° 506 ‘OF | "90) | 0272 04s tenes 1-4 Methy] oxide...... 404 | 1°7 15 14 14 SOs aeree are: ADS AN 7 i ale ar hes, 17 Li, sen jigileeee ENDED go eee esotes cok 404 | 26 | 26 | 25 | 2:5. >| "2: sila ee LS Sheer ets aes 373 —- | oO | 32141928 Bee sop 2°6 CON: poet. dhe 5 305 se be v3. at LSet) eae NSO eet bucesseace 308 = fe: 5a sae 2°44) 1B ee eat OS casedaunaeoh sedans: Ow ole 2. || Dd. alee = epee f° (0) OVS caacmaaace DOO Oe RIES LM, cS! 1 aleD sep 16 CHOIR Breve 5387 | 16 5s) | el 1-4 1-3 16 C15 E01 |: aan ADA a lelenal Gago p | vile 815 Mea ax 2:1 (ORE (3 ©) ranean a 456 | 1-4 1-4 lies} [2 Slab 1-5 Ca OB Tas. cczscase DOO a apd Oa iateS eae lG APalcs 1-4 BenzeneO, Hi, ...). 7060 4) Adele 12 | a2 Lat 1-4 Laws of Molecular Force. 241 This table makes it clear enough that, in applying Van der Waals’s generalization below the critical volume, we have to do with a first approximation only. The curves for all these diverse bodies excepting CS., while not identical, would form a compact bundle about a mean curve from which each body would have its own characteristic departure ; and this is just what our study of B and 8 in Table XXI. should lead us to expect. 7. Five Methods of finding the Virial Constant.—The first method is that which we have already exhausted, namely, by means of extended enough observations of the compression and expansion of bodies in the gaseous state. Second method : to obtain the virial constant / from one measure of the compressibility and of the expansibility at the same temperature of the body as a liquid. Writing our infracritical equation thus, RT JT eae) _ l at) (1+ B 'v—B/ Qv?’ op __ BR 38R VT Bed bP Ry 3p Aw. 2 B.t7=6 2 2eE oe OT But at ordinary low pressures the term p/T is a negligible part of this expression, and we can write Oia 6 pide OT 4° wT QW Now Op _ ov /dv_ _m dT _% or Oo Open 4 loo oO where a and w are the coefficients of expansion and the com- pressibility at T as usually defined. 81 _ R_wa, Ae Do aie 4. a 1= 5 (wo+$R) of = 5 (wo +39R Jo. In addition to giving usa value of J, this last equation gives a test as to whether the equation applies to a body or not, as the expression on the right-hand side is to be constant at all temperatures if ~ is measured at low pressures. But on | | O,H,, (Grimaldi)...! 8520 | ————q“— —— ——— Se ——___ 242 Mr. William Sutherland on the account of the experimental difficulties hitherto met with in the measurement of w, the equation gives no very delicate test, although it might with the improvements in accuracy made within the last few years. In addition to ethyl oxide, the two substances for which we have measurements of both a and p over the widest range of temperature are ethyl chloride, studied as to expansion by Drion and as to compression by Amagat, who has corrected Drion’s coefficients of expansion for change of pressure, and pentane, studied by Amagat and Grimaldi. The following are the values of / calculated from the data at different temperatures for these two substances, with the megadyne taken as unit of force. Temperature C..../ 0°. | 11°. | 139, 60°; / Bee: | | ee ed | 7450 | 7230 | 8000 | 8300 | 9250 | Cli GAmagat)...)0 2. | ce | 9200). | 2. | or | VORTEC Rees naee eee allel aoeabeys | | 5450-4 "Es | 5270 | This comparison has been made to show how, from mea- surements of liquid compressibility at present available, we can get only a fair idea of the value of /, but not an accurate measurement of it. Amagat has determined the compressibility of several other liquids at different temperatures (Ann. de Chim. et de Physique, sér. 5, t.xi.) ; so have Pagliani and Palazzo (Wied. Bezbl. ix.) and de Heen (Wied. ezdl. ix.), but their discussion would bring out nothing more than the above comparison has. De Heen’s results would appear to make / diminish with rising temperature in every case; but he measured his com- pressibilities in comparison with that of water at the same temperature, and to calculate their values used Pagliani and Vincentini’s values for water (Wied. Beibl. viii.), which make the compressibility of water much more variable with tem- perature than Grassi’s. If we used Grassi’s values in de Heen’s experiments, / would remain. nearly constant. We will accordingly use the compressibility-method of cal- culating / subsequently, only to illustrate the general agree- ment of. values derived from purely mechanical experiments with those found by the more accurate methods to which we now proceed. The values found by this second method are tabulated later on in Table XXIV. Third method of finding the virial constant 1: from the latent heat. If we differentiate with respect to T our equation Laws of Molecular Force. 243 for = eration -pressures (see Section 6), P(v—v%)) = " pdv, vy V7} we get dP avs a) dv oy dv, av (3 =) +P( (7 aT )=(°Ss ah do ot P (in dT CA ae ae 30p aT (v3 v1) =|" spo: Now from thermodynamics we have the relation JXN=(v3,—v,) TdP/aT, where X is the latent heat, oe ee a. oe JA= : Tsp which of course could have been written down immediately, for if we write it in the form Ir =|" {Gi oH )dv+ PoP, we remind ourselves that the latent heat of evaporation of a liquid is the heat supplied to neutralize a Thomson and Joule cooling effect. We must evaluate the integral in three stages, Op 1 OP ap Jf. TSpee= | tan o+ {08 T= pao | Toh ike using in each integral the ae that holds between its limits. In the first, vutk otk Op _ Ry, 24 or A 7) Op - l Cpe Baar, B ‘v—p 0st AG i er5 )- 944 Mr. William Sutherland on the In the third, T kv l po=RT(1+¥, =) 19h = RT a Pt Op 2)7 QW Hence n= | "(p+ oy Jao | ° {3 ( (p+ a) + Se +) (CG sa)- 5 he 03 1(*# % Idy 1(” Idv =| “piv + |, par | loth) * ie +h) 3 Céldv 3| 2 Vv 4 | Oe v 164 l 2v5 l 2K! = P(v3—%) 2) pdv + 7,08 ae) 3 9; °S wad +(- 2 i) oe v 4. v7} k 2 aa We must now evaluate the only integral that has been left unevaluated, te (LED ge ¥ dv (ld fi pav= | =, (lt 9) es le 1 1 (aa it =RTlog= + DT, se Flog”) il ] 8 2 ee Qk! byt :) — 7°74, Ree These last expressions are the only ones that introduce B and B into the value of JA, and it is desirable to remove these two constants. At low pressures we can neglect the pu term in the infracritical equation, and we get RT VT ad. oe By} v%31—-8 =e Co ot ae removing B by means of this we get pubig TN=P(vy—vy) + Glog, S +5(5- i) 1G wen) =2 (PBB : =) Laws of Molecular Force. 245 We can now remove # and greatly simplify this equation, if _ we apply it to latent heats near the ordinary boiling-point Ty. The last term taken in its entirety has a small numerical value compared to the rest, so that in it we can make approxi- mations without any sacrifice of accuracy worth considering : we have seen that 6 is approximately proportional to k (see Table X XI.) and v,, the volume of the liquid at the boiling- point, may be assumed to be approximately proportional to / the volume at the critical temperature, and k'=7k/6: hence the coefficient of (//2v,—R’T) in the last term is approxi- mately the same for all bodies and we can evaluate it for ethyl oxide; call it C. Again, in P(v3—v) neglect v, and assume the gaseous law Pv,;=RI,. And further, & is small compared to v3, so that 2v3/(v3+) is nearly 2, and its value for ethyl oxide can be applied to all bodies. B! =25R/13. Hence multiplying by M the ai weight we can write M/ Pie E 2Vs = 5(~ 1) tle = + 5 =} JU+MR (7 5 0—1)t. MRis the same for all bodies, and T, is the absolute boiling- point. This equation still involves & as well as /; when & is not known we must eliminate it by means of our previous assumption, namely, that k is proportional to v,, which we know to be approximately true; in so far as it is inexact it will introduce inexactness into our calculation of 1. Accord- ingly in symbols k/vy=7, where 7 is the same for all bodies, and can be found for ethyl oxide. Making the numerical reductions we get Ml/v,=66°5 MA—101T, as the equation which gives J in terms of the megadyne as unit of force, when A is the latent heat of a gramme in calories and v, its volume in cubic centimetres at the absolute boiling-point T,. ‘This equation will be abundantly verified afterwards in Table XXIV.; but meanwhile, if to test it we apply it to calculate the latent heat of ethyl oxide, we find X= 83'4, whereas several experimenters have agreed in an Betimate of about 90; but, on the other hand, Ramsay and Young (Phil. Trans. 1887) have made a special study of the terms in the thermodynamic relation JA= (v3—v,) TdP/d dhe and have so calculated values of % almost up to the critic: al temperatures, their value at the boiling-point is 84°4, and there is the same amount of discrepancy between their values at higher temperatures and Regnault’s experimental deter- minations. Yet Perot, who has made an elaborate study (Ann. de Ch. et de Ph. sér. 6, t. xiii.) both of X experimentally 946 Mr. William Sutherland on the and of the quantities involved in its calculation by the ther- modynamic relation, has found the most perfect harmony between the results of the two methods. Now at 30°C. Perot gives as the saturation-volume of the vapour 400°4, and the saturation-pressure °635 metre, while Ramsay and Young’s values are 374 and ‘648 metre; but if ethyl oxide were a perfect gas, under Perot’s pressure of *635 metre it would have a volume of 400°8, almost identical with his value: yet we cannot imagine that ethyl oxide under this pressure and at this temperature is so nearly a perfect gas as this would imply, unless there is some remarkable discontinuity in its behaviour at high volumes. Accordingly, in ‘spite of the thoroughness of the researches of both Perot and Ramsay and Young, we are on the horns of a triple dilemma, from which only some experimental repetition can deliver us, and de- monstrate where the cause of these discrepancies lies. Wiillner and Grotrian (Wied. Ann. xi.) have put on record the results of experiments which indicate the cause; they find the pressure - of condensation measurably different from the ordinarily measured saturation-pressure,—a fact explaining the difficulty of measuring v3; accurately, and showing also that the values of dP/dT are not so reliable as usually supposed. Our last equation is verified by, and shows us the cause of, an interesting relation that has been independently discovered and expressed in different forms, between the molecular latent heat and the boiling-point, by Pictet (Ann. de Ch. et de Ph. sér. 5, t. ix. 1876), ‘Trouton (Phil. Mag. xviii. 1884), and Ramsay and Young (Phil. Mag. xx. 1885), namely, that the molecular latent heats of fluids are nearly proportional to their absolute boiling-points. Now we have seen that T,=1201/409Rk (Section 4), and I have noticed that a large number of substances have their ordinary absolute boiling- points nearly equal to 2T,/3, and & is nearly proportional to v%, say is equal to 2°8v,, as it is for ethyl oxide. Hence we have 3 ere WAU) 2 409 R282,’ oe M/= 14°3 M RyT, = 1190»,T,, when the megadyne is the unit of force; hence from our equation for M/ in terms of X we have — 1190T,=66°5 MA—101 T, ; ©. 1291T,=66°5MA or MA=19-4T,, ~ Laws of Molecular Force. 247 or the molecular latent heat is proportional to the absolute boiling-point. (It is to be noted that M/=1190,T, gives a rough means of obtaining / from the boiling-points and the volumes at the boiling-points of liquids, which might be convenient when better data are wanting.) Robert Schiff (Ann. der Chem. cexxxiv.) has made the most accurate determinations to test this relation between molecular latent heat and boiling-point. For 29 compounds of the form C_H,,0,, from ethyl formiate up to isoamyl vale- rate, he finds MA=20°8T, in the mean, the greatest departures being 20°4 for propyl isobutyrate, and 21:1 for propyl for- miate ; for 8 hydrocarbons of the benzene series he finds a mean coefficient 20 with 19°8 for cymene and 20:6 for benzene as the greatest departures. To these 37 examples we will add the following from Trouton’s paper, doubling his numbers, as he used density instead of M. Taste XXITT.—Values of MA/T,. | O,H,Cl. CCl, | CS,. | | CHCl,. AsCl,. | SnCl,. | SO,,. 21 29 | 21 a1 20 | 23 Pin | | | | | | | (C,H,),0. (C;H,,).0. (CH,).CO. C,H. | (C,H,),C,0,,. 22 24 23 22 | 23 The mean value of the coefficient is higher than that deduced theoretically above (19:4), because in round fraction we wrote T,=2T,/3, but the general truth of the relation is well enough brought out. Fourth method of finding the virial constant /: from the critical temperature and pressure. Now we have (Section 4), T,=1201/409Rk, p,=361/409 k?, *. T,/p,=10K/38R and 1=409R?T?/400 p,, this is for compounds; for elements/=27R?T?/64p,.. Where both the critical pressure and temperature are known, this gives / theoretically with accuracy, but practically the diffi- culties in measuring the critical pressure introduce inaccuracy. In the relation T’,/p,=10%/3R, as R varies inversely as the molecular weight, we see that the molecular domains (Mole- cular volumes) of bodies at the critical temperature are 948 Mr. William Sutherland on the proportional to the quotient of critical temperature by critical pressure, a relation which Dewar has proved experimentally (Phil. Mag. xviii. 1884) for 21 volatile bodies, for which he has determined and collected the data. ‘These with other data since published enable us to determine values of / for certain bodies for which the other methods are not available. As there are many more critical temperatures determined up to the present than critical pressures, and as we have seen that an error in the critical temperature is of less relative importance than an error in the critical pressure, we can make ourselves independent of critical pressures with ad- vantage, by employing the approximation that has already been useful to us, that k is proportional to the volume of the liquid at the boiling-point or k=2°83v,. Then M/=409MRT /120= 800T 2; approximately, with the megadyne as unit of force. This is a more accurate form of the relation M/=1190T,v, given above, in which we assumed the approximation T,=2T,/3. 8. Fifth or Capillary Method of finding the Internal Virial Constant, with digressions on the Brownian movement in liquids and on molecular distances.—So far we have been proceeding on a purely inductive path, with two deductive guides in Clausius’s equation of the virial and in the law of the inverse fourth power, which requires that the internal virial should vary inversely as the volume. JBut now, in passing on to our fifth and most useful method of finding / from surface-tension, we must employ a deductive relation between / and surface-tension, furnished by the law of the inverse fourth power. In a previous paper (Phil. Mag. July 1887) it was shown that if the law of force between two molecules of mass m, at distance 7 apart is 3Am?/r*, then the internal virial for the molecules in unit mass is 57Ap log J./a, p being density, and L a finite length of the order of magni- tude of the linear dimensions of the vessels used in physical measurements, a being the mean distance apart of the mole- cules. ‘The ratio L/a remains the same for a given mass whatever volume it occupies, but I also assumed that J/a is so large a number that log L/a would hardly be affected by such large variations as might occur in the value of L when the behaviour of a kilogramme of a substance was compared with that of a milligramme. ‘T'o remove the haziness of this assumption, I will now make a more accurate evaluation of the internal virial. } 7 : ~ By definition it is $.4.223Am?/7*, and we will evaluate it Laws of Molecular Force. 249 for a spherical mass. To cast it into the form of an integral, take any molecule m amongst the number n in a spherical vessel of radius R; gather it to its centre as a true particle and spread the remaining n—1 in a uniform continuous mass separated from m by a small spherical vacuum of radius a, so chosen that the virial of m and the continuous mass is the same as that of m and the n—1 molecules. Suppose m at the point O, and the centre of the vessel at - C, and let OC=c. Take OC as axis of x and any two rec- tangular axes through O as axes of y and z. Let polar coordinates r@q be related to these in the usual manner. Then the equation to the surface of the sphere is (a—c)*? +y?+22=R? or r?—2er sin 0 cos 6 +c? —R?=0. Let 7, and r, be the two roots of this equation in 7 so that = R*?—c?. Then m?/r* can be replaced by mpr® sin 0 dé do dr/r*, and m?/r> by {\\mp sin 6 d@ dd dr/r. If we integrate with respect to 7 on oneside of the plane yz from ato 7, and on the other from a to 7, and add the two results, then we have to take @ and ¢ each between 0 and 7, thus: Lm2/r° =| ‘ome sin Od 0 db [| dr/r Dy dj], 0/0 a a The two integrals in brackets give log 7 7,/a?=log (R?—c?)/a?. Hence 2m?/r> = 2armp log (R®+ ¢?)/a?. Lo perform the second summation we can first add the values of the last expression for all the molecules at distance ¢ from the centre of the vessel, and write the result in the form 2apAmpc*dc log (R? —c?)/a?, and we then have R-a 4. 42233Am7/ = cnt e’'de log (R? —c*)/a?. 0 Kyaluating the integral, this becomes a 1 ; 2 R?, %*R+a BAnip? | 5 (R—a)*log a LS (R—a)?— 3 R°(R—a) + =z log }, in which, neglecting unity in comparison with the large number R/a, we get A7**R?{4 log 2R/a—16/3}. Phil. Mag. 8. 5. Vol. 35. No. 214. March 1898. S 250 Mr. William Sutherland on the But if W is the total mass in the vessel, then W =47r'p/3, and we get Warmp{3 log 2R/a—4}. When W =1 the first term of this becomes identical with the value of the internal virial previously given, with 2R written instead of L. Replacing R by its value in terms of W and p, we get for the internal virial of mass W, WaAmp(log 6W/mpa*—4). As pa® is constant, we see that for a given mass the internal virial for molecular force varying inversely as the fourth power is rigorously proportional to the density, but it is not purely proportional to the mass. Although the number 6W/mpa’ is a large one, and has a logarithm varying slowly with W, yet large enough variations in W can affect it appreciably, as we see if provisionally we accept Sir W. Thomson’s estimate of 2 x 10~-* centim. as the lowest possible value fora. Suppose 7p=38, then 6W/7pa’ is 10°°W/4, and if W is 4000, 4, or :004 grm., then the values of log 6W/zpa’ are as 30, 27, and 24, and we have a larger mass variation of the internal virial than is likely to have escaped detection in its effects, such as a difference in the density, expansion, com- pressibility, latent heat, and saturation-pressures of a liquid as measured on a milligramme, from their values as measured on a kilogramme. The raising of this difficulty suggests to us in passing that there exists a department of microphysics in which little has as yet been done by the experimenter, and that great interest would attach to a research determining when a mass variation of the properties usually spoken of as physical constants actually sets in. ; But meanwhile we must scrutinize more closely the meaning of our last result. According to the views of Laplace (and of the early elasticians), if a plane be drawn dividing a mass of solid or liquid into two parts, then, in consequence of mole- cular force, the one part exercises a resultant attraction on the other, and this has to be statically equilibrated by a pressure (called the molecular or internal pressure) acting across the plane, a conception which is necessary in any purely statical theory of elasticity. Adopting for the moment this mode of viewing things, we see that our result amounts to this, that the internal pressure is measurably greater at the centre of a kilogramme than of a milligramme. | But if we try to carry out the kinetic theory in its integrity, Laws of Molecular Force. 251 we must reject the idea of a statical pressure, and replace it by its kinetic equivalent of a to and fro transfer of momentum ; this may take place as a quite indiscriminate traffic of indi- vidual molecules across the plane, or as such a traffic modified by the existence of streams of molecules in opposite directions. If streams, or motions of molecules in swarms, actually exist in fluids, then our interpretation of the equation of the virial would have to take account of their existence. The kinetic energy of the motion of a swarm as a whole would not count as heat but as mechanical energy, and for the amount of it we should have approximately the kinetic energy of the swarm motion equal to the virial of the forces between the swarms. Therefore we require to divide the energy into two parts, that of molecular motion inside the swarm constituting heat and that of the swarm ; in the same way the internal virial is divided into two parts, one within each swarm, the other be- tween the swarms. But the swarms could on the average be regarded as equivalent to spheres of radius L, where L must be supposed nearly independent of mass and liable to the same variations with temperature and pressure as the linear dimen- sions of any quantity of the liquid, so that L is proportional to a, and our expression (theoretical) W Azp(3 log 2L/a—4) for the internal virial becomes purely proportional to the mass and purely proportional to the density, as 3W//4v our experimental internal virial for a mass W of a compound liquid is. This hypothesis would affect somewhat the rigorousness of certain thermodynamical relations as usually interpreted, such as JA=(v3—v,) [dp/dT, since it provides a supply of internal mechanical energy not taken account of ; but if this supply is only slightly variable with pressure and temperature it would make little difference in most parts of thermodynamics. With the addition of this hypothesis of molecular swarms, which will be used only in calculating molecular distances, and will not affect at all the rest of our work, the law of the inverse fourth power is brought into strict harmony with the behaviour of compound liquids and of elements both as liquids and gases. We must therefore inquire what experimental evidence there is for the existence in liquids of a motion of swarms of molecules, possessing the remarkable property of not being degraded to heat as ordinary visible motions are. In the motion long familiar to microscopists as the Brownian movement we have such evidence. Gouy has _ recently (Compt. Rend. cix. p. 103) recalled the attention of physicists to this remarkable ceaseless motion of granules in liquids. He states that it occurs with all sorts of granules, and with an S 2 252 Mr. William Sutherland on the intensity less as the liquid is more viscous and as the granules are larger. It occurs when every precaution is taken to en- sure constant temperature, and to ensure the absence of all external causes of motion. Granules of the same size but as different in character as solid granules, liquid globules, and gaseous bubbles, show but little difference in their motions—a fact which proves that the cause is to be looked for not in the granules themselves but in the liquid, the granules being merely an index of motions existing in the liquid. The most pronounced character of the motion is its rapid increase with diminishing size of granules, so that all that is seen under the microscope is the limit of movements of unknown magnitude. Gouy considers the Brownian movements to be a remote result of the motion of the molecules themselves, but according to what we know of molecular dimensions I fancy that the Brownian movement must be considered rather as a sign of the motion of swarms of molecules. If swarms of molecules are weaving in and out amongst one another, so that the average transfer of momentum at a point is the same in all directions, then the vibratory agitation of granules amongst the swarms is just what we should expect. The striking fact about the Brownian movement is that it is ceaseless; it is never degraded into heat. This alone forces us to conceive a form of motion existing in liquids on a larger scale than molecular motion but possessing its character of permanence ; in other words, the motion of swarms of molecules. The existence of swarms would not affect our views of the rise of liquids in capillary tubes as a purely statical question; so that, for the connexion between molecular force and surface-tension, we can use the calculation given in another paper (Phil. Mag. April 1889) (rather badly affected with misprints), where I have shown that the surface-tension of liquids that wet glass, measured in tubes so narrow that the meniscus-surface is a hemisphere, is given by the equation amp’ Ae/(2+V 2); where p is the average density of the capillary surface-film (to be written also 1/v), and ¢ is the distance which we must suppose to be left between a continuous meniscus and the base of a continuous column raised by its attraction, if the action between the continuous distributions is to be the same as in the natural case of discontinuous molecular constitution of meniscus and column. The distance e is not identical with the length a which occurs in our theoretical value of the internal virial of unit mass, 31 Amp (3 log 2L/a—4) = 9 Oe Laws of Molecular Force. | 253 but it is closely proportional to it. If we can find the relation between e and a, then from capillary determinations we can obtain relative values of the virial constant / which, as we have already found some absolute values of /, can be converted to absolute values ; at the same time, too, we shall be able to find a value of a the mean distance apart of the molecules. To find the relations between e and a we can proceed thus. If we have a single infinite straight row of molecules at a distance a apart, the force exerted by one half of it on the other is N=0 _N=O 3An? Swi =r, (p+n)ia® which can easily be evaluated as approximately 3°6Am?/a’. Two infinite continuous lines in the same line, of density m/a with distance e between their contiguous ends, would exert a force DM (ni a aay CTD (Cae) on one another; this is equal to Am?/2a’e. If, then, the continuous distribution is to be equal to the molecular, we nave Ca Oe ame 10) ul Again, if along two infinite axes one at right angles to the other and terminating in an origin O at its middle point molecules are arranged along each at distance a apart starting from O, then the force exerted by the unlimited row on the other is : P=O qN=O 3Amn p=o 3Am Pyar Paar Gry nich 1 pia” which can be evaluated at about 5Am?/a‘. Replace the rows by two continuous line-distributions of density m/a, the one terminating at a distance e from O: it is required to find e so that the force may be the same as this. The force is al { ees = Am?/a?e*. a é 0 (x? +y?)3 Hence in this case Gps | 6 0/ao er. From these two simple cases we get an idea of the relation between e and a. The case of a meuiscus attracting the column which it raises in a capillary tube is more analogous to the second than to the first, and it is easy to see that in the 254. Mr. William Sutherland on the case of the meniscus we can say that ¢ is not less than a/2°2. It will suffice to write e=a/2°2. Now according to the definition of a in our theoretical expression for the internal virial, it is the radius of the sphe- rical vacuum artificially used to represent the domain of a molecule ; but as it occurs in the expression log 2L/a, where 2L/a is a very large number and the value of LL is indefinite, we see that there is no inaccuracy in making it identical with athe mean distance apart of the molecules. However, for the sake of formal completeness, we can easily find the rela- tion between the two quantities which we have denoted by the one symbol a. Let us now denote by # the mean dis- tance apart of the molecules, that is the edge of the cube in a cubical distribution of the molecules; then, from the defi- nition of a, z and a are connected by the relation R LAm?/7? = { Am Anidr/a*r, the summation being extended to all the molecules in a sphere of radius R. By actual summation up to R=5z we find approximately a="9x. With our previous estimate of e as a/2'2, which we must now write 7/2°2 on account of our change of symbol for mean distance apart, we have the two equations, l= Am(4 log 2L/‘9x—16/8), a=mp’Ax/2°2(2 + / 2), We can replace p by p, the difference between them being necessarily very slight. Then for ethyl oxide we have the following data: « at the boiling-point according to Schiff is 1:57 grammes weight per metre, or 1:57/10° kilog. per em. ; lis 7500 kilog. em.*, and v,=1:44cm.? Eliminating A from the two equations, we have a relation between w and L, namely 2=T-5u 5 (9-2 logy 2L/-94—16/8). L being hypothetical is not known to us, but we can give ita series of possible values, and calculate by trial from the last equation the corresponding series of values for x, with the following results :-— L. Le 1/10° cm. 4°6/107 cm. 1/10* 7) rig | 7) P) 1/10° ,, 7) Ge Laws of Molecular Force. 255 As it is subsequently to be shown that in liquid ethyl oxide and in all regular compound liquids the molecules are paired, and that each pair acts on the others as if it were a single molecule, we may estimate it as likely that the mean distance apart of the pairs in ethyl oxide is between 1 and 10 micro- millimetres (1/10® mm.). This result, though 100 times as large as Sir William Thomson’s limits for the distance apart of molecules in liquids, namely 2 x 10-9 em. and 7 x 10-9 em., is yet in better agreement with the estimate of molecular dis- tances arrived at by Riicker (Journ. Chem. Soc. 1888) as the most probable result obtainable from the most important attempts yet made to measure the range of molecular forces. The most suggestive of these is Reinold and Riicker’s dis- covery, that the equilibrium of a soap-solution film becomes unstable when its thickness is reduced to between 96 and 45 micromillimetres, but again becomes stable when the thickness is still further reduced to 12 micromillimetres. At the latter thickness the film shows black in reflected light. If the intermolecular distances are nearly the same in soap-solutions as in liquid ethyl oxide, then the black film must be regarded as consisting of a single layer of molecules or groups of mole- cules (in the case of water the molecules will subsequently be shown to go in double pairs). This is an intelligible result, and gives the simplest explanation of Reinold and Riicker’s beautiful discovery of a stable thickness supervening on the unstable, for we recognize a single layer of molecules as a stable configuration. Of course it is to be understood that what we mean by the thickness of a single layer of molecules is the one nth part of the thickness of n layers; and if the black film is really only a single layer, it is in this sense that Reinold and Riicker’s estimate of 12 micromms. is to be taken, for they did not measure an actual distance from the front to the back of a black film, but only estimated from accurate and accordant measurements, made in entirely different manners, that the number of layers in the black film is to the number in a thickness of 1 centim. as 12 micromms. is to 1 centim. If the black film consists really of only a single layer of molecules, it is surely a hopeful sign for molecular physics that measurements should have been possible on it, though only visible through its invisibility. If, encouraged by this experimental support, we say that in round numbers the mean distance between the pairs of mole cules in liquid ethyl oxide is 10 micromms., then one gramme contains 2v, x 10° molecules, or the mass of a single molecule 1s 1/2°88 x 108 orm. =3°5/10%, 256 Mr. William Sutherland on the and so the mass of an atom of H is 3°5/74 x 10° =5/10" grm. nearly. It would lead us too far from our present purpose to discuss other estimates of molecular distance, especially as Reinold and Riicker’s measurement of the black film is the most defi- nite and striking yet made of these minute distances ; but the question of the range of molecular force is of special import- ance to us. Quincke (Pogg. Ann. exxxvii.) determined what thickness of silver it is necessary to deposit on glass so that the capil- lary effect on water may be the same as that of solid silver; that is, at what distance the difference between the molecular attractions of glass and silver for water becomes too small to be measured. He found the thickness to be about 50 micromms. Now, according to the law of the inverse fourth power, the attraction of a cylinder of radius c, length h, and density p on a particle of mass m on the axis at a distance z from the nearest end is easily calculated as 1 i 1 1 2g eth Ve+2 Vet (ethy If the cylinder consists of a length h, of silver with a length h of glass, the silver being near the particle, then, the suffixes 1 and 2 applying to silver and glass, the attraction of the composite cylinder is 1 1 2A,mp; Pe 2m (Aipx — Aspe) (= +h, Ve Ge rise a “Tees e? + 2? il 1 — 2A ,mpo7 (== ES etht+th, e+ (e+h, +h,)? Making the circumstances correspond to Quincke’s experi- ment, we have z nearly equal to the mean molecular distance in water, about 10 micromms.; h, is small compared to hy and ¢, and, according to Quincke, is 50 micromms. when the composite cylinder exerts the same force on m as if it were all silver ; accordingly the last expression reduces to the two terms 2A mp, /2—2m7 (Ayp,—Agp2)/(2 + hy), which permit us to compare the molecular force range /, with the molecular distance z. That the second of these terms should become negligible when h, is 50 micromms. is a result quite in accordance with the value 10 micromms. for z. Let us briefly compare the magnitudes of molecular and gravitational force. The most convenient plan will be to compare the two forces in the case of two single ethyl-oxide Laws of Molecular Force. 257 molecules at a distance of one centim. apart; that is, to calculate Am? and Gm?, where m is the actual mass of the molecule, and G the constant in the expression Gm?/r? for gravitation. In the expression a=mp*Ax/2°2(2+ V2), using the value 10 micromms. for # and the values previously given for the other quantities, we can find A, and then using the value 3°5/10" for the mass of a molecule of ethyl oxide we find Am?=9/10* in terms of the dyne. To calculate G we have 981 as the acceleration of gravitation ; the mass of the earth is 6 x 10° erm. and its radius is 6°37 x107%cm., so that Gm? = 2°1/10* in terms of the dyne. Hence at a distance of (1 centim. the gravitation of two ethyl-oxide molecules is about double their molecular attraction, or, allowing for un- | / | certainties in our calculation, we may say that at about 1 centim. apart two molecules exert the same gravitational as molecular force on one another. - We now return to the main business of this section, which is the Fifth Method of finding the virial constant J. This consists In using the equation already used for calculating molecular distances in the form [=7-5r%x(4 log 2,/:92—16/3)/s. Now , the molecular distance for different liquids, varies as mé v3, and the expression in brackets may be assumed to be the same for all bodies ; hence /=cavt/m*, where c is a constant whose value can be obtained on substituting in the case of ethyl oxide the known. values of /, 2, v, and m, or, more safely, by taking a mean value from several substances. But we must remember that we are using v the volume in the body of the liquid, instead of v that in the surface-film; a replacement which is not justified by experiment, seeing that for a given liquid «v* measured at different temperatures is not constant, the reason being that v varies much more rapidly with temperature than v. But, in our ignorance of the rela- tion between surface and body-density, all that we seek for from the above equation for /, is true values for / from mea- sured values for « Accordingly the question arises, Can we choose temperatures at which to measure @ for different sub- stances, so as to get true relative values of / irrespective of our ignorance of v? As we have seen (Section 6) that at equal fractions of their critical temperatures, and under equal fractions of their critical pressures, one liquid is approximately a model of another on 258 Mr. William Sutherland on the a different scale, we conclude that if we use the value of the surface-tension measured at a constant fraction of the eritical temperature, and under a constant fraction of the eritical pressure, we ought to get correct relative values of 7; as surface-tension is not appreciably affected by pressure, we can dispense with the condition as to pressure and use mea- surements of a made under a pressure of one atmosphere at a constant fraction of the critical temperature. I have chosen the fraction as two-thirds, because it gives a temperature near to the boiling-point of most liquids. Schiff’s abundant measurements (Ann. der Chem. ccxxiil., and, further, Wied. Gezb/. ix.) include not only the height to which different liquids rise in a capillary tube at their boiling- points, but also its temperature-coefficient, which is such as to show that the height in every case vanishes near the critical point. Let H be the height to which a liquid rises in a tube of radius 1 millim.; then if H really vanished at the critical temperature and varied linearly with temperature, we should at 2T,/3 have H=T,b/3, where b is the temperature-coefficient. But to use this would be to depend too much on the accuracy of b, If H, is the value at T;, the boiling-point, then T,=T, + H,/d, and H=H,+ (T,—2T./3)b=H,/3+ 1.6/3, which depends partly on H;, measured by Schiff, and partly on 6. Now «=Hp/2=H/20 ; “. Lor cav3/ms=cHv3/2m:, l= c( H,/3 -- T,b/3)v3/2ms. If H is measured according to the usual practice as the height in millimetres for a tube of radius 1 millim., that is, if a is measured in grammes weight per metre, then if / is desired in terms of the megadyne, gramme, and centimetre as units, ¢/2=5930, a mean value. Apart from all hypothesis about molecular force, our last relation between the virial constant and the constants of capillarity will be amply con- firmed by the extensive comparisons soon to be presented in Tables XXIV. and XXV. Meanwhile a few consequences of the relation may be glanced at. 9. Establishment on Theoretical grounds of Eétvés’s relation between surface-tension, volume, and temperature——dAccord- ing to the modified equation of the fourth method of finding 1, M’=800T.v,; and according to that of the fifth method, l=cavi/ms. The first of these equations would be more accurate if we replaced v, by v, which in the second means the volume at 2T,/3 ; so. M/=800T,v, and m the actual mass ‘Laws of Molecular Force. 259 of the molecule is proportional to M its molecular weight ; so that from the second we have M/ proportional to «(Mv)z, and hence e(Mr)% measured at 2T,/3 is for all bodies pro- portional to T,. Now in our notation the relation discovered by Hotvés (Wied. Ann. xxvii.) is d{a(Mv)3} /dT='227, or a(Mv)?=:227(T—T/), where T,! is a temperature very close to the critical ; and this is only a more general statement of the relation we have just deduced. As Hoétvos has verified his relation experimentally for a large number of bodies, his result is a verification also of our general principles. The form of his relation also induces us to examine a little more closely an important consequence of the form of our infracritical equation, which, when multiplied by M with the pv term removed at low pressures, becomes Mi _ VT Eee T 25." Bo v— =) : Now R’M is constant, and Ml/v is proportional to a(Mv)s, if a and v are measured at 2T,/3, or any other constant fraction of the critical temperature, and under these circumstances a( Mv) has been shown to be proportional to T,; hence if T is al, a being a constant fraction, we get T, proportional to VT k—v (14 sae . —=;) aT. ; VT ki —v so that 1+ B ip=6 critical temperature, is approximately the same for all bodies, a result which our study of Van der Waals’s generalization showed us to be approximately true. This shows that Hoétvis’s relation is rigorous only to the same extent as the constancy of this last expression is rigorous; as a matter of fact, exclu- ding the alcohols and water, Hoétvés finds the constant whose mean value is taken as *227 to depart from this mean value by not more than 5 per cent. in any individual case. ‘This brief discussion of Hétvés’s relation has therefore furnished us with additional proof of the general accuracy of the ap- proximations we have been forced to make in parts of our work. One of the main difficulties in the way of pushing on with the many interesting inquiries opened up by these relations lies in the fact that we do not know the relation between the densities in the body and in the surface-layer of a liquid. RM (1+ , measured at a constant fraction of the 260 Mr. William Sutherland on the We have to replace our relation E ein a varies as Ap*m* by the less accurate one, e 5 1 a varies as Ap*m*. Multiplying by (Mv)? or (M/p)*, we get the «(Mv)* of Hotvés proportional at all temperatures to AMp; and as d{a(Mv)*} dT is constant, and has been shown by Hétvés to be constant almost right up to the critical temperature, and to be the same for all bodies, we ought, if our assumptions were rigorous, to have AMdp/dT constant almost up to the critical tempe- rature and the same for all bodies (whence another approximate method of finding A or 1). Now dp/dT has been shown by Mendeléeff to be constant for many substances within ordinary temperature-ranges ; but the constancy does not hold up to the critical temperature, and the ultimate meaning of the apparent contradiction between Hétvés’s result and this is that, while for most purposes we may safely enough assume p proportional to p, we cannot so accurately proceed to the consequence dp*/aT proportional to dp /dT ; in fact, a change of temperature being accompanied by a change of stress in the surface-layer, the change of p with temperature is more complex than that of p. But within the range of temperature for which dp/dT is approximately constant, we have the important result that w/e ae = T d wrpr op MR (1+ eae is constant and, is approximately the same for all bodies. As I now consider the term differentiated to be not two thirds of the translatory kinetic energy of the gramme- molecule, but two thirds of the sum of the total kinetic energy and the chemic virial, I must replace the verbal statement of the last result as given in my paper (Phil. Mag. April 1889, p. 812) by the following :—The temperature-rate of variation of the sum of the total kinetic energy and the chemie virial of a molecule, measured at low constant pressure, is the same for all bodies (approximately). 10. Tabulation of Values of the Virial Constant, determined by four of the five methods described, and multiplied by the square of the molecular weight.—In the first place, I will give a comparison of the values of M*/ for those bodies to which existing data allow the application of three or four of the previously described methods. The multiplication by M? is for future convenience. The values obtained by the second Laws of Molecular Force. 261 (liquid compression and expansion), third (latent heat), fourth (critical temperature), and fifth (capillarity) methods are entered in the columns marked 2, 3,4,and 5. (The modified fourth method was used, namely, M/= 800 T,v,.) The units are the megamegadyne (10” dynes), grm., and cm. TABLE XXIV. re Substance. . 3. 4. 5. Sa Ne esti 26°5 257 27-2 26:9 | 1? Ly Ss Sanne Bee Rene pep oe COs erro rone oof 41°7 43°4 | COI Spec eOne ois Seen Baecel ap RARE 46:3 462 -| 456 2G) aaerecrreprepeccen 33:0 382 36'1 36°8 eNO fr civicaasis aac ae 22°3 28°3 26°5 | EP scioec des see rceline |i odes o2l 31°5 29:0 | BE os crecich cic'sansns xc age AS OR aia sree 45°3 Alpell | OE ses aecia owes sistsaieice yg Orr = steno 58:5 593 ipl BAIR See eae 40:0 43:1 42°7 43°8 O15 LA eee 59-0 558 56°2 56:4 (OLS FO een ner eee 360 31°3 ital Methyl butyrate ...... 65:0 60:4 556 56-1 Ethyl butyrate ......... 84:0 74:6 69:5 TAE3 The satisfactory agreement of these values, calculated for such diverse bodies from such diverse data, must be taken as the verification of the main principles so far unfolded—the chief of which as rezards molecular force is that for most compound bodies the internal virial term of the characteristic equation is //2v below the volume &, and //(v+) above that volume. We see, too, now how important for molecular dynamies is the detailed study of each of the constants k, B, and @ in the characteristic equations ; but for the present we must refrain from entering on such a study, and must consider the com- parison in the last table as closing for the present the general discussion of the characteristic equation. Our immediate object is now to ascertain the law connecting the value of M*/ for a body with its chemical composition. On the hypothesis of the inverse fourth power (with the sub- sidiary one of molecular swarms), ml = mm A(4 log 2L/a—16/3) ; so that, the bracketed expression being the same for all bodies, m7/ is proportional to m?A, and the law of m/ or M?/ will be the law of mA in the expression 3Am’/r* for the force between two molecules. In the Phil. Mag. for April 1889 | announced a law for the parameter A, calculated from Schitt’s capillary data, which applied fairly well to a large number ot organic compounds, but was affected with exceptions subversive of its generality. Applying now the more accurate method ot 262 Mr. William Sutherland on the calculation described as the fifth to all Schiff’s data, we obtain ample material for generalization, which can be supplemented by values calculated by the other methods. In the following Table the units are again the megamega- dyne, grm.,andem. For brevity the radicals methyl, ethyl, and propyl, &., will be denoted by the first two letters of their names, while the acid radicals-—-formic, propionic, &¢.— will be denoted by Fot, Prt, and so on, so that PrPrt stands for propyl propionate. The numbers entered under the heading $ will be explained when we are discussing the law of NPE TaBLeE XXV.—Values of M7/. First Method. | MI. S. Ml. S. 1 By Oa seer cae | 40:2 4:5 Te nicte nee Semone 22 “O04 COs os. ee aig: aligtc07 || Nuc.) ce eae 1:23 205 SO Scatter cece | 15-0 2°05 OFA ci. create eee 1:16 "195 ING en recbasce ts [ee eRe 1:25 Os Pipes <= 2-2 00 AN Oo etece caunat ceee | 88 1:3 O, 71 j.bcsecteeee 6:5 1:0 Third Method. | wz. | 8. | Mee hibit i) Oy Faerie Sad ee 61:3 6-1 IsoBwihet 28 G2 (ei ASO erick 4 does 49-0 52 HtDut:?.. gees 769 715 ES OIL Sener aes Mee 23°5 2:95 || -PrPrts yee 773 72 SiC ieacce- secant 473 5:05 Tso AmmHOt ..--2 ee 78:7 73 OL SLy aaa nee me Ec: 27-4 33 PrisoBut \). ie 89:1 8:0 Eee dies oe A007 «|, .4-5. | HtVaten. ee 895 | 80 ATCA) el OOo 79 Tso Burt. oe 92:5 8:15 PAA Oe cess 61:8 6°15 IsoAmAct ......... 93-1 8:15 Nit eae eae 48-7 5b, || Prue ee 92°5 815 CHa ate oe ee 35°0 4:0 TsoBuisoBut ...... 105 8-9 Led a are alae 90°4 8-0 PrVats eee hoe 106 89 idee. teats te 109-0 | 91 || IsoBuBut ......... 109 9-1 CH Benes. es. 49°4 5:2 IsoAmPrt ee 110 oly BU SO SO) dertcipae oid 109-0 all IsoAmisoBut...... 125 9°95 OM eae aaee 44-] 4-8 TSOREViat soso 126 10 aD) a0 er pee 35°6 41 IsoAmBut ......... 129 10°15 IMGACL iikats csc 36:0 4-1 TIsoAmVat ......... 147 11 BI ALCE Snore sono 47-6 Dall Ge onc coke eae 43:1 4:7 MeRrE 22k cae 47-5 Sil CF er ee 55'8 57 Lig Reece Pees 50°2 5p @, Nt eee 69°5 6°65 MeButiso ......... 60-4 6-04 C3H,, (meta)...... 714 68 isoBulloties es. 63°7 6:3 CH Pr. 2.2 85°9 775 18 oR IRe PR a ee 62°4 6:2 C,H,.(mesitylene)| 86:1 775 BEAGLE creep ns 62°8 6:2 C,H,, (pseudo- 87-1 7-8 MeBute .....c0 4. «0. 61°8 6°15 cumene)...... EtisoBut ......... 74:6 70 C,H, (eymene) .| 101 86 MGV 2S scot <2 74:1 70 | Laws of Molecular Force. 263 Table XXV. (continued). Fourth Method. | Mz S. M2, S | BU icc ank 58 Dipl Pe@ligmtecue too 346. |. 40 BI os cinws l@oee elo > NER oe uk... 100 | 1-4 bi. eee 96°) 14°” | IN Merc. c..1..00- 176 |..23 Oe ac. 2: AO, | NIEIMEM ele 23:5. | 30 Cn oe Aa teed Se | Nie, sai. Pe 36. Aa Ci) BGO 49" NA Bb ewe 2 | 27 Se FO oS ||| NH Bia es 41-4 | 4:55 0. 2 Tees || Nite wee. 655..| 6-4 Et TOs Se YN Pref 33-4. |. 3-9 C0 ae poe eee “| NE Deka: 676 | 65 Suc. 2 er 26:6 | 8:25 Fourth Method modified (not using critical pressures). | M. S. ee es: (ome), |... 380 | £3 || EKO,H,O ......... 48-6 ae B15 CHECHICL.) «02. 377 4:3 EON et date menret oe" ele Oh a LO) ae ener: 340 4:0 Mie © lire uate 16°8 2°2 CH,(OCH.). EC ot. a cece 26°4 32 (ethylal; Me } Sea 9 Pe@leine tre 326 | 38 GEMOTOOT). par (eg. | NEs cence noes 76) 11 Geval) os. i : NESMet eos 1b6:> | 21 TL, haa 418 -| 46 || NHMpe, .......:.... 935 3:0 COD IEU pdcocaen cena 51:2 5:4. INIMent er ame hoke 310- | 37 C12 cao SOON aia eer NIE! Sheet h 4-4 3:05 OIE pace eaoe eee 81:1 TA INAH Grr dae ee 43°5 4°75 EG a DO ue ea2sGs. Neen ee 66-4 | 65 JULES 3 CG ae 29:9 36 TBI) Bie e nese cuceaticn 31:0 o7 HEPrO _....-c.-s 524. | 5450 WNP oh 686 | 66 Fifth Method. \ M*/ 8. MZ S SE, cain os i000 ohee= 321 38 tet Cis Geena ates. 72:3 6°85 IMIG AGE 61 j..0.t000 35°6 4-1 el SOMS UG) cased cae. TAS 6°8 12 Ye) Cae Rear 44-2 48 Moe Viatt ywencte se sos. 69°7 6°7 135. eee See 45°4 49 TsoAmAct ......... 87-3 cs MMSE Rt occ je. esusd 44-8 4°85 TsoBuP rt) avis. 87:7 785 HO BWH Ob. «01... /05 56°9 5:8 Pr Bina eeenceeec cas 89°35 C95 PERN brs ciicieiicieicniselts 579 5:85 PrisoB nilieusk cess 87:7 T'85 EIDE SB esas oiciavesoueierd 58:5 5:9 HEN GIRO aiiidie cick ack | 86:5 78 DECIR UE... .necentiet 58'2 59 lisjoysWanl Seven secenee | 105 8°85 MeisoBut ......... d6°1 575 || IsoBuBut ......... + 106 8:9 IsoAmFot.........| 716 | 68 || IsoBuisoBut ...... 103 875 | TsoBuAct. ........< 70°6 675 || PrisoVat ......... | 103 SiS. | OE sie coscewsn ones 73:°3 6:9 | 264 Mr. William Sutherland on the Table XXV. (contenued). M/. 8. COREL SE ress chess ane®e eee: Normal hexane) 2.c:2sc.cessee- 59°3 6:0 COB 2 1 sere anatene metres on Diisobutyl..cs..-tek eee eee 90-6 8:0 Oh * josseneenecce ete Disoamyl! 7c. sseeceeee eee 1256 10:0 OE a (Pe tay 5, 4 ey Amylene "2. c.c2. cess oaneeeee 45:0 4:9 CER s Ui eean eae Caprylene: sis..cc.neesacseeeeee 91°8 81 OFA s RE in sas ara Ler penelich.ce.-saceomaeceneee 107-4 9:0 OTN aioe eee caste Diallya esc yecccnsceseseeee ceteris 54:8 5'6 (OF IER catann cy cen en Benzene! Shc cto..e-tee eee eee 43°8 4°75 CLTA SY. osttare tn toneee Volwene se ©: knee keane eee 56°4 5°75 Og nee oc aa ae ae Orthoxylene: ix. estas. secre 69-7 6°65 AUST. ce caterers enemas Maetaxyleme nase o:.ce sean le “Omg 6°65 COREL Fac hyena ane eee iParaxylene\.sec.snecateesssecee 70°3 6°7 OF leh Aupnsneehee roe mtanee Hithy benzene een. c.tors--2 cee 70°6 6-7 Ce acanaiearn: «cescaree Normal propylbenzene ...... 86°9 78 LE [ele sean ree on rae a Hthyltoluene paiess.e-ss ee eee 86°1 tip ORE sirsces, Socatac sanenue es IMesitylene:. cescse-panostecwcmse 85:3 7°65 CHANEL eet es etn OyiMMeno ecstacy eae | 103-0 8-75 G25 Omen e ts peel Chilorotoginissc sca acer eee 36°9 4-2 Oli sac teat Mec acurt ce Carbon tetrachloride ......... 45°6 4:9 (CECI) kek eens cece: Ethylene chloride ............ 44-4 4:8 CHE CHO gare scctass ccs Ethidene chloride ....... ate 38:1 4:3 PC gs eae oe Sans iPropyluchloride -.trscceeeee 37°9 4:3 J ESoyl Bi G1 Irs pe oe te a Isobutyl chloride ............ | 270 5:4 PSO AGW Hck anaes Isoamyl chloride ............ 66:4 6°45 CC). sak eens os C blorobenzener . 2.2. .cereeeee 57-7 5°85 (Dele Ie O/ Meaaen eee ae Chlorotoluene).>...sstes. nce 76:0 ee Cole Cl. acate asa cncpeee iBenzylechiloride = eee pee 82:2 75 0751 c Fal 0 | BAS nha os ee Propylene chloride............ 56°8 58 or ©) Hip Sire mina ae See ATS NC DWN RAN 2a ane anette. 65°6 6-4 Orie TA Oi ae acc nedeesiar Prichlorethame |< -.se8<.caeace 58-2 59 OE CO: 8 hecencces Hpichlorbydtin’ <....2:.-.---0 49-8 5°25 COPCOR: poke eens Chilorals 253 anos seca 509 5°35 CER CICO, Ht....<. . These show that there is not a constant difference in the value of M7 corresponding to the difference in the number of CH, groups contained. We can amplify this list of paraffins by using the material furnished by Bartoli and Stracciati (Ann. de Chim. et de Phys. sér. 6, t. vit.), who have determined the more important physical constants for all the paraffins from C;H), up to Cy,H3,. Their values of the capillary constants were found at about 11 degrees in every case. To obtain those at two thirds of the critical temperature, we have to use the values of the critical temperatures calculated by them from Thorpe and Riicker’s convenient empirical relation (Journ. Chem. Soc. xlv.), . p/(2T,—T) = constant, p being density at T. The following are the values of M*/ thus obtained :-— C;5H,.. C.Hy.. C,H, ¢. C,H, 6° CAs. C,H». C,H... AT*2 08 1 71 79°6 912 110 127 C,,H,,. C,H... C,H. C,,H,5. C, 5H. Ont, 147 iva LOB? Praieels 230 . wae Considering the assumptions involved in the.calculation of these values and the difficulty of obtaining the paraffins pure, the agreement for C,Hy,, CgH,,, and C,H. with Schiff’s numbers is excellent; but the higher we go in the series the larger is the temperature-interval for which we have to extrapolate, and the more uncertain do the values become. However, they are useful as giving a general idea of the course of M?/ in an extended series. On plotting these numbers as ordinates with abscissee representing the number of CH, groups in the molecule, a curve was constructed which proved to be the parabola M2] = 68 +-6682, where 8 is the number of CH, groups. It is only necessary then to determine on this curve the abscissa corresponding to Laws of Molecular Force. 267 the value of M?/ for any substance to obtain the number of CH, groups to which its molecule is equivalent as regards molecular force. 11. Definition of the Dynic Equivalent of a substance, and determination of its value for several Radicals—lIn the manner just described were obtained the numbers entered in Table XXYV. under the heading 8, which I propose to call the Dynic Hquivalents of the substances. The dynic equivalent of a molecule is the number of CH, groups in the molecule of the normal paraffin that exerts the same molecular force as it. The table shows that the atom of an element contributes the same amount towards the dynic equivalent of all molecules in which it occurs (except in the case of the simpler typical compounds) : thus, for example, consider the iodides from methyl to amyl iodide, and notice that each CH, group has the same value unity as in the paraffins, and that the iodine atom is equivalent to about 2°3CH, in every case. The same law holds throughout the table ; so that each elementary atom or radical has its own dynic equivalent, which can be easily determined. In the first place, it appears that the extra H, in the paratiins C,H,,,, can be neglected in a first approximation, because C;H,) has practically the same dynic equivalent as C;Hy., and CgH,, the same as CgHjs. It may be that the double binding in the unsaturated compounds compensates for the H, of the saturated, but I think that the simpler idea for the present is that the two terminal H atoms in a paraffin chain have a dynic equivalent so small that we may neglect it, or more generally the middle H in a CH; group is negligibie in a first approximation. If there is really such a ditterence between the middle H and the two others in CH;, we ought to find the dynic equivalents for the iso-compounds smaller than for the normal; and the table shows that the isobutyrates have equivalents smaller by °1 than the butyrates, while the iso- butyl salts of the fatty acids have dynic equivalents nearly all less than 1 greater than the propyl salts. But this is rather a matter for the chemist to work out in detail; it suffices to indicate the idea here, and to point out that it is in harmony with the lowering of boiling-points among isomers with in- creasing number of CH, groups. Accordingly, as a matter of detail, in the estimation of the dynic equivalents of the elements, it was assumed that the equivalent of C,H, ,,, C,H,,,,, and C,H,, is in each case n when normal and n—‘lp when the molecule departs from normality by p CH; groups. (In constructing my curve for dynic equivalents, for the sake of T 92 — 268 Mr. William Sutherland on the simplicity at first, I ignored the fact that two of the paraffins in Schiff’s data are iso-compounds.) From the tabulated values for the alkyl salts of the fatty acids, we get the following mean values for the dynic equi- valent of CO”O!:—in the formiates 1°85, acetates 1°92, pro- pionates 1°91, butyrates 1:92, isobutyrates 1°91, and iso- valerates 1°83, the mean for all being 1°9. From the oxides (ethers) and other compounds containing single-bound O, we find for its mean value °6, although in the ethers containing the benzene nucleus it comes out *8, while in the benzoates CO’’O' is about 2°5 ; so that the junction of the benzene nucleus with other groups seems to be accompanied with an increase in its value : witness also the bromide, iodide, and amine of O,H;, equal to the bromide, iodide, and amine of CH, although O,H, is less than C;Hj. by *25. This slight variation of the value of C,H, is the only anomaly amongst the numbers of Table X XV. excepting the simple typical com- pounds. The values ‘6 for O'and 1:9 for C’O! are in harmony with the results for all the other compounds containing oxygen. From the values for the benzene series of hydrocarbons we can get a value for H, in CH, and also some light on the important question of the structure of the benzene nucleus. Thomsen has been led by his thermochemical investigations to the conclusion that in benzene each carbon atom is bound to three other carbon atoms by a single bond to each (the “bond” phraseology is used merely for brevity, and not as expressing definite statical or dynamical facts). If we accept this conclusion, then the dynic equivalent of C,H,, minus that for C,H, is equal to the dynic equivalent of 3H, ; similarly, from the other members of the benzene series we get the values for 3H,, the mean result being 1:29 or °43 for Hy. The accepted structure for C,H,, diallyl is (CH,CHCH,),, or four whole CH, groups and two CH, groups with H removed from each ; and as the dynic equivalent of C,H,) is 5:6, we find that of H, to be -4. Again, recent investigations on the ter- penes (Wallach, Ann. der Chem. cexxy., ccxxvii., cexxx.; Briihl, ecxxxv.) show that the two ordinary forms can have their for- mule written CH;C;H,;(CH,).(CH).0, ; that is to say, they have 6 hydrogen atoms cut out of CH, groups, and as the dynic equivalent of CjoH,, is 9 we have that of 3H, as 1:0 or that of H, °33. Since the value °43 is derived from 10 accordant members of the benzene series, we will take it as the value of the dynic equivalent of H, in CH,. By similar but simpler reasoning the dynic. equivalents of Cl, Br, I, and other radicals are easily found, and the following is a list of mean values :— Laws of Molecular Force. Taste XXVI.—Dynic Equivalents. 269 CH,. 1a C. C"O'. O'. NETS. CN. 1-0 215 ‘OT 1-9 6 1-23 1:35 NO; CNS. s’, Cl. Br. I. 2:2 2°85 16 13 1-6 2°3 To illustrate the applicability of these values, I furnish a comparison of the values calculated by means of them for twenty substances with the values tabulated in Table XXV. TABLE XXVIII. Comparison of calculated and tabulated Dynic Equivalents. Cale. OREN? ess botetedas 4°8 (Ch dee a ee 88 (C518 1. C) eee area ean 4°3 Cab 6 aa eee 6:3 CREB ry fee sce.cs bce 36 O15 1531 3) a ae eee 6-6 OA8)S Ree 4:3 a kcces..: US JNUE GTO & Banepa 4:23 INH SEN Sei 6°23 Cale. Tab. Jager 5:35 53 a ee, 56 56 4°85 48 SEWARD 2°6 26 eee 66 6:5 i et 78 (Nl Be We 52 54 Ee 5:3 51 Sanaa ee 4:9 4-9 SETAE 79 79 If we now look at the dynic equivalents of the uncombined elements given in the first part of Table XXV., we may notice that they are remarkably small compared to the values in the combined state ; thus, that of H, is ‘04, of N, -205, of O, "195, and that of CH, is small too, 35, instead of 1 as it should be, seeing that CH, is the first of the paraffin series. Other typical compounds have small values : CO, has 1s 05, while CO”O! in more elaborate compounds has a value 1° 9, C,H, has 1, while C,H, has 2; and so on. been noticed in connexion with the molecular refraction of The same fact iis some of the typical compounds and some of their immediate derivatives, and it will yet prove a most important one in chemical dy namics. But meanwhile it is of greater importance 270 Mr. William Sutherland on ae for present purposes to notice that the dynic equivalents given for various radicals in Table XXVI. are closely proportional to their molecular refractions. 12. Close parallelism between Dynic Equivalents and Mole- cular Refractions.—As is well known, there are two methods according to which the molecular refraction is estimated, the first by means of Gladstone’s expression, (n —1)M/p, where n is index of refraction; the other by means of -Lorenz’s, (n? —1) M/(n? + 2) p. In a brief paper (Phil. Mag. Feb. 1889) I showed that the experimental evidence taken as a whole is in favour of the Gladstone expression, for which also a very simple theoretical proof can be given ; and, further, it was shown that it is best to measure (n—1)M/p if possible in the gaseous state. But as comparatively few measurements have been made on bodies in the vapour state I suggested that, as the Lorenz expression had been empirically proved to give more nearly the same value in the liquid and vapour states of a body, its value as determined in the liquid state and multiplied by 3/2 could be taken as giving the value of (xn —1)M/p in the vapour state. The result of the theoretical argument was that, if M/p is taken to measure the molecular domain wu, and if U is © the volume occupied by the molecule in the same units, and N is the index of refraction for the matter of the molecule, then (n—1)u = (N—1)U. Landolt, Briihl, and others have determined the values of the atomic refraction for several elements (Ann. der Chem. cexiii. p- 235), and by means of these and Masini’s data for sulphur (Wied. Sezbl. vi.) and Gladstone’s latest determinations (Journ. Chem. Soc. 1884), I have obtained the values of the refraction-equivalents of the preceding radicals in terms of that for CH, as unity. Mascart has given (Compt. Rend. Ixxxvi.) values of the refraction of a number of substances in the vapour state, from which, for the sake of comparison, I have calculated the refraction-equivalents for as many radicals as possible. The following Table contains in the second column the dynic equivalent, in the third the refraction-equivalent caleu- lated according to the Lorenz expression, in the fourth the refraction-equivalent calculated according to the Gladstone expression from Mascart’s data for vapours, and in the fifth that calculated by Gladstone from liquid data. The value for CH, in every case is 1. E Laws of Molecular Force. — 271 | Taste XXVIII. Comparison of Dynic and Refraction Equivalents. 1 2 3. 4 5 GH te 10 1-0 1-0 1-0 LT eile ‘215 | 28 19 17 eee a Aled ‘BT 54 62 66 BOLO: ot icae 1-9 1-4 15 15 (ae 6 35 4 37 1: 3 gelesen ae i 8 el need cl ied fase 1-01 oo eee P35) oh 1-18) oles 1-2 i eee 2-2 OT audd don 1-9 BW Nes ne DOG ete bees: 3-0
. Mr. William Sutherland on the We see that the ratio is small for the uncombined ele- ments and CH, and C,Hy,, a result of the important fact that while the refraction-equivalent of a non-metallic element is almost the same in the uncombined state as in the combined, the dynic equivalent is much smaller in the uncombined state of an element. The meaning of this fact will be discussed later on ; connected with it is the fact that the ratio for most of the typical compounds in the last table is notably less than unity. A molecule has to reach a certain degree of com- plexity before the summative law holds as regards its dynic equivalent ; the same may be said about its heat of formation. Further comment on the connexion between dynic equivalent and heat of formation must be deferred for a little. We can now give a formal enunciation of the law of the virial constant :—If the molecule of an organic compound is of a degree of complexity higher than that of the ordinary typical compounds, then the virial constant for one gramme of the compound is given in terms of the megamegadyne, gramme, and centimetre as units by the relation Ml = 68 +6682, where M is the usual molecular weight of the compound, and S is the sum of the dynic equivalents of the atoms in its molecule (measured in terms of that for CH, as unity). According to the law of force 3 Am?/r*, Am? is propor- tional to M?/ and therefore follows the same law. 13. Return to the Discontinuity during Liquefaction of Compounds and proof that it 1s due to the patring of Molecules. —The interpretation of the form of the internal virial expres- sion above the volume & is of the highest importance in the theory of molecular force, and can now be attempted in the light of the law for M7/. If the molecules of a substance do pair to produce an actual chemical polymer of it, then its molecular mass changes from M to 2M, while S the dynic equivalent changes to 2S, and consequently l or (68+°66 8?) /M? changes to a value given by ’ = (68/2+°668?)/M?. When § is small we see that the pairing of molecules to pro- duce a polymer causes the virial constant (for one gramme) to diminish to nearly the half of its value for free molecules ; when 8 is larger this statement becomes less exact. In the Laws of Molecular Force. — 273 ease of CO,, for example, if from Table XXV. we take 8 as 1°05, then l="00367 and’ U’=-00206, but in the case of ethyl oxide, with S=4'5, [="00738> and, —/7==:00491. In both cases we see that the pairing of the molecules to form a new chemical compound or polymer is attended with a reduction of the virial constant towards one half, but not exactly to one half of the original value. Now the data given in Tables I. and ILI. and the form of virial term taken to represent them, //(v+), along with the fact that below volume & the form is //2v, mean that in the limiting gaseous state the virial term is practically d/v, just as below k it is //2v ; hence we must regard the pairing of the molecules to be such as to cause the virial constant to become one half of its higher limit—in other words, the pairing must be different from polymerization. We are therefore led to differentiate the chemical and physical pairing of molecules by the statement that while chemical pairing alters the virial constant in the ratio (68+°66 8?)/(128+2°648?) or (14+°118)/(2+°448), physical pairing alters it in the ratio 68/128. or 1/2, The term °66 S? would thus appear to have a certain chemical significance. And now as to the form //(v+) connecting the two ex- treme cases. We can explain it in the following manner :— It will be shown when we come to treat of solutions that if a salt having a parameter of molecular force 3A (proportional to its virial constant /) is dissolved ina solvent with parameter 3 W so that there are n molecules of salt to one of solvent, then the solution behaves as if it consisted of molecules having a parameter 3 X given by the singular relation X= (W-4+nA“)/(L +7). Now, in a gas being compressed towards the volume f, let us assume that there are a number of pairs of molecules propor- tional to & and a number of single molecules proportional to w—k, and that the same relation applies to the mixture of paired and single molecules as to the solvent and salt in a solution, then, replacing W by J and A by //2 and n by 274 Mr. William Sutherland on the k/(v—k), we get for the reciprocal of the virial constant of the mixture ia( beets (relat ee X=lv/(v+h), and therefore the virial term is //(v +h). This would be no demonstration of the pairing of molecules in compounds, if we did not already have it proved in the case of the elements that the virial term varies inversely as the volume at all volumes. Remembering this we can accept our form //(v+k) as indicating the existence of a mixture of paired and single molecules, the number of pairs at volume v being to the number of single molecules as k to v—k. The form of the energy term, 2k RT (i+), must also be partly determined by this existence of pairs, but it would be foreign to our immediate subject to attempt to investigate it. 14. Brief Discussion of the Constitution of the Alcohols as Ligquids.—To learn a little more on the subject of pairing, it will be of some profit to consider briefly here the alcohols and water, which so far have been left aside, after having been proved in Table XII. to follow in the supracritical region a different law from the usual one. But also in the liquid state the alcohols and water, while conforming to the general liquid laws in many respects, are still exceptional in others. Thus Hotvos (Wied. Ann. xxvii.) has shown that the alcohols will conform to his generalization if at the lower range of tempe- rature, from 20° C. to 170° C., the molecules be considered complex (double relatively to ordinary liquids) and water also conforms if from 100° upwards its molecules be con- sidered double ; the molecular lowering of the freezing-point of water produced by the solution of bodies in it as measured by Raoult and compared with the molecular lowering for other liquids proves that relatively to these the molecule of ~ water is double. Taking all the facts into consideration, it seems to me that the alcohols and water may be assumed, in the liquid state, to have the pairs of molecules again paired, the second pairing, however, not being of so intimate a nature Laws of Molecular Force. . 205 as the first, consisting of a mere approximation of the first pairs without any change in the values of A or of J. According to this assumption we should expect the beha- viour of the liquid alcohols to be represented by a form similar to our infracritical equation, and we will assume _ Rr VT 3) fs jg R'T(1+ Rie aw Goal Dy where R" is about 2R. It was on the infracritical equation that: our second method of finding M?/ was founded, giving the relation which can be applied to Amagat’s data (Ann. de Chim. et de Phys. sér. 5, t. xi.), and Pagliani and Palazzo’s (Wied. Beil. ix.) for the alcohols. Again, our assumption enables us to apply the fifth or eapillarity method of finding M2 to the alcohols, if only we remember that the molecular domain becomes twice as large and its radius 2° as large as it would be with only one pair- ing; hence the equation for the fifth method becomes for the alcohols l= cav'/(2m)3. Schiff’s data are available. As the latent heat and critical temperature are largely dependent on the supracritical equation, we ought not to expect the formule for M?/ furnished by the third or latent- heat method and by the fourth or critical-temperature method to apply to the alcohols. But as the relation Mx = 19-4T,, or, empirically, MA = odes which was deduced in the dideuudl of the third method, does apply approximately to the alcohols, the constant being 6, we may as well, for purposes of comparison, see what the formule of the third and fourth methods give in the case of the alcohols. 276 Mr. William Sutherland on the TABLE XX X.—M2/ for the Alcohols. Method ...... Second. Third. Fourth. Fifth. Methyl .0..-<0.0-: 8 22 (11) 17 AS) 9:4 13; sh eager aneeeeoc 14 38 (19) PAL) 176 Propyl “..s)jn. These equations ought to give the same values of A~! what- ever the strength of the solution may be; and herein lies a first test of the truth of the principles involved. The following values of cA for NaCl are calculated from Volkmann’s data (Wied. Ann. xvii.) for its solution in water at 20°; w is taken as 18, although we consider the water molecule to be complex, but this does not affect the purely relative comparison being made :— ait ahs "105 084 "052 (35 ‘017 cA! . ° 1°34 1°38 1°47 1°46 4:42 Considering that the solutions range from saturation down to considerable dilution, the approach to constancy is satis- factory; but it will be noticed that, on the whole, there is a tendency for the value of cA—! to increase with diminishing concentration, and this same phenomenon is to be seen in the case of almost all Volkmann’s solutions, most pronoun- cedly in that of CaCl, :— eT Se eee ‘O91 "068 ‘O41 ‘O21 ‘O11 GRE) fe PeN 2A 2 op ZG 2°95 Ae & This case shows us that there is a certain amount of incom- pleteness in our theory of the capillarity of solutions, as indeed we ought to be surprised if there were not, when we try to apply our arbitrary definition of the molecular mass of a solu- tion to one which contains 56 parts by weight of CaCl, to 100 of H,O as the solution for which n=*091 does, and also when we assume that the concentration in the surface-layer is the same as in the body-fluid at all strengths up to saturation. If our object were an exhaustive representation of the connexion between the surface-tension of a solution and its concentration, it would be easy to introduce a slight empirical alteration into the above equations to make them exhaustive. For instance, ae Laws of Moleculur Force. 279 we might imagine that the effective value of W in a solution experiences a small change proportional to the concentration ; but the equations as they stand will prove to be sufficient for our purpose if, in comparing solutions of different substances, we calculate cA! for the same value of 2 throughout. In all. subsequent calculations n=18/1000. The experi- mental data for surface-tensions of solutions are abundant, the chief that I know of and have used being those of Valson (Compt. Rend. \xx., lxxiv.), Volkmann (Wied. Ann. xvii.), Réntgen and Schneider (Wied. Ann. xxix.), and Traube (Journ. fiir Chem. cxxxix.). The following Table contains the values of cA! for a certain namber of compounds, the surface-tension being measured in ‘rammes weight per linear metre and the half molecules of the salts of the bibasic acids being regarded as molecules. TABLE XX XI.—Values of cA. ior Br pcCk NO. POH: sO, 400, ib. S Gaetan 4°15 | 2°46 "83 | 161 83 | 161 Sich, oe SO0e p22 tr) 670), |, ode | 2. | 145 oe 4°74 | 3:06 | 1:45 | 2:30 | 1:37 | 2:30 | 1-95 ik ae 4:99 | 3:31 | 1-78 | 2:55 | 1-71 | 2-72 | 2-21 The study of this table brings out the fact that the differences of the numbers in any two rows or in any two columns are constant: thus the differences for the iodide and chloride of the four bases are in order 3°32, 3°29, 3°29, and 3:21, while the differences of cA—! for the Na and Li salts of the mono- basic acids are in order *59, °60,°62,°69, and °54. Accordingly each atom contributes a certain definite part to the value of cA for the molecule in which it occurs, and that part is independent of the other atoms in the molecule. I shall call this part the parameter-reciprocal modulus of the atom ; we have not at present sufficient data to get its absolute value in any case, but if we make Li our standard positive radical, and Cl the standard negative, we can calculate the average values of the difference between the parameter-reciprocal modulus of a radical and its standard,—thus in the case of iodine this difference is 3°28, and in the case of Na ‘61, and so on. Before tabulating these mean values I will give the values calculated for the salts of some other metals with the values for the same salts of Li subtracted. 280 Mr. William Sutherland on the TABLE XXXII. I Br Cl NO,. | 480, ob een ne Re 39 35 53 MGe ai... 632: 44 73 67 DD s ar Gi ce ¥ 1-67. | Smt Ba tae Vee 249 | 2:52 I7n j= liad. 1-35 2 1:33 10d ab bes 224 | 242 | 215 2:29 Min = lui c...s 1:17 93 | 12 To these we may add the following values, cbtained from the sulphates 3Fe—Li 1:27, 3Ni—Li 1:19, $Co—li 1:15, 4Cu—Li 1:49, JAI—Li *6, Fe, —Li *5, and 4Cr,,— Li 1:0; and the two following from the nitrates Ag—lLi 3°91, and 4Pb—Li 4°51. The following Table contains the values of the parameter- reciprocal moduluses of the different metals minus that for Li and of the negative radicals minus that for Cl. Tapia XXL. Mean Values of Parameter-reciprocal Modulus for the Metals with that for Li subtracted. | Na. K. NH. | 3Mg.| $Ca. | 4Sr. | 4Ba. 6L | 90 |—15] 42 | 6 Rhy a ae { 1:33 | 2:3 12 ] Pree . | $Ni. | 4Co. us | Ag. | 4Pb. | 2Al. ee ere 2 Ail | | 1:27 | 1:2 Hy 1:5 39 | 45 | 6 The same for negative radicals with that for Cl subtracted :— ie Br. NO,. On. / 380/59 apes 3°28 1°56 “81 ‘04 “86 “46 It may be worth mentioning that these differences show a pretty close parallelism to the corresponding differences of the atomic refraction given by Gladstone (Phil. Trans. 1870) but not close enough to be worth dwelling on. In the case of the organic bodies studied there was nothing analogous to this singular property possessed by these inorganic¢ compounds of having the reciprocal of the parameter A of molecular force separable into a constant and definite parts ~ Laws of Molecular Force. — 281 contributed by each constituent of the molecule. Thus we have characteristic of inorganic bodies in solution another of those properties called by Valson modular, who discovered that the density, capillary elevation, and refraction of normal solutions (gramme-equivalent dissolved in a litre of water) could all be obtained from the values for a standard solution such as that of LiCl by the addition of certain numbers or moduluses representing invariable differences for the metals and Li and for the negative radicals and Cl. Other properties of solutions have since been proved to be modular, as for instance their heats of formation from their elements and their electric conductivities. I think the modular nature of some of these properties of solutions is the outcome of this modular property in the parameter reciprocal of molecular force along with the additive property in mass. To prove this in the case of density would require a special investiga- tion, but if we assume the property for density we can easily deduce Valson’s result that the property applies to capillary elevation. Let h be the height to which a normal solution of any salt RQ rises in a tube of radius 1 millim., then hy poke HDR h=2a/p=2Xpi( ats Je. Let r and g be the density moduluses of the radicals R, and Q, being small fractions, then p=d+r+q where d is a con- stant nearly 1 ; also X1=(Wt+nA)/1+n), so that l+n (wknp\? n= 2( way naa )atr+ gyi ro |. Remembering that in the case of a normal solution n is small, being 18/1000, we can develop the last expression in powers of n as far as the first ; and it is evident that as p the mole- cular mass possesses the additive property and A~! possesses the modular property, then 4 must also possess the modular property, which is Valson’s result. 16. Second method of finding the virial constant for inorganic bodies or solid bodies in general from the properties of their solutcons.—In this method the compressibility of solutions is used. Ifa solution could be treated as an ordinary liquid we might attempt to apply the equation of our second method for liquids, namely, PyeG: AOi a a= 3(%% + gg rel 3 but as the solutions to be dealt with are all aqueous, and as a Phil. Mag. 8. 5. Vol. 35. No. 214. March 1893. U 982 | Mr. William Sutherland on the for water at ordinary temperatures is quite abnormal, it would be useless to attempt to apply this equation to them; but from the “ dimensions” of the physical quantities involved in it we may make it yield a correct form of empirical equation for solutions. If we neglect the small term 25R/26, and also the difference between v and v, at ordinary temperatures, the equation above suggests the simple form / varies as 1/up?, that is X-! varies as wp”, say KX~1=yp*, where K is a constant, and for water KW-!=y,, the compressibility of water, and as before we have X-t=(W-!+nA7})/(l+n). But on account of the rapid alteration of the compressibility of water with pressure, and its anomalous variation with temperature, we must be prepared to admit that the part of the com- pressibility of a solution due to the water in it is altered from its value in pure water, and is more altered the more the water is compressed in the process of dissolving the salt. Let this compression be measured roughly by the total amount of shrinkage that ensues when 1 molecule of salt is dissolved in 1000 grms. of water, call the shrinkage A, and let us amend the equation given above to KX~!=ypp?+/(A): Let suffixes aand 6 attached to symbols refer them to two different bodies, then , KX —KXs*=1,p2— Papi +F(A,) —7(4,); ut KX7!—KX1=Kn(A7!—A;,1)/A +n), oe Kn(Apt— As*)/(L +2) = ape— Hops thAa) — F(A»). Hence selecting pairs of bodies for which A,=A, approxi- mately, we ought to get “,p7— @,p; proportional to cA7*—cA;*, the values of the last expression being obtainable from Table XX XI. To facilitate the comparison I furnish the following broad statements about A founded on the study of data as to the molecular volumes of salts, both solid and in solution, given by Favre and Valson (Comp. Rend. Ixxvii.) Long (Wied. Ann. 1ix.),and Nicol (Phil. Mag. xvi. and xviii.). The modular property applies approximately to shrinkage on solution ; the shrinkage of a gramme molecule of LiCl is 2, and the shrinkage for : gramme molecule is increased when for Li is substi- tute K. Na. NH; _ 30a, 38r, $Ba. by-o' ‘i —d 10 {h 127s and when for Cl is substituted Br. i NO,. - 180, 2oe" by 0 0 0 8 14, Laws of Molecular Force. 283 After giving the values of up? in the next table we can pro- ceed with the comparison. TaBLE XX XIV.—Values of 10"pp?. cna) aa i We ENO gl SO ACOs Ms. | Soc ciae- 432 484 541 457 433 Witte he oe ..| 441 496 550 468 444 498 LC 454 507 557 480 450 437 ELS 443 493 544 466 449, Or ian 464 Soe ae 497 so 521 Lhe experimental data used are those of Rontgen and Schneider (Wied. Ann. xxix.), and those of M. Schumann (Wied. Ann. xxxi.) for CaCl, SrCl,, and BaCl,, in the case of which I calculated the compressibility for the half-gramme molecule according to his result that w—p,,=cp where p is percentage of salt, using a value of ¢ got from the more con- centrated solutions. An inspection of this table shows that 10’yp? possesses the modular property; it gives for instance the following dif- ferences for Na and Li, 9, 12,9, 11,11, with a mean value 10, and so on for the other metals; the mean values for the metals minus that for Li are :— Na. K. NH,,. Ca, iS8r. Ba. 10 20 8 32 65 89 ; and for the negative radicals minus that for Cl :— Br. L NO, 380, 300,. 52 105 25 0 —15. We can now select pairs of bodies for which A, =A, and test if {1,07 —[,0; is proportional to cA '—cA>1. The following are pairs of elements ands acterized by nearly equal shrinkage on solution with the values of the differences of 10’up? and of cA~ and also their ratio. TABLE XXXV. HKqual shrinkage pair...| K,Na. | Sr, $Ca.| 3 Ba, $Ca. | Br, Cl.| I, Cl. —_—_~—- - Mean diff. of 107up?...| 10 33 57 52 105 Mean diff. of cA~?...] 29 1:05 1:85 | 1:56 | 3:28 Ratio of differences ...} 34 3l 31 33 32 984 Mr. William Sutherland on the The agreement here is excellent, as will be seen more clearly if we compare bodies not having equal shrinkage, as K and Li, for which we get the 10"up? difference 20, the cA~* diffe- rence ‘90 with a ratio 22, or K and NH,, for which the two differences are 12 and 1:05 with a ratio 11. The agreement above is a verification of the theory of the compressibility of solutions, here barely outlined, and the equation 10°(4,p2—Myp;) =32 (cAZ!—cA;") when A,=A, nearly constitutes a second method of getting values of cA~1; but we will not use it, as it adds no bodies to our list. It suffices to have partly verified the principles on which the first method is founded by their application to quite another physical phenomenon, and especially the principle involved in the remarkable equation X—1=(W-!+nA)/(1+72). With the values in Table XXXITI. and that for LiCl, namely, 83, we can obtain the value of cA—! for any salt whose con- stituents are to be found in the table, or we can if we like use the actual values in Tables XXX. and XX XI1.; we can then cal- culate M?/cA—, which is proportional to M*/, or M77=CM*/cA—, where C is a constant. To connect the values of M?/ thus found with those previously given absolutely in Table XXV., we must find the value of C/c, which we can proceed to do in the following manner :— We have seen (Section 14) that we had better regard the molecule of water as doubled relatively to that of ordinary liquids, and as we have shown that the molecules are paired in ordinary liquids the molecules are doubly paired in water ; but it was suggested that the second pairing of the pairs was not attended with any alteration in the parameter of molecular force, and that the only effect of the second pairing was to make the radius of the molecular domain of water 2? as large as if water were an ordinary liquid. And, again, in the case of solutions the surface-tensions have been measured at about 15°C , whereas for comparison with our previous work they ought to have been measured at 2T,/3, which for water is about 150°C. At this temperature the value of the surface-tension of water reduces, according to Hitvés, to about °6 of its value at 15°C. Hence the equation, which treating water as an ordinary liquid and at 15° we wrote a, = Wwi/c, ought for double pairing and at 150° to become ‘6a,—=W23w#/c, and similar statements hold for the equation for «; so that values Laws of Molecular Force. — 285 of W, X,and A, as deduced from measurements at 15°, ought to be reduced by the factor ‘6/23, or 1/2, to give the desired values. Now in the case of homogeneous liquids in the equation l=cav*/m? giving 1 in terms of the megadyne we found a value 5930 for c/2, with the megamegadyne as unit of force c/2=00593; and we can use this same value in the case of solutions after we have halved our values of A, or doubled those of cA—! so far given ; hence using the values of cA so far given we get M*/=:00593M?/cA—1. Fortunately, a test of this argument is made possible by means of Traube’s data for the surface-tension of solutions of certain organic acids and sugars, for which the values of ‘00593M?/cA— are given in the following Table, as well as values of S found by the relation M?/=6S (the term ‘668? being omitted), and also values of S calculated from the dynic equivalents in Table XX VI. TaBLeE XXXVI. Oxalic Acid.) Citric Acid. Glycerine. | Mannite. (COOH),. |C,H,OH(COOH),.) C,H,(OH),.) C,H,(OH),. We ae es hove on gelo ds 19-4 43°5 33°5 63-0 Sa MPYIG. oa cees ss Be "2 56 10°5 S from dynic equiv. 4:2 9°7 5:0 10°0 Tartaric Acid. Dextrose. | Saccharose. C,H,(OH),(COOH),. | C.H,.05. | Ci.H»,0)). -| JU U) nee 6c eget On ee eee 389 721 112°5 IME OP eae retshi sa.ceeses ss 65 12:0 188 S from dynic equivalents 74 9-6 18:1 The agreement between the two sets of numbers is not all that could be desired, but it is good enough to show that the only part of M?/ effective in a solution is the linear term in M*%=6S+°66S?; and we have already seen that when the molecules of ordinary liquids pair during liquefaction the term ‘66S? is inoperative in the process, so that there is a certain resemblance in the relations of two paired molecules and those of solvent to those of substance dissolved. Returning to the inorganic compounds we can now tabulate the absolute values of M2l, calculated according to the rela- tion M7/=:00593M?/cA—. The manner of calculation is best illustrated by an example, say for KBr; first °83 is taken as the value for LiCl, and to it are added -90 and 1°56, taken from Table XX XITI., as the differences for K and Li and for 286 Mr. William Sutherland on the Br and Ol; the square of the molecular weight of KBr is divided by this sum and multiplied by -00593 to give the tabulated value of M2/ in terms of the megamegadyne. From the value of M2/ thus found the dynic equivalent S is caleu- lated by the relation M2/=6S, which has been seen to be appropriate to values of M?/ obtained from solutions. TABLE XXX V1I1I.—Values of M?/ and 8. Cl. Br. i NO,. 180n S)e 260. M7. S. | Mz. S. | M% S.|M¥%. S. | MW S. (Mz S Li...) 125 29 | 167 3-1) 257 43 171-28 qOGeees Na. ...| 13:7 23 | 208 35 | 28:0 4-7 1.188 3 1)) deems K ...| 185 $1 | 283° 4:7 | 82:4 5-4 | 235 39 | 1725 aaa NH, | 23:0 3:8'| 27-0 4:5) 81:0 52 | 25:0 427) 170m@e iMg | 104 1-7 | 17-7 80] 251 42 | 156 26) toa 4Ca...| 120 2:0 | 19-4 3:2 | 267 451173 29 ASr ...| 142 2-4 | 21:8 3:6 | 293 49] 195 32 3Ba...| 18:8 3:1 | 264 44 | 339 56 | 240 40 Ae Oa Dold gece ote eee? et tn jock: ieee 21 | 40d... 15°7 26 | 23:2 3:9°| 305 51 | 21:0 35 | 162527 4 11° 9G in | 168 eee Sie AgNO,. |3Pb(NO,),.| 3CuSO,. 4FeSO,. | 3NiSO,. IM 30°6 26°3 lS 11°4 12°3 oa Risentisece Bri 4:4 ied) 1-9 20 3CoSO,. sAl,(SO,);. | ¢Fe,(SO,)3. | 4Cr.(SO,),. IMEI bcccsnaen 12°7 89 12°6 9°6 iad Bs aakuree 21 1-5 21 16 The additive principle holds amongst both sets of numbers except in the case of NH,; see for instance the following list of the differences of S for the iodides and chlorides :—2°2, 2:4, 2°3, 2°D, 2°, 2°8, 2°59, 2°5. Now we have already seen that the modular principle applies to cA— (the modular principle applies when a quantity is given by the addition of moduluses to a constant, the additive principle is a special case of the modular in which the constant is zero) ; the additive principle apples to M the molecular weight: hence it would appear Laws of Molecular Force. 287 to be a mathematical impossibility that the modular or additive principle should apply also to M?/cA—!, rigorously ; or, more accurately, if the modular principle applies rigorously to one of the quantities cA~! and M?/cA—! it cannot apply rigorously to the other: but practically we find such relations amongst the numbers that both are approximately obedient to the modular principle. The case of NH, casts some light on the question, for with it cA—! shows the same differences in the values of the chloride, bromide, iodide, and nitrate as with the other positive radicals, while M?/cA—! does not do so: this case would make it appear that the modular principle applies rigorously to cA}, but not so rigorously to M?/cA—}. But leaving out of the count this case of NH,, significant as it is, we can find mean values for the differences of the dynic equivalents of all the metals and Li, and of all the negative radicals and Cl; if we can obtain the absolute value of the dynic equivalent of Li and of Cl, we shall have those for all the metals and radicals. Now from the organic compounds we have already got a value 1°3 for the dynic equivalent of Cl, and hence from the value for LiCl we could obtain that for Li. The value tabulated for LiCl is 2:1, but we can obtain a mean value fairer to all the other bodies by sub- tracting, for example, from the value for KI the mean difference for K and Li, and for I and Cl; in this way we arrive at a mean value 1:9 for LiCl, from which, taking the value 1°3 for Cl, weshould get °6 for Li. But the refraction-equivalents of the halogens are supposed by Gladstone to be a little larger in inorganic than organic compounds ; so that in the light of our previous knowledge of a close parallelism between dynic equivalents and refraction-equivalents it might be safer to assume that the dynic equivalents of Li and Cl in LiCl are in the ratio of their refraction-equivalents in that compound, namely, 3°8 and 10:7. According to this assumption the values for Li and Cl come out ‘5 and 1:4, which we will adopt as true and use in the calculation of the dynic equivalents of the elements given in the following Table. These are measured of course as before in terms of that for CH, as unity, and, again, for comparison there are written along with the dynic equivalents the refraction-equivalents in terms of that for CH, as unity, calculated from Gladstone’s values (Phil. Trans. 1870). 288 Mr. William Sutherland on the TABLE X XXVIII. Li. | Na. | K. | $Mg.| 3Ca. | 2S Pete ee | | | | Dynic equivalent ...... te 3D ‘Sh AGG ‘3 | 758 ‘9 | 4) Refraction-equivalent.. °5 63| 1:06] -46-| -68 | ‘90 | 1:04 ‘674 | = i i Ag. | 4Pb. | 3Cu.| $Mn. | 3Fe. | Dynic equivalent ...... 2°70 | 20 6 "5 6 xf 8 >| 8 76) 8 | +80 1) 5690 aga eayaeetoos Refraction-equivalent .. 2:06 1-63 4Cr.| Cl | Br. | ZL | NO, | 480,|400,.|4Cr0,. Dynic equivalent ...... 3 | 141 27 | 88 | 23 | 135 Refraction-equivalent.| °7 14 | 90°71 3:6" | 9-6 eee | | i Again we see a remarkable parallelism between the dynic and refraction-equivalents of the elements and radicals. Of course there are refinements which will yet have to be made in the calculation of the dynic equivalents, but it is not likely that they will make the parallelism seriously closer. 17. Meaning of the Parallelism between Dynic and Refraction Equivalents, and general speculations as to the volumes of the atoms and their relation to ionic speeds—We are now called upon to consider the meaning of this parallelism which has been demonstrated both for organic and inorganic compounds, and we shall be helped thereto by the very simple theory which I have given of the Gladstone refraction-equivalent (Phil. Mag. Feb. 1889), showing that to a first approximation (n—1l)u = T(N—1)U, where n is the index of refraction and w the molecular domain of a substance, N the index of the matter of an atom, and U its volume in the molecule. Hence the refraction-equivalent of an element is the product of the refractivity (Sir W. Thom- son’s name for index minus unity) of the substance of its atom and the volume of the atom (the volume of the atom being measured in terms of the unit in which the molecular domain, usually called molecular volume, is measured); so that the re- Laws of Molecular Force. 289 fraction-equivalent is a function of the two variables only, namely, the volume of the atom and the velocity of light through it. Now we have seen that the expression M/, as a whole, in one aspect appears to be not dependent directly on the molecular mass M, seeing that M?/ can be represented in terms of certain quantities which we have called dynic equi- valents. Hence, as / is proportional to A in our expression 3Am?/r* for molecular force, we see that in one aspect mole- cular force seems to be not directly dependent on the mass of the attracting molecules; and yet, on the other hand, in con- sidering solutions we found that the quantity A asserted its individuality as separate from the whole expression Am?, so that in another aspect there does appear to be a mass action in the attraction of two molecules. However, regarding M?/ or Am? as a whole, the simplest hypothesis we can make about the mutual action of molecules is that it depends most on the size of the molecules. This would make Am? a simple function of U; so that the dynic and refraction equivalents would have this in common, that they are both simple functions of U. Suppose, now, that the velocity of light through all matter in the chemically combined state is approximately the same, or that N is approximately the same for all atoms as constituents of compound molecules, then the refraction-equi- valents given by Gladstone are directly proportional to the volumes of the atoms in the combined state, and then the parallelism between dynic and refraction equivalents would mean that 8 is nearly proportional to the volume. It is very interesting, therefore, to inquire briefly whether there is any evidence to prove that Gladstone’s refraction-equivalents are proportional to the volumes of the atoms; and I think that in Kohlrausch’s velocities of the ions in electrolysis we have such evidence. If different solutions, such as those of KCl, NaCl, or 4BaCl, ere electrolysed under identical cireum- stances, then we know, according to Faraday’s law, that each atom of K and of Na, and each half-atom of Ba, may be considered to receive the same charge, so that they acquire their ionic speeds under the action of the same accelerating force. Accordingly, the ionic speed characteristic of an atom is reached when the “ frictional” resistance to its motion is equal to this accelerating force ; hence the “ frictional ”’ resistance is the same for all atoms, or rather for all electrochemical equi- valents. Now the “ frictional ” resistance will be a function of the velocity of the atom and of its domain (atomic volume) and of its actual volume as well as of the domain and actual volume of the molecule of the solvent; but if water is the solvent in all cases, the only quantities which vary from body 290 Mr. William Sutherland on the to body are the velocity and the domain and volume of the ions, so that we can say “ frictional” resistance = $(V, u, U), v V = F(u, U). Now the simplest connexion that one can imagine between the velocity and the domain and volume of the ion is that the velocity will be greatest when the free domain or the difference between the domain and the volume is greatest, or, to be more general, when the difference between the domain and some multiple of the volume is greatest; but if N is the same for all combined atoms, then U is proportional to the refraction-equivalent g. Hence the form of F is such that it contains w—ag, where a is a constant. On studying the experimental data I found that a might be considered unity, and that V is a linear function of w—q. There is a little difficulty in determining with accuracy the domain of an ionic atom in a solution. Nicol, in his work (Phil. Mag. xvi., xviii.) on the molecular domains of inorganic compounds in solution, has confined his attention almost entirely to differ- ences of domains, making the assumption suitable to his purpose that the inolecular domain of water is unaltered in solutions, whereas we should expect that the greater part of the shrinkage occurring on solution of an inorganic crystal happens in the water, which is far more compressible than the crystal. Accordingly I take the molecular domains of salts in the solid state, as given by Long in his paper on diffusion of solutions (Wied. Ann. ix.), as nearer to the true domain when they are in solution than Nicol’s values ; but to allow to a certain extent for the change of state on solution, I have assumed that in each case the water experiences four fifths of the total shrinkage and the dissolved salt one fifth. This is an arbitrary adjustment, and is of no material importance to the comparison to be made except as showing that the point has not been over- looked. In the following Table are given under wu the mole- cular domains, under g the molecular refractions (Gladstone’s), in the next column their differences, under & the specific mole- cular conductivities determined in highly dilute solution by Kohlrausch and shown by him to be equal to the sum of the velocities of the ions in each case. These are taken from his paper (Wied. Ann. xxvi.), with a few additions from an earlier one (Wied. Ann. vi.). Under & (calculated) are given values of the conductivity calculated from the equation k = 684+2°2 (w—g), 7 Laws of Molecular Force. 291 expressing the linear relation between conductivity or sum of ionic velocities and u—gq. TABLE XX XIX. U. q. uUu—q. k. X (cale.). AU een tees» 3 =i 53°5 39°3 18 107 108 ERE fi. esses 44 25 19 107 110 Lh a oee eee 36 18°8 iby 105 105 Shoe 41 32 9 87 88 1 (C151? deen poeR ee 32 21°7 10 87 90 ite OW ee roe 24 155 8:5 87 87 BG ine 55.2 5000 20°5 145 6 78 81 £MgCl, .....005. 20 14 6 80 81 2 02) 0: Lear 22 16 6 81 81 He 0] Ree 24 17-5 6:5 83 82 PCL, wowosina' 24 186 D4 86 80 22/710 Ul ule paeeeee 23 15°8 7 17 83 The agreement is here such as to prove a true connexion between conductivity and u—q, the more striking as no relation can be seen between conductivity and wu or q taken separately. The only bodies I have omitted from Kohlrausch’s latter list are the nitrates of some of the above metals and of silver, the hydrogen compounds of the halogens, and the ammonium compounds. These do not give results in harmony with those in the last table, and, indeed, we should hardly expect a compound radical like NO; to experience frictional resistance in the same manner as a single atom like Cl, and as to the hydrogen compounds they form a class by themselves with respect to many physical properties. It will be as well to show the amount of departure in these cases in the following Table :-— U. q. u—4. k. K (eale.). ASS ists’ pss 56 26 30 327 134 Teg) ere anaes 50 16 34 327 142 RG 2? earee snes 42 11 dl 324 136 KEN 53 72. as 47 22 25 98 123 NINO N 8 oat se 36 19 17 82 LOD INIEMINO Do Buccs 475 25°5 22 98 L116 iis L(G) ie areas 35°95 22-2 13 104 97 Kohlrausch has pointed out that there is some difticulty in determining the true connexion between ionic velocities and conductivities in the case of the bibasic acids SO, and COs, so that we must leave them out of the count for the present. 292 Mr. William Sutherland on the 18. An Attempt to Determine the Velocity of Light through the substance of the water-molecule.-—In spite of the excep- tions, the relation demonstrated in Table XX XIX. is suffi- ciently striking. To explain it, let us replace g by its value (N—1)U ; then, in interpreting the expression u—(N—1)U as occurring in our expression for the conductivity of a solu- tion, there are two methods of procedure: first, we can assume that w—U, the free or unoccupied part of the domain, is the most likely to occur, in which case N=2; second, that w—cU occurs in the expression for conductivity, and that ¢ happens to have the same value as N —1, on which supposition it would be desirable to determine N. .At present I know of only one way of attempting to find N or v/V, the ratio of the velocity of light through free ether to its velocity through the matter of an atom, namely by means of Fizeau’s experiment, repeated by Michelson and Morley, on the fraction of its motion com- municated by flowing water to light passing through it. Exactly in the manner of my paper (Phil. Mag. Feb. 1889, p- 148) we can estimate the effect of the motion of matter on the light passing through it. Let s be the distance travelled by light in water flowing through the ether at rest with a velocity 6 in the same direction as the light, v the mean velocity of light through the flowing water, v' the mean velocity through still water, v its velocity through free ether, V through a molecule of water, J the mean distance through a molecule, and a its mean sectional area ; then the total loss of time experienced by a wave of unit area of front or a tube of parallel rays, or, briefly, a ray of unit section in passing through the matter-strewn path s instead of a clear path in free zether, will be equal to its loss in a molecule multiplied by the number of molecules passed through in the path. This number, when the matter is at rest, is proportional to s, to a, and to p/M, or it varies as sap/M ; but when the matter is in motion it is reduced in the ratio 1—6/v": 1. The loss of time in each molecule is found thus: J/V is the time taken to pass through a molecule, and in this time the molecule moves a distauce 1/6/V and the unit wave-front moves a distance (1 + 6/V), which in free ether would take a time /(1+6/V)/v ; so that the loss of time in a molecule is 1/V—/(1+8/V)/2. Hence, the total loss of time in the path s may be written ) ksalp (1 Lea 1 3) abe) ge But the loss of time is also s/v!—s/v; equating the two ex- Laws of Molecular Force. 293 pressions and putting M/p=u and al=U, v/v"=n", o/ V=N we get | u(n!’—1) =U(N-1 _ “x )(1— en as k& is equal to 1, seeing that if 6=0 and U=w, then N must be equalto x. This equation is the companion to that for still matter, namely, u(n—1)=U(N—1). But to allow for deformation of the wave-front in passing through molecules it was shown (Phil. Mag. Feb. 1889, p- 150) that this first approximation might be altered to the form u(n—1)=U(N—1) +09, where ¢ is a constant, and this form was verified, so that we may write u(n!!—1) =U(N-1- °N) de ° nt + cp 5S & N Of, neglecting the term in 6? ; ; ws N as u(nl!—n) = —" U(N—1)(x oa +n") een UCN!) nee ON pee ed N" i os Ou(n—)) in ay) +n}. Now Mice Ted =U; vd xO MUR ah Galareaiue approximately, where z is the fraction of the water’s velocity imparted to the velocity v’ to change it to v’. Fizeau (Ann. de Ch. et de Phys. sér. 3, t. lvii.) found a value °5 for 2, while Michelson and Morley (Amer. Journ. Se. ser. 3, vol. cxxxi.), ina more extended and accurate series of experiments, found a value e="43+:02, which we will adopt. U(N—1)is equal to w(n—1) measured in the vapour of water, for which Lorenz (Wied. Ann. xi.) gives the value 5°6; the value for water at 20° C., according to his data is 6, and n is 1:333, which may also be taken as the value for n” where it occurs ; all these values being substituted in the equation ING) edt odie 4») 6 (i= ht) Noten, Und), - ) i! 294 Mr. William Sutherland on the give the value N=9. Hence the velocity of light through the water molecule appears to be one ninth of that through free ether. But before we could ascribe any degree of accuracy to this estimate we should need to be surer of the value of 2, whose measurement is attended with great experi- mental difficulties. It is much to be desired that we had similar measurements for other bodies than water, both liquid and solid, to permit of other estimates of N, so as to see if it is the same for all compound bodies, and also to decide be- tween the theory here sketched and Fresnel’s hypothesis, that matter carries its own excess of ether with it, so that a= (n?—1)/n?, which in the case of water is ‘437, in excellent agreement with Michelson and Morley’s experimental number ; but one such agreement is not sufficient to establish an hypothesis founded on such artificial grounds. However, if N=9 then N—1=8, and we have the electrical specific mole- cular conductivity k=68+2°2 (u—8U). Itis only a coinci- dence that this agrees so exactly in form with Clausius’s calculation that the number of encounters experienced per second by a molecule of volume U moving amongst a number of others of volume U is greater than that experienced by an ideal particle moving under the same circumstances in the ratio w:u—8U. Further experiment must elucidate the subject-matter of these speculations. 19. Suggested relation between the change in the volume of an atom on combination and the change in its chemical energy. —Returning to the idea that the dynic equivalent furnishes a measure of the volume of its atom, we can get a suggestive glimpse into the relation between the volume of an atom and its chemical energy. Kundt has recently (Phil. Mag. July 1888) shown that the velocities of light through the metals (uncombined) are as their electrical conductivities, being in the case of silver, gold, and copper greater than through free ether, and as in this case both n—1 and N—1 are negative, we see that (n—1)u or (N—1)U for the metals changes greatly when the metals pass from the combined to the free state. Now this is in strong contrast to the behaviour of the non-metallic elements, which have been shown in the case of O, N, C, 8, P, Cl, Br, and I to possess nearly the same values of (n—1)u in the combined and free states, and the same may perhaps be said of H. Again, in contrast to this approximate inalterability of (n—1)w for these non-metals we have the fact, already pointed out, that the dynic equivalents of H, O, and N are much smaller in the free than the combined state. If, then, the dynic equivalents give a measure of the volumes Laws of Molecular Foree. 295 of the atoms in both states, we must consider the volumes of free H, O, and N to be smaller than when they are combined, the change of volume corresponding to the change of energy on combination. [f this is true, then the elasticity and density of the non-metallic atoms (or the equivalents of these proper- ties in the electromagnetic or any other theory of light) are so related that although the density changes (N—1)U re- mains constant, whereas in the metallic atoms the relation between density and elasticity must be quite different, because, as we have seen, (N —1) U actually changes sign in some cases. It would be possible to determine approximate values for the dynic equivalents of the uncombined metals from Quincke’s data for the surface-tension of melted metals, and also to get some light on the constitution of salts from his measurements of the surface-tension of melted salts, but these would be most appropriately discussed in connexion with a general study of the elastic properties of solids. I have, however, satisfied myself that the dynic equivalents of the uncombined metals are different from their values in the combined state. To show the existence of an intimate relation between dynic equivalents and chemical energy we can enumerate the follow- ing propositions :—That in the great majority of inorganic compounds the evolution of heat accompanying the passage of an atom from the uncombined to the combined state is almost independent of the nature of the atoms it combines with, similarly the change of dynic equivalent of an atom on combination is almost independent of the nature of the atom it combines with ; that in organic compounds with the excep- tion of the simpler typical forms the same proposition as this applies both as regards heat and dynic equivalent. These general remarks are intended to indicate the most hopeful direction for the continuation of these researches to open up new fields ; and yet in old fields there is abundance of scope for the application ef the law of molecular force towards the acquisition of a knowledge of the structure of molecules, in the elasticity of solids, in the viscosity of gases and of liquids, in the kinetics of solutions, and many kindred subjects. Melbourne, February 1890. i996] XXVIII. The Fusion-Constants of Igneous Rock. — Part III. The Thermal Capacity of Igneous Rock, considered in its Bearing on the Relation of Melting-point to Pressure. By CaRL BarRus*. [Plate VI.] 1. FNTRODUCTORY.—tThe present experiments are in series with the volume-measurements of my last paper, and the same typical diabase was operated upon. Since it is my chief purpose to study the fusion behaviour of silicates, more particularly the relation of melting-point to pressure, the observations are restricted to a temperature-intervyal (700° to 1400°) of a few hundred degrees on both sides of the region of fusiont (§ 11). 2. Literature—LHxperiments similar to the present, but made with basalt, were published quite recentlyt by Profs. Roberts-Austen and Riicker§. The irregularities obtained by these gentlemen with different methods of treatment (heating in an oxidizing or a reducing atmosphere, repeated heating, sudden cooling), the anomalously large specific heat between 750° and 880°, where basalt is certainly solid, and the absence of true evidences of latent heat||, contrast strangely with the uniformly normal behaviour occurring throughout my own results. Basalt is chemically and lithologically so near akin to diabase (particularly after melting) that I anti- cipated a close physical similarity in the two cases. Unfor- tunately the account given of the basalt work is meagre. Detailed comparisons are therefore impossible. The elaborate measurements of Hhrhardt (1885) and of Pionchon (1886-7) are less closely related to the present work. APPARATUS. 3. The Rock to be tested About 30 grammes of diabase were fused in the small platinum crucible together with which they were to be dropped into the calorimeter. Two such charged crucibles were in hand, to be used alternately. ‘The molten magma, after sudden cooling, shows a smooth, appa- rently unfissured surface, glossy and greenish black. After * Communicated by the Author. T The geological account of the present work is begun by Mr. Clarence King, in the January number of the American Journal. { This was written some time ago. See American Journal, December 1891 and January 1892, A forthcoming Bulletin, No. 96, U.S. Geological Survey, contains the work in full, § Roberts-Austen and Ricker: this Magazine, xxxii. p. 855(1891). | Supposing basalt to solidify (§ 18) below 1200°, The Fusion Constants of Igneous Rock. 297 drying and weighing, the mass is often found to have gained 5 per cent. in weight. I was at first inclined to believe that this was attributable to water chemically absorbed by the viscous magma; but the water is only mechanically retained, for it passes off after 24 hours of exposure to the atmosphere, or by drying at 200° C. for, say, 30 minutes. Hence I weighed my crucibles at the beginning of each measurement, having previously dried them at 200°. The solid glass, sud- denly cooled from red heat, soon shows a rough and tissured surface, and its colour changes from black to brown, possibly from the oxidation of proto- to sesquisalt of iron, possibly from mere changes in the optical character of the surface (§ 2). Throughout the course of the work the charge of the crucibles was neither changed nor replenished. 4. Thermal Capacty of Platinum.—Data sufficient for the computation of the heat given out by the crucibles were published in 1877 by Violle*, whose datum for the high temperature (t) specific heat of platinum is ‘0317 + °000012¢. Hence the increase of thermal capacity from zero Centigrade to the same temperature is ¢(°0317 + -000006¢), which is the allowance to be made per gramme of platinum crucible. 5. Lurnace.—Inasmuch as heat is rapidly radiated from the white-hot slag, iit is necessary to transfer the crucible from the furnace into the calorimeter swiftly. I discarded trap- door, false bottom, and other arrangements for this purpose, because the mechanism clogs the furnace, interferes with con- stant temperature, and is too liable to get out of order. The plan adopted is shown in figs. 1 and 2 (Plate VI.), in sectional elevation and plan. ‘The body of the furnace consists of two similar but independent bottomed half-cylinders, A A and BB, of fire-clay properly jacketed, which come apart along the vertical plane cece. The lid, LL, however, is a single piece, and fixed in position by an adjustable arm (not shown). Hach of the halves of the furnace is protected by a thick coating of asbestos, CC, DD, and by a rigid case of iron, HH, FF. Set ser ews, 9999, pass through the edges of this in sucha way as to hold the fire-clay and asbestos in place. The horizontal base or plate of the casing H F is bent partially around the two iron slides, GG, along which the two halves of the furnace may therefore be ‘moved at pleasure while the lid is stationary ; as is also the blast-burner, H, clamped on the outside (not shown), and entering the furnace by a hole left for that purpose. * Violle’s calorimetric work will be found in C. &. Ixxxv. p. 5483 (1877), Ixxxvii. p. 981 (1878), Ixxxix. p. 702 (1879); Phil. Mag. [4] p. 818 (1877) Phil. Mag. 8. 5. Vol. 35. No. 214. March 1893. X 298 - Mr. Carl Barus on the Fusion The charged crucible is shown at K (figs. 1, 2, and 3), and is held in position by two crutch-shaped radial arms, N,N, of fire-clay, the cylindrical shafts of which fit the iron tubes P, P, snugly, and are actuated by two screws, R, R. More- over P, P are covered with asbestos (not shown), and thus subserve the purpose of handles, by grasping which the two halves of the furnace may be rapidly jerked apart. It is by this means that the crucible is suddenly dropped out of the furnace into the calorimeter immediately below (not shown). Care must be taken to have the arms N, N free from slag. ~ 6. Temperature.—As in the former work, the temperature of the furnace is regulated by forcing the same quantity of air swiftly through it at all times, but lading this air with more or less illuminating-gas, supplied by a graduated stop- cock. The amount of gas necessary in any case is determined by trial, and observations are never to be taken except after 19 or 20 minutes’ waiting, when the distribution of temperature is found to be nearly stationary. Nevertheless the tempera- ture of the crucible is never quite constant from point to ‘point. I therefore measured this datum at three levels—near the bottom, the middle, and the top of the charge, after the stationary thermal distribution had set in (see Tables, § 10). For this purpose the fire-clay insulator*, ¢¢, of the thermo- couple, ab, passing through a hole in the lid, is adjustable along the vertical. Before dropping the crucibie the thermo- couple is withdrawn from the charge and suspended above it. The cold junction is submerged in petroleum and measure- ments made by the zero method. . - When the charge is solid, a small platinum tube previously sunk axially into the mass (see fig. 3) enables the observer to make the three measurements for temperature as before. In my later work I also encased the insulator of the thermocouple in a platinum tube closed below (see fig. 1) when making these measurements for the molten charge. Slag being a good conductor at high temperatures, hydroelectric distor- tions of the thermoelectric data may not otherwise be absent. I state, in conclusion, that when constancy of temperature is approached the hole in the lid is closed with asbestos, and the products of combustion escape by the narrow seam in the side of the furnace, through which, moreover, crucible and appurtenances are partially visible. * These are cylindrical stems, 0°5 centim. thick, 25 centim. long, with two parallel canals running from end to end, through which the platinum ee are threaded. Cf. Bulletin U.S. Geolog. Survey, No. 54, p- 95 Constants of Igneous Rock. — 299 7. Calorimeter.—A hollow cylindrical box, provided witha hollow hinged lid, through both of which a current of cold water at constant temperature continually circulated, sur- rounded the calorimeter on all sides. Thus the temperature of the environment was sharply given, and the correction for cooling could be found and applied with accuracy. : The calorimeter was a vessel of thin tinned sheet iron, 28 centim. long, 8 centim. in diameter, having a water-value of 19 gramme-calories, and holding a charge of about 1200 grammes of water. The inside of the vessel was provided with a fixed helical strip running nearly from top to bottom, and was supported on a hard rubber stem. This could be actuated on the outside of the outer case from below, and served as a vertical axle around which the calorimeter could be rotated. In this way the water within the vessel was churned, and three small hard rubber rowels near the top gave steadiness to the rotation. I pass the description of this apparatus rapidly here, but shall recur to it in connexion with other. calorimetric work. The box or outer vessel of the calorimeter, with its pro- jecting stem, was movable on a small tramway, the. tracks of which lay at right angles to the slides G, G (figs. 1 and 2). Thus at the proper time the lid of the box was opened and the calorimeter rolled directly under the furnace. After receiving the crucible the calorimeter was again rolled away and the box closed, whereupon the temperature-measurements were made by a sensitive thermometer inserted through a hole in the lid. Were I to continue work like the present I should make the crucible bullet-shaped, and provided with a permanent central tube much like fig. 8. The splashing of water by the drop- ping crucible (an annoyance which is sometimes serious) would then be to a great extent obviated. RESULTS. 8. Method of Work.—While waiting for stationary furnace temperature I made the initial measurements for the cooling of the calorimeter in time series. Knowing, therefore, the time at which the body was dropped I also knew the tempe- rature of the water into which it was dropped, accurately: Similarly the three measurements for the temperature of the charge had just before this been made in time series. The experiments showed that ten minutes after submer- gence the crucible and charge might safely be considered cold, for the maximum temperature of the calorimeter was X 2 300 Mr. Carl Barus on the Fusion reached after 5 minutes. Hence the time from 10 to 15 minutes was available for making the final measurements for cooling ; knowing the extremes, I found the intermediate rates in accordance with the law of cooling. Thus, while the calorimeter was being constantly stirred, its temperature was measured at the end of each minute. Hence I knew the mean excess of its temperature above its environment during the course of every minute, and was able to add the corresponding allowance for elation and evaporation at once. How im- portant this correction is the Tables (§ 10) fully show. The only drawback against sharp values is the lag error of the thermometer ; but this is eliminated in a long series. I have bated that both the calorimeter aa the eaeible. were weighed before and after each measurement. The latter data were taken. 9. Arrangement of the Tables——The two crucibles (§ 3) and tubes (fig. 3) are designated I. and II. In all cases m is the mass of the charge, M the calorimetric value of the calorimeter (corrected for temperature), 7 the temperature of the environment. © is the temperature at the top, the middle, and the bottom of the charge at the time of submer- gence. The mean value is also given. The temperature of the calorimeter at the time specified is given under @, and a parallel column shows the correction of @ for radiation. Finally, the computed thermal capacity of the platinum cru- cible and appurtenances (correction fh), and the thermal capacity * h of the charge computed up to each of the con- secutive times, are found in the last columns. A few obvious remarks follow. Note that h reaches its true (constant) value in proportion as the body is cold. To avoid prolixity I have only given full examples of the data here defined at the head of each table. The remainder is abbreviated. 10. Tables——In the data of the first series (Table I.) only one value of ® is in hand for the liquid state. Moreover the construction of the furnace was somewhat faulty, not being flat-bottomed. Hence these results are of inferior accuracy as compared with Series II. (Table I1.), which are the best obtained. * The constant / is really the increase of thermal capacity above zero degrees Centigrade. Constants of Igneous Rock. 301 Tasie I.—Thermal Capacity of Diabase. First Series. Platinum crucible, I., 11:169 g.; Platinum tube, L[., -985 g. Platinum crucible, II., 11°271 g.; Platinum tube, IL., -654 g. . | | : | Mean 6. 'Correc- | Correc- ae meeetme., | OQ... | ME) 6. tion tion h. ; | | ho, Ue | re h. i———-| | ee |: ape? ee ee on eee ance Sees nee | | °C. | Minutes.; °C. | 2. °C. | g.-cal. | g.-cal. | eS ‘Dai esta NBO See ORAS Bape Ge daey: eases Immersion | . ee 12022. | 22:30) +02) | 179 | 967 | Taquid. | 2 ih oa 33:36 g.| 25:20) -06 355 | 3 | | 25°50) -11 367 | 5 | 25°58| -20 372 | | | 8 | 2540| -33 370 an | 11 25:25| 46 370 | 14 | 25:12] +60 370 iy Cee ee TBOGeHN5- OO ly eae || Sela Immersion | ernie) 2.2... 1145 g. | 36-04} 1:10 | 166 | 364 | Liquid. MMSE reir | ses... 33°75 g. Bagh ge |. 1378° | 99-16] ...... Ce REA ee Tare ceou | pie | 1202 g. | 30-97] 1:11 | 20°77 | 385] Liquid. Peas 29°32 g. | I} ia 1397 PCIe oe eee ae ee ae eeeiereion | La EAE tls Bios 1196 g. | 2440; 69 18-0 373 Liquid. OEE eg ere 32°22 g. a Se. eee eee yee) Dice ey mean es. iitverten fee | Ales, 1196 ¢g. | 29-98} 1:10 | 17-1 358 | Liquid. Bosse 29°16 ¢. | sel ee O | 1199 | 1166° PAs NPAs tail a eee |) See Immersion 14 1163 | 1195 ¢. | 22-98) -81 | 167 311 | Solid. 1138 | 82:22 ¢. ete O- | L 100) | LOT8S | | NOTIG | Si ee Immersion 14 1074 | 1196 g. | 27:25] -74 | 164 | 263] Solid. 1060 | 29:16 ¢. —- ce |S oe ———$————— —_—_—— =——_——___| __.___ Se ete | tt 0 LOR | PLOOWC 4 SOh = ees ee emia ah Immersion iu 998 | 1196 ¢. | 21°31] -47 | 139 | 242/ Solid, | 983 | 32-23 ¢. II. | 11 0 1035 | 1025° OG) SOONER De erate eet hee Immersion 14 1025 | 1195¢. | 25:55) -73 | 15:5 | 253] Solid. 1015 | 29:16 ¢. | oe | ee ee | ee ee | ee ef. 0 889 880° TGAHOUM Ah eeu a lvere meee Nt g eet ae Immersion | 11 880 | 1198 g. | 21:59} 41 | 120 | 204] Solid | 872 | 32:24 pg. Se eee eee Cea Eee iC a ) B27 | WSO9Cm 0-07 ues] one Lt eee Immersion | 14 | 827 | 1192g. | 2439) 65 | 121 191 | Solid. hee) | 833 | 29°16 g.| | | { | ; i | 302 Mr. Carl Barus on the Fusion TasLe [1.—Thermal Capacity of Diabase. Second Series. — = 10 10 | PALER 10 997 995 987 1260 1251 1243 | 1354 1333 948 949 | 1364 | 1854 — | 1339 877 873 870 | 1176 1164 1158 1215 1191 | 1186 782 780 780 | 1204 | -1195° | 1183 Mean 0. 1319 | 954 1 993° 26:27 g. i M. Mm. 1251° 1189 g. 26°39 g. 1192 ¢. 32°22 g. 1251° 1190 g. 26°07 g. | 1334° 1190 ¢. | 948° 1186 g. 32°22 g. 1352? >, | 1194 g. | 26°05 g. | 873° | 1191 g. | 32°20 g. | 11GG2 | LISis. | 25°97 g. 197° 1192 ¢. 25°95 g. 781° 1189 g. 3219 g. 1194° 1195 g. 25°90 g. (mecca 1 | Correc-| Correc-. | Time. 0. tion tion | Coe = 6. hee | Minutes. °C. | °C. | g.-cal. | g-cal. : yh fe) 18°94). o.0) =e Immersion 1 24-60; -04 206 | 236 Liquid. 2 26:°05| -10 305 3 26:52) -16 329 | 9) 26:61| -30 339 8. | 2645] -50 341 11 | 2625) -69 au) Gyo 14 26:08; -88 341 OF AAT. cence ee =. Immersion igi 20°61) -22 13:38 | 2383) Solid. 0 1934) \.c2%.) | 22 eee TS See: 4, 2649) _. 80 20°38 | 842°5| Liquid. 0 13°78) <2... | 2.28 Immersion 14 | 21°79| °84. | 224 | Sirah Ss nguid: 0 | 20-24) ...... eee Immersion | 14 | 2581, -94 | 18:0 | 2266) Solid. hues ae! Lose FV ee Sess 0 AAS) eee [gees tae | Immersion 14 24:82| °87 | 23:1 (| 3660) aiid: 0.) 14°83 sce ee eee Immersion 14 .| 20:13|- 46. | 2:9 9202 Salad: Os] 17-40, vezi | eae ee: | Immersion | 14 | 24-21) 77 | 19:2 | 3095) Liquid. 0 | (4488) <2) hee Immersion ea | 2113; 62 199 | 3185; Liquid. 0 19°36 Petes. Immersion yaa Be 23:61) -94 104 | 179-7 Solid. pot tl et : nod 0. 114:54|" cect | eee Immersion 145 | 21:22) -66 19:99 | 3179 Liguid. | | Constants of Igneous Rock. — 303 Table LI. (contznued). | Cone Mean 9. | Corree-| Correc- N pins é. M. Time. Q. tion LOMey yas fae | Mm. | 0 ser OC, | Minutes.| °C. °C. | g-cal. | g.-cal. era ibis | Li71° Y) TO S8i ee eee a AOE aot Immersion BETO |) 1192 ¢- 14 27°30 2 VAD | 16°7 | 301°6 Solid. 1166 | 32:20 g. | E |) 11 | 1106 | 1096°-| 0 - | 16-28! ...... | Behe Immersion 1094 | 1195¢: 14 | 23°24 “OL Lar 268°2 Solid. 1088 | 32-21 g. | | mene 95) 4ge 0, TSF) | ea... Immersion 1244] 1191v.| 14 | 2655; -89 | 21-1 | 3888] Liquid. 1238 | 25°49 g. MINIS | 1216201 0 81 13°67) ee ee Seasee Immersion 1216 | 1188¢.| 14 - | 21-60| “69 |-17-7 | 3303| Liquid. / 1202 | 29-43 ¢. ee ae = pe a, es aah CEES He ebie 1924)" 1215° 0 oS a 0 Wa C3, nega Peon See Ls Immersion 1216 | 1185 ¢. 14 26°27 ‘95 20°4 326°6 Liquid. 1205 | 25°57 g. For brevity the later observations were averaged per 3 minutes, and under / the mean value for the last 11 minutes is usually given. In Series I. the increase of temperature from top to bottom of the crucible is as large as 60° at 1200°, usually much smaller, however, and falling off pretty regularly to 6° at 829°. In Series II. the corresponding mean difference is about 25° at 1300°, 14° at 1000°, 10° at 800°. ‘The errors thus involved cannot be greater than 2 per cent. in the extreme case ; but since the distribution of temperature 1s measured, it is probably negligible except at very high temperatures. I am inclined to infer that the greater constancy of the solid distribution as compared with the liquid is due to greater thermal con- ductivity in the former case (solid), convection being neces- sarily absent in both. Considering the observational work as a whole, the data are satisfactory, seeing that an error of 0°1°C. in the calori- metric temperatures, initial or final, must distort the results at least 1 per cent. But the real source of error is probably accidental, and is encountered when the hot body falls through the surface of the cold water. INFERENCES. 11. Digest and Charts—In Tables III. and IV. I have summarized the chief results on a seale of temperature. The 304 Mr. Carl Barus on the Fusion results of the latter (Series II.) are graphically shown in the chart (fig. 4), in which thermal capacity in gramme-calories is constructed as a function of temperature *. are drawn through the points, showing the mean specific heats for the intervals of observations, solid and liquid. The letter a marks the region of fusion. TasiE III.—Thermal Capacity of Diabase. Mean specific heat, solid, 800° to i100° liquid, 1200° to 1400° . Latent heat of fusion, at 1200°, 24 g.-cal.; at 1100°, 16 g.-cal. 99 Solid. ‘romp Teena | 2 | 829 | 191. |} 1025 | 80 | 204 || 1078 1001 | 242 | H1166 | | Digest, of. § 15. | Thermal ‘| capacity. 253 263 all Straight lines “304. 350. Series I. Liquid. Thermal ‘| capacity. 358 Taste [V.—Thermal Capacity of Diabase. Digest, ef. § 15. Mean specific heat, solid, 800° to 1100° f liquid, 1100° to 1400° . Latent hea of fusion, at 1200°, 24 g.-cal.; at 1100°, 16 ¢.-cal. 29 Solid. Temp. ee Temp. oO te) 781 180 1096 873 202 (i171 948 227 993 238 | | Thermal capacity. Thermal ‘| capacity. ——— 370 385 | | | Series II. 290. 360. | 1352 Liquid. | | Temp,| capacity. | T%P+ capacity evinaeiel. - é 1166 | 310 || 1248] 339 1194 | 318 || 1251 | 340 1197] 319 || 1251] 342 1215 | 327 || 1334] 377 1218 | 330 367 * The corresponding chart for Table III. is almost identical with this. + Incipient fusion (?) at the base of the crucible. Constants of Igneous Rock. 305 In both the tables, III. and IV., the solid points lie on lines which, if reasonably curved, would be nicely tangent to an initial specific heat of about 0°2 at °C. The grouping, in other words, is so regular as to exclude the probability of anomalous features, either in the observed or the unobserved parts of the loci. The solid point near a (fig. 4, a similar point occurs in Table III.) alone lies markedly above the curve ; but inasmuch as in my volume work | found solidification to set in at 1100°, it is altogether probable that the occurrence at 1170° is incipient fusion (¢ 13). The regularity of the liquid loci (Tables III. and IV.) is slightly less favourable; but the discrepancies which occur are above 1300°, and obviously accidental (§ 10, end). 12. Specific Heat.—As regards the mean specific heats be- tween 800° and 1100° in Tables III. and IV., it will be seen that the intermediate datum would satisfy both groups of points about as well as the individual data given. A tracing made of the first group practically covers the other. The same remarks may be made for the liquid state. I have not attempted any elaborate reductions, since the equations of the necessarily curved loci would have to be arbitrarily chosen, and since values for specific heat are of no immediate bearing on the present inquiry. 13. Hysteresis.—Recurring to the suggestion of the pre- ceding paragraph, it appears that the fusion behaviour of rocks must be accompanied by hysteresis* of the same nature as that which I observed with naphthalene and other substances: for, whereas in my volume work with diabase I was able to cool the rock down to 1095° without solidifying it, evidences of fusion (at a, figs. 4 and 5) do not occur in the present work until 1170° is reached. The magnitude of the lag is thus of the order of (say) 50°, and its pressure-equivalent may be estimated as 500 atmospheres. 14. Latent Heat.—In virtue of the fact that the (upper) end of the solid locus (Tables II]. and IV.) may be carried so near the beginning of the liquid locus, the datum for latent heat is determinable with some accuracy, in spite of its sur- prisingly small (relative) value. Difficulties, however, present themselves in the determination of the true melting-point, a datum which can only be sharply defined when the tempera- ture of the crucible is quite constant throughout. I have, therefore, considered it preferable to state the conditions at 1200° and at 1100°, the former being nearer fusion and the latter very near solidification. The latent heats for these * Am, Journal, xlil. p. 140 (1891); of ibid., xxxvili. p. 408 (1889). 306 The Fusion Constants of Igneous Rock. temperatures are 24 and 16 respectively. The coincidence of results in both of the independent constructions (Tables ILL. IV.) is in a measure accidental. : 15. The Relation of Melting-point to Pressure.—The first and second laws of thermodynamics leid to the equivalent of James Thomson’s fusion equation, which in the notation of Clausius* is dT/dp=T(o—7)/Hr’ ; where T is the absolute melting-point, c—7 the difference of specific volumes solid and liquid at T, 7’ the latent heat of fusion, and EK Joule’s. equivalent. * Combining the present Series I. of thermal measurements with the former Series III. of volume measurements, I ob- tain at 1200°, since T= 1470°, co—r="0394/2°72 (where 2°72, is the density of the solid magma at zero), and 7’=24. | dT == == (ile ak and-at 1100°, since T=1370°, c—rT='0385/2°72, and 7 =16, —, —— 7 oe (a 1100 Similarly, combining the present (heat) Series IJ. with the former (volume) Series IV., at 1200°, since o—T='0352/2°72, and 7’ = 24, dT —— =°()19 ; dp pe and at 1100°, since o —7T=°0341/2°72, and te 16, ([) ~-026 dp 1100 Hence the probable silicate valuet of dT/dp falls within the margin (‘020 to ‘036) of corresponding data for organic sub- stances (wax, spermaceti, paraffin, naphthalene, thymol). I may, therefore, justifiably infer that the relation of melting- point to pressure in case of the normal type of fusion is nearly constant irrespective of the substance operated on, and in spite of the enormous differences of thermal expansibility and (probably) of compressibility. And in the measure in which this is nearly true on passing from the carbon com- pounds to the thoroughly different silicon compounds, is it * Warmetheorre, i. p. 172 (1876). 2 + For reasons to be stated elsewhere, 6m =a+'025p (where On is the melting-point in °C. at the pressure p atmospheres) will be assumed in making geological application of the above data. Notices respecting New Books. 307 more probably true for the same substance changed only as to temperature and pressure. In other words, the relation of melting-point to pressure is presumably linear. « In my work on the continuity of solid and liquid * these relations are corroborated for naphthalene within an interval of 2000 atmospheres. XXIX. Notices respecting New Bowes. Treatise on Thermodynamics. By Purer ALEXANDmR, M.A. London: Longmans, Green, and Co. 1892. rom the preface it appears that this book is ambitious: it claims to have elevated the science of Thermodynamics into an organic unity from being a mere collection of detached propo- sitions, to exhibit the thermodynamic relations as the outcome of physical, as opposed to mathematical, considerations, to have cleared away the fog that has enw rapped the subject of irreversi- bility, and, by an enlarged definition of entropy, to have opened up a mode of dealing with this subject, and, finally, to have dissipated the haziness that has overlain the subjects of Motivity and Dissipation of Energy. The idea is to be deprecated, however, that, as hitherto treated, the science of Thermodynamics has consisted of any more detached propositions than the two, representing the two laws, which are the necessary basis of this as of every other treatise on the sub- ject, viz. that of the conservation of energy and that of the perfec- tion of a reversible engine or its equivalent, together with their consequences ; and indeed a set of relations, which are the expres- sions in different forms of the same fact and which are all deducible from each other by simple transformations, does not constitute different but identical propositions. What the author has really done is to express the two laws, 7. e. practically the values of the dynamical equivalent and of Carnot’s function, in a manner even more general than that worked out (though not otherwise employed) by Clausius, viz. in terms of two general variables with any scale of temperature whatever, and then from these expressions to deduce particular thermodynamic relations by the substitution of particular variables : and it is these relations, which are necessarily identical, that constitute the “ detached propositions” above mentioned. Eyen if this method does not really tend to promote the organic unity of the science, it has without doubt its advantages and, by reason of its generality, should find place in some form or other in every formal text-book : it is certainly convenient if only as a simple mode of demonstrating certain identities and even of bringing to light identities, unimportant enough it may be, that might otherwise escape recognition. At the same time it is unlikely that general resort will be made to it for obtaining the really important * Am. Journ, xlii p, 144 (1891). 303 Notices respecting New Books. forms of the thermodynamic relations, each of which is patent on a glance at the corresponding infinitesimal cycle. In his investigation of these general expressions, the author prefers not to avail himself directly of the fact that infinitesimal changes of entropy and intrinsic energy are perfect differentials, and so, according to Lord Kelvin’s simple plan, to apply the corre- sponding criteria forthwith, this method savouring of mathematics only: he follows Clausius’ original lead instead, without, however, Clausius’ elaboration, and, taking an infinitesimal cycle composed of two pairs of thermal lines of any different types, he sums up the heat absorbed all round the cycle and also the changes of entropy, and equates the former sum to the area of the cycle and the latter to zero, this lengthier process being chosen as being of a more distinctly physical character than the other. In the second of these calculations the criterion of a perfect differential 1s of course necessarily arrived at, since the process of determining the eri- terion is essentially that of the method pursued ; attention might therefcre with advantage have been called to the mathematical character of this resulting equation, more especially as after reading Chap. XV., wherein is given Lord Kelvin’s method, a student will not be likely to have recourse to the other. Advan- tageous, too, would be the omission in this calculation of the signs of integration, which are finally discarded as quite unnecessary and are not even introduced into the other calculation on p. 42. With respect to irreversibility, itis pointed out that there may be processes which, though not actually reversible, are, so far as the working substance is concerned, in one direction equivalent to pro- cesses that are reversible, in which case the changes of entropy that occur in the working substance itself during such processes (termed conditionally irreversible, in contradistinction to zintrinsi- cally irreversible processes which have no such equivalents) depend only on its initial and final states. But we are not really helped by these considerations—which are not new—since it is the actual sources &c. and the actual variations of entropy with which we are really concerned. The proposed enlargement of the definition of entropy which is to help with the treatment of irreversibility greatly needs defence. It is ushered in with an objection to the definition of the entropy of a body or system as the sum of the entropies of its parts, ‘‘ which seems to me as unwarrantable as to define the temperature of a body or system as the sum of the temperatures of its parts,” so that to speak of entropy per unit mass “‘seems to me as un- warrantable as to speak of temperature per unit mass”; though no reason whatever is given or even hinted for likening entropy to temperature rather than to such another physical property as energy or volume. Such a definition of entropy is then desired as will make the entropy of any system whatever invariable when no heat passes into or out of it; and the author considers that he has obtained such a definition—which satisfies also his previous objection—in the formula X.rmg/S.7m, where m is the mass Notices respecting New Books. 309 of a portion of the system of which the entropy and absolute temperature are ¢ and r. Assuming, however, the formula for a single mass, consider a system of two masses m,, m, of the same substance with entropies ¢,, ¢, and at absolute temperatures 7,,7, respectively; and let these masses be respectively expanded and compressed adiabati- cally to the temperature - and then respectively compressed and expanded isothermally to the pressure p: the system is now in equilibrium, and, if vis taken such that no energy is lost or gained by the system and that the heat lost by the one mass is equal to that gained by the other, it is in that state of equilibrium which the system would finally attain in isolation. If, then, ¢ is the final entropy of the system, the heats lost and gained are m,t (¢,—¢) and m,7 (¢—@,), whence ¢=(m,¢,+m,9,) /(m,+m,), which does not satisfy the proposed formula except for r,=r, or ce ao, being thus considered a debatable subject, it is surpri- sing to see it postulated in the Introduction as an evident property of a substance and to find it treated as such without debate or explanation till the last chapter. In Maxwell’s opinion, “ itis to be feared that we shall have to be taught thermodynamics for several generations before we can expect beginners to receive as axiomatic the theory of entropy.” The account given of thermodynamic mnctivity and dissipation of energy is good and clear, and it is properly remarked that Clausius’ theorem of the tendency of the entropy of the universe to a maxi- mum is only a restatement in terms of entropy of Lord Kelvin’s dissipation theorem published thirteen years earlier. Though the book, therefore, does not seem quite to fulfil the pro- mise of the Preface, it will doubtless prove a useful mathematical introduction to the subject, which it does not pretend to treat experimentally, the few experiments that are referred to being mentioned only briefly and without detail. Its arrangement seems capable of improvement. Thus, it is not broken up into articles and its equations zre numbered consecu- tively from first to last, so that references are tedious: the theorem of the dependence on pressure of the temperature of the maximum density of water is placed where it seems to be dependent on thermodynamical considerations, while that of the equality of the ratios of the principal specific heats and of the principal elasti- cities is actually proved by such considerations, of which it is absolutely independent—as is obvious, since it was known to Laplace: and two general equations of very great importance, (216) and (217), are deduced only incidentally to prove that the principal specifie heats of superheated vapours are approximately functions of temperature only. There is some looseness of expression: thus the word perfect is used as equivalent to efficient, which leads to the solecisms more perfect and equally perfect ; the dyne, centimetre, and erg are called French units: the dynamical equivalent of heat is said to be B10 Notices respecting New Books. -* 772 on the Fahrenheit scale”; Mayer is credited with an experi- ment which was repeated by J oule, whose object in experimenting -is-rather made to appear as the justification of Mayer's hypothesis. Technical terms, too, are used without definition: thus the idea of efficiency 1s introduced on p- 26 without any explanation though -its quantitative measurement is concerned, and, indeed, when an -tmplicit definition is finally given on p. 35 in connexion witha Carnot cycle, it is in terms which are neither general nor such as Carnot could have accepted. it may also-be pointed out that in Chaps. XVI. and XVII. there is no Wee symbol for absolute temperature, though everywhere else the letter 7 is used ; that in Chapter XV. the muiceeieal specitic ation of entropy Abas from that adopted elsewhere; and that in (151) only a particular integral is given of the partial differential equation (150), the general solution of which is K=7* f(;*—3Ar,"p) corresponding to the characteristic v/7= U(p)+Ard\de 7—*f(7°--3Ar,"p). The notation is not all that can be desired; that of partial difterential coefficients is specially abused, after Clausius’ example, _In being applied to denote thermal capacities, and in Chap. XI. ‘the differential coefficients of p and A with respect to ¢ are con- tinually enclosed in brackets armed with some such subscript as 4, which is entirely incorrect, as these are not partial differential coefficients at all except with respect to the state of saturation ; elsewhere, too, occurs repeatedly the meaningless form (dr/dt)g, wherein 7 is an acknowledged function of ¢ only. These are, however, blemishes which do not impair the value of the book, but might be considered in view of a second edition. _Among its good points must specially be mentioned the stress that is laid on the proper definition of absolute temperature, though on p. 168 the author himself uses the definition to which he objects ; and there is an in‘eresting modification of Rankine’s characteristic for gases suggested w hich deserves discussion. It is further well remarked that even on the caloric theory Clapeyron’s version of -Carnot’s operations (which is that adopted in the book) would be improved by the adoption of Clausius’ modification,—which, by the way, is ascribed to J. Thomson, though contained in that memoir of Clausius which first set the subject on its new basis. It may _be here remarked that Carnot’s own version of his cycle requires no modification whatever, even from the new point of view. Die physikalische Behandlung und die Messung hoher Temperaturen. By Dr. Cart Barus. Leipzig: Barth, 1892. THE subject of pyrometry, although forming an important application of physics to manufactures, has not received from physicists the attention which it deserves. One reason for this is undoubtedly the difficulty of maintaining a constant high tempera- ‘ture, and another is to be found in the fact that the subject neces- -sitates a detailed study of the alterations produced in the properties -of matter by excessive heating. In order to measure any tempera- Notices respecting New Pooks. 311 ture absolutely, we must assume that some property of a substance remains constant at that temperature and at other known tempe- ratures. If this is not the case, the same temperature will have different values according tc the method by which it is measured, and its true value will most probably be that found by a majority of the methods. The author in his present volume has criticized the different methods of determining temperatures, and has given the results of experiments by himself and other workers in the same field, from which it appears that only three properties remain constant over wide ranges of temperature. These are the expan- sion of gases, the change of their viscosity with temperature, and the thermoelectric properties of certain wnetals, All these methods yield consistent results for the value of a given high temperature. . The second part of the volume is a discussion of the applicability of these three methods, and Dr. Barus pronounces in favour of the thermoelectric method. He then goes on to discuss the various forms of apparatus which might be used in applying this method ; from which it appears that a junction of platinum with an alloy of platinum and iridium or rhodium gives the best results. The book is the outcome of several years of difficult experi- menting, and it is to be hoped that it will encourage a closer study ot the properties of bodies, and especially of metals, at high tem- peratures. James L. Howarp. Hilfsbuch fur die Ausfuhrung elektrischer Messungen. By Dr. AD. HEYDWEILLER. Leipzig: Barth, 1892. Txis volume is not intended to serve as a text-book, but merely as an epitome of the various processes of electrical measurement. It gives in a collected form the different methods available for any particular kind of measurement, together with a short description of each; the formule necessary in order to calculate the results being likewise quoted, but not proved. In the majority of cases, however, the original papers and treatises are referred to for more complete information on this latter pomt. Under each experiment the author mentions the sources of error to which it is liable, and the devices for avoiding or eliminating them are stated, when such exist. This portion of the work has been carefully written, and will be found useful when the choice of a suitable method of measurement has to be made. At the end of the volume the various electrical constants have been tabulated, and four-figure logarithm and trigonometrical tables are also to be found there. Although the title of the book refers to electricity only descriptions of magnetic observations have also been given; but, as the author tells us im his preface, these are treated more briefly, and only those which are necessary in electrical measurements have been described. JamEsS L. Howarp. XXX. Proceedings of Learned Societies. GEOLOGICAL SOCIETY. (Continued from p. 150. } December 21st, 1892.—Prof. J. W. Judd, F.R.S., Vice-President, in the Chair. Sheet following communications were read :— 1. “On a Sauropodous Dinosaurian Vertebra from the Wealden of Hastings.” By R. Lydekker, Esq., B.A., F.G.S. 2. “On some additional Remains of Cestraciont and other Fishes in the Green Gritty Marls, immediately overlying the Red Marls of the Upper Keuper in Warwickshire.” By the Rey. P. B. Brodie, MAS, EeG:S: 3. “ Calamostachys Binneyana, Schimp.” By Thomas Hick, Esq., B.A., B.Sc. 4. “Notes on some Pennsylvanian Calamites.” By W. S. Gresley, Esq., F.G.S. 5. “Scandinavian Boulders at Cromer.” By Herr Victor Madsen, of the Danish Geological Survey. During a visit to Cromer in 1891 the author devoted much attention to a search for Scandinavian boulders, and obtained three specimens; one (a violet felspar-porphyry) was from the shore, and the other two were from the collection of Mr. Savin. ‘The first was considered to come from S.E. Norway, and indeed Mr. K. O. Bjorlykke, to whom it was submitted, refers it to the environs of Christiania. The author considered that the two specimens presented to him by Mr. Savin, who had taken them out of Boulder Clay between Cromer and Overstrand, were from Dalecarlia; and these were submitted to Mr. E. Svedmark, who compared one of them (a brown felspar-hornblende-porphyry) with the Gronklitt porphyry in the parish of Orsa, and declared that the other (a blackish felsite- porphyry) might also be from Dalecarlia. January llth, 1893.—W. H. Hudleston, Esq., M.A., F.R.S., President, in the Chair. The following communications were read :— 1. “ Variolite of the Lleyn, and associated Volcanic Rocks.” By Catherine A. Raisin, B.Sc. The district in which these rocks occur is the south-western part of the Lleyn peninsula, marked on the Geological Survey map as ‘ metamorphosed Cambrian.’ _ Some of the holocrystalline rocks are probably later intrusions. The igneous rocks, which are described in detail in the present paper, belong to the class of rather basic andesites or not very basic basalts ; they show two extreme types, which were probably formed by ee Intelligence and Miscellaneous Articles. 313 differentiation from an originally homogeneous magma. Corre- sponding to the two types of rock are two forms of variolite. These are fully described, and their mode of development is dis- cussed. The variolites occur near Aberdaron and at places along the coast. Their spherulitie structure often is developed towards the exterior of contraction-spheroids, and in this and in other particulars they correspond with those of the Fichtelgebirge and of the Durance. The volcanic rocks include lava-flows and fragmental masses, both fine ash and coarse agglomerate. They are associated with lime- stones, quartzose, and other rocks, which are possibly sedimentary, but which give no trustworthy evidence of the age of the variolites. 2. “ On the Petrography of the Island of Capraja.” By Hamilton Emmons, Esq. The rocks of Capraja consist generally of andesitic outflows resting on andesitic breccias and conglomerates. ‘The southern end seems to have formed a distinct centre of volcanic activity, whose products are younger in age and more basic in character than the rocks of the rest of the island, and may be termed ‘ anamesites.’ The lavas appear to have flowed from a vent at some distance from the cone which probably occurred here and gave out highly scoriaceous fragments. In the other parts of the island andesite is almost everywhere found, with patches of the underlying breccias here and there in the valley bottoms. The chief centre of activity prob- ably lay west of the centre of the island. Petrographical details of the andesites and anamesites, descrip- tions of the groundmass and included minerals of each, and chemical analyses are given. As regards the age of the constituents, the author arranges them in the following order, commencing with the oldest :—magnetite, olivine, augite, mica, felspar, nepheline. XXXI. Intelligence and Miscellaneous Articles. ON A NEW ELECTRICAL FURNACE. BY M. HENRI MOISSAN. HIS new furnace is made of two carefully plane pieces of quick- lime one placed under the other. In the lower one is a longi- tudinal groove for the two electrodes, and in the middle is a small cavity more or less deep acting as a crucible; it contains a layer ot a few centimetres of the substance to be acted upon by the are. A small carbon crucible may also be placed in it containing the substance to be calcined. In the reduction of oxides and the fusion of metals, larger crucibles are used, and through a cylin- drical aperture in the upper brick small] cartridges of the compressed oxide and carbon can from time to time be added. The diameter of the carbons which act as conductors will of course vary with the strength of the current; after each experiment the end of the carbon is changed into graphite. The current most frequently used was one of 30 amperes and Phil. Mag. 8. &. Vol, 35. No. 214. March 1893. iy, 314 Intelligence and Miscellaneous Artzcles. 55 volts; the temperature did not much exceed 2250°. A current furnished by a gas-engine of 8 horse-power was 100 amperes and 45 volts produced a temperature of about 2500°. Finally, thanks to the courtesy of M. Violle, we had at our disposal 50 horse- power ; the are in these cunditions measured 450 amperes and 70 volts, the temperature was about 3000°. With high-tension experiments certain precautions must be taken and the conductors be carefully insulated. Even with currents of 30 amperes and 50 volts, like those used at the beginning of the investigation, the face must not be exposed to a prolonged action of the electrical light, and the eyes must always be protected by means of very dark glasses. Electrical sun-strokes were very frequent at the outset of these researches, and the irritation produced by the are on the eyes may produce very painful congestion. The temperatures given are only approximate; they will be especially determined by M. Violle by methods to be afterwards described. A certain number of the results obtained are briefly enumerated. When the temperature is near 2500°, lime, strontia, and magnesia crystallize in a few minutes. If the temperature reaches 3000° the substance of the furnace itself—quick-lime—melts and runs like water. At this same temperature carbon rapidly reduces calcic oxide, and the metal is liberated freely ; it unites readily with the carbon of the electrodes, forming a calcic carbide, liquid at a red heat, and which can be easily collected. Chromic oxide and magnetic oxide of iron are melted rapidly at a temperature of 2250°. Uranium oxide when heated alone is reduced to protoxide, erystal- lizing in long prisms. Uranium oxide, which cannot be reduced by carbon at the highest temperature of our furnaces, is reduced at once at the temperature of 8000°. In ten minutes it is easy to obtain a regulus of 120 grains of uranium. The oxides of nickel, cobalt, manganese, and chromium are reduced by carbon in a few minutes at 2500°. This is a regular lecture experiment not requiring more than a quarter of an hour. By this method we have been able to cause boron and silicon to act on metals, and thus obtain borides and silicides in very beautiful crystals. This investigation is being continued.—Comptus Rendus, Dec. 12, 1892, ON THE DAILY VARIATIONS OF GRAVITY. BY M. MASCART. I have on former occasions used under the name of a gravity barometer an instrument by which the variation of gravity between different stations may be determined. The apparatus has the drawback of being very fragile, but the same arrangement haa great advantages in examining whether there are temporary Varia- tions in one and the same place. For some years past I have arranged a barometric tube contain- ing a column of mercury four metres and a half in length, which Intelligence and Miscellaneous Articles. 315 counterbalances the pressure of a mass of hydrogen contained in a lateral vessel. The whole apparatus is sunk in the ground with the exception of a short column of mercury at the top. The level of the liquid is compared with a lateral division, the image of which is formed in the axis of the tube, and the points may be fixed to within the ;4, of a millimetre. Direct observations at different times of day only showed a continuous course, the greater part of which was due to inevitable changes of temperature ; certain results can only be obtained by photographic registration. In the proofs submitted the differences of level are multiplied by 20; they correspond to the variations which are directly ob- served on a column 90 metres in length. The curves ordinarily present a very regular and slow course which is especially due to changes of temperature; but for some days sudden accidents are seen, the duration of which is from fifteen minutes to an hour, and which do not seem to be explicable otherwise than by correlated variations of gravity. These accidents may attain and even exceed 5), of a millimetre, which corresponds to so¢yp OF One second per day, supposing that they lasted the whole day. In order to have a term of comparison, it is sufficient to observe that if the difference between high and low water is 10 metres, the liquid layer would produce a variation of spy of the level value of gravity, that is one fifth of the preceding, The existence of these temporary variations of gravity appears undoubted and deserves attention. I intend to organize at the Observatory of the Parc Saint Maur an apparatus constructed with more care, from which all casual trepidation of the ground is excluded, and the indications of which can be continuously followed. Observations of this kind will no doubt present a peculiar interest in voleanic districts if the changes are due to displacements of masses in the interior.—Comptes Rendus, January 30, 1893. PRELIMINARY NOTE ON THE COLOURS OF CLOUDY CONDENSATION. BY C. BARUS. By allowing saturated steam to pass suddenly from a higher to a lower temperature (jet) in uniformly temperatured, uniformly dusty air, the following succession of colours is seen by transmitted white light, if the difference of temperature in question continually increases :—F aint green, faint blue, pale violet, pale violet-purple, pale purple, muddy brown-orange, straw-yellow, greenish yellow ; green, blue-green, grey-blue, intense blue, indigo, intense dark violet, black (opaque); intense brown, intense orange, yellow, white. Seen by reflected white light, the same mass of steam is always dull neutral white. If the colours enumerated be taken in the inverse order, be- ginning with white, they are absolutely identical with the inter- ference-colours of thin plates (Newton’s rings) of the first and 316 Intelligence and Miscellaneous Articles. second order, seen by transmitted white light under normal inci- dence. ‘Thus it is worth inquiring whether small globules of water, when white light is normally transmitted, affect it like thin plates. For a given homogeneous colour, if I be the intensity of the incident licht and & ( 04 to -05) the reflexion-coefficient, then after a single transmission the interference maxima and minima are (1-k)(1+)1 and (1—ky(1—-2 1; they differ only very slightly. But if there be an indefinite number of particles all of the same size available, then this process is in- definitely repeated in such a way that while the coloured light is not extinguished, the admixed white lght becomes continually more coloured. Hence, after a sufficiently great number of trans- missions, the emergent ray will show intense colour. Seen by reflected light, the case is almost the converse of this. For a single particle the masses which interfere are (Kl and k(1—<)?1) weaker, but nearly equal, and the interference is therefore very perfect. It is not, however, capable of indefinite repetition, for after each interference the direction is reversed. The light which emerges in a direction opposite to the incident ray must therefore have passed through the particles, 7. e. it has been brought to interference both by reflexion and by transmission, and its colour is thus virtually extinguished. The final point to be considered is the occurrence of black between brown and dark violet of the first order. Here, however, for relatively very small increase of the thickness of the plate, the colours run rapidly from brown through red, carmine, dark red- brown to violet. Hence these interferences are apt to occur to- gether and an opaque effect is to be anticipated. Particularly is this presumable, because the opaque field is coincident with the breakdown of the steady motion * of the jet. Thus it seems that the colours of cloudy condensation may, without serious error, be interpreted as a case of Newton’s inter- ferences by transmitted light. In so far as this is true, one may pass at once from the colour of the field to the size of the particles producing it; and the dimensions so obtained agree well with R. v. Helmholtz’s estimate made in accordance with Kelvin’s equation for the increase of vaponr-tension at a convex surface. In the study of the condensation phenomena vapour-liquid, the experi- mental power of a method, which is adapted for instantancous observation, and which, for a certain range of dimensions, not only discriminates between vapour and a collection of indefinitely small suspended water-globules, but actually defines their size, cannot be overestimated. An account of my work, together with other allied observations, will be given in the March number of the ‘American Meteorological Journal.’—Silliman’s Journal, February 1893. | * IT refer here to Osborne Reynolds’ work (Phil. Trans. iii. p. 935, 1883) with liquid jets, according to which, after a certain critical velocity is surpassed, the uniformly steady motion breaks up into eddying motion. I am also searching for Reynolds’ lag phenomenon (J. ¢. p. 957). THE ‘LONDON, EDINBURGH, ano DUBLIN PHILOSOPHICAL MAGAZINE AND JOURNAL OF SCIENCE. [FIFTH SERIES.] APREL 1893. XXXIL, On Plane and Spherical Sound-Waves of Finite Amplitude. By Cuaries V. Burton, D.Sc.* Part I.— PLANE WAVES. 1. HE subject of plane waves of finite amplitude has been considered by Riemann{; and so long as we confine our attention to the case where velocity and density are everywhere continuous, his investigation, as is well known, leaves little to be desired. It will not, therefore, be necessary here to make further reference to this aspect of the subject ; but there is one part of Riemann’s work which Lord Rayleigh has clearly shown to be unsatisfactory, and it is this point which we have now especially to consider. Lord Rayleigh says t:— | | a It has been held that a state of motion is possible in which the fluid is divided into two parts by a surface of discontinuity propagating itself with constant velocity, all the fluid on one side of the surface of discontinuity being in one uniform condition as to density and velocity, and on the other side in a second uniform condition in the same respects. Now, if this motion were possible, a motion of the same kind in which the surface of discontinuity is at rest would also be possible, as we may see by supposing a velocity equal and * Communicated by the Physical Society: read February 24, 1898, ¥ “Ueber die Fortpflanzung ebener Luftwellen von endlicher Schwing- ungsweite,” Gott. Abhandi. t. viii. (1860); reprinted in Werke, p. 145. { Theory of Sound, vol. ii. § 253, p. 41. Phil. Mag. 8. 5. Vol. 35. No. 215. April 1893. Z 318 Dr. C. Burton on Plane and Spherical opposite to that with which the surface of discontinuity at first moves, to be impressed upon the whole mass of fluid. In order to find the relations which must subsist between the velocity and density on the one side (w, p,) and the velocity and density on the other side (wz, p,), we notice in the first place that by the principle of the conservation of matter Polg=pity. Again, if we consider the momentum of a slice bounded by parallel planes and including the surface of dis- continuity, we see that the momentum leaving the slice in the unit of time is for each unit of area (p9v.=p1u1)Ue, while the momentum entering it is p;u,”. The difference of momentum must be balanced by the pressures acting at the boundaries of the slice, so that Pilly (U2— Uy) =p — Po = a(p1— po), =an/(@), m=an/(%) U,=a Un =A 5 : We Sosy P2 The motion thus determined is, however, not possible; it satisfies indeed the conditions of mass and momentum, but it violates the condition of energy expressed by the equation whence Won Lap AS 2 99 3 Ug 7 Uy =a log pi—a log po. 2. The assumed motion here criticised is one in which density and velocity are constant for all points on the same side of the surface of discontinuity, while this surface itself is propagated through the fluid with constant velocity. It is easily shown, however, that the same objection applies when, on either side of the surface, velocity and density vary con- tinuously in the direction of propagation, while the velocity of propagation of the surface is also allowed to vary. For let 8 (fig. 1) be a surface of discontinuity which is being propagated through the fluid, while the Fig. 1. planes A, B, parallel to S and lying on either | side of it, are fixed in the fluid. At a given instant let distance of S from A = m, ry) BB, S=n; density and velocity of fluid just to the left of Po U4, density and velocity of fluid just to the right of S=Ppo, w 5 velocity with which § is travelling = V. Sound- Waves of Fimte Amplitude. 319 Then, since A and B are fixed in the fluid, they are ap- proximately moving with the respective velocities uw, ug; m and n being taken sufficiently small. On the same under- standing, the mass of fluid between A and B (referred to unit surface) =mp,+mnp,; and since this mass must remain constant, d ap (mpi + Mpa) =93 2. e. in the limit, when m and n are infinitesimal, dm dn Bae aa Pee =0, or pi( V —2) =p.(V—w,). ni ir AC a Sabor 5 te Similarly, if p, and p. are the pressures corresponding to p; and pe, the principle of momentum gives:— p\—po= rate of change of momentum between A and B d = oF (u3p1m + Upon) = um pi(V—u)—Uaps(V—ue). » 2 - - + « (2) If the energy per unit volume corresponding to density p (in the absence of bodily motion) is called y(p), the principle of energy would further give Pi1—Poo= rate of change of energy between A and B = 3m( spin? + x(01)) + m(4 par +x(02) )} = feprs’ +x (Pr) (V —1) — faparle’ +x (92) t (Vue). (8) Since (1), (2), and (3) involve only the instantaneous values of w, Pi, U2, P2, and V, together with explicit functions of such values, while the space- and time-variations of all these quan- tities are absent from the equations, it is evident that the conditions to be satisfied at the surface S are the same as if Ur) Pi) U2) P2, V were absolute constants. We conclude then, that, with our assunvptions, a surface of discontinuity cannot be propagated through a fluid with any: velocity, uniform of variable, except under that special law of pressure for which progressive waves are of accurately permanent type. 3. What, then, becomes of waves of finite amplitude after discontinuity has set in? We may emphasize this difficulty, and at the same time obtain a clue to its solution, by con- sidering the following case (fig. 2):—-A is a piston fitting a Z 2 320 Dr. C. Burton on Plane and Spherical cylindrical tube (or, if we Fig. 2. please, is a portion of an un- limited rigid plane). All the air to the right of A is initially at rest and of uniform density, and then A is impulsively set in motion, and kept moving to the right with uniform velocity v. Consider the speed with which the disturbance generated by A advances into the still air to the right; it is evident that in all cases the front of the disturbance must advance faster than A. ‘Take, then, the case in which U> a, where a is the propagation-velocity of infinitesimal disturb- ances. Two alternatives present themselves :— (i.) If velocity and density are always either constant or continuously variable in the direction of propagation, the rate of propagation at any point will, in accordance with known principles, be = d / Ere and therefore at the front of the disturbance, where w=0 and p = the “undisturbed” density, the velocity of propagation will be simply =a; that is, less than the velocity with which A is advancing. Obviously this will not do. (ii.) If velocity and density are not always either constant or continuously variable, that is, if one or more surfaces of discontinuity are being propagated through the air, we are met by the difficulty explained in the last section. 4, A simple mechanical analogy will help to indicate the actual motion. A number of equal spheres, of the same material throughout, are capable of sliding without friction Fig. 3. {iHO—0—0—0=0=0- =1]}@=O=0=—0=—0=O= — 71 DO©=02 0-0 along a straight bar (fig. 3), and are connected together by a number of very weak and exactly similar springs (not shown), so that. when there is equilibrium they are equally spaced Sound- Waves of Finite Amplitude. 321 along the bar. If one of the spheres were moved backwards and forwards through a small range, a disturbance would travel through the whole system, but owing to the weakness of the connecting springs it would travel very slowly. Sup- pose, now, that the last sphere on the left hand is connected to a movable piston by a spring half the length of the others, but otherwise similar to them; and let this piston be suddenly moved to the right with a considerable velocity which is kept constant, and which we may call unity. The weak connecting spring between the piston and the first sphere produces no sensible effect until the two are almost in contact, when the sphere rebounds with velocity 2. This first sphere then strikes the second, imparting to it the velocity 2, and at the same time coming to rest. The positions of the spheres after successive equal intervals of time are represented in fig. 3, where the number written on any sphere represents its velo- city just after the impact which it is suffering. No number is written on those spheres which have not so far been affected by the motion. From this it will be evident that when the piston moves to the right with a constant velocity which is very great compared with the propagation-velocity of infini- tesimal vibrations of the system, the disturbance advances to the right with twice the velocity of the piston, provided that the diameters of the spheres are excluded from the reckoning. Now suppose that the spheres are too small and too close together to be individually distinguished; then, at any instant, the system will appear to be divisible into two parts, in one of which the velocity is unity, while in the other it is zero; and in the moving part the spheres will appear to be twice as thickly condensed as in the still part. That the constant velocity of the piston is very great compared with the propa- gation-velocity of small vibrations is of course only a sup- position introduced for the sake of simplicity. If, on the other hand, these two velocities are comparable, two adjacent spheres will always remain finitely separated from one another, and the velocity of any individual sphere within the disturbed stretch will never be as small as zero, or as great as twice the velocity of the piston ; the mean velocity within the disturbed stretch being equal to that of the piston. When the spheres are very small and very close together, we shall still have apparently an abrupt transition frem finite velocity and greater density to zero velocity and smaller density; and the energy, which is apparently lost.as the spheres pass from the latter condition to the former, exists as energy of relative motion and unequal relative displacement amongst the spheres in the disturbed stretch. : 5. Let us now compare the case just considered with the 322 Dr. C. Burton on Plane and Spherical case of § 3 (fig. 2): and first, concerning the nature of the analogy, it should be noticed that the individual spheres are not the analogues of the separate gaseous molecules, but that when both spheres and molecules are very small and very numerous, the apparently continuous properties of the system of spheres correspond to similar properties of the gas. The connecting springs represent the elasticity of the gas, iso- thermal or adiabatic as the case may be, and the energy of relative motion and unequal relative displacement amongst the disturbed spheres suggests that there is a production of heat over and above that which would be due to the (iso- thermal or adiabatic) change of density ; that is, a diss¢pative production of heat. The motion considered in the last section properly corresponds to the case where there is no conduction of heat, so that the connecting springs are the representatives of adiabatic elasticity, and the additional heat generated remains wholly within the more condensed part of the air. If we make the somewhat violent assumption that the tempe- rature of the air remains constant throughout, the additional heat generated will be conducted away isothermally, and the equivalent energy will be, for our purposes, entirely lost. To represent this case by means of our spheres we should have to regard the connecting springs as representing iso- thermal elasticity, while the energy of relative motion and unequal relative displacement among the disturbed spheres, as fast as it is produced, is to be consumed in doing work against suitable internal forces. 6. The mechanical system of spheres and springs, having suggested a solution, has served its purpose, and it now remains for us more closely to consider the aerial problem in the light of this suggestion. We may take, first, the case where the temperature is supposed to be invariable; for although such a supposition is necessarily far removed from the truth, it leads to very simple results, which indicate well enough the general character of the motion. Let the piston A (fig. 4) be moving to the right with constant velocity Fig. 4, v (which may be either less or greater than a, the velo- city of feeble sounds in air). Assume all the air between A and a parallel plane sur- face B to have the velocity v and density p,, while all the air to the right of B is at rest and has the density pp». Let the plane B move to the right with velocity V. Then the invariability of mass between A Sound- Waves of Finite Amplitude. 323 and a plane C fixed in the still air gives pi(V—v)—pyv=0; . . .. . 4) while from the principle of momentum, Pi (V— v) Olam 0's .=, hans Sosy tee (5) the pressure p being a function of p only, since the tempera- ture is supposed to be constant throughout. If we assume for this case the truth of Boyle’s law, so that p=a’p always, (5) becomes py(a? — Vv + v7) =pya”, SRR thea (6) which together with (4) is sufficient to determine V and p; when v and py are given. Taking all these quantities to remain constant throughout the motion, we see that at each instant the following conditions are satisfied :-— (i) Every necessary condition between A and B, since density and velocity are there constant with respect to space and time ; (1) Every necessary condition to the right of B, since the air there is at rest and in a constant uniform state ; (iii) Equality between the velocity of A and that of the air in contact with it ; (iv) At B, the conservation of mass and momentum, which are necessary conditions, and which, together with our supposition that the temperature is somehow maintained uniform, are sufficeent to determine what takes place at B*. Moreover, if at a time ¢ (reckoned from the instant when A was impulsively started into motion) we take the distance of B from A to be (V—v)t, so that initially B coincides with A, the initial conditions are satisfied. ‘Thus the assumed motion satisfies all the necessary con- ditions ; it is therefore the actual motion. 7. Let us now examine what occurs when no heat is allowed to pass by conduction or radiation ; a state of things much more nearly realized in practice. Suppose the motion of A and the condition of the undisturbed air to be the same as in the last section, while the (constant) velocity of B is now called V’, and the density and pressure of the air between A and B (called p’, p’ respectively) are also taken to be uni- form and constant. At each instant, in place of (4) and (5), we shall now have AANg= ©) gests hy. se ya nae) pruCV =v) = pi. ay. ew 6) (8) * Energy appears to be lost, because dissipatively produced heat is conducted away isothermally, 324 Dr. ©. Burton on Plane and Spherical Since we assume that there is no transference of heat by conduction or radiation, the rate at which the total energy of the system increases must be equal to the rate at which work is being done upon it by the piston A. Let @ be the abso- lute temperature to the right of B, that between A and B being 0’, and let us further assume for simplicity that P a const. : pe while y, the ratio of the two specific heats, is also supposed constant. It can then be shown without difficulty that the total energy per unit mass between A and B exceeds that to the right of B by Po O —O% fe es (y—1)po % 2° and multiplying this by p,V’, the mass of air which crosses one unit of the surface B in each unit of time, we obtain the rate (referred to unit area) at which the system is gaining energy. Again, the rate at which unit area of the piston does work on the system als Ee ges a ae Tet a ed eeiae and equating this to the rate of gain of energy, we obtain po mes wv PoV'! pe PO 505 V=PyV 5) + (y—1)0, (0 ,). a ° (9) We may also write equation (8) in the form plo(W'—v) = $F (p'6'—pr)s - ~~ (10) Po% and (7), (9), and (10) will then serve to determine V’, p', when ¥, po, 9 are given. Since we have taken all these quantities to remain constant throughout the motion, we see, as before, that at each instant all the necessary conditions are satisfied ; the principles of mass and momentum, together with our supposition that there is no exchange of heat, being sufficient to determine what takes place at B. Again, if ata time t from the commencement of the motion we take the distance of B from A to be (V’—v)é, so that initially B coin- cides with A, the initial conditions are satisfied. The assumed motion thus satisfies all the necessary conditions, and is there- fore the actual motion. 8. If we compare the results of the last two sections with Sound- Waves of Finite Amplitude. 325 those given by Riemann*, we shall find complete accordance so far as §6 is concerned, though with §7 the case is dif- ferent ; and this may be easily explained. We cannot in general investigate the motion of a (frictionless) compres- sible fluid by means of the equations of continuity and momentum, without further making some supposition as to the exchange or non-exchange of heat, and so we usually assume either that the temperature remains constant, or that there is no exchange of heat: in either case (provided the motion is continuous), the pressure is a function of the density only. Ata surface of discontinuity there is not only the ordinary heating effect due to compression, but also, as we have seen, a dissipative generation of heat, and so, when applying the equations of continuity and momentum at such a surface, we must know what becomes of this additional heat. Now in all cases Riemann makes the assumption that the pressure is a function of the density only, and this is necessarily equivalent to an assumption concerning the trans- ference of heat. Throughout most of his treatment of waves of discontinuity Riemann assumes that temperature is constant and that Boyle’s law holds good; accordingly our § 6 is entirely in harmony with his conclusions, in fact (4) and (5) are only particular forms of equations given by Riemann. Of course the hypothesis that a portion of gas can be instantaneously compressed to a finite extent without any appreciable change of temperature, is not in accord- ance with experience, but provided we accept the assump- tion that the temperature remains constant throughout, all that Riemann says concerning the propagation of waves of discon- tinuity under Boyle’s law will hold good. The assumption made in § 7, that there is no appreciable transference of heat, is probably much nearer the truth; but this is not in accordance with any assumption made by Riemann. When pressure is assumed to be a function of density only, and to vary with it according to the adiabatic law, 2t 2s wrtually assumed that at the discontinuity just so much heat remains in the gas as would be due to slow adiabatic compression, while the further amount of heat which is dissipa- twely produced 7s completely and instantaneously removed by conductzon. But though Riemann’s results may thus be justified by impossible assumptions concerning the diffusion of heat, we may more reasonably, following Lord Rayleigh, regard them as involving a destruction of energy. The real source of error lies in Riemann’s fundamental hypothesis. At the outset he supposes the expansion and contraction of * Loc, cit, 326 Dr. C. Burton on Plane and Spherical the air to be either purely isothermal or purely adiabatic, and thenceforward he treats the air as a frictionless and mathe- matically continuous fluid, in which pressure and density are connected by an invariable law. But in general the existence of such a fluid is contrary to the conservation of energy ; for as soon as discontinuity arises, energy will be destroyed. 9. It may not be out of place to conclude this portion of the subject by a short reference to a paper by Dr. O. Tum- lirz *. This author starts, as Riemann did, with the assump- tion that the pressure is a function of the density only, the law of pressure being further assumed to be the adiabatic law; and in order to avoid Riemann’s error, he explicitly uses the principle of energy applicable to continuous motion, in place of the principle of momentum. But the foregoing discussion will have made it clear, I think, that the solution of the difficulty is not to be sought for in this direction. In addition to the assumptions common to his own work and te that of Tumlirz, Riemann uses only the principle of mass and the principle of momentum ; and since by their aid alone he arrives at a completely determinate motion, it follows that any other motion consistent with the same arbitrary assumptions, and with the condition of mass, must violate the condition of momentum. We have seen, in fact, that there is dissipation of energy at a surface of discontinuity, so that the condition of energy applicable to continuous motion ceases to hold good. We are acquainted, too, with other instances where loss of continuity involves dissipation of energy ; for example, there is the case of one hard body rolling over another. As the result of his investigation, Dr. Tumlirz concludes that as soon as a discontinuity is formed it immediately dis- appears again, this effect being accompanied by a lengthening of the wave and a more rapid advance of the disturbance. In this way, therefore, he seeks to explain the increased velocity of very intense sounds, such as the sounds of electric sparks investigated by Macht. But it has already been pointed out [§ 3 (i.) |, that when density and velocity are every- where continuous functions of the coordinates, the front of a dis- turbance advancing into still air must travel forward with the velocity of infinitely feeble sounds. A greater velocity can only ensue when the motion has become discontinuous. * “Ueber die Fortpflanzung ebener Luftwellen endlicher Schwing- ungsweite,” Sitzungsb. der Wien. Akad. xcv. pp. 367-887 (1887). T Sttzungsb. der Wien. Akad, \xxv., Ixxvii., lxxyiii. Cf. also W. W. Jacques |On Sounds of Cannon], Amer. Journ. Sci, 3rd ser. xvii. p. 116 (1879). Sound- Waves of Finite Amplitude. 327 Part I].—SPpHERICAL WAVES. 10. When plane waves of finite amplitude are propagated through a frictionless compressible fluid, discontinuity must always occur sooner or later, and a moment’s consideration will show that there are at least some cases when the motion in spherical waves becomes discontinuous ; the question arises whether in any case it is possible (in the absence of viscosity) for divergent spherical waves to travel outward indefinitely without arriving at a discontinuous state. This question was suggested to me by Mr. Bryan, who at the same time kindly handed me notes of his manner of attacking the problem. His method was to write down the exact kinematical equation for spherical sound-waves, and then to obtain successive approximations to the integral of this equation. If it appears that after any number of approximations the integral would remain convergent for large values of the radius, we may con- clude that our equation holds good throughout, and hence that no discontinuity arises. If, on the other hand, the second or any higher approximation becomes divergent for large values of the radius, it is probable that the motion becomes some- where discontinuous. This method I have not followed out; but by another method which is, I hope, sufficiently con- elusive, I shall now endeavour to show that discontinuity must always arise. The case in which the motion loses its continuity compara- tively early requires no further consideration here ; we have only to concern ourselves with the case in which the initial disturbance has spread out into a spherical shell of very small disturbance whose mean radius is very great compared with the difference between its extreme radii. The equations applicable to the disturbance are then, very approximately, 8 te eee u or oP ec - for a given part of the wave, . (12) where p is the mean density, p+ép the actual density at a point where the velocity is wu, and a 1s the velocity of infinitely feeble sounds in air of density p; 7 is as usual the distance of a point from the centre of symmetry. Let us consider two neighbouring points M and N, on the same radius, each being fined in a definite part of the wave, the point M being behind N (.e. nearer to the origin), and the air-velocity at M ex- ceeding that at N by Au. Then, as the wave advances, each 328 Dr. C. Burton on Plane and Spherical part of it will be instantaneously moving forward with (very approximately) the velocity _ dp -£ +u dp determined by the corresponding values of p and w; so that M will be gaining on N at the rate ’] Aut! , [2 &xa 2 dp dp du approximately. We may admit then that the rate at which M gains on N is never < BAu, where B is a constant suitably chosen. Again, if Aju is the difference between the air-velocities at M and N at the time ¢=0, and 7g is the corresponding co- ordinate of M, we may admit that Ary 19 + at where A is a constant not very different from unity. Thus M gains on N ata rate which is Au, Aw is never < a 7 LESS = never < a Ser Ayu; and between the times t=0 and t=¢, the distance gained by M relatively to N will be at least ABAon| 0 4 pdt To + at : io salen ABAu”log °F“, : aR) 0 If B is finite and positive this expression increases indefinitely with the time, so long as the laws of continuous motion hold good. If Apr was the distance between M and N at time t=0, the time required for M to overtake* N will be not greater than the value of t, given by ie a —Ayr=ABAw log foie Yo or, when M and N are taken indefinitely close together at starting, by Tor Opps Ou log nt = a { AB( se oe 1.€., we have t =" en Gera. D) — 1) (15) ; ae * Cf. Lord Rayleigh, ‘Theory of Sound) vol. ii. p. 36. Sound- Waves of Finite Amplitude. 329 which gives us a finite upper limit to the time required for discontinuity to set in, provided B is finite. As our assump- tions only remain approximately true so long as the motion is continuous, (15) will only give an approximation to the time when discontinuity first commences, and accordingly the relation must be taken to refer to that part of the wave for which its right-hand side is a minimum. If B is negative (which is not the case for any known substance), the appro- priate part of the disturbance will be such that Qu/dr is positive. To determine approximately the value of B, we may refer to (13) and the inequality immediately following. If we assume Boyle’s law of pressure, so that / (dp/dp)=const., we have evidently B=1 very nearly. If we assume that the changes of density take place adia- batically, so that p ocp’ and y is nearly constant, the approxi- mate value of B becomes dap ee fd ie = oP. dp V dp : dp by means of (11) ; Date 9 e If, then, viscosity be neglected, we must conclude that under any practically possible law of pressure the motion in spherical sound-waves always becomes discontinuous, and a fortiori the same will be true of cylindrical waves. But inasmuch as our result for spherical waves depends on the existence of an infinite logarithm in (14) when ¢, is increased without limit, we may conclude that for waves diverging in four dimensions (or, more generally, in any number of dimensions finitely greater than three) there would be some cases where the motion remained always continuous. 11. The general question of spherical sound-waves of finite amplitude is by no means an easy one. In the case of plane waves we can write down at once from Riemann’s equations the condition that the disturbance may be propagated wholly in the positive or wholly in the negative direction. The respective conditions are* :— . wat |'a/P dose, Po dp where pp is the density of that part of the fluid whose velocity * Cf. also Lord Rayleigh, ‘Theory of Sound,’ vol. ii. p. 35 (8). 330 Dr. C. Burton on Plane and Spherical is reckoned as zero. No such simple criterion can be given for the existence of a purely convergent or purely divergent spherical disturbance ; a fact which may be readily seen from the equations for waves of infinitesimal amplitude. If ¢ is the potential of a purely divergent system of waves, we have rh=f(at—7), . te) where / is a function whose form is unrestricted. Let p be the ordinary density of the air, and p+6p the actual density at a point where the coordinate is r and velocity u. We have, then, on differentiating (16) the well-known relations 200 2) ) [Ga _ f(at—r) haan —_— ype y tea ° ° e (17) and 5 ; ogee *90— LAA"), Bees ees Pp From (17) and (18), (a2 —u)e=f(at—n), whence differentiating with respect to 7, and neglecting small quantities beyond the first order, neo —_ 8) 4 2r( a? —u)= —f'(at—?) by (18) ; therefore por 7 >; 2 ae (19) If, then, an infinitesimal spherical disturbance is to be purely divergent, this equation must be satisfied for every value of r. But since the left-hand side involves 6p/p as well as u, du/dr, and 9 (log p)/d”, it is evident that the question whether or not the equation is satisfied for some particular value of r does not depend solely on the state of things in the immediate neighbourhood of this value, but is influenced also by the value of p corresponding to the undisturbed air. We must not therefore seek to characterize a purely divergent dis- turbance by a differential equation expressing that, with respect to the air at each point, the disturbance is wholly propagated in the positive direction of r. 12. Not recognizing this, I had attempted to discover such an equation, and one step of the inquiry is reproduced here, for the sake of any interest which it may have. - Sound-Waves of Finite Amplitude. 331 Tt is required to write down the differential equation of an infinitesimal spherical disturbance, which is superposed on a purely radial steady motion. Though a steady motion extending inward to the pole would involve a violation of the principle of continuity, we may suppose that throughout a shell of finite thickness the distribution of density and velocity is such as would be con- sistent with steady motion ; the motion within such a shell would then continue steady, provided that its spherical boundaries were constrained to expand or contract in a suitable manner. In the absence of constraints the shell of steady motion would be invaded from without and from within by disturbances emanating from adjoining parts of the fluid, but, at points well within the shell, the character of the steady motion would necessarily be maintained for a finite time. Let ¢ be the potential of the steady motion. Let $+ be the potential of the actual motion so that and its derivatives are small. _Let p, p be the pressure and density in the steady motion. Let p +p, p+6p be the pressure and density in the actual motion, and assume that the pressure is a function of the density only. From the ordinary equations for the motion of compressible fluids we obtain = 3 (Sf), es (740) (rie 1 (SP +g oy) spk . ae ey GO) when small quantities of the second order are neglected. Subtracting (20) from (21) op - oOpow ee Ae (22) Now op _ dp op. pe dp pie therefore 0 op _ dp 10.o, ae Sieieds : Re ee (23) and the equations of continuity tor the steady motion and the 332 On Plane and Spherical Sound- Waves. actual motion may be written Op. _ 0¢ dp Cae °° See dp) 6 OP HPP) — — (p+ Bo) V°(h+H)— (SE + SHOR, whence by subtraction Oop Opdv dopded Sp PV PV b= 5 a, = 5 eee SG ) 3 was (2 (-+- SPS) fs expanding this and ee in (24) we get 00 ; __0¢0 eyes) BEM -o(Z) (45h) dp\— ,__ oP ov “Dot? (as) Fs ore dp\\/_ Od _ Hd _ I'GdW 79S eye Or Or Of Ores Nes Now differentiate (22) with respect to ¢ and we have, remem- bering (23), _ 4 243% _ lap 8p Or or rode: Ot! In this equation we have to substitute the value of Qép/dé from (25), and if we then put y= Wr, and perform the necessary reductions, we finally obtain as the differential equation satisfied By br, OX — (ew) SK + mw Ok 4 USK + v(S¥—%)= where a’=the variable 2 (in the steady iota Be a __ constant aie or pr? ie) 2u da __ 2u 2u oa ra ton2 (2) Ome. Vx 2au 2 (7) ; ae On a new and handy Focometer. 333 if the steady motion in question is a state of rest, «=O and p 1s a constant, so that U=0, V =0, and our equation reduces to the ordinary form for small spherical disturbances, If, on the other hand, y=, the motion may, through any finite distance, be treated as linear. We shall then have wu and p both constant, as well as a, and as before U=0, V=0. In that case Ovo Oh» OY 7 (?— ne =() YE (a?—wu Jan BE 5 and this, by a change of independent variables, is easily seen to be the appropriate form for small plane disturbances of a fluid whose motion is otherwise uniform. XXXII. On a new and handy Focometer. By Protessor J. D. Everett, /.R.S.* | ae focometer is designed to permit the distance of the _ “object”? from the screen to be varied, while the lens which is to throw on the screen an image of the “ object” is automatically kept midway between the two. This position, as is well known, gives both the sharpest definition and the simplest calculation. The instrument is constructed on the principle of the well- known toy~called lazy-tongs. A number of flat bars (fig. 1), OOOO all exactly alike, are jointed together in such a way that half of them are in one plane and the other half in a superposed | plane. With the exception of the end bars, each bar in either plane is jointed to three of the bars in the other plane, one joint being in the middle and one at each end. The end bars are jointed at the middle and one end only. All the bars in the same plane are parallel, and the two sets together form a single row of rhombuses all equal and similar, a side of a rhombus being half the length of a bar. The system has only * Communicated by the Physical Society: read February 24, 1893. Phil. Mag. 8. 5. Vol. 85. No. 215. April 1893. 2A 334 Professor J. D. Everett on a one degree of freedom, and its length is a definite multiple of the longitudinal diagonal of a rhombus. The joints are arranged in three rows, one down the middle and one along each edge, and the distance from joint to joint in any row is equal to this longitudinal diagonal. This common distance can be varied between very wide limits by pulling out or pushing in the frame, and we have thus a means of dividing an arbitrary Jength into any number of equal parts. I utilize only the middle row for this purpose, and utilize it only or chiefly for bisecting a variable distance. The pins on which the middle joints turn are continued upwards, as shown in fig. 2, to serve as supports for clips holding the object, the lens, and the screen. The lens is Fig. 2. Elevation. mounted on the centre pin, and the object and screen usually on the two end pins, as in fig. 2. In order to avoid flexi- bility, the clips are made short, and the pins, on which they are held by screws, rise only 14 inch above the frame. The base of each pin is a substantial disk (see fig. 3) which rests upon the table ; all the pins, not only in the middle row, but also in the two outside rows, terminate in such disks, which serve as the feet of the instrument, and slide upon the table when the frame is expanded or contracted. ‘The pins are of brass 4+ inch in diameter, and the bars are of +-inch mahogany, ? inch wide, and 13 inches in gross length. There are 18 of them, as shown in fig. 1. There are 9 pins in the middle row ; and when the object and screen are on the two end pins, the distance between them is divided by the other pins into 8 equal parts, any two of which should together make up the focal length. The unused pins are the most convenient handles for manipulating the frame. The screen may converiently be a piece of white card a little larger than a post-card, and a square of wire-gauze about half as big may be used as the object ; but a still better ‘ object’ is a cross of threads stretched across a square hole in a card. The light which passes through the square hole is very conspicuous on the screen before the correct distance is approached, whereas the shadow of the wire new and handy Focometer. 335 | gauze is almost invisible. Two thin cards about the size of post-cards should be taken, a hole a centimetre square should be cut through both of them, and they should be gummed together with the cross threads between them, the threads being in the first instance long enough to project beyond the eards to facilitate adjustment while the gum is wet. Waxed carpet-thread, or any very stout thread with smooth edges, is Fig. 3. A supporting pin. the best for giving a conspicuous and at the same time a sharp image. As the cross will sometimes have to be raised or lowered, the hole should be much nearer to one end of the card than to the other, in order to give a greater range of adjustment in mounting on theclip. One thread should be vertical and the other horizontal, in order that their simul- taneous focussing may serve as a check on the correct orientation of the lens. The instrument is intended to be used by placing it on a table of length not less than four times the focal distance which is to be measured. A lamp is to be placed either on one end of the table or on a stand opposite the end, at such aheight that its flame is about level with the tops of the clips. The clips should be fixed as low as possible on their supporting pins, unless it is necessary to raise them to suit the height of the lamp. In default of a lamp at the proper height, an adjustable mirror may be used instead, and made to reflect a beam of light from any large gas-flame in the room so that the beam shall pass along the tops of the clips. 2 A 2 336 Professor J. D. Everett on a When the lamp or mirror has once been adjusted to throw its light in the proper direction, it should not be disturbed, as all necessary adjustments can be better made by moving the instrument. The lens and screen may conveniently be mounted first, and the adjustments made so that the light collected by the lens falls on the screen as a horizontal beam. The cross is then to be mounted in such a position that a bright patch corresponding to the square hole is seen on the screen, sur- rounded by the shadow of the card. The frame must now be extended or compressed till the image of the cross appears in the bright patch ; and the lens, object, and screen should then be carefully set square by hand before the final adjustment. If the vertical and horizontal lines of the cross do not focus simultaneously, it is a sign that the lens needs setting square. The focussing having been completed, the distance of the object from the image is to be measured and divided by four. This will give the focal length ; and the calculation can be checked by measuring one or more of the four equal parts into which the distance is divided by alternate pins. Owing to slight play in some of the joints, or other mechanical imperfections, the theoretically equal distances may exhibit sensible differences, especially when the frame is nearly closed up; but the method of observation is so well con- ditioned that these inequalities do not practically affect the correctness of the result. In fact, if the distances of the lens from the object and image, instead of being exactly equal, are a+ and a—2, 2 2a fourth of the whole distance we are simply neglecting 2? in comparison with a?. Suppose the two distances a+a and a—x to measure 203 and 194 inches, which is a larger inequality than is likely to occur, the ratio of 2? to a? is 1 to 1600 ; and this error is negligible, in view of the fact that the doubt as to when the image is sharpest involves an un- certainty in the focal length to the extent usually of more than one per cent. : When the focal length does not exceed 10 or 12 inches, the instrument may be supported with the two hands and. pointed towards a gas-flame, which need not be at the same level, but may be at any height. A fairly good measure- ment can thus be made by one person, if there is opportunity for setting the instrument down on a table or floor when the lens needs setting square, and when the final measurement of distance is to be made. The friction at the joints of the 2 the true focal length is rs , and in taking it to be one new and handy Focometer. Boe frame is just sufficient to keep them from working while the instrument is being carefully set down. The chief difficulty is from flexure. Instead of receiving the image on a screen, it can be viewed in mid air. For this purpose I mount the cross on one of the two end clips, and a piece of wire gauze about the size of the palm of my hand on the other, setting the wires at a slope of 45° by way of contrast with the upright cross. The end which carries the cross should be turned towards the strongest light; as this renders the cross more visible to an observer behind the gauze, and also renders the glistening wires of the gauze more visible when the observer stations himself behind the cross. The adjustment for focus is made by lengthening or shortening the frame till parallax is re- moved. This is a very convenient way of establishing experimentally the fact of the interchangeableness of object and image. The instrument can also be employed to illustrate the general law of variation of conjugate focal distances, the lens being for this purpose shifted from the central pin to any one of the other pins, and the frame being then extended till the image is correctly focussed. Regarded as an optical bench, the instrument is remarkably light and handy. Its weight, including screen, cross, wire-gauze, and lens, is 2 lb. 10 oz. ; and a lecturer can carry it through the streets of a town without inconvenience. The dimensions and number of bars of the instrument as exhibited are recommended as the most convenient for general purposes. Ten bars only were constructed for the first trials, and any number included in the formula 4n+2 might theo- retically be employed. In order to prevent looseness at the joints, it would be well to make the holes in the bars bear against a cone below and another cone above, with a very slightly tapering wedge for adjustment, as indicated in fig. 3. If the instrument were to be set up permanently in one place, guides might be used for compelling the middle row of pins to travel without rotation, or the pin on which the lens is mounted might be a fixture; but as long as portability is to be preserved, | do not think that any arrangements for automatically preventing rotation would be practically bene- ficial. It is only in the large movements which precede the final adjustment that rotation occurs to any injurious extent. The instrument has been constructed from my drawings by Messrs. Yeates of Dublin, and the cost is trifling. [ 388 ] XXXIV. A Hydrodynamical Proof of the Equations of Motion of a Perforated Solid, with Applications to the Motion of a Fine Rigid Framework im Circulating Liquid. By G. H. Bryan”. Introduction. iE 1 the whole range of hydrodynamics, there is probably no investigation which presents so many difficulties as that which deals with the equations of motion of a per- forated solid in liquid. The object of the present paper is to show how these equations may be deduced directly from the pressure-equation of hydrodynamics, without having recourse to the laborious method of ignoration of coordinates. ‘The possibility of doing this is mentioned by Prof. Lamb in his ‘Treatise on the Motion of Fluids’ (pp. 119, 120), but he dismisses the method with the brief remark that in most cases it would prove exceedingly tedious. I think, however, that it will be admitted that the following investigation is more straightforward and simple than that given by Basset in his ‘ Hydrodynamics,’ vol. i. pp. 167-178. The usual method presents little difficulty when the motion of the liquid is acyclic, because the whole motion could in such cases be set up from rest by suitable impulses applied to the solids alone; anda consideration of Routh’s modified Lagrangian function shows that in this case the equations of motion can be obtained by expressing the total kinetic energy as a quadratic function of the velocity-components of the solid alone, and applying the generalized equations of motion re- ferred to moving axes. If, however, the solid is perforated, and the liquid is cireu- lating through the perforations, this method presents several difficulties. If the solid were reduced to rest by the applica- tion of suitable impulses, the liquid would still continue to circulate through the perforations, the “ circulation ” in any circuit remaining unaltered. From this and other circum- stances we are led to infer that these circulations are not generalized velocity-components, but rather that the quan- tities xp are generalized momenta. Now the kinetic energy of the system is naturally calculated as a function of the velocity-components of the solid and of these constant circu- lations (or the corresponding momenta) ; a form unsuited for obtaining the equations of motion. We ought either to have the kinetic energy expressed in terms of generalized velocity- components alone, or to know the “ modified Lagrangian * Communicated by the Physical Society: read February 24, 1893. Equations of Motion of a Perforated Solid. 339 function ” obtained by “ignoring” the velocity-components corresponding to the constant momenta or circulations. Hither of these expressions involves constants which cannot be deter- mined from the ordinary expression for the energy alone, and to determine them in the usual way it is necessary to resort to arguments based on a consideration of the “impulse” by which the motion might be set up from rest. In the following investigation the equations of motion are deduced from purely hydrodynamical considerations, and from them the modified function is found. In §§ 12-16 the equa- tions of motion are interpreted for the case in which the solid is a light rigid framework and the inertia is entirely due to the circulation of the liquid, and the results are applied to interpret the effective forces of the cyclic motion for a per- forated solid in general. General Hydrodynamical Equations. 2. Let a perforated solid bounded by the surface 8 be moving through an infinite mass of liquid (density p) with translational and rotational velocity-components wu, v,w, Pp, J, 7, referred to axes fixed in the solid, and let «,, «2, K3...Km be the circulations in circuits drawn through the various aper- tures. Then we know that ¢@ the velocity-potential of the fluid motion may be expressed as a linear function of the velocities and circulations in the form p=udut vpyt whut phy t Why t?hrt Zk. + (1) where evidently ¢,=0¢/du &c., and the coefficients dy... depend only on the form of the solid. If dy denotes the element of the normal to S measured from the solid into the liquid, (/, m, n) its direction-cosines, then, in the usual way, we have oe =I1(u—ry +92) +m(v—pzt+re)+n(w—getpy). . (2) The six coefficients gy... are single-valued functions of the coordinates, while the coefficients ¢, which determine the part of the velocity-potential due to the circulations are cyclic functions making Q¢,/Qv=O0 at the surface of the solid; these coefficients are supposed known for each form of solid, although their determination in any given case is generally beyond the range of mathematical analysis. 3. Let oj, o2,...0, be barriers drawn across the perfora- tions ; then, in the usual way, the kinetic energy of the liquid 340 -Mr. G. H. Bryan on the Equations of is found to be J, where ; 3 t= 1p |\p2% a+ 4px ||P do=B.+K. B3) Here J, is a quadratic function of the velocity-components of the solid, and is the kinetic energy when the motion is acyclic, and K is a quadratic function of the circulations. If the axes were fixed in space, the pressure equation (supposing no forces to act on the liquid) would be Pi , of pot (where p; = pressure, g, = resultant velocity of liquid). Owing to the motion of the axes, however, O¢/Q¢ must be replaced by the rate of change of ¢ at a fixed point, that is by — +3$9,)’=const., dp aan ee op an) O° o¢ a. Uo te) a — sep tet) a ee whence the pressure equation becomes — | Pi, Uh ae OG _ pede OF _ = we me ee) (wv RUS, (5 2 +39°= const. eae 5 | st.) The Mutual Reactions between the Solid and Liquid. 4, Let X,, Y;, Z;, L,, M,, N, be the component forces and couples which the solid exerts on the liquid ; then we have evidently Seas L, = \\ (ny—mz) p, dS. 21s GD) _ To reduce these expressions to the required form, we shall have to resort to repeated applications of Green’s formula. Since the velocity-potential @ is a multiple-valued function, it follows that in transforming volume integrals involving } we shall obtain surface integrals over the barriers 01, dg,... Om as well as over 8S the surface of the solid. On the other hand, the pressure p, and the velocity-components 04/02, 0¢/dy, 0¢/02 are single-valued and do not contribute barrier terms to the surface integrals. Moreover, since the circulations « are independent of the time, OF = Ub, +E, FI, + D4, +98, 476, and 0¢/0¢ is therefore a single-valued function of the velocity- components of the solid satisfying Laplace’s equation. Motion of a Perforated Solid in Liquid. B41 We also notice that Ody feke) l= a Ye ao ate mare tts (6) as may be at once seen by differentiating (2) with respect to w and p respectively. Substituting for p, in (5) in terms of the velocities, we have =e sale ds p : + {lf (u—yr + . + (two similar) F1US —al|{ (Sey y+ (38) ] pee The first line of a expression is, from (6), equal to ee Ou a eerar rome by Green’s transformation. os. that @, is inde- pendent of the time, this integral, taken throughout the liquid, becomes =523 2 al|i{ (S*) ey (82) } ans - pot OL ILS) esa ~ pdtou pot ou — By Green’s transformation the second line is equal to ={\\3 { (u—yr + 2q) oF + (two similar) \ dx dy dz = ~ {{\(-22 ¢ at a) dx dy dz -\\\f (u—yr + 2q) 2 + (two similar) ae dy dz, which by a second application of Green’s transformation becomes Oo 49 Mr. G. H. Bryan on the Hquations of =\| (mr—ng) dS —Zx\\(mr—ng) do + (V{2(u —yr+2q) + m(v—eptar)+n(w—agt+ yp) $ Seas 0p oe =(\(mr —ngq)odS— Sxc\\(m —ny)do +\| ae ds by (2). Lastly, the third line of (7) is, by Green’s transformation, "(Bb9% , 96 B'S , BH dS ={\\{8 Seo SRORRUN e serps p aedyde “(£29247 Ov 02 a Hence, adding the several terms together, we have The ~ dt Ou 1p {p\\modS = S«p\\mdo} — qip\\nodS _ Sxp\\ndo} 8) Now by (6), p\\mddS=p Obe 478 i {| Ov -e|\| OPIS: , BHIb. , BHO» a Ode =Sep| Be Sane AF an aie ~~ \da dy dz ~sl] ie Zaof NG) + REF) Jere = ao | 2 eee Therefore ie = g2_, £2 , aaa we a ”) da} +9 { S= oe " Cia 6. In like manner we have — ae-{f (ny —mz) as +]| | (u~yr+ - a (two similar) (ny—mz)dS Motion gi 6,08 Solid in Liquid. 343 LO +B“ 08) Jom “Hboe Yas) (v5! - so) du dy dz — ||) fy { e-yrte0) 2 + (tro. similar)? 9% =z} (w—yr+ 2q) o + (two similar) a dx dy dz On 060 , Of 0 , 060)/(,0b_,0¢ oe By t Bebe) Uae: 0 y Naadyde eee 02 pdt op Bs (two sim.) poste ve - $98 —\\\[o(9s 5 eave “(P5o fol ‘ oe) Shey yp eee Se Gye 9) — \da dy dz. (v—zp+2r) e + Cw “g+yp) By c dy Remembering that in this expression one factor of the surface integral is zero at every point of S, we have, by again applying Green’s transformation to the volume integral, ar made Op +w{ p\\m dds —Zxp\\mdo} —vf p\\npdS —Sxp\\ndos +r{p\\(l (le—nx) dds — —Xxp\\( (lz—na)do} —qip\\ (ma—ly) ddS — — xp \\ (ma—ly\do$ . . (10) Now, just as before, (le—mn)bdS= p || Pega all = =Sxp || 2 , da 2, (ieee 388, feb Od, 738 08, \ zi a: alll oe = Seo (( 0% gq © =3ep [|Site 0g’ 344 Mr. G. H. Bryan on the Equations of Therefore, d OL 1 = dt Op —w foe + Sep ||(m — oP de \ tne) ge a eo {| (n— =) da | 7 1 oe + xp | (t: —nw— ee da \ +g = == Sap || (may eae} Beene ul Application to the Equations of Motion. 7. The equations of motion of the solid may now be written down at once. Let 3! be the kinetic energy of the solid, T the total kinetic energy =%+ ‘3! ; and suppose that the motion takes place under the action of a system of external impressed forces and couples designated by X, Y, Z, L, M,N. Then the effective forces and couples to which the motion of the solid itself is due are X—X,..., L—L,..., respectively, and the six equations of motion of the solid referred to the moving axes are of the form dIOS LOS! Hawes! , dau "90 ' 230 ~~ 9 ne AS) SSG Sole Se tn Se ; q dt Op Ov w OY or Hence, on substitution, we see that the required equations of motion are found by writing T tor J and X, Y, Z, L, M,N for X,, Y;, Z;, L;, My, N, in equations (9) (11). The resulting equations may be written : x= 55, -"(85 +7) +{& +5) yr (14) t= ae = 0(S +0) 40o(& +6) =L—1L,. e (13) where &, 7, &, d, “, v are defined by the equations Motion of a Perforated Solid in Liquid. 345 g = 2xp|| (I 2 ada, de, ee (16) N= sep || (x (ny— mz— 928 \do, ewe te ce El) As Lamb has pointed out (‘ Motion of Fluids,’ p. 140), the six quantities (&, 4, ¢, A, w, v) are “the components of the impulse of the cyclic fluid motion which remains when the _ solid is (by forces applied to it alone) brought to rest” *. They are linear functions of the circulations and their form depends on the form of the solid. If there is only one aperture they - are all proportional to the circulation «. The Modified Lagrangian Function. 8. We shall now show that the motion of the solid can be determined in terms of Routh’s modified Lagrangian function, and shall find the form of this function for the system. Putting. H=T+éEu+nvt+Gwt+rAptpqtvr+F (kp), . . (18) where F'(«p) denotes any function whatever of the quantities Kp, we see that the equations of motion reduce to the standard form @ lel oat lal ir iu eae (iey OE ele! OH “Olt. @ils! : The function H, therefore, plays the same part in deter- mining the equations of motion of the solid as the kinetic energy T in the case of an imperforated solid (or any solid when the motion of the liquid is acyclic). It remains (i.) to determine what quantities are to be regarded as the generalized velocities if the quantities xp are regarded as generalized momenta ; (ii.) to find the form of the function F(«p) in order that H may represent the modified Lagrangian function. 9. Let y,, be the generalized velocity-component corre- sponding to the ignored momentum «,p. Then, as Routh has shown (‘ Rigid Dynamics, vol. 1. § 420), the modified La- grangian function H is of the form Ev > in PNR Oe hal F<. ce ts. E28) * Our & 7, 6, A, w, v are the same as the &, no, fo, A 0) Hoy Yo Of Lamb, or the’ X,Y), 3, &, Mi, "I of Basset’s § Hydrodynamics.’ 346 ‘Mr. G. H. Bryan on the Equations of and therefore by equating the two expressions for H we must have Eutnutfotrptpqtwr+F (x) =—ZKpy. . ~ (22) Since y,, is the generalized velocity-component corre- sponding to the momentum kmp, therefore oH 0. Kp = Xm ° . ° ° e (23) Now H is a homogeneous quadratic function of the six velocities (u...,0...) and the momenta xp; therefore | oH oH oH 2H =2u s- + Sxp sae == 7 —Xkpy. . (24) Hence, from (21), . H H H 2139 + Sepy = Sud Sapo AS 5) The portions of T and H which involve only the momenta xp, and are independent of the six velocities (u..., p...), must arise from the terms 2«py in the above expressions (24) (25), and must therefore be equal and of opposite sign in the ex- pressions T and H respectively. Hence, since from (8) T=2'+3,+K, the portion of H which is independent of the six velocities (@..., p...) must be —K, so that, H=2/4+ 31+ (ut nut Gwt+rApt+pyqtvr) —K =T +(Eutnvtcwt+rAptuqtvr)—2K, . . (26) and therefore F(ep)=—2K. .. The function F'(«p) does not enter into the six equations of motion of the solid, but its form requires to be determined if we wish to reduce the equations of motion of the whole system to the canonical or Hamiltonian form. The Generalized Velocities and Momenta. 10. Comparing (21) with (27), we see that LKpX=2K—(Eu+ nu+lwt+rApt+puyqt+vr). . (28) Now equation (3) may be written in the form Bigg ih) malas +...tp,+...+2«,)d8 +24 2 (ug, + 1 tpbyt...+ 2kde)do. (29) Motion of a Perforated Solid in Liquid. B47 ~ But by § 2, 0¢,/0v=0 all over the surface 8 of the solid. Hence, equating the terms independent of the six velocities (w...,p...) on the two sides of (29), we have 79 C= , », v being integrals taken over the finite surfaces of barriers are in general finite. If we choose as our axis of wx the Poinsot’s central axis of the impulse whose six components are &, 7, £ Ar, @, v, the modified function will reduce to the form H=ButAp—Ki eee If there is only one aperture, &,7,¢, 2, u,v are all pro- portional to the circulation « and the central axis of the impulse is fixed in position relative to the solid: if there are several apertures the position of the axis depends on the ratios of the circulations through the various apertures, but throughout the motion it in every case remains fixed rela- tively to the solid. The six equations of notion (19) (20) now reduce to rl); 0, ) Nears, M=wE+rA, " 54.) ee ) Motion of a Perforated Solid in Liquid. 349 Since these equations do not involve w or p, we see that no forces will have to act on the solid in order to maintain a screw motion whose axis coincides with the central axis of the umpulse. 13. To interpret the equations still further, let us suppose that w and p are both zero, since they do not enter into the equations of motion. ‘Then the motion whose components are (0, v, w, 0, g,7) consists of two screws whose axes are the axes oi y and z respectively, and, by the theory of screws, these are equivalent to a single screw whose axis is a certain straight line intersecting the axis of # and perpendicular to it. We may take this straight line as our axis of ¢, for hitherto we have only fixed the position of the axis of «. We have then v=0, g=0. The equations (34) therefore reduce to 4 xXx—(; L=0, Y=7e, M=we +a} eee too) Zi=), N=0: Hence the solid is acted on by a wrench (Y, M) whose axis is the axis of y. Thus the axis of the impressed wrench is perpendicular to the central axis of the impulse of the fluid motion, and to the axis of the screw motion of the body. Let II be the pitch of the impulse, w the pitch of the screw motion of the solid, P the pitch of the impressed wrench, then | A w M N=5, ee Pay and therefore by (35), | Pesan LL fae Aisa ok: 1a (Gl) is the relation connecting the three pitches. In particular, if » = 0 the equations of motion give Z=0, M=wé#, showing that a couple M about the axis of y will produce translational motion with velocity M/E along the axis of z. 14. More generally, let the motion be a screw motion about an axis whose inclination to the axis of w is @ and whose shortest distance from that axis is a. Take this shortest distance as the axis of y, and let the screw motion consist of a linear velocity V combined with an angular velocity ©, the pitch V/O being denoted, as besore, by a. Phil. Mag. 8. 5. Vol. 35. No. 215. April 1893. 2B 350 Mr. G. H. Bryan on the Equations of It will be readily found that the six components of the screw motion are u=Vcosd+QOasiné, p=Ocosé, v=0, q=9, 3 - (87) w=VsinOd—Qacosé, r=Qsin 8, so that the equations (34) now give A=0, 1;=0, Y=02siné, M=VEsin@—Oaz cos 0+0A sin | (38) =: N=0, The impressed wrench therefore has for its axis the shortest distance between the axis of the screw motion of the solid and the axis of the impulse of the cyclic fluid motion. To find the pitch of the wrench, we have, by division, = = 5 —a.cot 0+ = that is, P= e—acot@+Il. .. 7) yee 15. In the case of a fine massless circular ring A vanishes, or the impulse of the cyclic motion is purely translational. For it is clear that the axis of the ring is the axis of this impulse (the above axis of z), also the fluid motion will evidently be unaffected by rotating the ring about its axis; and therefore the modified function is independent of the angular velocity p. The equations (34) now become K—0; L=0, Se), M=we, | (40) ZL=—q2, N=—vée. Hence a constant force Y along the axis of y causes uniform rotation with angular velocity Y/E about the axis of z, and a constant couple M about the axis of y causes uniform translational velocity M/E along the axis of z. It is to be noticed that the impressed wrench never does work in the resulting screw motion, in accordance with the principle of Conservation of Energy. 16. The above results show the effective forces produced by circulation of the fluid on any perforated solid whatever. In the general case the modified function contains the quadratic terms 2+, in addition to the terms of the first degree con- sidered in the above investigation. If we suppose that the solid is moving in any given manner, the six equations of motion (19, 20) determine the components of the impressed wrench (X, Y,-Z, L, M, N) necessary to maintain the given Moton of a Perforated Solid in Liquid. 351 motion. This impressed wrench may be divided into two parts, one being due to the terms 3/+2Z, in the modified function, the other being due to the terms Eutnvt+ GwotrAp+pg+yr. The first portion is the same as if the motion were acyclic, and represents, therefore, the wrench which would have to be impressed on the solid in order to maintain the given motion if there were no circulation. The second part represents the additional wrench which must be applied on account of the circulations, and the equations to determine it are of the forms found above. We notice, in particular, that if the solid has any screw motion whose axis coincides with the axis of the impulse of the cyclic fluid motion, the latter wrench vanishes; so that the forces required to maintain the motion are unaffected by the circulations. In other cases the additional wrench is about an axis perpendicular to the axis of the impulse. This is true whatever be the form of the solid and the number of the circulations ; but, as has already been pointed out, the position of the axis of the impulse relative to the solid is not in general independent of the circulations unless the solid has . but a single aperture. It is probable that these results might be made to furnish mechanical illustrations of certain physical phenomena ; but with these we are not concerned in the present paper. Note on the foregoing Paper. Concerning the proper measurement of the impulse of the eyclic motion, a difficulty arises ; for, as Mr. Bryan remarks, this motion cannot be set up from rest by impulses applied to the solid alone. Suppose, however, that we close each perfora- tion by a barrier in the usual way, and let the barriers be acted on by the impulsive pressures xp, K.p,... respectively. And instead of these impulsive pressures being due to external forces, suppose that they are due to some immaterial mechanism attached to the solid. In general, an impulsive wrench must act on the solid to keep it at rest, and this wrench ts the required impulse of the cyclic motion; for the only other impulses acting on the system are due to the mutual reactions of the solid and fluid, exerted partly over the surface of the solid and partly through the barriers and attached mechanism, and such mutual reactions cannot affect the impulse. The wrench thus found is of course the same as would be obtained by supposing the impulses on the barriers to be due to external impulsive forces, and compounding with these the 2B2 352 Mr. G. H. Bryan on the Equations of impulse then necessary to hold the solid at rest. This is in agreement with Prof. Lamb’s investigation, which Mr. Bryan has quoted. More generally, if the solid is in motion, and the liquid is also circulating, we may suppose the instantaneous motion to have been set up from rest by an immaterial mechanism con- necting the barriers with the solid at the same time that the requisite external impulses act on the solid. The resultant of these last is, as before, the impulse of the whole motion, and is identical with that found by supposing the barriers actuated by impulses from without, and compounding with these the impulse then necessary to give to the solid its instantaneous motion. The same point may be further illustrated by supposing the circulations « to vary continuously during the motion. To effect this variation we may suppose finite uniform pressures, P,...P,,, to be exerted over certain ideal surfaces which occupy the positions of barriers. The rate of variation x of any circulation is given by P=xp, and in order that it may take place without the direct operation of external forces and couples we may conceive the pressure P to be due, as before, to some highly idealized mechanism attached to the solid. As before, the only forces capable of modifying the impulse are the external forces acting on the solid ; and the equations of motion are therefore still to be found by equating the impressed force- and couple-components to the corresponding variations of the ‘‘ impulse.” Since we know the expressions for the impulse-components corresponding to a given instan- taneous motion of the solid and given circulations, we have only to remember that in these expressions the «’s are functions of the time, and, just as before, the equations of motion are directly deducible from Hayward’s formule. Hquations (19) (20) of Mr. Bryan’s paper will thus be applicable to the present case, provided that in the value of H given by (27) the «’s are allowed to vary. 7 An investigation proceeding from a consideration of the impulse of the whole motion is not so entirely satisfactory, I think, as the direct method given by Mr. Bryan ; but, at the same time, this brief attempt to interpret the impulse of the cyclic motion may not be without interest.—C. V. Burton. — Note added by the Author. Dr. Burton’s note is of much value as showing more exactly what is meant by the “ impulse ” of the motion in the Motion of a Perforated Solid in Liquid. 353 ordinary investigations given by Prof. Lamb, and, in a less intelligible form, by Basset. The equations of motion under finite forces may be deduced by equating the change of momentum in a small time-interval d¢ to the impulse of the impressed forces, taking into account the fact that in the interval 6¢ the origin has a displacement of translation (wdz, vdé, wot) and the axes have rotational dis- placements ( pdt, g6t, 76¢), so that the final momenta are referred to a different set of axes to the original momenta. The mode of forming the equations of motion is given by Prof. Greenhill (Encyclopedia Britannica, art. “ Hydro- mechanics ’’) for the case of acyclic motion, but it is hardly so obvious why in thus forming the equations of motion of a perforated solid, it is necessary to include in the “impulse” terms representing the components of the wrench applied to the barriers as well as to the solid. We may, however, sup- pose the changes which actually occur in the time o¢ to have been produced as follows :— 1st. Let the solid and fluid be reduced to rest by an impul- sive wrench applied to the solid, and transmitted to a series of barriers crossing the perforations. The components of this ~wrench will be found to be ot or au + &, SCT ap +r, &c. ... 2nd. The barriers being rigidly connected with the solid, let the latter receive small displacements whose translational and rotational components are (wot, vdé, wot, pdt, godt, rdt) and let the solid come to rest in its new position. The fluid will evidently also come to rest, and therefore no impulse will be impressed on the system by this change (as may be otherwise seen by supposing the change to take place very slowly). 3rd. Let the solid be set in motion with velocity-compo- nents (w+ Qu/dt.dt,... ptdop/dt.dt...) referred to the new positions of the axes, and let the circulations « be started in the new position of the solid by a suitable impulsive wrench applied to the solid and transmitted from it to the barriers. Then the impulse of the impressed forces (components Xdt..., Ldt...) is the resultant of the wrenches required to stop the whole system in the first process and to start it again in the third. It is, therefore, that impulse which must be compounded with the total impulse in the initial position in order to obtain the total impulse in the final position. Whence Hayward’s equations of motion follow at once (as or 354 Prof. G. M. Minchin on the Magnetic shown in Greenhill’s article above referred to), and they take the form of the above equations (14), (15). If we were merely to stop the solid in the first process without stopping the liquid, the cyclic motion would cause the liquid to exert a pressure on the solid in the second pro- cess, and the impulse of this pressure would not be zero, but would have to be taken into account in forming the equations of motion. It would be wrong, therefore, to deduce the equations of motion from the impulse applied to the solid alone, as is evident in the analogous case of a solid containing one or more gyrostats. XXXV. The Magnetic Field of a Circular Current. By Professor G. M. Mrycuty, 1.A.* LERK MAXWELL gives a method of drawing the lines of magnetic force due to a circular current (‘ Hlectricity and Magnetism,’ Art. 702) by means of a series of circles and a series of parallel lines. ‘The object of the following paper is to show how these curves can be described by a slightly different method, and to exhibit the geometrical connexion of the series of circles. Let AQBQ' be the circular current whose sense is indicated by the arrows, the plane of the circle being that of the paper; Fig. 1. ene, ~ 2 fee es Se et ee let P be any point in space, PN the perpendicular from P on the plane of the circle, and NAOB the diameter of the circle drawn through N. We shall calculate the vector potential of the current at P. Draw any ordinate, QQ!, of the circle perpendicular to BA; and consider two equal elements of length of the circle, each equal to ds, at Q and Q!. Resolving each of these along and perpendicular to QQ!, we see that the latter components are in opposite senses, and hence their vector potentials at P cancel * Communicated by the Physical Society: read March 10, 1893. Field of a Circular Current. 355 each other, since PQ = PQ’. If Ww is the angle QOA, a=radius of circle, 1=current strength, the components of ids along Q’Q being equal and in the same sense, the two elements of current at Q’ and Q conspire in giving a vector 22 cos PQ Hence the total vector potential at P is perpendicular to the plane PON. -If, therefore, OA is the axis of «x, the perpendicular at O to the plane of the circle the axis of z, and the diameter at O perpendicular to AB the axis of y, the components of the vector potential being, as usual, denoted by F, G, H, the only component existing is G; but, by taking the components of the vector potential at a point indefinitely close to P in the direction of the axis of y, we easily find that potential .ds perpendicular to the plane PON. ae _G | dy = a" Hence if X, Y, Z are the components of the force of the current per unit magnetic pole at P, since this force is the curl of the vector potential, we have dG dG G Sa aa, Yi = (): L=— + oe? where 2(=ON) and y (=NP) are the coordinates of P. If along the line of force at P the increments of the co- ordinates are Aw, Ay, we have ae GE VA Hence along this line we have AG dG G Tn At + a + — Aas 0, i.€., G.e= constant along the line of force. We shall therefore calculate the vector potential, G, at P. Hvidently G = 2i| SON 5 0 PQ a nd 9 VMat+a+y*?—2aecos p e 2 "e+e pty? avian : D —D) dp, 356 Prof. -G. M. Minchin on the Magnetic denoting the denominator by D. Now let ~p=a—o, and let p?=(a+a)?+9’, p?=(a—a)?+¥4”’, so that p=PB, p'=PA. Then ay o wT p> +p? ie, t G= 2a‘, 1 ihe 2pA ¢ do, [2 = A=A/ 1—(1-§) sin? $. 7 Let o=2¢, and Bal — Gs: then, finally, where hia (res <2 {pK-8)-K}, where K and E are the complete elliptic integrals of the first and second kinds with modulus &; so that the quantity in brackets is a function of the ratio — simply. | 27,2 Also, since p?— p”=4aa, we have a= ee G .« which is constant along the line of force is given by the equation ,and the quantity G .a=ip{2(K—E) —#’K}. It is thus seen that at every point in space G is of the ! form . if. c ) ; so that at all points on the surface for which : is a constant, the value of G will vary inversely as p. The I surface for which © is constant is a sphere having its centre on the line BA produced and cutting the sphere having BA for diameter orthogonally. If we assign a series of values to ! the ratio f. we obtain a series of spheres having their centres on BA and cutting the given sphere orthogonally, the radius of each sphere of the series being, therefore, the length of a tangent from its centre to the sphere described on BA; for, given the base, BA, of a triangle, and the ratio of the sides, the locus of the vertex is a circle whose diameter is the join of the points which divide BA internally and externally in the given ratio. The surface locus of the vertex is the sphere generated by the revolution of this circle. > Field of a Circular Current. 357 On account of the symmetry of the current round its axis through O, the lines of force and those of constant vector potential are the same inall planes through the axis. We may, then, confine our attention to the plane PON, and suppose fig. 2 to be in this plane, the current being Fig, 2. in this figure represented in projection by the line BA. Describe a series of circles having their centres on BA pro- duced and cutting the circle described on BA as diameter orthogonally. Along each of these circles, then, the ratio ee es e e e PB is constant, P being any point on the circle. Consider first the lines of constant vector potential. For each of the circles let the value of the quantity 2 (K—E)—K be calculated. Denote this quantity by Q for any one circle ; then Q — AQea p so that if we wish to trace out the line of constant vector potential for which G has any given value, we can find the point, P,in which it cuts any circle of the series by measuring 358 Prof. G. M. Minchin on the Magnetic the length PB such that 4 _ 4Q PB=-G. 4. Let PT be any circle of the co-orthogonal series cutting BA at nand m. Then for this circle i p Bn mB’ and if this ratio is denoted by s, it is well known that Or Ue Cam where C is the centre of the circle. Now the modulus, &, of the elliptic integrals which belongs to the circle mPn is Ag 1 Pe) he Ba1—sts hence AB 2 AD a BC’ or the square of the modulus is inversely proportional to the distance, BC, of the centre of the circle from B. The circles employed by Clerk Maxwell in drawing the lines of force can be easily shown to be this co-orthogonal system whose centres are ranged along BA produced. For, his rule is to assign a series of values to @, and construct a series of circles whose centres lie on BA, the radius of each being 5 (cosec 6—sin @), while the distance of its centre from O is 5 (cosec 9+sin @) ; the modulus belonging to this circle is sin 8. For the series of circles he then calculates the values of the expression (constant for each circle) sin 6 (K—H) assigned line of force is found by drawing a certain right line perpendicular to BA. It is at once found that this series of circles is precisely the co-orthogonal system above described ; but Clerk Maxwell’s modulus is not the same , and the point on each circle which lies on any ! function of the ratio = or of the radius of the circle selected, Pp as that adopted above; for, with Clerk Maxwell, if r is the radius of any circle of the series and & the corresponding modulus, es (z— k), 2 \k Field of a Circular Current. 359 whereas above we have _2V71-# f= je eo. Of course (as stated in a note by Clerk Maxwell) the elliptic integrals depending on the one modulus can be transformed into elliptic integrals depending on the other ; and in this case the transformation is the well-known one of Lagrange. But the constructions for the points in which any given line of force cuts the series of circles will not be the same in both cases—those of Clerk Maxwell depending on a series of right lines perpendicular to BA, and those above indicated de- pending on a series of radial distances from B. When we propose to draw the line of constant vector potential through any point, P, which lies on a circle whose constant is Q,, let PB be p); then the point, R, in which this line meets any other circle, whose constant is Q,is found from the relation men he Ge where p= BR. This latter method has a certain advantage for the eye, inasmuch as it enables us to see readily those circles of the series outside which the line of constant vector potential through any proposed point lies. Consider now the lines of force. With the above value of © Q, the quantity which is constant along a line of force is p.k’Q, so that on each of the above circles in fig. 2 we must now mark the number £?Q. Denote this by Q’. Then the above relation for points on the same line of constant vector potential becomes for the lines of force / p= and the construction proceeds in the same way. The con- stants, Q’, for the above series of circles, beginning at the innermost, are :— "A841; :4301 ; °3775; °3396; °2782 ; °2376; :1954; °1727. . The values of the Q’s diminish outwards for the circles; so that if we consider the line of vector potential at any point, S, suppose, which is such that SB is greater than the distance from B of the point along AC in which any circle interior to that passing through 8 cuts the line BAC, it is at once obvious that the line of vector potential which belongs to 8 is wholly outside all such circles. The numerical values of Q for the 360 Prof. G. M. Minchin on the Magnetic circles in fig. 2 are marked at the circumferences, and as much of the line of potential belonging to P is drawn as is justified by the number of circles represented in the figure. The fundamental proposition of electromagnetism is that the intensity of magnetic force produced at any point in presence of electric currents is the curl of the vector potential Fig. 3. A P Q B P 0 at the point. But if in the field there is a current in an in- finitely long straight wire, AB, we find that at every point in the field the vector potential due to this current is infinite. Hence it seems impossible to deduce the magnetic force, and the lines of magnetic force, from the above fundamental pro- position. This result is unsatisfactory, and it manifestly points to some defect in our definition of the vector potential. We are presented with a similar unsatisfactory result in the general theory of gravitation potential. Thus, taking the common definition of gravitation potential, if AB is a limited uniform bar attracting according to the law of inverse square, we know that the potential which it produces at any point, P, is proportional to log (cot > cot =) where A= 7 PAB; B=ZPBA. Now, if the rod extends to infinity, this ex- pression becomes infinite. I have shown (‘ Statics,’ vol. ii. Art. 332) how this difficulty arises, and how it is to be remedied by mending the definition of potential. The diffi- culty is avoided in a similar manner with regard to the vector potential. Thus, since we are concerned only with differential co- efficients of the vector potential, the ordinary components, F, G, H of this vector may have added to them any constant quantities whatever. This amounts to saying that the vector potential at any variable point, P, in the field is the vector potential at any fixed point, O, plus the vector difference between P and O. It does not matter whether the vector at O is infinite or not: it is a constant in the field. As in the general gravitation field we are concerned with dzjerences Field of a Circular Current. 361 of potential only, so in the electromagnetic field we are concerned with vector differences only. Let us, then, calculate for the infinite straight current AB the vector difference between P and a point O on the per- pendicular, Pp, at a constant distance Op=a from the line. Let Pp=r, and let an element, ds, of the line AB be taken at any point, Q; let 2pPQ=0. Then the vector difference, Ea hdis ds due to this element, at P is OP —Q07™ M7 + (a—2") cos’OS * cos 6" Double the integral of this from 0=0 to 0= 5 is the vector difference at P due to unit currentin AB. LHxpanding the Py poe ge )s we have the radical in ascending powers of » Cc 3 vector equal to 0. ee ee Lac 2f {an 7g 008 Ot oe ate COW 6 oo Palen) =—4$n? +40? —FAt+ sirens and this=log,(1 +) =2 log- . Thus, then, the vector dif- ference at any point, P, is measured by C—2 log», where C is a constant; and this gives the known value of the magnetic force at P, viz., — a (where G is the vector potential), perpendicular to the plane PAB, i.e. where & i isa constant. In this way, then, the inconvenience of deal- ing with an infinite vector potential in presence of an infinitely long (or very long) straight current is avoided. e lines of constant magnetic potential, or the loci of points, P, at which the given circular current subtends a constant conical (“solid”) angle, are the orthogonal trajec- tories of the lines of force, and can be drawn when these lines are drawn. It is not easy to draw these equipotential curves independ- ently, or even to deduce their typical equation from that of 362 Prof, G. M. Minchin on the Magnetic the lines of force by the mathematics of orthogonal trajec- tories. The magnitude of the conical angle subtended at any point by a given circle can be expressed in finite terms by means of complete elliptic integrals of the third kind. The para- meter involved in these integrals will depend on the way in which they are taken. If a sphere of unit radius is described round P as centre, and lines are drawn from P to the points on the circum- ference of the given circle, BMAI, fig. 4, these lines will intercept on the sphere a spherical ellipse, bmat, whose area is the conical angle subtended by the circle at P. The minor axis of this ellipse is the great circular are ab determined by the lines PA, PB, while the major axis, mi, is determined by the chord, MI, of the circle which subtends a maximum angle, MPI, at P. This line is determined by drawing the bisector, Fig. 4. PC, of the angle BPA, meeting BA in O; then MI is the chord through C perpendicular to the plane BAP. The point cin which PC meets the surface of the sphere is the centre of the spherical ellipse. Now, given any curve, mpi, fig. 5, on a sphere of unit Fig. 5. radius, its area is ja cos #)dg, where, if o is any point on the sphere inside the area, @ is the circular measure of the Field of a Circular Current. 363 spherical radius vector op drawn to any point, p, of the curve, and ¢ is the angle between the radius op and any fixed arc, oa, drawn ato. If, as said, the pole o is inside the area, goes from o to 27; but if o is outsede the curve, the area has a different expression, viz.:— if cos Odd, the longitude angle ¢ obviously starting and ending with a zero value. If o is on the curve, the expression for the area is again different. In calculating the area of the above ellipse it would be natural to choose for pole (0) the point n in which the sphere is cut by the line PN; but this leads to difficulties when the position of P is such that n falls on the ellipse. This will happen when P is on any perpendicular to the plane of the circle of the current drawn at any point on its circumference; and, moreover, the choosing of n for pole will lead to expres- sions for the conical angle which present its values in forms which are apparently discontinuous for points P which project inside and outside the area of the given circle BMAI. Such discontinuity must not exist, and to get rid of it from the expressions requires troublesome transformations of elliptic integrals of the third kind. We must, then, choose for pole a point which is always inside the spherical ellipse. The simplest point is the point o (fig. 4), in which the sphere is cut by the line PO which joins P to the centre, O, of the given circle. This point is, of course, always inside the ellipse. Let, then, Q be any point on the given circuit, and p the point in which PQ cuts the ellipse. Taking for the fixed plane of longitude through o the plane baP, or BAP, and denoting the angle poa by ¢@, the area of the ellipse is (7d —cos op)dd, i. e., 2a —{ "cos op .dd. Denoting, as before, the position of Q by. the angle , or QOA, we easily find, if PN=z, PO=r, ON=a, v2 d = 6 ° © e d vo) 27 + at gin” ap Vr, — —ax cos cos 00 = aaa Pr / y+ a — Que COS yp? Hence ar ty 2 7” — AL COS cos op -dp=2e | be CONN Gs EY 0 0 Vp +a’—2arcosy 2 +2° sin“ 364 The Magnetic Field of a Circular Current. Putting ~~=7—y, this becomes dy ? 2e| Jea/1—Psi?§ — Hsin? X + 75 Paap bs STi aang SPOOR sin [2 where, as before, p=PB, p'=PA, and ?=1— ie . If we put ¥=2e, this becomes if A ; ye — a? da | naga? pA / 2? +2’ sin? 20’ where A= V 1—F?’ sin’ o. To reduce this to elliptic integrals, we must resolve the fraction 1/2? + 2? sin? 2 into two fractions. It is easily found that xo) 2+2" sin’ 20=2 +42’ (sin? o—sin* o) =(V72+0?+a—24 sin? o)(V 2 +2?—a2+4+ 22 sin’ @). Let v denote the sine of the angle between PO anu the axis of the current (or PN); then the expression, after resolution into partial fractions, becomes vad =D i 1 akc ASN oS eee i itv iyawe) The aia of this expression which has A in the deno- minator is at once the sum of two complete elliptic integrals of the third kind; and the portion which has A in the nume- rator is easily reduced to the same form. The result is eae a 0 where N=1—v+ > sin’w, and N! is the value of N when v is changed to —v. Hence we have two elliptic integrals of the third kind, one with (= ae , k) for parameter and mo- dulus, and the other with (— 1l+y then, we have for the oe expression of the conical angle subtended by the circuit at P the value ae crs aha , #). In the usual notation, eee eae pr = On Hydrolysis in Aqueous Salt-Solutions. 365 Of course it is not pretended that this expression is the most convenient for the purposes of calculation: the approxi- mate value of the conical angle which is given by a series of spherical harmonics is that which should be employed; but it may be well to give the complete expression in the above form, which I have not seen published anywhere. XXXVI. On Hydrolysis in Aqueous Salt-Solutions. By Joun SHE Ds, B.Sce., Ph.D.* e)* dissolving potassium cyanide in water it is partially decomposed into potassium hydrate and hydrogen cya- nide. This action of the water in producing decomposition is ealled hydrolysis. Probably all salts are hydrolysed in aqueous solution to a certain extent, but in the majority of cases the amount of hydrolysis is so excessively small that the means which we have at our command are not sufficiently delicate to enable us to detect it. Besides the salts there is another im- portant class of compounds, namely the esters, which are sus- ceptible to hydrolysis on being mixed with water. Methyl and ethyl acetate, for example, are decomposed by water to a considerable extent into acetic acid and the corresponding alcohol. The extent to which hydrolysis takes place is regu- lated by the law of mass action as enunciated by Guldberg and Waage. In all cases we are dealing with a state of chemical eden or balanced action which is usually represented thus :— KCN + HOH =— KOH+HCN, or CH;,COOC,H; + HOH =— C,H;0H + CH;,COOH, the sign =—— being substituted for the ordinary sign of equality as suggested by Van’t Hoff. Now, a priori, we should expect a substance, for example potassium cyanide, which is formed from chemically equivalent quantities of acid and base to be neutral, and we have every reason to believe potassium cyanide, as such, to be so. Its solution in water, however, as is well known, has a strongly alkaline reaction, and the above explanation of hydrolysis furnishes us with no reason why the solution should react alkaline rather than acid, since the hydrolysed fraction of the potassium cyanide still exists in the solution as chemically equivalent quantities of acid and base. Here Arrhenius’ theory of electrolytic dissociation comes to our aid, and shows us that although we may have in the solution equivalent * Read before the Swedish Academy of Science, Stockholm, 11th January, 1893, Communicated by the Author. Phil. Mag. 8. 5. Vol. 385. No. 215. April 1893. 2C Pe ir, ern dope? 2 TD 366 Dr. J. Shields on Hydrolysis quantities of potassium hydrate and hydrogen cyanide, yet the former is very largely dissociated into its ions, and, therefore, in a particularily favourable state for entering into reaction with the indicator, whilst the latter is not so. Accordmg to the same theory, if we add other salts to a solution of hydro- eyanic acid, which, per se, is only slightly electrolytically dissociated, then the amount of dissociation is diminished many thousand times, and this is practically what occurs in the solution under consideration. The presence of the un- hydrolysed potassium cyanide causes the dissociation ratio of the hydrocyanic acid to be vastly decreased. | ‘There are salts, on the other hand, whose solutions have an acid reaction. This is due to the fact that the acid, which is one-of the products of hydrolysis, is more highly electrolyti- eaily dissociated than the base which is formed at the same time. Usually the above facts are expressed by saying that the base is stronger than the acid, or vice versa. if hydrocyanic acid were as nearly completely dissociated as hydrochloric acid is, at the same dilution of course, then probably a solution of potassium cyanide would be as nearly neutral as one of potassium chloride, for Ostwald has pointed out that all acids when completely dissociated are equally strong. In this memoir, salts of strong bases with weak acids only have been considered. The investigation was undertaken at the suggestion of Dr. Svante Arrhenius, in Stockholm, and the main object in view was the determination of the amount of free alkali in aqueous solutions of such salts as potassium cyanide, sodium carbonate, &c.; that is, of salts whose solutions - exhibit an alkaline reaction, or act as mild alkalies. I should like to avail myself of this opportunity to express to Dr. Arrhenius my warmest thanks for the help which he se willingly gave me and for the interest which he all along took in the work. A research, “ Zur Affinitiitsbestimmung organischer Basen” (Zeits. f. physikal. Chemie, vol. iv. p. 19,1889), on somewhat - similar lines, has already been carried. out by Dr. James Walker. In it the relative strengths of different organic bases were measured ; but one of the experimental methods which he adopted could have served equally well for the determination of the amount of free acid in aqueous solutions of salts of the bases. As a general rule, it will be found that the determination of the amount of free alkali in solutions of the above salts is beyond the scope of ordinary analysis. A reaction which enables us to do so, however, is known. The velocity with which the salt-solutions saponify methyl or ethyl acetate gives wn Aqueous Salt-Solutzons. 367 us a measure of the quantity of free alkali which they contain. The essential condition for saponification to take place is the presence of hydrogen or hydroxyl ions. Now Walker’s method was based on the presence of hydrogen ions, whilst in the experiments about to be described we are dealing with hydroxylions. This places us, as it were, on vantage ground ; for, since hydroxyl ions saponify much more rapidly than hydrogen ions, it is thus possible to work with more dilute solutions where perturbing influences are reduced to a minimum. To return once more to the typical example of the salts under investigation, potassium cyanide, let us for a moment consider what takes place when we dissolve this body in water. + Besides the undissociated KON we get a great number of K and CN ions, the water itself, too, is slightly dissociated into > - + H and OH ions. Now the H ions coming into contact with the CN ions unite with them to form HCN which is uncharged, being practically undissociated, whilst the hydroxyl ions re- main free and counterbalance the potassium ions. The water goes on continually supplying hydrogen and hydroxyl ions, which are disposed of in this way, until equili- brium takes place. If we now make up a small inventory of the principal constituents of the solution we get :— + a 1 and 2, K and ON ions. 3, KCN undissociated. 4, HOH undissociated (say). 5, po undissociated (say ), and, corresponding to this, 6 and 7, K and OH ions. 6 and.7 taken together represent the quantity of free potash present in the solution. The task which now lies before us is comparatively easy, but before proceeding to deduce formule for the calculations it is as well to point out what will be proved later on, namely, that potassium cyanide itself is not an active agent of saponification. Attention may also be directed to the fact that the dissociation of the hydrogen cyanide is so excessively slight in presence of the salt, that it cannot exercise any appreciable influence on the velocity of saponification: the truth of this will be the more readily ad- mitted if we bear in mind that hydrogen ions are much less active than hydroxyl ions. What has already been said regarding the influence of the salt on the dissociation of the hydrogen cyanide applies equally well to the water. When ethyl acetate is saponified by a solution of potassium 2C2 368 Dr. J. Shields on Hydrolysis hydrate, the velocity of the reaction is represented at every instant by the general equation & =hO—n) (C2), « «+ = ee Q) where k is the coefficient of velocity of reaction, C and C, the concentrations of the ester and base respectively at the com- mencement, and 2 the quantity of ester which has undergone change during the time ¢. . In the case of the salt-solutions we wish to determine the concentration of the base, z.e., the amount of active free alkali at the commencement, the coefficient of velocity for the various bases being already known. On dissolving potassium cyanide in water we get KOH + HENg=— KCN Sale (quantity KOH x diss. ratio) x (quantity HCN x diss. ratio) = (quantity KCN x diss. ratio) x (quantity HOH x diss. ratio). The dissociation ratios of potassium cyanide and potassium hydrate, water and hydrogen cyanide, do not alter appreciably with change of concentration in the solution, and may conse- quently be regarded as constant. (Arrhenius, Zeits. f. physikal. Chemie, vol. v. p. 17, 1890.) The quantity of water as compared with the other substances is supposed to be infinitely great and regarded as a constant K. The saponification of ethyl acetate by means of aqueous potash takes place according to the equation :— CH;COOC,H; + KOH=CH;COOK + C,H;08 ; and if we represent by C, the initial concentration of the potassium cyanide, by A the concentration of the free potassium hydrate, and by 2 that of the potassium acetate formed, then C,—#2—A will represent the actual concentration of the potassium cyanide, and A+w that of the hydrocyanic acid; all of course being expressed in the same unit, namely, gram-molecules per litre. From the equilibrium, KOH +HCN =~ KON+ HOH we now get, using our new symbols, the equation A(A +a)=K(C,—2—A), ee which represents what takes place at any stage of the reaction. After the first few moments, however, when A becomes very small compared with 2, we may write the equation thus :— aa Kina), ‘ in Aqueous Salt-Solutions. 369 Now, in the general equation (1) C,;—w the concentration of the base is what we now call A, so that we may re-write it in the form Cp a a Be a e e e e ° . (4) Combining (8) and (4) we get de be K (Ci) (5) dt °C—a k unis which on integration gives the solution : Cy . C,—2, C C—2 oe p= 0, log nat. pean C0 log nat. ae of k(t,—to) - (6) k, the specific coefficient of velocity, is known, and for potash at 24°-2 C.is numerically equal to 6°22. Having got K froin equation (6) all that remains to be done in order to know how much free potash is present in the solution at the commence- ment is the calculation of A from equation (2). At the beginning, when «=0, IR (Cpa Baan ie 8 elgg CG) from which we get A in gram-molecules per litre. The percentage amount of potassium cyanide which has been decomposed by the water is therefore 100A OF : It is here unnecessary to describe in detail the apparatus and method which I used to determine the velocity of the saponification of ethyl acetate by the salt-solutions, as it was precisely similar to that which has already been employed by Ostwald (Journ. f. pr. Ch. [2] vol. xxxy. p. 112, 1887), Arrhenius (Zerts. f. physikal. Chemie, vol. i. p. 110, 1887), and others. Measured volumes of a known strength of salt-solu- tion and of ethyl acetate were mixed at the temperature of the thermostat. (For the construction of the thermostat, c. see Zeits. f. physikal. Chemie, vol. ii. p. 564, 1888.) From time to time small fractions of the mixture were withdrawn by means of a pipette and titrated as expeditiously as possible. In calculating the concentration of the salt at the com- mencement, it has been assumed that the volume of the mixed solutions of salt and ester is the sum of the volumes taken separately. This is of course, strictly speaking, not true, but the deviation from the truth is so small as to be entirely negligible. I shall now proceed to give the experimental 370 Dr. J. Shields on Hydrolysis results which I obtained. The first column in the tables contains the time ¢ expressed in minutes since the beginning of the reaction. The second and fourth columns C,—2 and C—z contain the concentrations of the salt and ester re- spectively in hundredths of a gram-molecule per litre. The third column contains x the quantity of ester which has under- gone change, also expressed in the same unit. In the last column will be found the constant expressed in arbitrary units. Here it may be noticed that the first few values have been neglected in accordance with the derivation of the formula. From the mean value of these the characteristic constant K has been calculated. A represents the amount of free alkali in gram-molecules per litre, and besides this will be found the percentage amount of salt which has been hydrolysed in the solution experimented on and at the temperature at which the experiment was carried out. It is conceivable that the addition of ethyl acetate to the solution of salt would disturb the existing equilibrium, but a discussion of this question is reserved for a later part of the memoir. Potassium Cyanide. Solutions of this salt of four different concentrations were examined, namely, +, 4, 4, and ~, normal. The tempera- ture at which the experiments were made was 24°20. The value of k, the coefficient of velocity for potash at this temper-_ ature, is 6°22. Nitrophenol was found to be the most suitable indicator, and enabled me when titrating with decinormal = Potassium Cyanide. t. O,—2. z. O—x. 0 94°74 0-00 39°34 4 93°40 1°34 38°00 16 92:28 2°46 36°88 (313) x 1077 | 39 91-40 3°34 36°00 324 90 88°72 6:02 33°32 385 210 86°40 8°34 31:00 337 353 84:20 10-54 28°80 342 580 81:20 13°54 25°80 378 -Mean=353 x 1077 K=0:000928. A=0:00296, or 0°31 per cent. of salt hydrolysed. hydrochloric acid to observe the end point pretty accurately. _ wn Aqueous Salt-Solutions. St IN : d —- Potassium ( vyanide. 4 : i be | CLs | a. hy eK Cre | etd ae eSeS INCE clue Aa | | 0 | 2348 0:00 39:34 Go|. 222s | O96 i. esses 7). re) 2198s) || 50, saree 1) (117) x 10s! ef IO) | 1:9 S786 4 TBS Sheet . 2012. | SOO at |, weonos: 4 219 2) Sd ok s ee 20 |. Bl 216 oem | 144 GO4> 7 ee3s30E" 4) 226 Bee | 1598 | 7:50 Sted, F206 1394 - |. 13°00 10-48 D886 1 | 225 2789 | 9:82 13°65 2568 |° 245 Mean=221 x 10-7) K=0-00121. A =0-:00168, or 0°72 per cent. of salt hydrolysed. N ee: — Potassium Uyanide. 10 t C,—2. ff C—x 0 9°52 0:00 48°70 2 9°23 0:29 48°41 | 6 8:87 0°65 48:05 (251-5) x 10-6 12°5 8:67 0-85 47°85 123°8 33 815 kes fae 47-33 12671 6Ooioin. 767 1:85 46:85 | 131-2 130 6°78 2°74 45°96 =|: 1451 209 6°25 3°27 45°43 Messy 319 5°56 3°96 44-74 J41°8 1372 | 2°93 6°59 42°11 | 1376 | i i Mean=133'8 x 10-8 K=0:001204. A =0°00107, or 1:12 per cent. of salt hydrolysed. Sra 372 Dr. J. Shields on Hydrolysis N Potassium Cyanide. AQ) t. C,—z. Pe | C—z. | SS | 0 2:38 0:00 48°70 2 2:20 0-18 48°52 45 2-10 0:28 48-42 (449) x 10-6 8:5 2:00 0:38 48-32 782 22 1-83 0°55 48°15 602 44 1-59 0-79 47-91 683 112 117 1-21 47-49 759 191 100° “| “ps8 47°32 634 303 0-72 1-66 47-04 765 1351 0:16 2-22 46°48 742 | Mean=702'4 x 10-§ K =0:001336. A =0:000557, or 2°34 per cent. of salt hydrolysed. é 40 Potassium Cyanide (concentrations in 5}5 gram- molecule per litre). | t C,—2 | a C—x, | | | 0 4-73 0:00 97-40 | | 2 4-42 031 97-09 | 5 411 0-62 96°78 | (1050) x 10-6 10 3°86 0:87 96:53 (893) | 23 3°57 1:16 96-24 728 | 36 3:26 1-47 95°93 728 | 60 |) 99204 1-79 95°61 686 | 122 2:30 2-43 94-97 720 | 180 2:02 271 94-69 653 | Mean =703 x 10-5 K = 0-001328. A =0°000553, or 2°35 per cent. of salt hydrolysed. Sodium Carbonate. Experiments were made with 1, +4, 94, and 2, mole- cular normal solutions of sodium carbonate. The titrations were made with the aid of phenol phthalein at the ordinary temperature of the laboratory. In this way the amount of standard acid added corresponded only to one half of the real concentration of the salt in hundredths of a gram-mole- cule per litre, as the solution becomes practically neutral when the unaltered sodium carbonate has been converted into sodium hydrogen carbonate. This would necessitate the doubling of in Aqueous Salt-Solutions. 373 the apparent concentrations ; but since the exact point of neutrality was difficult to observe, two series of experiments were made to eliminate as much as possible the experimental error and the sum of the apparent concentrations taken to represent C,—2. Consequently, in the tables for sodium car- bonate there are two extra columns (I. and II.) with the sum of the numbers contained in them given under the column C.—.. The temperature at which all the experiments on sodium carbonate was made was 24°2C., and the co- etlicient of velocity & for sodium hydrate at this temperature is taken at 6°23. _ (mol.) Sodium Carbonate. t. fe IT. U,— 2. Le C—x. 0 19-00 19-00 38°00 0-00 48-70 2 18-15 18°10 36°25 1-75 46°95 4 17-40 17:27 34°67 33 45°37 | (150) x 10-6 8 16°55 16°65 33°20 4°80 43°90 | 129 2 15°95 15°99 31°94 6:06 42°64 | 138 20 15°15 15°15 30°30 7:70 41:00 | 135 30 14-72 14-74 29 46 854 40-16 | 112 50 13°23 13°26 26°49 11-51 37:19 | 136 85 11:80 11-95 23°75 14:25 34:45 | 136 155 10°10 9:97 20°07 17°93 30°77 | 141 Mean = 132°4 x 10-6 “ (mol.) Sodium Carbonate. t. ih Ma Osea. | Aaa Coe. 0 9-40 9°40 18-80 0-00 48°70 2 9-07 9:05 18°12 0°68 48:02 4 8°85 8°10 16°95 1-85 46-85 | (625) x10-° 8 7°85 7:60 15°45 3°35 45°35 815 12 7:30 7:25 14°55 4°25 44°45 839 16 6°95 6:90 13°85 4°95 43°75 854 20 6°60 6:62 13°22 5°53 43°12 880 24 6°40 6°35 12°75 6°05 42°65 874 32 5°82 6-08 11:90 6:90 41°80 885 66 5:12 5:10 10°22 8°85 40°12 741 Mean =841 x 10-6 K=0:01954, =0°00596, or 317 per cent. of salt hydrolysed, 374 Dr. J. Shields on Hydrolysis ah (mol.) Sodium Carbonate. Ree ere y ae 2...) Oa z. : | are Seals 7 one TA Tce Sia 0 | 477 | 477 | 954 | 0:00 | 48-70 : 2 | 430 | 433 | 863 | 091 | 47-79 | 4 3:84 | 3°90 T74 | 1:80 46:90 278 x 10-* 8 344 | 350 | 694 | 260 | 46:10 | > a7 | 12 0/2301. [83-18 |) 6492] 93-35 | 45-a5 ee | | | 16 290 | 2-96 5°86 3°68 | 45:02 255 32 247 | 2:25 4°72 4:82 | 43°88 243 40 209 | 207 4-12 542 | 43-28 266 62 152 | 160 a12 | G42 | 49:98 283 92 1-22 1:24 246° | 7-08 ..| 41-62 269 Mean= 265 x 10-5, K=0-02383. A =0°00465, or 4°87 per cent. of salt hydrolysed. N 0 (mol.) Sodium Carbonate. l l ; | | | t, I Il | G,-2.| 2 | Cm~s Sass eens | ==... 0 2°38 238 | 476 | 000 |) 458 2 | 195 | 225 | 420 | 056 | 4814 4h. STS 180 | 35d 1-21 47-49 634 x 10-5 8 1:35 153 | = 288 1-88 46°82 676 12 1°22 1:23 | 2-45 2°31 46°39 698 16 1:16 ay 2:27 2°49 | 46°21 613 20 1°02 1-07 2°09 267 | 4603 579 28 0-75 0°85 160° | SiG Maes 665 56 0°49 0°41 0-90 3°86 | 44-84 656 . Mean=646 x 10-5 K=0-02586. A =0:00838, or 7°10 per cent. of salt hydrolysed. Potassium Phenate. Carbolic acid or phenol is another well-known weak acid which forms a crystalline salt with potash. As an experi- ment with this salt seemed likely to be interesting, solutions of it were prepared by mixing equivalent quantities of solu- tions of potash and phenol of known strength and then diluting until solutions of the salt of the required concentration were obtained. Two sets of experiments were made; one with in Aqueous Salt-Solutions. 375 zo and the other with =, normal solutions. The indicator used for titration was nitrophenol. The temperature of the thermostat was 24°1C., and the coefficient of velocity for potash at this temperature was taken as 6°19. Each set of experiments was done in duplicate, the separate results being given in the columns I. and II. The mean of these is contained in the column C,—wz. In the case of the =, normal solution the concentrations are ex- pressed in 5}, instead of ;}5 gram-molecule per litre, as before. N Potassium Phenate. 10 t 1 EE C,—2. a. C—xz. 0 9-62 9°62 9-62 0:00 48°70 2 8-80 8:80 8°80 0:82 47°88 4 8°30 8:20 8:25 1:37 47°33 | (1383) x10-5 6 8-03 8:00 8:01 161 47:09 107 8 781 CCT HEU 1°83 46°87 101 10 766 7-60 7°63 1:99 46°71 95 12 TAD 7:43 7:44 2°18 46°52 96 16 7:09 (US a es) 2°53 46:17 99 22 6°75 6°71 6:73 2°89 45°81 97 30 6°20 6:10 6°15 347 45:23 109 Mean=101x10-5 K=0:00925. A =0:002936, or 3°05 per cent. of salt hydrolysed. ny Potassium Phenate. 50 t aL II. C,—4 Ai C—z. 0 3°90 3°90 3°90 0:00 97°40 2 3°15 3:10 312 0-78 96°62 4 2°78 2°80 2°79 ei 96:29 | 567x10-5 i) 2°60 2°67 264 | 1:26 96°14 611 6 2°49 2°54 2°52 1-38 96°02 627 8 2:27 2:27 2°27 1:63 95°77 (704) 12 2°10 2°04 2:07 1°83 95°57 596 16 1:88 1-86 1:87 2°03 95°37 578 20 1-66 1-64 1:65 2°25 95°15 613 eR A hiasteee 1:46 1:46 2°44 94-96 616 OD Ue sends 1-29 1:29 2°61 94°79 629 Mean=605 x 10-5 K=0-00939. A =0°001305, or 6°69 per cent. of salt hydrolysed. 376 Dr. J. Shields on Hydrolysis Borax. Several experiments were made with solutions of borax, but the results were by no means as satisfactory as could be desired. The chief difficulty seemed to be in the want of a suitable indicator. After trying about twenty I finally selected litmus as the one which gave the best results. Next to litmus came rosolic acid. I first of all prepared a solution of litmus of a certain purple tint to act as a guide or standard, and then I added acid to the solution under examination until it became of the snes tint. I shall only give one series of experiments with a =4, molecular normal solution of borax, so that some conception may be formed as to the amount of hydrolysis in solutions of borax. The temperature of experiment was 24°-2C., and the co- efficient of velocity for sodium hydrate corresponding to this temperature is 6°23, N 39 (mol.) Borax. | t C,-2 L Ca 0 5°85 0.00 48°70 4 5°82 0:03 48°67 8 572 0-13 48-57 (30) x 10-6 30 5°55 0:30 48°40 (22) 188 4:10 1°75 46°95 120 1190 2°73 3°12 45°58 86 2885 1-40 4-45 45°25 95 4375 0-95 4°85 43°85 94 | Mean = 99x 10-6 K =0:00050. A =0:000738, or 0°92 per cent. of salt hydrolysed. The Influence of Dilution on the Amount of Hydrolysis. The table which follows contains the general results of the foregoing experiments and shows the effect of dilution on the amount of hydrolysis. The first column gives the approximate concentration of the solution, the second the amount of free alkali in the solu- tion in gram-molecules per litre, and the last the percentage amount of salt hydrolysed. see in Aqueous Salt-Solutions. 377 - Concentration. A. Hydrolysis. N z KON Be i onhee nee 0:00296 0:31 per cent. 2 mere 5 ak lp 0-00168 072 ,, N Pe laos Se 0-00107 ae N : ‘ =. ae 0000557 Danes B Gaol. )Na,00 0-00804 2-12 im (mo .)Na, Zot eees 0 wiz 9 N 00596 i0 5 Sh ae CR Ate 0:00596 317 a N 00465 0 et eacties <<’ moe 0:00465 4°87 vs 0:00338 7-10 Fee c N BMOMIOR eeeesecee 0-00294 S0b) N Bp OMe 0:00131 669 a Gael N 0007 0:92 39 (mol.)Na,B,O, ... 0:00074 56 A glance at the table will show that among the four sub- stances examined the greatest amount of hydrolysis occurs in the case of sodium carbonate. The numbers cannot pretend to a very high degree of accuracy, chiefly on account of the difficulties in obtaining suitable indicators for the titration of the solutions, but the following regularity is easily discernible. The amount of free alkali contained in the salt-solutions is proportional to the square root of the concentration of the salt. This is, however, not strictly true, but more nearly expresses the truth the greater the dilution of the solution. A rough calculation on the numbers for the two most concentrated solutions of potassium cyanide shows that there is a deviation from the law of about 13 per cent., whilst for the less concen- trated solutions the deviation is reduced to about 4 per cent. If the dilutions be plotted as ordinates against the percentage amount of salt hydrolysed as abscisse, curves are obtained. Fig. 1 represents the curves for potassium cyanide and sodium carbonate. ‘These curves enable us to see at a glance the per- centage of salt hydrolysed at any given dilution. For example, Dilution. 378 Dr. J. Shields on Hydrolysis Fig. 1. Percentage of Salt hydrolysed. reading from the curve, there should be 1°65 per cent. of the potassium cyanide decomposed in a 34, normal solution of that salt. If calculated from the above law, the amount of hydrolysis is 1°58 per cent. Now if the salt itself were the cause of the saponification of the ester, the velocity of the reaction which is proportional to the amount of free base present would have been very nearly directly proportional to the concentration of the salt; but it has been found approximately proportional to the square root of the concentration, consequently the view that the salt itself produces the saponification is untenable. The law which has just been enunciated is what we should expect from the theory ; for if we again take the case of potassium cyanide, we get, neglecting the dissociation ratios as formerly, : KOH+HCN ==> KCN+HOH, 0. Gee) Ne where C, is the initial concentration of the potassium cyanide, and the fraction of it which has been hydrolysed. When « is very small compared with C,, the above equation becomes C= V7 Cos wn Aqueous Salt-Solutions. 379 that is to say, the amount of free potash is proportional to the square root of the concentration of the potassium-cyanide solution. Tt has long been known that water decomposed certain salts, with formation of free acid and free base, but the amount of such decomposition has up to the present time only been measured in a few cases. It is true some guesses at it have occasionally been made, but they have proved rather unsatis- factory. For example, it has been supposed (see Ostwald’s Lehrbuch der allgem. Chemie, vol. ii. p. 187, 2nd edit.), from measurements of the heat of neutralization of hydrocyanic acid by caustic soda, that a solution of sodium cyanide con- tains only one fifth of the salt as such, whilst the other four fifths are decomposed into free acid and free base. The experiments which I have made on the velocity of reaction show that in a tenth-normal solution of potassium cyanide only about one per cent. of the salt is decomposed in the way indicated. The results which J. Thomsen (Thermo- chemische Untersuchungen, vol. i. p. 161) obtained on neutra- lizing one molecule of sodium hydrate with n molecules of hydrogen cyanide are as follows :— n. NaOH Aq, nHCN Aq. i 13°68 heat units. iL 27°66 i 2 27°92 = These numbers indicate that the amount of heat which is ‘developed increases in the same proportion as the quantity of hydrogen cyanide added, until there are equivalent quantities of acid and base present. An excess of acid, then, produces only a very slight alteration in the value of the heat of neutralization. Now manifestly this small increase in the heat of neutrali- zation means that the first equivalent of hydrogen cyanide has almost all combined with the sodium hydrate. The cause of the incomplete combination is due of course to the mass action of the water. Inshort, it would seem that only a small fraction, presumably about one per cent., of the potassium cyanide is decomposed by the water into free acid and free base. This corroborates the result which I have obtained by a totally different method. A guess which H. Rose (Jahresbericht, 1852, p. 311) hazarded as to the amount of hydrolysis in an aqueous solu- tion of borax is just as unsatisfactory. Rose supposed that 380 Dr. J. Shields on Hydrolysis this substance in pretty dilute solution was almost entirely decomposed into acid and base; but the preceding experi- ments go to prove that in a =; molecular normal solution rather less than one per cent. is decomposed by the water. If the statement that the amount of free alkali in the solution is proportional to the square root of the concentration holds good for borax, then a solution in which the borax was com- pletely hydrolysed would be almost infinitely dilute. Rose has described a very interesting experiment which is intended to show the decomposition of borax by water. A tincture of litmus reddened with acetic acid is added to a concentrated solution of borax until the red colour has almost but not quite disappeared ; the whole is then diluted with water, when the red colour changes to blue. I have repeated this experiment, and find that a solution prepared in the way Rose has indicated becomes distinctly blue on dilution. Joulin (Bull. Soc. Chim. de Paris [2] vol. xix. p. 844, 1873), how- ever, could not observe this change of colour, and moreover has attempted to show that water exercises no decomposing influence at all on salts; but there is little doubt that he has been too hasty in coming to this conclusion, and that Rose, at least qualitatively speaking, was right. Trisodium Phosphate. A preliminary experiment with a X solution of this salt showed that the velocity of reaction, on saponifying ethyl acetate, was singularly great when compared with what had been observed in the case of the other salt-solutions, and in fact closely approached that for a =, normal solution of caustic soda itself. This seemed to indicate that the solution under examination was almost entirely hydrolysed in the sense of the equation 3 Na;PO,+ HOH =Na,HPO,+ NaOH. The formulze which have hitherto been employed are of no use in this case, for they depend on the condition that A should be very small compared with 2 Here A can in no case be neglected ; consequently the equation (3) he K(C, — a) is inapplicable. eae Ss The general equation dx becomes d: 7G =KG—2)(C-0), 2... 8) in Aqueous Salt-Solutions. | 381. when we substitute for the concentration of the base that of the sodium phosphate. Instead of K we may write ky, where we is a factor which expresses the ratio of the amount of free alkali present to’ what would be present if the hydrolysis of one sodium atom was complete. Hquation (8), on integration, gives the solution . Cy—2 S20. log nat. (a G—0, °s nat. en =hu(t;—t), Gag — log Gap = 04843 ku (—4)(C—C), + @) from which we can calculate m at the time ¢,. In order to determine pu at the commencement, the different values of mw are plotted against the times, and the curve so obtained prolonged. The point at which it cuts the axis for the time t=0 gives the value of w at the commencement. Hixperiments have been made which show that Na,H PQ, is only slightly hydrolysed ; so if we neglect this and assume that the equation Na,PO,+ HOH=Na,HPO,+ NaOH represents the posszble quantity of caustic soda which can be formed in the solution, then 100 represents the percentage amount of the caustic soda which actually eavsts in be solution. The following experiments were made with a =, molecular normal solution of trisodium phosphate at 24°-2 C., at which temperature the coefficient of velocity of reaction for caustic soda is 6°28. The concentrations are expressed in 3}5 of a gram-molecule per litre, and the employment of phenol _ phthalein enabled the titrations to be made pretty accurately. i a (mol.) in Phosphate. t. I. II. C,—2. oR C—x. pe 0 3°81 J81 3°81 0:00 4°87 2 2°93 2°95 2°94 0:87 4:00 0:945 4 2°41 2°45 2°43 1:38 349 0882 6 2:06 2°03 2°04 1-77 3°10 0873 8 182 | 177 | 179 | 202 | 2:85 | 0-831 10 158 | 155 | 156 | 295 | 362 | 0-897 12 135 | 140 | 137 | 944 | 243 | 0-897 16 112 | 114 | 113 | O68 | 219 | o-788 20 091 | 094 | 093 | 288 | 1:99 | o-v780 4 079 | o8 | o7v9 | 302 | 185 | o-v64 | 30 063 | O66 | o64 | 317 | 170 | 0-738 Phil. Mag. 8. 5. Vol. 85. No. 215. April 1893. 2D~ Coefficient wu. 382 Dr. J. Shields on Hydrolysis If the equation Na;PO,+ HOH =Na,HPO,+ NaOH represented accurately the amount of hydrolysis, then mw at the commencement should be 1:00. A glance at the last column of the table shows that the equation must be nearly true. In order to find approximately the initial value of p, a curve (fig. 2) has been drawn by plotting the values of w as ordinates against the times ¢ as abscisse. . Time, in minutes. By referring to the curve it will be found that the initial value of w is 0°98 at least ; that is to say, at least 98 per cent. of one of the sodium atoms in Na;PO, exists as free caustic soda in a = molecular normal solution of the salt at 24°-2 C. In other words, although trisodium phosphate exists in the sclid state, yet in dilute solution it is for the most part decomposed into hydrogen disodium phosphate and sodium hydrate. This result is in entire agreement with Berthelot’s recent researches. in Aqueous Salt-Solutions. 383 Allusion has already been made to the fact that hydrogen disodium phosphate is only slightly hydrolysed when dissolved in water. ‘This salt behaves rather differently from the others. During the saponification the solution, which is at first alkaline, becomes neutral and then acid. For the sake of comparison with trisodium phosphate, the following set of experiments was made witha 50 (mol.) solu- tion of hydrogen disodium phosphate at 24°°2 C. The solution was prepared from a sample of the salt obtained from Kahl- baum, and had a slightly alkaline reaction. The titre of the solution during saponification was as follows :— N setae 30 (mol.) Hydrogen Disodium Phosphate. | ee ee Time. Titre. min. 7 0 0:06 ado g--mol. per litre (alkaline), 2 0-04 A; Er haes 5 0:00 Neutral. 32 0-06 zdo0 g.-mol. per litre (acid). 120 0-10 2 226 0-15 ” r 380 0°17 . ? 1380 0-30 a ‘ 2815 0:41 ‘s x 4500 0-52 j 33 The titrations were made with phenol phthalein. At the commencement the solution contained 0:0003 gram- molecule of free soda per litre. The case is a very complicated one, but possibly the bulk of this alkalinity is due to the formation in the solution of tri- sodium phosphate ; there is still, however, a minute amount of free alkali in the solution, owing to the hydrolysis of hydrogen disodium phosphate. The following attempt has been made to measure it, but no stress must be laid on the results. I give the calculations here merely for the sake of comparison with trisodium phosphate, and to show that at the best there is not much free alkali in the solution. The calcu- lations were made with the help of equations (6) and (7). It is evident, of course, that what we measure here is the quan- tity «2. The initial concentrations of the salt and ester, expressed in hundredths of a gram-molecule per litre, are 4°76 and 48°76. 2D2 384 Dr. J. Shields on Hydrolysis If we start at the point where the mixture is neutral we may construct the following table, from which we can calcu- late the quantity of free alkali in the solution at the point of apparent neutrality. This quantity, as has already been sug- gested, is perhaps due to the hydrolysis of hydrogen disodium phosphate ; whilst the quantity of free alkali determined by direct titration is due to the presence of trisodium phosphate, formed according to the equation 2Na,HPO,=Na;PO, + NaH,PQ,. The influence of the dihydrogen sodium phosphate has been neglected altogether. : te C.—«. ap. C—x. 0 4:76 0:00 48°70 27 4-70 0:06 48-64 115 4-66 0:10 48°60 64x 10-8 221 4-61 0-15 48°55 (86) 375 4:59 0-17 48°53 65 1375 4°46 0:30 48°40 59 2810 4°35 0:41 48°29 55 4495 4:24 0:52 48:18 54 Mean = 59x107° K=0-00000236. A=0-:000038, or 0°07 per cent. of salt hydrolysed. The amount of free alkali determined by direct titration is 0°63 per cent., whilst that determined from the velocity of saponification, starting at the neutral point, is 0°07 per cent. ; it is therefore evident that the total amount of free alkali in the solution is very small when compared with what is present in a solution of trisodium phosphate. Sodium Acetate. After having estimated the amount of hydrolysis in salts of strong bases with some of the weakest acids, it was thought desirable to extend the experiments a little and determine the amount of hydrolysis in a salt of a stronger acid, for example acetic acid. For this purpose a tenth normal solution of sodium acetate was prepared and investi- gated in the same manner as the salts of the weaker acids. The calculation of the results, however, was in this case much simplified, owing to the fact that the concentrations of the salt and ester did not alter much during the reaction, consequently in Aqueous Salt-Solutions. 385 the mean values have been employed in calculating the rharacteristic constant. If, in the equation (5), de 1 1_ K(CG—z) dig@en bes og be we substitute for C.—a and C—w their mean values 9°316 and 48°49, which were obtained from a series of experiments made at 24° 2 ©., where k=6'23, we get: deel BI IGK d 4849 623° 4%” which on integration gives the solution ay" — x67 6:23 x 48°49 x 9-316 K= ty— to | Having got the characteristic constant K, equation (7) enables us to determine A, the amount of free soda in the solution at the beginning, expressed in gram-molecules per litre. The solution was titrated with the help of phenol phthalein. In this case of course a, which is expressed in hundredths of a gram-molecule per litre, was measured directly. The values of x in the following table are the means of two con- cordant sets of experiments. N et i0 Sodium Acetate. t. C,—<2. x. C—x2. 0 9-52 0-000 48°70 1224. 9-46 0-060 48-64 3952 9:455 0-065 48-635 6882 9 385 0-135 48:565 2:58 x 10-6 21252 9:20 0-320 48-380 4-98 25550 9:20 0-320 48-380 4-06 34160 9-165 0°355 48-345 3°72 41290 9:14 0380 48°320 3:51 Mean = 9°316. Mean=48'49. Mean=—3°76x10-°. K=0:0000000668. A=0:00000798, or 0°008 per cent. of salt hydrolysed. According to these measurements and calculations, it will be seen that in a tenth normal solution rather less than +4) per cent, of sodium acetate is hydrolysed into free acid and 386 Dr. J. Shields on Hydrolysis free base ; thus, | - CH,COONa+ HOH === CH,COOH+NaOH. Tt has already been stated that the presence of free weak acids has no measurable influence on the velocity with which the saponification takes place. This is equally true in the case of sodium acetate, where acetic acid is one of the products of hydrolysis, and is also formed on the saponification of ethyl acetate. Arrhenius (Zeits. f. phystkal. Chemie, vol. v. p. 2, 1890) has thoroughly investigated the change of the dissociation ratio of acetic acid on the addition of sodium acetate, and has shown that it may be regarded as nil in presence of large quantities of its salts. By referring to the table it will be seen that the experi- ments on sodium acetate lasted for a considerable time, and it is conceivable that the water itself may have played an im- portant part in the saponification of the ester. In order to test this a blank experiment was made with water and ethyl acetate under the same conditions as the experiment with the — sodium acetate, and after the lapse of nearly three weeks the solution of the ester was only slightly acid. If, then, pure water, in virtue of its being electrolytically dissociated to a small extent, produces such an inappreciable effect, we can easily conjecture how infinitely slight this effect will be in presence of a strongly dissociated salt like sodium acetate. The Influence of the Ester on the existing Equilibrium. A]l the preceding deductions regarding the amount of hydrolysis in aqueous solutions of salts of strong bases with ‘weak acids are based on the assumption that the equilibrium in aqueous solutions, KCN+HOH <> HCN+KOH, is not disturbed by the presence of small quantities of ethyl acetate. ‘To justify this assumption, I have made some expe- riments in which the concentration of the ester was varied, whilst the concentration of the salt remained nearly the same. Now, if the presence of the ester produced any change in the state of equilibrium, we should expect an alteration in the concentration of the ester to be accompanied by a corre- sponding variation in the amount of salt hydrolysed. The following tables contain the results of experiments, on an approximately 0-1 normal solution of potassium cyanide, made at 25°-0 C., at which temperature 4=6°54. in Aqueous Salt-Solutions. 387 I. Concentration of Ester = 0°4870 g.-mol. per litre. s C,—2x. oD. C—x. | 2 0 10:08 0:00 48°70 2 9-70 0°38 48°32 6 9-46 0°62 48:08 (100) x 10-8 10 9-20 0:88 47°82 143 20 8:81 1:27 47°43 153 40 8:38 1:70 47:00 142 84 7°70 2°38 46°32 141 152 700 3°08 45°62 140 264 6:20 3°88 44°82 137 1484 2°90 718 41°52 139 Mean = 142x10-° K=0:001305. A=0-00114, or 1:13 per cent. KCN hydrolysed. II. Concentration of Ester = 0°2005 g.-mol. per litre. é C.—2. 2X. C—-x. eee 1038 000 |. 20:05 2 10:20 0-18 19:87 6 9-99 0:39 19:66 (27) x 10-6 12 9°77 0-61 19:44 (36) On 9-41 0-97 19:08 39 63 8:90 1-48 18°57 40 131 8:26 2-12 17-93 42 243 7-67 2-71 17°34 39 1463 4-85 553 1452 41 1683 4-56 582 14:23 49 Mean = 40x10-§ K=0:00151. A =0:00124, or 1:20 per cent. KON hydrolysed. III. Concentration of Ester =0°1013 g.-mol. per litre. | t. Ob hho x. C—x. 0 10-4902 Ae O00 1013 2 10°40 0-09 10-04 10 10:16 0:33 9:80 (103) x 10-8 37 9-66 0:83 9:30 130 104 9°19 1:30 8:83 143 | 215 8:57 1:92 8-21 160 | 1435 6-40 4-09 6-04 164 | 1655 6-26 4-93 5-90 150 Mean = 149x10-8 K — 0:00 148. A=0:00124, or 1:18 per cent. KCN hydrolysed. 388 On Hydrolysis in Aqueous Salt-Solutions. The next small table contains the collected results of these experiments. Cone. Ester. K. A. KCN hydrolysed. 0:4870 | 000131 0-00114 | 1:13 per cent. 0:2005 0:00151 000124 4 ae2inae | ie | 01013 000148 | 0°00124 The numbers show that the concentration of the ester has no measurable influence on the amount of hydrolysis, since the figures in the last column do not arrange themselves in a series which is either gradually ascending or descending. The differences between them are probably chiefly due to experimental error. The mean value is 1°17, and the greatest deviation from it is less than 5 per cent. Résumé.—The general results of this investigation may briefly be stated as follows :— 1st. It is shown how the velocity with which salt-solutions saponify ethyl acetate may be utilized to determine the extent to which hydrolysis has taken place in aqueous solutions of salts of strong bases with weak acids. 2nd. The amount of hydrolysis has been measured in solu- tions of the following salts; and in 4, molecular normal solutions between 24°-25° C. the amount of salt which is decomposed by the water is :— Potassium cyanide 1:12 per cent. Sodium carbonate . oa Potassiam phenate ... . . s-Oa eae Borax (about) ; 0-5 ss Sodium acetate 0-008 7? Ath. Trisodium phosphate can scarcely be said to exist in a 345 molecular normal solution, as it is almost completely hydrolysed in the sense of the equation ; Na;PO,+ HOH=Na,HPO,+ NaOH. 5th. The presence of small quantities of ethyl acetate in the solution does not materially disturb the equilibrium, KCN + HOH 22— KOH + GR University College, London, [ 389 J XXXVII. Suggestion as to a possible Source of the Energy required for the Life of Bacilli, and as to the Cause of thew small Size. By G. Jounstone Stoney, M.A., D.Sce., F.R.S., Vice-President, Royal Dublin Society *. ie that part of the material universe which man’s position in time and space, and the limitations of his senses, permit him to investigate, the Dissipation of Energy is so prevalent that instances of the reverse process can seldom be clearly traced out, though many such can be dimly seen. Under these circumstances, even possible instances, such as that dealt with in this paper, are instructive if they are of a kind to be fully understood. They are also important, for if the universe is permanent, there must be, or have been, or be about to be, parts of the universe where the Concentration of Hnergy is as largely predominant as its dissipation is within our experience. Some bacilli, e. g. some of the nitrifying bacilli of the soil, are said to be sustained by purely mineral food, while they furnish ejecta which contain as much potential energy as the food, or more. If this be the case, they must be supplied with a considerable amount of energy to enable them to evolve protoplasm and the other organic compounds of which they consist, from these materials. Now many bacilli are so situated that this energy is certainly not obtained from sun- shine, and it is suggested that it may be derived from the gases or liquids about them. The average speed with which the molecules of air dart about is known to be nearly 500 metres per second—the velocity of a rifle-bullet ; and the velocity of some of the molecules must be many times this, probably five, six, or seven times as swift. We do not know so much about the velocities of the molecules in liquids as of those in gases, but the phenomenon of evaporation and some others indicate that they are at least occasionally comparable with those of a gas. Accordingly, whether the microbe derive a part of its oxygen or other nourishment from the gases, or from the liquids about it, it is conceivable that ONLY THE SWIFTER MOVING MOLECULES can penetrate the microbe sufficiently far, or from some other cause are either alone or predominantly fitted to be assimi- lated by it. Now if this be what is actually taking place, the adjoining air or liquid must become cooler through the withdrawal from * From the Scientific Proceedings of the Royal Dublin Society, vol. yili, part i. Communicated by the Author, 390 Dr. G. J. Stoney on the Source of the it of its swiftest molecules ; and, in compensation, an amount of energy exactly equivalent to this loss of heat is imparted to the microbes and available for the formation within them of organic compounds. It is further evident that if this be the source of energy upon which bacilli and cocci have to draw, the minuteness of their narrowest dimension will be of advantage—probably essential—to them. Presumably it would only be limited by such other necessary conditions as may forbid the diminution of size being carried beyond a certain point. The diameter of a bacillus is frequently as small as half or a third of a micron, which brings it tolerably well into the neighbourhood of some molecular magnitudes. The transference of energy here suggested may be what occurs notwithstanding that it does not comply with the Second Law of Thermodynamics, which states that heat will not pass from a cooler to a warmer body, unless some ade- quate compensating-event occurs, or has occurred, in con- nexion with the transference. This law represents what happens when vast numbers of molecular events (which are the real events of nature) admit of being treated statistically, and furnish an average result. It, therefore, has its limits : and the communication of energy from air to minute organ- isms which is described above, is an example of a process which is exempt from its operation ; since this transference is supposed to be brought about by a discriminating treatment of the molecules that impinge upon the bacillus of precisely the same kind as that which Maxwell pictured as made by his well-known demons. It therefore belongs to the recognized exception to the Second Law of Thermodynamics, viz., that which occurs in the few cases in which we can have under observation the special consequences of selected molecular events, instead of, as on all ordinary occasions, being only able to measure an average outcome from all the molecular events in the portion of matter we are examining. If some bacilli—those which live on mineral food—obtain their whole stock of energy in the way here indicated, it may be presumed that all bacilli get at least a part of what they require in the same way. Should the reader have any doubt as to whether the pro- cess here described is one of those that contradict the Second Law of Thermodynamics, he may satisfy himself on this head by the following considerations :— LTE Imagine a perfect heat-engine within an adiabatic envelope with some bacilli and an abundance of their mineral food, all Energy requred for the Life of Bacilli. 391 ‘being at one temperature. If events take place as supposed above, the bacilli receive sufficient energy from the sur- rounding medium to enable them to assimilate their mineral food, and thereby to grow and multiply. Meanwhile the medium becomes cooler. We may then suppose that the new bacilli which have come into existence, and all the excreta, are used as fuel in the heat-engine, and that its refrigerator is as near as we please to being at the temperature to which the medium has been reduced. The combustion of the fuel may take the form of resolving the bacilli and excreta back into the mineral substances from which they had been evolved, except that these are now at the temperature of the combus- tion. Let us next reduce this temperature in the heat-engine to the temperature of the refrigerator. During this process a portion of the heat may be converted into mechanical energy ; and at the end of the process everything within the enclosure is in the same state as at the beginning, with the sole excep- tions that some of the bodies within the enclosure are now at a lower temperature than at the beginning, and that the heat which they have lost has been converted into mechanical energy. It thus appears that the contents of the adiabatic envelope may be regarded asa heat-engine, all the parts of which start at a certain temperature, and which yields mechanical energy, while the only other change is that some of its parts are cooled to a lower temperature. This contradicts the Second Law of Thermodynamics as formulated by Lord Kelvin, if we leave the word “inanimate” out of his enunciation. His state- _ ment of the axiom is :—‘‘ It is impossible by means of inani- mate material agency, to derive mechanical effect from any portion of matter by cooling it below the temperature of the coldest of surrounding objects.” It is legitimate here to omit the word “inanimate,” as its insertion merely means that cases of exception to the law may be met with in the organic world ; and if this be stated it will need to be added that cases of exception may also be found among inorganic processes: the correct statement being that the law does not apply to individual molecular events, and that therefore it need not be obeyed in the cases, whether organic or inorganic, in which any observable effect is the outcome of one-sided molecular events. - It should be borne in mind that the heat of a given portion of matter is the energy * of motions of and within its molecules; * The energy here spoken of may be partly potential: in fact while motion is going on, the “energy of the motion,” or a part of it, usually fluctuates between being kinetic and potential. 392 Intelligence and Miscellaneous Articles. not necessarily of all such motions, but of those among them which are capable of restoring energy to the parts of the molecule carrying electra (see Stoney on “ Double Lines in Spectra,” Scientific Transactions of the Royal Dublin Society, vol. iv. part xi.) whenever the motion of the electron has transferred energy from the molecule to the ether. As ful- filling this criterion we are probably to include all irrotational motions within the molecules, and we must also include rela- tive motions of the molecules—all of them indeed if time enough be allowed for turmoil within a fluid to subside. It does not include any motion which the molecules have in common, as in wind, or in the rotation of a wheel. When these circumstances are taken into account, it is obvious that the energy of the heat-motions of an individual molecule undergoes rapid fluctuations, while there may be a definite average of the energy of these motions, whether esti- mated by what happens in an individual molecule over a sufficiently long period of time, or when estimated by what occurs simultaneously in all the molecules of a body. In other words, the motions of an individual molecule do not from instant to instant conform to the Second Law of Thermo- dynamics, although the law may apply both to the average of the motions of a single molecule taken over a long period of time, and to the average of the simultaneous motions of vast multitudes of associated molecules. As regards molecular motions (the motions within a solid, or motions within a fluid that do not produce currents in the fluid), the millionth of one second is a long period. XXXVIII. Intelligence and Miscellaneous Articles. ON THE MAGNETIZATION OF IRON RINGS SLIT IN A RADIAL DIRECTION. BY H. LEHMANN. ee chief results of the present research may be summed up in the following principles, which hold for an imperfectly closed ferromagnetic ring, the radius of which is large in comparison with the radius of the section :— 1. The demagnetizing factor, or the factor which, multiplied by the mean magnetization, gives the mean factor of the demag- netizing force, is constant up to about half the saturation. 2. The coefficient of dispersion (Strewungs-coefficient), the ratio of the mean induction to that in the slit, is constant up to half saturation. 3. The region of the dispersion of the lines of force is limited essentially to the vicinity of the slit, and is narrower as the magnetization increases. 4, The coefficient of dispersion is independent of the radius of the ring; in regard to its constancy (2), it only depends on the Intelligence and Miscellaneous Articles. 398 relative width of the ring d/r. The empirical expression for this dependence is a linear one of the form ete 7 where h is a constant which, for the Swedish iron investigated, has the value 7, and will presumably have values differing but little from this in the case of other ferromagnetic metals. This will probably be the case more especially in the kinds of iron used in technical processes. 5. When the empirical constant 2 is known, the factor of demagnetization can be calculated from the geometrical dimensions of the system by the formula Ne 2d d aN? Pan = Earl in which p is the radius of the ring, r that of the section, and d the width of the slit. This formula holds with the same limitation as (1), (2), and (4), that is, up to demisaturation. In general the equation holds, 2d medi 1 ayy (p—z) in which y is the factor of dispersion. 6. For high magnetizing values the factor of demagnetization approaches the limiting value Nope 5 are me a) ee: The previous results may find an approximate application even in imperfect magnetic circuits of complicated shapes.—Wiedemann’s Annalen, No. 3, 1893. N= THE SPECIFIC HEAT OF LIQUID AMMONIA. BY C. LUDEKING AND J. E. STARR. The specific heat of liquid ammonia, though it has often been the subject of calculation in development of theory and practice, has not yet been satisfactorily determined experimentally, if we except the work of Regnault. His results, however, were unfortunately lost during the Paris Commune. He assumed the specific heat to be 0°799. Since then the interest in this constant has very considerably increased through the rapid development of the artificial ice industry. Generally the specific heat has been taken at unity. Thus De Volson Wood in his ‘Thermodynamics,’ page 337, recommends this value “ until the experimental value is determined.” | It was our good fortune to have ready access to all the means necessary for executing the somewhat laborious experiments involved, and we take this opportunity to present briefly the a94 Intelligence and Miscellaneous Articles. results of our work. The liquid ammonia used in the experiments was found on examination to contain 0°3 per cent. of moisture and on spontaneous evaporation to leave only a trace of residue. The impurities were therefore of no consequence in influencing the result to the limit of accuracy intended. Of this liquid ammonia 10°01 grams were introduced into a small steel cylinder of 16:122 c.c. capacity, stoppered by a steel screw. The mode of filling was quite simple. After cooling the cylinder in a bath of the liquid ammonia itself and while still immersed, it was possible to pour it brimful by means of a beaker. The steel screw stopper, also previously cooled, was then inserted and drawn almost tight. On then removing the cylinder from the cooling bath, the liquid contents gradually expanded and escaped in quantity proportional thereto, and besides a very small vapour space was allowed to form as is indicated in the experimental data. Then the stopper was driven tight. Thus the error in the result due to the latent heat of condensation of vapour of ammonia in the course of the experiments was reduced to a minimum and rendered, as will be seen, almost inappreciable in its influence. The cylinder was perfectly free from leakage and remained constant in weight during each series of determinations. It was suspended in the drum of a Regnault apparatus heated by the vapour of carbon disulphide. The entire mode of procedure was in all details that commonly used in the Regnault method. After the cylinder had been heated for about six hours, it was dropped into a brass calorimeter whose water value was 1°36 cal. and which contained 150 grams of water. In each experiment it required very nearly two minutes to raise the calorimeter to its maximum temperature. The influence of loss by radiation was reduced to a minimum by the Rumford manipulation. The thermometers used were standardized, carefully compared, and read to hundredths of a degree by means of a magnifying lens. The experiments were conducted sufficiently far from the critical temperature, which according to Vincent and Chappuis is 131° C. The following are the data of Experiment 1 :— Weight of steel cylinder and ammonia. .. 81-008 grams. Weight of steel cylinder ............%. 70°998 9 Weicht of ammonia ..j.e0es52<. . AEG 10-01 25 The specific gravity of liquid ammonia being 0°656, the volume of 10°01 grams is 15:26 c.c. Total water value of calorimeter, thermometer, Bit WVAIeE ne. cs SEE A. ss 151°76 cal. ‘Water value of steel cylinder ............ 8°34 cal. eMmEperavure OF di... eos. s 5 ts ee 25°4 C. Temperature of steel cylinder ............ 46°51 C. Temperature of calorimeter after immersion 26°69 C. Temperature of calorimeter before immersion 24°44 C, ftsse in temperaburers 1. Aa crew. ss. ys bot 2°25 C. Intelligence and Miscellaneous Articles. 395 Thus 341:46 cal. were given off by the cylinder in cooling 19°82 or 17:23 cal. for one degree. Of this 8°34 cal. are due to the steel cylinder itself, leaving 8°89 cal. for 10°01 grams of liquid ammonia or 0°888 per gram=specific heat. In a second and third experiment the values 0°897 and 0896 were obtained. The determination of the specific heat of liquid ammonia would be influenced, as stated, by the latent heat of condensation of part of the small quantity of vapour present, when the cylinder cools in the calorimeter. This would to a degree be neutralized by the contraction of the liquid ammonia itself in the cooling and the consequent formation of more vapour space. It seemed desirable to ascertain the influence of these factors collectively by experiment. or this purpose specific heat deter- minations were made in a way somewhat different from the ordinary. The steel cylinder was cooled in an iron shell in melting ice, instead of being heated, and then introduced into the warm calorimeter water. The mode of precedure was in detail similar to that described above, and we will therefore only give our results. In three experiments the values 0°878, 0°863, and 0-892 were obtained. They are a trifle lower in their average than the results obtained by the ordinary method. It.is reasonable to assume that they are somewhat low, while as stated the other results are presumably somewhat high ; and in order to arrive at the specific heat of this substance nearest the true value from our experimental evidence, we will take the average of our six values, viz. : 0-888 0-878 0-897 } 1st series, 0-863 $ 2nd series, 0-896 0:892 and state it as being=0°8857. _ We beg herewith to acknowledge our obligations to Chancellor W.S. Chaplin and Prof. Wm. B. Potter for kindly placing the laboratories under their charges at our disposal.—Stlliman’s Journal, March 1893. ON THE OFFICIAL TESTING OF THERMOMETERS. BY H. F. WIEBE. In the year 1885 the Imperial Standards Commission undertook on a large scale the official testing of thermometers which is of such great importance both in science and in practice ; while pre- viously only a few institutions, such as the Naval Office, had occupied themselves to a limited extent with the investigation of thermometers. These official testings were transferred to the recently established Physical Technical Imperial Institute, to which since then a great number of thermometers have every year been sent for investigation. (In Ilmenau there is a branch for these testings.) Through the great progress which has been made since Jena glass has been used for thermometers, it has been possible to undertake a permanent guarantee for the results obtained in such testing ; and from the uniformity of this glass the thermometric constants, once determined, may be universally adopted. The testing takes 396 Intelligence and Miscellaneous Articles. place in two ways—either by comparison with a standard thermo- meter at different temperatures, or by calibration and determina- tion of the thermometric constants. The comparison of the thermo- meters is made between 0° and 50° in water-baths; above 50° in boiling-point apparatus with reversing condensers, in which liquids of various boiling-points are used for the determinations. The following liquids were found to be especially suitable :— Boiling-point. Boiling-point. Clvoroform “i262: .-- 60°6° Toluole \.. ..«s ptibuan i \ etbartny) dss but - bf BS sin eC S2—] ptibuan — et? > ben : e . bap sin Multiplying the disturbance by itself with —z in place of +1, we have for the light intensity, >= bapx? sin ees 2 sin cs The first term indicates spectral lines in positions given by the equation : a 7 = 3 with intensities given by the last integral. The intensity of the spectral lines then depends on the form of the groove as [ \ eBOz+uy) ds || ( etibrtuy ds]. sin in Theory and Practice. . A401 given by the equation «=/(y) and upon the angles of inci- dence and diffraction. The first factor has been often discussed, and it is only necessary to call attention to a few of its pro- perties. When baw=27N, N being any whole number, the expres- sion becomes n”?, On either side of this value the intensity decreases until nbay'=2aN, when it becomes 0. The spectral line then has a width represented by p/—w! = 2F nearly ; on either side of this line smaller maxima exist too faintly to be observed. When two spectral lines are nearer together than half their width they blend and form one line. The defining power of the spectroscope can be expressed in terms of the quotient of the wave-length by the difference of wave-length of two lines that can just be seen as divided, The defining power is then nN*=na 3 Now na is the width of the grating. Hence, using a grating at a given angle, the defining power is independent of the number of lines to the inch and only depends on the width of the grating and the wave-length. According to this, the only object of ruling many lines to the inch in a grating is to separate the spectra so that, with a yiven angle, the order of spectrum shall be less. Practically the gratings with few lines to the inch are much better than those with many, and hence have better definition at a given angle than the latter except that the spectra are more mixed up and more difficult to see. It is also to be observed that the defining power increases with shorter wave-lengths, so that it is three times as great in the ultra-violet as in the red of the spectrum. This is of course the same with all optical instruments such as telescopes and microscopes. , The second term which determines the strength of the spectral lines will, however, give us much that is new. First let us study the effect of the shape of the groove on the brightness. If N is the order of the spectrum and a the grating-space, we have e=Il(singd+sin py) = =~, ba, since sin —<" ==()) 2 * An expression of Lord Rayleigh’s. 402 Prof. Henry A. Rowland on Gratings and the intensity of the light becomes proportional to [ iy il (F242) ds}[ (fe —ion(J2t Sy) ds}. It is to be noted that this expression is not only a function of N but also of lJ, the wave-length. This shows that the intensity in general may vary throughout the spectrum ac- cording to the wave-length, and that the sum of the light in any one spectrum is not always white light. This is a peculiarity often noticed in gratings. Thus one spectrum may be almost wanting in the green, while another may contain an excess of this colour; again, there may be very little blue in one spectrum, while very often the similar spectrum on the other side may have its own share and that of the other one also. For this reason I have found it almost impossible to predict what the ultra-red spectrum may be, for it is often weak even where the visible spectrum is strong. The integral may have almost any form, although it will naturally tend to be such as to make the lower orders the brightest when the diamond rules a single and simple groove. When it rules several lines or a compound groove, the higher orders may exceed the lower in brightness, and it is mathe- matically possible to have the grooves of such a shape that, for given angles, all the light may be thrown into one spectrum. It is not uncommon, indeed very easy, to rule gratings with immensely bright first spectra, and I have one grating where it seems as if half the light were in the first spectrum on one side. In this case there is no reflexion of any account from the grating held perpendicularly: indeed, to see one’s face the plate must be held at an angle, in which case the various features of the face are seen reflected almost as brightly as in a mirror but drawn out into spectra. In this case all the other spectra and the central image itself are very weak. In general it would be easy to prove from the equation that want of symmetry in the grooves produces want of symmetry in the spectra—a fact universally observed in all gratings, and one which I generally utilize so that the light may be concentrated in a few spectra only. Example 1.—SQuaRE GROoVEs. When the light falls nearly perpendicularly on the plate, we need not take the sides into account but only sum up the surface of the plate and the bottom of the groove. Let the depth be X and the width equal to a m in Theory and Practice. 403 The intensity then becomes proportional to ES sin? 7 sin? wy X, This vanishes when . N=m, 2m, 3m, &e. ; l The intensity of the central light, for which N=0, will be Tes ho 7s (x7 x This can be made to vanish for only one angle for a given wave-length. Therefore, the central image will be coloured and the colour will change with the angle, an effect often observed in actual gratings. The colour ought to change, also, on placing the grating in a liquid of different index of refraction, since \ contains I, the index of refraction. It will be instructive to take a special case, such as light falling perpendicularly on the plate. For this case, o=0, X=1(1 + cos), and p=lsinp= Hence =0, 1, 2, 3, &e. rat{lea/i -(5 hb The last term in the intensity will then be ‘ Small 1 N\2 2 as sin 4X17 + ee, As an example, let the green of the second order vanish. In this case, /="00005. N=2. let a=-0002 centim.,.and b=: Then —_X[20000 + /(20000)?— (10000)"] =n. Whence pre i 8 37300" where n is any whole number. Make it 1. Then the intensity, as far as this term is concerned, will be as follows :— 404 Prof. Henry A. Rowland on Gratings Minima where Intensity is0.|| Maxima where Intensity is 1. Wave-lengths. -Wave-lengths. Ist spec....| *0000526 0000268 | 0001000 | 00003544 | -00002137 2nd ,, ...| °0000500 ‘0000266 0000833 | 00003463 | -00002119 ord ,, ...| *0000462 0000263 =| 0000651 | 00003333 | -00002089 4th ,, ...| °0000416 ‘0000259 | 0000499 | 00003169 | -00002050 thy oaere &e. &e. | &e. &e, &e. The central light will contain the following wave-lengths as a maximum :— "0001072, :00003575, °0000214, &e. Of course it would be impossible to find a diamond to rule a rectangular groove as above, and the calculations can onl be looked upon as a specimen of innumerable light distribu- tions according to the shape of groove. Every change in position of the diamond gives a different light distribution, and hundreds of changes may be made every day and yet the same distribution will never return, although one may try for years. Example 2.—TRIANGULAR GROOVE. Let the space a be cut into a triangular groove, the equations of the sides being e=—cy and w=c'(y—a), the two cuttings coming together at the point y=u. Hence we have —cu=c(u—a), and ds=dy-V/1+c?, or dyV¥1+c?. Hence the intensity is proportional to EN. 1 (Ee. ow 1 V(1+c¢?)(1+e¢?) . mu(u—cr) . m(a—u)(w+er) aes UN) | sl a cos [(H+eA)(a—u)—n(u—er)] t pf 1+¢ ea Dg bam 2p—m+1 ey we sin ou : 7 2m 2 Now the first two terms have finite values only around the points — =mNz, where mN is a whole number. But 2p—m-+1 is also a whole number, and hence the last term is zero at these points. Hence the term vanishes and leaves the intensity, omitting the groove factor, sin? n a sin? n—/ x + (bv) 2 sin fee ‘ sin? bape 2m F 9 | in Theory and Practice. 409 The first term gives the principal spectra as due to a grating- space of < and number of lines nm as if the grating were perfect. The last term gives entirely new spectra due to the erating-space a, and with lines of breadth due to a grating of n lines and intensities equal to (duv)?. Hence, when the tangent-screw is used on my machine for 14,436 lines to the inch, there will still be present weak spectra due to the 14,436 spacing, although I should rule, say, 400 lines to the millim. This I have practically observed also. The same law holds as before that the relative intensity in these subsidiary spectra varies as the square of the order of the spectrum and the square of the deviation of the line or lines from their true position. | So sensitive is a dividing-engine to periodic disturbances, that all the belts driving the machine must never revolve in periods containing an aliquot number of lines of the grating ; otherwise they are sure to make spectra due to their period. As a particular case of this section we have also to consider Periopic HRRors oF RuLING.—THEORY oF “ GHOSTS.” In all dividing-engines the errors are apt to be periodic, due to “drunken” screws, eccentric heads, imperfect bearings, or other causes. We can then write Y=Na+ a, sin (en) +a sin (en), + ke. The quantities ¢,, ¢, &c. give the periods, and a, ay, Ke. the amplitudes of the errors. We can then divide the integral into two parts as before, an integral over the groove and spaces and a summation with respect to the numbers. UU y" y"-y s| e—BAt+Ky) ds = Set | e—tbAntny) ds, y' 0 It is possible to perform these operations exactly ; but it is less complicated to make an approximation, and take y!—y'=a, a constant as it is very nearly in all gratings. Indeed the error introduced is vanishingly small. The integral which depends on the shape of the groove will then go outside the summation sign, and we have to perform the summation Se—ibu | aon+ a, sin er + asin eyn+ &e. 410 Prof. Henry A. Rowland on Gratings Let J, be a Bessel’s function. Then cos (usin 6) =Jo(u) +2[Jo(u) cose p+dy(u) cosyh+ &e.], sin (usin 6) = 2fJy(w) sind +33(u) sing d+ Xe. |. Bye e— usin? — cos (usin d) —2 sin (usin d). Hence the summation becomes ( g-ibpagn x [J o(buay) + 2(—23 ,(bua,) sin en + Jo(buay) cos 2e;n— Ke.) Ss x [Jo(buae) + 2(—t3 (buy) sin egn + J 2( buy) cos 2en — Xe.) x [Jo(buas) + &e.) | Lx [ &e. ]. Case I.—Si1ncGLE PERIoDIC HRROR. In this case only ap and a; exist. We have the formula pine sin” Seteimag a? 4 ae sins Hence the expression for the intensity becomes 2 2 \ sin n wal | sin n ts ot +] Jo(bua,) ———— 7+ J," (bya | Pens (+9 OH a | 2 2 2 4 ee 2 | sin pete ta | 4 ee, + &e. om e1 | sin | J As n is large, this represents various very narrow spectral lines whose light does not overlap, and thus the different terms are independent of each other. Indeed, in obtaining this expression the products of quantities have been neglected for this reason because one or the other is zero at all points. These lines are all alike in relative distribution of light, and their intensities and positions are given by the following table :— in Theory and Practice. 411 Places. Intensities. Designations. = = ah J0°(bmay). Primary lines. . 0 . fe pe ca Jy?(bpey a1). Ghosts of 1st order. 2e fg=bt a Jo°(bpya2). Ghosts of 2nd order. p= Pe < J3°(bpras)- Ghosts of 3rd order. &e. &c. ac. Hence the light which would have gone into the primary line now goes to making the ghosts, so that the total light in the line and its ghosts is the same as in the original without ghosts. The relative intensities of the ghosts as compared with the primary line is . Jn’ (bya) Jo” (bua) This for very weak ghosts of the first, second, third, &c. order becomes 2 4 6 Ay 2 Ag 6 Ag The intensity of the ghosts of the first order varies as the square of the order of the spectrum and as the square of the relative displacement as compared with the grating-space ap. This is the same law as we before found for other errors of ruling; and it is easy to prove that it is general. Hence The effect of small errors of ruling is to produce diffused light around the spectral lines. This diffused light is subtracted from the light of the primary line, and its comparative amount varies as the square of the relative error of ruling and the square of the order of the spectrum. Thus the effect of the periodic error is to diminish the intensity of the ordinary spectral lines (primary lines) from the intensity I to Jo*(bua,), and surround it with a sym- metrical system of lines called ghosts, whose intensities are given above. When the ghosts are very near the primary line, as they nearly always are in ordinary gratings ruled on a dividing- 412 Prof. Henry A. Rowland on Gratings engine with a large number of teeth in the head of the screw, we shall have 2 LZ 2 A \ _ oe J bay (u+ i )+d pha, (1 = 2J,°bayu nearly. Hence the total light is by a known theorem, Jo? + 2[J,?+J,.?+ &e. |=1. Thus, in all gratings, the intensity of the ghosts as well as the diffused light increases rapidly with the order of the spectrum. This is often marked in gratings showing too much crystalline structure. For the ruling brings out the structure and causes local difference of ruling which is equivalent to error of ruling as far as diffused light is con- cerned. For these reasons it is best to get defining power by using broad gratings and a low order of spectra, although the increased perfection of the smaller gratings makes up for this effect in some respects. There is seldom advantage in making both the angle of incidence and diffraction more than 45°, but if the angle of incidence is 0, the other angle may be 60°, or even 70°, as in concave gratings. Both theory and practice agree in these statements. Ghosts are particularly objectionable in photographic plates, especially when they are exposed very long. In this case ghosts may be brought out which would be scarcely visible to the eye. As a special case, take the following numerical results :-— N= 1. 2. 3. @ gl 1.4. 11 22 a; 25 50? 100 25’ 50° 100, 2555p aumm (xt) 4 td TG) 63’ 252? 1008 16 63° 252° = 7? 28? 102" In a grating with 20,000 lines to the inch, using the third spectrum, we may suppose that the ghosts corresponding to “ — = will be visible and those for i 1 a 50 very trouble- 0 25 in Theory and Practice. 413 some. ‘The first error is a;= zo9hp95 in. and the second =spo000 m. Hence a periodic displacement of one Set of an inch will produce visible ghosts and one five- hundredth-thousandth of an inch will produce ghosts which are seen in the second spectrum and are troublesome in the third. With very bright spectra these might even be seen in the first spectrum. Indeed an over-exposed photographic plate would readily bring them out. When the error is very great, the primary line may be very faint or disappear altogether, the ghosts to the number of twenty or fifty or more being often more prominent than the original line. Thus, when bya, = 2°405, 5°52, 8°65, &e. =2nN-, 0 the primary line disappears. When bjs, =0, 3°83, 7:02, é&e. =20N-, 0 the ghosts of the first order will disappear. Indeed, we can make any ghosts disappear by the proper amount of error. Of course, in general ics toet » Ji, He) n—2° Thus a table of ghosts can be formed readily and we can always tell when the calculation is complete by taking the sum of the light and finding unity (see p. 414). This table shows how the primary line weakens and the ghosts strengthen as the periodic error increases, becoming 0 at InN = 2-405. It then strengthens and weakens periodi- 0 cally, the greatest strength being transferred to one of the ghosts of higher and higher order as the error increases. Thus one may obtain an estimate of the error from the appearance of the ghost. Some of these wonderful effects with 20 to 50 ghosts stronger than the primary line I have actually observed in a grating ruled on one of my machines before the bearing end of the screw had been smoothed. The effect was very similar to these calculated results. Phil, Mag. 8. 5. Vol. 35. No. 216. May 18938. 2F 414 Prof. Henry A. Rowland on Gratings GGO: | 600: | ITO: vl “Sip | ool p TOL. | 40. | GO0- 0cO: | GOI | PIT €00: | LTO: | T90- eee . . ° eee see ° eae ee eee . eee ° see vee eee eee eee eee eee eee ee ° eee 80: T10- eee ee eee eee eee . sein 0.01 * $99.8 CS he OTOL ok ina 06a¢ a Ove oe ae * ZEB. Ba (Ns "* 409% ee Fie a in Theory and Practice. 415 DovusLE Pertopic ERROR. Supposing as before that there is no overlapping of the lines, we have the following :— Places. Intensities. = = [Jo(dyae) Jo(bazp) |?. Primary order. 0 e ‘ 7 taee a [91 (a 41) JoC are) ]?. | Ghosts of Ist Bs : r order. M2 = et ba [Jo (basme) Ji (daefe) ]?. | ete, M3 = b+ = [Js (bays) J, (Daopes) ]?. 7 aa 2e 5 | hosts ef 2nd fs, = eat Ta [Jo (ba,p4) Jo (Daopt4) |. G oe 2 ; | s= wtp — [Fo(bams) Fa(daqes) +2 be = WETS, [Ty (Barge) Ta(Daaue) ). > 2 Pe ai [J o(Daypez) Ja (Deof47) |?. “ Y \ Ghosts of 3rd ps = B45 —— [Io(aypts) Js (Baus) }* | ae Uy 3 : Hy = wp [3 (betof49) Jp (batopte) ]?. Ac. ae. Each term in this table of ghosts simply expresses the fact that each periodic error produces the same ghosts in the same place as if it were the only error, while others are added which are the ghosts of ghosts. The intensities, however, are modified in the presence of these others. Writing c,=ba,p and c.=bapy. The total light is 2357(c,) Jo° (ce) 2517(e1) Jo?(co) 2071 2/., r Jo (¢,) Jo’ (cg) + | + 2c.) J (co) } i Fone a0) oe o (C1) Jo (C2 which we can prove to be equal to 1. 2F 2 416 Prof. Henry A. Rowland on Gratings Hence the sum of all the light is still unity, a general pro- position which applies to any number of errors. The positions of the lines when there is any number of periodic errors can always be found by calculating first the ghosts due to each error separately; then the ghosts due to these primary ghosts for it as if it were the primary line, and so on ad infinitum. In case the ghosts fall on top of each other the expression for the intensity fails. Thus when e.=2e,, 3, = 3, uc., the formula will need modification. The positions are in this case only those due to a single periodic error, but the inten- sities are very different. Places. 2QaN 5 = [Jo(bayw)T y(basu) |. 0 = pt ap [J if (bap) J 0 (bap) —J 3(bayfy) JS 2 (Dae p11) = Ke. | 2 & ~~ bag + [Js (Gap) Ss (42p41) re 3(bayp5) 3; (baopey) + &e. ]?. ‘Ke eG We have hitherto considered cases in which the error could not be corrected by any change of focus in the objective. It is to be noted, however, that for any given angle and focus every error of ruling can be neutralized by a proper error of the surface, and that all the results we have hitherto obtained for errors of ruling can be produced by errors of surface, and many of them by errors in size of groove cut by the diamond. Thus ghosts are produced not only by periodic errors of ruling but by periodic waves in the surface, or even by a periodic variation in the depth of ruling, In general eee ever, a given solution will apply only to one angle and consequently, the several results will not be identical : - some cases, however, they are perfectly so. Let us now take up some cases in which change of focus can occur. ‘The term «7? in the original formula must now be retained. | Let the lines of the grating be parallel to each other. We can then neglect the terms in z and can write r2= 2 ver nearly. Hence the general expression becomes ered 10(AZ+ py—Ky2 Se ees: where « depends on the focal length. is i very (ead aad hence « is small. ; vis 16 oppose The integral can be divided into two parts—an integral over the groove and the intervening space, and a summation for all the grooves. The first integral will slightly vary with in Theory and Practice. AIT change in the distance of the grooves apart, but this effect is vanishingly small compared with the effect on the summa- tion, and can thus be neglected. ‘The displacement is thus proportional to DS eib(uy—Ky?) Case I.—Lines at VARIABLE DISTANCES. In this case we can write in general y=an+a,n? + apn’ + &e. AS K, %, a, &¢., are small, we have for the displacement, neglecting the products of small quantities, Dd etlelant ayn2+ agn3+ &e.)—Ka2n2] Hence the term an? can be neutralized by a change of forms expressed by wa,=«xa®. Thus a grating having such an error will have a different focus according to the angle n, and the change will be + on one side and — on the other. This error often appears in gratings and, in fact, few are without it. A similar error is produced by the plate being concave, but it can be distinguished from the above error by its having the focus at the same angle on the two sides the same instead of different. According to this error, a,n?, the spaces between the lines from one side to the other of the grating, increase uniformly in the same manner as the lines in the B group of the solar spectrum are distributed. Fortunately it is the easiest error to make in ruling, and produces the least damage. The expression to be summed can be put in the form See" + tb( wa, — Ka?)n? + ibpagn? + ib [wag + 2b (wa, — Ka?)?] n4 + &e. | The summation of the different terms can be obtained as shown below, but, in general, the best result is usually sought by changing the focus. This amounts to the same as varying « until wa,—Kxa?=0 as before. For the summation we can obtain the following formula from the one already given. Thus n—1 1 . sm np . 3h e2tpn P pip(n—1), in p Hence = 1: Ame Chine ae ™sin np m2ipn — ip(n—1)f rane eA ee a ane (inn? (z+éln 1)) Tar 418 On Gratings in Theory and Practice. When 2 is very large, writing = =pn=aNn+q, we have a—1 Mon > nine2tpr — —¢ (2 4 +4) S: Js g @ dq q Whence, writing ¢ = b(uay—xe), i bpoag, c" = bl pas + tb (pa,—xa’)’], cl" = &e., the summation is ( n’ nti( SHES ee ) | : (a pes 1 94. |) + (2c0 + aoe + 4c 13+ ia | ous yn ye & | salleeanen i(e; + 363 + 6¢ Te a cng q _ (et n° )\S | ( Sag ae 5 4 5, ore +2\ 6 a. | + &. } dsnq_ eos si dq q q @ sing _ —2q cos g + (2—¢?) sing dey q° anes _ (69) cos g— (6—3¢') sing dy’ g q | &e. &e. These equations serve to calculate the distribution of light intensity in a grating with any error of line distribution suitable to this method of expansion and at any focal length. For this purpose the above summation must be multiplied by itself with +2 in place of —2. The result is for the light intensity On the Differential Equation of Electrical Flow. 419 4 e 3 See E+ (ach + 205 + ce aa q t /dq q n 8 4 5 3 ot Q —_ (es ieee ke.) a wag + &e. \ { 8 16 dg q n nt d’ sing anes a sin g a (oN + be. ee + &. ¢ - As might have been anticipated, the effect of the additional terms is to broaden out the line and convert it into a rather complicated group of lines, as can sometimes be observed with a bad grating. At any given angle the same effect can be produced by variation of the plate from a perfect plane. Likewise the effect of errors in the ruling may be neutralized for a given angle by errors of the ruled surface, as noted in the earlier portions of the paper. XL. On the Differential Equation of Electrical Flow. By T. H. Buaxestey, J/..4.* apes object of this paper is to point out that the theory of electrical discharge, as exemplified in the mathe- matical expressions employed to represent the physical facts, is incompetent to explain all the phenomena observed in extreme cases; and to show that the admission of certain properties of matter not usually recognized is the only way of satisfactorily obviating the imperfection of the existing views. In some of the investigations I shall not employ exclu- sively algebraical symbolic methods, but, where it may more advantageously be adopted, I shall avail inyselt of the geome- trical method. Such cases most frequently arise where magni- tudes under consideration are capable of having negative values. All tidal effects, using the word in its most general sense, involve such magnitudes. Hlectrical currents in a given conductor may have all possible values in one direction or in the opposite direction, but are otherwise restricted. The projection of the line joining two points in space upon a fixed straight line is a geometrical magnitude of this sort. With respect to the direction in space, sometimes one of the projected points will be on one side of the other * Communicated by the Physical Society: read March 24, 1893. 420 Mr. T. H. Blakesley on the Differential projected point, sometimes on the other. So that sucha line has all the properties necessary for representing another magnitude of the same character. . In this way I shall most generally make the projection represent Hlectromotive Force, but occasionally Field of Magnetism at a point. As to matter of nomenclature, the only scientific term which | shall employ admitting of any doubtful interpretation, is the Effective Electromotive Force. By this term I intend to convey the idea of that eleciromotive force which is numerically equal to the product of the current and the resistance, at a point of time. Asa department of State has recently employed the term in a totally different sense, this statement has appeared to me to be necessary in the interests of proper explanation. The effective electromotive force is the algebraical sum of all the impressed and induced electromotive forces, and is here represented by E. If V is the sum of all the impressed electromotive forces and F is the sum of all induced electro- motive forces, then the equation among their quantities is V+F=E universally. ? Geometrically, if AB, BC are lines whose projections on some one fixed straight line represent the sum of the im-. pressed and the sum of the induced electromotive forces respectively, then the projection of AC will represent the effective electromotive force. The three lines must form the sides of a triangle, those corresponding to the impressed and induced electromotive forces being taken the same way round the triangle, that corresponding to E being taken in the opposite direction. Now if the actual changes in the magnitudes are harmonic, and of the same period, it is clear that the lines A B, BC, AC must remain of constant length and the triangle must rotate in its own plane at a uniform rate of such a value as to perform a complete revolution in the period of the har- monic change. ‘The triangle thus shows admirably the way in which these magnitudes succeed one another in phase. It also foliows from the properties of harmonic motion that if two magnitudes have the same harmonic period, but differ in phases by a quarter of the whole period, the corresponding lines to be projected are at right angles with each other. And hence the rate of variation of an harmonic magnitude differs in phase from the magnitude itself by a quarter of the period. But in the simplest case of a circuit being plied with an harmonic electromotive force V, it is generally considered that the induced electromotive force varies as the Equation of Electrical Flow. 4AQ1 rate of change of the current ; that is gC > Lidl eG i> ie > eae for H=RC, where C is the current, R the resistance, and L is the coefficient of self-induction. The equation already given then becomes yee Lo? =n RC. Multiplying through by C ee integrating through a com- plete period, VeanL foo? ari cat The first term represents the work done by the source of the disturbance. The second term vanishes. The third term represents work done in heating the circuit. Hence the whole work done has gone to heat the circuit. Now it is admitted on all hands that when the period is sufficiently short a radiation of energy into space takes place. A portion of this radiated energy is sometimes caught by means of a neighbouring circuit and converted into heat. A coefficient of mutual induction and a corresponding extra term is then introduced into the equation. But are we to suppose that radiation would not proceed into space were there no neighbouring conductor? Itis against proba- bility, against the electromagnetic theory of light. If electromagnetic waves are capable of being sent into space, we can no longer look upon the operation of establish- ing a current in a circuit as analogous to bending a stiff spring or displacing rigid wheelwork. The wheelwork must have indiarubber spokes or teeth. The above equation takes no account of this radiation whieh j is expended outside the wire, nor of any other work done else- where than in the conductor ; and this latter the equation states to be exactly equal to the ener gy expended in propa- gating the electromotive force. Hven supposing a portion of the field is occupied by some material whose passage through a cycle of magnetization involves the loss of energy, in the form of heat, this, equally with wave-propagation through space occupied by perfectly elastic matter, will not be accounted for by the equation. Now of such phenomena as radiation of energy in electro- magnetic waves, or absorption of energy in the field, there is 422 Mr. T. H. Blakesley on the Differential ample evidence. Therefore an equation will not meet such eases in which the induced electromotive force is taken as entirely in quadrature with the current, or when F is wholly of the form pee . dt Hence, in the geometrical representation it is clear that the induced electromotive-force line must not be exactly at right angles with that of = the effective electromotive-force line; 7. e. the angle BC A is not exactly a right angle; and it is easy to see that it must be greater than a right angle, for B C may be resolved into BD.DC, where BDC is a right = angle and A C D is one straight line. For C then the whole work done is equal to gD yal 7A cell the conductor is The work done in heating J ° A ea and the differ- ence, or the work done in the field, is see Hence, if D lies on the side of C neurer to A, A D would be less than A C, and the work done by the discharge would be less than that required to heat the conductor: in other words, energy would have to be received from space. Hence the induced electromotive forces may be represented by two components—one A D in quadrature with the current, and one D C in opposition to it, dC -L& -a¢, where % may or may not be a constant, but is in kind a resistance. The equation among the electromotive forces may be written dC V—L--—’AC=RC. Multiplying through by Cdt and integrating through a complete period, {v Cdt—L jc - dt= R| Cae + facta, The second term on the left vanishes as before, the first term representing the whole work dove. On the right the Equation of Electrical Flow. 423 first term heats the conductor and the second term gives energy to space. We may go somewhat further into the causes of such an in- duced electromotive-force component if we employ the geometrical mode of symboli- B zing the electric quantities. BC,the induced electromotive-force line, should be at right angles to the induction through the circuit, for it is the rate of increase of the latter D which produces the former. Hence if A H is a perpendicular let fall upon BC pro- C duced, A E will represent the phase of the magnetic induction. But AC being in E phase with the current is in phase with the field. Hence HAC, or CBD which is equal to it, is a magnetic phase-lag, and A E may be said to be in phase with the effectve field, and therefore with the induction. This suggests that if we employ the lower lines of the figure to represent fields, we may make up a triangle A CE such that A Cis the impressed field, C E an induced field, and A E an effective Cc field, of course when, as usual, projected on a fixed line ; C EH being perhaps, though by no means certainly, at right angles to AE. E However, whether CHE here has in any a case two components perpendicular and parallel respectively to A EK or not, it appears very certain that the perpendicular component must exist. Assuming at first that it alone exists,— If we employ small letters :— » for impressed field = AC, f for induced field =CH, e for effective fied =AH, 1 = coefficient of magnetic self-induction, so that A and yw for the permeability, I for the rate of magnetic induction, 1. @. per square centim., we have To obtain an equation of energy from this we must multiply (not by I, as analogy would at first sight perhaps dictate) by dl y : oe dt x cross section, for the formula for energy is 424 Mr. T. H. Blakesley on the Differential [?e-*m | = [we ~2t— me || welt ?m? lt = | Field | ane ia i a1 \(F) a = (Fo dt. Here the term on the right hand oe necessarily, and the work expended, if any, is equal to ( tan? B ~ sec? B—1’ and cos? B= : already obtained ; 1 Am tst 40° KL therefore ea 2 te aa 2 te te 1 (a therefore IaV KL ea the form usually quoted if we neglect the second term of the denominator. I purpose to show that in a discharge of the sort here con- templated (which has been shown to be the result of the ordinary premisses given at page 425) there will be no work done by any electromotive force which lags at an angle 6 behind the current, provided the initial condition is one of zero-current. And, further, that the source of H.M.F., which is represented by the side of the isosceles triangle in advance by the angle 8, of the effective H.M.F., does all the work of heating the circuit and no more. It will thus be seen that there is no provision in the theory for expenditure of power in the field, and hence that the theory does not explain the well recognized phenomenon of radiation into space. To establish the above-mentioned propositions, take the — product of the projections of two lines undergoing variations corresponding to the two radii vectores of two equiangular spirals of the same characteristic angle 8 and period, and differing in phase by the angle 2y. One of these quantities may be expressed by Equation of Electrical Flow. 431 EY ou ae tam8sin O+y. The other by Ore be nb sin @—y. The product is 26 ab.e ™Bsin O+y SID @—y, or 20 ab.e tamB (sin? @— sin’y), This quantity, multiplied into an element of time dt, has to be integrated through one period. Since = = = the integral 1 becomes abt a e eer (cos 2y— cos 20) dd, or mem tanB cos Yy dO — a pp oraces 26 dé. The first term of the integral is abt 8a The second term is ae ——cos 2y tan Be — =r 20 abt pale DB orcs 3, sin 8 cos B +20 ‘ ee and therefore the ce ig expressed :— Abts | = a Br ° This expression has to be taken between limits. If we con- template one revolution only the limits will be ®,+27 and @,, and the Definite Integral becomes Abts 20, 3 1—sin 8 cos B+ 3+ 20, +tan B cos Qyte™ tus( 1—e ~ ane ). If the limits are infinity and @, the integral becomes _. 26, us af ae Bcos2y—sinBcosB+203¢ me . (a) aie {sin 8 cos 8 +20—tan @ cos 2y}. Hither of these expressions becomes zero when tan 8 cos 2y=sin 8 cosB+ 20; 2G 2 432 Mr. T. H. Blakesley on the Differential or cos 2y=cos 8 cos B+ 26, showing that the condition that no work shall be done in the electric problem depends on the initial circumstances, 7.e. 0; -is involved. If 2y= the condition of no work becomes cos 8+ 26, =1, which is satisfied when Hence if the initial condition be that of no current, the line bisecting the angle between the line of effective H.M.F. and that of the self-induced E.M.F. makes —§ with the line @=0, and it is thus proved that on the whole no work is done in the field. If, on the other hand, we make é,=+ B : 1 2 7 and start from a point where the current is zero, we have in the above expression, when proper substitutions are made for a and 3, the value of the work done on the circuit by the discharging condenser. The integral between infinity and @, becomes, when 6,= C and ab. ty . F =e — {1— cos 26} sin 8.e tanB; or id Ais ee ORME ? sin®Be tank, ; iD ELIE Eh ecw § In this case 6= Rand ae tan sin Bis the potential difference between the plates of the condenser at starting =Vj, say, =Vsin8. Hence the expression becomes My ager. fd R:a,52 iS Ve (E and V being now the full sides of the triangle, properly E interpreted), and Z.y =e B by the geometry of the triangle, and further, Equation of Electrical Flow. 433 tan game mad thereiore = = ty Aq and the work pei’ ? i ty or ty sin? B sR 2cos 6 2tan 6 [ae Ge which is the expression we should obtain if we integrate the square of the current multiplied by Rdt, seen as follows :— In the general expression («) obtained above for the pro- by 2 tan B’ sin? 8, duct of the projections make a=H, b= = and 0,=0, y=0 the expression («) becomes sa {tan 8 —sin B cos 8} Pegee! an sin 6 cos f5, or EK? ty ; aR a B—sin 8 cos P}, or [Dee in t, sin” B, as above. Thus the whole of the work goes to heat the wire, and, further, substituting in the equation for E in terms of V, it may be shown to be entirely derived from the charged con- denser. The work may be written, eliminating E, 2V? cos B ty R Aar Ne ty O18) Kae cos B sin’ 8. sin’, or Now V/?=V’sin? @, and thus the work is t VR cos? B, . ry t or, since cos*B= a 1 V17ts KR = and é = —— Pree On oe VK — 5) 9 which is the ordinary expression for the energy stored in the condenser ; and this appears from the investigation to he 434 On the Differential Equation of Electrical Flow. entirely expended in heating the circuit, and there is no margin for the exhibition of power elsewhere. Suppose a line A B to represent (E) the line of effective E.M.F. At the extremity A set off AC as the direction of the line representing c the P.D. of the condenser. Then, as the condenser contains all the energy that is going to be expended on the circuit and on the ether, from what has been said it is clear that A C must be rather longer than the side of the isosceles triangle; for, if not, the energy stored will not do more than «a £ we heat the circuit. If therefore a perpen- dicular be dropped upon A B from GC, it will fall at a point nearer B than A. Join C B, and, further, draw C D to meet AB produced in D, and so that C DA is an isosceles triangle on A D as base, and therefore CDA=8. Now CB must be the line repre- senting the resultant of the induced electromotive forces F, and however complicated the case may be this line CB is equivalent to two components CD, DB: of which CD results in no expenditure of power because it is in a phase B behind the current, and DB is in phase directly opposed to the current, and therefore resulting in whatever expenditure of energy takes place outside the circuit, and therefore in the ether or in magnetic bodies, or in neighbouring or surround- ing conductors. Asin the former case of sustained oscillations, it may be shown that BCD isa magnetic lag necessary for the exhibition of such phenomena. The electromotive force DB may be expressed by —AC as before, and the general equation Vo E—s takes the form Vee be! nC dt and, as this may be written V-L& =(R+2)C, we see that the extra consideration required to express the actual state of things is simply that the resistance of the circuit is virtually increased. In the previous work it is necessary to write (R+)) in all the equations. Heat of Vaporization of Liquid Hydrochloric Acid. 435 The actual work done altogether is derived from the charged condenser. This is divided between the circuit and the field in the ratio R:X. It may happen, therefore, that if the circumstances of the discharge are such as to make X very large in comparison with R, the ordinary heating-effect may be minimized. Among such causes is frequency, and in this consideration is to be found the true explanation of some of the experiments of M. Nikola Tesla. The energy of the discharges which that physicist encountered was expended in chief part in radiation which his body did not check, and not in current through his body. It is here suggested that the best way to measure radiation would be to measure the defect in the heating of a _ circuit, taking care to note the P.D. of the condenser at the moment previous to discharge. In ordinary sustained oscillations, as derived from a machine, the alternations are not of sufficient frequency to make the effect of X perceptible. Hlectromotive forces of induction in- volve the period in their denominators, and it is reasonable to suppose that induced magnetic fields do the same; and if the period of the electromagnetic vibrations becomes com- parable with that of light, it is conceivable that mere heating might vanish, as in the solar spectrum light has less heating- effect than radiation of smaller frequency from the same source. XLI. Note on the Heat of Vaporization of Liquid Hydro- chloric Acid. By K. Tsuruta, Rigakush, Tokio, Japan*. | the thirtieth volume of the Proceedings of the Royal Society of London Mr. Ansdell gave a full account of a series of experiments on the condensation of hydrochloric acid. At the end of the paper he promises another commu- nication containing his considerations on some thermodyna- mical quantities relating to that gas, but this, so far as I am aware, has never appeared. Although his measurements have often been referred to and used by other physicists, yet some of the deductions that can be made from them appear still left untouched, for instance the heat of vaporization, which forms the subject of this note. For the sake of convenience of reference I- here reproduce those measurements as contained in the following Table given by Ansdell :— * Communicated by the Author. 436 K. Tsuruta on the Heat of Vaporization eel B ea |. m E F | a eS == | oe ip gee eee 1 | 4 [19781 | agp | (755 | Teme) eee 2, | 995 11896 | ges | 790 | 1505 | 939 3, | 188 |10350| soy | 885 | 1239 | 37°76 4 | 11 | or77 | sty | 874 | 1080 | 41-80 2 | eon 910 | 9892 | 45°75 6. | 2675 6969 | a5, 900) 7. | 38:4 | 55°75 }*t | 1019 | B50 loam | g | 394 | 4485 | ais | 1068 | 419 | 66-95 | 9. | 448 | 3634 | aaa | 1196 | 308 | 520 10, | 48 | 8138) gem | 1200 | 261 | 8080 11. | 494 | 27-64 | arg | 1292 | 218 | 8475 12. | 5056 | 2670 |... 14:30 | 1-79 | 85:33 eon | 346 | | The column A gives the temperature of the gas. The column B gives the volume of the saturated vapour at point of liquefaction. The column © gives the fractional volume of the gas at point of liquefaction in relation to the initial volume under one atmospheric pressure. The column D gives the volume of the condensed liquid. — The column E gives the ratio of the volume of the gas to that of the liquid. The column F' gives the pressure in atmospheres. These data alone are incomplete to enable us at once to deduce by calculation the heat of vaporization in terms of the usual units (metre and kilogramme). Here are given only the relative volumes of the saturated vapour and con- densed liquid, so that their specific volumes at different tem- peratures, which are wanted, are unknown. it will, however, be enough for our purpose if we know their densities. Now, Ansdell gave as results of independent measurements the densities of the condensed liquid at different temperatures. An interpolation formula, obtained between those densities of Liquid Hydrochloric Acid. 437 and those temperatures, when combined with the numbers given in the second and fourth columns of the above Table, will enable us to find the corresponding densities of the satu- rated vapour. The results thus found were not very satis- factory. Another way to overcome the difficulty is to make use of the numbers in the third column, which give the volumes of the saturated vapour just at the point of lique- faction in relation to the volume occupied by the mass of the gas at the temperature ¢° (column A*) and under the pressure of one atmosphere. If the specific volume of the gas under the normal circumstances be known in terms of the usual units, this together with the coefficient of expansion under that pressure will give us the specific volumes of the satu- rated vapour at different temperatures. Now, Biot and Arago{ give the density of hydrochloric acid under the normal circumstances to be 1:2474 in reference toair. There- fore, the specific volumes under consideration will be given by the following :— il i fractional Bae 1998 1-247: | volume | ree When a long time ago I began my calculation I was not able to get any information with respect to the coefficient of expansion, and I assumed it perhaps not far from the value 0:008665. Quite recently, however, I have found that it was determined by Regnault f as long ago as 1843 to be 0:003681, and so I have proceeded to recalculate. Of course no great differences were thus wrought in the final values of the heat of vaporiza- tion. It is, moreover, to be remarked that Regnault himself did not put much confidence in the accuracy of his value on account of an unavoidable admixture of air, very small though it was, with the gas he investigated. The formula for the heat of vaporization (according to the notation of Clausius) becomes :-— —__ 10883 1 di fractional a\ dp , TE T393 ‘Toa7 | volume |* (+44) (1-2 au: in which the ratio o/s is to be supplied by the numbers in the second and fourth columns of the above Table. * As it must have been, although it is not explicitly mentioned, t+ Wiillner, Lehrbuch der Physik, iii. p. 150. { Ann. de Chimie et Physique, série 3, tome iv. IN 438 Heat of Vaporization of Liquid Hydrochloric Acid. o was calculated from the following interpolation formula found by the method of least squares :— p=28'451 + 0°4914 t+ 0:012463 #, in the evaluation of whose constants the numbers in the eleventh row in the above Table were omitted, because the representative point in the p- and ¢-curve was much out of the general course. p (calculated) in the following Table are from the above interpolation formula, whose use is amply justified by the numbers in the difference-column. | | } | | | iP P ; o P,P | us || (observed). | (calculated). Tinie =e 5 | j | atm. atm. calor. | 1. 4 29°8 |), a h061 +0°81 61-02 2. 9:25 | 33°9 34:10 +0°20 64-99 | 3. 138 37°75 3760 —O0°15 65°77 4, 18:1 | 41°8 41°45 —0°37 65°45 dD. 22 | 45°79 | 45°29 —046 || 63°51 Geo, Sen We pd 50°57 —043 | 60:02 7. 30-4 58°85 | 58:76 —009 | 5317 | 8. 39°4 | 66°95 67:15 +020 || 45-18 ae) ASS | 152 7547) | «= 4026 I ae tO) as 80°8 80°75 | —005 | 30°08 a4 2 494 84:75 8914 | —161 | 20°49 1954) P5056.) || 85°33 85:22 0a 13. 51 | i | H | | The manner of variation of these numbers for 7, as deduced from the observations of Ansdell, is very remarkable. From 4° to about 14° the heat of vaporization increases, attains there a maximum value, then decreases in a regular manner, but from about 45° onwards it diminishes quite rapidly, as if the gas were preparing for the critical point (51°25), at which the heat of vaporization is to vanish. Among those substances whose heat of vaporization was investigated by MM. Cailletet and Mathias * we have no in- stance like hydrochloric acid. It is much to be desired that any one who has proper instruments in his possession will take the trouble to decide whether the anomaly is real or whether there were some mistakes in our data. * Journ. de Physique, tom. v. 2° série, 1886. Also, zbid. tom. ix, 2e série, 1890. [ 439 7 XLII. Note on the Flow of Water in a Straight Pipe. By M. P. Rupsx1, Priv. Doe. in the University of Odessa *. T is a known fact that the law of resistance to the motion of a liquid in pipes and channels of great size differs much from that in capillary tubes. It is also known that this differ- ence is due to the presence of eddies in great pipes, while in capillary tubes the liquid flows in straight lines. Prof. Osborne Reynolds + has shown that there exists a certain critical mean velocity, depending on the diameter of the pipe and on the temperature (7. e. viscosity) at which the eddies must appear. He thinks that the appearance of eddies is due to the instability of rectilineal motion. But Lord Kelvin ¢ has shown that at least for small disturbances the rectilineal motion is stable provided the coefficient of viscosity is not zero. Although Lord Rayleigh § thinks that Lord Kelvin’s proof is not quite convincing, it seems to me to be so, because the steady rectilineal motion with zero velocity at the walls satisfies the condition that the loss of energy shall be the least possible. This motion belongs to the type which was shown by Helmholtz to have this property ||. Now itis known that generally the motions, which in a certain manner satisfy the minimum or maximum condition, are stable. The same question was also treated by Mr. Basset 4]. He has found the rectilineal motion unstable. As far as I can understand him, from a short communication, it was only after he had introduced in the expression of resistance a term depending on the square of relative velocity. In doing so he has anticipated the law of resistance proper to the eddying motion. On the other hand, he finds that without this term the steady rectilineal motion remains always stable. His results also agree closely with the results of Lord Kelvin. It seems to me that all this clearly agrees in showing that it is not the question of stability or instability which arises here, but another one. In speaking of stability we mean ¢o ipso the tacit assumption that the eddying motion may be also expressed with the help of functions satisfying the common partial differential equations of viscous fluid * Communicated by the Author. + Phil. Trans. 1885, p. 935. { Phil. Mag. 5 ser. xxiv. pp. 188 and 272. § Phil. Mag. 5 ser. xxxiv. p. 67, || Basset, Hydrodynamics, vol. ii. p. 356. 4] Proceedings Roy. Soe. vol. lii, no, 317, p. 273. 440) On the Flow of Water in a Straight Pipe. motion. Our equations of disturbed motion serving to inves- tigate the question of stability are the same hydrodynamical equations with certain terms neglected. These equations, as Lord Kelvin has proved, show that the undisturbed motion is stable. But if we introduce something that is not contained in the hydrodynamical equations, as Mr. Basset has done, we find the sought instability. In other words, our hydrodynamical equations, which we know to be strictly true only for small relative velocities, are now shown to be, in the case of water, of very limited im- portance. They are not able to express the eddying motion. In the motion which they are able to express, any surface drawn within the liquid is supposed to be strained in a con- tinuous manner. In the eddying motion these surfaces are continually breaking and again reforming, an opinion which seems not to be new to hydraulicians *. The opinion that it is with a real breaking that we have to do is strongly supported by a striking fact observed by Prof. Reynolds. The eddies appear only at a certain distance from the entrance of the pipe. This distance is diminishing when the velocity increases, but diminishes asymptotically. Now it is a known fact that the breaking of bodies, solid, plastic, or plastico-viscous, depends not only on the amount of the strain, but also on the velocity of straining. Even hard bodies sustain a great strain when the straining is slow enough ; on the other hand, fleazble bodies, when very rapidly strained, Sreak down. On the other hand, when the liquid enters the pipe tumul- tuously, but with small mean velocity, the viscosity begins to act at advantage, the breaking ceases, and the eddies die out. Reynolds has shown that this reversal trom tumultuous to quiet motion occurs at a critical mean velocity, which ceteris paribus is about 6-3 times smaller than the other mean velocity which renders the quie* motion impossible. All other features of the phenomenon—the dependence of critical mean velocity, z.e. of the critical rate of straining, on the viscosity and on the size of the tube—are clearly in best accord with the hypothesis of breaking for a certain critical rate of straining. The existence of two critical velocities—a greater which makes the quiet motion impossible, and a smaller which makes the tumultuous motion impossible—is very interesting, and shows similitude to many other physical phenomena. * See Boussinesq, ‘* Kssai sur la théorie des eaux courantes,” Mém, Sav, Etr. vol. xxiii. p. 5. er 44 @ 7 XLIL. Liquid Friction. By Joun Pury, F.R.S., assisted by J. GRAHAM, B.A., and C. W. Huatu*. : [Plate VIL] PIECE of apparatus such as is used in this investi- gation was designed and partly constructed in Japan in 1876 ; it is described in my book on Practical Mechanics (1883). The specimen actually used by us was constructed at the Finsbury Technical College in 1882, and has been occasionally used since that time, but no complete sets of observations were attempted till October 1891. The simplest hydrodynamical condition of viscous fluid is that of the fluid bounded by two infinite parallel planes, the fluid in one boundary being at rest, the velocity in the other boundary being constant and in the plane. Motions in a pipe and near a vibrating disk, or even near a steadily rotating disk, are rather complicated. Our apparatus was designed to approach as nearly as possible to the conditions subsisting between the infinite planes. Between two such planes, if V is the constant velocity of one of them, the other being at rest, and 0 is their distance asunder, the fluid being of uniform density, and gravity being neglected, if 2 is measured at right angles from the fixed plane, the equation of steady motion is d? Vv . dz’ = 0, SyMeEE Tt 1 eis Mine key sn (1) a DF NGS By Fem ae ome iaas a (-) and the tractive force per unit area required at the moving plane to maintain the motion is «V/b, where mw is the co- efficient of viscosity. We have used, instead of planes, concentric cylindric surfaces of as large radii and as small difference in radii as could be conveniently constructed and used (see Pl. VII. fig. 2). EEE is a cylindric trough, of which the curved parts K and E are brass. The inner and outer radii of this trough are 10°39 and 12°65 centimetres. C, which forms the bottom, is of iron; and the whole trough can be rotated about its vertical axis at any desired speed by driving the pulley P from a coned pulley D with numerous steps. G is a hollow brass cylinder supported by a steel wire L, of 0:037 centim. diameter, 67°78 centim. long, whose axis coincides with the axis of the trough and the axis of * Communicated by the Physical Society: read March 24, 1893, 449 Prof. J. Perry on Liquid Friction. - rotation. G may be raised or lowered relatively to the trough. The outer radius of G is 11°63 centim., the inner being 11°41 centim. The whole apparatus is supported on a stand, with three adjustable feet. We exhibit also some photographs of the apparatus in position, showing how it was driven. — The trough contains the liquid whose viscosity is to be measured : when it rotates, G tends to rotate ; and when for any constant speed G is in equilibrium, the twist in the steel wire measures the torque due to the tractive forces with which the liquid acts upon G at its inner and outer surfaces. The twist was measured by the angular motion of a pointer clamped on the wire at a distance of 59 centim. from the fixed end. To test the accuracy of our assumption that the fluid behaved as if between parallel plane surfaces, let us consider the actual motion in which the stream-lines are circles. Consider the motion of a stream-tube of section 6r 6z, «2 being measured axially and 7 radially. The tangential ? e s e e . du Uv e force on unit cylindric surface of radius 7 is (Ss Re if v is the velocity. The moment due to all such forces on the inner surface of our ring is The moment tending to increase the velocity of the ring due to forces on the cylindric parts of it is therefore Cte AGG ET + a= — 3) 8r Bars also, due to the plane faces we have the moment d?v Qerpr®—. Sy. Bx. ie or. 6a Equating the sum of these to the rate of increase of the moment of momentum of the ring, we have i AGGv hi Oe, CO apade dtd Pp tde ad 7 7 as the equation of motion in co-axial circular stream-lines. Now the discontinuity at the edge, and also the nearness of 2 the bottom of the trough, cause the term ad to be important; dx but the solution seems to be very difficult. Maxwell satisfied himself (Collected Papers, vol. ii. pp. 16-18) that the dis- — continuity at the edge of a vibrating disk could be allowed Prof. J. Perry on Liquid Friction. 443 for as a virtual increase in the radius of his disk, and the assumption that the behaviour of his fluid was the same as if his disk were part of an infinite disk. The correction not being readily obtained for a disk, he assumed it to be the same as for the straight edge of an infinite plane surface. We are certainly not less correct in taking the same correction for the edge of our cylinder*. Following Maxwell, there- fore, we assumed that when our cylinder G was immersed to the depth AB or J in the fluid it was really a portion of length /-++X of an infinite cylinder of the same diameter. We 2 therefore neglect a in (3), and we use Ge bedtn. 30 2. p CIE ET Gi Pe ST oe VN ete (4) When the motion is steady, that is when dv/di=0, the solution is . Ey Pa aM wet! LAS A) If v=v, when r= R,, and v=0 when R=R,, then v= Ry (7 — R,?/r) /( RY — R,’) ° We must now distinguish between the space outside the suspended cylinder and the space inside it. The radii of the inner and outer surfaces of the suspended cylinder are 11°41 and 11°63 centim., and the inner and outer radii of the trough are 10°39 and 12°65 centim. Our cylindric surfaces were not perfectly true, although great care was taken to make them so ; and the radii given are only average dimensions. But, inasmuch as slightly tilting the apparatus or otherwise putting the axis of the suspended cylinder out of coincidence with the axis of the trough made only small differences in the observations, we did not think that such inaccuracies of workmanship or mea- surement as existed could affect our results. Even when the tilting of the apparatus was quite evident to the eye, the tractive torque was found to be only slightly increased by the tilting. Of course, as the suspended cylinder * It is to be remarked that Maxwell assumed, generally, that there was no radial motion of his fluid. Now there must have been radial motion, his disks resembling centrifugal fans in their action, creating a variable flow always outwards between his fixed and moving disks; and the energy wasted in producing this flow is neglected by him. We do not know the amount of this error, and he may have satisfied himself as to its insignificance. Prof. Maurice FitzGerald in criticizing this proof has pointed out the fact that on James Thomson’s theory of river bends there must exist a radial motion of an interesting kind in our apparatus. 444 Prof. J. Perry on Liquid Friction. got closer and closer to the side of the trough the torque did increase, and became very large when the suspended cylinder nearly touched the side of the trough. Again, it was observed that at our highest speeds the amount of wetted surface did not perceptibly alter ; and we are, we think, justified in assuming that the surface of the liquid was always a plane surface. It is evident that the tractive forces on the suspended cylinder are the same whether we assume the trough to revolve steadily at m radians per second, the suspended cylinder being at rest, or the suspended cylinder to revolve steadily at w radians per second and the trough to remain at rest. We shall therefore, for ease of calculation, always assume the trough to be at rest and the suspended cylinder to be revolving at w radians per second. Then the velocities of its inner and outer surfaces are, in centimetres per second, 11:41 and 11°63. On any cylindric surface the tractive force per unit area : B being p(—) is == @ from (5); so that, whether for the outer or inner space, if R, is the radius of the suspended moving cylindric surface, and R, the radius of the fixed surface, the tractive moment per centim. of length is + Arrow Ry /(R?/R?—1). Taking actual sizes, this is 0°5 per cent. greater than the value obtained by calculating the forces on the assumption that the fluid moves in plane layers as in (2), 6 being the actual thickness of fluid 1:02 centim., and V being the actual velocity at the mean radius. We may, in fact, imagine the speeds to be increased by 0°5 per cent., and make all caleu- lations as to viscosity on the assumption of motion in plane layers. The tractive torque per centimetre of length of cylinder is, in our case, 19010yo, or 1991 ny if the angular velocity is given as x turns per minute. If / is the wetted length in centimetres, and A is the virtual additional length repre- senting the edge effect, the total torque is 1991 nu(l +2). The total observed motion of the pointer being D degrees, and the torque per degree being a, the torque due to tractive forces acting on the cylinder is aD = 1991 nu(l+A) ; and if this law is found to be true experimentally, then p =aD/{1991(1+a)n}. . 2 . . ©) Prof. J. Perry on Liguid Friction. 445 Two methods of determining the torsional constant of the wire were employed :— First Method.—A fine cotton thread was wound round the outside of the suspended cylinder and passed over a nearly frictionless pulley (the pulley of an Attwood’s machine) to a scale-pan. The thread was nearly horizontal as it left the cylinder. In this way it was found that the twisting moment required to produce a pointer-rotation of one degree was 1531 dyne-centimetres. In making the measurement as the weight of the scale-pan and its contents was gradually increased, the steel wire was drawn away from the vertical, and therefore from the middle of the scale; but the stand was tilted to counteract this effect. | The effects due to solid friction were eliminated by taking the mean of the limiting weights for equilibrium. When the weight was 30 grams, one tenth of a gram either added to or taken from the scale-pan produced a perceptible change in the position of the pointer ; so that the solid friction was small. Second Method.—The suspended cylinder was allowed to vibrate, twisting and untwisting the wire ; and its times of oscillation were noted. ‘The observations were repeated when a known moment of inertia had been added. Unloaded, it made 40 complete oscillations in 583 seconds, or one oscillation in 14:575 seconds. We then attached to the cylinder an iron bar of rectangular section, whose own moment of inertia had been determined accurately by previous experiments (found to agree with calculation on the assumption that it was homo- geneous), this moment of inertia being 566°2 (in gram- centimetre? units). The time of a complete oscillation was now found to be 21:425 seconds. It follows that the moment of inertia of the suspended cylinder is 487°72, and the tor- sional constant of the wire is readily obtained. ‘This constant being corrected on account of the position of the pointer, it follows that to produce a rotation of the pointer of one degree requires a torque of 1552 dyne-centimetres. This is greater than the constant derived from direct measurement by 13 per cent. ; but, on the whole, we are rather inclined to accept the number obtained directly, as we are not quite sure that the mean position of the iron bar was at right angles to the mag- netic meridian. Hight quite independent measurements of the diameter of the wire were made by men experienced in making such measurements ; and the mean value was ‘0371 inch, the greatest and least being "0373 and ‘0369. Using this mean value, and the directly measured torsional constant, it would seem that the modulus of rigidity of the steel is 7°71 x 10”. Phil. Mag. 8. 5. Vol. 35. No. 216. May 18938. 2H 446 Prof. J. Perry on Liquid Friction. As an error of ‘0004 inch in the diameter measurement leads to an error of 4 per cent. in the modulus of rigidity, and as the modulus of rigidity usually taken for steel is 8°19 x10", we believe that our constant 1531, as directly measured, is sufficiently correct for practical purposes. In using (6), then, we take a to be 1581. The virtual addition \ ought, by Maxwell’s formula, to be 0:52 centim. in our case. But the bottom of the trough H was only 0°5 centim. from the edge B of the suspended cylinder in most of our experiments, and we do not know how to calculate for this. Our experiments have shown that when this distance is 0°5 centim. the twisting moment at a given speed is practically the same as when the distance is much greater ; but we did not know this from any theory, and, besides, it is always rather dangerous to depend upon a theoretical calculation of X such as Maxwell was compelled to use. It is possible, also, that a correction of the same kind ought to be introduced for capillary and other actions at the surface of the liquid. The action of the atmosphere was in any case negligible, because when there was no liquid present in the trough, so that there was an action of the air several times greater than ever occurred during the experiments, the deflexion was quite imperceptible at much higher speeds than those used in the experiments. The temperature being kept as nearly as possible constant, but probably varying between 18°°9 C. and 20° 1 C. (stated as 19°°5 C.), the following experiments were made with sperm-oil, beginning with a small quantity in the trough and . ending with a large quantity. The bottom of the trough was in every case 0°5 centim. below the edge of the suspended cylinder. TasLe I.—June 9th, 1892. | Defiexion D when MN, | ) ] | | ¢=0°O em. | /=2°5 em. | 7=5 em. l=7-d5 em. | /=9-9 em. | 50 24 67 112), 1, tee 49 re hy cs = 196 | 48 | | 40 oo eae 3. ee 163 39 fn, fea ee 23 io: | | | 175 8 k 57 ees ae RRs. 2 24 39 Ae NE gi ial b> ld 40 115 | 11 | | a a es Prof. J. Perry on Liquid Friction. 447 As the deflexion is sufficiently nearly proportional to the speed to allow of corrections by this rule when the cor- rections are small, we have corrected the above observations to ene speeds 50, 40, 174, 114; and we obtain the following results :-— | Values of 2. Values of /. cs | 50. 40, Mie 114 | 5 24 18 Sms 5 | 25 67 54. | 25 16 5:0 1h 93 40 | 27 | TD 165 132 7 Cie | | 99 | 200 163 735 | 51 | D and / were then plotted as the coordinates of points on squared paper ; and it was obvious that for each value of n these points lay very nearly in a straight line, and all the straight lines passed through the point/=—0°8. Itis curious that the lmear law should hold for such small values of / as 0-5 centim., and for high speeds as well as low speeds. We shall presently see that some of these speeds are considerably above the critical speed at which (4) ceases to represent the motion. We may take it, then, that »=0°8 centim., which is greater than the calculated value 0°52. The discrepance cannot be due to the distance BH being small, for we have altered this distance and found no perceptibly different results. As already stated, it may be due to some capillary surface action. Taking a=1531 and X=0°8, we have (6) becoming e—0T6Dne@tOSe . . . . @) Of course our results are consistent with our equations of motion only so long as D/(¢+0°8) is proportional to n. Many observations have been made with this apparatus during the last year on various liquids, under very different conditions of temperature and speed and depth. We give here a set made on sperm-oil. In all cases the bottom of the trough was 0°5 centim. below the edge of the suspended cylinder. Keeping the oil at a constant temperature we ran the trough at a number of speeds, and repeated at other constant tempe- ratures. The results are given in Tables LV. to XI. When a temperature had to be taken the rotation was stopped and a thermometer dipped about halfway down in the oil, the reading being taken at the end of about half a minute, 2H 2 448 Prof. J. Perry on Ligud Friction. A small Bunsen flame was applied underneath the trough when a temperature higher than the room had to be main- tained for a considerable length of time. As the temperature varied slightly, and we wished to reduce our observations to constant temperatures, we afterwards made two sets of observations at very varying temperatures but constant speeds. These later observations we shall consider | first. They are given in Tables II. and III. TABLE IJ.—March 29th, 1892. (d=8°275 centim.) pote {a D) a a OF 1): EN | L. LE peed = — = = a Pesoa iss f 189 10> 21-09 | ‘400 | +446 | 395 | 171 | 165 |- 1760 | 834 9) eee 40 195 || 150 | 1653. |- 31877) Gees 40 24-0 | 184 .| 1477 | -Os7) | aan 40 253 | 1965 | 1394 | -268 254 | 40 89 | 1115 | 12:28 236 PS ial 40 32:0 109 11:46 40 42-5 | 88 9-70 i 40 469 81 8-65 40 585 | 67 TU | 40 64.0 | 58 6-39 aor emo | 56 bisa fl | | | ee Ue a cg | | 40 85:5 | 5:12 | | The numbers in the column headed av are obviously ; De n l+nr intended to be corrections of D/(/+ 2) for the constant speed of 40 revolutions per minute. TABLE II1.—March 380th, 1892. (/=7:78 centim.) 7 ] : 9a) | SO ae er | ‘Dea oe Fee HB calculated. aes —_———_|—- — SS —- —___|_ —= | 8°75 52) 1160 ©) 19-19 | Sige 2-06 975 | 80 85 9°15 0-78 0:82 92 | 100 57 6:56 0-73 | 062 9-0 108 47 548 | 047 | 9056 9:0 16°6 36:5 | 4:96 | 0363 | — 0-366 9-2 248 26°5 | 3:02 | 0-258 0259 9-0 35-0 19:5 | 2:27 =| 0-194 0196 9-0 47-0 140 1:63 0-139 0:137 9-0 565 10-2 119 | 0-101 0-104. 9-0 67:0 8-0 0-93 0-079 0-081 9-0 89:0 5-4 063 0-060 0-058 9-0 84:5 6-0 070 | 0054 0-054 a Prof. J. Perry on Liquid Friction. 449 The numbers headed : S are intended to be corrections of D/(J+2) for the constant speed of 9 revolutions per minute. We have plotted the numbers in the last columns of these tables with @ upon a sheet of squared paper; but it is unnecessary to publish the resulting curves. We exhibit them to the members of the Society. Knowing what has been done by Prof. Osborne Reynolds, it seemed unlikely that one simple formula should satisfy either of these curves ; that is, it was likely that in the lower curve there was some temperature for which the speed n=9 was a critical speed, and there was also a temperature for which n=40 was a critical speed. We therefore used the curves merely for small temperature-corrections in our other experiments, in which we kept the temperature nearly constant. It was therefore without much interest that, in preparing this paper for publication, we tried to obtain empirical formulee for these curves ; and at first we used, not the observations themselves, but the observations as corrected by curves drawn upon squared paper. When log (@—4:2) and log Try are plotted as coordinates of points on squared paper, we were astonished to find that when n=9 the points lie in two straight lines. The allinea- tion of the points is very striking, even when the uncorrected observations are taken, and leads to the following empirical formula :— Letting @ denote @—4:2, and letting y denote D/(/+)) the torque as measured in dégrees deflexion of pointer per unit length of wetted cylinder ; then, at the constant speed orn 9, yo =constant for temperatures above 40° C. yp =constant for temperatures below 40° C. On plotting logy and log @¢ for the constant speed n=40, the points are not found to lie so nicely in straight lines, but there does seem to be some sort of discontinuity at a tem- perature of about 45° C. At first we thought that these temperatures were the tem- peratures at which the speeds n=9 and n=40 were the critical speeds, and we were greatly concerned because our result seemed to be quite out of accord with the reasoning of 450 Prof. J. Perry on Liquid Friction. Prof. Osborne Reynolds*. As his ingenious theory has been completely verified by experiments made upon the very smallest and largest pipes with flowing water, and as it is simple we had adopted it for the reduction of our experiments. According to his theory, Tk or, as we shall call it, y, ought to be proportional to 7 until n exceeds a certain value; this value being a function of u/p, where p is the density of the fluid. Now the alteration of p with temperature in such a liquid as sperm-oil is so small that the error in neglecting it is small in comparison with our errors of experiment. Neglecting, then, the alterations in p, the theory of Prof. Reynolds leads to y = al?-*n*, . en where F is a function of the temperature, n the number of revolutions per inute ; where «=1 until the critical speed m, 1s reached, n. being proportional to I’, and « having a higher value than 1 for all speeds above the critical; @ is a constant. This is on the assumption that Prof. Reynolds’s theory would lead to the sume result in our case as in his pipes. Now, in the first place,it seemed absurd that the temperatures for which the speeds 9 and 40 were the critica] speeds should be so near to one another as 40° C. and 45° C. But a much more serious consideration was this. According to. any rea- sonable application of the theory to our case, at constant speed, if yp” is constant when the speed is less than the critical speed, and if yd* is constant when the speed is above the critical speed, then s ought to be less than m, whereas 1°349 is about twice 0°686. We came to the con- clusion that the point of discontinuity has nothing whatever to do with the critical speed ; indeed, we subsequently found it probable that n=9 does not become the critical speed until the highest temperature of Table III. is reached. Using the deflexions in Table ITI. to determine « according to (7), we have the results given in column 5 of the Tables. The numbers in column 5 of Table I. are calculated for tem- peratures lower than 26° C., which is about the temperature at which 40 is the critical speed. In some of the following tables, giving the results of experiments made at various constant temperatures, we have also given values of w. There * “ An Experimental Investigation of the Circumstances which deter- mine whether the Motion of Water shall be Direct or Sinuous, and of the Law of Resistance in Parallel Channels,’ by Osborne Reynolds, F.R.S., Phil. Trans. pt. iii, (1883), | Prof. J. Perry on Liquid Friction. 451 is as much consistency in all these results as might have been expected. We lay most weight upon the results given in Table ITI., which lead to the laws ro 2:06(0—4-2)\e 8 below 40° Cy. 22. |. (9) p= 21-60(G—4-2)-!* above 40° ©. .... . (10) We have searched in books in vain for a mention of a dis- continuity in any other physical property of sperm-oil about this temperature ; but we have already begun to experiment on its other physical properties, as it is unlikely that there should be a discontinuity in the law for the viscosity alone. At the same time, we may say that our chemical friends see no reason for a confirmation of our belief. In the tables we give the viscosity as calculated from these formule ; and it will be seen that they agree well enough with the observed viscosities. TasBLe [V.—March 18th, 1892. (l=6°15 centim. Temperature Constant, 17°°5 C.) , or 1 _ DU-LA). M 36 114 16-41 351 39 121 17-41 344 54 172 24-75 352 69 245 35:26 80 300 43°16 92 B45 49-64 28 74 10°65 356 16 52 7-48 360 | 13 A ee 500 349 8°75 o7 3:98 349 { The column headed pw is 0°769D/n(l+ A), and has no meaning at a speed greater than the critical speed. The critical speed, 7, is probably about 50. The first three and last four values are probably measurements of w. The average value of these seven is w=0°351. Formula (9) would make pf to be 0°349. Plotting logy and logn as the coordinates of points on squared paper, the points lie very nearly in a straight line indicating yan until the critical speed, about n=50, is reached, and for all higher speeds the points lie nearly in another straight line indicating y an’, 452 Prof. J. Perry on Liquid Friction. Taste V.—March 21st, 1892. (=6°075 centim.) 0° C, Nn. 1D; Y- pi. 22:5 9:25 24°5 3°40 ‘283 232 11 28°0 397 ‘278 22°7 14:2 37 5:16 ‘280 22:0 17-2 45 6°15 ‘279 25:0 27 68 10:19 ‘277 24-5 23 57 8-41 281 24-0 32 “Eh 11-20 ‘269 23:0 90 340 48:00 22°5 102 410 - 56°96 23:0 80 276 38°94 24-0 72 224 32°58 24:5 56 169 24-95 24-0 48 129 18°76 23°5 43 _ 108 15 42 ‘278 230 38 eo 13-69 ‘217 The column headed y is D/(/ +) corrected to the constant temperature of 24° C. by a correction of about 3 per cent. per degree. The numbers in the last column have no meaning for speeds higher than n=about 48. The average value of p, the viscosity, in the first seven and last two observations is 0-278. Formula (9) would make w for this temperature 0-266. Plotting logn and logy on squared paper gives points lying nearly in two straight lines, showing that y an to the critical speed n=about 43, and above that speed y an'*", TaBLeE VI.—March 21st, 1892. (J=6:075 centim.) — | | | G2. | n 1D), | y SS ae a a Eee 29°5 | 38 81 | 11-63 30 | 43 95 13°82 31 48 114 16:99 30°5 56 134 19-73 30°5 60 147 | 2165 | y here means D/(/+ 2) corrected to the constant temperature of 30° C. by a correction of 24 per cent. per degree. yp as calculated from (7) would have no meaning, as the critical speed for this temperature is about 28 revolutions per minute, and we give no column headed w. y¥ is very nearly an, Prot. J. Perry on Liquid Friction. 453 TaBLE VIT.—March 22nd, 1892. (/=5°4.25 centim.) | g°C n Dp: y HL 56 38 49-5 792 59 42 59 9:20 55 54 125 11°31 56 58 88 14:13 56°5 14 116 18°79 575 108 158 26°32 58°5 29 34 578 56 24 25 4-01 "1282 57 17°95 ll 1-81 ‘0791 57 155 14 2°31 "1148 54 155 12 1-82 ‘0903 55 16 14 2°19 1054 y means D/(/+X) corrected to 56°C. by a correction of 24 per cent. per degree. The critical speed is probably below n= 24, and for speeds greater than the critical y «n!* nearly. For speeds less than this the average value of pu is 0°103. According to (9) the value of mw for 56° C. is 0°1055. Plotting logy and logn as the coordinates of points on squared paper gives points which may be said to lie on two straight lines, but the errors of observation are too great. For n>24 we might perhaps say that y «n!?5; but it seems hardly fair to draw conclusions from this set of observations. TasnE VIIL.—March 24th, 1892. (/=7:025 centim.) in 0° OC. nN. D. | y. | bh. | 30 100 363 45 24. | 30°8 78 250 31°79 31 115 404 51-64 31 32 62 7:92 ‘1903 | = 3l 22 47 6:01 ‘2103 | 3} yy 37 Ae 14 | 39 13 29 3:80 49 | 31 ll Dae) 3°00 “2097 | 30 9:2 20 2°50 209 -yis D/(l+X) corrected to 31° C. by a correction of 24 per cent. per degree. The numbers of the last column have no meaning for speeds higher than n about=32. The average value of w is 0°210. According to (9) the value of w for en CO. is 0°216. Below n=382, y an, Above n=382, we may perhaps say that y an, : . Prof. J. Perry on Liquid Friction. TaBLE [X.—March 28th, 1892. (=6°525 centim.) 0° C: n, D. | Yy- 81 38:5 3 | 518 80°5 56 63 | 8-557 80 69 88 | 11-80 79-5 84 112 | 14-70 Bus 104 134 18-29 83 92 116 16-157 | y means D/(l+2) corrected to 81°C. The law seems to be 7 «n!? nearly. TABLE X.—March 23rd, 1892. (/=7:025 centim.) 0°C. n Pp; Y: 82 17°5 16 2°06 82 14 11 1:23 | 82 26 26 3°35 | 81 32 33 4-22 80 11°5 8:5 1:08 | 82 10 Gia 0°84 If it is assumed that n= 10 is not much above the critical speed, w may be calculated as 0°0646. According to (9) p=0°062 for 81°C. y an* may be taken as the law. Taste XI.—March 24th, 1892. (/=6-7 centim.) D y. HB. 65 4 8 1:07 091 66 10:8 9 1:21 | -086 65:5 17 16 914. | 2asza 64:5 21 21 279 | 65 23°5 26 3:46 | ee on65 29 32 426 | | 65 114 210 28:00. | | 66 102 162 21-82 | 645 88 156 20:10 | 65 66 112 14-93 [24 66 52 74 9-96 66 44-5 59 7-94 66 38 46 6:19 | y is D/(1+2) corrected to 65°C, jw has no meaning except for the first three speeds, and the mean of these three is 0-091. According to (9) the value of w for 65° C. is 0-085. j Prof, J. Perry on Ligud Friction. 455 Above the critical speed, which is possibly below n=17, the law is probably y an’. lt is not worth while to publish any of the observations which we have made upon other liquids, nor to publish the curves we have drawn for sperm-oil, although we exhibit them before the Society. Hrrors of one degree in obser- ving temperature were quite possible, and errors of half a degree in the deflexion of our pointer were also possible. Small fluctuations in speed were continually taking place, so that the pointer was never quite still, the motion of the fluid was therefore not truly steady. It is our determination to repeat the whole work with improved apparatus. In the meantime, however, it will be observed from Table III. that there is fair agreement in the law connecting w with tem- perature, from all the sets of observations. There is, on the whole, a very fair agreement with what we venture to call Prof. Reynolds’s rule, ie =a en, where « has the value 1°33 or 1 according as n is above or below the critical speed*. The sheet of squared paper on which we have plotted all our values of log y and log n for the various constant temperatures shows that the errors of observation are too great for the establishment of this value of «; but it is the probable value. It shows, however, in the allineation of the points of discontinuity, with sufficient accuracy that y, co n,”, if the rule is taken to be generally true; and although there is some little vagueness always in one’s observations just about the critical speed, we may take y-=0°009 n,? without very ereat error. Indeed, we are satisfied with the substantial agreement of all our observations with the formula hee be 2—k P y=( ae95) ny * Prof. Reynolds, in criticizing a proof of this paper, has been kind enough to point out that his rule for pipes does not necessarily apply to the fluid in our apparatus. We had not seen the reprint of his Royal Institution lecture, else we should have known that the condition of the liquid in circular flow is inherently stable or unstable according as » is greater or less than the radius of the fixed cylindric surface. As he points out, the liquid in the outer space is inherently stable for velocities far exceeding the critical velocity (if there is one) for plane surfaces, whereas the liquid in the inner space is unstable from the first. We directed the attention of the meeting to the fact that Tables IV., V., VI., and VIII. give unmistakable evidence of the truth of what we have called Prof. Reynolds’s Rule, however difficult we may find it in explanation. 456 Prof. J. Perry on Liquid Friction. where a='009 and «=1'33, That is, for low speeds we have the law SIE ad PS At the critical speed the law suddenly changes to Ss a( eg s) > which holds for all higher speeds which we have tried, The critical speed = 1444, 1 ea oa OO a. and =O, OF WI WE. It is to be recollected that p is too nearly constant for us to say with certainty that a is proportional to p, as the theory requires. The errors of observation were so great that it was not worth while finding accurately the most probable values of « and a. We wish it to be understood that our apparatus was very carefully constructed, and great care was taken in making the observations ; but it is our intention to pursue the investiga- tion with apparatus much more carefully constructed. Vibratory Hxperiments. In designing the apparatus it was our intention to obtain wu from the damping of the rotational oscillations of the suspended cylinder about its vertical axis, the trough being at rest. We meant in this way to obtain w for velocities very much smaller than those which could be employed in our steady motion ex- periments. A considerable number of observations were made, but when we tried to make calculations of ~ we found that our mathematical difficulties were too great, and after many months of effort we are forced to say that we are unable to utilize these observations. In equation (4) assume that v=we'*, and w may be obtained in Bessel functions. Unfortunately, as there are two surface conditions, doth particular solutions of the Bessel equation are necessary, and the work of reduction be- comes very great. An approximate solution is obtained by taking r= R-+ 4a, R being the radius of the suspended cylinder, and taking the equation (4) to be Oy yk aie 6? de Rida RO ame Making this assumption in the case of steady motion, it was | found that it was sufficiently correct for practical purposes. (11) i 4 : 4 Prof. J. Perry on Liquid Friction. A457 The following numbers show the sort of error introduced, taking R=10, and 1 the greatest value of w. = Values of v. festa OD = =a Values of x. | On the assump- | Correct. | Approximate. | tion of motion | 'in plane layers. De ee ee es 0 \ l | 2 7914 7914 8 5 4875 4872 5 7 2895 2892 3 1-0 0 | 0 0 ) The solution of (11) for vibratory motion is easy enough ; but we found it still difficult to calculate w from our observa- tions. Hven when we assume that the motion is in plane layers, so that the solution used by Maxwell is employed, we find that our - is too great for a logarithmic decrement to exist with such amplitudes and times of oscillation as we had employed in the experiments, and it was impossible for us to repeat the experiments under the same conditions again at slower velocities, because the apparatus had been taken to pieces and could not be fitted up again in exactly the same way. When we say that a logarithmic decrement did not exist, we mean that it was not constant, but varied with the amount of the oscillation. or the tractive force to be pro- portional to the velocity of the cylinder it is necessary for 4/p and the periodic time to be so great that the velocities of the fluid at all places shall be in the same proportion as if the motion were steady. . After this paper was written we asked Mr, J. B. Knight, of the Chemical Department of the Finsbury 'lechnical College, to make measurements of the specific gravity of sperm-oil at different temperatures. His results give a very striking con- firmation of the views expressed in the paper as to a discon- tinuity of some kind due to rise of temperature. As all the authorities whom we have consulted seemed to see no possible reason for a discontinuity in the rate of change of « with temperature in sperm-oil at about 40°C., it is possible that these results may be of importance. ae 458 Miss Earp on the Effect of the Replacement oj Temperature Cent. | Specific Gravity. 25 | 831 30 | 8306 35 828 40) | 826 45 8758 50 8753 5d | “OT ET We are now arranging a piece of apparatus which will give, not the absolute value of the specific gravity, but with great accuracy relative rates of the change of specific gravity with temperature *. We shall make experiments of the same kind upon other animal oils. XLIV. Note on the Effect of the Replacement of Oxygen by Sulphur on the Boiling- and Melting-points of Compounds. By Miss A. G. Harpf. N various papers published in the Philosophical Magazine t Carnelley has called attention to the effect produced on the boiling-point and melting-point of compounds by replacing one element in the compound by another belonging to the same group. He gives numerous examples (mostly organic compounds) to show that in the case of the halogen com- pounds, when one halogen is replaced by another of a higher atomic weight, both the boiling- and melting-point are corre- spondingly raised. As a further instance of the same kind of thing he gives the following series of the ethyl carbonates and sulpho-carbonates to show that the boiling-point is raised in proportion to the amount of sulphur introduced in the place of oxygen. He also points out that the same series shows that a definite effect is produced by a change in the arrangement of the molecule without any change in the number of sulphur atoms. ‘ Doe 5) : a VO See OG E, BP. Zon. Cen H. B.P. 196°. co B.P. 156° cages : } Gs fe) + 0—C i; SC,H. Ge ae: s1° OX ee 24 \o--0,H, B:Psi6h; \sc,H, B.P. 240°. * We described at the Meeting results obtained for other specimens of sperm-oil, with the new apparatus, which exhibited no discontinuity. Yet we can find no reason to doubt Mr. Knight’s measurements. + Communicated by M. M. Pattison Muir. t Phil. Mag. Oct. 1879. j Oxygen by Sulphur on Boiling-points of Compounds. 459 He does not, however, mention the way in which this eftect is reversed in the cases in which the oxygen of the hydrowyl group is replaced by sulphur, and I therefore conclude that it escaped his notice. By examining the large number of boiling-point data given by him in his tables I have found the following rule to be perfectly general :— The replacement of oxygen by sulphur in a compound always raises the boiling-point except in those cases in which the oxygen of the hydroxyl group is replaced by sulphur, and then the re- verse effect is very marked. | In obtaining data in proof of this I have been confined of course mainly to organic compounds, and of these I have only given the simpler instances, and such of the more com- plicated compounds as have a known structural formula. The reason for this is obvious, since Kopp has shown that the boiling-point of isomeric hydrocarbons is not the same, show- ing that a mere rearrangement of the atoms in a molecule is sufficient to affect the boiling-point without any change in number or kind. The fact is further exemplified in the series of ethyl-carbonates given above. In the following list of compounds containing hydroxyl and their sulphur analogues, it will be seen that the replace- ment of the OH by the SH group always lowers the boiling- point, and that in the case of bodies of low molecular weight the difference is considerable, but decreases as we ascend a homologous series*. Diff. RP oid etocrssussacce- SOIKSE\ Ee Once merase. 100 | 161°8 TEL SU ee oe ORIEL CHOBE. oicdinc ick kha 67 46 Ls SBP | Os OSL, Gees nr oye. 784 | 42 CEL) ere LAG SE (CHLOE WR occ os 197 51 BEUOHOH SH .....0.0.:.. 90 | CH,CHCH,OH............... 96 6 SEMOE-CH SH «.......5.. (igen COHEOE CH ORs. 09o)4.0. 97 30 MEELVOCHSH 1 ......006..0 Sinn OH OOH Gres .sr, 83 26 fo )SOHCH,SH:.........:. Sse (CH) CHO OH 1. 108 20 CH,OH,CHSHCH, ......... 84 | CH,CH,CHOHOH.......... 99 15 OH(CH,).CH,CH,SH ...... 120\ | OH(OH,),CH,CH,OH ... 131:5 | 11:5 WCVCHOHSH ............-.. 137 CCl CHOMOH,.... 1). 149 26 JOS oa NY GCC IECXO)E [Nat Oly eee 180 8 BEI (SEL) 0.0.55 250 lcasesecens DAS ee ON (OED). © hss. vccedons 270 27 OH (CH.),CH,SH. ......... 1450 | OH,(CH,),CH.OM ...... 157 12 ROME OELSH .......ccccasccdes sh Wy /Ol BU XODELCOUSIAN SAA eae lle! 205 11 OPH CH.SH (a) .....50000.- een | Os Ole OF (a) vente 188 0 i, (G) 3. are 188 * (Gis ce emenet 201 13 (yy) a eae 188 rea (Cy) eek. 198 10 CO) 5 ah Coie OH COON aCe tet 17 24 OLE OSH (a)......000cccce BtGw "C,H OHO (e) i i.08. 6. 245; 29) + Exception :—C,,H,SH(a) 285 C,,H,(OH)(a) * The only exception to the rule is that marked +, and isin the case of a body of high molecular weight and complicated constitution. 460 Miss Earp on the fect of the Replacement of Again, in the following list of compounds containing oxygen not in the condition of hydroxyl, it will be seen that the normal rule is followed. : Diff, 5 | ° GHIGHS oN eee 205 | CH,CHO Si | 184 (GEORe oo ern: 300:.| (CH,).0.... 138 | 187 (OH So tes 41 | (CH,),0... aoean. 64 (OH OSH Phe... 200 | (CH.),CO, 1... 91 109 (HAC ys ee. 64 | (C,H(CH)O a li | 58 Ce a ee 99 |(C/H.).0 -.... oa 35 | 87 OH(CH OHOHS =... 114 | origi, ) CH, OHO .... ee ae COR Vu Rel ee Oi 249 | (C,H,),CO, nna 125 | 1b MESOHGHE We. 1 | mG One a B8 | 96 (GHIOHCH is ap 140 | (CH,CHCH,,0 20m 82 | 58 (GHICHCH an eh... 188 | (CH.CHCH.),0, «1.0... 171 17 (Po SO ae 180 | (Pr),0(«) ....2 s2 | 48 . es i 01 | @... e 60 | 60 CoS Cenc kel he 310 | (RtOCH,)>..... am 193 | 87 CinecGstias aah ia. 204. | 0,H.00,H. a 172 | 32 (GHLOECH.GH,).S .......... 182 | (GH.CH.CH,CH,),0 .. 140 | 42 CREHOIECING oe eee 215 | CAC CHORt am 185 | 30 GEER a 950 | (C.H,.),0 (Iso) eae 175 | 7 (Gao de alee oo: 339 | (CLH 0"... ee 978-288 | 5444 GS. ee. 392.| (CH ).O ae 246 | 46 GHICOSCH, «7 .. 95 | CELCOOCH, aa 56 | 39 beCens: soot ce ee 169 | "CO(OCH,), ©). eam 90 | 79 @HCOSOH Lg es 115 | CH,COOU-H, 4. Gem 77 | 88 PE OOSCH (a) 8 uk 35 | CH{COOCH (a) «+. 102 BB es 124 ged eee Carcoods Aus i ir 984 | C,H C0000 ae 276 8 CELLOSC ie ee 249, | G,H,COQU, Hy aaa 212 | 30 CIOCUN Gee 132 | CHLOCN .\. Jem 90 | 49 CHeNCS ee 119 | CH-NCO ... 44 | 75 OH CHGH NOS... 150 | CH.CHCH,NCO ......... 82 | 68 GRAISONI(G) sees 151: | C,H,OCN (B) ... aa 67 | 84 Gi(OH;),CH,NCS...... 162 Ci(CHT,),CH.NCO a 110 | 52 GuOOseO, et 984 | C,H.COOCO,.... ama 276 Wilks fie sae cies weer oY | (SONGS eee ee 218 |.C,HNCO ....aaee Coe Be GaTOHENON eet) 943 | O-H-CH,NOO ce 175-200 ie SObines Meee ee 156-160, CCIO0CL, -..... (about) 100 | To the above may be added the series of ethyl carbonates quoted at first, and also the following inorganic compounds:— OSs Wate css 42°6 GOs.) tieeeeee —782 CSC] ie yee-kes-- 71 COC vs: secre 82 1S) C) eee renee 125 POC, .tocceee 197 By arranging the data rather differently it is easy to see that the abnormality hes entirely with the hydroxy! group. Thus, if we take any group of sulphur compounds of one type, we shall find the boiling-point increases with the molecular weight as well when the hydrogen of the SH group is replaced by a hydrocarbon radical as in any other case. Oxygen by Sulphur on Boiling-points of Compounds. 461 Such, for example, are the following :— le} ae ~61°8 H,S......—61'8 Histo 2 e =618 CH,SH ...... 21 Gh USiengs 36 C,H.SH ... 172 me (CH.).S-...... Aiea,” (C.),S... A, O,H.SC,H, 204 VH,.CH,S 64 Pr,S («) .. "130 Poe (CAHBcies o> Taking in the same way the corresponding oxygen com- pounds, we find that by replacing OH by OX, where X stands for any hydrocarbon radical, unless very complex, we lower the boiling-point of the compound considerably, whereas when the exchange is simply between different hydrocarbon radicals the change is in the normal direction. elec... 100 Te Obs sec. 100 HOVSGRae 100 CH,OH ...... 67 C,H,OH...... 78:4 (C,H,OH_... 180 Beco .. —23 | B, (C,H,),0.... 35 B, O,H,00,H,... 172 eneH.O... 11 (Pr,)O («) .. (C,H,),0...... 246* From these data it is evident that the fact that water, which has a lower molecular weight than even any of the “permanent” gases (except hydrogen) will remain liquid up to a very high temperature, is only one particular and well- marked case of the general effect of the hydroxyl group. It has been objected by Ostwald and others that the com- parison of boiling-points is unsatisfactory, inasmuch as in some cases it is possible that the vapour-pressure curves of different substances may cross one another at some point; and in that case, if some other than atmospheric pressure were taken as the standard, the relative position of the boiling- points would be reversed. It is difficult to plot the vapour-pressure curves for H,O and H,S on the same scale, since the pressure of H,S varies by many atmospheres ; while that of H,O varies through the same range only by a few inches, so that it has to be repre- sented on the H.S scale by a line following the zero. The H.S curve is, however, perfectly normal, and shows no ten- dency whatever to approach the zero at any point short of infinity. Hence the objection about the crossing of the eurves falls to the ground in this case. The same may be shown by comparing the curves for CO, and CS,; only in this case, of course, the sulphur compound follows the zero line, while the other is highly inclined. With regard to the melting-points of oxygen and sulphur compounds the same general rule holds ; but exceptions are not rare, particularly in the cases of more complicated com- pounds, and naturally it is among these that the larger number * In this case the destruction of OH is not sufficient to balance the effect of introducing the second carbon ring. Phil. Mag. &. 5. Vol. 35. No. 216. May 1893. 21 402-- Notices respecting New Books. of melting-point data are given. In all probability the ten- dency to form molecular groupings and other unknown factors tend to obscure the effect on melting-points due to the change of constitution alone. Another point which I think may be noticed with advan- tage from the series just given on page 461, and which, as far as | am aware, has been hitherto neglected, is the effect on the boiling-point of the symmetry of the molecule, unsym- metrical molecules tending to boil higher than symmetrical ones. Consider the series A,, page 461. Between the first and second members of the series there is a large difference, the molecular weight beg increased and the symmetry of the molecule destroyed at the same time. Between 2 and 3 of the same series, on the other hand, there is a much smaller difference ; the molecular weight is increased but symmetry is restored, and the two things act against one another. Again, consider the series B,. Between 1 and 2 in this series the destruction of hydroxyl lowers the boiling-point, the destruction of molecular symmetry tends to raise it, the result being that the difference only of the two effects is small. Between 2 and 3 the destruction of hydroxyl and the resto- ration of symmetry act together, and the resultant effect is large. The same effects may be noticed by comparing A, and By in the same way, and also by comparing the first, second, and fourth members in the series A; and B; respectively. XLV. Notices respecting New Books. An Elementary Treatise on Modern Pure Geometry. By R. Lacutan. (London: Macmillan. 1893. Pp. x+288.) N R. LACHLAN is a recognized master of the Geometrical craft, and the work before us well maintains his reputation. His primary object is to meet the new Cambridge Tripos regula- tions, in which provision is made for the introduction of a paper on “ Pure Geometry.” All that could fairly be looked for in such a paper is given by the writer, or is led up to by him. He has not, however, contented himself with such a limited supply as this would require, but he has written with a view to allure students on to the arcana of the science. After a careful perusal we have detected very few errata. On page 53, Ex. 4 is obviously a slip, and in line 3 from bottom for Bw read By, for Cw read Cz. Page 55 line 13 contains a small clerical error: the opening Notices respecting New Books. 463 sentence of §116 is not sufficiently guarded to be accurate. In Ex. 3, page 70, it is not stated what point S’is. On page 161 line 11, for “polar” read “ poles.” Two or three clerical errors are easily corrected. The following historical one occurs on page 78, Ex. 6: “ Mr. H. M. Taylor’s paper was read before the London Mathematical Society on Feb. 14th, 1884,” whereas he had previously published his Note, “ On a six-point circle con- nected with a triangle,” in the ‘ Messenger of Mathematics,’ vol. xi. (May 1881—April 1882). If we mistake not, the “circle” had previously been given by him ina Trinity paper. In conclusion we are glad to say that the text is not overburdened with corol- laries and superfluous matter, the figures are excellent, and there is a most judicious and varied selection of exercises. Revue Semestrielle des Publications Mathématiques rédigée sous les auspices de la Société Mathématique d Amsterdam. Tome L., 1* partie. (Amsterdam. 1893. 104 pp.) THE object which the Mathematical Society of Amsterdam has in view in putting forth this Revue is * de faciliter l’étude des sciences mathématiques en faisant connaitre, sans délai de quelque import- ance, le titre et le contenu principal des mémoires mathématiques publies dans les principaux journaux scientifiques.” Primarily it is intended for the use of its own Members, but the Society has rightly judged that such a publication, if well conducted, will be of service to a much larger circle of readers. This opening number contains titles of papers printed in about 120 journals, 19 of which are British and 8 American. A careful list of the titles is drawn up with various particulars of interest (pp. 87-104). The title of each communication is preceded by a system of notation adopted at the recent Congres International de Biblio- eraphie des Sciences Mathematiques, and is followed by a very concise Compte-rendu of the contents. We may say that the Revue, though its objects are similar to those of the well-known Fortschritte der Mathematik (Berlin), does not aim so high, for in the generality of instances the insight into any paper given by the notices here is little more than a student would inter from the bare title. Its merit is that a much earlier record, if the editors keep up to date, will be available for authors and readers. The papers tabulated from this Journal are comprised in Vol. xxxiv. (Nos. 206— 209) and are seven in number. ‘Twoare given by the titles only : of the others a fair abstract is given. Lord Rayleigh’s papers are assigned to “J. W. S. Rayleigh.’ We wish the Society good success and a large clienteéle. -f 1464.) XLVI. Proceedings of Learned Societies. GEOLOGICAL SOCIETY. [Continued from p. 313.] January 25th, 1893.—W. H. Hudleston, Esq., M.A., F.R.S., President, in the Chair. ae following communications were read :— 1. “On Inclusions of Tertiary Granite in the Gabbro of the Cuilin Hills, Skye; and on the Products resulting from the Partial Fusion of the Acid by the Basic Rock.” By Prof. J. W. Judd, F.RS., V.P.G.S. The author first calls attention to previous literature bearing on the subject of the extreme metamorphism of fragments of one igneous rock which have been caught up and enveloped in the products of a latereruption. The observations of Fischer, Lehmann, Phillips, Werveke, Sandberger, Lacroix, Hussak, Graeff, Bonney, Sauer, and others show that, while the porphyritic crystals of such altered rocks exhibit characteristic modifications, the fused ground- mass may have developed in it striking spherulitic structures. On the north-east side of Loch Coruiskh, in Skye, there may be seen on a ridge known as Druim-an-Eidhne, which rises to a little over 1000 feet above the sea, a very interesting junction of the granitic rocks of the Red Mountains with the gabbros of the Cuilin Hills. At this place, inclusions of the granitic rock, sometimes having an area of several square yards, are found to be com- pletely enveloped in the mass of the gabbro. ‘The basic rock here exhibits all its ordinary characters, being a gabbro passing into a norite, traversed by numerous segregation-veins ; the acid rock is an augite-granite, exhibiting the micropegmatitic (‘ granophyrie ’) and the drusy (‘ miarolitic’) structures, and it passes in places into an ordinary quartz-felsite {‘ quartz-porphyry ’). Within the inclusions, however, the acid rock is seen to have undergone great alteration from partial fusion, and it has aequired the compact texture and splintery fracture of a rhyolite; weathered surfaces of this rock are found to exhibit the most remarkable banded and spherulitic structures. Microscopic study of the rock of these inclusions shows that the phenocrysts of quartz and felspar remain intact, but exhibit all the well-known effects of the action of a molten glassy magma upon them. The pyroxene, however, has been more profoundly affected, and has broken up into magnetite and other secondary minerals. The micropegmatitic groundmass, which was the last portion of the rock to consolidate, has for the most part been completely fused, and in some places has actually flowed. In the glassy mass thus formed, the most beautiful spherulitic growths have been developed, the individual spherulites varying in size from a pin’s head to a small orange. These spherulites are often Geological Society. 465 composite in character, consisting of minute examples of the ‘common type enclosed in larger arborescent growths (‘ porous- spherulites’) of felspar microlites, with silica, originally in the form of opal and tridymite, but now converted into quartz, lying between them. All the interesting forms of spherulitic growth which have been so well described by Mr. Iddings from the Obsi- dian Cliff in the Yellowstone Park, and by Mr. Whitman Crossfrom the Silver Cliff, Colorado, are most admirably illustrated in these inclusions of the Cuilin Hills. It is interesting to note that the nuclei of some of these large spherulites consist of fragments of the micropegmatitic granite which have escaped fusion. Among the new minerals developed in these inclusions, by the action on them of the enveloping magma, are pyrites and fayalite (the iron-olivine). The phenomena now described are of interest as setting at rest all doubts as to the order of eruption of the several igneous masses of the Western Isles of Scotland. That the gabbros are younger than the granites was maintained by Macculloch in 1819, by J. D. Forbes in 1846, by Zirkel in 1871, and by the author in 1874. In 1888, however, Sir A. Geikie asserted that these conclusions were erroneous ; he insisted that the granites were erupted after the gabbros and basalts, and that they are, indeed, later than all the voleanic rocks of the district except a few basic dykes which are seen to traverse them. The occurrence of the remarkable inclusions of granite within the gabbro now removes all possibility of doubt on the subject, and proves conclusively that the granite was not only erupted but had consolidated in its present form before the outburst through it of the gabbro. 2. “ Anthracite and Bituminous Coal-beds. An Attempt to throw some light upon the manner in which Anthracite was formed ; or Contributions towards the Controversy regarding the Formation of Anthracite.” By W.S. Gresley, Esq., F.GS. The author does not seek to advance any new theory in this communication, nor to proclaim new facts of any importance, but to put old facts in something of a new light, in order to aid the inves- tigations of others. His main object is to establish two facts, viz.:— that the associated strata of anthracite-beds are more arenaceous than those containing so-called bituminous coal-beds, and that the prevailing colours of the sandstones, grits, etc., of anthracite regions are greyer and darker than those of regions of bituminous coal. To these facts may perhaps be added a third, that the more anthracitic the coal-beds, and the more siliceous the enclosing strata, the harder and tougher these associated strata are. While recognizing that the rocks of many anthracite regions have undergone great disturbance, he cites other areas where coal-basins have been much folded, without any corresponding production of anthracite in considerable quantity. The modes of occurrence of anthracite are illustrated by many instances observed by the author in the Old and New Worlds. ie pe I 466 Geological Society :— February 8th.—W. H. Hudleston, Esq., M.A., F.R.S., President, in the Chair. The following communications were read :— 1. “‘ Notes on some Coast-Sections at the Lizard.” By Howard Fox, Esq., F.G.8., and J. J. H. Teall, Esq., M.A., F.B.S., F.G-S. In the first part of the paper the authors describe a small portion of the west coast near Ogo Dour, where hornblende-schist and serpentine are exposed. As a result of the detailed mapping of the sloping face of the cliff, coupled with a microscopic examination of the rocks, they have arrived at the conclusion that the serpentine 1s part and. parcel of the foliated series to which the hornblende- schists belong, and that the apparent evidences of intrusion of _ serpentine into schist in that district are consequences of the folding and faulting to which the rocks have been subjected since the banding was produced. The interlamination of serpentine and schist is described, and also the effects of folding and faulting. Basic dykes, cutting both serpentine and schists, are clearly repre- sented in the portion of the coast which has been mapped, and these locally pass into hornblende-schists, which can, however, be clearly distinguished from the schists of the country. The origin of the foliation in the dykes is discussed. The second part of the paper deals with a small portion of the coast east of the Lion Rock, Kynance. Here a small portion of the ‘oranulitic series’ is seen in juxtaposition with serpentine. The phenomena appear to indicate that the granulitic complex was intruded into the serpentine ; but they may possibly be due to the fact that the two sets of rocks have been folded together while the granulitic complex was in a plastic condition, or to the intrusion of the serpentine into the complex while the latter was plastic. 2. “ On a Radiolarian Chert from Mullion Island.” By Howard Fox, Esq., F.G.8., and J. J. H. Teall, Hsq., M.A., EUR SineG a: The main mass of Mullion Island is composed of a fine-grained ‘oreenstone,’ which shows a peculiar globular or ellipsoidal structure, due to the presence of numerous curvilinear joints. Flat surfaces of this rock, such as are exposed in many places at the base of the cliff, remind one somewhat of the appearance of a lava of the ‘ pahoehoe’ type. The stratified rocks, which form only a very small portion of the island, consist of cherts, shales, and limestone. They occur as thin strips or sheets, and sometimes as detached lenticles within the igneous mass. The chert occurs in bands varying from a quarter of an inch to several inches in thickness, and is of radiolarian origin. The radiolaria are often clearly recognizable on the weathered surfaces of some of the beds, and the reticulated nature of the test may be observed by simply placing a portion of the weathered surface under the microscope. The authors describe the relations between the sedimentary and Remarks on certain Islands in the New Hebrides. 467 igneous rocks, and suggest that the peculiar phenomena may be due either to the injection of igneous material between the layers of the stratified series near the surface of the sea-bed while deposition was going on, or possibly to the flow of a submarine lava. The forms of the radiolaria observed in the deposit, and also their mode of preservation, are described in an Appendix by Dr. G. J. Hinde. 3. “* Note on a Radiolarian Rock from Fannay Bay, Port Darwin, Australia.” By G. J. Hinde, Ph.D., V.P.G.8. 4, “ Notes on the Geology of the District west of Caermarthen.” Compiled from the Notes of the late T. Roberts, Esq., M.A., F.G.S. To the east of the district around Haverfordwest, formerly de- scribed by the author and another, an anticlinal is found extending towards Caermarthen. The lowest beds discovered in this anticline are the Tetragraptus-beds of Arenig age, which have not hitherto been detected south of the St. David’s area. They have yielded eight forms of graptolite, which have been determined by Prof. Lapworth. The higher beds correspond with those previously noticed in the district to the west; they are, in ascending order: (1) Beds with ‘ tuning-fork’ Didymograpti, (2) Llandeilo limestone, (3) Dicranograptus-shales, (4) Robeston Wathen and Sholeshook Limestones. Details of the geographical distribution of these and of theic lithological and paleeontological characters are given in the paper. February 22nd.—W. H. Hudleston, Esq., M.A., F.R.S., President, in the Chair. The following communications were read :— 1. “On the Microscopic Structure of the Wenlock Limestone, with Remarks on the Formation generally.” By Edward Wethered, F.G.S., F.R.MS. 2. “On the Affinities (1) of Anthr He a, (2) of Anthracomya.” By Dr. Wheelton Hind, B.S., F.G.S. 3. ‘ Geological Remarks on certain Islands in the New Hebrides.” By Lieut. G. C. Frederick, R.N. As far as can be judged from the soundings obtained, the New Hebrides are probably situated on a bank lying from 350 to 400 fathoms below the surface of the ocean and running in a N.N.W. and §.8.E. direction, with a deep valley between it and New Cale- donia. The only two soundings obtained between these two groups are 2375 and 2730 fathoms, the former within a short distance of the New Hebrides. Of the islands, Tanna is voleanic—an active volcano, apparently consisting entirely of fragmental material, being situate on its eastern side. Kfaté has some volcanic rock, but is chiefly of coral formation. It rises to a height of 2203 feet, and in some parts has’ a terraced appearance, the terraces denoting distinet periods of 468 Geological Society. upheaval. Coral was found to the height of 1500 feet above sea- level. To the north of Efaté are Nguna, Pele, and Mau, of volcanic | origin, and no coral has been found on them above sea-level; whilst | Moso, Protection, and Errataka, to the west of Efaté, are of coral | formation and similar in character to the adjoining coast of Efaté. | In the vicinity of the coral isles is very little coral-reef, especially when the shores are steep. Delicate live corals were brought up from depths of 28, 39, and 42 fathoms off Moso, 37 fathoms near Mau, and 40 fathoms off Mataso. Mataso is a volcanic island with a narrow fringing-reef. Makura (6 miles N. of Mataso) and Mai are also volcanic, with narrow fringing-reefs partly surrounding the former and entirely encircling the latter island. A short distance west of Mai is Cook’s Reef, of atoll formation. The Shepherd Isles are all of volcanic formation, apparently recent, and no coral was found growing around their shores. Mallicolo Island is of volcanic and coral formation. At one place in this island coral was found at a height of about 500 feet above sea-level. March 8th.—W. H. Hudleston, Esq., M.A., F.BS., President, in the Chair. The following communications were read :— 1. “On the Occurrence of Boulders and Pebbles from the Glacial Drift in Gravels south of the Thames.” by Horace W. Monckton, Esq., F.L.S., F.G.S. North of the Thames near London, the Glacial Drift consists largely of gravel, which is characterized by an abundance of pebbles of red quartzite and boulders of quartz and igneous rock. With the ex- ception of very rare boulders of quartz, the hill and vailey-gravels of the greater part of Kent, Surrey, and Berkshire are entirely free from these materials. The author points out that the River Thames is not, however, the actual southern boundary of the distribution of these Glacial Drift pebbles and boulders, though the number of localities where they are found in gravels south of that river is few. The author describes or mentions several, of which the foilowing are the most important :—Tilehurst, Reading, Sonning, Bisham at 351 feet above the sea, Maidenhead, Kingston, Wimbledon, and Dartford Heath. 2. “‘Onthe Plateau-Gravel south of Reading.” By O. A. Shrub- sole, Esq., F.G.S. This paper contains observations on the gravel of the Easthamp- stead-Yately plateau. The constituent elements of the gravel are described, and the author notes pebbles of non-local material near Czsar’s Camp, Easthampstead, on the Finchampstead Ridges, and at Gallows Tree Pit at the summit of the Chobham Ridges plateau. He mentions instances of stones from the gravel of the plateau (described in the paper) which may bear marks of human workmanship. He furthermore argues that the inclusion of pebbles of non-local origin Inéelligence and Miscellaneous Articles. 469 in the gravels may be due to submergence of the plateau up to a height of at least 400 feet above present sea-level, and cites other facts in support of this suggestion. He concludes that the precise age of the gravel can only be more or less of a guess, until the mode of its formation has been definitely ascertained. 3. “A Fossiliferous Pleistocene Deposit at Stone, on the Hamp- shire Coast.” By Clement Reid, Esq., F.L.S., F.G.S. This is practically a supplement to a paper, ‘On the Pleistocene Deposits of the Sussex Coast,’ that appeared in the last volume of the Quarterly Journal. An equivalent of the mud-deposit of Selsey has now been discovered about 20 miles farther west, and from it have been obtained elephant-remains, and some mollusca and plants like those found at Selsey. Among the plants is a South European maple. XLVII. Intelligence and Miscellaneous Articles. ON VILLARI’S CRITICAL POINT IN NICKEL. BY PROF. HEYDWEILLER. eS magnetism of iron, nickel, and cobalt changes under the influence of stretching forces. Villari first observed a special behaviour of iron in reference to this attribute, namely that with moderately strong magnetization small stretching forces increase the magnetism, while larger forces diminish it; thus the strength of the magnetism is graphically represented as a function of the load, the ordinates of the curve firstincrease up to a maximum and then diminish to far below the original values. The point of the curve at which the ordinate again reaches the original value is named Villari’s critical point. In nickel this property has not been observed up to the present ; in this case, so far as hitherto known, the magnetism steadily decreases with increasing load. But with strongly magnetized soft iron also, with small load, the original increase of the mag- netism vanishes, and it was thought probable that with sufficiently weak magnetization nickel also possesses a Villari’s critical point. Experiments have confirmed this expectation. In observing the changes in the very feeble magnetizations, it was found necessary to work with a very sensitive arrangement. A chemically pure nicke) wire, 46 cm. long and 0°15 em. thick, was suspended vertically with its lower end very near (3°5 em. distant) the upper magnetic needle of an astatic system, and so that small longitudinal displacements caused no perceptible altera- tion in the direction of the needle. An intensity of magnetization I=1 C.G.S. unit corresponded to about 90 p throw with 110 p scale distance. The reduction of the observed numbers to absolute measure was effected by comparison with an auxiliary magnetometer with single needle. Phil. Mag. 8. 5. Vol. 35. No. 216. May 1893. 2 K 470 Intelligence and Miscellaneous Articles. The observations were conducted with alternate leading and unloading, the strength of field remaining constant. The load never exceeded 1 kilog. per sq. mm. cross section of the wire. With small strength of magnetization under 2 ©.G.S. units and with the smallest loads, soft annealed nickel shows a small decrease of magnetism, with somewhat larger an increase, which may rise to 26 per cent. of the total magnetism, and finally again a decrease with increasing load. Thus, for example, for the intensity of magnetization I=0-97 C.G.S. units with a load of p gr. per sq. millim. cross section, there were obtained the following respective variations of magnetization él I | let é1/I. D. “SUE 28 —0:006 347 +0:067 46 —0-011 490 +0042 63 0014 7138 +0257 102 —0:019 904 +0162 165 =0029 || 977 +0155 | 246 +0015 || | With stronger magnetization the increase becomes continually smaller; moreover after-effects of the preceding loading and phe- nomena of hysteresis show themselves to a considerable degree. Hard-drawn nickel presents the same phenomena with much stronger magnetization still, even though in feebler degree. Thus with a hard-drawn nickel wire, for 155-5 C.G.S. units the variations of magnetization with a load of p gr. per sq. mm. were :— D. é1/I. p. 61/1. 9 —0:0034 84 +0187 18 —0:0052 113 +0:0180 27 —0-0054 246 +0-0122 33 —0-0062 360 +0-0080 42 +0°0081 490 —0:0304 56 +0:0186 740 — 00682 ‘We may therefore assert that, with reference to the above= discussed phenomena, the behaviour of nickel agrees well with that of iron quantitatively but not qualitatively. The detailed communication of the method of experimenting and ~ the results will be given in another place.—Svtzb. Wirz. Phys.-med. Ges. March 11, 18938. Intelligence and Miscellaneous Articles. 471 ON THE INTERFERENCE-BANDS OF GRATING-SPECTRA ON GELATINE. BY M. CROVA. Photographed gratings applied on bichromated gelatine by M. Izarn’s* method may give rise to straight or curved inter- ference-bands, sometimes very irregular, in the spectra which they produce ; similar bands have been produced by Brewster f in other circumstances. These phenomena are obtained with great beauty on the spectra obtained by reflexion on gelatine-gratings on silvered glass. M. Izarn, in mentioning these interference-bands, expresses the opinion that they are connated with the interference phenomena by parallel gratings which I formerly investigated ¢. Sunlight reflected from a heliostat 1s caught on a very narrow slit the image cf which is projected upon a screen ; a very small image of the sun is produced at the focus of this lens, which is received on the striated surface of a grating photographed on gelatine on silvered glass; the real images of the slit and of the diffracted spectra are received on a screen placed in the conjugate focus of the slit in respect of the lens. The diffraction spectra are furrowed with large rectilinear black bands parallel to the rays, and which are almost absolute minima, the intensity of the rays reflected on the silvered surface being very little less than that of the rays which fall on the gelatine. With a copy of a fine Brunner’s grating, which I owe to the kindness of M. Izarn, the spectra of the first order present a large © dark band in the green when the grating is very dry; if the surface is breathed on the band is displaced towards the violet ; other and closer ones enter at the red end, and their number rises to three when the deposit of moisture confuses the projection. The same phenomena are produced but in the opposite direction during drying, and the displacement. of the bands becomes very rapid if the evaporation is accelerated by blowing air over the grating. If the incident light extends over the whole height of the erating instead of only to a small portion of the surface which is obtained by varying the distance from the lens, the fringes are curved, become irregular, and are sometimes serrated. The phenomenon is due to the interference of two parallel gratings; the one real, situated at the surface of the gelatine in the points in which the incident wave meets its discontinuous part; the other virtual, which is its image in the silvered mirror. Their distance, which is virtually constant, is the optical path, 2 ne, e being the thickness, and » the index of the gelatine. At the focus of the lens, since the light only affects a small part of its surface, the thickness of the gelatine is virtually constant. * Comptes Rendus, vol. exvi. p. 506. t+ Phil. Mag. [4] vol, Xxxi. pp. 22 and 98 (1866). t Comptes Rendus, vol, Ixxu, p. 855, and vol. Ixxiv. (1871-1873). 472 Intelligence and Miscellaneous Articles. lf, on the contrary, the light extends over a considerable sur- tace, the thickness of the gelatine varies at different parts, especially if the plate has been placed vertically while drying ; the bands are then bent while diverging, and their greatest divergence is at the part where the layer is thinnest. When the grating has been prepared, the distortion of the bands is very irregular ; but after a great number of hydratations followed by dryings the phenomenon becomes more regular. After fixing the grating in water and drying, the gelatine possesses, as is known, i kind of temper which is manifested by its accidental double refraction; but when it has been hydrated and dried slowly a great number of times its structure becomes more homogeneous, aud the bands no longer possess serrations. It is possible that such alternations injure the good keeping of the gratings, and it is thus desirable to keep them in a dry place. Observing the band-spectra in the goniometer they appear like broad and very dark spaces, but if sun-light is used condensed on the slit, by a cylindrical lens, the pivot lines of the spectrum are defined in these spaces with marvellous precision. ‘The production of these parasitical bands does not affect the accuracy of measure- ments made with these gratings. With gratings in gelatine on transparent glass these phenomena are scarcely perceptible by reflexion or by transmission, owing to the almost total identity of the refractive indices of gelatine and glass. If the mdex of gelatine is taken at 1°52, it is easy to calculate the thickness of the layer of gelatine as a function of the number of bands contained in the spectrum reflected on silver; I have thus found that in the copy which I use the thickness of the layer is 0-04 millim. when it is dry, and about 0°16 millim. when it is at its maximum hydratation; this number is only approximate, as the index varies with the quantity of water it contains. M. Izarn’s gratings are of admirable sharpness, and examined in the microscope they do not differ from the original ; in a Fro- ment’s grating, a hundred one, which I possess, the opaque interval is virtually equal to a fifth of the transparent interval: this is also the case with M. Izarn’s copy; this is not a negative but a posi- tive. The transparent intervals are the bands of insoluble gelatine, while the opaque intervals are the places where the soluble gelatine has been dissolved away by the water; but owing to the extreme fineness of the intervals, the water by capillary action has hollowed out cylindrical grooves which to a plane wave behave like an opaque body. When the opaque interval is very great compared with the transparent one, the opposite might take place; but it is easy to see that even when the two intervals are transparent, the difference of the refractive indices of gelatine and air is sufficient to produce phenomena identical with those of the grating. This question calls tor new investigations.—Comptes Rendus, March 27, 1893. LH E LONDON, EDINBURGH, ann DUBLIN PHILOSOPHICAL MAGAZINE AND JOURNAL OF SCIENCE. [FIFTH SERIES.] JUNE 1898. ALVIN. Electrochemical Effects due to Magnetization. By GHoRGE OWEN Squier, PA.D., Lieut. U.S. Army *. INTRODUCTION. H# infiuence of magnetism on chemical action was the subject of experiment by numerous investigators during he first half of the present century t. Up to 1847 we find by no means a uniformity of statement in regard to this subject, and secondary effects were often interpreted as a true chemical influence. Among the earlier writers who main- tained that such an influence exists may be mentioned Ritter, Schweigger, Débereiner, Fresnel, and Ampére; while those of opposite view were Wartmann, Otto-Linné Hrdmann, Ber- zelius, Robert Hunt, and the Chevalier Nobili. Professor Remsen’s discovery, in 1881, of the remarkable influence of magnetism on the deposition of copper from one of its solutions on an iron plate, again attracted attention to the subject, and since then considerable work has been done directly or indirectly bearing on the question. Among other experiments by Professor Remsen { were the action in the magnetic field of copper on zinc, silver on zinc, copper on tin, and silver on iron, in all of which cases the magnet evidently exerted some influence. With copper sul- phate on an iron plate the effects were best exhibited, the * Communicated by the Author. + Wartmann, Philosophical Magazine, 1847, (8) xxx. p. 264. t American Chemical Journal, vol. iii. p. 157, vol. vi. p. 480; ‘Science,’ vol. i. no. 2 (1883). Phil. Mag. 8. 5. Vol. 35. No. 217. June 18938. 21 FFE en ee Re 474 Lieut. G. O. Squier on the Electrochemical copper being deposited in lines approximating to the equipo- tential lines of the magnet, and the outlines of the pole being distinctly marked by the absence of deposit. Messrs. Nichols and Franklin * were the next to conduct experiments bearing on this subject. They found that finely divided iron which has become “ passive ” through the action of strong nitric acid suddenly regains its activity when intro- duced in a magnetic field, and also that when one of the two electrodes immersed in any liquid capable of chemically acting upon them is placed in a magnetic field, a new difference of potential is developed between them due to this magnetization. ‘They ascribe these effects to electric currents in the liquid produced indirectly by the magnet, which currents go in the liquid from the magnetized to the neutral electrode. Professor Rowland and Dr. Louis Bell ft were the first to note the “‘ protective action”’ of points and ends of magnetic electrodes, and to give the exact mathematical theory of this action. Their results were directly opposite to those of Messrs. Nichols and Franklin, who found, as stated above, that points and ends of bars in a magnetic field acted like zines to the other portions, or were more easily dissolved by the liquid. The method of experiment adopted by Professor Rowland was to expose portions of bars of the magnetic metals placed in a magnetic field to reagents which would act upon them chemically, and study the changes in the electro-chemical nature of the exposed parts by fluctuations in a delicate galvanometer connected with the two bars. Iron, nickel, and cobalt were experimented upon, and nearly thirty reagents were examined in this manner. The results are summed up in the following statement :—“ When the magnetic metals are exposed to chemical action in a magnetic field, such action is decreased or arrested at any points where the rate of variation of the square of the magnetic force tends towards a - maximum.” | Other investigations in this field are those of Andrews f, who employed iron and steel bars from eight to ten inches long with their ends immersed in various solutions, and one bar magnetized by means of a solenoid. The protective action was not noted, but, on the contrary, the magnetized #* American Journal of Science, vol. xxxi. p. 272, vol. xxxiy. p. 419, vol. xxxv. p. 290. + Phil. Mag. vol. xxvi. p. 105. { Proceedings of the Royal Society, no. 44, pp. 152-168, and no. 46, pp. 176-198. Liffects due to Magnetization. 475 bars acted as zincs to the neutral bars, thus indicating that they were more easily attacked. Practically the same results were obtained by Dr. Theodor Gross * ; soft iron wires, 8 cm. long and 3 cm. in diameter, coated with sealing-wax except at the ends were exposed to various liquids. When one electrode was magnetized, a cur- rent was obtained going in the liquid from the magnetized electrode to the non-magnetized electrode. It thus appears that there is at least an apparent incon- sistency between the protective results of Professor Rowland and Professor Remsen, and those of Nichols, Andrews, Gross, and others, who find the more strongly magnetized parts of iron electrodes more easily attacked than the neutral parts; and it was with the object of endeavouring to reconcile these results, and of studying the exact nature of the influence exerted by the magnet, that the experiments recorded in this paper were undertaken. APPARATUS AND MEruop oF INVESTIGATION. The method of investigation was that adopted by Professor - Rowland in his previous work on the subject, since its facility and delicacy permitted the effects of the magnet to be observed whenever there was the slightest action on the electrodes by the solution examined, and the investigation - could thus be carried over a wide range of material. A large electromagnet was employed to furnish the mag- netic field, and, at a distance sufficient to prevent any direct influence due to the magnet, a delicate galvanometer of the Rowland type was set up. Small cells were made with iron electrodes of special forms, coated with sealing-wax except at certain parts, and immersed in a liquid capable of acting chemically on iron. The whole was contained in a 50 cubic centim. glass beaker, and when joined to the connecting wires of the distant galvanometer was firmly clamped between the poles of the electromagnet. In the course of the examination of anumber of substances it was found necessary to use two galvanometers—one specially made by the University instrument-maker and very sensitive, which was employed with acids which evolve hydro- gen; the other, much less sensitive, was best suited to the violent “ throws” with nitric acid and iron. The samples of iron used throughout the experiments were obtained from * “Ueber eine neue Entstehungsweise galvanischer Strome durch Magnetismus,” Stizwngsberichte der Wiener Akademie, 1885, vol. xcii. (1885) p. 1873. 2152 a ae versio tare ast 2 aad Bae a 476 Lieut. G. O. Squter on the Electrochemical Carnegie, Phipps, and Co., of Pittsburg, and were practically pure. In order to insure a uniform density of surface, the elec- trodes were turned from the same piece and polished equally with fine emery-cloth. The magnet could be made or reversed at the galvanometer, and its strength varied at will by a non-inductive resistance. The electrochemical effects due to the magnetic field could thus be studied with facility by the fluctuations of the galvanometer-needle. The original difference of potential, which always existed between the electrodes, was compensated by a fraction of a Daniell cell, so the effects of a variation of the magnetic field could be ob- served when no original current was passing between the electrodes. The standard cells were made with care, and under uniform treatment possessed at 20° C. an electromotive force of 1:105 volt. The connexions with the compensating cir- cuit, which contained a finely-divided bridge, were so arranged that from its readings the difference of potential between the distant electrodes became known at once without involving the resistance of the cell or of the galvanometer. Since quantitative measurements of the effects observed were desired, a preliminary step was to calibrate the electro- magnet for a given distance apart of the pole-pieces. The method employed was the well-known one of comparing the galvanometer deflexions produced by a test-coil in the 4eld with those of an earth inductor in series in the circuit. Since the effect of the sudden addition of a certain strength of field was wanted instead of its absolute value, the de- flexions with the test-coil were taken for simple “make” or “ break ’”’ and not for reversed field, thus eliminating the residual magnetism of the pole-pieces. In the formula applicable, viz., H amnwv d EY mga a! ee in which d and d’ represent the deflexions due to the inductor and test-coil respectively, H and H’ the earth’s field and the field to be measured, n and n’ the number of turns, and a and a’ the radii of the coils, the particular values were :— mna’ =20716 square centim. ma” =6'788 square centim. Distance between pole-pieces 3°5 centim. Effects due to Magnetization. 477 H’=1299:48 d'H, and as d’ varied from 3), to 16, the range of field employed was from 65 to 20,800 H. A curve was constructed so that from accurate ammeter readings in the field circuit the strength in absolute measure could be read off at once. EXPERIMENTAL RESULTS. Preliminary.—The first experiments were made with very dilute nitric acid and iron electrodes—one a circular disk of 5 millim. radius, and the other a small wire 1 centim. long and 1 millim. in diameter, turned te a sharp point at one end. The peint was placed opposite the centre of the disk, at a dis- tance of 1 centim. from it, and the whole placed so that the cylindrical electrode coincided with the direction of the lines of force. When the minute point and the centre of the disk were exposed to the liquid, and the magnet excited, a momen- tary “throw” of the galvanometer was observed in the direction indicating the point as being protected or acting as the copper of the cell. When the pointed pole was slightly flattened at the end, and the insulation so cut away that the surfaces of exposure on the two electrodes were exactiy the same, the throw of the galvanometer on making the field was very much diminished, although still perceptible, since the disposition of lines of force would still be very different over the two plane surfaces of exposure. With ball-and-point electrodes precisely similar pheno- mena were observed as with a disk and point, except to a less degree. The gradual reversal of the current shortly after exciting the field, the independence of the throw of the direction of the current through the magnet, the disappearance of the throw when the nature of the magnetic field at the exposed parts became the same, and the effects of artificially stirring the liquid, were observed exactly as described by Messrs. Rowland and Bell. In the course of a large number of preliminary experi- ments with nitric acid, it was soon observed that under certain conditions the effect of suddenly putting on the magnetic field was to produce a less rapid deflexion of the galvanometer in the opposite direction, or indicating the point as acting asa zinc. Plainly this irregular behaviour, due to the magnet, required a more systematic study than it had yet received. It had been found that the reversal of the current, which regularly followed the “ protective throw,” was decreased or destroyed by anything which prevented free 478 Lieut. G. O. Squier on the Electrochemical circulation in the liquid, and that an acidulated gelatine, which was allowed to harden around the poles, was best suited for this purpose. The great irregularity observed in any one experiment made it necessary to eliminate everything possible which might mask the true phenomenon, if any ac- curate comparisons were to be drawn between the effects observed in the different cases; accordingly a standard form of experiment was adopted, which was carefully repeated many times. The cell found best suited for this purpose was composed as follows :— Disk electrode, diameter.................. 14:4 millim. thickness! .)..c. 4 ae Dib ito tig Point electr ode, total length ............ L524, Se RA _ diameter, oso weee 44, ss length of point......... D2 sug Distance of point from centre of disk... 10 5 The same electrodes were used aacianeen any set of experi- ments, being carefully cleaned and polished each time. With nitric acid the liquid was finally made up as follows :— Distilled water ............... 10 grammes. Flardscelatine ace. 245.2 1 gramme. C. P. nitric acid (sp. gravity 1°415) 0533 gramme. ‘The gelatine and water were allowed to stand until the former had dissolved without the application of heat, when the acid was added and the whole thoroughly mixed. Too strongly acidulated gelatine would not harden at all. In some cases, in order to protect the point from the ‘beginning, the electrodes, secured as usual at the ends of two small glass tubes containing the connecting wires, were tirmly clamped in the proper position between the poles of the magnet, and the magnetic field put on before the cell was completed, by pushing the beaker containing the solution up in position round the electrodes. With this cell a series of parallel experiments were con- ducted to obtain the variation of the effects with time, the amount of iron salts present, the fluidity of the solution, and with constant and variable magnetic fields. A. Behaviour of the Cell with Time, in the Earth’s Field. The cell was placed entirely outside the magnetic field, and galvanometer-readings taken at intervals of one minute for three hours. The curve fig. 1 (I.) shows these results. Posi- tive ordinates indicate a current from the point to the disk, Hifects due to Magnetization. 479 and negative ordinates the reverse current. Other experi- ments with fresh solutions, same electrodes, same exposed area, and every condition as nearly as possible the same, gave curves of practically the same character, and the one given is selected to illustrate. The curve indicates that the original current was to the point electrode; this gradually decreased, owing to polarization, until after a hour and five minutes it reversed slightly, but again reversed thirty-five minutes later, and after a little more than two hours the deflexion became perfectly constant, remaining so indefinitely. . The iron salts formed could not move with facility from the exposed surfaces through the hardened gelatine, and were easily outlined from their brown colour, as the whole appa- ratus was placed in a strong light. B. In a Uniform Magnetic Field. The cell was next placed in the magnetic field, which was kept practically uniform (about 15,650 H) for three hours, and galvanometer-readings taken as before. The electrodes were magnetized before being introduced into the solution, so as to protect the point from the begin- ning. In order to prevent the influence of the rise of temperature due to the heating of the field coils of the electromagnet, the whole cell was packed with cotton-wool between the poles. As Gross and Andrews observed, the temperature effect was small, the solution rising but 0°°7 C. in half an hour. The curve fig. 1 (I1.) shows the results of these observa- tions. It is seen that the original current was, as before, to the point electrode, and about the same in value. ‘This reversed after forty-five minutes, and rapidly increased to approximately twice its original value at the end of one hour and twenty minutes, and, instead of again reversing, remained indefinitely with the point electrode as a zinc. ‘The distri- bution of the iron salts in this case was quite unlike the former. Notwithstanding the gelatine, the powerful magne- tization of the exposed point gradually drew the iron salts from the disk as fast as they were formed, and concentrated them symmetrically about the point, giving the solution in this region an almost black appearance. After waiting a sufficient time to be assured that further presence of iron salts would not effect the permanency of the existing electromotive force, the magnetic field was gradually decreased without ever breaking circuit, by increasing the 480 5 i | ba Pe H i : ee i 4 H bi ee i i H uJ i | ee 000% 1 i () ; i ; Lieut. G. O. Squier on the Electrochemical PT ee ee eT HEEEBSS0E (a> cSRREEe ze eS pes te] ENE . : ig i Klee Fill Ateteceen (loatat GARR Rei ae sate SClNGEaaa JSNeRBea ee gers es he eee ee LPS fee Eee cle Ae sf | a8 SEE Ee E ACERE CEE EEC ee ee eee Fake AEE CAEP CED EE I) ar Pest tes TNE a Ear yin eb HBR a } = 3 5 i Fig.3 Effects due to Magnetization: 481 liquid resistance in the field current. This change of resist- ance was necessarily made more or less suddenly, and the deflexion experienced at each increase of resistance a not very sudden throw toward reversal, in every respect the same as had been repeatedly observed in the preliminary experiments, and very different from the characteristic “ pro- tective throw,” which is always sudden and in one direction. By simply varying the field current with care, as explained above, the deflexion could be reversed again and again at will, and could also be held at the zero of the scale, indicating no current at all, as long as desired. When once the field was entirely broken, the iron salts were released from the control of the exposed pole, seriously disturbed by gravity, and putting on the field again failed to reproduce the results noted above. The only elements of difference in the two cases are, (a) the magnetized condition of the metal, (0) the distribution of the iron salts formed by the reaction. Although, as the curves indicate, the average electromotive force with the magnetic field was much greater than in the former case, yet this electromotive force is due to the difference of action at the two exposed surfaces, and, as will be pointed out later, the total amount of iron dissolved and passing into solution in the two cases is probably not very different *. Quantitative experiments are wanting on this point. The influence of the magnetized condition of the metal and its magnitude is exhibited in the phenomenon of the “ pro- tective throw,” which is always observed with apparatus sufficiently delicate unless itis masked by other secondary phenomena. Since the electrodes were embedded in hardened gelatine, there could be no convection-currents in the liquid, and this can be eliminated. Hvidently the great difference in the behaviour of the cell in the two experiments described is principally due, either directly or indirectly, to the distribu- tion of the iron salts formed by the reaction in the two cases. The principal t¢me effects of the magnet were :— (a) To produce a higher potential at the point of greater magnetization. (b) To increase the rate of change of the potential between the electrodes and the absolute value of this potential dif- ference. (c) It also appears from both curves that after a certain distribution of iron salts is reached, further presence of the same does not affect the permanency of the current established. * Fossati, Bolletino dell’ Elettrictsta, 1890. 482 Lieut. G. O. Squier on the Electrochemical Since the time effects of the magnet were so marked, it was thought possible that a “ cumulative ” effect, due to the earth’s field alone, might be detected after a sufficient time had elapsed. The apparatus was made as delicate as possible, and parallel experiments conducted, the electrodes first being placed in the magnetic meridian, and afterwards perpen- dicular thereto. No positive difference could be detected. C. Convection-Currents in the Liquid. As has already been stated, the reversal of the current which regularly followed the “ protective throw ” was found by Messrs. Rowland and Bell to wholly disappear when har- dened acidulated gelatine was substituted for the dilute acid solution, so that when the magnet was put on a permanent deflexion of much less magnitude was obtained instead of a transitory throw. ‘This indicated that currents in the liquid cannot be neglected, and their study was next undertaken. Since hardened gelatine completely prevented the reversal of the current, and with no gelatine it regularly appeared after a short time, a large number of experiments were made, in which the amount of gelatine was varied continuously between these limits. As expected, the effects also varied—the greater the fluidity of the solution, the more quickly the reversal occurred. In the light of what was already known concerning the presence of iron salts, some of the experiments were continued over a considerable time, and in others iron salts were intro- duced artificially, to increase the effects. It was soon found that by starting with a fresh hardened gelatine, with which the “ protective throw” was the only feature, and gradually increasing the fluidity of the solution and the amount of iron salts present, both effects were exhibited at the.making of the field—first, the sudden throw of the needle always in the direction to protect the point, and immediately thereafter the comparatively slow “ concentration throw” in the opposite direction. By making the conditions still more unfavourable for the “ protective throw,” it gradually diminished until en- tirely masked by the second effect, so that making the field produced a deflexion in the direction indicating a current from the point. With the proper conditions, both of these effects could be studied with the greatest ease: first, one made prominent, then both equal, then the other made prominent at will. The “protective throw’ could be traced until it became a mere Liffects due to Magnetization. 483 stationary tremor of the needle at the instant of its starting on the “concentration throw.” This latter, though called a “throw,” can be made to vary from an extremely slow continuous movement of the galvanometer deflexion, as in experiment B already described, to a comparatively rapid deflexion at the instant of making the magnet. By using simply a dilute nitric-acid solution with no gela- tine, and inserting a thick piece of glass between the electrodes, the concentration effect was delayed enough to allow the ‘protective throw” to first appear, with consider- able iron salts in the solution; and on making the field both effects were observed as described above. It now appears that the reversal of the current, uniformly observed in the experiments of Messrs. Rowland and Bell, was but a form of the “‘concentration throw” mentioned above, and that we can regard the substitution of the hardened acidulated gelatine for the dilute acid as merely separating these effects, so that the former can be studied by itself; in other words, the reversal of the current would have occurred just the same after a sufficient time had elapsed. Turning to the experiments of Drs. Gross and Andrews, they employed but one magnetized electrode, which was not pointed. In this case the nature of the magnetic field at the two exposed surfaces would be very much more nearly the same than when a pointed electrode is employed. This arrangement is not, therefore, suited to bring out the delicate “‘»rotective throw,” and it is not surprising that the concen- tration effect was the prominent feature observed. We have now a complete reconciliation of the directly opposite results referred to in the introduction. The “ pro- tective throw ” is due to the actual attraction of the magnet for the iron, and is always in the direction to protect the more strongly magnetized parts; while the “concentration throw ” is always in the opposite direction, and depends upon the distribution of the iron salts present in the solution, and the convection-currents in the liquid. The concentration of the products of the reaction about the point would tend to produce a ferrous reaction instead of a ferric, and experiment shows that a higher electromotive force is obtained with cells in which a ferrous reaction takes place than with those in which a ferric reaction occurs; and this change in the character of the reaction produced by the concentration prob- ably accounts, at least in part, for the increased electro- motive force at the point. ee a ne ee 484 Lieut. G. O. Squier on the Electrochemical D. The Iron Salts about the Point Electrode. The effect of artificially stirring the liquid, and the direct influence of the fluid condition of the solution on the de- flexions observed, at once suggested movements of the liquid, produced indirectly by the magnet. In order to locate these currents and determine their potence, a small cell was made of two rectangular pieces of glass held by stout rubber bands to thick rubber sides. Perforations in the sides admitted the electrodes, which were point and disk as before. The cell, between the poles of the electromagnet, was in a strong light, and the movements in the liquid were easily perceptible from the displacements of suspended particles introduced for the purpose. When very dilute nitric acid was placed in the cell and the magnet excited, some interesting phenomena were observed. The liquid, at first colourless, almost immediately assumed a pale brown colour about the point, but nothing appeared at the disk electrode. The iron salts were drawn as soon as formed towards the point electrode, since here the rate of variation of the square of the magnetic force is a maximum. As more iron was dissolved, a surface approximating to an equipotential surface of the pointed pole, and enveloping the coloured iron salts, was observed enclosing the point and at some distance from it. The outline of the surface became darker in a short time, and finally two or more dark contours, separated by lighter portions and symmetrical with the outer one, appeared between it and the point, indicating maxima and minima of density. When the magnetic field was gra- dually increased, this surface usually enlarged without breaking up and holding the iron salts within it. On further strength- ening the magnetic field to about 16,000 H, the ridges merged into one thick black envelope around the point. This phenomenon is best studied with but little iron salts present, and by watching the point electrode with a micro- scope while the strength of the magnetic field is increased and decreased continuously. The sections (fig. 3) show the general form of these contours with different strengths of field. Upon breaking the field everything dropped from the point suddenly to the bottom of the cell, and on making the field again it required a few seconds for the salts to reappear at the oint. ‘ This, at least partially, accounted for the sudden effects often noticed at breaking the field circuit, and the compara- a ne Hffecis due to Magnetization. 485 tively smali ones at ‘‘make,” especially with certain salt- solutions, such as copper sulphate. The outer envelope which held the iron salts together, and limited the immediate influence of the magnetized point, was distinctly defined within the liquid, and easily observed by the reflexion of the light from its convex surface. The persistency with which the iron salts were held about the point was shown by moving the cell with respect to the electrodes, when the contour remained approximately intact, passing bodily through the liquid without being broken up. H. Electromagnetic Rotations. The small dust particles present in the liquid were drawn radially toward the point until they reached the surface described, when they pierced it and began to revolve rapidly about the point inside this surface, in the opposite direction to the currents of Ampere. Reversing the poles of the magnet produced surfaces of the same appearance but opposite rotations. When the current from a Daniell ceil was sent through it. seemed to have very little effect upon the rotations, showing them to be controlled by the powerfully magnetized point. The electromagnet was arranged with its field vertical, and the point electrode along the lines of force as before. This arrangement gave better control of the surfaces formed, since gravity now acted symmetrically about the point. When a single iron rod about 3 millim. in diameter, and placed vertically in the cell, was substituted for the two elec- trodes, two rotations were observed which were uniformly dextro about the north-seeking pole of the rod, and levo about the south-seeking pole. About the central neutral portion no rotations were observed. When the rod was covered with a thin coating of vaseline the rotations entirely disappeared as expected. Wartmann™ observed similar rotations about soft-iron cylinders adhering to the poles of a magnet, and he ascribed them to electric currents in the liquid which proceed from the periphery of the cell radially to the surface of the rod. The explanation of these rotations follows at once from what we know of the time-effects produced by the magnet. A higher potential is always produced at points of greater magnetization, causing electric currents in the liquid from the more strongly magnetized to the weaker parts of the iron. Applying this fact to the exposed conical point electrode, we see that local electric currents exist from its vertex to the other parts of the surface, returning by way of the metal. In the case of the vertical rod, these currents pass from the poles * Philosophical Magazine, xxx. p. 268 (1847). ‘ Fi 5 iy 4 ¢ ! ot er ih RRS AE pe we 486 Lieut. G. O. Squier on the Electrochemical at its ends, through the liquid, to the neutral portions, returning as before. These currents*, under the influence of the poles themselves, would cause electromagnetic rotations of the liquid, as we find them. The mere mechanical influence of these rotations, as in the case when the liquid is artificially stirred, is to increase the chemical action upon the point, causing it to tend to act more like a zinc, which experiment confirms. F’. Acids which attack Iron with the Evolution of Hydrogen. Professor Rowland had observed the ‘ protective throw ”’ with such acids to be extremely small, and difficult to detect except by very sensitive apparatus. The sensitive galvano- meter was set up and every precaution taken against inductive effects. A telescope and scale were used in this part of the work. Several substances were first examined, among them being hydrochloric acid, acetic acid, perchloric acid, chlorine water, copper sulphate, ferric chloride, sulphuric acid, &e., but as these observations added nothing to the results already obtained they are not given here. After several trials a standard sulphuric-acid solution was made up as follows :— Distilled water faces ee eee eee 10 grammes. Grelatame: ghee WA an ee 1 gramme. O.P. Sulphuric acid, sp. gr. 1°826 ... 1:062 gramme. More strongly acidulated gelatine would not harden, and weaker solutions gave too small effects. The “ protective throw ” was detected, but the point very soon became completely covered with minute bubbles of hydrogen, so that the electrodes had to be cleaned constantly. The effect of adding hydrogen dioxide to the solution was next tried, since this would facilitate the removal of the hydrogen as soon as formed, which was thought to act merely mechanically. When about 1 cubic centim. of H,O, was added to the solution the ‘ protective throw” became much more promi- nent, and the gas bubbles only appeared in small quantities aftera considerable time. Further addition of small quantities * The rotations produced in liquids by axial currents, e. g. currents coinciding with the direction of the magnetic lines of force as distinct from radial currents, have been studied by Dr. Gore (Proceedings of the Royal Society, xxxiil. p. 151). J. M. Weeren, Berichte der Deutschen Chemischen Gesellschaft, No. 11 (1891). Effects due to Magnetization. 487 of the dioxide showed the “ protective throw” to be very decided with sulphuric acid when the hydrogen 1s removed from the surface of the electrodes in this manner. G. The Electromotive Force. Several attempts were made to obtain the relation between the strength of field and the electromotive force developed in the “protective throw”; but it was difficult to obtain con- sistent readings owing to the trouble of balancing the original deflexion, and the small absolute values of this electromotive force when hardened gelatine was employed. A curve was constructed, however, showing the variation of the galvanometer deflexion with the strength of field, using nitric-acid solution without gelatine. This is shown in fig. 2. The readings were taken one after another as rapidly as possible, to eliminate the damping effects of the iron salts formed. The curve exhibits the general character of the variation. In the regicn from about 3500 H to 8000 H the greatest rate of change occurred, and beyond 10,000 H the curve became nearly horizontal for the particular electrodes used. Curves were also constructed for the “concentration throw” on making the field under different conditions, and they were approximately right lines, more or less inclined according to the amount of iron salts present. With the sulphuric-acid solution already given the electro- motive force varied from 0:°0033 to 0:0078 of a volt, while with the nitric-acid solution it became as great as 0°036 of a volt. In making all the solutions used with the different substances amounts were taken proportional to their particular molecular weights, and then halved or doubled until of suit- able strength to give results with the galvanometer. It was thought possible at the beginning that this might lead to some relations between the protective results and the strengths of the particular solutions ; but the general irregular cha- racter of the whole phenomenon prevented comparisons in this respect, and all that can be stated is, that both the “protective throw” and the concentration effect in general increased rapidly with the strength of the solution. H. Influence of a Periodic Magnetic Field upon the Cell. An experiment was made to determine the behaviour of the standard nitric-acid cell when the magnetic field was made and broken at regular intervals over a considerable time, and curves were drawn showing the variation of the “ throw ” with 488 Lieut. G. O. Squier on the Electrochemical time, and the fluctuation of the original deflexion caused by this treatment. The strength of field was about 11,000 H., and the experiment was conducted without compensating the original deflexion, and by making the field for one minute, then breaking for one minute, and so on. One of the curves is shown in fig. 1 (III.), in which posi- tive ordinates are values of the concentration throw at “ make,” and negative ordinates the values of the “ protective throw.”’ Experimenting was not begun until the gelatine had com- pletely hardened, and since the electrodes would tend to become polarized while the gelatine was hardening, the “ pro- tective throw” was very small, and soon masked by the concentration effects. After about five minutes, making the field had very little effect at all, but began to show decided “ concentration throws ”’ ten minutes later, and these rapidly increased with time, as the curve indicates. Considering the fluctuation of the original deflexion, the effect of this periodic field was to tend to reverse it, just as in the case of the uniform field in experiment B, but much more slowly, since the field was on but half the time in this case. The cell also showed the iron salts almost entirely about the point, forming a thick black envelope. i Summary. The principal results of this investigation may be sum- marized as follows :— Whenever iron is exposed to chemical action in a magnetic field, there are two directly opposite influences exerted. (a) The direct influence of the magnetized condition of the metal, causing the more strongly magnetized parts to be protected from chemical action. This is exhibited in the phenomenon of the “ protective throw,’ which is always in the direction to protect the more strongly magnetized parts of magnetic electrodes. The “ protective throw ” is small, often requiring delicate apparatus to detect it, and is soon masked by the secondary concentration effects. As to the absence of the “protective throw” with acids which attack iron with the evolution of hydrogen, the hydrogen acts merely mechanically, and when removed by adding to the solution small quantities of hydrogen dioxide, the ‘“ protective throw ”’ becomes very decided. In the curve, fig. 2, representing the variations of the “protective throw’ with the strength of the magnetic field, Effects due to Magnetization. 489 we trace at once the magnetization of the point-electrode. Since only the minute point was exposed to the liquid, it would become saturated for comparatively small magnetizing forces, and the curve indicates that this occurred at about 10,000 H., beyond which the curve becomes practically hori- zontal. ‘This further establishes the direct connexion between this “ throw” and the variation of the magnetization of the exposed point, and confirms the explanation of Professor Rowland, that it is due to the actual attraction of the magnet for the iron, and not to any molecular change produced by magnetization. : (6) The indirect influence of the magnet caused by the concentration of the products of the reaction about the more strongly magnetized parts of the iron. This tends to produce a higher potential at the more strongly magnetized parts, and finally establishes permanent electric currents, which go in the liquid from the more strongly magnetized to the neutral parts of the iron. This concentration-effect increases rapidly with the amount of iron salts present and the fluidity of the solution. The convection-currents in the liquid are themselves a consequence of this same concentration, being electromagnetic rotations produced by the action of the magnet upon the local electric currents between different parts of the iron. As to the permanent current due to the magnet which is finally set up between the electrodes, as shown in fig. 1 (II.), it is probably owing to a change in the character of the reaction produced by the concentration of the iron salts about the more strongly magnetized parts, which would tend to cause a ferrous instead of a ferric reaction to take place, and thus increase the electromotive force. Physical Laboratory, Johns Hopkins University, May 1892. Note.—Since the completion of the above investigation, a number of experiments have been performed similar to those of Professor Remsen. Starting with the known existence and direction of the electric currents in the liquid, it was thought that these might lead to some explanation of the peculiar form of deposit in equipotential lines. A number of interesting facts have been noted, but they are withheld for further experiments. Go OS: Phil. Mag. 8. 5. Vol. 35. No. 217. June 1893. 2M f 490 ] XLIX. Onthe Applicability of Lagrange’s Equations of Motion ina General Class of Problems; with especial reference to the Motion of a Perforated Solid in a Liquid. By CHARLES V. Burton, D.Se.* i | ee wr, p,... be some only of the coordinates of a material system, so that when the values of W, ¢,... are given the whole configuration is not completely determi- nate. But suppose it known that the kinetic energy T can be expressed as a homogeneous quadratic function of ab, d, sig’ only ; so that we may write OT = (rb) W242 (bb p+... 3 (br), (d),... are functions of W, d,... only Nag: We also suppose it known that (1) continues to hold good so long as the only (generalezed) forces and impulses acting are of types corresponding to UW, dese. 5). 2. Suppose, now, that such impulses of these types were to act on the system that yr, ¢,.. were all reduced to zero; the expression for the kinetic energy would accordingly vanish, and the system would be at rest. By supposing the last operation to be reversed, we see that the motion at any instant could be produced from rest by impulses of the types corre- sponding to aby by.» only... Ee can 3. Let 2, y, z be the Cartesian coordinates at time 7 of a mass-element m referred to fixed axes, and let T be the kinetic energy of the system at the same instant. Further, let A be the “action” when the system moves without additional con- straint from one configuration to another, and A+6A the action when by workless constraints the path is slightly modified, so that in place of the coordinates z, y, z we have w+6e2, ytoy,z+6z. Then ft SA ={Im(aéba + Ysy + 26z) | —[ Xm(ada + yoy + 262) | : + aterm which necessarily vanishes; . . (4) where [ | and {} denote the values of the quantities enclosed at the beginning and end of the motion considered. Suppose further that, both at the beginning and at the end, the values of Wy, $,... are the same for the one motion as for * Communicated by the Physical Society: read March 10, 1893. + Thomson and Tait’s ‘ Natural Philosophy,’ 2nd edit. Part I. § 327. On Lagrange’s Equations of Motion. 491 the other, so that initially and finally dw, 5¢,... are all zero. Jt does not follow that all the dx, dy, 5z’s are zero ; but Lm( toa + ydy + 282) is the so-called “ virtual moment” of the actual momenta in the hypothetical displacement 62, dy, dz; that is, the virtual moment, in the same displacement, of the impulse necessary to produce the actual motion from rest. In virtue of °), therefore, and of the initial and final vanishing of dy, d¢,.. he see that the bracketed terms of (4) must both be zero ; ence The inerement 5A vanishes and A has a stationary value for all worklessly effected variations of path which leave the initial and final values of Ww, ¢,.... unaltered. . (3) 4. Lagrange’s equations for the coordinates yp, $,... may now be written down at once, since the investigation of Thomson and Tait* becomes applicable to the present case without modification. It will be noticed that in their equa- tions (10) and (10)%, § 327, the sign of OV/d¥ should be reversed. We have thus a perfectly general proof of the proposition : If the kinetic energy of a material system can be expressed as a homogeneous quadratic function of certain generalized velocities wr, b,... only, the coefficients being functions of Wr, b, ... only, and if ifs remains always true so long as the only forces and impulses acting are of types corresponding to Ww, h,..., the equations of motion for the coordinates Yr, d,... may be written down from this expression for the energy, in accordance with the Lagrangian rule. Provided only that the stated conditions are satisfied, we need not consider whether the whole confiqura- tzon zs determined by the values of vf, 25 On what is the nature of the cqgnored coordinates. . . HAE | Suaaa tee ty (HAN) 5. Passing over the known spottenicd of this result to the motion of solids through an irrotationally and acyclically moving liquid, we come to the more general case of a perfo- rated solid, with liquid irrotationally circulating through the apertures. Take as coordinates any six 6, 6’,... which deter- mine the position of the solid, together with y, y’,... equal in number (m) to the apertures; each y being the volume of liquid which, starting from a given configuration, has flowed across some one of the m geometrical surfaces, required to close the apertures, these surfaces being supposed to move along with the solid. Of course the coordinates 0, 6’,... v. x’,... are insufficient * Loe. cit. 2M 2 492 Dr. C. V. Burton on the Motion of a to determine the entire configuration of the system (including the positions of all the particles of liquid); but we shall see immediately how, in virtue of the proposition (A), Lagrange’s equations may be written down. 6. Since an increment dy in one of the coordinates y is the volume of liquid which flows across a barrier-surface (1. é., which flows through an aperture relatively to the solid), the generalized force corresponding to y must be conceived of as a uniform pressure exerted over the said geometrical surface, by means of some immaterial mechanism attached to the solid; while the impulse corresponding to y is of course a uniform impulsive pressure applied in the same manner. [rom hydro- dynamical considerations we know that the measure of such an impulsive pressure is pdx, where p is the density of the fluid, and 6« the change produced in the circulation through the corresponding aperture. Hence the impulses corresponding to y, y’,... are Kp, p, . «2 2 aio where x, «’,... are the circulations through the various apertures. 7. Now when the motion of the liquid is irrotational, we have T =a homogeneous quadratic function of 0, 0’,...«,«’... only ; coefficients functions of 4, 6’... only; X,X ++. = homogeneous linear functions of 6, 6’,... x, «',... only ; coefficients functions of 6, 6’,... only. Since the y’s are equal in number to the «’s, let us suppose the last-written system of linear equations to be solved for the «’s in terms of the ¥’s ; we then have x, ’,...= homogeneous linear functions of 6, 6’,... XX’; only. coefficients functions of 0, 0’,... only. Substituting in the expression for T we get T = a homogeneous quadratic function of 6, Oa ¥, x, .. only; coefficients functions of 0, 0’,... only. This, then, remains true so long as the motion of the liquid is irrotational; in other words, so long as the only forces and impulses acting are of types corresponding to 6, 6’,... (since these are applied to the solid), y,7’,... (since these are uniform over the barriers, by § 6). If we identify Wy, $,... with the coordinates 0,0’,...4,%',--. of the present example, we see that the proposition (A) of § 4 is immediately applicable to this case. We may therefore oe. Perforated Solid in a Liquid. 493 ignore all other coordinates, and from the kinetic energy expressed as a function of 0, 0’,...y, x’,... write down the Lagrangian equations for 0,6’,... and, if we wish, for y, x’,... also. These latter, however, are less directly intelligible, since in general they involve finite pressures continuously acting over geometrical surfaces drawn through the liquid. 8. If we wish to picture the application of the principle of least action (§ 3) to the present case, we may proceed as follows: —Let the system start from the configuration (1.) and move without additional constraint or influence to the configuration (II.). Then let it start again from the confi- guration (1.) with the same velocities as before, and durin the motion let infinitesimal additional forces act on the solid, _while infinitesimal pressures, uniform over each barrier- surface, are impressed on the liquid ; the total rate at which the additional influences do work being at each instant zero. Further, let the additional influences be so adjusted that the system, after following a slightly different path, passes through a configuration such that 0, 6’,... x, x’,... are all the same as for (II.). Then, to pass from the configuration (II.) to the present configuration requires no displacement of the solid, and only such displacement of the liquid that the total volume which crosses any barrier-surface is zero. In such a change of configuration impulses of the types 0, 6',... y, x’,... would have no “virtual moment,” just as forces applied to the solid and uniform pressures applied to the barrier-surfaces would give rise to no virtual work. aia 9. At this stage it will be convenient to replace 6, 6',... by the components u,v, w of linear velocity and p, g, r of angular velocity, which determine the instantaneous motion of the solid along and about axes fixed in itself. The Lagran- gian equations for the six coordinates 0, 6’,... must accord- ingly be replaced by the forms suitable to moving axes. The expression for the energy in terms of the velocities now becomes a homogeneous quadratic function of w, v,; w, p, 9; 7; ¥, x',... in which all the coefficients are known to be constants. Let us apply the method due to Routh*, and modzfy this function with respect to the coordinates y, y',... If T be the value of the kinetic energy in terms of the velocities alone, the modified function (@.e. the kinetic part of Routh’s modified Lagrangian function) Ce a = T—Kpy—x'py! — nat CO) * Rigid Dynamics,’ vol. i, chap. viii. 494 Dr. C. V. Burton on the Motion of a from (6). Itis further known that the whole energy of the system =H-+K, . . =o! where Eis a function of u..., p..., only, and K is a function of the momenta xp only. Suppose, now, that the solid were brought to rest by forces applied to it alone: HE would vanish along with u, v, w, p, g, 7, while the circulations «, and con- sequently also K, would remain unaltered. The generalized velocities x, y',... would in general have changed, becoming, let us suppose x%, Xo,--- and the kinetic energy would accordingly have become K=Lpyy ti pyl + ...): 2a re Now let V=NVotX V=NItx' ~ . » . . (0) so that each x1 is that part of the flux of liquid (volume per unit time) which takes place across a barrier-surface owing to the motion of the solid itself. Having regard to (8), (9), and (10) our equation (7) for T’ becomes T’=(H+K)—2K—x«pyi—epy. . . . (1d) Let us write for the velocity-potential of the acyclze motion P=ud,+ vd, + wh, + ph, +qP, +7, + - (12) and for the value of x, across the barrier-surface « we have ¥1 =\\{% —[ul+vm+ wnt p(ry—mz) + 9(lz—nz) +r(ma—ly)] bdo, peters ke where 2, ¥, z are the coordinates of the element do and 1, m,n are the dircction-cosines of its normal y, all referred to the system of axes fixed in the solid. From (12) and (18) sub- stitute in (11); thus T’=E-K+ uSap|| [— ono + similar terms in v, w, + pnp | (ny —mz— oer \aa +similar terms in g, 7, . (14) where the summation refers to the m barriers. _ Remembering (8) it will be seen that T’ is now expressed in the proper form, namely as a function of u, », w, Ps, 7, and Perforated Solid in a Liquid. 495 the momenta xp, «’p,... only. By means of the relations - Be je ae ne = Oe es dap dv "aw "dg ©! a the equations of motion of the solid can at once be written down. X,..., L,..., are of course impressed force-and couple- constituents. 10. Since the kinetic energy due to any number of per- forated solids, moving in circulating liquid, can be divided into two parts, of which one is a function of the component velocities of the solids alone, and the other a function of the circulation-momenta alone, the above method may obviously be extended ; in fact a slight change in (14) will-render it at once applicable to the more general case. We shall have, evidently, VY=H-K+ Sniep {| (1 oo a0 +similar terms in v, w, Ze SpBep| | (ny—me— oo ria+ similar terms in g, 7, (15) where H is still the energy due to the motion of the solids and the acyclic motion of the liquid, and K the energy due to the circulations. In each barrier-term the first } denotes sum- mation with respect to all the solids, and for each u or p, &c., the second > denotes summation with respect to all the barriers of the system. These hydrodynamical results are not new, but the method of proof is in some respects different from anything that has yet been given, and will, I hope, be found intelligible and fairly simple. In an admirable memoir, just communicated to the Physical Society, Mr. Bryan has given a direct hydrodynamical proof of the equations holding good for the motion of the system in question ; but it seemed to me also desirable that the problem should be rigorously treated by the method of generalized coordinates, avoiding any assumption as to the impulse of the cyclic motion, and proceeding entirely from the principles established by Lagrange, and extended by Hamilton, Routh, and Hayward. When this paper was in proof it contained some remarks on the ignoration of coordinates, as treated in Thomson and Tait’s ‘ Natural Philosophy’*. Calling y, x’,... the inde- * Part I. § 319, example G. 496 Mr. A. B. Basset on the Finite pendent coordinates which, together with Wy, ¢,... determine the whole configuration of the system in §§ ],..., it was suggested that, in hydrodynamical and kindred applications, there was a difficulty in proving that OT/dx, dT/dx’,--- were all zero. But the difficulty, if indeed it should exist, is easily removed. For since the actual motion at any instant could be generated from rest by impulses of types corresponding to W, ?,... only, we have throughout the motion olfoxy—0, dT/ox'=0,233 and by the Lagrangian equations for y, y’,..., since all the generalized forces are of types corresponding to W, @¢,..., we get egtyor dol. al =e. a — > — =, =9,... dt ox Ox bE ON 2 HOM : whence or or —— =(), — =0 =e sie Ox Oe L. Note on the Finite Bending of Thin Shells. By A. B. Basset, IA., F RS ie HEN a thin shell of any form is bent in any manner, the most convenient way of obtaining the equations of equilibrium is to consider the stresses which act on a small element of the shell bounded by four lines of curvature on the deformed middle surface. If OAD B be a small curvilinear Fig. 1. Cc rectangle bounded by the four lines of curvature OA, AD, DB, and BO, the stresses across the section A D (as pointed out in my previous papers{) consist of the following * Communicated by the Author. + Proc. Lond. Math. Soe. vol. xxi. pp. 33 and 53; Phil. Trans. 1890, p. 433. Bending of Thin Shells. 497 quantities, viz.: T, = a tension across A D parallel to OA; M,= a tangential shearing-stress along A D; No =a normal shearing-stress parallel to OC; G,= a flexural couple from C to A, whose axis is parallel to A Ds ya torsional couple from B to C, whose axis is parallel to OA. Similarly the stresses which act across the section BD consist of :— T, = a tension across B D parallel to OB; M,= a tangential shearing-stress along B D: N, = a normal shearing-stress parallel to O Ol; G, = a flexural couple from B to C, whose axis is parallel to BD; l= (cs torsional couple from C to A, whose axis is parallel to O B. By resolving the stresses and bodily forces (such as gravity and the like), which act upon the element, parallel to the axes OA, OB, and OC, and by taking moments about these lines, we obtain the six equations of equilibrium of the element ; but as these six equations connect ten unknown quantities, namely the ten stresses which act across the sides of the element, they are insufficient for the solution of the problem. 2. In the case of a bell, or of a railway bridge which is thrown into a state of oscillation by a passing train, the displacements are all small quantities, and under these cir- cumstances the ten sectional stresses can be expressed in terms of the displacements of a point on the middle surface and their differential coefficients ; and owing to the fact that these displacements are small, we may neglect their squares and products when determining the stresses, and their cubes &c. when determining the potential energy due to strain. There is, however, another class of problems of considerable importance in which the deformation is finite instead of infinitesimal ; and to such problems the theory of thin shells is inapplicable. 3. An ordinary clock-spring is one of the most familiar examples of the finite bending of a thin plate or shell. Such springs consist of a naturally curved steel strip whose thick- ness is somewhere about one thirtieth of an inch, and whose breadth is from an eighth to a quarter of an inch according to the size of the clock ; and when the clock is wound up an amount of bending takes place which it would be unsate to treat as infinitesimal. ‘The hair-spring of a watch also 498 Mr. A. B. Basset on the Finite involves a case of finite bending; but as its cross section is approximately square, the theory of the bending of wires* would be more applicable. Similar examples, such as spring balances and other mechanical appliances where springs are employed, will readily suggest themselves; and the question whether the theory of wires or the theory of thin shells is most appropriate depends upon the nature of the spring. If the cross section does not differ much from a circle or a square, the former theory would appear to be the most applic- able; if, on the other hand, the breadth of the spring is considerable compared with its thickness, it would be better to regard it as a thin shell. When the natural form of a spring is a plane curve, and the spring is bent into another plane curve, the problem may be completely solved by the methods explained in chapter viil. of my ‘ Elementary Treatise on Hydrodynamics and Sound.’ The mathematical treatment is the same whether the spring be regarded as a wire or as a thin strip of metal like a clock- spring; the only difference being that the flexural rigidity is different in the two cases. If, however, a piece of clock- spring is twisted as well as bent, or a thin plate or shell is deformed in a finite manner, the solution of the problem pre- sents difficulties of a rather formidable character. 4, Whenever the deformation is finite, the displacements of a point on the middle surface are not small quantities whose squares and higher powers may be neglected, and therefore it is useless to attempt to express the stresses in terms of these quantities; but since any deformation involves a change in the values of certain geometrical quantities, such as the cur- vature and torsion of certain lines drawn on the middle surface, the most appropriate course to pursue would be to endeavour to express the stresses in terms of such geometrical quantities. There is one class of problems which can often be solved without much difficulty, which occurs when a plane surface is bent without extension into a developable surface ; or when a developable surface is bent into a plane, or into some other developable surface such that the lines of curvature on the old surface are lines of curvature on the deformed surface. This method can generally be applied when a plane plate is bent into a conical or cylindrical surface ; but it could not be applied in the case.of a right circular cone which is bent into a cone whose lines of curvature are not identical with those of the former cone. The success of this method, in cases where it can be applied, depends upon the circumstance that the flexural couples Gy, * See Proc. Lond. Math. Soc. vol. xxiii. p. 105. es Bending of Thin Shells. 499 G, can be expressed in terms of the changes of curvature, and also that in the special cases alluded to a sufficient number of the ten stresses are zero to enable the remainder to be determined by means of the general equations of equi- librium. 5. We shall now determine these couples, using Thomson and Tait’s notation for stresses and elastic constants, and Love’s notation for strains. Fie o Let O A, OB be two lines of curvature on ‘ the middle surface of the undeformed shell ; O,, O, the centres of principal curvature ; let oa, ob be the curves in which the planes OA O,, OBO, meet any layer of the shell. Let p,, p. be the principal radii of curvature at O, let Oo=7, and let 2h be the thickness of the shell. Also let accented letters denote the strained positions of the various points. If P denote the traction along oa, and R the normal traction along Oo, P=(m+n)o,+ (m—n) (a, +03) =%n{(1+H)o,+Ho,}+EHR,. . . . (1) where | EH=(m—n)/(m+n). Now __ dal —oa and ai ee OG ENS | SUI ee ne eee OA Times OW aa oe n' =(1 +43). Since we neglect the extension of the middle surface, O'A'=OA, whence Uh pee UPL =m (— ~) 4 1 1+%/p; P1 Pi Pi Tira! 1 n R =n ( et a + pi! | magn Mates) | e e (2) Similarly, ae seg yf RK 1 " a=n(o at pe! | men ~Blaite) f° e (3) The value of Gy is h G.=| Pains, la tetidiees @ (/(4) —h 500 Mr. A. B. Basset on the Finite Now, according to the fundamental hypothesis of my former papers it follows that, provided there is no eaternal pressure, R must be a quadratic function of h and n, and con- sequently the retention of R will lead on integration to terms in Ge» of a higher order than h?, which are to be neglected, since the solution we require is an approximate one which does not contain higher powers of h than the cube. Accordingly if we substitute the values of o,, a2 from (2) and (3) in (1), and the resulting value of P in (4) and integrate, we shall obtain | = 4 3 f = a a (= as ~) : Similarly, h G)= =) Qn dn, —h which gives an oe ee (i 2 , a git {0+ (S ele ae ae Equations which are equivalent to (5) and (6) have been given by more than one writer on elasticity ; but attention has not always been called to the fact that they depend upon the express conditions that the surfaces of the shell are free normal pressures, and also that the extension of the middle surface may be neglected. When a plane plate is bent into a developable surface Pi=p,=; also one of the quantities p,', or ps! (say pe’) is infinite ; whence (5) and (6) become Gy= $nl3(1-+E) /p/! > Gy = —$nh*H/p,' } where G, is the couple about a generating line of the develop- able. Since the extension of the middle surface is neglected, equations (5) and (6) would not apply to the case of a plane plate deformed into a surface such as a portion of a sphere. 7. Asan example of the preceding method, we shall con- sider the case of a plane plate of thickness 2h, which is bounded by two radii CA, CD, and two ares OB, AD of concentric circles ; and we shall inquire whether it is possible to bend this plate into a portion of a right circular cone in ~ which OA, BD are generators, and OB, AD are circular sections. We shall assume for trial that the bending may be effected by means of tensions, normal shearing stresses, and flexural Bending of Thin Shells. 001 couples applied to the edges ; so that the tangential shearing stresses and the torsional couples are zero. Fig. 3. o) B D Let « be the semi-vertical angle of the cone, r the distance of any point on OADB from ©, Then pi =p =; p2=0; p/=r tana; whence | G,=4nh? Hr! cota, Gy = —$nh3(1+ B)r— cota. The equations of equilibrium are d qn (hit) T=, a) dT, as, +N,cos a=0, d dN q,p Nz") sin «+ oat —T.,cosa=0, > (8) dG, AE + Ny sine=0, d £ (Gor) —Nor + Gy=0. | Let 4nh3 (1 + E) cota=h, then Ci. —k/r, whence No=—hk/r*, N,=0, whence T,=4& tan a/72, and therefore A ktane h= fie ee , ? where A is the constant of integration. From these equations we see that all the stresses are per- 502 Prof. Angstrém on the Intensity of fectly determinate except T,. If CO=a, CA=8, and T,, To denote the tensions along OB, AD, we have 7 A ktan @ | Za ae : PA hime (? + | al eee) Cee: ae from which it appears that either T, or T, may, if we please, be made zero, provided the other be properly determined. The above results would also apply to a belt of a complete cone, bounded by two circular sections. LI. Bolometric Investigations on the Intensity of Radiation by Rarefied Gases under the Influence of Electric Discharge. By Kyvr Ayestrou*. ()* E of the peculiar difficulties attending the quantitative determination of the amount of energy radiated by gases in vacuum-tubes is the extreme feebleness of its intensity. In his recent work in this field, executed at the Hochschule at Stockholm, Prof. Angstrém attacked the problem by the bolometric method, which, although leaving something to be desired as regards sensitiveness, led to some important results. Another obstacle lay in the well-known difficulty of obtaining the gases in a state of such purity that the spectrum exhibited by the discharge through them in a vacuum-tube showed no foreign admixture, such as the carbon-bands seen whenever grease is used for joining surfaces, or where the flame touches in the process of soldering. The discharge-tube used for the most careful experiments was thoroughly cleaned after soldering-in two electrometer- terminals, and attaching two short lengths of tubing at right angles near each end. The latter were to receive the elec- trodes, whose construction required particular care. Into a short capillary tube a piece of platinum wire was introduced from one end and a piece of thoroughly cleaned aluminium wire from the other. The tube was then heated so as to form an air-tight junction between the two wires, and was then fitted into a glass plate. After removing all grease the tube covering the aluminium wire was cut off, so that the latter acted as a perfectly clean electrode, and the glass plate hold- ing it was fitted on to the short tube attached to the discharge- * Abstract from Wiedemann’s Annalen, No. 3, 1893, by E. E. Fournier d’Albe, B.Sc., Royal College of Science. Radiation by Rarefied Gases. 503 tube. The joints were made air-tight by means of sodium silicate, which proved to be a highly useful cement, and did not give rise to any impurities. Short lengths of tubing containing mercury were placed round the platinum wires to convey the current to the electrodes. The behaviour of four gases only was investigated, viz. hydrogen, oxygen, nitrogen, and carbonic oxide. Hydrogen and oxygen were prepared by electrolysis of pure newly- distilled water acidulated with phosphoric acid. The nitrogen was obtained by passing pure air over heated copper-turnings reduced by hydrogen. Carbonic oxide was prepared by the reaction of sulphuric and oxalic acids, and purified by passing through caustic potash. In producing these gases all rubber tubes were dispensed with, and the different parts of the generating apparatus were soldered together. The discharge-tube was connected through a Kundt glass spring and a set of cleaning-tubes to the tube used for intro- ducing the gas, a mercury-valve, and the air-pump. © The mercury-valve consisted of a U-tube communicating at the bottom with a long tube full of mercury. By varying the level of the mercury by means of a reservoir the valve could be opened and closed. The tube for introducing the gases corresponded in the main to Cornu’s arrangement. A vertical glass tube is filled with mercury whose level can be varied by means of a reservoir connected through a flexible tube, as in the case of the mercury-valve. At a point some distance from the bottom is attached a capillary U-tube, the end of which, in the process of filling, is introduced into a small reservoir containing the gas. Lowering the mercury esta- blishes a connexion with the discharge-tube through the drying-tubes, and on raising the level the gas is shut off from the atmosphere. | The current was furnished by a battery of 800 small Planté accumulators, regulated by means of a liquid resistance con- sisting of cadmium iodide dissolved in amyl alcohol, and measured by a dead-beat reflecting-galvanometer. The fall of potential in the discharge-tube was measured by a Mascart quadrant-electrometer. The bolometer used for the experiments consisted of two gratings cut out of tinfoil mounted in ebonite frames. These frames were placed one behind the other in a tube with double walls, the posterior one being protected from radiation by a small double screen. Four diaphragms were mounted in the tube in front of the gratings, to diminish air-currents. The grating absorbing the radiation occupied a circular space of 16 millim. diameter. It was blackened by precipitated 504 Prof. Angstrém on the Intensity of platinum and smoke. The four branches of the Wheatstone- bridge arrangement, of which the gratings formed two, had each a resistance of about 5 ohms. In order to be able to rapidly test the sensitiveness of the combination, a constant resistance was introduced as a secondary circuit into one of the branches. The opening or closing of this circuit usually made a difference of 75 scale-divisions. If not, the reading was reduced to that standard sensitiveness. The bolometer was separated from the end of the discharge- tube by a double screen with a perforation, inside which was suspended a small screen. This was quickly pulled up to expose the bolometer. The strength of current through the discharge-tube was measured by the galvanometer, the diffe- rence of potential within it by the electrometer, and the deflexion of the galvanometer in the bolometer circuit was read from minute to minute. ‘The latter gradually increased, owing to the warming of the walls of the discharge-tube. By suddenly breaking the current and again observing the bolometer the radiation of the tube-walls was eliminated. Another method of elimination was by interposing a plate of alum about 4 millim. thick, which totally absorbed the radia- tion from the glass. Another source of error was the reflexion from the walls of the tube. The end of the tube opposite the bolometer was closed by a plane-parallel plate of rock-salt. This occasioned a loss by reflexion, whereas the other surfaces entailed a gain. Both were corrected by introducing a small copper box heated by steam circulation into a tube of the same construction as the discharge-tube, observing the bolometer deflexions, and repeating with the box alone. Prof. Angstrém states his main results as follows :— 1. For a given gas and a given pressure the radiation of the positive light is proportional to the intensity of the electric current. 2. For a given gas and pressure the composition of the radiation is constant and independent of the strength of current. 3. On increasing the pressure of the gas, the total radiation for a given strength of current increases as a rule, slowly at low, more rapidly at high pressures. At the same time the composition of the radiation changes, inasmuch as the ratio of the intensity of the shorter waves to the total radiation decreases. Thus the distribution of the intensity in the spectrum changes in such a manner that with diminishing pressure the intensity of radiation increases for the shorter wave-lengths. 4, The ratio between the intensity of total radiation and Radiation by Rarefied Gases. 505 the current-work increases continuously with diminishing pressure of gas. 5. The useful optical effect of the radiation (here given by the ratio of the intensities of the radiation passing through the alum plate and the total radiation respectively) is very high for some of the gases at low pressure (about 90 per cent. for nitrogen). But the useful optical effect of the work spent is not very great (about 8 per cent. for nitrogen of 0-1 millim. pressure). 6. The intensity of total radiation must be considered as a secondary effect of the discharge, and depends upon the mole- cular constitution of the gas. 7. Whatever views we hold concerning the nature of the gaseous discharge, this investigation appears to confirm the hypothesis of Hittorf, E. Wiedemann, and others, that the radiation is not a pure function of the temperature of the gases, but must be regarded as anomalous (“ irregular,” “* luminescence ”’), If we call “irregular” a radiation in which the spectro- scopic distribution of the energy is anomalous, there are certain facts observed by Prof. Angstrém which lead to the conclusion that the radiation in question is irregular. The radiation did not show any relation to the absorptive power of the gas at ordinary temperatures. Again, the radiation,— which in nitrogen at 2 millim. pressure is still rich in dark rays,—rapidly changes in quality when the pressure de- creases, and at 1 millim. consists almost exclusively of light radiation. Prof. Angstrém supposes that the radiation of the gas during electric discharge consists of two parts, one of them regular, the other irregular. With decreasing pressure the former decreases, whilst the irregular radiation increases in proportion as the motions are less obstructed by the mass of the gas. At constant pressure a certain portion of the energy in each molecule is converted into radiation ; as the strength of the current increases, the number of active molecules, and hence also the radiation, increases in the same proportion as the current. The number of active molecules being relatively small, the damping effect of the rest may be taken as constant, and the composition of the radiation remains practically unaltered as the current increases. On increasing the pres- sure, however, the damping effect changes, the anomalous dispersion is more easily transfermed into a normal one, and the radiation becomes richer in infra-red rays. A greater proportion of the energy supplied is spent in heating, and for the same current-work the total radiation decreases with increasing pressure. Phil. Mag. 8. 5. Vol. 35. No. 217. June 1893. 2N 506 Mr. E. C. Rimington on Luminous But in view of the difficulties of the investigation, the paucity of available material, and the approximate nature of the results in this almost unexplored field, no final decision can as yet be arrived at. A tabulation and a graphic repre- sentation of the results, with diagrams of the apparatus and a full discussion of methods and corrections, will be found in the original paper. LIT. Luminous Discharges in Electrodeless Vacuum-Tubes. By HE. C. Rimineron*. See reading a paper in conjunction with Mr. E. W. Smith on November 25th, 1892, before this Society, on “ Experiments in Electric and Magnetic Fields, Constant and Varying,” the Author’s attention has been drawn to a paper contributed by Mr. Tesla to the ‘ Hlectrical Hngineer’ of New York, July 1st, 1891, in which the luminous ring- shaped discharge obtained when a Leyden jar is discharged through a coil of wire surrounding an exhausted bulb is attributed to the electrostatic action of the surrounding wire, and not to the electric stress set up in the rarefied dielectric in consequence of the rapidly oscillating magnetic induction through the bulb. As one experimental proof of this assertion Mr. Tesla gives the following experiment :—“ An ordinary lamp-bulb was surrounded by one or two turns of thick copper wire, and a luminous circle excited by discharging the jar through this primary. The lamp-bulb was provided with a tinfoil coating on the side opposite to the primary, and each time the tinfoil coating was connected to the ground, or to a large object, the luminosity of the circle was considerably increased.”’ The author repeated this experi- ment with two Leyden jars arranged as in fig. 1, and found that when the spark-gap was sufficiently large to produce a bright ring when the tin- foil was not connected to earth, doing so produced no noticeable difference in the brilliancy ; but that, if the discharge were faint, it was ren- rendered considerably brighter on making the earth connexion. Better results were, however, obtained on * Communicated by the Physical Society: read April 28, 1893. + Ante, p. 98. yy Bie Discharges in Electrodeless Vacuum- Tubes. WENO connecting the tinfoil to either of the outside coatings, A or B, of the jars instead of to earth. This result led the author to try a series of experiments to endeavour to determine the cause of the effect, of which the typical ones are here given. Hzperiment 1 (videfig. 2). A Fig. 2. S and B are the outside coatings of a pair of Leyden jars (those employed were about pint size). Cand D two vertical and paral- lel metal plates, at a distance of about one foot from the jars. The spark-gap, 8, is adjusted by a screw, so that the spark-length can be varied by small amounts when necessary. A single turn of wire, a , encloses an exhausted bulb, and its ends are connected to A and B, as shown in the figure, so that a the part nearest to C is connected to A, and 6 to B. Two loose wires, e and /, are also connected to A and B. The spark-gap is now shortened until there is just no luminous ring in the bulb. The plates C and D are then connected to the outer coatings A and B by means of the two loose wires, with the following results :— (1) Ato C. Bright ring. (2) Bto D. Bright ring. (3) A to C and B to D simultaneously. Bright ring. (4) A to D. ; : (5) B to ©. ; No luminous ring. (6) A to D and B to C. Expt. 2.—The wire turn ab is removed from the bulb, given a half twist, and then replaced ; so that a is now nearest to D, and 6 to C. Plates not connected, no luminous ring. (1) Ato C. (2) B to D. fs luminous ring. (3) A to C and B to D. (4) A to D. (5) B to C. trig ring. (6) A to D and B to C. Hapt. 3.—Arranged as in Expt. 1, case (1) or (2). Cis then connected to D, and the ring becomes less bright. Expt. 4.—Arranged as in Expt. 1, case (1). © and D 2N 2 ee a ma WS PT ee OY oa jae x EE ate ok 2. = es aso ~ 508 Mr. E. C. Rimington on Luminous connected. On approaching C to the bulb, ring becomes brighter. On approaching D less bright. If arranged as Expt. 1, case (2), the reverse happens. All the above four experiments give the same effects if the turn of wire be larger than the bulb, as in fig. 3, only a longer spark-gap has to be used. Eept. 5—A single turn of wire (fig. 3), a 6, larger than the bulbis employed, and between the bulb and the ring a semicir- cular strip of tinfoil or metal T is placed. The wire is connected as in Expt. 1. The spark-gap is arranged to give no ring. Con- necting T to B bright ring, T to Anoring. The reverse hap- pens if the tinfoil is placed in position T’ as shown by the dotted line. Haupt. 6.—A piece of gutta- percha covered wire is bent into shapes shown in figs. 4 and 5. On placing either of these over bulb as in fig. 6, a figure of eight-shaped luminous Fig. 38. Fig. 4. Z 6 h c discharge is obtained, and there is no noticeable difference between the two. Fig. 5. 7 6 h c Expt. 7—Putting the wire (fig. 4) on bulb as in fig. 7, a Discharges in Electrodeless Vacuum- Tubes. 509 single broad band-ring is obtained, as the two turns will help one another with respect to magnetizing effect. Doing the same with the wire (fig. 5) a discharge is obtained shaped like the sector of an orange, as shown by the dotted lines, fig. 7. Fig. 6. Fig. 7. Expt. 8.—Bending a wire as shown in fig. 8, and placing a bulb in the loop 6 ¢, there is no effect even with a long spark- gap, although the potential difference between the sides Fig. 8. cand } would be much greater than in the case of a single turn. Putting a bulb in the loop, be, of fig. 4 at once gives a bright ring. a 510 Mr. Ki. C. Rimington on Luminous Hxperiments 6, 7, and 8 seem to show that ring, or other shaped, sharp luminous discharges can only be obtained with the wire so wound as to give magnetic induction through the bulb, while the first five experiments show that an electro- static field in the bulb may help the effect. ‘The theory the author has come to after consideration of the above and other experiments is:—That if the H.M.F. due to rate of change of magnetic induction acting in the dielectric of rarefied gas be insufficient to break it down and produce a luminous discharge (owing to the spark-gap being too short), the electrostatic field between the plates C and D, or between one of the plates and part of the wire, if correctly timed with respect to the rate of change of current in the wire, will commence the breakdown of the gas, thus allowing a less H.M.F. due to the magnetic induction to complete it. To put this to the test, a single turn of wire was put round a bulb and the spark-gap adjusted so as to give a very faint or no luminous ring ; on the top of the bulb was laid a piece of tinfoil connected to one pole of a + in. spark induction- coil ; when the coil is worked the tube is filled with a faint glow: if now the Leyden jars are charged and discharged there will be sometimes a ring in the bulb which will be occasionally quite bright. The reason it cannot be always bright is of course that the discharges of the induction-coil are periodic, as are also those of the jars, and it is only when the two are properly timed (i.e. the P.D. due to the coil coming either just before or simultaneously with the spark) that there will be a bright ring. This experiment seems to settle the question and show conclusively that a properly timed electric stress in the bulb due to an electrostatic field will allow an E.M.F. due to the alternating current in the wire to produce a breakdown of the rarefied gas, which the latter is too small to effect without the aid of the former™*. In Expt. 1, when A and C are connected this field will exist between © and 0 the side of the turn of wire remote from C, and must therefore pass through the bulb. When A * To prevent misconception, it had better be definitely stated that this electrostatic stress does not necessarily act in the same direction as the E.M.F. due to the rate of change of magnetic induction. In experiments (1) to (5) the direction of the former will be through the bulb from side to side, while that of the latter is a circle coplanar with the wire. As the discharge in a gas is of a nature more or less electrolytic, being accompanied by the splitting up of the molecules, it seems reasonable to suppose that anything which increases the number of dissociated molecules will enable a smaller stress to produce a breakdown in the form of a luminous discharge. Discharges in EHlectrodeless Vacuum- Tubes. bit is connected to D, as the strongest field is between 6 and D, where thé P.D. is greatest, it does not pass through the bulb ; in fact the field in the bulb willsimply be that due to the P.D. between a and 0, or the same as it is if the wires e and / are disconnected. ‘The results of Experiments 2, 3, 4, and 5 are also obviously explained by this theory. To treat the subject mathematically. We have the well- known equations for the discharge of a condenser : Lo +Re=- = where K is the capacity, and Pa dq dt Combining these, &q , Rdg 1 see, © Kid To obtain an oscillatory discharge 4L must be greater than Oe Putting a for == and b for ee emo 5 the solution ig pee wees oa ee where @ =eun'| ~-) and @ is the initial charge. This may be more conveniently written p= Qe EFF os un, where ay) or tang=—+ = _ KR ae) eee 4L—KR* Eas i oe If the oscillations are to be rapid, RP must be large compared 4 R2 to 42 Therefore 7 will be some small angle. Instead of quantity we may write P.D. of the condenser, or ares) 5 Vee Va +P cos (e—n). ig ogee} i oe 512 Mr. E. C. Rimington on Luminous The current C= dq — Q — ~p ae biG Ol Now the electric stress acting in the bulb is proportional to et sin bt= asindt.. . . (3) de the rate of change of current, or to — ; “ile and Oe TING Gi OS ——— Ss bt). scare C2 ee (asin bt + 6 cos Jt) (4) The current itself will be a maximum or minimum when de fe ioe 3 ?,é. when asin bt+b cos bt=0, : or when a eee — Als tae : a KR? Therefore l¢=0, and is in general nearly equal tol 5 The maximum values of the current occur when bi=0, 27+0, 474+, &e., and the minimum values when bt=7r+6, 3874+0, 57+4+8, Ke. This is shown in the curve (fig. 9), the points M,, M., M3, &c., representing the maximum and minimum values of the . 7 current. The distance O A represents 0, and A B= °) =P 9 It is now necessary to consider when the rate of change of . ae A the current is greatest. Ai will be a maximum or minimum C4 2 when ne —(), dt? Now iE V + he a = ope (a? —L*) sin bt + 2ab cos bt} = 0. Hence | in a = 2. 2 RY Ka Sg on 2L—-KR? Let 2L—KIi? y will be in general a small angle. Discharges in Electrodeless Vacuum- Tubes. 513 The rate of change of current will be greatest (either a maxi- mum or a minimum) when bt=—y, w—-y, 27—y, Ke. Obviously 0¢ cannot equal —y, so that the rate of change of current is greatest for values 7—y, 27—y, d&c.; or at points “44, M2, #3, &e. in the curve (fig. 9), and HF=y. If Fig. 9. R ty, Dotted curves are values of the exponential 77 ° 21 é = Sc Se Z e YA LUES OF CURRENT M,, M,, M;, M, are the maximum values of the current. p,, m2, us are the points where the rate of change of current is greatest. the oscillations are to be very rapid KI? must be negligible compared to 4L ; in which case tan y= He tan yn = Wo we also he! Mr. E. C. Rimington on Luminous and they are both very-small angles, hence y=2” approxi- mately, or HEF =2AB. When bt=7—y, Ue == ie de vy e fy 25 we 6 or if the oscillations are very rapid, de = eB ye pee If, however, ¢=0, re Cpe NU: so that the greatest rate of change of current occurs at the first instant of discharge, although this is not a mathematical maximum. HKiquation (4) may also be written de _ V Ve+E dt bL n being the same angle as before. It is now necessary to consider the values of the P.D. between the outside coatings A and B of the Leyden jars. Let / and r be the inductance and resistance of the coil connected to the outer coatings, and L and R the same for the whole circuit. Let v,—v,=« be the P.D. bevmeen the outer coatings at any instant t. Then e cos (bt-+9); ae) Vice c= e@ sin bt, bL and 2=0,—v. er +1, dt Ve, : ware {(r+la) sin bt + lb cos bt} Vee Dy Oey Seay Ea I =a, V Pb +(r+ la)? cos (bial) ee where ” ae tan 7! = ! USER PGD 7! will be in general a small angle not very different from ; Discharges in Electrodeless Vacuwm-Tubes. 515 and if : = nor the time-constant of the coil equals the time- constant of the whole circuit, ; =~ =—2a, a ., tang = j = tan n, or y' =n. That is # is in phase with v the P.D. at the inner coatings of the jars. To find the maxima and minima of x we have ee: ae [ {ar + l(a? —b7)} sin bt+ b(r + 2la) cos bt] =0. ut b(r + 2la) a tame = ar+Ua2—2) _ (rL—Rl) VK(4L—KR) S L(KRr +21) = tano. Then « has its greatest positive or negative values when bi=5, +8, 27+56, Kc. Sis in general a small angle, and is positive if L l ane and negative if he (Pers If eae ; ar ae 60; If = be not greater than : the first largest value of a will occur at t=0, and as the rate of change of current is also greatest at this instant the two will occur simultaneously. The next greatest value of 2 occurs when pees (itz 2 -), th and the next greatest rate of change of current when bt=7 —¥. Sa a ee 516 Mr. KH. C. Rimington on Luminous 6 will be less than y, if be nearly equal to so that the de dt’ but the value of z will not differ very much from its maximum maximum value of x will occur after the maximum of de . ; ; : when a is A maximum®*. This bears out the results obtained in experiments 1 and 2, though, of course, the electric field in the bulb will be that due to the P.D. between one of the plates, C or D, and the opposite side of the turn of wire, and this will only be about half that between the outer coatings A and B. Moreover, the phase of the potential of C will not be quite the same as that of A, on account of the inductance of the connecting wire e. Experiments 1 and 2 were, however, tried with the plates C and D, and the con- necting wires removed, the turn of wire ab being moved so as to bring either a or b nearest to A or to B, and the results obtained were practically the same as those of experiments 1 and 2. Effect of Size of Surs. When different-sized Leyden jars are employed with the same length of spark-gap the luminous ring is more brilliant * The above investigation into the value of the P.D. between the outer coatings will only give correctly the state of things when a steady swing has been set up in the circuit; as evidently when ¢=0 the value of w also equals zero, so that 2 must start in phase with the current; it will, however, rapidly get out of phase with the latter, and finally be nearly in quadrature with it, This is due to an initial wave starting from the spark-gap which runs round the circuit. Possibly the value of x can be empirically represented by one of the two subjoined formule :-— AEN emerge £= VPP (tla)? sin {(bt-+p)(1—e-P4)t, Ne Veat = : * w= Ty NPG (r-Hla)? sin {Bt + y (1—e-Pe)}, = where P= = —yn', and p some constant. Dr. Lodge, in his researches on the A'and B sparks, approximately represents the initial values of 2 by the current multiplied by the impedance of the conductor 7, or makes Veut t= — (?b?-+r* sin bt. The initial maximum of z will consequently roughly coincide with the maximum of the current, or be near the point M, of fig. 9, and will thus come about a quarter of a period before the second maximum rate of change of current, point p, (fig. 9). Discharges in Electrodeless Vacuum- Tubes. Dali with larger jars. Now the E.M.F, acting in the rarefied gas, and producing the breakdown of the same, is proportional to de di’ Also the greatest value of de ta first occurs is when ¢=0, dt and then de V a yk and the next is for very rapid oscillations VS as Ai = ey 2 Ibg So that the first value of the E.M.F. acting in the gas is independent of the capacity, and the next and succeeding values are less the greater the capacity. The effect on the eye, however, of the luminous ring will be the time-integral of the discharge or approximately depend on | The whole limits of ¢, viz., from 0 to «©, cannot be taken at once, as < keeps reversing, and this reversal will not affect the luminous discharge. Referring to the curve (fig. 9) it will be seen that the first reversal must take place at M,, when bt=80, and subsequent ones for values 7 +0, 277+ 0, KXc., of bt. It is therefore necessary to take first the limits 6 and 0, then a+6 and 6; 27+0 and r+40, and so on, alternately writing the integrals plus and minus. * de =e We eae “t sin Ot | \ a = aL le sin b¢ | le sin bt 2r+0 + ee sin ot | — &e.ad inf. : 7+ Remembering that sin ( 7+0)=—sin 0, sin (27+0)= sin @, sin (37 + 0) = —sin 9, and so on, 518 Mr. E. C. Rimington on Luminous this gives ” de ae a) Gero) © (On + 6) i, a = zy, sine Ga + e2 +e6 +e. \, The series in the bracket is a geometrical progression, in a which the constant factor is e@"; and, since a is negative, this is less than unity. Hence “6 * dc Gps 2V sin 0 eb nade 6L 7 and tan 0= ee oie or sin@= We KR’, also 4L—KR sin @ — — 4/7 kale e tenner age re) => 46 { eo = 2V oe aad » at a 1—e RY ee) = eV W—=KR?—e J 4L—KR? et Ogg Sa _=eand ra /_KRE_ = 4L— — 41,--KR? Then the denominator =e*—e?-9, and ealtet 5 + 3 ea 2ay y? 3u7y ig omer ih ia oa B - + &e., . 2xy eo 3n*y __ 3ay? y oot tt ee. 38> + terms of the 4th, 5th, &. powers. Discharges in Electrodeless Vacuum- Tubes. 519 Now wz and y will in general be small fractions, since KR? is usually much less than 4L. If the oscillations are very rapid, @ is very nearly equal to y Hence y=2x approximately. Then e’—e*’ becomes 9a ig 6 = 2a (1 ae =) approx. Therefore the time-integral ) ap prox., av4/8 = 4/*(1- =) ~ 2e(14 ©) =) e and c= ty / KR? aoe Ee sien meoN/ (bk 4 eke so time-inte or approx. mw RK au (I~ “55, Now from this it is seen that the effect of increasing the capacity would be to slightly diminish the time-integral, and consequently probably make the brillianey of the laminous discharge less, if it were not that increasing the capacity diminishes the real resistance of the circuit, since it makes the oscillations slower, and the resistance R for copper for rapid oscillations approximately equals /46/ Ry; where / is the length of the wire, and R, its resistance for steady cur- approximately. rents. Now b= VEL - Therefore so that the time-integral is very roughly proportional to the fourth root of capacity. There is also another reason why larger jars might produce a brighter discharge, even though the ae integr al were less. With larger jars ines time foleen for the amplitude of the cur- rent to sink to a value at which it becomes insignificant will LR —— 520 Mr. E. C. Rimington on Luminous be longer than in the case of small ones. Now, as the initial value of 2 is the same whatever the size of the jars, the after values (although their time-integral is less and their actual values less also) last longer in the case of larger jars. When the breakdown of the dielectric of rarefied gas is once ees See de begun by the initial ai the values of 7 necessary to keep it up may probably be very much less, and consequently the smaller values of = lasting longer, as given by the larger jars, may produce a luminous discharge more brilliant to the eye than the larger values of = lasting a shorter time, as given by the smaller jars. The actual results obtained with a ring of four turns of wire containiny an exhausted bulb about 24 inches in diameter were that the differences in brilliancy, obtained by using half-gallon jars, pint jars, or very small jars made from spe- cimen glasses, were not so very great. Other Effects. Apparently unclosed Discharges. A closed luminous discharge is not the only one that can be obtained. Mr. Tesla, in 1891, pointed out that by wrap- ping a wire round an exhausted tube so as to form a coarse- pitched spiral, a luminous spiral discharge is obtained. He was apparently only able to obtain a very feebly luminous spiral, but the author has succeeded in getting one quite as brilliant as in the case of the ring-shaped discharge obtained, with a bulb. Fig. 10. In fig. 10 two half-gallon jars have their outer coatings connected by a wire, A B, bent as shown in the figure. Over J *~ Discharges in WB icopradeless Vacuum- Tubes. Sb DY -the wire is laid an exhausted tube, C, with a tinfoil cap*, T, at one end; T is connected to the outer coating of the jar nearest to it. The object of this is to utilize the electrostatic effect and make the tube more sensitive to breakdown by the electromagnetic one. When the jars discharge, a straight luminous band is observed in the tube directly over A B. If the tube C be now moved towards the jars, even by a very small amount, a closed circuit discharge will be obtained. _There is apparently, then, a tendency for the luminous dis- .charge to form a closed circuit whenever possible ; and it .seems probable that even when the discharge is apparently not closed, as in the case of the spiral or the straight line, _the electric stress acting in the rarefied gas takes the form of a closed circuit, but is only intense enough to produce sharp luminosity close to the wiret. To further test the ques- tion an unclosed ring tube was made, and when it was placed inside a coil of wire no trace of a single luminous band could be seent. A small glass tube was also bent so as to form a spiral of four turns, and exhausted. A wire following the spiral was attached to it, but this also gave no trace - of luminous discharge. Magnetic Kffects of Discharge. The ring discharge in a bulb or closed circular tube acts like a metallic circuit as far as magnetic effects are concerned. This may easily be shown by the following experiment. A coil of three or four turns of wire has a similar one wound with it to form a secondary ; the latter is connected to a third coil, in which is placed an exhausted bulb. The first ‘coil is connected to the outside coatings of the jars (fig. 1). ‘The spark-gap can be adjusted so that a fairly bright ring is * Tt is not always necessary to use this cap, as, if the exhaustion is high enough to give green phosphorescence of the glass, with the two half-gallon jars in series, the discharge can be obtained without the cap. With another tube of lower vacuum the author finds the cap necessary. + That is, the return part of the discharge is so diffused and feebly luminous as to easily pass unnoticed in comparison with the sharp and brilliant luminosity close over the conductor. The same applies to the spiral discharge, each turn of the spiral probably forming a closed circuit by itself. t On afterwards repeating this experiment the author obtained a dis- charge in parts of the tube, and with half-gallon jars in the whole tube. The discharge, however, was a closed one, as there were two distinct bands in the tube, one on the side next to the coil and the other on the side farthest away from it. This is what might be expected if the magnetic induction be sufficiently strong. Phil. Mag. 8. 5. Vol. 35. No. 217. June 1893. 20 LGPL TOC ATTEN IALTEOA E 522 Mr. E. C. Rimington on Luminous produced in the bulb. If now a second bulb is placed within the first coil a luminous ring will be formed in it, and the ring in the other bulb will be much weakened or altogether extinguished. Exactly the same effect is produced if a metal plate or closed coil be brought near the first coil in lieu of the bulb. Sensitive State of Discharge. If a single turn of insulated wire surround one of the exhausted bulbs as in fig. 1, and the spark-gap be adjusted so as to produce a rather faint luminous ring (the fainter the better); on approaching the finger and touching the wire at any point the discharge appears to be repelled, and takes the shape shown in fig. 11. Instead of touching the wire with the finger a small piece of tinfoil may Fel be laid between the wire and the bulb, Pen. as at A (fig. 11), and this may be touched by the finger or connected to any large object, insulated or otherwise ; the effect produced is the same. Connecting the tinfoil to one of the outer coatings of the jars does not produce this effect, and it is scarcely, if at all, visible when the luminous ring is brilliant, due to a longer spark-gap. With a wire ring of several turns the author has not been able to obtain it. If a turn of bare wire be employed the effect is produced when the finger is brought very near to the wire, but if it be brought into actual contact the effect is no longer visible. This apparently shows that it is due to the capacity between the finger or tinfoil and the wire; it is probably of the same nature as the “ sensitive state’ in an ordinary vacuum tube, ADDENDUM, May Ist, 1893. Since writing the above the author has made a further experiment* which at first sight appears to contradict the one{ given in the paragraph on ‘‘ Magnetic Effects of Dis- charge,”’ * Called hereafter the second experiment. shown when the paper was read. + Called hereafter the first experiment. This experiment was Discharges in Electrodeless Vacuum- Tubes. 523 A ring (R) of four turns of wire is joined in series with a single turn, and the two are connected to the outside coatings of the jars. In the single turn a bulb is placed and the spark- gap adjusted until a fairly bright ring is produced in it at every discharge. If now a closed ring of thick copper-wire, a metal plate, or a ring of several turns, similar to R, and with its ends joined, be laid on R to act as a secondary, the luminous ring in the bulb is brighter ; on substituting for this an exhausted bulb and placing it in R, there will be a brilliant ring-discharge in it, while the discharge in the other bulb will be rendered fainter or altogether extinguished. In this experiment the exhausted bulb secondary appears to act in the reverse way to a metallic secondary. The author then made the following experiments :— (a) A ring of four turns of guttapercha-covered wire pre- cisely similar to R was made, its ends were connected to an ordinary Geissler tube. When this was used as secondary it acted exactly in the same manner as the exhausted bulb both in the first and second experiments, the Geissler tube being brilliantly illuminated. (6) The Geissler tube was then removed, and the ends of the secondary coil connected to the coatings of a small Leyden jar. The effects produced by this secondary were the same as those produced by the exhausted bulb in both experiments. (c) The ends of the secondary were connected to the loops of a glow-lamp to act as a resistance (about 100 ohms). This acted similarly to the exhausted bulb in both experiments. (d) A disk of gilt paper (imitation) and also a ring of the same were used as secondaries; these acted similarly to the bulb in both experiments. When the discharge took place there were brilliant sparks produced at various spots on the paper, wherever there was any flaw in the gilding, showing that considerable energy was dissipated there. (e) The secondary coil of four turns had its ends joined by a strip of gilt paper about 6 inches in length, with a con- siderable number of flaws in the gilding (produced purposely, by bending the paper sharply in several places, so as to obtain considerable sparking). This acted similarly to the bulb and dimmed the discharge in the bulb surrounded by the single turn. On shortening the length of gilt paper between the ends of the secondary, the discharge in the bulb was less dimmed. The results of these five experiments are, that any of tho above secondaries are able to reduce the mutual induction between the primary and secondary in the first experiment sufficiently to render faint or altogether extinguish the 202 FE ay ee BEL Se . +6 Te ALM aa OE + i LOE ICDL EN PIE PRED AP oem LS SN 524 Luminous Discharges in Electrodeless Vacuum- Tubes. discharge in the bulb, and act similarly to an exhausted bulb secondary. In the second experiment a low resistance se- condary behaves in the reverse manner to an exhausted bulb secondary, while (c) and (e) show that a high resistance put externally into the secondary circuit, and (d) that a secondary having a high resistance in itself, act in a similar manner to an exhausted bulb secondary. (6) shows that if the ends of the secondary be attached to a capacity it behaves like the bulb. ' The most probable explanation seems to be the following:— The amount of energy in the jars when charged is a fixed quantity for a given spark-gap; this energy will be mostly expended in the coil R and the single turn and bulb (the second experiment). If, now, we can make energy be ex- pended elsewhere, as in a secondary, we shall have diminished the energy received by the bulb, and this will in general dim it or altogether extinguish it. This will explain what happens when an exhausted bulb secondary is used ; also experiments (a), (c), (d), and (e). With regard to experiment (6), energy may have been expended in heating the glass of the jar on account of electric hysteresis. Moreover, this secondary did not dim the bulb so much as the others, but was found to be capable of improvement in this respect by including some resistance (in the shape of the glow-lamp or a strip of gilt paper) in its circuit. In the case of a low-resistance secondary the energy dissi- pated in it will be small, since its impedance will not be much lessened by its being of low resistance on account of the high frequency. This does not explain, however, why the dis- charge in the bulb is brighter when a low-resistance secondary is used*, A further experiment was then made. The coil R in the second experiment had a similar secondary 8 placed in it; this was connected 1c another similar coil T. The spark-gap was lengthened until a brilliant luminous ring was produced in a bulb placed in T. The bulb in A was then moved away from A until there was a very faint luminous ring init. On removing the bulb from Ta very slight brightening of the * Tnis energy explanation is probably not a complete one. Working out the frequency in the cases of no secondary, a secondary of four turns short-circuited, and the same with its ends joined through 100; the author finds that the damping-term is increased when either secondary is used, but more so with the 100 in circuit. The frequency is much the same with the 100 in circuit as when there is no secondary, but with the secondary short-circuited the frequency is about doubled. This may account for the increase in brightness of the discharge in the bulb. On the Psychrometer and Chemical Hygrometer. 525 _ faint ring of the bulb in A was observed. Instead of placing an exhausted bulb in T, a coil of four turns with its ends joined through 100 was laid on T, and the bulb in A adjusted A one turn; S, R, and T each four turns. to give a very faint ring; on removing the coil from T a decided brightening of the discharge in the bulb was observed. This experiment seems to show fairly conclusively that in- creasing the energy in the circuit of the secondary S dimi- nishes the brightness of the discharge in the bulb placed in A*. LIL. Comparative Experiments with the Dry- and Wet-Bulb Psychrometer and an improved Chemical Hygrometer. By M. 8. Pemsrey, W.A., WB., Radcliffe Travelling Fellow ; late Fell Hxhibitioner of Christ Church, Oxford. ne vom the Radcliffe Observatory, Oxford.) URING the late winter it seemed desirable to make a series of comparative experiments with the Dry- and Wet-Bulb Psychrometer and an improved Chemical Hygro- meter, in order to ascertain the accuracy of the results given by the Psychrometer for temperatures below the freezing- oint. : A series of comparative experiments, made by me in the summer of 1889, had shown that the amounts of moisture calculated from the psychrometric readings varied by +6 per cent. to —9d per cent.from the amounts actually found by the * Since writing the above the author finds that Prof. J. J. Thomson has observed the effects noticed in the second experiment, and gives an explanation practically identical with the above. + Communicated by Mr. E. J. Stone, #.R.S., Radcliffe Observer, 226 Mr. Pembrey on Comparative Haperiments chemical method. The mean difference, however, in the above series was insensible*. The Chemical Hygrometer employed in both series was that introduced by Dr. Haldane and the author f. The absorption-tubes were placed in a small wooden box with wire partitions to prevent them from knocking against each other. The entrance-tube, by which the air to be examined passed into the hygrometer, was fixed through a small perforation in a rubber partition covering a hole in the box. In this way any possibility of air being taken from the inside of the box was avoided. } The comparative experiments were made in the following manner. ‘The weighed absorption-tubes were placed in the shed containing the psychrometer about ten inches below the bulbs of the thermometers. The wet- and dry-bulbs were then read off; the absorption-tubes were connected by a long piece of rubber-tubing with the aspirator. Air was now drawn through the tubes at a rate of 1500 cub. centim. per minute, until about 11,500 cub. centim. of the air had been taken. Five readings of the temperature of the water and of the air in the aspirator were taken during each period of observation. When the aspiration was finished, the readings of the wet- and dry-bulbs were again taken, and the absorption- tubes disconnected and stoppered. The period of observation generally lasted about ten minutes. Simultaneous determinations with two chemical hygro- meters were made in the previous, but not in the present series of observations. In order, however, to check the com- pleteness of the absorption and any errors in weighing, a second pair of absorption-tubes was connected up with the first pair. The results for the psychrometer were calculated, not from my own readings, but from the mean of three other readings —one at the beginning, one at the middle, and one at the end of each period of aspiration. These readings were obtained from the continuous photographic record of the wet- and dry- bulbs taken at the Radcliffe Observatory. It is possible to read off this record to two minutes and to one-tenth of a degree Fahrenheit. The accuracy of the readings has been proved by years of use and comparison with eye-readings. In every case care was taken to have the wet-bulb properly moistened about a quarter of an hour before the observations. * Phil. Mag. April 1890, p. 314. | t ‘An Improved Method of Determining Moisture and Carbonic Acid in Air,” Haldane and Pembrey, Phil. Mag. April 1890. 527 with the Psychrometer and Chemical Hygrometer. TABLE I. CS i Ete Ee we NEE a eel Sle we > I OE Ses eR Re ee Weight of Time during which Gain in weight] Variation in |vapour calcu- ITE: Dry-bulb | Wet-bulb Experi- Dates air was aspirated eee ee of absorption- weight of test- lated from beat S : (mean of | (mean of ment. through absorption- a vial tubes, first [pair of absorp-|psychrometer von CHOATE three three tubes. Fe ees air. tion-tubes. | by Glaisher’s readings). | readings). P y method Tables. ; cub. centim. erm. erm. erm. per cent. wie 5 1.......| 8 Jan. 1893.| 2.26 — 2.31 p.m. 5,802 "0209 + -0002 0198 —5 311 29:0 Dette’ 3 10.15 -10.19% a.m. 5,630 "0154 +0002 ‘0164 +7 20°1 20:0 Sh actiocel| a2) A 10.43 -10.14 _,, 11,552 ‘0289 +:0003 0288 —0 20°0 196 Acces geal a59 3 10.41 -10.51 ,, 11,278 0303 +0001 0297 —2 21-0 20°5 Disnegsa|c0 iy 10.20 -10.29 __,, 11,358 ‘0445 +0001 0470 +5 30°7 29'9 Ooocee alloc 3 11.2% -11.12 _,, 11,396 0481 — ‘0002 0480 —0 30°9 30°4 The ss Sy 3 10.45 -10.54 ,, 11,174 0431 +0005 0427 —1 28°6 28:1 Sie sel 9) ” 11.213-11.83 _,, 11,202 0439 +0002 ‘0448 +2 28°5 28°2 Ot line, 5 10.14 -10.23 _,, 11,302 ‘0576 — ‘0002 "0589 +2 341 33'8 WO ecesat |e ‘5 10.45 -10.54_,, 11,320 ‘0587 +0003 0583 —0 343 33°9 Acc ag LO. ‘5 10°7 -10.16 ,, 11,370 "0574. + 0004 0575 +0 347 34:2 Dees texe saelis9 ) 10.39 -10.48 __,, 11,410 0578 +:0001 ‘0603 +4 352 347 WSs coxcae( LL i 10.14 -10.23 _,, 11,428 0481 +0002 0476 —1 32'3 30°9 Lee NET at 528 Mr. Pembrey on Comparative Experiments The aspirator used was that described in the paper pre- viously mentioned*. The aspirating-bottles were covered with felt, so that the temperature of the water generally varied only a tenth or two.of a degree Centigrade, never more than half a degree, during the period of observation. The volume of air aspirated has always been corrected for temperature, aqueous vapour, and barometric height. In calculating the tension of aqueous vapour from the chemical determinations the table given by Shawf has proved very valuable. The preceding Table (I.) shows that the amounts of moisture calculated from the psychrometric readings by Glaisher’s Tables vary, when compared with the gravimetric determina- tions, from —5 per cent. to +7 per cent. The mean, how- ever, is ‘0430 to ‘0426 grm., or less than +1 per cent. for the psychrometer. The tensions given by the chemical determinations have been calculated, and are compared in Table II. with those obtained from the psychrometer by means of Glaisher’s, Haeghens’, Guyot’s, and Wild’s tables. Nae tree Ee Psychrometer. Experiment Chemical 9 ‘| method. Glaisher. | Haeghens.| Guyot. Wild. millim. millim. millim. millim. millim. | a eee 3°45 3°20 3°44 3°45 3°47 De there i. 2-60 2-67 2°73 ORD a ee Desctiowec way 2-49 2°36 2:58 2°56 2 7 a oe Sie 2°56 2°36 2-70 2:64 26 De Mee ose acres a1 3°83 4:01 3°98 3:93 2 Giraieseccu net 4-03 4:06 4°20 4-16 AT Tae ae = Be 3°70 3°63 3°80 3°78 S48 eee 3°75 378 3°84 ool 3°83 es iin 2 4-87 4-85 4-84 4-82 4°83 MOR aerate at 4°95 4°85 4-84 4:82 | 4:80 1B sey Se Se ae 4°85 4-87 4°86 4-82 4°80. DA Sees ee 4°86 4-98 4-97 4:92 5°00 WS ates ae 4°05 3°86 4°23 3°96 | 4°17 WMisanves. cone: 3°84 3°80 3°93 3°88 | 3°89 In order to make this paper more complete, the cor- responding tables of the previous experiments are here reproduced. * Phil. Mag, April 1890, p. 309. tT On Hygrometric Methods,” Phil. Trans. 1888, A. ~~ 529 with the Psychrometer and Chemical Hygrometer. e . e CONDAAA Fw DH oh a Date. ites a om her We a 20 Le Za 5; 5 Aug. 1889. Ot al % oy Des cham * The rubber of one of the stoppers 16 July 1889. ‘TasueE EID, Time during which air was aspirated. 11.39-11.48 a.m. 11.39-11.45 a.m. 11.10-11.16 a.m. 11.6 -11.12 a.m. 11.45-11.52 12.13-12.16 p.m. 11.52-11.58 a.m. 11.48-11.54 a.m. 11.21-11.27 a.m. WO) SIDIEAG/ AN 11.24-11,80 aa. 1L.é 52-11. 39 A.M. Corrected volume of air aspirated through each pair. cub. centim. 07123 5722 5723 5780 5681 5732 5707 5709 5756 5776 5731 5755 Gain in weight of pair I, determina- tion A. 0510 ‘0575 ‘0678 ‘0583 { Gain in weight of pair 2, determina- tion B. erm. ‘0430* 0524 0512 0508 ‘0610 0435 ‘0687 ‘0564 0510 ‘0572 ‘0675 0585 Weight of vapour caleu- lated from readings of psychrometer by Glaisher’s Tables, 7th ed. erm Percent- age diffe- rence of pyschro- meter over chemical method. per cent. 0450 0552 0520 0519 ‘0600 (0452 0668 0548 0495 0552 0678 0553 +54 Dry- bulb (mean of 3 read- ings). pike 61:6 58'3 61:3 63°7 d7°9 61:5 65°6 625 63:0 64:1 61:0 64:6 Wet- bulb (mean of 3 read- ings). Variations of test pair 3, showing that carrying the tubes about introduced no error of weighing. grm. +0001 +0002 — ‘0002 +0002 +0003 — ‘0002 — 0003 +0000 +0002 +-0001 +0002 — 0001 was found to be split on reaching the Observatory, and bei accounts for sire slight excess in weight of this pair of tubes, ’ 530 On the Psychrometer and Chemical Hygrometer. TaBeE LV. Psychrometer. | ; Chemical | Experiment. | method. Glaisher. | Haeghens.| Guyot. | Wild. | nee Le | as ee. | millim. millim. millim. millim. millim. | eee ae ae 743 776 737 731 74 Bias ae hc 3 915 9°55 9 54 9°51 9°5 Ou, de acueee 8:99 9-00 8:88 8°87 89 a a 8-78 8:99 8°74 877 88 Dg ceeeencee 10°70 10°72 10°75 10°76 10:7 Coit 7:63 778 739 7:34 74 Les desea 12°15 11-72 11°78 11-80 Grd co eer on 9-91 965 9:57 9°57 96 OS ae enes 8-90 8:68 8°45 8:43 85 LON eee 10:00 9°52 9°38 9°41 94 | Da eae 11°82 11°84 11:93 11:93 1 eS ae LAR sa ee 10:23 9°67 S95 9°57 9°5 pe hee ee ih | ee a Means: 9-64 SRD 9°44 9°44 9°44 Regnault*, during his comparative experiments with the _ psychrometer and his chemical hygrometer, made a series of determinations in which the temperature of the air was below the freezing-point. The experiments were made in December 1846 and January 1847. The lowest temperatures during the sixteen determinations were —6°°89 C. for the dry-bulb and —7°:74 for the wet-bulb ; the highest —0°13 and —0%69 respectively. The chemical determination lasted from three- quarters of an hour to one hour ; readings of the psychrometer were taken every five minutes. 7 The results showed variations of the psychrometer over the chemical method ranging from +11 per cent. to —3 per cent., the mean being about +4 per cent. In conclusion | must express my hearty thanks to Mr. Stone, the Radcliffe Observer, who has given me every facility to make these and the previous experiments, and has always aided me with his advice. I must also thank his assistants, Messrs. Wickham, Robinson, and Maclean. * Annales de Chimie et de Physique, t. xxxvii. 1853, p. 274. sel | LIV. Water as a Catalyst. By R. E. Hucuss, B.A., B.Sc., F.CS., late Scholar of Jesus College, Oxford, Natural Science Master, Eastbourne College *. Ss further chemical changes have been investigated, and the influence of the absence or presence of water on the progress of the change has been determined. Last year the author showed (Phil. Mag. xxxilil. p. 471) that dried hydrogen-sulphide gas has no action on the dried salts of lead, cadmium, arsenic, &c.; and, in conjunction with Mr. F. Wilson, it was shown that dried hydrogen-chloride gas is without action on calcium or barium carbonates (Phil. Mag. poecnvep.. 117). Silver chloride prepared in the dark, dried perfectly in an air-bath, and then placed on a watch-glass in a desiccator partially exhausted, was found to be not perceptibly darkened in sunlight even after an exposure of some hours ; whereas a rapid darkening takes place if moisture is introduced. It isa well-known fact that paper, especially ordinary glazed writing-paper, when moistened with a solution of potassium iodide and exposed to the light, becomes of a brownish-violet tint—due doubtless to the decomposition of the KI and libe- ration of the iodine. The author finds that the progress of this change is subject to several conditions. A solution of potassium iodide placed on glass or porcelain becomes brown only after an exposure of some days. ‘This change, it is suggested, is due to either the organic matter or the ozone in the atmosphere. A piece of ordinary filter-paper soaked with a saturated solution of KI was dried in the dark. When placed ona watch-glass under a desiccator, no change took place on ex- posure even after some days; although crystals of the salt were formed on the paper. Moreover, generally speaking, the wetter the paper the deeper was the tint produced. In fact the tint was proportional to the quantity of water present. When no water was present, then no change took place. Further, a strip of filter-paper floated on the top of a solution of KI for quite two hours in bright sunlight before any per- ceptible darkening occurred, although the underside had assumed a deep brown tint. But this change also depends on the kind of paper used ; * Communicated by the Author. [As some of Mr. Hughes’ results have been anticipated by Mr. Baker (Proc. Chem. Soc. May 4, 1893, . 129), he wishes it to be stated that the MS. was received by us on April 21st.—Ebs. | 532 Mr. R. E. Hughes on Water as a Catalyst. thus strips of highly glazed note-paper, ordinary filter-paper, Swedish filter-paper, and vegetable parchment were cut, soaked in the same KI solution, and exposed side by side to bright sunlight. It was found that after some hours a grada- tion of tints was thus obtained, the deepest being that on the glazed paper, whereas the tint of the parchment was almost imperceptible. Hence this change is perhaps due to the traces of chlorine invariably present in glazed paper. The depth of tint in the same paper was affected by the surface on which the paper lies. Thus, if lying on blotting-paper the change was very minute, slightly more perceptible on glass or polished surfaces, and most evident when on wood or other rough surface. ‘This chemical decomposition also took piace in the dark but more slowly; further, once the paper was quite dry, no perceptible deepening in tint was observed. A solution of potassium iodide may be kept in sunlight for an indefinite period, provided it is not exposed to the atmo- sphere. ‘This change is doubtless due to organic matter or ozone present in the atmosphere, but is dependent on the presence of moisture; whereas the staining of paper by this solution is due to the chlorine present or other constituent of the glaze, and is also dependent on the presence of moisture. Silver nitrate behaves closely similarly, as also to a lesser degree does platinum chloride. Some experiments were then made to determine the question whether dried hydrochloric-acid gas has any action on dry silver nitrate. The gas was passed through a tube containing copper filings (to remove chlorine), then through a series of drying- tubes containing strong H,8Q,, and finally over P,O; con- tained ina tube. This dried gas had no action on dried blue ~ litmus-paper. The silver nitrate was contained in a porcelain boat, and had been previously heated to incipient fusion. The gas was allowed to pass slowly through for about two hours. IT IE Oe a Pe Ta OE. ee i en ie ae Dah a Ne Crew NES i i a EES [ 540 ] INDEX tro VOL. XXXV. ACTINOMETER, on a chemical, ee Ammonia, on the specific heat of , liquid, 393. Angstrom (Prof.) on the intensity of radiation by rarefied gases under the influence of electric discharge, 502. Anthracite and bituminous coal-beds, on, 465. Averages, on a new method of treating correlated, 63. Bacilli, on a possible source of the energy required for the life of, 389. Baily (W.) on the construction of a colour map, 46. Baly (KE. C. C.) on the separation and striation of rarefied gases by the electric discharge, 200. Barus (Dr. C.) on the fusion con- stants of igneous rock, 173, 296; on the colours of cloudy conden- sation, 315. Basset (A. B.) on the finite bending -of thin shells, 496. Becher (H. M.) on the gold-quartz deposits of Pahang, 75. Bictite, on a secondary development of, in crystalline schists, 150, Blakesley (T. H.) on the differential equation of electrical flow, 419. Boiling-points of compounds, on the elfect of the replacement of oxygen by sulphur on the, 458. Boltzmann (Prof. L.) on the equili- brium of ws viva, 153. Bonney (Prof. T. G.) on the Nufenen- stock, 148; on some _ schistose ‘“‘oreenstones” and allied horn- blendic schists from the Pennine Alps, 149 ; on asecondary develop- ment of biotite and of hornblende in crystalline schists from the Binnenthal, 150. Books, new :—Sawer’s Odorographia, 73; Blake's Annals of British Geology, 145; Alexander’s Treatise on Thermodynamics, 307 ; Barus’s Die physikalische Behandlung und die Messung hoher Temperaturen, 310; Heydweiller’s Hulfsbuch fur die Ausfuhrung elektrischer Mess- ungen, 311; Lachlan’s Ele- mentary Treatise on Modern Pure Geometry, 462; Revue Semestri- elle des Publications Mathéma- tiques, 463; Bedell and Crehore’s Alternating Currents, 534; Hol- man’s Discussion of the Precision of Measurements, 539. Boron, on the properties of amor- phous, 80. Bosanquet (R. H. M.) on mountain- sickness, and power and endurance, 47. Breissig (F.) on the action of light upon electrical discharges, 151. Bryan (G. H.) on a hydrodynamical proof of the equations of motion of a perforated solid, 338. Burton (Dr. C. V.) on plane and spherical sound-waves of finite. amplitude, 317 ; on the motion of a perforated solid in a liquid, 351, 490. Catalyst, on water as a, 531. Chattock (A. P.) on an electrolytic theory of dielectrics, 76. Collins (J. H.) on the geology of the Bridgewater district, 150. Colour-blindness, on, 52. Colour map, on the construction of a, Condensation, on the eolours of cloudy, 316. Contact-action and the conservation of energy, on, 134, Cooke (J. 1.) on the mals and clays of the Maltese Islands, 148. INDEX. 541 Crova (M.) on the interference- bands of grating-spectra on gela- tine, 471. Current, on the magnetic field of a circular, 354. D’Arsonval galvanometer, on high resistances used in connexion with the, 210. Dielectric, on the attraction of two plates separated by a, 78. Dielectrics, on an electrolytic theory of, 76. Diffusion of substances in solution, on the, 127. Dispersion, on some recent determi- nations of molecular, 204. Dyuic equivalent of a substance, definition of the, 267. Karp (Miss A. G.) on the effect of the replacement of oxygen by sulphur on the boiling- and melt- ing-points of compounds, 458. Edgeworth (Prof. F. Y.) on a new method of treating correlated averages, 63. Electric discharge, on the separation and striation of rarefied gases by the, 200; on the intensity of radi- ation by rarefied gases under the influence of, 502. discharges, experiments with high frequency, 142; on the action of ight upon, 151. fields, constant and varying, experiments in, 68. Electrical discharge, on the potential of, 538. flow, on the differential equa- tion of, 419. furnace, on a new, 313. properties of pure nitrogen, on the, 1 vibrations, on the disengage- ment of heat occurring when, are transmitted through wires, 537. Electrochemical effects due to mag- netization, on, 473. Electromotive force, on the relation of volta, to pressure, &e., 97. Emmons (H.) on the petrography of the island of Capraja, 312. Energy, on radiant, 113; on contact action and the conservation of, 134; on the distribution of kinetic, among Kelyin’s doublets, 160; on a possible source of the, required for the life of bacilli, 389. Equations of motion of a perforated solidin liquid, on the, 338, 490. Kquipotential lines in plates tra- versed by currents, on a visible representation of the, 151. Everett (Prof. J. D.) on a new and handy focometer, 333. Fluorite, on the refraction of rays of ereat wave-length in, 44. Focometer, on a new, 333. Foote (A. E.) on a meteoric stone seen to fall in South Dakota, 152. Force, on the laws of molecular, 211. Fox (H.) on some coast-sections at the Lizard, 466; on a radiolarian chert from Mullion Island, 466. Frederick (Lieut. G. C.) on the geology of certain islands in the New Hebrides, 467. Friction, on liquid, 441. Furnace, on a new electrical, 315. Fusion constants of igneous rock, on the, 173, 296. Galitzine (B.) on radiant energy, 118. Galvanometer, on high resistances used in connexion with the D’Arsonval, 210. Gases, on the separation and stria- tion of rarefied, by the electric dis- charge, 200; on the intensity of radiation by rarefied, under the influence of electric discharge, 502. Geissler’s tubes, on a property of the anodes of, 538. Gelatine, on the interference-bands of grating-spectra on, 471. Geological Society, proceedings of the, 74, 146, 312, 464. Glacial Drift, on the occurrence of boulders and pebbles from the, in oravels south of the Thames, 468. Gladstone (Dr. J. H.) on some recent determinations of molecular refraction and dispersion, 204. Gold-deposits, on the Pambula, 76; of Pahang, on the, 75. Goldstein (11.) on a property of the anodes of Geissler’s tubes, 558. Gore (Dr. G.) on the relation of volta electromotive force to pres- sure &e., 97. ” a a I a lt ae all Dell 542 INDEX. Gratings, on a certain asymmetry in Prof. Rowland’s concave, 190; in theory and practice, on, 397. Grating-spectra on gelatine, on the interference-bands of, 471. Gravity, on the daily variations of, 314, Greenstones, on some schistose, from the Pennine Alps, 149. Gresley (W. S.) on anthracite and bituminous coal-beds, 465, Hall’s phenomenon, explanation of, 151. Heat of vaporization of liquid hydro- chloric acid, on the, 435. , on the disengagement of, when electrical vibrations are transmit- ted through wires, 537. Helmholtz (Prof.) on colour-blind- ness, 52. Heydweiller (Prof.) on Villari’s critical point in nickel, 469; on the potential of electrical dis- charge, 538. Hornblende, on a secondary develop- ment of, in crystalline schists, 150. Hughes (R. E.) on water as a catalyst, 531. Hull (Prof. E.) on the geology of Arabia Petrea and Palestine, 146. Hydrochloric acid, on the heat of vaporization of liquid, 455. Hydrolysis in aqueous salt-solutions, on, 365 c¥, Hygrometer, comparative experi- ments with the dry- and wet- bulb psychrometer and an im- proved, 525. Interference-bands of grating-spectra on gelatine, on the, 471. Tron rings split in a radial direction, on the magnetization of, 592. Irving (Rev. A.) on the base of the Keuper formation in Devon, 147. Judd (Prof. J. W.) on inclusions of Tertiary granite in the gabbro of Skye, 464. Kinetic energy, on the distribution of, among Kelvin’s doublets, 160. Klemenéic (Dr. 1.) on the disen- gagement of heat occurring when electrical vibrations are trans- mitted through wires, 537. Lagrange’s equations of motion, on, 345, 490. Lefevre (J.) on the attraction of two plates separated by a dielectric, 78. Lehmann (H.) on the magnetization of iron rings split in a radial direction, 592. Light, on the diffusion of, 81; on the action of, upon electrical dis- charges, 151. Liquid, motion of a perforated solid in, 358, 490. Lommel (E.) on a visible represen- tation of the equipotential lines in plates traversed by currents, 151. Ludeking (C.) on the specific heat of liquid ammonia, 393. Luminons discharges in electrodeless vacuum-tubes, on, 506. MacGregor (Prof. J. G.) on econtact- action and the conservation of energy, 134. Madsen (V.) on Scandinavian boul- ders at Cromer, 312. Magnetic field of a circular current, on the, 354. fields, constant and yarying, experiments in, 68. 4 Magnetization of iron rings split in a radial direction, on the, 392. , on electrochemical effects due to, 4738. Mascart (M.) on the daily variations of gravity, 314. Melting-points of compounds, on the effect of the replacement of oxy- gen by sulphur on the, 458. Meteoric stone seen to fall in South Dakota, on a, 152. Michigan, on the geology of the iron, gold, and copper districts of, 74. Minchin (Prof. G. M.) on the mag- netic field of a circular current, 354. Moissan (H.) on the properties of amorphous boron, 60; on a new electrical furnace, 513. Molecular force, on the laws of, 211. refraction and dispersion, on some recent determinations of, 204. Monckton (H. W.) on the occurrence of boulders and pebbles from the Glacial Drift in gravels south of the Thames, 468. Motion of a perforated solid in liquid, on the, 338, 490. Mountain-sickness, remarks on, 47. IN DEX. Nickel, on Villari’s critical point in, 469. Nitrogen, on the preparation of pure, 1 Ohm’s law, on a necessary modifica- tion of, 65, Oxygen, on the effect of the re- placement of, by sulphur on the boiling- and melting-points of compounds, 458. Pembrey (M. S8.), comparative ex- periments with the dry- and wet- bulb psychrometer and an im- proved chemical hygrometer, 525. Perry (Prof. J.) on liquid friction, 441. Pickering (S. U.) on the diffusion of substances in solution, 127. he (Dr. W.) on colour-blindness, ae (F. D.) onthe Pambula gold- deposits, 76. Pressure, on the relation of volta electromotive force to, 97. Psychrometer, comparative experi- ments with the dry- and wet-bulhb, and an improved chemical hygro- meter, 525, Radiant energy, on, 115. Radiation by rarefied gases under the influence of electric discharge, on the intensity of, 502. Raisin (Miss C. A.) on the variolite of the Lleyn, 312. Refraction of rays of great wave- length in rock-salt, sylvite, and fluorite, on the, 35. , on some recent determinations of molecular, 204, 270. Reid (C.) on a fossiliferous Pleisto- cene oi at Stone, 469. Rigollot (H.) on a chemical actino- meter, 77. Rimington (E. ©.), experiments in electric and magnetic fields, con- stant and varying, 68; on lumi- nous discharges in electrodeless vacuum-tubes, 506. Roberts (T.) on the geology of the district west of Caermarthen, 467. Rock, on the fusion constants of igneous, 173, 296. Rock-salt, on the refraction of rays of ereat wave-length in, 35. Rowland (Prof. H. A.) on gratings in theory and practice, 397. 543 Rubens (H.) on the refraction of rays of great wave-length in rock- salt, sylvite, and fluorite, 35. Rudski (M. P.) on the flow of water in a straight pipe, 439. Rydberg (Dr. J. R.) on a certain asymmetry - in Prof. Rowland’s concave gratings, 190. Salt-solutions, on hydrolysis in aque- ous, 365. Sanford (f.) on a necessary modifi- cation of Ohm’s law, 65. Shells, on the finite bending of thin, 496. Shields (Dr. J.) on hydrolysis in aqueous salt-solutions, 365. Shrubsole (O. A.) on the plateau- gravel south of Reading, 468. Smith (F. J.) on high resistances used in connexion with the D’Ar- sonval galvanometer, 210. Smith (W.), experiments in electric and magnetic fields, constant and varying, 68. Snow (B. W.) on the refraction of rays of great wave-length in rock- salt, sylvite, and fluorite, 35. Solid, on the motion of a perforated, in liquid, 338, 490. Solution, on the diffusion of sub- stances ria Ae Sound-waves, on plane and spherical, of finite amplitude, 317. Squier (Lieut. G. O.) on electro- chemical effects due to magnetiza- tion, 473. Starr (J. E,) on the specific heat of liquid ammonia, 393. Stoney (Dr. G. J.) on a possible source of the energy required for the life of bacilli, 389. Sulphur, on the effect of the re- placement of oxygen by, on the boiling- and melting-points of compounds, 458. Sumpner (Dr. W. E.) on the dif- fusion of light, 81, Sutherland (W.) on the laws of molecular foree, 211. Swinton (A. A. €.) on high frequency electric discharges, 142, Sylvite, on the refraction of rays of ereat wave-length in, 43. Teall (J. J. H.) on some coast- sections at the Lizard, 466; on a MRE ee ee bn Sos ULE IN RB EMA I ATEN SOE EAE OT | CITE EE EOI LIONEL EN 4 OI 8 MELE ETE NY LITTON SIE GE IO en SE eapat ieaciey tee anaheim ners Serpents wees atone : 6 JA pee es = 544 = INDEX. radiolarian chert from Mullion Island, 466. Thermodynamics, on the signa of the second law of, 124. Thermometers, on the official testing of, 595. Threlfall (Prof. R.) on the electrical properties of pure nitrogen, 1. Tsuruta (K.) on the heat of vapo- rization of liquid hydrochloric acid, 435. Vacuum-tube in a varying and in a constant electric field, theory of a, COT. Vacuum-tubes, on luminous dis- charges in electrodeless, 506. Variolite of the Lleyn, on the, 312. Villari’s critical point in nickel, on, 469. Vis viva, on the equilibrium of, 153. Volta electromotive force, on the re- lation of, to pressure &e., 97. Wadsworth (Prof. M. E.) on the geology of the iron, gold, and copper districts of Michigan, 74. Water, on the flow of, in a str aight pipe, 489. —- as a catalyst, 531. Waves, on plane and _ spherical sound-, of finite amplitude, 317. Wiebe (HL. F’.) on the official testing of thermometers, 395. END OF THE THIRTY-FIFTH VOLUME. Printed by Jaytor and Francis, Red Lion Court, Fleet Street. Elana SoSW Val, 66 Mek ie Mintern Bros : | 5 00 iS | } | } | | | DIAGRAM OF APPARATUS tor the Continuous Preparation OF PURE NITROGEN. | | | | Mintern Bros. lith. Seeeieniaes imeem inane ee = Pilll., Wid®-.-O.U-VOL-ou -Fi-il +O Lf +O uve c) nel, dito | pea | C O ye . . O € re ‘ 5K GE 72 at > "SULY() 2D PUNIS ISO * = o2 aS 2 So S Vol parr e aod to | Phil. Ma a nel, + Roch -salt (ove ©) teal, Slee Svlvcte \ (ehkove b) nda] llaorite (eurve ec) 400 500 100 SYOLW NE ROCK-SALT. 10 2b Mintern Bros lith : UAT 2 Sodg Uta TUTyAy, apouibya) sxaibay uw aunpouaduey apoubyuay saatboqud anne diay a Cig Ci = SA eee ig (aps rH al LI 21 So 41 e4e1 Te) NEO + (OD We Oeeco a LD W ° 00 a) oa S = Aa 18 fate 5 N om. . > ¢ S . ~ 3 3 S & : : ® OPEO: OO: vo es a . r A pet nn a cet me eee ae tia penal f at so" ; ; F , ‘ oe . Phil. Mag.$.5.Vol.85.PLIV. S OSCTpLILATOIR « RESONATOR Phil.Mag.S.5 Vol 35.PLIV. _ S | | OSCILLATOR. » RESONATOR » Pig. 5. i Fig.7. b 1 Mintern Bros. lith- = : : 5 Pll. Mas. 5.6. Vol.3o0. PI. V. LOCK Appoar nt Contractrow ~--==p5~-- 20 a Sal he, ie an He y 1 ve, elu a (bef) u net ar owt ) Same. Sectional at right angles 4 prece dug : PN LET IT TEL Sy SA HE A A A Z77 s ° h DS A | ea | us + oO N . \ ° o ee ° es Verticad micrometer and . yy | APU LENCE S. Seale Ma YB Pars es oS) k d B) WO (AL IUAD SLELYDS SLI SPLLEPLSLELLD, | | | | | | Secltonal pla oF fasauce T7777 HS Yi} the finsion lube, the sight tule, he bumers, | | Seglicnal elevation of the liirmace, showtuy ele. Seale Yq . Same. Sectional ¢ c devation » the FN NF Hel ) Arm te hold the Tinsion lihe. Perforated ving, Minterms ros Jit Fig.G. Clay envelope of the platinum finsion Ube i Melual Contraction Appar né Contraction Plul.Mag.S.5.Vol.35 Pl V. is = S I ~ G) S = ~ k F\ re \ q rary | na wi | Z| \ i 7 1F < : S 5 5) = IL = = ll a i Sess Phil.Mag. S.5.Vol.35. Pl. VI. aha ili) i coe. Gucble, showy the solid charge & aaaal platuum tuhe. Scale "4. E ek. gectzonal elevatum cf the ZY Thanace & appurtemances yy, SS showing the cucablei place. a] a ; NN rir WOO Nis RRs KKK SSS iG ji RN “ ie P N N Yi LA N Y a=. NS QOS UN SKY AL AK LS, ASNSgys MM ELH Ww ASSN SSS bE WzzZz7 ee PASO scat WORSE oT Sete 7 SS SS g Pee 2, Sectonal plan of furnace & cruchle. 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