7? i*k^ ^,. ''A ,*i ~.fA Sf's // ft. / ' ft* if J&MW . < WE *■ 'A & 7 «- <3^ c Zfa.* ^.^ *2&?& ^^m^ '^^i :^^ ^ ' fr- "- ' ^>. .'V sai ~n Certain Derivatives of Furfuracrylic Arid. By II. B. Gibson and C. F. Kahnweiler . . . 364 III. On the so called Dioxymaleic Acid. By W. S. Hi n drixson ; . 376 CONTENTS. vii Page XXVI T. An Address delivered at the Meeting of April 10, when the Rumford Medals were j)resented to Professor A. A. Michelson. By Joseph Lovering 380 Proceedings 403 Memoirs : — George Rumford Baldwin 429 Jonathan Ingersoll Bowditch 435 Samuel Kneeland 438 Frederick Augustus Porter Barnard 441 John Call Dalton 445 Ezekiel Brown Elliott . 447 Michel Eugene Chevreul 452 Rudolf Julius Emanuel Clausius 458 Franciscus Cornelius Donders 465 List of the Fellows and Foreign Honorary Members . . 471 Statutes and Standing Votes of the Academy .... 479 Rumford Premium 488 Index 439 PROCEEDINGS OF THE AMERICAN ACADEMY OF ARTS AND SCIENCES. VOL. XXIV. PAPERS READ BEFORE THE ACADEMY. I. CONTRIBUTIONS FROM THE CHEMICAL LABORATORY OF HARVARD COLLEGE. ON THE ACTION OF SODIUM MALONIC ESTER ON TRIBROMDINITROBENZOL. By C. Loring Jackson and W. S. Robinson. Presented June 13, 1888. In an earlier paper from this laboratory,* the preparation of tribrom- trinitrobeuzol and its action with ammonia and aniline were described, and the announcement was made that the study of the behavior of this very reactive body would be continued. G. D. Moora and one of us accordingly have taken up the action of sodium malonic ester upon it, in the hope of substituting for each of the bromine atoms the radi- cal of malonic ester, CH(COOC.2H.)2, and obtaining in this way a substance which might have yielded interesting derivatives. As, however, an entirely different product was the result of the reaction, it seemed wiser to study it with the much more accessible tribrom- dinitrobenzol, which acted in the same way, and to confine the work on the trinitro compound, which at best can be obtained only with difficulty, to those points in which the two substances showed a dif- ferent behavior. In this paper, therefore, we give the results obtained up to the present time from the action of sodium malonic ester on * These Proceedings, Vol. XXIII. p. 138. VOL. XXIV. (N. S. XVI.) 1 2 PROCEEDINGS OF THE AMERICAN ACADEMY tribromdiuitrobenzol, which we are obliged to publish now, although in some respects the work is not so finished as we could wish, because the departure of one of us from Cambridge will prevent us from con- tinuing the investigation together. The most important of these results can be summarized briefly as follows. Sodium malouic ester under the conditions used by us removes from tribromdiuitrobenzol only two atoms of bromine, one of which is replaced by the radical of malonic ester, the other by hydrogen, so that the formula of the product is C6H2Br(N02)2CH(COOC2fL)2. This substance shows marked acid properties, and, although of a pale yellow color itself, forms salts most of which are dark blood-red ; of these the sodium salt was analyzed, and its formula proved to be C6H2Br(N02)2CNa(COOC2H5)2. The yellow copper salt was also analyzed, but proved to be a some- what complex basic salt. The bromine contained in the substance is easily removed by treatment with aniline, the product being C6H2CcH5NH(N02)2CH(COOC2H5)2, which also gives a blood-red sodium salt with a formula similar to that of the salt derived from the original substance, but the acid prop- erties of the anilido compound are much less pronounced. When heated with strong hydrochloric acid the bromdinitrophenylmalonic ester gives ethylchloride and a new substance melting at 170°, the analysis of which led to the formula C(.H2Br(NO.)),,C;,H502, but the determination of its constitution must be postponed till a later paper. Action of Sodium Malonic Ester on Tribromdiuitrobenzol. If .in alcoholic solution of sodium malonic ester is added to tribrom- diuitrobenzol (melting point 192°) dissolved in ether, the first drop imparts to the ethereal solution a blood-red color, which increases in intensity as more of the solution of sodium malonic ester is added, and the liquid contains the sodium salt of a new substance, which we pre- pared in the following way. To an ethereal solution of a weighed quantity of tribromdinitrobenzol we added an alcoholic solution of sodium malonic ester in the proportion of three molecules of the ester to one of the tribromdiuitrobenzol. The following were found to be OF ARTS AND SCIENCES. 3 convenient proportions : 20 grm. of tribromdinitrobenzol, 16 grm. of raalonic ester dissolved in 100 to 150 c.c. of absolute alcohol and treated with 2.4 grm. of sodium as sodic ethylate. It was not neces- sary to add the ester gradually, and there was no perceptible evolution of heat during the reaction. The mixture was allowed to stand in a corked flask at ordinary temperatures for three or more hours, and the dark blood-red liquid thus obtained filtered from the precipitate of sodic bromide, which had been deposited, acidified with dilute sul- phuric acid, which changed the dark red color to pale yellow, and filtered once more to remove the sodic sulphate formed. The filtrate was then distilled on the water bath until most of the ether had passed over, when the residue in the flask deposited, as it cooled, crystals of the new substance mixed with a large quantity of unaltered tribrom- dinitrobenzol. The mother liquor from these crystals was allowed to evaporate spontaneously, and left a red or yellow oil mixed with a small additional quantity of the crystals, which were separated from it, and the oil allowed to stand in an, open dish for some weeks, when it deposited an additional quantity of the crystals. The crystals, whether obtained by cooling the hot alcoholic solution, or from the oil by long standing in the cold, were purified by dissolving them in a little hot alcohol, and adding a moderately strong aqueous solution of sodic hydrate (the common laboratory solution diluted with its own volume of water), which converted the new substance into its soluble sodium salt, but left the tribromdinitrobenzol unaltered, the red solu- tion was then poured into a large quantity of water, and the tribrom- dinitrobenzol removed by filtration. If the solid crystals were treated directly with the aqueous solution of sodic hydrate, the tribromdinitro- benzol was left in a form which clogged the filter very badly, whereas when an alcoholic solution was used, as directed above, no difficulty was encountered in the filtration. The red filtrate was acidified with dilute sulphuric acid, and the precipitate purified by crystallization from hot alcohol until it showed the constant melting point 75°-76°. After being dried in vacuo, its composition was determined by the following analyses. I. 0.2061 grm. of the substance gave on combustion* 0.2910 grm. of carbonic dioxide and 0.0602 £rm. of water. II. 0.2013 grm. gave 0.2827 grm. of carbonic dioxide and 0.0511 grm. of water. * Care must be taken to heat the substance very gradually, as it shows a tendency to explode in the combustion tube. 4 PROCEEDINGS OP THE AMERICAN ACADEMY III. 0.1075 grm. gave 0.2780 grm. of carbonic dioxide IV. 0.1926 grm. of substance gave 12.4 c.c. of nitrogen at a temper- ature of 20° and a pressure of 740 mm. V. 0.221 1 grm. of substance gave by the method of Carius 0.103C grm. of argentic bromide. VI 0.2005 grm. gave 0.0937 grm. of argentic bromide. Found. I. II. III. IV. V. VI. Carbon 38.51 38.30 38.38 Hydrogen 3.24 2.83 Nitrogen 7.17 Bromine 19.91 19.88 These results agree about equally well with the numbers calculated from two different formulas, as appears by the following comparison. Calculated for Found Calculated for C0HBr(NO, ).,('( C02C2H5)2. Mean. CGH2Br( N02)2CH( C02C2H;)2. Carbon 38.71 38.40 38.51 Hydrogen 2.72 3.03 3.21 Nitrogen 6.94 7.17 0.91 Bromine 19.85 19.89 19.75 The first of these formulas, in which the two atoms of bromine removed from the tribromdinitrobenzol have been replaced by the bivalent radical =C(C02C2H.)2, seems at first sight the most probable, especially since W. II. Perkin, dr. and others have observed the strong tendency of sodium malonic ester to react in this way ; but although this is the only formula we have been able to find which ex- plains easily the removal of two atoms of bromine in this reaction, we are inclined to reject it in favor of the second one, in which one atom of liromine has been replaced by the univalent radical -CH(C02C2H5)2, and the other by hydrogen, for the following reasons: — First, the formation of a sodium salt is hard to reconcile with the lirst formula, unless, indeed, sodic hydrate was added to it, t giving CTI15r(N011)liOHCNa(C02C2TI,)2; but our analyses of the sodium salt, given later in this paper, prove that it contains no hydroxy], and to make this proof more convincing we prepared the suit, for one of our analyses from sodic ethylate, as * Tin* water was lost in tins analysis, t Wislicenus, Ann. Chem., ccxlii. 23. OF ARTS AND SCIENCES. 5 the radical CJLO, which in this case would be added instead of hydroxyl, would make a very great difference in the percentage com- position of the salt; but this preparation, like the others, gave on analysis numbers corresponding to the formula C0H2Br(NO2)2CNa(COOC2H5)2. Secondly, the ease with which the sodium salt is formed, and with which it is decomposed by an acid giving the original substance, mili- tates against the first formula, as we can hardly suppose that a ring of carbon atoms, such as must be assumed in this formula, would break, when treated with an alkali, and reunite under the influence of an acid in dilute solutions. Finally, we may add that the meta position of the bromine atoms replaced deprives the first formula of any support from analogy.* The principal objection to the formula CGH2Br(NO:,)2CH(COOC2H;i)2, which we adopt, is that we cannot account as yet for the formation of such a substance by the reaction of sodium malonic ester on tri- bromdinitrobenzol. We hope, however, that a careful study of the quantitative conditions of the reaction, and of the oil which is the secondary product, will throw light on this part of the subject ; but owing to the departure of one of us from Cambridge, its further investigation must be postponed till next autumn. The yield was far from satisfactory, 14 grm. of tribromdinitroben- zol after treatment with 12 grm. of malonic ester and 1.7 grm. of sodium, as described above, giving only 4.3 grm. of the bromdinitro- phenybnalonic ester instead of the 14 grm. required, if the whole of the tribromdinitrobenzol was converted into the new substance, that is, 30.7 per cent of the theoretical yield. A large amount of the tri- bromdinitrobenzol was recovered, however, amounting to 5.5 grm., or 39.3 per cent. This leaves 30 per cent unaccounted for, which prob- ably remains dissolved in the oil deposited by the alcoholic mother liquors ; but that the dissolved substance is bromdinitrophenylmalonic ester admits of great doubt, as we have not succeeded in obtaining any considerable quantity of this substance from the oil by treatment with aqueous sodic hydrate. This point will be investigated more thor- oughly hereafter. We have tried several modifications of the process, in hopes of improving the yield, but none of them have given satisfac- tory results ; if, for instance, the proportion of sodium malonic ester is * Compare J. Stanley Kipping, Ber. d. ch. G. 1888, p. 32. 6 PEOCEEDINGS OF THE AMERICAN ACADEMY increased in order to bring more of the tribromdinitrobenzol into the reaction, any gain from this cause is more than compensated by the larger amount of the product taken up by the greater quantity of oil, which is only in part deposited on long standing. Nor was the yield increased by longer standing, or by boiling the materials with a re- verse condenser ; in this latter case the product came down in an oily form, and with, if anything, rather a smaller yield was much harder to purify. Properties of the Bromdinitrophenylmalonic Ester, CGH2Br(NO,)2CH( COOC2H5)2. The substance crystallizes in pale yellow flattened needles, or long plates terminated by a single plane, which forms with the sides angles not very far from 90°, but distinctly obtuse and acute. It melts be- tween 75° and 76°, and shows a tendency to explode at high tem- peratures, so that the heat must be applied carefully when making a combustion of the substance. It is not very soluble in cold alcohol, but freely in hot, more soluble in methyl than in ethyl alcohol, freely soluble in ether, benzol, or glacial acetic acid, even more so in chlo- roform, moderately soluble in acetone or carbonic disulphide, nearly insoluble in ligroine or water. Strong sulphuric' acid in the cold has little action on it, although perhaps a small quantity dissolves ; on warming the mixture, complete solution takes place, and addition of water precipitates a solid, which seems to consist principally of un- altered bromdinitrophenylmalonic ester mixed with a small amount of a substance with a higher melting point, probably the compound formed by the action of concentrated hydrochloric acid in sealed tubes (see page 11). Nitric acid, either strong or fuming, dissolves the bromdinitrophenylmalonic ester in the cold, but does not produce any change of color. In this respect, it differs markedly from the corre- sponding trinitro compound. If the acid solution is warmed, decom- position seems to take place. The bromdinitrophenylmalonic ester possesses well-marked acid properties, as was to be expected, since it contains a hydrogen atom standing between the two carboxyls of the malonic ester and a phenyl, which, as Victor Meyer* has shown, frequently exercises a negative influence, much heightened in this case by the presence of the two nitro groups. Sodic hydrate in either aqueous or alcoholic solution at once converts it into a soluble red sodium salt, and the same salt is * Bcr. d. ch. G. 1887, p. 534, 1888, p. 1291 et seq. OP ARTS AND SCIENCES. 7 formed by an alcoholic solution of sodium malonic ester, by sodic car- bonate dissolved in water, or by acid sodic carbonate mixed with very dilute alcohol. The aqueous solution of the salt is, however, entirely decomposed by carbonic dioxide, the original substance being precipi- tated. An aqueous solution of the sodium salt prepared by treating an excess of the original substance with a solution of sodic hydrate gave precipitates with salts of all the common metals except those of the alkalis. Most of these precipitates were red, and among them the following were especially characteristic : — Baric, strontic, or calcic chloride, dark brick-red. Magnesic sulphate, rust color. Zincic acetate, dark chrome-orange. Basic plumbic acetate, very dark brick-red. The neutral plumbic acetate gave a yellow precipitate, which turned white when in contact with an excess of lead salt. Cupric sulphate, dark golden yellow. Ammonic hydrate also dissolved the substance with a red color, but the salt was decomposed on trying to evaporate off the excess of ammonia on the water-bath, leaving a whitish residue, which seemed to consist principally of the original substance, with a small amount of decomposition product. The substance is in fact easily decomposed by either ammonic or sodic hydrate, and our rather unsatisfactory ob- servations on these reactions will be found on page 11. The sodium salt boiled under a reverse condenser with ethylbromide in alcoholic solution, passed from red through purple, bluish green, green, and brown to reddish yellow ; sodic bromide was formed, and the other product was an oily substance, which solidified after some time. It will be studied later. The bromine atom in the bromdinitrophenyl- malonic ester seems to be removed with comparative ease. Up to this time, we have studied its behavior in this direction only with aniline (see page 9). The Sodium Salt CGIT2Br(X02)2CXa(COOC,II,V, This substance was prepared by dissolving some of the bromdini- trophenylmalonic ester in alcohol and adding a little sodic hydrate, care being taken that the hydrate was not in excess; a little ether was then added, and the mixture evaporated rapidly in a Bmall beaker sunk throughout its whole length in the water-bath. The ether vapor kept the air from coming in contact with the liquid, while the alcohol was being heated to its boiling point. The residue, after all the alcohol had evaporated, was extracted with benzol to remove the excess of the 8 PROCEEDINGS OF THE AMERICAN ACADEMY ester, and then dried by gentle warming, and standing in vacuo over paraffine and sulphuric acid. These precautions were adopted to avoid the contamination of the substance with the carbonic dioxide of the air. The same substance was obtained when sodic ethylate was used instead of sodic hydrate, and Analysis III. was made with a sample prepared in this way. I. 0.1950 grm. of the substance ignited with sulphuric acid gave 0.0324 grm. of sodic sulphate. II. 0.1354 grm. gave 0.0216 grm. of sodic sulphate. III. 0.1943 grm. gave by the method of Carius 0.0838 grm. of argen- tic bromide and the filtrate gave 0.0330 grm. of sodic sulphate. IV. 0.2148 grm. gave 14.3 c.c. nitrogen at a temperature of 25° and a pressure of 759.6 mm. Sodium Calculated for ,Br(N02),CNa(C02C2H5)2. 5.39 i. 5.38 Found. II. III. 5.16 5.50 IV. Bromine 18.74 18.35 Nitrogen 6.55 7.42 The results of these analyses show that the substance is the normal salt, containing but one atom of sodium, and the important bearing of this point on the determination of the formula of the bromdinitro- phenylmalonic ester has been discussed already. (See page 4.) Properties. — The salt forms a dark blood-red powder, easily sol- uble in water, alcohol, or ether. From a solution containing much sodic hydrate, the salt can be extracted with ether ; but pure water, on the other hand, extracts the salt from its ethereal solution. Its aqueous solution is decolorized by carbonic dioxide bromdiuitrophenyl- malonic ester being precipitated. The copper salt seemed from its appearance to promise excellent results on investigation, and was accordingly prepared as follows. An alcoholic solution of the bromdinitrophenylmalonic ester was treated with a small quantity of sodic hydrate taking care that the ester was in large excess, and then poured into a volume of water sufficient to precipitate all the unaltered ester; after filtering, an alco- holic solution of cupric chloride was added, and the precipitate washed first with 50 per cent alcohol, then with water, and finally once with hot alcohol ; it was then dried in vacuo. It is not necessary to pro- tect the salt from contact with the air during its preparation, as it is not perceptibly affected by carbonic dioxide. It gave the following results on analysis. OF ARTS AND SCIENCES. 9 I. 0.2052 grm. of the salt was treated according to the method of Carius and gave 0.0844 grm. of argentic bromide. The fil- trate was freed from argentic nitrate, and the copper precipi- tated by electricity from a sulphuric of nitric acid solution giving 0.0197 grm. of copper. II. 0.2073 grm. treated in the same way gave 0.0864 grm. of argentic bromide and 0.0198 grm. of copper. III. 0.1455 grm. gave 0.0138 grm. of copper. Calculated for HOCu2[C6H2Br(NO,)2C(COoC2H5)2]3. Copper 9.36 i. 9.60 Found. II. 9.55 in. 9.48 Bromine 17.70 17.50 17.74 From these results it would appear that the substance is a basic salt, or, at least, that it is not the normal salt, and in spite of its very promising appearance is not fitted to throw light on the nature of the original substance. We have not thought it worth while, therefore, to examine it more carefully. We may add, that the salt changes color from a lighter to a darker yellow soon after it is prepared, which we are inclined to ascribe to the conversion of ClCu2[C6H2Br(N02)2C(C02C2Hs)2]3 into the corresponding hydroxyl compound by the action of the water in which it is suspended. Properties. — The copper salt forms an obscurely crystalline pre- cipitate of a golden yellow color, with a very slight greenish tinge. It is essentially insoluble in water, alcohol, or ether, and is a compar- atively stable substance, as it seems to be unaltered by exposure to the air, or by heating to 100°. Strong nitric acid, even in excess, de- composes it, setting free the bromdinitrophenylmalonic ester. Anilidodinitrophenylmalonic Ester, C6H5NHC6H2(N02)2CH(COOC2H5)2. This substance was made by mixing the bromdinitrophenylmalonic ester with aniline in the proportion of one molecule of the ester to two of the base. The solid becomes yellow almost immediately, and the action has come essentially to an end after the mixture has stood for a few minutes in the cold. As a measure of precaution, however. we always heated it gently for a few minutes to make certain that all the bromine had been removed. The product was purified by cystallization from alcohol, until it showed the constant melting point 118°, dried at 100°, and analyzed. 10 PROCEEDINGS OF THE AMERICAN ACADEMY I. 0.2104 grm. of the substance gave on combustion 0.4262 grm. of carbonic dioxide and 0.0903 grm. of water. II. 0.1886 grm. of the substance gave 16.9 c.c. of nitrogen at a tem- perature of 22° and a pressure of 766.6 mm. Calculated for Found. C6H2(NHCGH5)(N'0,)2CH(C02C2H5)2. I. II. Carbon 54.68 55.24 Hydrogen 4.56 4.77 Nitrogen 10.07 10.24 Properties. — The anilidodinitrophenylmalonic ester forms flattened needles terminated by one or two planes, which form much more oblique angles with the sides than those which appear in the bromdi- nitrophenylmalonic ester. It is also found occasionally in star-shaped groups of needles, has a bright yellow color, and melts at 118°. It is only slightly soluble in cold alcohol, much more soluble in hot, but not freely even in this. More soluble in methyl than in ethyl alcohol ; soluble in ether, or in carbonic disulphide ; freely soluble in benzol, glacial acetic acid, or acetone, very freely in chloroform ; essentially insoluble in water or ligroine. The best solvent for it is alcohol. Concentrated hydrochloric acid does not dissolve, or act on it in open vessels, either hot or cold. An aqueous solution of sodic hydrate acts on it in the cold only very slowly and imperfectly, but gives a red solution when boiled with it., In alcoholic solution sodic hydrate converts it into a red soluble salt ; the anilido compound therefore still possesses acid properties, but these are much less marked than in the corresponding bromine compound ; the negative influence of the dinitrophenyl therefore has been partly neutralized by the introduc- tion of the basic aniline radical CrH.NH. The Sodium Salt C6H2(C6H5NH)(NOJ2CNa(COOC2H5)a. This substance was formed in the same way as the sodium salt of the bromdinitrophenylmalonic ester ; that is, by treating an alcoholic solution of the substance with alcoholic sodic hydrate not in excess, evaporating to dryness with a little ether on the water-bath, and extracting the excess of the ester with benzol. It was dried at 100°, and analyzed. 0.1180 grm. of substance gave 0.0194 grm. of sodic sulphate. Calculated for Found. C0H2(CCH3N H X NO A,C \a( C02C2H5)2. lium 5.24 5.32 OF ARTS AND SCIENCES. 11 Properties. — It resembles the sodium salt of the bromdinitrophenyl- malonic ester closely in appearance and solubility, but is of a some- what lighter red. Its solution is decomposed, when treated with carbonic dioxide. Experiments on the Saponification of BromdinitrophcnyhnaJonic Ester. In taking up this subject we considered it necessary to study the action of alkalis on the ester, although, owing to the ease with which the nitro groups are attacked, we had little expectation of reaching satisfactory results. In this we were not deceived, but we think it best to give a brief account of these experiments before describing our more successful work with strong hydrochloric acid in sealed tubes. A solution of sodic hydrate in water, if boiled with the brom- or anilidodinitromalonic ester, gave a brownish red solution, from which acids precipitated nothing ; but after acidification, and extraction with ether, an unpromising oil was obtained in very small quantity. Cold alcoholic sodic hydrate with the anilido compound gave a somewhat more promising result, but in this case also most of the substance seemed to be decomposed. The bromine compound after standing for two weeks with ammonic hydrate at ordinary temperatures was con- verted into a similar brown solution, which on acidification gave a resinous brown precipitate and a yellow filtrate, from which ether ex- tracted a substance melting above 200° , ammonic bromide being formed during the process. This is the only one of these products which seems worth further investigation. o Action of Hydrochloric Acid.* "When the bromdinitrophenylmalonic ester was heated with strong hydrochloric acid in a sealed tube to 140°-145°, it was decomposed, and upon opening the tube a gas was given off in tolerable quantity, which burnt with a green-bordered flame, and was without doubt ethylchloride. About one gram of the substance and :><> c.c. of common strong hydrochloric acid were used in each tube, and the temperature should not be allowed to go above 150°, as in this r:i-- an impure product was the result. If proper care was used in the heating, the tube contained crystals, or a clear liquid, from which crystals were deposited after the pressure was relieved; these were * All our work on this part of the subject must lie regarded as preliminary. 12 PROCEEDINGS OF THE AMERICAN ACADEMY filtered out and the filtrate thrown away, as it gave almost no residue on evaporation, and no extract when shaken with ether. The crystals were purified by crystallization from dilute alcohol (three parts of water to one part of alcohol). If the temperature was kept below 150°, the product was nearly pure, as it came from the tube ; but if it had risen above this point, a small quantity of a lower melting substance was formed, which it was almost impossible to remove with dilute alcohol. In this case the best plan was to dissolve the substance in chloroform, when the impurity separated at first as a pasty mass, leaving the principal product in solution, which after one crystalliza- tion from dilute alcohol showed the constant melting point 170°. It was dried at 100°, and analyzed with the following results. I. 0.1307 grm. of substance gave on combustion 0.1634 grm. of carbonic dioxide and 0.0278 grm. of water. II. 0.2162 grm. of substance gave 0.2688 grm. of carbonic dioxide and 0.0495 grm. of water. III. 0.2136 grm. of substance gave 18.3 c.c. of nitrogen at a temper- ature of 22° and a pressure of 760 mm. IV. 0.1197 grm. gave 10.2 c.c. of nitrogen at a temperature of 28° and a pressure of 762.9 mm. V. 0.2212 grm. of substance gave by the method of Carius 0.1365 grm. of argentic bromide. VI. 0.2120 grm. gave 0.1275 grm. of argentic bromide. VI. 26.29 25.59 These numbers agree tolerably well with those required for the formula CcH2Br(N02)2C3H502. Calculated. Carbon 33.86 Hydrogen 2.19 Nitrogen 8.77 Bromine 25 08 But the formula cannot be considered definitely established, until we have supported our analytical results by a careful study of the deriva- tives of the substance. Found. I. ii. III. IV Carbon 34.10 33.91 Hydrogen 2.37 2.54 Nitrogen 9.48 9.3 Bromine OF ARTS AND SCIENCES. 13 Properties. — The substance crystallizes from dilute alcohol in yel- lowish white narrow plates, sometimes half a centimeter in length which are made up of needles attached to another needle acting as a midrib at very acute angles, giving an exact imitation of a feather or more commonly of one side of a feather ; this form is very character- istic, and, when not so well developed, the substance can be recognized by the formation of narrow plates, usually smooth on one' side and rather irregularly serrated on the other, or upon the ends. The plates often occur in radiating groups, the members of which form very acute angles with each other. From methyl alcohol or ether it crystallizes in very slender needles, much branched at very sharp angles, often forming circular groups resembling certain seaweeds. It melts at 1 70° , is not very soluble in cold alcohol, freely in hot, more soluble in methyl than in ethyl alcohol, freely soluble in glacial acetic acid or acetone, tolerably soluble in ether, slightly soluble in benzol either cold or hot, or in carbonic disulphide, slightly soluble in cold chloroform, more soluble but not freely in hot, nearly insoluble but not quite so in cold water, more soluble but still very slightly in hot, essentially insoluble in ligroine. The best solvent for it is chloroform, or a mixture of alcohol and water. Its behavior with alkalis is very characteristic. If a drop of an aqueous solution of sodic hydrate is added to the sub- stance dissolved in alcohol, the solution takes on a dark but brilliant Prussian green color. This solution becomes colorless on addition of hydrochloric acid, but turns green again on addition of sodic hydrate. The green alcoholic solution, if allowed to evaporate spontaneously, leaves a brownish yellow residue, and a solution of the same brown- ish yellow color is obtained if an excess of sodic hydrate is added to the original substance. If the yellow solution, in whichever way pre- pared, is acidified with hydrochloric acid, it loses its color, and oil-drops are precipitated, which solidify in time. These dissolve in sodic hy- drate with a brownish claret * or pale magenta color, which is unal- tered by dilution with water, but turns green on addition of alcohol. The substance melting at 170° is not affected by an aqueous solution of sodic carbonate. The further study of these interesting reactions has been broken off by the summer vacation, but will be continued in thi- laboratory in the autnmn. * A somewhat similar change of color was observed during the action "i ethylbromide on the sodium salt of the bromdinitrophenylmalonic ester. 14 PROCEEDINGS OF THE AMERICAN ACADEMY II. CONTRIBUTIONS FROM THE CHEMICAL LABORATORY OF HARVARD COLLEGE. ON SODIC ZINCATES. By Arthur M. Comey and C. Loring Jackson. Presented June 13, 1838. Although the solubility of zincic hydrate in alkalis is one of the most familiar facts in chemistry, very few attempts, so far as we can find, have been made to determine what compounds exist in such a solution. The reason for this is not far to seek, as the results ob- tained by the few who have studied this subject are so decidedly unsatisfactory, that they are not likely to induce others to take up this line of work. The first important papers in this field appeared in the Annalen der C/iemie unci Pharmacie in 1834, having been brought out by a prize offered from the Hagen-Bucholz foundation for work on zincic oxide. Of the various competitors Laux,* who was most successful in his work on this part of the subject, found that a solution of zincic oxide in caustic alkali, if covered witli a layer of alcohol, gradually deposited little shining crystals, which were easily soluble in water, and, he states, contained equal molecules of zincic oxide and the alka- line oxide (Zn02K2). These crystals were decomposed by heat, giv- ing a white powder, which contained one molecule of alkaline oxide to two of zincic oxide, but no analyses of either of these substances are given. Two other competitors for this Hagen-Bucholz prize, Bonnet t and Sander,J also touch on this subject, but their results are of less importance. Sander, in fact, comes to the conclusion that no defi- nite compound is formed when zincic oxide is dissolved in a caustic alkali. The next paper on the subject was published in 1842, by Fremy, § * Ann. Ohcm. Pliarm., ix. 183. \ Ibid., ix. 181 t Ibid., ix. 177. § Comptes Rendus, xv. 1106. OP ARTS AND SCIENCES. lo who states that the compounds formed by zincic oxide and an alkali were in general deliquescent and amorphous, but by using a potassic hydrate solution of zincic oxide, and adding to it a small quantity of alcohol, long needles were obtained, which he considered a " bi- zincate of potassa." It was immediately decomposed by water into zincic oxide and potassic hydrate. A few years later, in his article in the Annales de Chimie et de Physique,* Fremy states that he has met with great difficulties in obtaining the crystals, and hopes to re- turn to the subject when he has determined the conditions under which they are formed. Neither of his papers contains analyses, and he has never published anything more on the subject, the reason for which we can well understand after our unsuccessful attempts to pre- pare potassic zincates. The work on the ammonic zincates has led to about the same un- satisfactory results, no analyses of laboratory products having been published; but Malaguti t gives an analysis of an incrustation found upon a brick in the vault of a privy, which had the composition 3ZnO. 4NH3. 12H20. The only other research which has approached this subject is one by Prescott,* published in 1880, on the solubility of zincic oxide in caustic alkalis. He found that more alkali is needed for complete solution of the zincic oxide than would be required by the following reaction, ZnS04 + 4 KOH = Zn(OK)2 + K2S04 + 2 IT,0, but this excess was smaller in the case of sodic or ammonic hydrate than with potassic hydrate; also that the excess of alkali could be neutralized in such a solution without precipitating zincic hydrate, until the amount was reached indicated by the reaction given above. Addition of a large quantity of water precipitated the zincic hydrate from the solution, even when it contained the excess of alkali. The effect of dilution and temperature on the solubility were also studied, but the determination of the composition of the substances formed did not come within the scheme of his work. As, therefore, we could find in the chemical literature no analyses of a zincate, with the exception of Malaguti's ammonic zincate, we decided to take up the subject, and fortunately began our work with the sodic zincate, since this proved to be the one of them all which can be most easily prepared. * Ann. Chim. Phys., Ser. 3, xii. \ Cliem. News, xlii. 30. f Comptes Kendus, Ixii. 413. 16 PROCEEDINGS OF THE AMERICAN ACADEMY The principal results which we have obtained can be briefly sum- marized as follows. From a solution of zincic oxide in aqueous sodic hydrate two crystalline sodic zincates can be separated by the action of alcohol; the principal product, which fuses below 100°, has the formula Zn30(.Na4H2 . 17 H20, the other, which does not fuse at 30UJ, is (Zn02NaH)2 . 7 H20. Both substances are decomposed into ziucic oxide and sodic hydrate by water or alcohol. We had hoped at first to extend our work to other ziucates, but, after a number of experiments, have abandoned this intention, as with potassic hydrate no crystalline or definite compound could be obtained, and, although amnionic hydrate gave a product crystallizing in needles, it was ob- tained with difficulty, and proved to be of varying composition. We give, however, at the end of this paper, a brief account of the negative results of these experiments, and of some others in similar directions. Preparation of the Sodic Zincates. The sodic zincates can be prepared by the action of sodic hydrate on either metallic zinc, zincicJoxide, or zincic hydrate, and the jiroduct seemed to be the same in every case. It is most convenient, therefore, to prepare them from zincic oxide, as the metallic zinc dissolves very slowly, long boiling with aqueous sodic hydrate being necessary to pre- pare a sufficiently strong solution. On the other hand, we have not succeeded in preparing the sodic zincates from sodic carbonate, as a mixture of this substance with zincic oxide showed no loss of weight even when kept at a white heat for some time. The method adopted by us consisted in dissolving ziucic oxide in a strong aqueous solution of sodic hydrate,* with the aid of heat, in a flask, which was usually closed with a cork fitted with a set of potash bulbs, to prevent the absorption of carbonic dioxide by the alkaline liquid, but this precau- tion was not absolutely necessary. The solution, after it had cooled, was treated with twice or three times its volume of alcohol, and the mixture, after being thoroughly shaken, allowed to stand securely corked for about twenty-four hours. During this standing two layers were formed, a heavy aqueous solution, and a lighter alcoholic liquid. These were separated, the aqueous solution treated again with alcohol in the same way, and this extraction with alcohol repeated until the heavier portion solidified shortly after it had been removed from the alcohol, which happened usually after the third or fourth extraction. The crystalline mass thus obtained we have called fusihle sodic ziuc- * The sodic hydrate used by us had been purified by alcohol. OF ARTS AND SCIENCES. 17 ate, because it melts below 100°. The second sodic zincate was ob- tained from the alcoholic washings, which were mixed, and allowed to stand in a corked flask, when after some time, which varied from a few hours to several days, white crystals were deposited on the sides of the flask, which gradually increased iu quantity. The formation of these crystals did not occur invariably, but they could often be made to appear by adding more alcohol to the washings. This compound deposited from the alcoholic washings does not fuse even at 300°, anil we shall call it infusible sodic zincate. Analysis of the Fusible Sodic Zincate, Zn306Na4H., . 1 7 II20. This substance is the principal product of the reaction, forming, as nearly as we could estimate, over 90 per cent of the total product. Since both water and alcohol decompose it, a further purification seemed impossible, and we were obliged to analyze it as it was obtained by the precipitation with alcohol, simply drying it by pressure between filter paper under heavy weights. The method of analysis, which we adopted after trying several others, consisted in dissolving the substance in dilute sulphuric acid, and precipitating the zinc by means of a measured quautity of a stand- ard solution of sodic carbonate. The zinc was weighed as oxide. The filtrate was acidified with sulphuric acid, evaporated to dryness, weighed, and then the amount of sodium calculated after subtracting from the total weight of the sodic sulphate the weight of sodic sulphate corresponding to the sodic carbonate added. I. 0.4720 grm. of the substance gave 0.1744 grm. of zincic oxide and 0.2080 grm. of sodic sulphate. II. 0.6420 grm. of the substance gave 0.2302 grm. of zincic oxide and 0.2718 grm. of sodic sulphate. 0.8802 grm. of substance from the same preparation lost at 240° 0.3920 grm. of water, and the dried product gave on heating with chromic oxide in a stream of dry oxygen 0.0342 grm. of water. III. 0.9682 grm. of the substance gave 0.3370 grm. of zincic oxide and 0.3992 grm. of sodic sulphate. 0.8770 grm. of substance from the same preparation lost at 240° 0.4021 grm. of water. i. ii. TIT. Zinc 29.66 28.7. B 27.93 Sodium 14.28 13.72 13.36 Water 44.:. i 15.88 Constitutional "Water 3.88 VOL. XXIV. (N. S. XVI.) 18 PROCEEDINGS OP THE AMERICAN ACADEMY Each of these three analyses was made with a sample from an en- tirely separate preparation, in order to determine whether the substance had a definite composition, and when it is remembered that it could not be purified by crystallization, and was dried only imperfectly by pressing with filter paper, the agreement is as close as could be ex- pected ; but it is obvious that in a case like this the atomic ratios are of much more importance than the percentages, and we have accord- ingly calculated them as follows. Atomic Ratio of Zinc to Sodium in Fusible Sodic Zincate. Zinc Sodium. T. 1. 1.36 II. 1. 1.35 III. 1. : 1.35 The agreement between these numbers proves conclusively that the substance is a definite compound, and that the proportion of zinc to sodium is as three to four. In trying to calculate a formula for it, we have felt much doubt in regard to the amount of water of crystalliza- tion for the reasons given above ; but the one finally adopted by us gives percentages which agree so well with those found, that it cannot be far from the truth, especially as the amounts of water found are about as much higher than those calculated as was to be expected. The constitutional water, on the other hand, comes very high, but we do not have much faith in this determination. Calculated for Zn306Na4H., 17 H20. Zinc 28.28 Sodium 13.30 Water 44.24 Constitutional Water 2.60 To prove that the substance contained water, and not alcohol of crystallization, a combustion of it was made in the usual manner, but only a mere trace of carbonic dioxide was obtained. The formula of this substance, Zn30GNa4H2 . 17 II20, agrees, except in water of crystallization, with that of the substance analyzed by Malaguti (see page 15), which, written in the same way, becomes Zn.,Oi;(NH4)4H2 . 9 H20. This, as has been mentioned already, is the only zincate of which an analysis has been published. We have made only one analysis of another preparation of this sub- stance, which is comparable to those given above ; this gave about the Found. I. II. in. 29.66 28.78 27.93 14.28 13.72 13.36 44.54 45.83 3.88 OF ARTS AND SCIENCES. 19 same percentage of zinc, 29.45, but a much larger amount of sodium, 19.56, which was undoubtedly due to a small quantity of sodic hydrate left adhering to the crystals, as this was the first preparation we made, and therefore was not pressed out so thoroughly as the later ones, after we had become more familiar with the manipulation. Properties of the Fusible Sodic Zincate. The substance as precipitated by alcohol from its solution in aqueous sodic hydrate forms a white mass, made up of radiating crystals, often of considerable size. It fuses at about 70°, but, owing to the diffi- culty of drying it, no attempts were made to determine the melting point accurately. Water decomposes it rapidly and completely, con- verting it into a white insoluble powder, which gave on analysis the following result. o 0.1990 grm. of the substance gave 0.1910 grm. of zincic oxide and no sodic sulphate. Calculated for Found. Zd02H2. ZnO. Zinc 65.72 80.28 77.03 The substance therefore seems to be principally zincic oxide mixed with a slight impurity of the hydrate. Alcohol decomposes it in a similar way, but more slowly, as is shown by the following percentages obtained from the analyses of two preparations (IV., V.), which we had attempted to purify by washing with alcohol. in. IV. v. Zinc 27.93 29.96 33.36 Sodium 13.36 12.27 10.48 III. is one of the analyses already given. The substance for this analysis was only pressed with filter paper. IV. was a sample which had been washed three times with common alcohol, while the substance which had the composition given under V. had been washed four times with absolute alcohol. These numbers show that the action of the alcohol consists in gradually removing the sodium as sodic hydrate, and this point is brought out even more sharply by a comparison of the atomic ratios. Ziuc : Sodium. nr. i. 1.35 IV. 1. 1.16 V. 1. 0.89 20 PROCEEDINGS OF THE AMERICAN ACADEMY It follows from what has been said on this subject, that care must be taken not to continue longer than is absolutely necessary the treat- ment with alcohol during the preparation of the sodic zincate. Al- though the substance is decomposed by both alcohol and water, it seems to exist during the process of mauufacture dissolved in a mix- ture of these solvents in presence of an excess of sodic hydrate, an observation which is confirmed by that of Prescott (see page 15). It is insoluble in ether, and absorbs carbonic dioxide rapidly from the air. At 100° it loses only 12 molecules of its water of crystallization, as is shown by the following analysis. 0.4720 grm. of the substance analyzed under I., when heated to 100° in a stream of pure dry air, lost 0.1510 grm. of water. Calculated for a loss of 12H20. Found. 31.23 32.00 Water Analyses and Properties of the Infusible Sodic Zincate, (ZuOaNaH),.. 7H20. This substance, which crystallizes from the alcoholic washings obtained in the preparation of the fusible compound just described, is formed in comparatively small quantities. As nearly as we could estimate, only a few per cent of the total product consisted of it. As like the fusible compound, it is decomposed by both water and alcohol, no attempt was made to purify it further, but it was analyzed after drying at ordinary temperatures by the method already described (see page 17). I. 0.7470 grm. of the substance gave 0.3124 grm. of zincic oxide and 0.2913 grm. of sodic sulphate; 0.4762 grm. of substance from the same preparation lost at 220° 0.1637 grm. of water. II. 0.6044 grm. of the substance lost at 300° 0.2066 grm. of water, and gave 0.2700 grm. of zincic oxide and 0.2355 grm. of sodic sulphate. Calculated for Found. (Zn0,NaH),7H20. I. II. Zinc 35.32 36.78 35.86 Sodium 12.50 12.62 12.62 Water 34.24 34.37 34.19 The considerable difference between the percentages of zinc is not greater than was to be expected, when the impossibility of purifying OF ARTS AND SCIENCES. 21 the .substance is remembered. Each of these analyses was made with a sample from a separate preparation, and we add the following analy- sis, made early in the work simply to determine the ratio between the zinc and sodium, no care having been taken to dry the substance. III. 0.7025 grm. of slightly moist substance gave 0.2260 grm. of ziucic oxide and 0.1951 grm. of sodic sulphate. The percentages derived from this analysis are of course of no value, but it gives an atomic ratio which agrees with those from the preceding analyses so closely that there can be no doubt that this substance possesses a definite composition. Atomic Ratio of Zinc to Sodium in the Infusible Sodic Zincaie. Zinc : Sodium. I. 1.03 1. II. 1.03 1. III. 1.02 1. A combustion of the substance showed that it contained no alcohol. This substance undoubtedly corresponds to the crystalline body obtained by Fremy (see page 15), who assigned to it the same ratio between the zinc and potassium. Laux (see page 14), on the other hand, ascribed to his crystals, which were soluble in water, the formula Zn02K2, but stated that upon heating these crystals he obtained an amorphous powder, which showed the ratio of 1 : 1 between zinc and potassium ; that is, the same obtained in the crystals by Fremy and us. We have met with no substance corresponding to the soluble crystals of Laux. Properties. — The infusible sodic zincate crystallizes from a .solution in dilute alcohol containing an excess of sodic hydrate in white needles, sometimes over a centimeter long, forming loose radiating groups usually of a conical shape, but occasionally circular or spherical. It does not melt even at 300°, and is decomposed by alcohol, or water, if these solvents are free from sodic hydrate, absorbs carbonic dioxide from the air, but much less rapidly than the fusible compound, and does not lose the whole of its water of crystallization until heated above 200°. "We have not succeeded in finding any other definite compound among the products of the action of sodic hydrate on zincic oxide, and, if any other exists, it can be only in very small quantity. 22 PROCEEDINGS OF THE AMERICAN ACADEMY After we had settled the composition of the sodic zincates, we turned our attention to the study of other zincates, and also tried some ex- periments with magnesic oxide. The results of all this work were negative, but nevertheless we think it best to give a brief statement of what we have done. In all our attempts to prepare potassic zincate we encountered the difficulties already mentioned by Fremy ; in fact, we have not suc- ceeded in obtaining in any experiment the crystals described by him, although we have modified the process employed in a number of dif- ferent ways ; but the solution of zincic oxide in potassic hydrate, when treated with alcohol according to the method which had yielded such good results with sodic zincate, gave only amorphous precipitates, which looked like zincic oxide, but were not wholly free from potas- sium ; as the absence of crystalline form left us no means by which we could judge of the purity of this substance, we did not think it worth analysis. With amnionic hydrate the results looked more promising at first, as the solution of zincic hydrate in amnionic hydrate occasionally gave a small quantity of crystals, after it had been mixed with alcohol and allowed to stand ; but in this case there was no separation of the liquid into two lavers. These crystals looked very much like the infusible sodic zincate described above, but the analyses of four preparations showed that they had no constant composition, the following percent- ages being obtained. I. II. III. IV. Zinc 48.66 45.90 59.96 Ammonia 7.35 4.58 3.67 5.28 In view of these results, it did not seem worth while to continue the investigation. In beginning this research we had hoped, by acting on the sodic zincate with a cobaltous salt, to obtain Rinman's green, and in this way throw some light on the composition of this pigment. These hopes have not been fulfilled, as the zincates were decomposed by alcohol or water, as already stated, and therefore the action could not be carried on in solution, and the melted fusible zincate, when treated with cobaltous chloride, cave only a blackish precipitate with no shade of green. The same result was'obtained when an ethereal or absolute alcohol solution of cobaltous chloride was allowed to act on the zincate. We have also made many attempts to purify Rinman's green, prepared according to the usual method, in order to fit it for analysis, but none OF ARTS AND SCIFNCES. 23 of these have succeeded, the substance being decomposed by solutions of alkalis or acids, iu fact even by a solution of carbonic dioxide under pressure, which dissolved both zincic and cobaltous carbonates, and finally left a blackish gray residue. Although magnesic hydrate does not dissolve in sodic hydrate under ordinary conditions, we thought that possibly a very strong solution of sodic hydrate might have some solvent action at its boiling point, and, upon trying the experiment, obtained long prismatic crystals, which, however, we found contained only a mere trace of magnesium ( 0.39 per cent), and consisted of the crystallized sodic hydrate recently obtained by Cripps,* as shown by the following analytical results. I. 0.5620 grm. of the substance lost 0.2150 grm. of water. II. 0.4115 grm. of the substance gave 0.4585 grm. of sodic sulphate. Found. II. 36.11 The curious point about this observation, which alone makes it worth recording, is that the solution of sodic hydrate used could not be made to crystallize before it was treated with magnesic oxide, but after such treatment crystallized so rapidly that it was impossible to filter it. The experiment was repeated several times, each time with the same result. What the cause of this difference in behavior may be we have been unable to determine, but think that possibly a small quantity of sodic carbonate in our solution of sodic hydrate may have prevented the crystallization, which took place as soon as this was converted into hydrate by the magnesic oxide. Calculated for ] (NaOH)3 4 H.,0 i. Water 37.50 38.26 Sodium 35.93 * Pharm. Jour. Trans , Slt. 3, xiv. 833 (1884). 24 PROCEEDINGS OF THE AMERICAN ACADEMY III. STUDIES FROM THE NEWPORT MARINE LABORATORY. XXI. — A PRELIMINARY ACCOUNT OF THE DEVEL- OPMENT AND HISTOLOGY OF THE EYES IN THE LOBSTER. By G. II. Parker. Presented by Alexander Agassiz, October 10, 1888. The following is a brief statement of the results obtained frotn study- ing the development and histology of the eyes in lobsters. The method in which the optic nerve appears to terminate is so exceptional, that, before making a final publication on this subject, it seems desirable to seek confirmation in the structure of the eyes in other Crustacea. As this will delay the appearance of the paper, and since iu other direc- tions definite conclusions have been reached, it seems advisable to publish now an account of my present conclusions. The first indication of the optic apparatus in the young lobster is a pair of ectodermic thickenings on either side, and slightly in front of where the mouth is to appear. The superficial part of each of these thickenings gives rise to the retina, and the deep part to the optic ganglion. The ganglionic portion is cut off from the retinal portion by the ingrowth of the basement membrane. In certain regions, how- ever, the basement membrane does not cut the connection between the retina and ganglion. These primitive connections persist in the adult as optic nerve fibres. In the eye of an adult lobster each ommatidium consists of at least sixteen cells. Directly under each corneal facet are found two flat lentigeuous cells (corneal hypodermis). Under these are four retino- phoroe, one for each angle of the corneal facet. The retinophora? are extremely elongated, and extend from the deep face of the corneal hypodermis to the basement membrane. From the corneal hypoder- mis to the spindle the four retinophora? are closely applied to one another. At the distal end of the spindle they separate, passing around that structure as fibres. As they approach the basement membrane they converge slightly, and terminate on the retinal surface OF ARTS AND SCIENCES. of that membrane. Under the centre of each ommatidium the base- ment membrane is considerably thickened, and it is on this thickening that the four retinophorse terminate. Each ommatidium has ten pigment cells, — two distal and eight proximal. The distal cells surround the retinophora; in the region of the crystalline cones, and from this region they are continued inward as fibres till they pass through the basement membrane. The eight proximal pigment cells are closely applied to the spindle, the fibres of the four retinophorse passing between them. Seven of these are deeply pigmented ; one is without pigment. The eight cells extend only a short distance in front of the spindle ; the seven pigment cells proper are continued inward as large fibres through the "basement mem- brane. In addition to the sixteen cells just described, each omma- tidium has two or three irregular cells filled with a pigment, brownish by transmitted, white by reflected light. These cells envelop the proximal half of the spindle, and extend to the basement membrane. The spindles themselves do not reach the basement membrane. The sixteen cells already described are ectodermic in origin. The two or three additional cells may be from either an ectodermic or me- sodermic source, but the evidence thus far gathered points decidedly to their ectodermic origin. The basement membrane, as was previously mentioned, has a thick- ening in it under each ommatidium. Around a given thickening there are four openings through the membrane. Each opening, however, is placed between two thickenings, so that in reality only half of each cluster of four openings belongs to a given thickening. There are two classes of openings, one with a single small and four large fibres, and another with one small and three large fibres, passing through. Each thickening has two of each class accompanying it. Of the fourteen large and four small fibres passing through the four open- ings, only one half, or seven large and two small fibres, belong to a given ommatidium. These represent the seven deep and two super- ficial pigment cells. After passing through the basement membrane, these fibrous ends of the pigment cells thicken considerably, and, having grouped themselves in bundles, pass inward, constantly di- minishing in calibre, till they reach the optic ganglion. The optic nerve between the retina and first optic ganglion is composed oi these fibres bound together by a small amount of connective tissue. All attempts at isolating any other form of fibres have failed, and it would therefore seem that the fibres of the optic nerve terminal' these nine pigment cells. 26 PROCEEDINGS OP THE AMERICAN ACADEMY Investigations on Light and Heat, made axd published wholly or in pakt with Appropriation from the Ruiiford Fund. IV. ATMOSPHERIC ECONOMY OF SOLAR RADIATION. By Arthur Skarle. Presented October 10, 1888. The terrestrial atmosphere acquires energy from the solar radiation by direct absorption, by the absorption of terrestrial radiation, and by conduction from terrestrial solids and liquids. It loses energy in three corresponding ways ; by radiation into space, by downward radiation, and by conduction. As some time must elapse between the acquisition and the loss of any given amount of energy, the air always contains a certain accumu- lated store of activity resulting from the solar radiation, and manifested in warmth, expansion, and movement. It is a general and apparently well founded belief, the reasons for which need not here be repeated, that terrestrial temperatures are maintained to a great extent by the aid of this atmospheric accumulation of energy ; so that a far lower temperature would prevail in the absence of the air. The hypothesis which has been current until recently with regard to this protective action of the atmosphere depended upon a supposed effect of selective absorption, which has now been largely, if not entirely, disproved by Langley's experiments. The supposition, indeed, was always some- what difficult to reconcile with the familiar fact that celestial bodies appear redder at a small than at a great altitude ; since, so far as the visible spectrum is concerned, this proved that among the constituents of the atmosphere there were some, abounding in its lower strata, which absorbed radiations of small wave-length more readily than the others. Hence it did not seem probable that the radiation from ter- restrial substances the temperature of which was far below red heat would be absorbed by the air with peculiar readiness, and thus pre- vented from escaping into space. This reasoning, however, could not be conclusive, and actual experiment was required to overthrow the assumption that the air was much more transparent to solar than to terrestrial radiation. As we are now obliged to abandon this assumption, it is natural to OF ARTS AND SCIENCES. 27 inquire whether the known phenomena of conduction will suggest a better explanation of the protective action of the atmosphere than can be afforded by the observed laws of absorption and radiation. By con- duction, fluids acquire heat most readily when hot bodies are applied to their lower surfaces, in consequence of the convection currents thus established. On the other hand, the application of cold bodies to their lower surfaces, as it does not originate such currents, withdraws their heat only by the much slower process of conduction through their own substance. Hence, an undisturbed atmosphere will acquire heat more readily by contact with warm ground than* it loses heat by contact with cold ground. Part of the heat thus acquired might have been conducted to adjacent portions of the ground in the absence of the atmosphere, but another portion would have been directly radiated into space. It now becomes a question whether the atmosphere thus heated will discharge its recently acquired energy by radiation into space as readily as the ground would have done in the absence of an atmosphere. Without undertaking to decide this question, it will here be assumed that the heat acquired by the atmosphere from warm ground will not be radiated as readily as it would have been radiated by the ground itself. Since it will not be readily lost by conduction, in the absence of violent agitation of the air, for the reason already given, the hypoth- esis seems admissible that it tends to accumulate, and to increase the stock of energy contained in the atmosphere much more efficiently than can be done by the processes of absorption and radiation. If we admit the existence of this tendency, we have next to consider what natural provision can be suggested for checking its effects when they have attained a certain magnitude ; for it is obvious that they do not increase indefinitely. If we suppose atmospheric energy to be manifested only as heat, its accumulation would ultimately be checked by an increasing radiation from terrestrial solids and liquids ; if mani- fested only by expansion, it is perhaps possible that portions of the atmosphere would be driven off into space, carrying away the energy mechanically ; but a more immediate check is afforded by that portion of the accumulated energy which displays itself as atmospheric move- ment. When the winds have attained a certain degree of violence, they disturb the portions of the air which would otherwise remain stagnant over the colder parts of the ground, and the process of heat- ing the atmosphere from beneath gradually ceases to retain sufficient advantage over that of cooling it from beneath to permit a furtbej accumulation of energy. 28 PROCEEDINGS OF THE AMERICAN ACADEMY If a permanent increase should take place in the amouut of solar radiation, it is clear, upon the present hypothesis, that some time would elapse before the increasing agitation of the atmosphere put an end to the increase of its energy. The stock of atmospheric energy in gen- eral, and that part of it manifested as heat, would thus be permanently increased. The terrestrial temperature would be raised, tempests would be more frequent and severe, and the entire atmosphere would probably occupy more space. On the other hand, a permanent diminution in solar radiation would tend to diminish the agitation of the air, and, although the terrestrial temperature would decline, this loss of temperature would not be so great as that which would have occurred if the winds had maintained their previous force. The atmosphere, accordingly, acts as a check upon extreme variations of heat and cold ; when little heat is received, it will be better economized than when the supply of heat is excessive, although particular regions may have, in the former case, a very severe climate. The observed association of extreme cold with still air, and the greater violence of tempests in the heated portions of the world, on the whole, are among the facts tending to support the hypothesis above explained. In the present discussion, the consequences resulting from the com- pressibility of the atmosphere have thus far been neglected, and what has been said above would be equally applicable to an atmosphere wholly incompressible. But in such an atmosphere the distribution of heat would materially differ from that actually observed. As a con- vection current rises, the air composing it expands, from the removal of pressure, and its energy largely ceases to exhibit itself as heat. Under these circumstances, the solid and liquid particles carried up with it are reduced in temperature, and made less capable of radiation into space than before. It may likewise be supposed, indeed, that the expanded air itself will have its previously small capacity for the dis- charge of its energy into space still further diminished. The addi- tional tendency to retain energy, thus suggested, would demand more consideration if the discharge were effected by any process of the nature of conduction ; that is, if the outer surface of the atmosphere were chiefly instrumental in the process. In this case, the expansion of the ascending air would be a highly important means of delaying the escape of energy received by conduction from warm ground ; and an incompressible atmosphere might not in any considerable degree protect the planet which it surrounded. OF ARTS AND SCIENCES. However slightly the expansion of ascending currents may cluck the escape of energy, it is certain that the subsequent descent of the air composing them must exhibit more and more of its remaining energy in the form of heat. This phenomenon is generally recognizul by recent writers upon meteorology, and there can be little doubt that it powerfully affects the relative climates of places at different alti- tudes. The climate of an elevated region is colder than that of the sea level, because a smaller part of the atmospheric energy appears there as heat, and a larger part as expansion. Whether this is a suffi- cient explanation of the observed difference of climate can scarcely be determined until we have more knowledge with regard to the actual extent and velocity of the convection currents of the atmosphere. The considerations above set forth indicate the conclusion, that the effect of conduction, aided by convection currents, is probably an im- portant means of maintaining the present terrestrial temperature, as well as the present distribution of warmth in different latitudes and at different elevations. Jf this conclusion should hereafter find a more satisfactory basis in observation and experiment, it would have some interesting applications to the climate of the larger planets. Their extensive atmospheres, subjected to a powerful force of gravitation, may perhaps enable them to economize very efficiently the compara- tivelysmall quantity of solar radiation which they receive. Another branch of inquiry connected with the same general subject relates to the conditions of temperature in different parts of the ocean. The atmospheric and oceanic currents prevailing in former times are also frequently discussed by geologists. If the atmospheric convection currents have the effects here attributed to them, they may help to account for some of the unexplained phenomena of prehistoric climates, the evidences of which have remained to the present day. 30 PROCEEDINGS OF THE AMERICAN ACADEMY V. THE CRYSTALLINE STRUCTURE OF THE COAHUILA IRONS. By Oliver W. Huntington. « Presented October 10, 1888. In a previous paper on the crystalline structure of iron meteorites,* the author described two cleavage crystals broken from a specimen of the Butcher meteorite (Coahuila), but, from the compact nature aud softness of the iron, no further examples of cleavage were at that time obtained. Recently, however, on examining a large number of small sawed slabs of the same iron in the Harvard Collection, one slab was found to be intersected by an angular crack, as shown of actual size in Fig. 1. On taking the slab in the hand, it was found that the two portions could be readily separated by a slight pressure, and the Fig. 1. surfaces, though considerably oxidized, showed sharply defined crystal faces extending through the entire thickness of the plate (about six millimeters) and forming angles of about 132° and 90°. As this cleavage was so very striking, an attempt was made to break another slab artificially. It was mounted in a vice for the purpose, and the projecting portion struck with repeated blows of the * American Journal of Science, 3d series, vol. xxxii. pp. 281-303. OP ARTS AND SCIENCES. 31 hammer. The slab broke readily along the jaws of the vice, exhibit- ing a superb crystalline cleavage, the faces of the crystals having a most brilliant lustre, almost like antimony, and, though the iron was soft enough to cut with a knife, yet some of the single cleavage faces were nine or ten millimeters in extent. These crystal faces usually formed angles of about 132°, or else right angles, though in some parts there were sharp projecting points, formed by the meeting of two rectangular planes with a third set obliquely. Furthermore, all the faces were most beautifully striated by numerous sets of fine parallel lines, easily distinguished by the eye, generally making angles with each other of 127°, 90°, and 53° respectively, a few of the lines appearing to be parallel to the intersections of the faces. Fig. 2 shows enlarged one set of crystal faces as they appeared on the surface of fracture. The planes were absolutely perfect, and lar^e enough to be readily measured with an application goniometer. Thus Fig. 2. Fig. 3. it was found that the plane B made with C a right angle, B and A an angle of about 132°, A and C an angle of about 109°; and the small plane D, set obliquely on the solid angle thus formed, made an angle of about 125° with B and C, and 164° with A. The plane E and the one parallel to it were the sawed faces of the slab. All the other planes forming the surface of fracture were parallel to the ones shewn in the figure, and they could all be referred to faces of the twin cube, as shown in Fig. 3, where the corresponding faces are lettered the same and placed in a parallel position. The striations already men- tioned appeared most markedly on the face A, that being the largest, and therefore the one most easily examined. Fig. 4 shows, on a large scale, this plane referred to the face of a cube, only the most prominent of the striations being represented, in order to preserve clearness in the figure. It will be seen by the 32 PROCEEDINGS OF THE AMERICAN ACADEMY diagram, that all the lines follow the intersections of the different members of an ordinary cube twinned on all of the trigonal axes, and 'OV\d IVlj Mesb p^o-Tl y Y»ounceaJ Fig. 1. there were no markings on the face which could not be thus referred. However, on examining the triangular face D of Fig. 2, it appeared in marked contrast to the face just described, as all the markings were parallel to the octahedral edges, thus forming simple triangles. A large number of specimens of the Butcher iron were afterwards examined, and they all exhibited the same crystalline cleavage on a fresh fracture. Moreover, it made no difference in what direction the slab was broken, the planes always showed a prevalence of the 132° angle (theoretical angle 131° 48' 37"), with here and there the sharp projecting points already referred to, but, contrary to expectation, the simple cube angles seldom appeared, though in some parts they were evident. It now appeared important to examine the cleavage of the Sancha Estate or Saltillo iron (Santa Rosa), which has been considered part of the same meteorite as the Butcher specimens. For this purpose Mr. S. C. H. Bailey sent us a wedge-shaped slab which had been sawed to a thin edge and then broken, giving a surface of fracture about seventy millimeters long and two millimeters wide in the thick- est part, diminishing towards the two ends. The crystal faces over this surface were very small, and appeared to have a grayer color than those of the other irons. When this surface was examined under a low power microscope, the crystals were found to be all simple cubes, looking exactly like a specimen of galena, and, instead of the faces being striated as in the Butcher irons, they exhibited the little crys- talline projections and depressions which are so characteristic of some alloys. However, on the face of the slab there was the suggestion of two cracks crossing at angles of about 132° and 53°, and an attemnt OF ARTS AND SCIENCES. 33 was made to break the specimen parallel to one of these cracks, with the expectation of getting the planes already described in the previous iron. When the slab was mounted in the vice and struck with the hammer, there at once appeared on the surface numerous very fine cracks parallel to the two directions just mentioned, and at once suffjrestine l DO C the two sets of fine parallel lines which are first brought out on an etched surface of this iron but are obliterated by the continued action of the acid. Finally, the slab broke, but exhibited only a siucde plane through the entire extent of the fracture (33 mm. in length by G mm. in breadth), and, instead of being striated, there was developed a very striking flaky surface as if little thin layers had resisted the cleavage. parting at last with irregular edges more or less separated from the main surface. An attempt was next made to break the slab at ri-ht angles to the first direction, in order to get other crystal faces; but, instead of breaking along the edge of the vice, as a Butcher specimen readily would have done, the Saltillo iron broke again with the same single cleavage plane, at right angles to the desired direction and running directly down into the jaws of the vice, entirely regardless of the way it had been clamped and the blows of the hammer applied. Every attempt to break the slab gave the same result. It would only break in the two directions indicated by the first fine cracks, and corresponding to the angle that a cube face makes with the adjacent face of a twin cube, and always broke along a single plane exhibiting the flaky surface already mentioned. The only way of getting a different fracture was to saw the specimen to a thin edge, and so force it to break in the desired direction, and then it would present a surfaa fine cubes wholly different in character from the large striated faces of the Butcher irons. Just at this time we received from Ward and Howell a large slab of a new meteorite found in Allen County, Kentucky, and the whole character of this iron, including the etched surface, so closely resembled the Coahuila specimens that we were interested to see whether it would show any striking cleavage. Ward and Howell kindly Furnished ua with some small slabs, and, on breaking them in the way already described, they showed exactly the same characters as the Saltillo iron. The fine parallel cracks appeared under the first blow- of the hammer, and then the slab broke regardless of the way it was clamped in only the two directions at angles of about 132 and ■'>'■'> , presenting a single cleavage plane with the marked flaky appearance characteristic of the Saltillo iron. vol. xxiv. (n. s. xvi.) 3 34 PROCEEDINGS OF THE AMERICAN ACADEMY Exactly the same result was obtained in breaking slabs of the Maverick County* iron, and also the iron from Chattooga County, Georgia,! both of which were described as independent falls, although closely resembling the Coahuila specimens. Now it will be borne in mind that the Coahuila irons form a group by themselves, their etched surfaces appearing so markedly different from any other known meteorite, and for this reason, together with a resemblance in composition, they have commonly all been considered to belong to one fall. But, after examining the structure of the Butcher irons and that of the Saltillo or Saucha Estate as exhibited by the cleavage, it is impossible to class them as portions of a single original mass. And, on the other hand, when we compare in the same way the Saltillo iron with those of the Allen County, Chattooga County, and Maverick County meteorites, it seems equally impossible to believe that they did not at one time form a single meteorite, espe- cially when they also resemble each other in composition as shown in the following analyses, though to be sure it is hard to tell how far such analyses can be depended upon as a means for comparison or distinction of irons. % Allen Co. § Santa Rosa. || Maverick Co. IT Chattooga Co, Iron 94.32 95.82 94.90 94.63 Nickel Cobalt 5.01 trace 3.18) .35 \ 4.97 .21 Sulphur .34 • . . . • > • . .... Phosphorus .16 .24 .... .21 Carbon .12 .23 99.95 99.59 10U.U0 99.99 That these masses were found in places so remote from each other does not seem to preclude their having belonged to one individual, since the Rochester meteorite was seen to pass over the States of Kansas, Missouri, Illinois, Indiana, Ohio, and is supposed to have passed over Pennsylvania and New York, and thence out to sea, drop- ping fragments in its course. It therefore is possible that at some remote period an enormous iron meteorite may have passed over the * Amer. Jour. Sci., 3d series, vol. xxxii. p. 304, October, 1886. t Ibid., vol. xxxiv. p. 471, December, 1887. t Ibid., vol. xxxiii. p. 500, 1887. § Ibid , 2d series, vol. xix. pp. 160, 101, May, 1855. || Ibid., 3d series, vol. xxxii. p. 304, October, 188G. IT Ibid., vol. xxxiv p. 472, December, 1887. OF AETS AND SCIENCES. 35 entire breadth of the Uuited States, the main mass reaching Mexico, but large fragments breaking off and falling during its passage across the country. Two irons commonly classed under the general head of" Coaliuila'' have not been included in the above consideration. They are labelled in the Harvard College collection, " Hacienda de Concepcion," * and " San Gregorio Iron, Chihuahua, Mexico," f both bearing the signa- ture of Dr. H. B. Butcher. The specimen of the Hacienda de Con- cepcion was small, and had been hammered, so that its structure could not be conclusively studied, but it appeared to be markedly different from any of the other Mexican irons. The San Gregorio iron, of which there were numerous specimens, ap- peared to be made up of very striking octahedral plates, and therefore must be placed among a very different class of irons from the Coahuila group, which it has been the purpose of this paper to describe. * Amer. Jour. Sci., 2il series, vol. xix. p. 1G3, 1855. t Ibid., 3d series, vol. ii. p. 336, 1871. 86 PROCEEDINGS OP THE AMERICAN ACADEMY VI. CONTRIBUTIONS TO AMERICAN BOTANY. By Skreno Watson. Presented October 10, 1888. 1. Upon a Collection of Plants made by Dr. E. Palmer, in 1887, about Guaymas, Mexico, at Muleje and Los Ayigeles Bay in Lower California, and on the Island of San Pedro Martin in the Gulf of California. The peninsula of Lower California and that portion of the Mexi- can mainland which borders the intervening Gulf, though reputed a sterile land, have always wherever they have been explored yielded a rich harvest of novelties to the botanical collector. Much therefore was expected from so keen and careful a collector as Dr. Palmer, when he undertook to spend a season at Guaymas, and from that point to explore such other places as might be accessible to him. Though the season of 1887 proved very unfavorable on account of its dryness, the result has nevertheless been very satisfactory. Of the 415 native species collected, 89 species, or more than one fifth, are wholly new, and many others are of great interest in various respects. The larger part of the collection was made about Guaymas itself, which town lies on the eastern side of the Gulf of California, in the State of Sonora, in lat. 28° N., and 250 miles south of the United States boundary. It is hemmed in closely by very rocky hills and low mountains (of 1200 to 1500 feet altitude), intersected by narrow val- leys. The artificially watered gardens, with their irrigating ditches and brush fences, protecting and favoring the growth of numerous native plants, the rocky islands in the harbor, and the valleys and mountains around, wore all alike searched. Dr. Palmer remained here from the middle of dune to the middle of November, during which time there were only occasional slight showers, which commenced in August. The sp< cies obtained here numbered 283, of which 40 were also OF ARTS AND SCIENCES. :,7 found in other localities.* Muleje, upon the western side of the Gulf, 90 miles from Guaymas, is described as in a dry, barren, and moun- tainous region, where except in the very short rainy season the only green vegetation to be seen is along the banks of a small crei k. This place was visited early in dune, and again late in December. Of the 49 species collected here, 24 occurred elsewhere, mostly at Guaymas. Los Angeles Bay, also on the peninsula, about 200 miles northwest from Guaymas, was visited at an unusually favorable time, after a rain which was the first that had fallen in twenty-two months and when vegetation was in full bloom. The surrounding country is very mountainous, some of the ridges having an altitude of 2,000 to 3,000 feet. About a month was spent here (from November 22 to December 20) and 112 species were collected, of which 23 had been found previously. The remaining station was the island of San Pedro Martin, lying about 80 miles northwest from Guaymas. This island has a circumference of about 4i- miles and an altitude of 1,200 feet, and is exceedingly rough and rocky, intersected by canons and largely covered with guano. A very few small fig trees were found, but the only useful wood is furnished by the Ccreus Pringlei, which forms almost a forest over the summit. During an eight days' stay (Octo- ber 24 to November 5) only 19 species were collected, of which seven were not peculiar to the island. The characteristics of the flora of the region bordering the Gulf of California, so far as shown by this collection, are for the most part those common to the flora of the whole arid region of the interior, from southeastern California, Arizona, and New Mexico southward into Mexico, distinct in a great measure from that of California proper on the one side, and that of the Gulf States on the other Nearly or quite two thirds of the sjiecies range northward beyond the Mexican boundary. In the mountains about Guaymas we find a < siderable number that are identical with or allied to species thai have recently been collected by Pringle and Palmer in the mountains Chihuahua. We have here also probably the northern limit on the Pacific coast of the tropical or subtropical genera Rkizophora, fftema- toxyloiu Portlandia, Oitharexylum, Pedilanthus, Ficus, etc. The pro * Cultivated and introduced plants are not included in the numbers al piven. Sixteen species of the collection are considered of this character, viz. : Oligomeria glaucescens, Portulaca i, Gossypium herbaceum, Trip) foliuta, Melilotus parviflorus, Tamarindus Tndicus, Capsicum ca . C. an- mtum, Crescentia alata, B'tu vulgaris, Panicum sanguinale, Sorghum II El usine Mgyptiaca, E. Indica, Eragrostis major, and Lolium 38 PROCEEDINGS OF THE AMERICAN ACADEMY portion in which the several orders are represented in the collection is somewhat remarkable. Of the 415 species, one fourth are equally divided between the Gru mi 'nece (50) and the Compositce (50). Another fourth includes only the four orders Leguminosce (44), Euphorbiacece (32), Malvaceae (17), and Solanacece (15). These are followed by the Ngctaginaceoe (15), Convolvidacece (13), Asclepiadacece (10). and 53 other orders with still fewer species. The important orders lianunculacece, Rosacece, Saxi'fragacece, Umbelliferce, Ericaceae, Ouptdiferce, Coniferce, and Orchidacece are wholly unrepresented. Excluding the Cypera- ccce and Graminece, there are only five endogenous species in the entire collection. For the determination of the species the Cyperaceae were referred to Dr. N. L. Britton, Curator of the Torrey Herbarium, the Gra- minel ex- posed rocks high in the mountains about Guaymas. (-"'.*.) POROPHYLLUM CRASSIFOLIUM. SuffYuticose, much branched and compact: leaves somewhat fleshy, linear, attenuate al base, gland- tipped and often setosely apiculate, \ to 1 inch loug or often less: heads terminal on the short stout brauchleu : bracts broad, obtuse, 8 or 4 lines long, the yellowish flowers nearly twice longer: ach lines long. — Apparently near P. tridentatum, Benth., from Magdalena Bay, but the leaves are wholly entire and the flowers are much Ion 58 PROCEEDINGS OP THE AMERICAN ACADEMY than the involucre. Muleje, on rocky hills and on sandy beaches near salt water; also collected by Dr. Palmer in 1870 on Carmen Island. (423.) Nicolletia Edwakdsit, Gray. Annual; ray white with a red- dish stripe on the outer side. Common on sandy plains and stony ridges at Los Angeles Bay. (4G'J.) Dtsodia porophtlloides, Gray. Mountain-sides, Los Angeles Bay. (531.) Pectis prostrata, Cav. In gardens at Guaymas. (145.) Pectis angustifolia, Torr. The awnless form. Ravines near the beach; Los Angeles Bay. (G57.) Pectis (Pectothrix) Palmeri. Closely resembling P. papposa, but the solitary setas at the base of the leaves more slender, the peduncles longer (1 or 2 inches), the longer hairs upon the achenes straight and slightly thickened upward (not at all uncinate or capi- tate), and the pappus merely scabrous (not barbellate). — Hillsides near Guaymas. (652, 653.) What may perhaps be a form of this with the pappus reduced to an irregular subfimbriate margin was col- lected on a rocky island in Guaymas harbor. (655.) Pectis Coulteri, Gray. Low and diffuse, somewhat viscid- pubescent, with leaves an inch long or less. — In gardens at Guaymas and on islands in the harbor. (143, 654.) Pectis punctata, Jacq. In sandy ravines and high upon the mountains about Guaymas. (224. 656.) Triciioptilidji incisum, Gray. Stony ridges at Los Angeles Bay. (563.) Bebbia juncea, Greene. Flowers yellow, very fragrant. Sandy ravines at Muleje and Guaymas. ('^•) Peucephyllum Schottii, Gray. A shrub, 3 or 4 feet high. Stony ridges at Los Angeles Bay. (587.) Senecio Lemmoni, Gray. Mountain-sides near Los Angeles Bay. (577.) Perezia Palmeri. Tall and branching, green and minutely glandular-pubescent throughout: leaves thin, oblong-lanceolate, acu- minate, sessile and cordate at base, very acutely dentate and denticu- late, 6 inches long by 2 wide or smaller: heads few on the branchlets, pedunculate, ^ inch long, many-flowered; involucre campanulate with thin acute bracts, the lower ovate and subacuminate : flowers "lilac": achenes glandular-puberulent. — To be grouped with P. patens and P. carp/to/epis. On mountainsides near Los Angeles Bay ; rare. (527.) OF ARTS AND SCIENCES. 59 Tkixis angustifolia, DC, var. latiuscdla, Gray. A very compact shrub. 2 or 3 feet high, common upon the summit of S. Pedro Martin Island. (408.) Lobelia splendens, Willi Near a waterfall in the mountains above Guaymas. (301.) Jacquinia pungens, Gray. "San Juanico " ; a small evergreen tree, 12 to 15 feet high, the wood useless even for fuel. The globose fruit is 8 or 9 lines in diameter, the seeds several, oblong-peltate, im- bedded or enclosed in the resinous-waxy placenta. The flowers are used by the Indians to give a durable yellow color to the palm-leaves used in making baskets, etc., and they are also strung like beads and worn for ornament. About Guaymas. (G9.) Sideroxylon leucopiiyllum. A small tree, 5 to 8 feet high and sometimes a foot in diameter : leaves finely white-tomentose on both sides, oblong-elliptic or -lanceolate, obtuse or acutish, subcuneate at base, short-petiolate, 2 inches long or less: flowers rather crowded in the axils on short pedicels, 5-merous ; calyx tomentose, campanu- late ; corolla greenish yellow, 2\ lines long : staminodia petaloid, en- tire, broadly lanceolate, equalling the corolla: ovary densely villous. — The fruit was not collected. The wood is hard, burning with much smoke. In deep canons near Los Angeles Pay. (516.) Vallesia dichotoma, Ruiz & Pavon. A large evergreen bush with white fruit, which is eaten by children, and its juice is used for inflammation of the eyes. This specific name is adopted as the oldest in the genus, in preference to the later V. glabra of Link. The spe- cies so named that is found in Florida and the West Indies appears to have longer pedicels, a larger calyx, a longer corolla with longer nar- rowly oblong lobes, and the leaves oblong rather than lanceolate. — In garden hedges and sandy ravines about Guaymas and Muleje. (32.) Haplopiiyton cimicidum, A. DC. High in the mountains about Guaymas. (228.) Philibertia linearis, Gray, var. heterophylla, I rray. Flow- ers creamy white; fruit 3 inches long. At Muleje and Guaymas. (5.) Philibertia Pavoni, Ilemsl. Climbing. 5 to 0 feet high : lea very white-tomentose beneath; flowers white. The same as :; l<> Palmer, 1886. In ravines at Guaymas. (195.) Asclepias subulata, Decaisne. " Vumete"; til'' juice an active emetic. Common in dry arroyos about Guaymas. (■><.) Asclepias albicans. Erect, 4 feet high, white-puberulent : lea verticillate in threes, very narrowly linear, mostly decid B : umb-h short-pedunculate, many-flowered, pube at, the pedicels half an inch 60 PROCEEDINGS OF THE AMERICAN ACADEMY long : lobes of the greenish corolla tinged with brown, narrowly ob- long, acute, nearly 3 lines long ; column short ; hoods yellowish, shorter than the anthers, somewhat thickened dorsally and bluntly beaked, the sides subquadrate and the nearly straight subulate spur scarcely exserted : follicle erect on the erect pedicel, 4 inches long, smooth. — In rocky ravines near Los Angeles Bay. (588.) Metastelma Pkinglei, Gray, var. (?), with longer and acuter calyx-lobes and the filiform lobes of the crown somewhat shorter ; flowers yellow. — Hillsides near Guaymas. (626.) Metastelma albiflora. Glabrous or nearly so ; stems twining, 4 feet long : leaves petiolate, narrowly oblong to linear, short-acumi- nate, 6 to 10 lines long: flowers white, in sessile fascicles, the pedi- cels very short: calyx-lobes narrowly linear, acuminate ; corolla a half longer (nearly 2 lines), densely villous within, the lobes narrowly lanceolate ; crown of 5 very narrow and attenuate scales attached to the very short column and equalling the distinct corneous cuneate- obcordate anthers ; appendage of the anthers oblong. — Exposed cliffs near Guaymas. (223.) Pattalias* Palmeri. Stems slender, several from a rather thick branching rootstalk, slightly puberulent or glabrate, a foot long or more : leaves very narrow, 2 inches long or less, sessile, acute : flow- ers (2 to 6) yellow, on pedicels 1 or 2 lines long or less : corolla 2 lines long, twice longer than the calyx: lobes of corona ovate, attached to the column at the base of the anthers, lanceolate, acute, half the length of the stout conical beak : follicle 4 inches long by 3 lines broad, narrowed at base and long-attenuate above. — Near a sandy beach at Muleje. (424). — A second species of this genus is P. angustifolius, a Sonora plant doubtfully referred by Dr. Torrey in the Mexican Boundary Report to Metastelma, and more recently by Dr. Gray to the extra-tropical South American genus Melinia. It is of similar habit, but has petiolate leaves, a longer calyx, the crown at the base of the column, the anther-tips much more conspicu- ous, and the beak of the stigma narrow and columnar. * PATTALIAS, a new genus of the Asclepiadacece, of the Metastelma group. Calyx 5-parted, the lohes narrow, acuminate, eglandular. Corolla becoming opcn-campanulate, 5-parted, narrowly convolute in the bud, naked, the lobes lanceolate. Crown of 5 distinct fleshy entire lobes inserted upon the short column, exceeding the short anthers. Stigma surmounted by a prominent conical or columnar entire beak, exceeding the membranous erect tips of the anthers. Follicles smooth, slender. — Low twining herbaceous perennials, with narrowly linear opposite leaves, and small flowers shortly pedicellate in an axil- lary nearly sessile umbel. OF ARTS AND SCIENCES. CI Rothrockia cordifolia, Gray. In shady ravines, etc., about Guaymas. (213.) Himantostemma Pringlei, Gray. In an orange grove at Guay- mas. (318.) Marsdenia edulis. Stem frutescent, with corky bark when old, climbing: leaves rather thick, uudulate, ovate-lanceolate, acuminate, rounded at base, glabrous, 1 to 4 inches long, petiolate : flowers in a nearly sessile simple or compound umbel, the calyx and short pedicels pubescent: calyx-lobes ovate, acutish ; corolla cream-color, rather fleshy, 2£ lines long, cleft to the middle, the throat very villous: lobes of the crown subulate-acuminate, a little shorter than the tall conical bifid summit of the stigma : fruit ovate, obtuse, smooth, 3 inches long; seeds suborbicular, 3 lines long. — "Talajote"; the green fruit is eaten. On sandy saline mesas near salt water, Guaymas. (150, 658). Gilia (Eugilta) Palmeri. Annual, erect and branched, some- what pubescent with floccose tomentum especially in the axils, a foot high : leaves alternate, very narrowly linear, entire, pungent, 1 \ inches long or less: pedicels scattered, about an inch long: corolla " violet," 5-parted, the spreading lobes oblanceolate, acute and den- ticulate, 5 lines long, the calyx half as long: filaments very slender and anthers small : capsule oblong, equalling the calyx ; cells several- seeded. — Near G. rigidula. On stony ridges near Los Angeles Bay. (593.) Ellisia chrtsanthemifolia, Benth. Shady mountain-sides near Los Angeles Bay. (580.) Phacelta crenulata, Torr. A small-flowered form. Stony ridges at Los Angeles Bay. (592.) Piiacelia (Eutoca) pauciflora. Annual, setosely hispid, lax and very slender, a foot high or more : leaves (except the uppermi pinnately divided, the oblong segments pinnatifid: dowers few, shortly pedicellate in a short loose simple or geminate raceme: calyx-lobes setosely hispid, linear-oblanceolate, 2 becoming 4 lines long, equalling the corolla (scarcely 3 lines long) ; appendages narrow and united at base over the filament: stamens and style included, the style cleft to the middle: capsule ellipsoidal, obtuse, 2 lines long, 8-seeded. — Tech- nically of the Eutoca section, hut closely related to P. hispida. On mountains near Los Angeles Bay. ( 583. ) Cordia Grf.ggii, Torr., var. (?) Palmeri. Leaves somewhat larger (5 to 9 lines Ion?), ovate-oblorig, acute to obtuse, more abruptly cuneate at base on a slender petiole 2 to 1 lines long, and with m 62 PROCEEDINGS OF THE AMERICAN ACADEMY numerous serratures : corolla more broadly funnel-form, the limb 12 to 15 lines broad; calyx-teeth slender, nearly equalling the tube. — A shrub, 5 to 8 feet high, in gravelly ravines about Guaymas. (112.") Cordia (Myxa § Spiciformes) Palmeki. A shrub, 4 or 5 feet high, the young branches and lower side of the leaves finely pubescent : leaves oblong-lanceolate, attenuate at base, very shortly petiolate, acut- ish, rather coarsely toothed, scabrous above, 1 to 2^ inches long by 3 to 6 lines broad: spikes pedunculate, loose, tomentulose, 1 to 1A inches long: corolla 3 lines long, twice longer than the calyx: fruit red, ex- serted, nearly 3 lines long. — " Yerba del pasmo." In ravines in the high mountains above Guaymas. (281.) Bourreria Sonorje. A shrub, about 10 feet high, with stout very leaf}' branches : leaves very roughly papillose-scabrous above, soft-pubescent beneath, obovate to oblong-spatulate, obtuse or retuse, attenuate to a very short petiole, entire, 1^ inches long or less : flow- ers few on slender pubescent pedicels 2 to 5 lines long : calyx cleft to the middle, the deltoid lobes acute, half the length of the corolla- tube ; corolla greenish yellow, puberulent, 5 lines long, the lobes oblong, acute; filaments glabrous, exserted : fruit black, depressed- globose, 2| lines broad. — Near a waterfall in the mountains above Guaymas. (289.) Coldenia* angelica. Annual, prostrate, wide-spreading, some- what hispid : leaves ovate to rhombic, acute, strigose-hispid on the margin and finely appressed-pubescent, entire or the margin sinuate, irregularly 2-3-nerved each side of the midvein : calyx nearly 2 lines long, the narrowly acuminate hispid lobes nearly twice longer than the tube ; corolla " mauve," 3 lines long ; filaments slender, adnate nearly to the middle, with a short obtuse prominent appendage at * Two other species of this genus may be defined as follows : — C. brevicalyx. White with a close fine pubescence and scarcely at all hispid : leaves very like those of C. angelica in form and veining: calyx very short (1 line), the broadish acute lobes shorter than the tuhe; corolla 2 lines long; filaments slender, slightly dilated below the insertion: nutlet subglo- bose, much smaller; embryo similar. — Confused with the true C. Palmeri as to characters of flower and fruit. Ou the lower Colorado (Palmer, 1869; C. Palmeri, Gray, Proc. Am. Acad. 7. 292, and Syn. Fl., in part) ; San Ber- nardino (147 W. G. Wright, 1880). C. Palmeki, Gray. Limiting the species to the one of Palmer's original specimens which has the leaves " plieate-lineate by about G pairs of straight and strong veins," it may be otherwise distinguished by the 5-parted calyx (1^ lines long), the lobes linear and acute. The corolla is 2 \ lines long, with the rather stout fi'ament somewhat dilated below the insertion. The fruit is unknown. OF ARTS AND SCIENCES. 63 base: nutlet globose, nearly £ line broad: cotyledons thick, orbicular. — Very common on sandy bottom* near Los Angeles Bay. (517.) A flowering specimen collected by M. E. Jones at San Queutin is probably the same, but is more woody and apparently perennial. Heliotropium Curassavicum, Linn. Muleje. (15.) Heliotropium phyllostachyum, Toit. On rocky mesas at Guaymas. (232.) Krynitzkia axgustifolia, Gray. Tlie root was formerly used as a purple dye by the Indians. On stony ridges at Los Angeles Bay. (606.) KitYNiTZKiA ramosissima, Greene. Stony ridges, Los Angel Lay. (551.) Ipomcea coccinea, Linn. Mountain ravines near Guaymas. | :!10.) Ipomcea hederacea, Jacq. In ravines near Guaymas. (295.) Ipomcea leptotoma, Toit. Very common about Guaymas. (231 .) Ipomcea Bona-nox, Linn. River-banks at Muleje. (33.) Ipomcea triloba, Linn., var., with glabrous calyx. Collected also by Pringle in 1884 in Santa Cruz Valley, Arizona, and by Palmer (213) in 1885 in Chihuahua. In hedges and ravines about Guaymas. (306.) Ipomcea Palmeri. A vigorous climber, glabrous : leaves digi- tately divided, on slender petioles, the 5 segments linear-lanceolate, attenuate to each end, obtusish, 1 to 4 inches long: peduncles 1- flowered, 2 to 4 inches long: calyx glabrous, becoming 1 }, inches long, the sepals oblong, obtuse, chartaceous in fruit; corolla white, 2 inches long, with broad tube and rather narrow limb : anthers much twisted, a little exserted : stigma biglobose : capsule globose, ! inch broad, 4-valved, 4-seeded ; seeds very finely pubescent. — "Flowers with the odor of Stramonium." Margin of a dry creek-bed near Guaymas. (75.) Jacqtjemontia Prtnglel Gray, var. glabrescens, Gray. Flow- ers "pale blue with white lines." Hills near Guaymas. ('-"•' I.) Jacquemontia Palmeri. An erect slender annual, or at length somewhat climbing, simple or branched, a foot high or more, sparingly soft-pubescent: leaves ovate, usually cordate at base, acute, punctate, 15 lines long or much less, rather shortly petiolate : flower- few (1 to 5), scattered on slender peduncles : calyx-lobes ovate-lanceolate, 2 to 2^ lines long; corolla blue, 3 or 4 lines lung: capsule globose, equal the calyx, the four valves splitting equally to the base : seeds Bomewhat roughened. — In shade in the mountains about Guaymas. (221 ) EVOLVULUS LINIFOLIUS, Linn. Mountains about (iu.iyn: 'I.) 64 PROCEEDINGS OP THE AMERICAN ACADEMY Cressa Cretica, Linn. Guaymas, near salt water. (303.) Cuscuta umbellata, HBK. About Guaymas, upon species of Boerhaavia. (173.) Cuscuta Americana, Linn. With small flowers and entire scales, as in C congesta, Benth., from Acapulco, which is referred to this species. About Guaymas. (331.) Cuscuta (Eugrammica) Paliieri. Very slender: umbels soli- tary or in loose fascicles, few-flowered, the pedicels about equalling the flowers : calyx subcampanulate, acutely lobed, about half as long as the corolla-tube ; corolla white, persistent, 1^ lines long, the lobes equalling the tube, lanceolate, subacuminate, becoming reflexed : sta- mens half as long, the filaments rather stout ; scales very short, del- toid, fimbriate : styles slender, the longer equalling the stamens : capsule globose, small (% line broad), breaking away at base. — At Los Angeles Bay, very common, covering prostrate Euphorbias, etc., and forming sheets several yards in extent. (544.) Solancji nigrum, Linn., var. nodiflorum, Gray. " Yerba mora"; the young leaves and tops are much used by the Indians in cooking. At Muleje and Guaymas. (9.) Solanum Hindsianum, Benth. Erect, very thorny, 3 to 6 feet high ; flowers light to dark purple. " Perhaps distinct from S. elce- agnifolium" (Gray). Guaymas. (109.) Physalis pubescens, Linn. Muleje and Guaymas. (14.) Physalis angulata, Linn. ? Flowers yellow with brown base; fruit edible. About gardens at Guaymas. (G22.) Physalis angulata, Linn., var. Linkiana, Gray. Stem succu- lent, 3 feet high ; flowers " white with green centre" ; fruit fleshy and edible. At Guaymas. (175.) Physalis ? Resembling an entire-leaved P. pubescens, but the pedicels elongated ; fruit tinged with purple when ripe, sometimes eaten and used in cooking. Rocky ridges, in shade, at Los Angeles Bay. (561.) Physalis ? Prostrate, very finely pubescent, the upper side of the small ovate to rhombic-lanceolate irregularly blunt-toothed leaves nearly glabrous: calyx-teeth deltoid; corolla 6 lines broad, yellow with dark brown centre : anthers yellow : fruiting calyx puberulent, subglobose with open orifice, 6 to 8 lines long, equalling the pedicel. — Guaymas. (94.) Physalis ? Flowers in the dried specimens purplish blue, but described as " drab with wood-colored centre." Under shaded cliffs in the mountains about Guaymas. (G21.) OF ARTS AND SCIENCES. 65 Capsicum baccatum, Linn. A perennial, 5 feet high, with small red fruit which is sent to San Francisco as " chiltepin peppers." Guaymas. (136.) Capsicum cordiforme, Mill., var. globosum, Dun. ? A culti- vated perennial, 6 feet high, with globose orange-colored fruit. Guay- mas. (135.) Capsicum annuum, Linn. Various cultivated forms. Guaymas. (137-140.) Lycium Richii, Torr. Unarmed, 6 to 8 feet high ; flowers lilac ; fruit edible. Like the type of L. Palmeri, Gray. At Muleje. (4.) Lycium Ricnn, Torr., var. A very thorny shrub, sometimes 15 feet high ; pedicels shorter ; flowers " violet" ; fruit edible. In alka- line bottoms about Guaymas. (71.) Lycium Andersoni, Gray, var. pubkscexs. A shrub, 4 or 5 feet high, resembling var. Wrightii, but finely pubescent, the calyx half a line and the corolla 3 lines long with a very narrow tube ; flow- ers " lavender," tetramerous, the filaments glabrous : berries red. — In stony ravines near Los Angeles Bay. (559.) Lycium barbinodum, Micrs? A loose shrub, 5 feet high, with black wood, small white flowers, and scarlet fruit. Hillsides and ravines at Guaymas. (230.) Lycium carinatum. A thorny glabrous shrub, 1 or 2 feet high : leaves narrowly spatulate, 3 lines long or less, glaucous : pedicels clavate, compressed, 2 or 3 lines long: calyx bifid, the broad acutish lobes carinate ; corolla 4-lobed, white, 2 lines long, the tube very short and the throat scarcely as long as the lobes : stamens -4, villous- tufted at the point of insertion, equalling the corolla : fruit said to be red. — " Sal sieso." In large patches near Guaymas. (178.) Lycium ? A shrub, 4 feet high, with woolly nodes, very broadly spatulate leaves, and " white flowers." The specimens are without flowers or fruit, and the reference to this genus is only a conjecture. Guaymas. (337.) IS'icoTiANA trigonophylla, Dun. At Muleje and on San Pedro Martin Island. (18. 4'.0.) Nicotiana Clevelandi, Gray. Common at Los Angeles Bay. and used for smoking by the Indians. (55 G.) Mohavea viscida, Gray. Flowers lemon-color with brown dots, the lower stamens wholly wanting in the flower examined. On stony ridges at Los Angeles Bay. (597.) Antirrhinum cyatiiiferum, Benth. {A. chytrospcr mv >» , Gray.) In gardens at Guaymas. (152.) \OL. XXIV. (S. b. XVI.) 5 66 PROCEEDINGS OP THE AMERICAN ACADEMY Antirrhinum Kingii, Watson, var., with longer pedicels. Col- lected also in Sonora by Pringle in 1884. Among rocks near Los Angeles Bay. (589.) Stemodia durantifolia, Sw. Flowers white. Muleje. (25.) Conobea intermedia, Gray. In dried roiky river-bottoms in the mountains about Guaymas. (241.) Mimulus moschatus, Dougl. On wet rocks near Guaymas, (664.) Crescentia alata, HBK. The gourd-like fruit is subglobose, about 4 inches in diameter, 1 -celled (as also the ovary), filled by the pulpy parietal placentae and numerous flattened obcordate seeds (4 lines long). The species appears to be in every respect a Crescentia. It is cultivated at Guaymas, under the name of " ayal," for shade and for the medical properties of the fruit, which is filled with water and the liquid afterwards taken as a remedy for contusions and " internal bruises." (85.) Martynia althe^efolia, Benth. Flowers yellow, lined with orange and dotted below with brown. Guaymas. (114) Martynia fragrans, Lindl. Flowers honey-scented. In low moist places at Guaymas. (326.) Martynia Palmeri. Stems herbaceous, prostrate, from a large yellow fusiform root : leaves opposite (the upper alternate), long- petiolate, ovate-cordate, obtuse, the margin sinuate, 14; inches long or less : inflorescence floccose-pubescent and viscid ; pedicels 2 or 3 inches long ; bracts at base of calyx ovate, short, becoming thickened and spongy : calyx campanulate, 5-toothed, 4 to 6 lines long, the throat oblicme ; corolla 1| inches long, buff with orange and red stripes and the throat dotted with red : stamens 4 ; seeds irregularly oblong, angled and more or less prominently tuberculate, 3 lines long. — Root resembling a carrot and often weighing 3 or 4 pounds ; flow- .ers carnation-scented. The green fruit and the seeds are used for food by the Yaqui Indians. Sandy places at Los Angeles Bay. (599.) Elytraria tridentata, Vahl. " Cordoncillo" ; used as a remedy for fevers, venereal diseases, etc. In shaded places at Guaymas. (285.) Ruellia tuberosa, Linn. Under hedges at Guaymas. (98.) Ruellia ? A shrub, 4 feet high, with glandular-pubescent narrowly ovate leaves (6 to 10 lines long), and 1 to 3 flowers in the axils upon a very short peduncle ; bracts very small : calyx-lobes linear, acuminate, 5 or 6 lines long ; corolla light purple, 2 inches long, the tube equalling the calyx and the dilated throat longer than OF ARTS AND SCIENCES. 67 the lobes : stamens unequal : capsule 6 to 9 lines Ion"-, acuti seeded. — In moist shaded places on the mesas and in ravines about Guaymas. (196.) Beloperone Californica, Benth. Shaded spots in the moun- tains, at Muleje and Guaymas. (16.) Dianthera Sonor^e. Perennial (?), the herbaceous stems very finely roughish-puberulent, about a foot high : leaves ovate to lance- olate, shortly petiolate, acutish, sparsely pubescent on the margin and veins beneath, 1 or 2 inches long; spikes dense, terminal, sessile, soli- tary, 1 \ inches long or less ; bracts imbricated, oblanceolate, acute and mucronate, strongly 3-nerved and ciliate, 4 to 6 lines long: calyx 4-parted, the very narrow attenuate ciliate segments 2 lines long; corolla cream-color, 8 lines long, the straight narrow tube somewhat longer than the limb: anther-cells parallel, nearly equal, separated by a rather narrow connective. — Near a creek in the mountains about Guaymas. (240.) Jacobinia ovata, Gray, var. subglabra. Branches glabrous and leaves nearly so; flowers in short spikes; otherwise apparently identical with the original of the species. Shrubby, 4 to 6 feet high, the flowers bright scarlet. Mountain ravines near Guaymas. (264.) Lantana Camara, Linn. A nearly glabrous form. " Confiturea"; used as a preventive of hydrophobia. Plains about Guaymas. c2~- 1. 1 Lippia (Zapania) Palmeri. Near L. graveolens ; shrubby, 3 to 5 feet high : leaves ovate to elliptical, the blade decurrent upon the short petiole, obtuse or acutish, rugose, subcrenately toothed, finely substrigose-pubescent, an inch long or often much less : peduncles solitary or in pairs in the axils, very short; heads often few-flowered, 2 to 6 lines long; bracts decussate, the lower united to the middle, the upper distinct: calyx thin, not carinate ; corolla salverform. — "Origano"; with a strong sage-like odor and used as a potherb. In arroyos about Guaymas. Flowers white or cream-color (277, 644), or rose-color (643). ClTKAREXYLU.Yl (CaCOCALYX) FLABELLIFOLIUM. A tall shrub, the younger portions more or less pubescent with shorl spreading hairs: leaves thin, flabelliform, truncate or rounded above and cre- nately few-toothed, abruptly contracted to a short petiole, \ inch lung or less : racemes terminal or sometimes axillary, sessile, loosely I ered; pedicels very short : calyx 5 nerved and -angled, acutely toothed, 3 lines Ions, becoming thin and dilated and loosely enclosing the fruit; corolla dark violet. 6 lines long, the yellowish tube shorter than the calyx, tomentose within, the broadly expanded limb with D< 68 PROCEEDINGS OF THE AMERICAN ACADEMY equal rounded lobes : fifth stamen anantherous : fruit black, 2 or 3 Hues long. — Differing from Citharexylum in foliage, in the large violet flowers, and in the calyx enveloping the fruit. The juice of the fruit stains a persistent black. Mountain ravines about Guay- mas. (237.) Bouchea dissecta. Annual, slender, erect, branched, very finely puberulent or glabrate, 2 feet high : leaves thin, petiolate, ovate in outline, pinnately cleft nearly to the rhachis, the narrow segments entire or 1-3-toothed .: spikes slender, elongated, nearly sessile, the appressed flowers about equalling the internodes ; bracts very small, subulate: fruiting calyx 3 or 4 lines long, narrowly and acutely toothed ; corolla white, scarcely exserted : fruit linear, 6 lines long, conspicuously long-beaked. — Peculiar in its dissected leaves. On rocky ridges about Guaymas. (259.) Vitex mollis, HBK. "Uvalama"; a small tree with fragrant violet-colored flowers and black edible fruit. At Muleje. (3.) Hyptis Emorti, Torr., var., with leaves less tomentose. A shrub, 3 to 6 feet high, known as " salvia " and used for seasoning. Sandy bottoms near the beach at Los Angeles Bay. (573.) Hyptis Palmeri. Shrubby, 6 to 8 feet high, more or less hoarv- puberulent throughout: leaves petiolate, lanceolate, rounded or cuneate at base, acute, crenately denticulate or the larger more coarsely toothed, 1 or 2 inches long: flowers in loose umbel-like very shortly pedunculate axillary cymes, the upper nearly naked ; pedicels slender, 1 or 2 lines long : calyx narrowly turbinate-cylindrical, white furfuraceous-puberu- lent (like the pedicel), the slender teeth more than half the length of the tube ; corolla lilac. — " Salvia " ; used for rheumatism. Common in arroyos about Guaymas. (278.) Salvia privoides, Benth. At Guaymas. (320.) Stachys coccinea, Jacq. Near a waterfall in the mountains above Guaymas. (300.) Plaxtago Patagonica, Jacq. On stony ridges at Los Angeles Bay. (524.) Mirabilis tenuiloba, "Watson. A foot high or more, with flesh v leaves and white flowers ; fruit globose, 2 lines in diameter. Moun- tains near Los Angeles Bay. (600.) Mirabilis Califormca, Gray. Flowers purple. Mountains, Los Angeles Bay. (001.) Allionia incarnata, Linn. Guaymas. (100.) Bqerhaavia paniculata, Rich. Rocky ledges at Guaymas. (003.) OF ARTS AND SCIENCES. 69 Boerhaavia ? A doubtful species, not in good fruit, between the last and B. hirsuta. Common iu gardens at Guaymas, widely procumbent (172) or smaller and upright (172.1,). Boerhaavia erecta, Linn. Bloom white, becoming pink. High mesas at Guaymas. (182.) Boerhaavia erecta, Linn., var., with narrow leaves ; a common western form. Guaymas. (678-680, 684-687.) Also what is prob- ably an abnormal form of the same. (682.) Boerhaavia alata. Apparently erect, 2 feet high, much branched, puberulent, reddish: leaves narrowly oblong to linear, or the lower broader, H inches long or less: inflorescence loosely paniculate, the slender pedicels (1 to 3 lines long) solitary or subumbellate : perianth pink, 2 lines long: stamens (5) and style included: fruit nearly 2 lines long, truncate, more or less broadly 5-winged, the wings often broader than the body, narrower below. — On a small rocky island in Guay- mas harbor. (332.) Boerhaavia triqdetra. Similar to the last, puberulent ami viscid, procumbent : leaves lanceolate, acute or oblusish : pedicels very short (about ^ line) : perianth pink, a line long: stamens (2) and style included: fruit a line long, truncate, broadly obpyramidal, very acutely 3-4-angIed, the sides rugose. — Allied to B. pterocarpa, which has still smaller flowers (^ line long) with 2 or 3 stamens, and a broader-bodied wing-angled fruit attenuate to a stipe-like base. Sandy plains and stony ridges near Los Angeles Bay. (521.). Boerhaavia Wrightii, Gray. (B. bracteosa, Watson.) Flowers "waxy white'': distinguished from the following triandrous spicate species by the usually conspicuous thin bracts and the broader fruit, which is obtuse and acutely angled. Los Angeles Bay. (603 I Boerhaavia Xante Annual ; stems sparingly branched, Bome- what floccose-pubescent and puberulent, or glabrous above, occasionally with viscid spots, 2 feet high or less: leaves ovate to oblong-ovate or the upper narrowly lanceolate, sinuate, obtuse or acute: flowers large, in a rather loose raceme an inch long or less ; bracts lanceolate and bractlets linear, acuminate: perianth " white,*' spreading, 11 lin< stamens (4) and style long-exserted: fruit obloug-obovate, obtuse, ;• line long, rather acutely 5- (4-6-) angled, rugose in the intervals. First collected by Xautus (n. 93) at Cape Saint Lucas. Sands m< Guaymas. (681.) Boerhaavia Palmeri. Resembling tie' last ; stems procumbent or ascending, glandular-pubescent nearly tbrougl t : spike-like ra- ceme short and dense in flower, 4 lines long or less, about 6 lines long 70 PROCEEDINGS OF THE AMERICAN ACADEMY in fruit ; bracts obovate and bractlets lanceolate, acuminate, ciliate : perianth " white," f line long : stamens (3) and style included : fruit a line long, clavate, obtuse and obtusely-angled, the rather shallow intervals transversely rugose. — Dry sandy soil near Guaymas. (683.) It is also n. 209 of Palmer's collection in 1885, from Hacienda San Miguel near Batopilas, Chihuahua. — B. Coulteri (Senkenbergia Coulteri, Hook.) is a similar species, but less glutinous and the loose slender spikes more elongated ; bracts and bractlets very narrow ; perianth a line long; fruit clavate, 1 to 1^ lines long, truncate, the angles acutish and the channels extending to the very apex. Coul- ter's specimen (n. 1425) is labelled as from " Mexico." Arizona specimens of Palmer's early collections, 378 Rothrock from Camp Grant, and specimens of Pringle's collection in 1881 from the foot- hills of the Santa Catalina Mountains appear to be the same. Boerhaavia spicata, Choisy, var. (?) Palmeri. Similar to the preceding group ; stems procumbent or ascending, finely pubescent : leaves thin, nearly glabrous : flowering racemes open and very slen- der, becoming 1 or 2 inches long ; bracts lanceolate or linear, acu- minate ; bractlets none : perianth pink, ^ line long : stamens (2) and style included : fruit clavate-oblong, a line long, obtuse and mostly obtusely angled, the channel very narrow and sinuate. — Sandy mesas about Guaymas. (141.) — Typical B. spicata, as shown by a flow- ering and fruiting spike from Pavon's original specimen in Herb. Boissier, which was very kindly loaned me for comparison by M. Barbey, is peculiar in the ovate or ovate-lanceolate acute dark- colored bracts (with a pair of very narrow bractlets at the base of the young fruit), and in the conspicuous brown nerves of the nearly truncate perianth (^ line long). The fruit in the specimen is still young. The stamens are described as solitary, and but one was detected in the first flower examined, though there were two in the second one. I have seen no specimens that correspond to the type. The form of Texas, New Mexico, and Arizona that has been referred to this species is usually more glandular than the var. Palmeri, the leaves thickish and scabrous, and the perianth about a line long. It may be distinguished as var. (?) Torreyana. Boerhaavia scandens, Linn. An " evergreen, its many weak stems hanging upon bushes and fences, with greenish yellow flowers, and the fruits adherent to everything they touch." Near Guaymas. (146.) Abronia umbellata, Lam. Sandy plains near Los Angeles Bay. (604.) OF ARTS AND SCIENCES. 71 Cryptocarpus (?) capitatus. A scraggy shrub, 10-15 feet high, with rigid divaricate branches aud branehlets, the younger portions finely pubesceut throughout: leaves alternate, entire, mostly broadly obovate, obtuse or acutish, cuneate at base, 1 or 2 inches long includ- ing the slender petiole (3 to 6 lines long) : peduncles solitary, axillary, naked, becoming 6 to 9 lines long, bearing a globose head (4 to 6 lines broad) of cymosely clustered flowers on very short minutely bracteate pedicels ; involucre none : perianth cream-colored, turbinate-campanulate, very shortly and obtusely 5-toothed, a line lone : stamens 5, distinct, the slender filaments exserted ; anthers rounded : ovary obliquely linear-oblong, acute, shorter than the slen- der included style, attenuate to the base; ovule solitary, sessile, erect; fruit unknown. — A single head of flowers was collected in August, but it appears to be a winter bloomer, as the January specimens show an abundance of imperfectly developed flowers. In most of its char- acters, so far as known, the plant is certainly closely allied to Cryp- tocarpus. The fruit and fuller flowering specimens may, however, modify the reference. Near Guaymas. (6-47.) Achyronychia Cooperi, Torr. & Gray. Los Angeles Bay. (545.) Amarantus fimbriatus, Benth. Sandy plains near Los Angeles Bay (515), and in gardens at Guaymas (154, in part). Amarantus venulosus, Watson. Gardens at Guaymas. (154, in part.) Amarantus Palmeri, Watson. Varying in habit from procum- bent or ascending to erect and 5 or G feet high, and in the more or less slender or compact spikes, which are often much elongated. It is one of the commonest plants in Sonora and Lower California after the setting in of the rains, in gardens aud cultivated fields and in all bottom lands. It is valuable as a forage plant, and the seeds are largely gathered and sold in the markets for making bread and "attole." The collection includes numerous forms. (76-78, 127- 134, 312, 675, 676, 688.) Amarantus Palmeri, Watson, var. (?), with very thin-acarious broad perianth-segments, the midvein scarcely reaching to the apes j seeds rather smaller. — On an island in Guaymas harbor, near salt water, prostrate. (3 11 4-.) Cladothrix lanuginosa, Nutt. Gardens at Guaymas. (157.) Gomphrena Sonora, Torr. Rocky mountain-sidea above Guay- mas. (252.) Frozlichia alata, Watson. By irrigating ditches near Guaj mas. (245.) 72 PROCEEDINGS OF THE AMERICAN ACADEMY Iresine alternifolia. A shrub, 6 feet high, the young branches finely white-tomentose : leaves often or mostly alternate, thin, ovate or sometimes oblong-ovate, obtuse or acute, truncate or cuneate at base, tomentulose beneath, nearly glabrous or glabrate above, an inch long or less: flowers dioecious, in mostly broad rather open and nearly sessile panicles 2 to 4 inches long, scattered or subapproximate along the ultimate branches, § line long, the staminate pubescent, with very short bracts, the pistillate with smooth and shining bracts. — In the mountains about Guaymas. (276.) Chenopodium album, Linn. Guaymas. (72, 73.) Chenopodidm ambrosioides, Linn. "Hipasote"; Guaymas. (171.) Beta vulgaris, Linn. "Acelga"; Guaymas, in old gardens. (115.) Atriplex elegans, Dietr. Upright, 3 feet high. Guaymas. (117, 122.) Atriplex Barclayi, Dietr. Though varying somewhat in habit, as well as in fruit, the specimens are apparently all to be referred to one species, which is very probably the same as the little known A. Barclayi from Magdalena Bay on the Pacific side of the peninsula. The specimens from about the gardens at Guaymas are noted as growing 2 or 3 feet high. Those from the beach and islands of the harbor are low, and evidently sometimes perennial. (118, 119, 670, 677, pistillate ; 123, 673, 674, staminate.) Atriplex linearis. Dioecious, woody at base, 1 to 8 feet high, much branched, the branches slender : leaves canescent, narrowly linear, -| to 2 inches long, attenuate to the base : staminate flowers in mostly small globose clusters in slender spikes bracteate below ; pistil- late flowers in similar spikes, sessile or shortly pedicellate, solitary or somewhat clustered, the bracts 2 or 3 lines long in fruit, lanceolate with broad free and more or less spreading tips, the sides irregularly tuberculate and developing 4 broad wings, which are more or less deeply toothed or lacerate. — Near forms of A. canescens, which is very variable in its fruit but appears never to have the tips of the bracts so large and conspicuous. In alkaline soil about Guaymas. (120, 121, 235.) Su^da Torreyana, Watson. Very common on sea beaches and in alkaline soil, in large bunches 2 to 6 feet high. The ashes are used in soap-making. Muleje and Guaymas. (13, 329.) Spirostachys occidentalis, Watson. Sea-beach at Guaymas. (330.) OF ARTS AND SCIENCES. 73 Phaulothamnus spinescens, Gray. A thorny shrub, 10 feet high ; fruit a drupe with white fleshy pericarp, the embryo surround- ing copious mealy albumen. About Guaymas. (68.) Stegnosperma halimifolium, Benth. An upright evergreen, 5 or 6 feet high, with fleshy leaves, white flowers, and red pulpy fruit. At Muleje, on the island of San Pedro Martin, and at Guaymas. (31, 400.) Eriogonum inflatum, Torr. "Tivinagua"; much used as a remedy for fevers. Muleje and Los Angeles Bay. (24, 574.) Eriogonum fasciculatum, Benth. Los Angeles Bay, abundant ; 1 or 2 feet high. (549.) Eriogonum insigne, Watson, var., with the small leaves round- ovate instead of reniform, and the sepals broader. On mountains near Los Angeles Bay. (585.) Polygonum Persicaria, Linn. High mountains above Guay- mas. (211.) Antigonon leptopus, Hook. & Arn. " San Miguelito " ; its long black wiry roots develop large tubers at intervals, which have a pleasant nutty flavor and are an article of food with the Yaqui Indians. About Guaymas. (59.) Aristolochia brevipes, Benth., var. acuminata, Watson. " Yerba del Indio " ; the root used for aches and pains. About Guaymas. (174.) Loranthus Spirosttlis, DC. ? Leaves narrower than described (2 to 3| inches long by 2 to 5 lines broad), and sessile or subsessile. Flowers white and very fragrant ; fruit ovoid, 3 lines long, said to be red. About Guaymas, growing on fig, lime, mesquite, and other trees, the stems elongated, rooting or hanging in long tangled masses, (199.) Loranthus (Psittacanthus) Sonor^e. Glaucous and glabrous, the slender stems 3 or 4 inches long: leaves alternate, very narrowly linear or terete, 1 or 2 inches long and less than a line broad : flowers solitary or in pairs, terminating the branchlets, on pedicels 3 lines long or less; ovary a line long, subtended by a very shallow cupule and a short lateral bractlet; perianth scarlet, an inch long, the petals dis- tinct : fruit unknown. — Hillsides and edges of ravines about Guaymas, growing upon Bursera microphylla. (287.) Phoradendron flavescens, Isutt. Guaymas, on Maytenus phyllanthoides. (88.) Phoradendron Californicum, Nutt. About Guaymas, in lai bunches, chiefly upon the thorny mimosas and acacias. (665*.) 74: PROCEEDINGS OP THE AMERICAN ACADEMY Pedilanthus macrocarpus, Benth. Growing in large masses, the flowers and fruit bright crimson. A decoction of the plant is used as an active cathartic. Mountains and hills about Los Angeles Bay. (605.) Euphorbia capitellata, Engehn., var. laxiflora. Differing from the type of the species in the looser cymes, the mostly smaller gland-appendages, the glabrous capsules, and more sparingly toothed leaves. In gardens (83, 142) and high in the mountains (210) about Guaymas. Specimens from a sandy spit in the harbor (317) vary also in having the narrow and narrowly acuminate leaves nearly all entire, the involucres few in the cymes, and the stipules of the floral leaves shorter and less dissected. Pringle's n. 699 of his 1885 collection in Chihuahua, referred doubtfully to E. pycnanthemum, belongs rather to this variety of E. capitellata. Euphorbia Brasiliensis, Lam. At Guaymas. (81, 82.) Euphorbia albomarginata, Torr. & Gray. At Guaymas. (93.) Euphorbia (Cham^esyceye) intermixta. Annual, prostrate, glabrous : stipules broadly triangular, entire ; leaves more or less broadly oblong or obloug-ovate, obtuse or acutish, oblicpuely truncate or subcuneate at base, 3 lines long or less, several times shorter than the internodes : involucres solitary in the forks and axils, pedunculate, turbinate-campanulate, \ line long; glands dark brown, reniform, with a usually conspicuous white or pinkish appendage : capsule glabrous, rather acutely lobed : seeds (immature) pinkish, oblong, angled, smooth. — Near E. cordifolia among the Leiospermce. Guaymas. (187, in part; distributed with E. ylyptosperma.) Euphorbia trachysperma, Eugelm. High mesas about Guay- mas. (183, 319.) Euphorbia Magdalene, Benth. ? A low glabrous shrub (the branches finely tomentulose), with slender elongated virgate branches: leaves opposite, very shortly petiolate, oblong (2 to 4 lines long), ob- tuse at both ends, shorter than the internodes (upon the short spurs shorter, broadly elliptical, and exceeding the internodes) : involucres solitary, terminal on the spurs, w line long, the broad subreniform glands and appendages entire: styles long, 2-parted : fruit unknown. With little doubt the same as Bentham's species from Magdalena Bay, though not fully agreeing with the description. At Muleje, in dry ravines. (26.) Found also by Palmer in 1870 on Carmen Island. Euphorbia tomentulosa, "Watson. With white glands and ap- pendages and green capsules, or pinkish, or dark purple ; U to 3 feet high". Mountains; Los Angeles Bay and Guaymas. (216, 536.) OF ARTS AND SCIENCES. 7,", Euphorbia serpyllifolia, Pers. On gravelly ridges near Guav- mas. (187.) Euphorbia setiloba, Engelm. Near the bea;h, Los Angeles Bay. (629.) — About Guaymas. (185, 1851 634.) The latter a more open form with longer internodes and larger leaves, and the appendages less deeply 3-4-lobed. Euphorbia petrina. Near E. setiloba ; annual, prostrate, much branched and slender, more or less densely pubescent throughout with short spreading hairs: leaves very shortly petiolate, entire, obliquely ovate or oblong-ovate, obtuse, somewhat cordate at base, 3 lines long or usually much less: involucres solitary in the axils, shortly' pedun- culate, minute, turbinate-campanulate ; glands greenish, reniform, un- appendaged : capsule (and pedicel) pubescent, \ line long : seeds oblong-ovate, quadrangular, strongly and irregularly 3-4-rugose or -pitted. — Common among rocks at summit of San Pedro Martin Island. (412.) Euphorbia portulana. Of the same group ; annual, prostrate, much branched and slender, the minute and sparse pubescence spread- ing : leaves oblong to broadly elliptical, obtuse at both ends, entire, petiolate, 4 lines long or less: involucres oblong, f- line long, nearly glabrous, somewhat contracted above ; lobes subulate, slightly ciliate ; glands dark purple, the appendages variable in form, often unequal (1 or 2 larger), entire or nearly so, white or pinkish: stamens very few : ovary villous ; styles bifid nearly to the middle : capsule sub- acutely lobed, nearly a line long : seed oblong, tetragonal, very strongly 4-5-rugose. — Island in Guaymas harbor. (321.) Euphorbia gi.yptosperma, Engelm. High gravelly ridges at Guaymas. (187, in part.) Euphorbia polycarpa, Benth. Several forms, belonging chiefly to the variety with scarcely appendiculate glands {E. micromera, Boiss.). By garden fences at Guaymas and on islands in the harbor (96, 324, 335), and at Los Angeles Bay on sandy bottoms, sometimes covering many yards of surface (632, 633). — Also var. hirtella, Boiss., in like localities at Los Angeles Bay. (630.) Euphorbia Florida, Engelm. In rocky places high in the moun- tains above Guaymas. (20'J.) Euphorbia maculata, Linn., or near it; the glands unappendaged and capsules glabrous. Abundant in low sandy places about Guaymas. (186.) Euphorbia pediculifera, Engelm. Stony ridges near I Angeles Bay. (631.) 76 PROCEEDINGS OF THE AMERICAN ACADEMY Euphorbia pediculifera, Engelm., var. linearifolia. Closely resembling the ordinary form in the characters of the inflorescence and fruit, but erect and branching above the base, the stem and leaves mostly glabrous ; leaves thin, glaucous beneath, linear, acutish at both ends, an inch long or less. In both forms the appendages are unequal, the upper pair larger and oblique. — Hills and mountains about Guay- mas. (215, 627.) Euphorbia Californica, Benth. ? Probably not only this spe- cies but also E. Hindsiana, Benth. A shrub 3 or 4 feet high, with slender branches ; leaves round-obovate, 3 to 6 lines long, obtuse or retuse, on very slender petioles longer than the blade: peduncles ter- minal, mostly solitary : appendages lobed or merely crenate even in the same involucre : lobes of the capsule (2 lines long) scarcely cari- nate. — High mountain ravines above Guaymas. (260.) Euphorbia misera, Benth. A shrub 3 to 5 feet high. On stony mountain-sides above Los Angeles Bay. (514.) Euphorbia eriantha, Benth. Rocky ridges about Guaymas and Los Angeles Bay. (84, 518.) Simmondsia Californica, Nutt. Common about Guaymas. (343, 344.) Jatropha canescens, Mull. " Sangre en grado." A shrub, 3 to 8 feet high, with rose-colored flowers, and thick clustered roots. A decoction of the plant is used as a mordant in dyeing, and the juice as a remedy for warts, diseased gums, sore throats, etc. Common on the mesas about Guaymas. (103.) Jatropha spathulata, Mull., var. sessiliflora, Mull. " Tocote prieto." A shrub, 5 to 15 feet high, common about Guaymas and Los Angeles Bay. The fruit of this variety appears to be always 1- coccous. The bark is used as a mordant and for tanning, and is ex- ported for these purposes. It is also a dye, giving a reddish brown color, but is injurious to cloth. (164, 576.) Jatropha Palmeri. A shrub, the branches softly pubescent: leaves round-ovate, coarsely and very acutely sinuate-dentate (the teeth glandular-tipped), densely and subtomentosely pubescent on both sides, 1-J inches long by 2 wide or smaller: panicles shorter than the leaves; flowers apetalous, the white cylindrical pubescent calyx 4 or 5 lines long, with round-ovate lobes: stamens of male flowers 10, in two unequal ranks, the filaments connate and disk densely tomentose : ovary densely pubescent (becoming 3 or 4 lines long), the styles twice bifid. — Apparently referable to Midler's subsection Calyptrosolen, but it is more shrubby in habit and the calyx is less deeply lobed. Only OF ARTS AND SCIENCES. 77 a single plant found at a high elevation in the mountains above Gun- mas. (302.) Croton Pringlei, Watson. With a minty odor. Ravines and mesas about Guayrnas. (180.) Argythamnia sericophylla, Gray. In gravelly waste places about Guayrnas. (108.) Argythamnia Neo-Mexicana, Mull. Several forms, all of which appear to belong to this species. Plains and mountain-sides about Guayrnas. (80, 624, 625.) Argythamnia Palmeri. Stems numerous, erect, H to 2 feet high, rather sparsely appressed-villous except on the young branches : leaves oblong to lanceolate, acute, more or less attenuate to a very short petiole, entire, 1| or 2 inches long or smaller : flowers apparently dioecious, the pistillate solitary or in pairs in the axils, on recurved pedicels 1 or 2 lines long; sepals 2 lines long, becoming 4 lines in fruit; petals pilose, ovate-lanceolate, shortly acuminate: styles bifid, the stout branches dilated upward and hispid on the inner side : seeds ovate-globose, over a line long, coarsely reticulate-pitted. — High in the mountains above Guayrnas. (247.) Manihot angustiloba, Mull. Growing 2 or 3 feet high. In the shade on high mountains above Guayrnas. (233.) Acalypha Pringlei, Watson, var., with the pubescence scarcely or not at all glandular, and the teeth of the bracts more numerous (often 13). Mountains above Guayrnas. (219, 262.) Tragi a n.epet.efolia, Cav. Hedges about Guayrnas. (63.) — Also var. amblyodonta, Mull. (623.) Sebastiania (?) bilocularis, Watson. A shrub or small tic-'. sometimes 15 feet high. " Yerba flcche " ; the juice is au exceedingly active and violent cathartic, and the fresh bark is used by the Indians ' to stupefy fish. Common on the shores and in the hills and mountains about Guayrnas. (234.) Celtis pallida, Torr. A thorny shrub, 6 feet high or more, with orange-colored fruit. Guayrnas. (89.) Ficus (Urostigma) Palmeri. A tree 8 to 12 feet high, l)r.m< li- ing near the ground ; young branchletswhite-villous-pul)( >■■• lit : leaves at first densely white-tomentose beneath, becoming Dearly equally green on both sides and finely pubescent or suhglabrous above, rather thick, ovate, with a somewhat cordate or roundel base, acute, '■> inches long by 2 or 2^ broad, on petioles an inch long: fruit in pairs in the axils, on stout peduncles 6 lines long, globose thick and fleshy, <'■ lines in diameter, subtended by an irregular disk like involucre '■> lines 78 PROCEEDINGS OF THE AMERICAN ACADEMY broad : fertile flowers sessile, the perianth of three distinct sepals ex- ceeding the compressed ovary, the lateral ovate and somewhat concave, the other carinate ; abortive pistillate flowers very similar, but upon a short stout pedicel and the lateral sepals narrower ; staminate flowers also short-pedicellate, the perianth of three large oblong- obovate sepals ; anther sessile, broad, obtuse. — Fruit edible. On San Pedro Martin Island; rare. (413.) Ficus (Urostigma) fasciculata. A tree with a large trunk (8 feet high) bearing a widely spreading top, the lower limbs horizon- tal, sending down and supported by aerial roots ; foliage and rather slender branchlets wholly glabrous : leaves somewhat crowded at the ends of the branchlets, thin, oblong-lanceolate, short-acuminate or acute, 3-nerved at the rounded or acutish base, puncticulate above, finely reticulated beneath, 1^-2^ inches long, on petioles \ inch long : fruit solitary in the axils, on slender peduncles 2 lines long, sub- tended by a 4-lobed involucre, depressed-globose with a sunken orifice, 5 lines in diameter (immature) ; flowers all on short stout pedicels, somewhat oblique, the perianth short, gamophyllous, unequally and irregularly 2-3-lobed, the lobes short and obtuse ; style of some of the pistillate flowers filiform and entire, of others bifid ; anther sessile, ovate, acute, the cells rather long-apiculate. — Cultivated at Guaymas, but said to be native to the region. (646.) Ficus (Urostigma) Sonor^e. A tree 15 to 40 feet high, with- out aerial roots, glabrous throughout : leaves as in the last, but more scattered on the branchlets and more cuneate at base, the larger nearly 4 inches long: fruit solitary, on slender peduncles 4 or 5 lines long, subtended by an irregular disk-like involucre, globose, 5 lines in diameter : fertile flowers sessile, the perianth cleft to the middle with broad acutish lobes, shorter than the globose nutlet, which develops much mucilage when wetted; abortive pistillate flowers with a stipi- tate oblong-obovate empty ovary (not mucilaginous) surrounded by a tubular-funnelform 3-cleft perianth ; st iminate perianth similar, but shorter and somewhat broader, the anther ovate, acute. — Fruit black, edible, and known as "Nacapuli." Cultivated at Guaymas (92), and also found wild in the ravines of the mountains (645). In its foliage it closely resembles F. turbinate/. Brodi.ea Palmeri. Stem H to 2 feet high, bearing numerous bulblets at and below the surface; leaves linear, a little shorter than the scape, 8 lines broad or less : pedicels numerous, J to 1 inch long or more : corolla purple, 6 to 8 lines long, funnel-form from a narrow base, cleft to the middle, the throat coronate with a row of very short OF ARTS AND SCIENCES. 70 thin laminae between the principal veins : filaments 6, naked, scabrous, free from near the top of the tube and nearly equalling the corolla; anthers basifixed, liuear, 1£ lines long: capsule equalling the peri- anth, ovate, narrowed to a short stipe, the cells 2-seeded. — Of the Seubertia section, though with the basifixed anthers of Eubrodicea. Abundant in low places on the sandy plains about Los Angeles Bay. (596.) Washingtonia Sonoiue. A tree reaching 25 feet in heieht and a foot in diameter : leaves 3 or 4 feet in diameter, somewhat irlaucous. very filiferous, upon rather slender petioles which are armed with stout curved spines: spadix slender, 5 or 6 feet long: fruit about 3 lines long, the flattened-globose seed 2 to 2| lines in the longest diameter. — Apparently distinct from W. filifera and W. robusta in its more slender petioles, more glaucous leaves, and smaller fruit. The seeds are used for food by the Indians. It may here be noted that in the " Genera Plantarum " the genus Waslu'ngtonia is placed in the group having basilar styles, though it is correctly described as having the style ter- minal. In secluded canons in the mountains about Guaymas. (311.) Potamogeton pectinatus, Linn. " Grama " ; used in decoction " to purify the blood." In a small lake near Muleje. (23.) Naias major, All. " Saragossa." Abundant in a shallow lake near Muleje. (20.) Junctts* robustus, "Watson. In brackish water. Muleje. (34.) Cyperus speciostjs, Vahl. Margin of a fresh-water lake near Muleje (36), and high in the mountains above Guaymas (010). — C. LjEvigatus, Linn. Near Muleje and at Los Angeles Bay. (39, 509.) — C. aristatus, Rottb. At Guaymas, near the harbor ami also high in the mountains (193, 637), and on the summit of San Pedro Martin Island (417). — C. esculentds, Linn. At Guaymas. (208.) — C. articdlatus, Linn. High in the mountains above Guaymas. (636.) — C. ferax, Rich. At the same locality. (639.) Eleocharis capitata, R. Br. Same locality. (635, 635.1.) Fimbristylis laxa. With pale glumes. Same locality. (638.) Scirpus Olxeti, Gray. At Muleje. (37.) Paspalum distichum, Linn. High in the mountains abo Guaymas. (693.) — P. pchiflorum, Ruprecht. At Muleje and Guaymas. (45, 79.) * The following Juncacea. and Cyperacece were determined by Dr. N I- Britton, and the Graminew l>y Dr. George Vaset. 80 PROCEEDINGS OP THE AMERICAN ACADEMY Eriochloa punctata, Desv. At Muleje (44), and at Guaymas. Panicum sanguinale, Linn. At Muleje (48), and the var. cili- are near Guaymas (269, 695). — P. Hallii, Vasey. About Guay- mas. (206.) — P. dissitiflokum, Vasey, n. sp. In deep ravines and by irrigating ditches about Guaymas. (159, 190.) — P. fascicu- latum, Sw. Plains and foothills about Guaymas. (207.) Also var. majus, by ditches. (158.) — P. paspaloides, Pers. Near Guaymas. (690.) ■ — P. colonum, Linn. At Muleje (46), and about Guaymas. (51, 202.) — P. lachnanthum, Torr. Not eaten even by goats. About Guaymas. (54, 348.) — P. capillare, Linn., var. At Guay- mas. (208.) Setaria composita, HBK. About Guaymas. (53.) — S. cau- data, E. & S. At Guaymas and upon a small sandy island in the harbor. (340.) Also var. pauciflora. At Guaymas. (191.) Cenchrus echinatus, Linn. At Guaymas. (168.) — C. myo- suroides, HBK. Near salt water on an island in Guaymas harbor. (327.) — C. tribuloides, Linn. On the ruins of the old French fort at Guaymas. (349.) — C. Palmeri, Vasey, n. sp. Near Guaymas and at Los Angeles Bay. (271, 689.) Hilaria cenchroides, HBK., var. longifolia. Islands in Guaymas harbor. (347.) Cathesticum erectum, Vasey & Hack., and var. Abundant on mesas and hillsides and in gardens about Guaymas, and on islands in the harbor. (161,345.) Heteropogon contortus, R. & S. Hillsides and mountains about Guaymas. (267.) Sorghum Halepense, Pers. Gardens and fields about Guaymas. (64.) Aristida dispersa, Trin. Gardens and fields about Guaymas. (66.) — A. bromoides, HBK., and var. On rocky ridges at Los Angeles Bay. (503, 504.) — A. Schiedeana, Trin. & Rupr. Hedges and rocky ledges about Guaymas. (55, 268.) — A. fugitiva, Vasey, n. sp. On sandy beaches at Los Angeles Bay. (501.) Stipa Californica, Vasey, n: sp. In mountain canons about Los Angeles Bay. (505.) Muhlenbergia spiciformis, Trin. Rocky hills near Guaymas. (272.) — M. tenella, Trin. Island of San Pedro Martin, common among rocks; the only grass. (416.) — M. debilis, Trin. Plains and mountains about Los Angeles Bay. (510.) Sporobolus cryptandrcs, Gray. Abundant about Guaymas. (65.) — S. humifusus, Kunth. Abundant about Guaymas in the OF ARTS AND SCIENCES. s] rainy season. (188.) — S. Virginicus, Kuntli. On islands in Guay- mas harbor. (338.) — S. Domingensis, Kunth, and vars. Common about Guaymas. (160, 165, 696.) Agrostis verticillata, Vill. At Muleje. (41.) Chloris elegans, Kunth. Near Los Angeles Bay. (506.) . Bouteloua aristidoides, Thurb. About Guaymas (162, 194), and at Los Angeles Bay (507). — B. Rothrockii, Vasey. Gardens and fields at Guaymas. (166.) — B. arenosa, Vasey, n. sp. Plains and ridges about Guaymas. (189.) — B. bromoides, Lag. Moun- tains and ledges about Guaymas. (201.) — B. polystaciiya, Torr. Sandy bottoms near the sea at Los Angeles Bay. (346 ?, 508.) Also var. major. Common about Guaymas. (204, 205.) Eleusine Indica, Gaertn. Common at Muleje. (35.) — E. JEgyi'Tiaca, Pers. About Guaymas. (275, 328.) Leptochloa mucronata, Kunth, and var. Common about Guaymas. (50, 192, 694.) Pappophorum apertum, Munro. On the old fort at Guaymas and on rocky mountain-sides. (274. 350.) — P. Wrightii, Watson. Rocky ridges near Bay of Los Angeles. (51ft) Cottea pappophoroides, Kunth. Rocky island in Guaymas harbor. (339.) Triodia pulchella, HBK. On a high rocky point above Los Angeles Bay. (500.) Diplachne imbricata, Vasey. Common at Muleje (47), and at Guaymas. — D. dubia, Benth. High in the mountains above Guay- mas. (270, 273.) — D. Tracyi, Vasey. Same locality. (691.) — D. viscida, Scribner. Same locality. (692.) Phragmites communis, Trin. At Muleje. (38.) Eragrostis major, Host; forms. At Muleje (40. 401), and about Guaymas. — E. Pursiiii, Schrad. At Muleje. (42, 49.) Also var. diffusa. . Common about Guaymas. (167.) Distichlis maritima, Raf. At Muleje. common. (43.) Lolium perenne, Linn. In a garden at Guaymas. (52.) Notholvena* Lemmont, Eaton. In high mountains Dear Guay- mas. (266.) — N. cretacea, Liebm. (JV! Californica, Baton.) Rocky mountain-sides above Los Angeles Bay. (552.) Cheilanthes Prixglet, Davenport. Rooky mountain ]<■'! near Guaymas. (265.) — C. myriopiiylla, Desv. .Mountain- at Los Angeles Bay. (553.) * The Ferns were determined l>y Prof. D. C. Eatox. vol. xxiv. (nt. s. xvi ) 6 82 PROCEEDINGS OF THE AMERICAN ACADEMY Pell^a Seemanni, Hook. Shaded rocky ledges in the mountains about Guaymas. (226.) — P. Wrightiana, Hook. The form with numerous pinnules (P. longimucronata, Hook.). Los Angeles Bay. (554.) Indeterminable Species. 179. Flowering specimens from a tree growing on sardy plains about Guaymas, described as 12 to 15 feet high and 1 to 5 feet in diameter, with very green bark and a dense symmetrical top. Its wood is said to be useless even for fuel. The young branches are finely pubescent, and the leaves are alternate, coriaceous, entire, linear with a cordate base, obtuse, glabrous and veiny above, very strongly reticulate-veined beneath, with a stout midnerve and the margins revolute, about 3 inches long by 2 lines broad, the very short petiole (a line long) jointed upon the stem ; stipules none. The flowers as collected are in loose simple naked racemes 2 inches long, the scattered spreading pedicels 2 or 3 lines long. They are probably dioecious, as all those collected have only an imperfectly or scarcely at all developed ovary. The calyx is .very small, 6-8-parted, apparently valvate ; petals none; stamens about 20 (18-22) upon a prominent lobed hypogynous disk (nearly equalling the calyx), the filaments distinct, slender, 3 lines long, and the anthers short, basifixed, 2-celled, and longitudinally dehiscent. The most fully developed ovaries are smooth, oblong, somewhat obcompressed, 2-celled, with a nearly sessile thick 2-lobed stigma, and apparently one or more (?) pairs of collateral rudimentary ovules upon the axis. The relations of this remarkable species are very obscure, and must await fuller material for their determination. It will probably be found to belong to the Tiliacece. 307. " Yerba del ayre " ; foliage only of an unrecognized shrub, found in ravines about Guaymas. A decoction of the leaves#is used as a remedy for paralysis. 2. Descriptions of some New Species of Plants, chiefly Californian, with miscellaneous Notes. Silene Bernardina. Finely glandular-pubescent throughout ; stems slender from slender rootstocks, a foot high, few-flowered : leaves very narrowly linear-oblanceolate, 1 or 2 inches long: pedun- cles slender, 1-3-flowered : calyx cylindrical, J- inch long, with oblong- ovate teeth ; petals greenish, 8 lines long, the blade cleft to below the OF ARTS AND SCIENCES. 83 middle into four equal narrow lobes; coronal appendages nearly half the length of the blade, thin, 2-parted, the outer segment linear, entire, the inner oblong and lacerate ; claw naked, broadly auriculate : stamens included, unequal: capsule oblong, shortly stipitate. — Of the S. Lem- moni and S. occidentalis group. On shady slopes in Long Meadow, Tulare Co., California; Dr. E. Palmer, June, 1888 (n. 185). Erigeron sanctaru:m. Perennial and dwarfish, the branches of the rootstock very slender and naked, bearing one to several erect or subdecumbent 1-flowered stems, leafy except toward the top. a span high or less, rough-pubescent : leaves entire, narrowly oblanceolate, becoming linear above, the lower an inch long (or sometimes longer and with a slender petiole): heads medium-sized; involucre of nu- merous very narrow acuminate bracts in two series, the outer hispid, densely so at base: rays many, purple or fading to white; pappus simple. — Not closely allied to any other of the Euerigeron section. Collected by Mr. T. S. Brandegee in the Santa Inez Mountains, Cali- fornia, also near Santa Barbara, and on the island of Santa Rosa, 1888. B^eria (Edb^eria) Parishii. Low and slender, much branched, pubescent with loose woolly hairs : leaves narrowly linear, acute, mostly pinnately cleft with one to several pairs of lobes : heads small, 2 lines high or rarely more ; involucral bracts 10 to 12, thin and lax, the midvein not prominent : ligules short : style-tips truncate, with an oblique apiculation on the inner side : achenes slender, with- out pappus. — Resembling epappose small-headed forms of /!. gracilis, differing in the pubescence and cleft leaves and in the apiculate style- tips, and approaching the B. platycarpha group. On the foothills of the San Bernardino Mountains, at 1500 feet altitude; collected by Mr. S. B. Parish, in May, 1888. Bahia Palmeri. Low and slender (not 6 inches high), somewhat soft-pubescent and resinous-atomiferous : leaves mostly alternate, en- tire, very narrowly linear, an inch long or less: heads sessile and somewhat clustered, narrowly turbinate, 2-6-flowered ; involucral bracts 3 or 4, narrowly oblanceolate, acutish, whollj green and her- baceous: rays none; corolla-lobes ">, more or less unequal : achenea rather broad, obtusely quadrangular, finely striate and gland ular- puberulent ; pappus of 8 to 1<) thin obtuse oblong-spatulate denticu- late chaff, narrowed and thickened toward the base, half tin- length of the corolla-tube. — An anomalous species, intermediate between Schkuhria and Bahia as defined by Dr. Gray, and tending t'> invali- date the distinction drawn by him between the genera. It is placed 84 PROCEEDINGS OP THE AMERICAN ACADEMY in Bahia as nearer to the section Achyropappus of that genus than to Schkuhria § Hopkirkia, especially in the characters of the involucre and achene. Found by Dr. E. Palmer (n. 1 G8) on low slopes aud ridges in Long Meadow, Tulare Co., California, June, 1888. Cacalia tussilaginoides, HBK. In the notes made by Dr. Gray (as given in these Proceedings, vol xxii. p. 432) upon the speci- mens collected by Dr. Palmer in Jalisco (n. 1G8, of 1886), which he referred with some uncertainty to this species, the words, "ex char." should have been erased in the proof-reading. These were in his notes as sent from the Kew Herbarium, where he had found only the Coulter specimen to which he alludes. Later, he examined at Paris Humboldt's original specimens upon which the species was based, with the result that he directed the retention of the reference, though leav- ing it still questionable. Microseris anomala, Watson, in Proc. Amer. Acad., 22. 474. This species was described under a misapprehension of the character of the pappus. It is without a doubt a form of M. meter ochceta, Gray. The mature fruit of this species is still unknown. Collinsia Wrighth. Low and divaricately branching (3 or 4 inches high) , glandular-pubescent and viscid : leaves opposite, linear- oblong or -lanceolate, entire, about an inch long : flowers pedicellate, 1 or 2 in the axils, the uppermost in a naked umbel ; calyx 2 lines long, the narrow lobes obtusish ; corolla but little longer, the tube and throat shorter than the broad obtuse lobes of the limb, the lower lip blue, the upper yellowish : capsule equalling or a little shorter than the calyx, 2-seeded : seeds oblong, nearly terete, with a deep ventral sulcus. — Near C. Torreyi, with the habit and flowers of O. parvi- flora. On the Greenhorn Mountains, Kern County, California, at 6,000 to 7,000 feet altitude ; collected by Mr. W. G. Wright aud Dr. E. Palmer in June, 1888. Mimulus (Eumimulus) deplexus. A dwarf slender annual, 2 or 3 inches high, sparingly viscid-puberulent : leaves linear to linear- oblong, entire, less than \ inch long : pedicels exceeding the leaves, soon widely spreading or usually reflexed : calyx glabrous, narrow, not strongly nerved or angled, nearly equally and obtusely toothed, 2 to 2^ lines long ; corolla 6 or 7 lines long, the narrow tube nearly twice the length of the calyx, the broad limb deeply bilabiate; upper lip deep purple, with emarginate lobes, the lower deep yellow with bifid lobes, somewhat hairy and spotted below: capsule \\ lines long : seeds brownish, irregularly ovate to oblong-ovate, some- what rugulose longitudinally. — A very pretty little species, of the OF ARTS AND SCIENCES. 85 r same group with M. bicolor, montioides, aud rubellus. The placenta splits at the apex. Collected by Dr. E. Palmer (n. 17G) in June, L888, on the drier edges of low wet places in Long Meadow, Tulare Co., California. Louteridium Donnell-Smithii, Watson, Proc. Amer. Acad. 23. 283. In the description of this curious Guatemalan genus the calyx is inadvertently described as inverted. It is of course the three upper sepals that are united into one, the two lower remaining distinct. The same plant has since been detected in my own collection made in Guatemala in March, 1885, — found in flower at the plantation on the Chocou River and noted as growing from 3 to 9 feet high. Eriogonum: (Ganysma) Es.meraldense. Leaves all radical, hispid, especially on the margins, round-obovate, cuneate at base, small (an inch long including the petiole), the rest of the plant wholly glabrous and glaucous : stem slender, repeatedly dichotomous above ; bracts small, deltoid to oblong ; pedicels very slender, 2 or 3 lines long, mostly strongly reflexed : involucres narrowly turbinate, .1 line long, cleft to the middle : flowers glabrous, white or pinkish, the oblong to oblong-spatulate segments nearly ecpial, retuse or obtuse, ^ line long. — Near E. glandulosum, but wholly destitute of glands. Found by Mr. W. H. Shockley, July, 1888, in Esmeralda Co., Nevada, at Candelaiia, and on Miller Mountain at 7,000 feet altitude. Eriogonum (Oregoxium) gracilipes. A dwarf cespitose per- ennial, with compactly branched caudex and crowded oblanceolate tomentose leaves, ^ inch long or less : peduncles slender, % to 2 inches long, glandular-puberulent : involucres few in the small solitary head, turbinate, tomentose : flower glabrous, more or less deep rose-color, exserted. — Of the E. Kennedyi group, distinguished most conspicu- ously by the glandular-puberulent peduncle. On the White .Moun- tains, Mono Co., California, at 13,000 feet altitude; W. II. Shockley, August, 1888. Ne.uastylis Prixglet. Stem a span high, terete, usually simple, 1-leaved near or above the middle: radical leaves shorter than tli<' stem, 1 or 2 lines broad, 2-3-nerved (the nerves somewhat winged alternately on the two sides) ; spathe-bracts unequal, the larger nearly equalling the solitary pedicel, 1 \ inches long: flowers very fragrant, of a delieate pale blue, the segments oblong-oblanceolate, obtusish, the outer 15 lines and the inner 13 lines Ion-, minutely apiculate : stamineal column nearly 2 lines long, half the length «-t the linear yellow anthers: divergent Btigma-lobes 1! line, long: capsule oblong, 5 to 10 lines long. — Collected by -Mr. ('. <;. Pringle 86 PROCEEDINGS OF THE AMERICAN ACADEMY in 1887 (n. 1378) in the mountains of Chihuahua in fruit, and de- scribed from plants in flower at the Cambridge Botanic Garden in July, 1888. Nemastylis Dugesii. The plant described by myself as a Tigridia in Proc. Am. Acad. 20. 375, based upon drawings by Prof. Duges, should doubtless have been referred rather to Nemastylis, as the style-branches are plainly represented to be alternate with the anthers. Calathea crotalifera. Low; leaves oval, abruptly acute at each end, 1J to 2 feet long by 10 or 12 inches broad, yellowish green, the midvein with a narrow whitish margin, paler beneath ; petiole 2 or 3 feet long, at base sheathing the one or two peduncles, which are 8 or 10 inches high : spike erect, distichous, G to 10 inches long, the bracts (20 to 40) closely imbricated, duplicate-reniform, subtruncate, 1^ inches long or less, yellowish green tinged with red ; bractlets doubly winged on the back : flowers mostly included, yellowish ; sepals scarious, 4 to 6 lines long, about half the length of the petals. — In wet shaded places at the base of the El Mico Mountains near Yzabal, Guatemala, April, 1885 ; also received in flower from Messrs. Reasoner Brothers, of Manatee, Florida, cultivated from Guatemala roots. The resemblance of the spike to the rattle of a Crotalus sug- gests the name. Sisyrinchium anceps, Cav. Having had occasion to investigate the nomenclature and synonymy, as well as validity, of the species of Sisyrinchium found within the limits of Gray's Manual, I would again propose the restoration of the above name for one of our forms. The error made by Linnaeus in uniting the Tournefortian Bermudiana from Bermuda with the species that had come into cultivation in Eu- rope from this country was recognized by the botanists generally of that day, and the two species were kept distinct afterward, as they had been before. Miller (1768) was the first to give a definite binomial name to the American plant, calling it S. angustifolium, and the form intended by him is easily recognized from his description, and from the figure given by Dillenius, which represent a plant with a simple stem bearing a single spathe. In 1783, Lamarck published the name S. gramineum for what as described by him and afterward, figured by Redoute would appear to be the same thing. In 1788, Cavanilles gave the name S. anceps to what might also be considered the same, except that his figure shows a plant with a branching stem. Michaux afterwards in his Flora described two species (S. Bermudiana and S. mucronatum) as found by him in the Atlantic States. Of these, OF ARTS AND SCIENCES. 87 S. mucronatum is the old species, i. e. S. angustifolium of Miller. His S. Bermudiana is distinguished as having a broadly winged branching stem and equally bracted spathes, and he cites S. anceps, Cav., as probably a variety. Nuttall in his "Genera" simply mentions three species, S. anceps, S. mucronatum, and S. Bermudiana, and Sweet is cited (" Brit. Fl. Gard., 2 ed., 498 ") as having given to the last the name S. Nuttallii. Later Americau botanists have endeavored to dis- tinguish two species, S. anceps and S. mucronatum, by the characters of the perianth, spathes, and stems, but with so little satisfaction that more recently Dr. Torrey and Dr. Gray have united them as varieties under the Bermudan species S. Bermudiana. A comparison of such fruiting specimens as have come in my way have shown an evident difference in the seeds of our common species, some being globose, quite strongly pitted, and less than \ a line in diameter, others more angled, rather less pitted, and about twice larger (rather more than ^ line broad). This difference of seed appears always to accompany a difference of habit, the larger seed belonging to the simple stemmed form (S. angustifolium), while the plant with smaller seeds is always branching, bearing several spathes. This seems to justify the reten- tion of the two species of our early botanists, and, restoring Miller's name for one, there seems to me no good objection to keeping up Cavanilles's name for the other. Both species are very commonly dis- tributed through the eastern United States, from Canada to the Gulf. The species of the Gulf region still need investigation. Allium hyalinum, Curran in herb. Bulb-coats gray, the areolae of the peculiar reticulation narrowly linear and much contorted : leaves several, very narrow : scape slender, a foot high or less ; spathe bifid, unilateral ; pedicels rather few, an inch long or less : perianth white to purplish, broad, 3 to A\ lines long, the acute segments broadly lanceolate to ovate, the inner somewhat narrower : stamens a third shorter, the filaments dilated at base: ovary not crested.— First col- lected at Salmon Falls in Eldorado Co., California, by Mis- M. K. Curran, June, 1881 ; also recently found by Mr. T. S. Brandegee on Santa Cruz Island. The flowers much resemble those of A. cam- panulalum, which is a stouter plant with broader leaves, the reticula- tion in the bulb-coats minute and extremely sinuous, the filaments more slender, and the ovary crested. 88 PROCEEDINGS OF THE AMERICAN ACADEMY VII. THE DETERMINATION OF CHROMIUM IN CHROME IRON ORE. By Leonard P. Kinnicutt and George W. Patterson. Presented January 9, 1889. The complete decomposition of chrome iron ore, and the determination of the amount of chromium, is one of the difficult problems of quanti- tative analysis. Of the very many methods that have from time to time been published, one given last year by Donath * using barium dioxide as the oxidizing and fusing agent, seemed the most expeditious and simple. The method as given by him was as follows. One part of the very finely divided mineral was mixed with five times its weight of barium dioxide, and heated for one half-hour in a porcelain crucible over one Bunsen lamp. The semifused yellowish green mass thus obtained was treated with dilute hydrochloric acid. After a few hours, all the chromium was found in solution as the chromate of barium. The barium was precipitated with sulphuric acid, and the filtrate from the barium sulphate neutralized with sodium carbonate, and a few drops of an alkaline solution of permanganate of potassium added to oxidize any chromium that might have been reduced. The excess of permanganate was then removed by the very careful addition of fer- rous sulphate, and the amount of chromium determined volumetrically. Donath, however, did not publish any results to show the accuracy of the method, and it was on this account that we were led to repeat his work. A few experiments were sufficient to satisfy us that the perfect de- composition of chrome iron ore from Pennsylvania could not be accomplished in the manner described by Donath. A number of fusions of the very finely powdered and sifted mineral with five or even ten times its weight of barium dioxide were made, and in every case the residue contained a greater or less amount of the black unde- composed mineral. Also we were unable to obtain any porcelain cru- cibles in which more than one fusion could be safely accomplished ; while if the fusion was made in platinum crucibles, we obtained, as * Dingler's Polytechnisches Journal, vol. cclxiii. p. 245. OF ARTS AND SCIENCES. 89 was also noticed by Donath, a comparatively large amount of the sesquioxide of chromium. Another serious difficulty was met with later in the process ; namely, in determining the exact point where sufficient ferrous sulphate had been added to reduce the excess of permanganate of potassium, used in oxidizing the small amount of reduced chromic acid. The change of color of the solution being so slight as to be almost useless as an indicator. We were therefore unable, with the most careful manipulation, to obtain satisfactory results with the above process. In our study of the process we made a great many experiments with different fusing mix- tures, and also tried various ways of oxidizing the small amount of sesquioxide of chromium we always found present in the solution. The result of these experiments have enabled us to formulate a very quick and simple process, which, as can be seen by the results given below, is also, as regards accuracy, very satisfactory. About three tenths of the very finely divided mineral is mixed with twenty times its weight of a mixture containing equal parts of dry sodium carbonate and barium dioxide, and heated in a platinum cru- cible with the full flame of one Bunsen lamp for one half-hour. At the end of this time a quiet fusion is obtained and the decomposition is completed. The crucible is then placed in a beaker, covered with water, and hydrochloric acid added, a little at a time, till the mass is completely disintegrated. The crucible is then removed, the solution made strongly alkaline with caustic potash, and five or six cubic centi- meters of a five per cent solution of hydrogen dioxide added to oxidize the small amount of reduced chromic acid that may be present. The solution is now boiled for twenty minutes to remove any excess of hydrogen dioxide, made acid with hydrochloric acid, and the amount of chromic acid determined by the aid of a standardized solution of ferrous chloride. Six analyses of a sample of chrome iron gave the following per cents of chromium sesquioxide. 1. 2. 3. 4. 5. 6. 49.87 49.97 49.84 49.85 49.88 49.87 The solution of ferrous chloride used was kep( under oil and titrated before each analysis. One cubic centimeter equalled aboul 0.015 gram of chromium sesquioxide. Salisbury Laboratories, Worcester Polytechnic Institute. 90 PROCEEDINGS OP THE AMERICAN ACADEMY VIII. CONTRIBUTIONS FROM THE PHYSICAL LABORATORY OF THE MASSACHUSETTS INSTITUTE OF TECHNOLOGY. XXXI.— THE STRENGTH OF THE MICROPHONE CURRENT AS INFLUENCED BY VARIATIONS IN NORMAL PRESS- URE AND MASS OF THE ELECTRODES. By Annie W. Sabine. Presented by Charles R. Cross, Norember 14, 1888. The experiments described in the present paper, undertaken at the suggestion of Professor Cross, constitute a study of the variation of the current in the secondary circuit of a microphone transmitter, as related to variations in the normal pressure and in the mass of the electrodes of the microphone. They form a continuation of work of a similar character which has been prosecuted in the Rogers Labo- ratory during the past few years, and a portion of which has already been presented to the Academy.* The instruments used were similar to those previously employed by Messrs. Patterson and Tucker, and described in the latter of the two articles just referred to. The electrodynamometer was calibrated by means of a Hartmann galvanometer, using reversals in the ordinary manner so as by four readings to eliminate the effect of the earth's magnetism on the suspended coil. The microphone contact was set into vibration by the sound of a stopped organ-pipe (C4 of 512 vibrations) kept as constant as possible by means of an air-blast furnished with a regulating air-chamber. Weights were gradually added to the upper (anvil) electrode, so that the mass of this and its pressure on the lower electrode were thereby increased by measured amounts. The weights added were usually in the form of thin copper washers weighing t8q of a gram each, though fractions of this weight were used in some cases. One chromic acid cell was used as a battery. * See Proc. Am. Acad., Vol. XXI. p. 248 ; Ibid., Vol. XXIII. p. 228. OP ARTS AND SCIENCES. M The character of the results obtained will be seen by an inspection of Figure 1, which gives the curve showing the relation between the normal pressure and the resulting current, with electrodes of the ma- terials employed in the Blake transmitter, viz. a platinum hammer and a hard carbon anvil electrode. The abscissas represent the normal pressures, i. e. the added weights, and the ordinates the currents pro- duced in the secondary. The data from which this curve is construct d will be found in the following table. The load is given in terms of the arbitrary unit employed ; the currents are given in milliamperes. Table. Remarks. Load. Current. 0 0 .5 .18 1.0 .46 Loud, goo 1.5 .48 ti u 2.5 .56 «( it 3.0 .49 3.5 .45 Faint, go< 4.0 .33 a a 4.5 .21 5.0 .19 The curve shows a rapid rise at first, as the mass of the anvil elec- trode, and with it the pressure between the electrodes, is increased, which rise soon reaches a maximum, the curve then falling off rapidly at first, more slowly afterwards. The nature of the curve is interesting, and requires explanation. In his article already referred to, Mr. G. W. Patterson, who obtained similar results to my own, considers the curve to be composed of two separate branches, the rising portion of the curve corresponding to a motion of the electrodes sufficient to break the circuit, and the falling portion to the case when the pressure is too great to allow this to occur. The curve (these Proceedings, Vol. XXIII. p. 235, Fig. h constructed upon this hypothesis greatly resembles one of the experi- mental curves shown in Fig. 3 of the same paper. There is less resemblance, however, to the lower curve in Fig. •'!, and but littl<- to the curve shown in Fig. 1 of this article, which was obtained under exceptional conditions of quietness of the piers upon which the appa- ratus was placed. The sound in a receiving telephone placed in ih<' secondary circuit is so harsh for this portion of the curve, thai one might well infer that actual breaks i ccurred ; but this is very doubtful, and such breaking is certainly not essential to the production of the 92 PROCEEDINGS OF THE AMERICAN ACADEMY results which are obtained. In fact, the article referred to assumes that the varying pressure on the contact due to the action of the given sound-waves will always have the same maximum value, ± S. This would be approximately true were the normal pressure between the two electrodes alone to be varied, but the effect of the addition of weights, as in the method of experiment adopted, is to increase the Fig. 2. 0 % \ \ 3 4 5 6 Fig. 3. mass at the same time that the normal pressure is increased, and under these circumstances the effect of a sound-wave of given intensity will necessarily be to give to the corresponding pressure-variation a va- riable value, increasing with the added mass, and hence, with the form of apparatus used, as the normal pressure is greater. The effect of this will be to cause at first a gradual increase of current in the secondary, OF ARTS AND SCIENCES. 93 which increase is succeeded by a diminution of current when the mass is still further increased. This will be apparent from an inspection of the curve shown in Figure 2, which illustrates in a general manner the relation of the pressure between the electrodes to the current in the primary circuit. In this the momentary changes in pressure, Ap, Ap', Ap", etc , due to the sound-waves, and corresponding to loads and normal pressures p, p\ p", etc., have increasing values within certain working limits, owin£f to the increasing mass of the anvil electrode. The currents in the primary also increase, though at a gradually diminishing rate, as the pressure between the electrodes is increased, so that the increments of current, Ac, Ac', Ac", corresponding to the pressure-changes Ap, Ap', Ap", have increasing values up to some point, as a, after which they decrease. This being the case, it is evident that the current in the secondary will at first increase to a maximum, and afterwards diminish, since the currents in the secondary corresponding to press- ures p, p', p", etc. will be proportioned to Ac, Ac', Ac", etc., and this is precisely the curve which is obtained in the experiments. The explanation just offered seems therefore to be the' true one. The matter was still further tested by carrying out a set of experi- ments similar to those already described, except that the variations in normal pressure were brought about by means of a spring instead of by adding weights. In such a case the successive values of Ap in the curve (Fig. 2) would be of the same magnitude, while Ac would continually diminish. The current in the secondary should therefore have its maximum value when the initial normal pressure is least, and continually diminish as that pressure becomes greater. The experimental results verified this conclusion, as will be seen by reference to Figure 3, in which the normal pressures are represented by abscissas, and the currents in the secondary by ordinates, as before. The curve is approximately a straight line. It is possible that the deviations from this are due to instrumental imperfections, as the apparatus used did not allow of more than an approximate determi- nation of the pressure applied by the spring. Eogers Laboratory of Physics, June, 1888. 94 PROCEEDINGS OF THE AMERICAN ACADEMY IX. CONTRIBUTIONS FROM THE PHYSICAL LABORATORY OF THE MASSACHUSETTS INSTITUTE OF TECHNOLOGY. XXXII. — RESEARCHES ON MICROPHONE CURRENTS. By Charles R. Cross and Annie W. Sabine. Presented November 14, 1888. In continuation of studies described in former papers from the Rogers Laboratory, the authors have observed the variations in the secondary- current which occur under different circumstances as to mass and normal pressure when the material of the electrodes of a microphone is varied. The methods and apparatus employed were identical with those described in the immediately preceding paper in the?e Proceed- ings (page 89). In the first series of experiments both electrodes were made of the same material, the hammer electrode being a very small button, and the anvil electrode a large one, as in the Blake transmitter. As the mass and pressure upon the anvil electrode were varied, the currents in the secondary at first increased up to a maximum, and afterwards diminished, as shown in the article just referred to, as well as in the curves given with the present paper. Tables I. to XVI. give the numerical results obtained, and Figures 1 to 14 are curves showing the relations between the variables, the loads being abscissas, and the corresponding currents in milliamperes the ordinates. The unit of weight adopted was -j85- of a gram. The remarks in the third column of the tables indicate the nature of the sound heard in a receiving tele- phone placed in the secondary circuit. The current was in all cases zero when the load was zero. TABLE I. Electrodes. — Iron, Iron. Load. Current. Remarks. 1 .19 Sound rough and unsteady. 2 .24 Slirill, clear, metallic, unsteady, 3 .16 u a it it Load. 1 2 3 4 5 6 7 Load. 1 2 3 4 5 6 OF ARTS AND SCIENCES. 95 TABLE II. Electrodes. — Platinum, Platinum. Load. Current. Remarks. Quality good ; fluttering, metallic. 1 .43 2 .02 Qualii 3 .73 4 .23 5 .10 TABLE III. fluttering. Electrodes. — Carbon, Carbon. Current. Remarks. .44 Harsli ; loud. .63 IC It .71 Quali ty good ; fluttering. .67 II n slight fluttering, .27 i t tt faint fluttering. .18 It u a a .12 tt tt t€ ft TABLE IV. Electrodes. — Platinum, Carbon. Load. Current. Remarks. Harsli and loud. 1 .43 Hars 2 .59 3 .67 Qual 4 .59 5 .12 Fain 6 .09 TABLE V. Quality good and clear, some fluttering. U it it tt te Faint, fluttering. Electrodes. — Carbon, Platinum. Current. Remarks. .445 Harsh and loud. .61 Clear : good quality. .66 Clear; some fluttering. .63 Faint; good quality ; some flutt< .29 n n it tt >> .20 ■( ii ii " 9Q PROCEEDINGS OF THE AMERICAN ACADEMY .4 *■©.. js> n-Fe V -/V / 2 3 4 Fig. 1. / .4 A / \ •3 ■3 « 5 .180 faint. 6 .099 11 11 << >< TABLE XIV. Electrodes. — on, Iron. Load. Current. Remarks. 1 .345 Rough, steady. 2 .515 3 .615 Good quality. 4 .560 t- 7V ,7 i .5 A 7~ a 3 j 5 Fig. 8. Fig. 9. An i i '0 \ Ft - n X ' 2- 3 4 5 Fig. 10. / <2 3 4 5 6 Fig. 11. OF ARTS AND SCIENCES. llll -7V ft -C I 2 3 4 5 6 Fig. 12. i 2 3 4 5 6 Fro. 13. ' 2 3 4 5 6 7 Fig. 14. 102 PROCEEDINGS OF THE AMERICAN ACADEMY TABLE XV. Electrodes. - - Copper, Carbon. Load. Current. Remarks 1 .390 Rough and loud. 1.6 .490 « << 2 .590 (i « 2 5 .550 << (£ 3 .250 « H 3.5 .130 i» 60 70 INDUCED CUfiRCHT. Fig. 1. OF ARTS AND SCIENCES. 11. "» One of these curves is shown at 1, Figure 1, the core in this cum- being a cylindrical bar of Norway iron 4| inches long and \ of an inch in diameter, and the diaphragm an ordinary disk of ferrotype iron •_'1'J inches in diameter and yj^ of an inch thick (No. 31 I». W. G.). Table I. gives the data from which Figure 1 was constructed. The strength of field is given in terms of the tangents of the angles of de- flection of the magnetometer needle. The induced current is given in arbitrary units, as only relative values are needed. A determination of the value of the deflections was made by observing the excursion due to the discharge of a condenser through the ballistic galvanometer, and it was found that the abscissa 100 on the curves corresponds to a sudden discharge of approximately 0.00000097 of a coulomb through the coils of the galvanometer. 31. TABLE I. i, Norway Ikox. — Diaphragm, Disk of Ferrotype Iron, N Strength of Induced Strength of Induced Field. Current. Field. Current. . . . 0.7 .211 20.5 .016 3.3 .229 19.8 .044 12.0 .248 19.2 .058 19.3 .270 18.7 .089 23.3 .302 18.0 .118 27.0 .342 16.9 .141 26.8 .390 16.1 .132 26.6 .454 14.7 .146 25.3 .530 13.8 .164 23.8 .625 12.7 .182 22.5 .773 12.0 .196 21.6 1.014 11.5 Cores of Bessemer steel and of untempered soft steel were also used, with results given in Tables II. and III. TABLE II. ESSEMER Steel. — Diaphragm, Disk of Ferrotype Iron, •ength of Induced Strength of Induced Field. Current. Field. Ciirri'iit .005 2.0 .279 L7.8 .030 7.7 .:;:::: 16.7 .082 20 7 .390 1-"'" .137 26.7 .507 18.6 .160 24.8 .<;.'.". 11.7 .191 21.2 .748 10.8 .213 19.3 .'jut 9.7 .248 18.6 1 099 8.7 116 PROCEEDINGS OF THE AMERICAN ACADEMY TABLE III. Core, Untempeeed Soft Steel. — Diaphragm, Disk of Ferrotype Iron, No. 31. Strength of Field. Induced Current. Strength of Field. Induced Current. .031 8.2 .275 18.0 .049 12.0 .321 16.5 .089 22.0 .388 15.2 .137 25.9 .473 13.8 .157 24.9 .618 12.7 .171 22.9 .776 11.0 .194 21.1 1.011 9.5 .216 19.7 An examination of Figure I, as well as of the various curves fol- lowing it, will show that the effect of increasing the strength of the magnet of the transmitter is in all cases to cause at first a rather rapid increase of the strength of the induced current, which later increases less rapidly, rising soon to a maximum value, from which it falls off, at first rapidly, and afterwards more and more slowly as the strength of the field is further increased. We proceed to consider the explana- tion of these results. It is evident that three distinct sources of variation exist to affect the current furnished hy a magneto transmitter as the strength of the magnet is increased. First, the direct effect of the increased strength of field in which the diaphragm moves is to increase proportionally the strength of the induced current, since it increases correspondingly the rate of change in the number of lines of force enclosed by the coil of the instrument ; second, an approach toward saturation of the magnet, so far as it alone is concerned, will tend to diminish the induced current, on account of the smaller variation in the strength of the pole due to a given motion of the diaphragm ; and, third, the nearer approach toward saturation of the diaphragm will have the same tendency. The rapid rise in the induced current at the beginning is of course due to the predominating influence of the increasing strength of the field in which the diaphragm moves, as both core and diaphragm are then but slightly magnetized. The subsequent changes in the current must be explained by a consideration of the increasing magnetization of either the core or the diaphragm, or both. It will be seen by comparing Tables I., II., and III., that the value of the maximum induced current for a given excursion of the diaphragm OF ARTS AND SCIENCES. 117 is approximately the same with all the three cores used, and that the same is true as to the strength of held corresponding to this maxi- mum current. Moreover, saturation curves constructed for the several cores showed that in all cases the magnet was still very far removed even from half-saturation when the maximum induced current was ob- tained. From these facts it appears that the degree of saturation of the magnet is practically unimportant, so far as the general results shown in Figure 1 are concerned. It remains to observe the part played by the increasing magnetiza- tion of the diaphragm. Other things remaining the same, as this ap- proaches more and more closely towards saturation the increase in the number of lines of force passing between it and the magnet on the approach of the diaphragm to the magnet must become smaller and smaller, and this change will tend to oppose the effect of the increased absolute strength of the magnetizing force. The small mass of the diaphragm will evidently cause it to show the effect of an approach to saturation while the core is far below that condition. And such an ac- tion will clearly explain the observed changes in the current strength. In order to test this matter still further, the experiment was tried of varying the mass and material of the diaphragm. The results are shown by the curves in Figures 1, 2, and 3, which are constructed from the data given in Tables I. to X. ; further results of the same character are given in Tables XI. and XII. TABLE IV. Core, Norway Iron. — Diaphragm, Two superposed Disks of Ferrotype Iron, No. 31. Strength of Induced Strength of Induced Field. Current. Field. Curreut, .016 5.0 .184 49.3 .054 19.3 .205 50.2 .070 25.7 .229 48.0 .081 28.5 .266 40.3 .089 30.2 .306 31.8 .103 35.0 .342 27.7 .119 38.5 !483 18.7 .133 40.7 .530 11.9 .144 42.7 .607 8.3 .155 45.7 .830 7.0 .169 47.0 1.018 5.0 118 PROCEEDINGS OF THE AMERICAN ACADEMY moN Ul U> N «• M 60 .0 UU 90 HU *m 120 vi/ducco cunm/7 Fig. 2. C ft; V3 ytQ iO at, ~$Z ip 60 60 70 60 so induced current. Fig. 3. OF ARTS AND SCIENCES. 119 TABLE V. Core, Norway Iron. — Diaphragm, Three superposed Disks of Ferrotype Iron, No. 31. Strength of Field. Induced Current. .000 0.5 .018 3.2 .047 8.0 .079 14.2 .084 14.7 .096 17.0 .110 19.7 .118 21.8 .135 25.5 .151 28.3 .175 33.0 .213 39.0 .249 46.3 .277 49.8 .313 55.3 .329 58.7 TABLE VI, Strength of Induced Field. Current. .346 59.7 .366 60.7 .390 61.3 .416 63.0 .445 62.3 .479 61.0 .514 58.5 .550 55.7 .591 52.4 .637 48.7 .659 47.3 .765 41.7 .854 36.7 .983 30.0 1.180 22.8 Core, Norway Iron. — Diaphragm, Sheet Iron, No. 21. :ength of Field. Induced Current. Strength of Field. Induced Current. • > • 0.3 .456 96.7 .016 3.1 .477 94.0 .058 13.7 .499 92.5 .082 20.3 .521 90.5 .102 25.2 .536 88.3 .125 31.2 .573 86.7 .150 37.8 .584 84.0 .178 45.5 .637 81.0 .213 54.7 .675 76.7 .249 63.8 .724 72.8 .296 75.5 .784 .348 86.2 .851 .378 92.3 .949 67.8 .416 96.7 1.001 49.1 .437 97.8 120 PROCEEDINGS OP THE AMERICAN ACADEMY TABLE VH. Coke, Norway Iron. — Diaphragm, Sheet Iron, No. 22. Strength of Induced Strength of Induced Field. Current. Field. Current 1.7 .410 942 .018 4.7 .431 92.0 .047 11.7 .452 88.3 .075 19.7 .473 85.0 .088 22.3 .494 81.2 .100 26.0 .516 77.5 .123 32.5 .541 74.7 .146 39.5 .566 71.3 .171 48.2 .601 67.7 .194 54.2 .635 64.0 .218 61.3 .659 60.0 .240 66.9 .719 56.7 .262 73.2 .779 53.0 .292 81.3 .851 48.0 .313 87.7 .946 44.0 .342 92.7 1.072 39.3 .372 94.3 1.091 38.3 TABLE VIII. Core, Norway Iron. — Diaphragm, Sheet Iron, No. 23. Strength of Field. Induced Current. Strength of Field. Induced Current. ... 1.7 .272 109.3 .026 10.0 .289 113.8 .068 26.8 .310 119.3 .086 33.0 .339 118.6 .096 39.0 .382 114.1 .116 47.0 .420 102.9 .139 66.3 .458 82.2 .162 65.8 .499 68.7 .176 72.3 .629 67.6 .194 78.3 .582 48.0 .216 86.4 .652 39.9 .229 90.0 .751 30.8 .242 96.3 904 23.7 .255 101.8 1.011 19.0 OP ARTS AND SCIENCES. 121 TABLE IX. 3RE, Norway Iron. — Diaphragm, Steel, No. 26, Untempere Strength of Field. .004 Induced Current. 7.7 Strength of Field. .281 Induced Current. 66.7 .019 11.5 .313 G3.8 .054 20.5 .342 60.4 .095 32.2 .380 56.3 .105 34.5 .422 50.5 .128 42.0 .483 44.7 .153 48.3 .530 39.0 .178 55.7 .5JB4 35.3 .200 G0.3 .652 32.0 .227 64.3 .810 28.2 .236 67.0 TABLE X. 1.043 24.3 Core, Norway Iron. — Diaphragm, Steel, No. 26, , Tempered, Strength of Field. Induced Current. Strength of Field. Induced Current. .002 7.8 .344 36.3 .019 10.4 .400 32.0 .008 18.5 .406 26.9 .096 23.8 .545 21.7 .128 30.3 .642 17.7 .151 32.4 .662 17.3 .180 37.0 .732 15.2 .214 40.2 .816 13.8 .246 40.0 .854 13.0 .272 39.5 1.025 10.0 .304 37.9 TABLE XI. ire, Norway Iron. — D IAPHRAGM, Steel, No. 22, Untemperei Strength of Field. Induced Current. Strength of Field. Induced Current. .007 6.2 .272 86.7 .023 8.0 .302 34.8 .070 17.3 .340 33.0 .103 23.0 .392 29 7 .121 26.4 .458 •J';.;: .139 30.1 .538 28 2 .157 32.8 .666 28.0 .176 35.0 .HIT 21.7 .202 37.1 .77:: L9.8 .224 34.9 1.046 17.6 .246 37.0 122 PROCEEDINGS OP THE AMERICAN ACADEMY TABLE XII. Core, Norway Iron. — Diaphragm Steel, No. 30, Tempered. Strength of Induced Strength of Induced Field. Current. Field. Current. .007 6.2 .272 36.7 .023 8.0 .302 34.8 .070 17.3 .340 33.0 .103 23.0 .392 29.7 .121 26.4 .458 26.3 .139 30.1 .538 23.2 .157 32.8 .566 23.0 .176 35.0 .647 21.7 .202 37.1 .773 19.8 .224 ... 1.046 17.6 .246 37.0 TABLE XIII. Core, Norway Iron. — Diaphragm, Steel, No. 30, Untempered. Strength of Induced Strength of Induced Field. Current. Field. Current. .005 5.2 .331 31.2 .031 11.7 .376 28.9 .082 24.2 .437 26.0 .103 29.7 .512 23.3 .130 37.7 .632 20.4 .160 41.9 .735 19.7 .200 38.3 .819 18.0 .231 36.2 .956 16.3 .272 35.2 Curve 2, Figure 1, represents the results when two of the ordinary ferrotype diaphragms were superposed, forming a diaphragm of double thickness, and Curve 3 of the same figure shows the results when three such diaphragms were superposed. Each diaphragm was 0.01 of an inch thick. The curves of Figure 2, marked 21, 22, 23, respectively, show the results of similar experiments with diaphragms of sheet iron whose thickness was 0.030, 0.027, 0.024 of an inch, respectively (Nos. 21, 22, 23, B. W. G.). Figure 3 shows the results when a steel dia- phragm 0.017 of an inch thick (No. 2G) was used, the curve U being that for untempered steel, and T that for tempered steel. Steel dia- phragms respectively 0.026 and 0.012 of an inch thick (Nos. 22 and 30) gave similar results, as will be seen from Tables XL, XII., and XIII. OF ARTS AND SCIENCES. 123 An inspection of these curves shows immediately that the greater the strength of the field required to saturate the diaphragm, the - in con with the edge of the diaphragm, while the other, about which the coil is wound, is placed in its usual position opposite the centre. Bui as :i general rule little or no gain has seemed to result therefr • ■■■ far U can be judged by the performance of such instruments in actual prac- 124 PROCEEDINGS OF THE AMERICAN ACADEMY tice. It is quite probable in tbis case tbat the increased approach to saturation of the diaphragm may have so great an effect as entirely to prevent the expected improvement- It will also be seen from our results, that an increase in the thickness of the diaphragm of a magneto transmitter tends to allow of the use of a stronger magnet, and for a given amplitude of vibration to produce a stronger current. But it must be remembered, on the other hand, that the greater rigidity of the thick diaphragm will diminish this range of vibration under the action of the voice, a difficulty which may to a certain extent be remedied by using a diaphragm of large diameter. Rogers Laboratory of Physics, October, 1888. OP ARTS AND SCIENCES. 125 Investigations on Light and Heat, made and published wholly oe in paet with Appeopeiation feom the Rumfobd Fond. XII. AN ACCOUNT OF A NEW THERMOGRAPH, AND OF SOME MEASURES IN LUNAR RADIATION. By C. C. Hutchins, assisted by Daniel Edward Owen. Presented by Professor Trowbridge, March 13, 1389. During the winter of 1886-87 the writer carried out at Cambridge a series of experiments with the bolometer and other sensitive heat- measuring devices, the intention being, if the apparatus could be made to perform satisfactorily, to attempt the solution of some problem in radiation. One in particular in mind was that of the radiation from rocks, as important from a geological standpoint. It was also thought possible that the work might be made a valuable supplement to Lang- ley's investigations in lunar radiation. After two or three months of preliminary experimentation the matter was abandoned, and the further pursuit of the subject was not undertaken until October, 1887. In designing a working apparatus for use in the research thus resumed, some modification of the thermo- pile suggested itself, and a contrivance was finally adopted constructed upon the principle embodied in that familiar instrument. This new device possesses the sensitiveness necessary for accurate and delicate work, and at the same time is very simple in operation. This last is an important feature, for in all instruments intended for measuring small quantities of heat the matter of simplicity is a very grave one. It hardly needs saying, that the number of the parts in the instrument should be limited to as few as possible, and that the whole should be as simple as it can be made. Multiplication of parts leads to inaccu- racy in performance with almost absolute certainty. It is the element of simplicity that has, until recently, rendered the ordinary thermopile the most successful instrument possible to be employed in dealing with small quantities of heat. The failings of the thermopile, however, are so numerous and so fatal that it becomes an instrument of pn ion in the hands of a very few, who must serve a long apprenticeship in its use. 126 PROCEEDINGS OF THE AMERICAN ACADEMY Impressed with the number of the difficulties which beset the use of the thermopile, the writer set about a systematic study of the condi- tions necessary to their removal. It was soon observed that a great advantage could be gained by employing a single thermal junction, instead of many, and by condensing the heat rays upon this one by means of a concave mirror. All of the advantages of the thermopile are thus retained, while its most serious failing — the slowness with which the large mass of metal presenting the sensitive surface parts with its heat — is obviated altogether. The condensing mirror fulfils the function of multiplied junctions, while the single union of bars employed in the new instrument rapidly attains thermal equilibrium under any series of conditions. This preliminary proposition having been laid down, — that a single junction of two metals, suitably supplemented by a concave mirror, can be made as effective as a larger number of junctions without the mirror, — various experiments were next undertaken with a view to ascertaining the best form for the single junction, as well as the most suitable materials to enter into it. With these ends in view a great number of unions were made, including some very delicate combina- tions into which tellurium was introduced. The bars of metal used in these experiments were made very thin, and in attempting to form certain junctions great difficulty was experienced ; for when very thin bars of easily fusible metals are to be soldered together, it is some- times almost impossible to perform the act properly, without melting the bars. In such cases the electro-deposition of silver or copper in the junction succeeds admirably. As the outcome of these experiments it was learned that the best results could be obtained from a junction formed by two of the stronger metals, worked into very thin strips, the opposite ends of the metal ribbon thus formed being attached to copper rods — the terminals — with the point of junction midway between. The reasons for such a construction and the advantages especially to be derived from it are briefly these. It is plain that a thin strip of metal will not only take up and part with its heat in a much shorter period of time than will a thick bar, but that it will also, in a given interval, be raised to a much higher temperature than the thick bar. The strong metals are employed for the obvious reason that the brittle metals cannot be made into very thin leaves and at the same time remain self-sustaining. Further, thin strips of even such metals as iron and copper, the thermo- electric force of which is comparatively feeble, brought into conjunc- tion, give a greater electric current when excited by a feeble radiation OF ARTS AND SCIENCES. 127 than is obtained from a junction of bars of antimony and bismuth under similar circumstances. Finally, to employ a condensing mirror having the junction at its focus is simpler than to multiply the number of junctions, and, moreover, it adds nothing to the resistance of the circuit. Instruments. The Thermograph. There will now be described, in detail, the instrument which was the outgrowth of the principles touched upon above. It is not beyond the power of one possessed of very ordinary mechanical skill, and who may be perforce his own instrument-maker in matters like the present. The measures will be given in inches, since most workmen still employ that unit. A cvlinder is turned from vulcanite, or some hard wood. 3 in. lon<» and 1 in. in diameter. For f in. at one end this cylinder is made of less diameter by -^s in., in order that it may receive and hold firmly a piece of brass tubing 3 in. long, 1 in. in external diameter, and ^.y in. thick. The end of the cylinder carrying the tube will be designated in what follows as the " front end." The cylinder is next pierced, in the direction of its length, with two J in. holes lying upon the same diameter and ^-e in. apart. Through these holes copper rods are firmly driven, being left to project -J- in. above the front end of the cylinder. They are allowed to project f in. from the back end of the cylinder, and are afterwards bent apart somewhat to facilitate the attachment of screw cups. The front ends of the rods are made somewhat smaller than the other portion by filing. The thermal junction is made as follows. Some bits of rather wide watch-spring are procured, together with some rolled sheet nickel. A strip of the same width as that of the watch-spring is cut from the nickel, and, the ends of the spring and of the piece of nickel having been scarfed with a file, the two are united by means of the strongest hard solder obtainable. For convenience in handling, it is well to leave the piece of watch-spring long. The compound strip can now be made straight upon the edges, and worked thin with a line file. Trial is occasionally made with a screw caliper, and when the thick- ness has been reduced to .02 mm. it is best to discontinue. The solder junction must be very perfect, or it will be pulled apart in the filing. With great care and patience the thickness of the strip of metal can be reduced to .01 mm., but there is no compensating ad- vantage for the labor expended. When finished, the wide strip can 128 PROCEEDINGS OF THE AMERICAN ACADEMY be cut with scissors into several narrow bands, and preserved in a dry bottle. To complete the thermograph, a strip is selected from the stock, laid across the rods at the front of the cylinder, and secured in place with a little soft wax. The wax permits the strip to be shifted, until it is proved by measurement that the junction is exactly midway between the rods, when the strip is permanently fixed by soldering it to the rods. A small concave mirror of glass, silvered upon the first surface, is now fixed to the front end of the cylinder, between the copper rods, with glue or varnish. The mirror should be \ in. in diameter and of | in. focus. When in place, the junction in the metal strip should be exactly at its focus. The brass tube is carefully blackened within, and is provided with diaphragms, the openings in which are determined by the character of the work for which the instrument is intended. The front end of the brass tube is also furnished with a suitably perforated end-piece of the same material as the cylinder. For some purposes the tube of the instrument requires to be made longer than that of the sample de- scribed above, and for other purposes it may be dispensed with. For linear measurements, as in spectrum work, it is only necessary to re- place one or more of the diaphragms by slits at right angles to the direction of the strip. The apparatus is particularly successful in dealing with small quantities of heat at a point. When employed for this purpose, the condensing mirror is not used, the junction being merely placed behind a small hole in a trif>le screen, formed by two plates of metal separated by a thick plate of cork or other non-con- ducting substance. If for any particular purpose it should be desired to make use of a strip thinner than can be produced by the methods given above, it can be prepared after the following manner. A flat plate of copper is rubbed with graphite and nickel-plated over one half its surface. It is then dried, rubbed with graphite a second time, and the nickel-coated end dipped in melted paraffine nearly to the junction of the nickel and copper. The remaining half of the copper surface can now be plated with iron from a solution of the citrate, the nickel already deposited being protected by its paraffine coating. When the entire thin film is afterward stripped from the copper backing, one half of it will be nickel, the other half iron, and it can be cut into narrow strips as before. The writer has to learn that there is any advantage to be gained from employing strips made in this manner, and they are certainly difficult of manufacture. In general, thin films of electrically deposited metals OF ARTS AND SCIENCES. 129 are hard to manipulate, for they possess the elasticity and brittleness of highly tempered steel, and usually require careful annealing. The Galvanometer. The galvanometer intended to accompany the heat-measuring device should receive as careful attention as the device itself. The writer had had some previous experience in the construction of sensitive galvanometers before attempting the research of which the present article is an account ; nevertheless, several different forms were tried before one was found exactly adapted to the thermograph. The re- quirements to be met were, in brief, first, considerable sensitiveness, and secondly, rapidity of working, — qualities which are to some ex- tent incompatible, but which have, as far as possible, been combined in the instrument in use. It would have been possible to produce an instrument much more sensitive than the one actually employed, had the rate of working been left out of account; but nothing is more annoying than to be obliged, when time is precious and opportunities for observation are perhaps few, to wait for a galvanometer needle to come to rest ; consequently the element of time has had the first consideration. The galvanometer adopted for use with the thermograph has four coils, each containing about four feet of wire 0.063 in. in diameter. The wire was twice shellacked and baked before beinjj wound. The coils are contained between brass plates, which constitute the body of the instrument, the inner faces of the two plates, which are in contact, being grooved for the passage of the staff of the needle and its sup- porting silk fibre. The needle thus swings in an entirely closed space but little larger than itself, and needs no damping vanes to bring it quickly to rest. Two minute scales of mica are attached to the needle to prevent it from being turned completely round. The astatic system has the magnets fixed upon a very slender aluminum staff two inches in length. The magnets are from ] in. to g in. in length, and very slender. The mirror is flat, and | in. in diameter. Much of the suc- cess of the instrument depends upon the perfection of the mirror. It is difficult to obtain perfectly plane mirrors, and. moreover, those to be had in the market are too heavy. They can be made, of great per- fection, by selecting a perfectly flat piece of thin plate glass, cementing it to a thicker piece of glass for a support, and then grinding it down to the thickness of stout letter paper. A very thin sheet of glass is thus obtained, from which circles of the required size can be cut with a diamond. The glass being now silvered upon the Burfaoe, the polish VOL. XXIV. (\-. S. XVI.) 9 130 PROCEEDINGS OP THE AMERICAN ACADEMY of which was not destroyed by the grinding, we have a first surface reflector which will bear a high magnifying power if the mirror be not strained in mounting. The scale is read in a novel manner. The cell in which the mirror swings is closed by a bit cut from the centre of an ordinary spectacle lens of from 36 to 48 inches' focus. The scale is located as in the ordinary arrangement of telescope and scale, but instead of the tele- scope we have the following device. A tin or paper tube is provided, and in it, at a distance of five inches from one end, is placed a lens, three inches in diameter, and of six inches' focus. The end of the large tube has a draw-tube, which is closed by a metal plate provided with a peep-hole at its centre. The peep-hole may be made to occupy the focus of the lens by sliding the draw-tube backward or forward as required. A horse-hair or very fine wire is stretched across the tube in the focus of the lens opposite the draw-tube, so that it may be clearly seen by the eye applied to the peep-hole. This arrangement is to be mounted in the place occupied by the ordinary telescope, which it far surpasses both in definition and in the breadth of the field of view. The whole apparatus when in position opposite to the gal- vanometer constitutes a telescope, of which the lens in the galvanome- ter is the object-glass, the large lens in the tube the eye-piece, and the scale the object viewed. The definition is quite remarkable, the fibre of the paper upon which the scale is ruled showing clearly, as though seen through a magnifying-glass. The details of construction of the entire apparatus having thus been outlined, it remains to speak of the action of the whole. As an ex- ample of the accuracy that may be expected in the performance of the instrument, the following test may be taken. October 23d, 1888, the sun was taken as a source of heat, the rays being reduced by passage through a small opening. The following galvanometer deflections were obtained : — Divisions. Divisions. First 162 Sixth 164 Second .... 162 Seventh .... 162 Third ..... 161 Eighth 161 Fourth .... 162 Ninth 161 Fifth 162 Tenth 162 The observations were taken rapidly, occupying less than ten min- utes in all. No great effort has been made to secure superior sensitiveness, yet the heat from the face of a person at a distance of fifty feet is measur- OF ARTS AND SCIENCES. 131 able. A comparison was made between tbe thermograph and a ther- mopile of forty-eight couples. Using the same galvanometer for each, the thermograph proved about twelve times as sensitive as the other instrument. The limit of sensitiveness could be very much extended, if it were desired, by the use of a more delicate galvanometer. As actually adjusted, the galvanometer employed gives a deflection of one scale division for 0.00000007 Ampere, the period being ten seconds. The constant of Langley's galvanometer was 0.0000000013 Ampere, or fifty times less. Radiation from Rocks. As experiments upon the radiating power of rocks and minerals were the first in which the new instrument was employed, they will be first discussed. The want of a standard of radiation which should be more satis- factory than a lamp-black-coated surface was seriously felt in these experiments. Lamp-black is a hygroscopic substance, and radiates differently when in different states, unless it be applied with sufficient varnish to make it water proof. But if it be mixed with the smallest possible amount of varnish, and applied to a surface, then the radiating power is different from that of the same surface coated by camphor smoke. Also, it appears to radiate differently when applied in the same manner to different substances. The writer has always found ordinary white pumice-stone a better radiator than the same black- ened. There is no other instance in which so variable and imperfect a standard is tolerated. The writer has employed as a working standard in these experiments a piece of pure quartz finely ground with emery but unpolished. Such a standard seems to possess many advantages. Quartz is readily obtainable in a pure state. It is im- perishable and unalterable at any ordinary temperature. It has the great merit of perfect definiteness of composition. The measures of radiation from the rocks were made as follows. Each specimen had a wooden handle adapted to it, for convenience in handling when hot. The rocks were heated in an oven intended for drying chemical precipitates. The oven was of heavy iron, and was heated from beneath by numerous small gas jets. It was found that. after the gas had been lighted about an hour, the temperature of the oven became constant, and remained so for any length -.1' time. rock under experiment and the quartz standard were placed in tl"' oven together, side by side, and after the lap- of an hour they were removed, first the quartz and then the rock being quickly taken from 132 PROCEEDINGS OF THE AMERICAN ACADEMY the oven, presented before the opening in the thermograph, and the deflection noted. The specimens were then returned to the oven, and some time allowed to elapse before the experiment was repeated. In this way as many measures were obtained from each specimen as could be made in the course of a day, i. e. from ten to thirty. The method seems far from perfect, but it was the best of several that were tried. To reduce the results to the lamp-black standard, a very careful comparison was made between the radiating powers of blackened and unblackened faces of the quartz. The temperature at which the measures were made was near 100°. The results are given in the following table, the radiation from a blackened surface of quartz being taken as 100. Name. Locality. Character. Radiating Power. Lava Lava Lava Lava Lava Pumice Lava Scoria Pumice Trap Trap Obsidian New Red Sandstone Flexible Sandstone Slate Slate Feldspar Gypsum Iceland Spar Mica Serpentine Quartz Amphibnle Tremaolite Pyrite White Marble Mica Schist Granite Hawaii Vesuvius D'Auvergne D'Auvergne Hawaii Vesuvius Vesuvius Vesuvius Nova Scotia Mt. Kineo Pembroke Georgia Pennsylvania Georgia Topsliam, Me. Hebron, Me. New York Imperfectly fused. Black Dense. Gray Basaltic. Dark Scoria. Light red Well fused. Red Common. White Vesicular. Black Very light and porous. Black Red Dark Light gray Black 91.2 90 4 81.8 86.5 91.9 71.3 86.3 91.6 89.1 83.2 94 88.5 89.3 85.9 89.8 84 1 88.5 86 85 76.3 891 90.8 91.4 85.5 76.4 86.7 80.8 93.5 Red From coal beds, with pyrite. Red Pure white Pure white Pure Common. Green Pure. Transparent Common. Green Pure white Fine-grained. An inspection of the table shows a remarkable uniformity in radiat- ing power for materials so diverse in character. The large number of volcanic rocks was selected, because it seems probable, from its physi- OF ARTS AND SCIENCES. 133 cal features, that the rocks of which the surface of the moon is made up are of volcanic character. Lunar Radiation. While the light received from the moon has been frequently meas- ured by many different observers, the more important problem of its dynamic radiation has been solved by but a single person. Observers previous to Langley can pretend to so little accuracy in their results, that our knowledge of lunar radiation may be said to rest upon his authority alone. This condition does not arise from any lack of in- terest in the subject, — on the contrary the problem has always been a fascinating one, — but is due to the fact, that, previous to the invention of the bolometer, no instrument existed capable of dealing accurately with so small an amount of heat as the moon affords. Great interest, therefore, cannot fail to attend the results of careful observation, made with competent instruments, and tending to increase our knowledge of the subject. The first trial of the new thermograph on the moon was made on January 27, 1888. The apparatus, tested at that time, has been regu- larly employed since, and has performed so satisfactorily that it has scarcely been altered from its original form. The arrangement of the thermograph for the measurement of lunar radiation is this. An oblong box of pine wood carries at one end a silvered glass mirror, 0.196 metre in diameter, and of one metre focus. This mirror is ad- justable by screws passing through the end of the box and bearing upon its back. Near the other end of the box is fixed a grooved block, upon which the thermograph may be placed and secured. The block is also provided with adjusting screws, so that the thermograph may be made to point exactly at the centre of the mirror. The mirror is inclined, so that the moon's image is thrown into the opening of tin- thermograph, and brought to a focus upon the strip. The whole arrangement is that of a Herschel's telescope with the thermograph in place of an eye-piece. To secure accuracy in pointing, the opening in the thermograph is made of such a size as just to receive the cone of rays from the large mirror, and, a rim of white paper being glued about the opening, the slightest departure from a central position of the cone of rays is an- nounced by the appearance of light upon this paper. A window oi plate glass has its place in the side of the box, just in front of tin- position occupied by the thermograph, and a person looking through this can readily direct the image of the moon into the orifice of tin- 134 PROCEEDINGS OF THE AMERICAN ACADEMY thermograph. A telescope, with cross wires, is also attached to the box, and may be used to direct it, but the former method is much the more satisfactory. The eutire apparatus is mounted upon a massive telescope tripod. The mounting has tangent screw motions, and is provided with a ver- tical circle for reading the altitudes. An hour or two before it is in- tended to observe, the apparatus is mounted in the open air, in order that it may have time to acquire the external temperature. Two strands of heavy electric light wire pass from the thermograph to the laboratory, where they are attached to the galvanometer, which is mounted upon a firm pier. For some reasons the effect of phase should precede all other con- siderations as a subject of investigation, but it has been postponed until later. The subjects that have engaged our attention, up to the present time, may be for the most part classed under two heads : 1. The comparative intensity of radiation of the full moon and of the sun. 2. The absorptive effect of the earth's atmosphere upon the radiation of the moon. These two topics will be considered in turn. It is obviously impossible to confine the observations to the time of full moon without giving undue time to the investigation ; hence the effect of phase demands to be considered. To avoid the introduction of errors from this source the following precautions have been taken : 1. To confine the observations to the three days nearest full moon. 2. To measure always the radiation from a constant area of the moon's surface. To fulfil the conditions of the second jitrecaution, there is placed, close to the strip of the thermograph, a diaphragm, the open- ing in which is much smaller than the moon's image which falls upon it. Thus there may be a large change of phase, and the opening still remain full of the moon's image. This arrangement would completely remove the difficulty, provided that the moon reflects like a flat disk, as Zblner thinks, — which is not at all certain. It is believed, how- ever, that, when taken in connection with the first precaution, the out- standing error cannot be large. The method has the disadvantage of reducing the available heat by about one half; but, as it is, the heat is sufficient to drive the needle off the scale with the galvanometer in its most sensitive condition. The controlling magnet is set so that a deflection of between one and two hundred scale divisions is obtained, corresponding to a period of between five and ten seconds' vibration of the needle. OF ARTS AND SCIENCES. 135 One observer being stationed at the galvanometer, and a second at the instrument out of doors, at a signal from the first, the latter brings the image of the moon into the opening of the thermograph, and the deflection occasioned is noted and recorded by the observer at the gal- vanometer. In this manner a set of ten readings is taken, and, the altitude of the moon being measured at the beginning and the end of the set, the mean of the ten deflections is taken as the deflection cor- responding to the mean altitude. About six minutes are required to make a set of the readings. The following series, selected at random from the observation-book, will serve as an example of the results obtained. Date. — February 24, 1888. Mean Altitude. Mean Time. Deflection. Mean Deflection 62° 40' 7 h. 34 m. .... • • • • • • • • ■ • • 171.5 • • * • . . . . . 172 • • • • • • • . . 168.5 • • • • • • • , . 166 . • • • • • • • • 171 . . . • • • • • . 174 • • • • • • • • • • 172 • • a • • • • • . 175 . a • • • ■ • » • • 173.2 a a • • • *• • . . 175 a . a • • • • • • ■ • a • • 171 8 The probable error of a single observation, when the moon is the source of heat, is considerably greater than is the case with an arti- ficial source, or even with the sun. The cause is, in part, due to in- visible clouds of vapor floating in the atmosphere, as Langley thinks. It has been observed that immediately after rain this effect is particu- larly noticeable, even when the sky appears perfectly clear to the eye. There is another cause, which doubtless exerts a large influence ; that is, the irregular radiation of different portions of the moon's surface. It has been found* that, photographically, the mean bright- ness of the dark region is to that of the bright rejrion in the ratio of 55 to 100. We might be prepared to expect large differences in the radiant energy of the respective regions, and the average radiation may therefore be more closely attained from a series in which the in- dividual readings vary considerably, than from a more perfectly con- cordant set. * Annals of Harvard College Observatory, Vol. XVIII. No. IV. 136 PROCEEDINGS OF THE AMERICAN ACADEMY Having obtained a sufficient number of sets, as perfect as may be, we have next to effect a comparison between the deflections produced by the moon, and the deflections brought about by the sun under simi- lar circumstances of observation, — such as altitude, height of barom- eter, etc. The heat of the sun's rays must be reduced in some manner in order to bring them within the range of the same instru- ment employed in measuring the feeble radiation of the moon. Both Lord Rosse and Langley accomplished the reduction by passing the sun's rays through a small ojjening, and placing the heat-measuring appliance in the diverging beam. The enormous differences that appear in the results of observers who have measured the light of the moon, and compared it with sun- light, put us upon our guard against sources of error, and impressed upon us the necessity of going over the ground by independent methods. Let us consider the probable sources of error in the above mentioned method of comparison : — 1. Errors of observation. These are small, and can be reduced to any extent by repeating the observations. 2. Absorption by the mirror, used in condensing the lunar rays. The mirror is always kept perfect by frequent silvering, and a flat mirror, silvered by the same process, is employed in reflecting the sun's rays to the small opening. 3. The plate of metal in which is the perforation becomes a source of heat when the sun's rays are thrown upon it, and would increase the heat indication. This effect is avoided by placing the thermograph so far from the metal plate as to render its influence practically imperceptible. 4. Effect of diffraction at the opening. Unknown. As an example of the results obtained by this method, let us take the observations of April 25 and 26, 1888. On the night of April 25, the deflection produced by the moon at an altitude of 42° was 184.8 scale divisions. We have also : Semidiameter of condensing mirror . . 95 mm. Focus " " . . 1000 mm. Semidiameter of moon, augmented . . 17'. Hence we have, for the concentration of the moon's rays, ^_ opq 1 (1000 X sinlT')2 ~ OF ARTS AND SCIENCES. 137 Had the moon's rays, uncondensed, acted upon the thermograph, the deflection would have been : 1S4 8 .„, ' = 0.5003 scale divisions. o09.1 On the following morning, the altitude of the sun being 42°, its rays were reflected through a small opening, and being received by the thermograph, placed at a distance, a deflection of 147.16 scale divisions was found to be the mean of 30 readings. The opening through which the sun's rays were reflected was a carefully reamed hole in a metal plate. Its diameter, being measured under the micro- scope, with the aid of a stage micrometer which purported to be divided into tenths and hundredths of a millimeter, was found to be 1.67 mm. A paper screen received the spot of light, formed by the rays from this opening. The diameter of the spot was 40.6 mm. The thermograph was thrust through an opening in the screen until its strip lay in the plane of the paper. The spot of light could then be thrown into it by turning one of the screws of the heliostat. We have for the reduction of the sun's rays: M, = 615.3. 1.672 Had the thermograph received the undiminished sunbeam, the de- flection would have been : 615.3 x 147.16 = 90596. The ratio of the sun's radiation to that of the moon is, therefore, 90596 0.5008 = 180,900. Second Method. In the second method, the sunbeam is employed without diminution, but its effect is reduced by interposing a resistance in the galvanom- eter circuit. This method is free from all objections, as far as can be seen, for its accuracy depends upon the measurement of a resistance, an operation which can be accomplished with great accuracy. More- over, it removes any effect due to minor disturbing causes, such as the heating of the metal plate in the first method, since, when a large resistance is interposed, the apparatus becomes insensible to such influences. The resistance of the thermograph, galvanometer, and the connect- ing wires, is 0.2095 ohm. On October 21, 1888, the sun's altitude 138 PROCEEDINGS OF THE AMERICAN ACADEMY being 31°, 100 ohms were added to the resistance of the circuit, and when the sun's rays were thrown directly into the thermograph a deflection of 114.6 scale divisions was obtained. Without the 100 ohms of additional resistance, the deflection would have been : 100 X 1U.6 . . ■ — — = 54<00 scale divisions. 0.209a That same evening the moon was observed at an altitude of 30° 15', the deflection being 124.59 scale divisions. From its augmented semi- diameter, 14' 52". 7, and the same constants as in the previous example, we find the deflection for the uncondensed moonbeam to be 0.2945 of a scale division. The ratio of 54700 to 0.2945 is 186,300. The results obtained by the two methods are here tabulated. Ratio of Sun Radiation to Moon Radiation. First Method. Second Method. March 30, 1888 . . . 181,000 October 18, 1888 . . . 187,200 April 25, 1888 .... 180,900 October 21, 1888 . . . 186,300 October 18, 1888 . . . 167,400 Mean of the five results 184,560 The results given by the two methods do not show the wide dis- agreement so noticeable in the comparative light of the two bodies, as found by different methods. This fact is strong evidence in favor of the accuracy of the mean result. In reality, the problem of the total comparative radiation of the sun and moon is in many respects simpler than the problem of the comparative light intensity of the two bodies. In the former case, there is freedom from all personal bias ; the meas- urements are all given by the indications of the instruments directly, and, in general, the chances for error seem to be fewer. Lord Rosse found the ratio of solar to lunar radiation to be 80,000 to 1. Langley obtained the ratio 96,509 to 1. Provided the moon were a flat disk, reflecting perfectly all of the sun's rays that fall upon it, we could not receive more than one 97,000th part of the solar heat from such a disk, as Zolner has shown. The close agreement of his result with this number Langley considers to be largely a matter of chance, or, rather, of constant errors, tending in an unknown degree to increase the observed values. It would be a priori quite improbable that we should, under the circumstances of reflection from the lunar surface and subsequent OF ARTS AND SCIENCES. 139 passage of the reflected rays to the surface of our planet, receive any- thing like the maximum possible radiation. Our atmosphere cuts off a considerable portion of the lunar rays. It has been observed that aqueous vapor is particularly efficacious in stopping them. It may not be uninstructive, as illustrating the minuteness of the quantity of heat that we receive from the moon, to express it in terms of melting ice. It will not be far from the truth if we say that the sun's rays will thaw through an inch of ice in 100 minutes, whence it follows, f'iom our determination, that the rays of the moon will melt the same thickness of ice in 18,456,000 minutes, or 35 years. That portion of the solar rays not reflected from the lunar surface is absorbed by it, and radiated at different wave lengths. At what wave lengths we do not know, and whether or not those rays are capable of passing our atmosphere we cannot tell. An idea of the general character of the lunar rays may be gained from experiments with absorbing media. For example, on April 25, 1888, the per- centage of lunar rays transmitted by a plate of quartz was determined. The quartz plate was 5 mm. thick, cut perpendicularly to the axis of the crystal. It was arranged to be drawn before the thermograph by a thread, so that the observations could be made in pairs, alternately with and without the quartz. The results were as follows : — Moon's Altitude. Deflection through Quartz. Deflection without Quartz. Per Cent transmitted. 13° 38.4 137.2 34.6 19° 54 4 157.0 27.9 24° 30' 51.3 163.2 31.4 Mean of the whole (GO readings) . . . 31.3% An attempt was then made to find some artificial source of heat whose radiations would be transmitted by the plate of quartz to the extent, approximately, of 31%. It was discovered that a coil of platinum wire, in a Bunsen lamp, turned as low as possible, very nearly fulfilled the requirement. We may say, then, that in general character the rays from the moon resemble those from an incandescent platinum wire. The plate of quartz used in the above experiments transmits 93.3% of the sun's rays. A study of the reflection of the sun's rays from rocks may serve, to some extent, to aid in the lunar problem, and to this end a few experi- ments have been made, after the following manner. The thermograph is mounted upon a strip of board, which can ho turned about a pin passing through it and into the table below. 'I he rock under experiment is held in a clamp a short distance in front of 140 PROCEEDINGS OF THE AMERICAN ACADEMY the instrument. The board bearing the thermograph is moved about the pin by drawing upon a cord, and is brought back to place by an opposed spiral spring. Should it not be desired that the thermograph remain continuously exposed to the radiation from the rock, it may be turned away from it by a pull upon the cord. When a reading is to be made, the cord being released, the spiral spring draws back the board, which is stopped at the proper position by a pin fixed in the table. The rock under examination is given a flat surface by grinding it upon a sheet of glass with emery. The sun's rays are directed upon it by a heliostat, the diameter of the solar beam being limited to 26 mm. by a circular diaphragm. On November 4, 1888, a slab of white marble was made the subject of experiment. The distance from the slab to the thermograph strip was 217 mm. The mean deflection obtained was 82.5 scale divisions. Had the marble slab reflected perfectly in every direction the solar rays that fell upon it, the ratio of the radiation received at the thermo- graph strip to the solar radiation would have equalled the ratio of the area of the cross section, of the solar beam employed to the area of the hemisphere of which the distance from the marble to the ther- mograph strip is the radius ; or, 82.5 7rl32 Solar Radiation o n 2172 From which we find, Solar Radiation = 45980 scale divisions, upon the supposition of perfect reflection by the marble. The thermograph was next placed in the direct solar beam, with a resistance in the galvanometer circuit, and the true solar radiation was found to be measured by 84170 scale divisions of deflection. Hence, of the solar rays falling upon it, the marble slab reflected part, or 54.6%. In the same manner, it is found that a surface of black slate reflects 3>S% of the solar rays. We learn, then, that of the solar rays falling upon rocks a large portion is absorbed and conducted through the mass of the rock, the remaining portion being reflected. In both of the cases given, the sunlight was flashed upon the rock when the reading was to be made, the rock remaining, practically, at the temperature of the room. It appears, therefore, that the solar rays are about equally divided into two portions, one of which is reflected directly, the other absorbed, conducted through the mass of the rock, and radiated in long waves. If the rocks were in large masses, and continuously acted upon by the OF ARTS AND SCIENCES. 141 solar rays, their temperature would be considerably raised by the ab- sorbed heat. The radiation of a body like the moon must consist, in considerable part, of emanations from such a heated surface ; and it becomes important to inquire whether our atmosphere is permeable by such rays. Lord Rosse found, at the time of total lunar eclipse, that with tl;e disappearance of the last ray of light from the vanishing moon radia- tion, to which his thermopile was sensitive, vanished also. On the night of January 28, 1888, the first systematic observations were made by the writer and his assistants with the previously described apparatus. The moon rose eclipsed. A reduction of the observations shows that 19 minutes before totality the deflection was 11.2 divisions. o (t tt (( it a u n o (t During first minute of totality " " 3.2 " Mean of 30 readings taken during total phase 2.09 " After the total phase had passed, but while the moon was still in the penumbra, .254.4 was obtained as the mean of 20 readings. No attempt was made to observe continuously. The evening was so intensely cold, that one could not stand quietly in the open air for any length of time without freezing. The inference to be drawn from these observations is, that all but a minute portion of the rays from the lunar soil and rock are cut off by our atmosphere, for it is impos- sible to conceive that a surface like that of the moon, upon which the sun has been shining continuously for many days, should suddenly cease to radiate upon withdrawal from the sunshine. It is very questionable, then, if at any time we receive any considerable portion of the radiation from the lunar rocks. The results given above are in substantial agreement with those obtained by Dr. Boedicker during the same eclipse. He employed a thermopile, and condensed the lunar rays with the three-foot speculum of Lord Rosse. He says,* that, twenty minutes before totality com- menced, the heat was reduced to less than five per cent of what it waa before first contact with the penumbra. He also observes, that the heal radiated by the moon commences to diminish long before first contact ; and that the heat, after last contact with the penumbra, did not mount immediately to what it had been before first contact with penumbra. It was intended, upon the occasion of the total lunar eclipse of July, * Nature, March 8, 1888. 142 PROCEEDINGS OF THE AMERICAN ACADEMY 1888, to make as complete an investigation as possible of these and allied matters. With this purpose in view, two complete sets of apparatus were prepared, and two parties of observers were in the field. Upon the night of the eclipse, however, it rained, and observa- tion was consequently impossible. If we are to conclude that our atmosphere is opaque to radiations from the lunar rocks, we must endeavor to explain the observed be- havior of the lunar rays, with reference to absorbing media, upon the hypothesis of selective reflection. We have found that 31% of the lunar rays will pass through quartz ; and if it is observed that ordi- nary rocks absorb and reflect selectively, taking up the short waves, and reflecting the long, the absorption of the lunar rays may be as effectively explained as upon the supposition that we receive radiations from the lunar rocks. We have arranged to reflect the solar rays from rocks, and, by placing in the path of the reflected ray the same quartz plate that was used in the lunar observations, have ascertained the amount of absorp- tion. The results are shown in tabular form below. .. . . Mean Deflection Mean Deflection Per Cent Material. without Quartz. through Quartz, transmitted. Red Lava, Porous .... 153 112 73 Quartz 131 116 88 Black Lava 82 65 80 White Marble 180 147 82 Slate 103 77.8 79 Direct rays of sun transmitted .... .... 93 The results show that selective absorption takes place, but to an extent quite limited, and altogether insufficient to explain the great absorption of the lunar rays. When we consider the great differences in character of the specimens of rocks experimented upon, as compared with the very inconsiderable differences in the transmitted rays, it seems useless to undertake to find a material that shall absorb so large a proportion of the short solar waves that only one third of the re- flected rays will pass through the quartz plate. The question is how to reconcile the results here obtained with the eclipse observations, showing that our atmosphere is nearly opaque to radiations from the lunar rocks. The materials for the solution of this problem do not seem to be at hand. It is, of course, possible that the materials of the moon's surface may absorb selectively to a much greater extent than those that we have examined. On the other hand, if the lunar surface were of very light and porous materials, OP ARTS AND SCIENCES. 143 like our volcanic pumice rocks, a withdrawal of the solar rays might be attended by so sudden a fall of temperature as to explain the eclipse observations. Somewhere between the two the explanation probably lies : but at present we can do little better than conjecture. Atmospheric Transmission Curve. An attempt has been made to construct a curve which would show the transmission of the atmosphere for lunar rays at every altitude of the moon. Observations for this purpose have been made, at every opportunity, for nearly a year, and already amount to some thousands in number. It has been customary to begin the observations at moon- rise, or, if the moon were already in the sky, as soon as the evening temperature had become sufficiently stationary, and to continue them until culmination. The working of the apparatus is attended with considerable fatigue, and it is not possible for one person to operate it uninterruptedly. Tbe readings, therefore, are made in sets of ten or twenty with a short rest between the sets. Sometimes a third person has measured the altitudes with a portable transit, while two gave their attention to making the readings ; but usually the same person has directed the thermograph-box and taken altitudes at .the beginning and the end of each set, the mean reading of each set being regarded as the deflection corresponding to the mean altitude. Below is given the work of the night of February 28, 1888. Con- siderable difficulty has been experienced in obtaining the deflections for the high altitudes, as it very frequently happens that, late in the even- ing, clouds arise from the ocean near at hand and obscure the sky. On this particular evening the sky was very serene and beautiful until 10 h. 40 m., when the clouds arose. Because of this unusual seren- ity, this series of observations shows more than ordinary regularity, although less than the customary number of observations was made to a set. 144 PROCEEDINGS OF THE AMERICAN ACADEMY February 28, 1888. Barometer 30.35. Thermometer — 13° C. j Altitude. Time p. m. Deflection. Altitude. Time p. m. Deflection. O ' h. m. o » h. m. 3 10 7 24 67.2 20 0 9 5 174.3 7 30 7 51 128.6 20 30 9 8 177.5 8 0 7 53 129.4 23 10 9 24 183.1 8 30 7 56 134.5 23 30 9 27 185.3 11 0 8 13 146.6 24 0 9 31 187.1 11 30 8 15 147.5 24 30 9 33 184.1 12 0 8 19 149.0 25 0 9 36 188.1 12 30 8 22 152.2 25 30 9 40 188.3 15 0 8 34 158.3 26 0 9 44 189.0 15 30 8 37 160.3 28 10 9 56 191.0 16 0 8 41 161.6 28 30 9 58 192.0 16 30 8 44 165.1 29 0 10 2 193.4 19 0 8 59 168.1 33 40 10 31 202.1 19 30 9 2 172.3 To illustrate the effect of the weather upon such ohservations as these, we may compare with the above the following table, made up from the results of October 21, 1888. On the former occasion the air was very calm, and from its low temperature ( — 13° C), must have been quite dry. The evening of the latter date was fine, after many days of fog and rain, and, although clear to the eye save for the merest visible milkiness, the drifting clouds of vapor were made manifest by the irregular transmission of the lunar rays. October 21, 1888. Altitudes Deflections. Altitudes. Deflections O ' 6 45 105.1 20 15 182.7 11 45 146.1 21 0 175.7 12 15 149.1 22 45 178.7 15 45 163.3 29 45 187.8 17 0 159.1 31 0 191.8 Following Langley * we may find the approximate transmission coefficient for a column of air capable of supporting one decimeter of mercury, by employing the formula t = (M2/?2 - M^) rf, * American Journal of Science, vol. cxxv. p. 176. OF ARTS AND SCIENCES. 145 The dates upon which this has been determined, together with the principal quantities entering into the computation, are here given in tabular form. Table of Transmission Coefficients. Date. 1888. Altitude (1). Altitude (2). d2. dv ft. ft. M2/3j — MjjS^ t. O ' o ' Feb. 28 12 0 33 40 149.0 202.1 7.696 7.676 22.47 0.9866 28 15 0 29 0 158.3 193.4 7.696 7.696 13.52 0.9852 March 29 14 54 30 25 112.2 143.4 7.645 7.640 14.42 0.9832 Oct. 18 22 30 41 0 174.5 222.3 7.670 7.070 7.82 0.9708 The mean of the values of t is 0.9852, and t 7.6, the amount of lunar radiation transmitted by the entire atmosphere at the ordinary pressure, is 0.8925. Summary. I. We have shown how an instrument may be constructed, capable of measuring very minute radiations. II. We have measured the radiations of several rocks at near 100°, and presented the results in a table. III. We have found that the heat which our planet receives from the moon is to that from the sun as 1 to 184,560. IV. We have compared the lunar rays with solar rays reflected from rocks, with reference to the absorption of each by quartz. V. We have constructed a curve, representing the change of trans- mission of lunar rays by our atmosphere with changes in altitude of the moon. VI. We have found that our atmosphere, at the ordinary pressure, transmits 89.25% of the vertical lunar beam. VOL. XXIV. (N. S. XVI.) 10 146 PEOCEEDINGS OP THE AMERICAN ACADEMY XIII. ON THE CHARGING OF CONDENSERS BY GALVANIC BATTERIES. ' By B. O. Peirce and R. W. Willson. Presented March 13, 1889. I. The Use of Water Cells. The different methods which are commonly used for comparing the capacities of condensers often lead to widely different results. Several condensers may be apparently of the same capacity when tested by one process, while each differs from all the others under a second set of conditions. Every condenser has its own character- istics, and these must be specially studied before it can be used in accurate work. The present investigation grew out of the discordant results which one of us obtained in attempting to compare condensers made in dif- ferent ways. Our experiments have removed some of our own diffi- culties, and we think that an account of our work may prove useful to others. We shall begin by considering the behavior of different batteries when they are suddenly called on to furnish definite quantities of elec- tricity in definite short times, and in this first paper we shall give some results which we have obtained in using water cells. These results are interesting, because the water battery possesses in an exaggerated degree some properties which are common to all bat- teries, and which may seriously affect* the quantity of electricity fur- nished to a large condenser by a cell with which it is connected for a short time only. The cells that we used were made of ordinary " 2^ ounce wide mouth flint glass bottles," filled to the neck with faucet water, and containing each a strip of zinc and a strip of copper placed vertical and nearly par- allel to each other, at a distance apart of about two centimeters. The * Von Beetz, Wied. Ann., xxvi. p. 24, 1885. OF ARTS AND SCIENCES. 147 cylindrical part of each bottle under the neck was about six centimeters high, and four centimeters in diameter, and each strip of metal was of such a size as to expose a surface of seven square centimeters on each of its sides to the liquid. The resistance of each cell as measured by the use of alternating currents* was nearly 1200 ohms. Of a large number of such cells at our disposal, we found 240 sufficient for our purpose, and a switch-board enabled us to arrange these easily in various com- binations of groups of twenty cells each. The condensers which we used in this part of our work were nine in number, including one of a capacity of one microfarad subdi- vided into fractional parts. This condenser, which was made by Messrs. Elliott Brothers and marked by them No. 72, we took as a standard. As we shall show when we come to discuss the characteristics of different condensers, the ratios of the capacities of the other condensers to the capacity of this one varied somewhat with the time of charging, but, when this remained constant, were the same, whatever the kind of battery used. The capacity of each of the condensers for each time of charging was measured in terms of the capacity which No. 72 has when charged for one second by a battery of small internal resistance. The capaci- ties of five of the other condensers, as determined in the manner just described, did not vary on the average by more than two per cent when the time of charge was decreased from 2.0 seconds to 0.01 second, that is, in the ratio of 200 to 1. By combining the different condensers, we were able to get within one twentieth of a microfarad any capacity from 0 to 11 mf., a range which was amply sufficient for our purposes. Most of our work on water cells was done with the help of a four- coil mirror galvanometer (A), of 3300 ohms' resistance. For some pur- poses, however, only one of the coils was used. The period of the complete swing of the galvanometer needles was 27 seconds, and the ratio of two successive swings 1.058. Unlike some of our other gal- vanometers, this one, when used ballistically, within the limits which we set for our experiments, gave throws which seemed to be func- tions only of the quantity of eleetricityf discharged through it. that is, independent of the tension of this electricity at the instant of dis- charge. A minute coil of wire, placed in the core of one of the * F. Kohlrausch, Wied. Ann., xi. p. 663, 1 t See Lord Rayleigh, Phil. Trans., I't. 2, p. Gl!», 18S2. 148 PROCEEDINGS OF THE AMERICAN ACADEMY galvanometer coils, through which by means of a double key the current from a small thermopile could be sent in either direction, served to damp the oscillations of the needle after a throw had been given. A few of our measurements were made with the help of another four-coil galvanometer (B), of 3000 ohms' resistance. The period of a complete swing of its needle was 52.7 seconds, and the ratio of succes- sive swings 1.068. With scale placed at a distance of one meter from the mirror, one microcoulomb when discharged through this galva- nometer gave a throw of 45 mm. For intervals between 0.01 sec. and 0.5 sec, the apparatus shown in Figure 1 was used. It consists of a pendulum with an iron bob, A, eight inches long, two inches in diameter, and weighing 7 lb., and a brass rod ^ inch in diameter weighing 2.8 lb. The axis of suspen- sion is formed by a brass rod 2^ inches long held between pointed screws. Upon this axis and concentric with it are placed two ebonite disks, F, G inches in diameter and | inch thick. The face of each of these disks is armored through about half of its circumference with a strip of German silver ■£% inch in thickness, held by rivets passing through the disk, and the edge of the armature is turned true with the edge of the disk. The disks are placed with their armored faces adjacent, but separated by an ebonite washer 5 inches in diameter and ^V inch in thickness. One of the disks is fixed to the pendulum rod, while the other can be revolved about their common axis so that the two German silver strips may overlap to any desired extent ; the arc a, attached to the movable disk, serves to clamp the two disks firmly together, and also to deter- mine approximately the amount of the overlapping. To each of the German silver strips is joined a wire, b, which dips in a mercury cup, g, connected with one of the two points between which the circuit is to be made ; to avoid as far as possible any interference with the motion of the pendulum, these mercury cups are placed very close to the axis of suspension. The pointed screws upon which the pendulum swings are held in a frame, c c, of wrought iron, which is itself swung between two pointed screws, d d, perpendicular to the axis of suspension of the pendulum. By rotation of the frame c c upon these screws, the axis of the pen- dulum is easily levelled. To the frame c c is attached a pillar, e, carrying a copper wire, / 5% of an inch in diameter, in such a position that its end runs with OF ARTS AND SCIENCES. 149 Fig. 1. 150 PROCEEDINGS OF THE AMERICAN ACADEMY' light friction in the narrow groove between the two disks as the pen- dulum swings ; both the end of the wire and the sharp edges of the disks are somewhat rounded to prevent undue wear. If the two disks are clamped together in a position such that the unarmored part of one is opposite the armored part of the other, and that as the pendulum swings the wire leaves one German silver strip just as it reaches the other, it will be in contact with each armature successively, but will establish metallic contact betweeu them and close the circuit between the mercury cups at most for a very short interval ; if, however, the armatures overlap for a certain number of degrees, contact will be maintained while the pendulum swings through just that number of degrees of its arc. The front disk, which is rigidly fixed to the pen- dulum rod, is so placed that it comes in contact with the copper wire just as the pendulum reaches its lowest point. If therefore the arma- tures overlap, for instance, 10°, and if the pendulum is urawn out to a known point upon one side of its arc so that the copper wire rests upon the unarmored side of the " fixed " disk, then, when the pendu- lum is allowed to fall, metallic connection will exist between the disks while it is rising through 10° from its lowest point. From this "arc of contact" the time of contact is easily determined. The time of vibration of the pendulum is 1.181 sec, and the arc of initial displacement 28° 56'; the decrease of arc in one complete vibration is about 30'. The length of the arc of contact may easily be determined within one minute. This uncertainty may give rise to an error in the com- puted time varying from 0.00022 sec. for an arc of 1°, to 0.00042 sec. for an arc of 25°. The errors arising from a wrongly assumed value of the initial displacement, and from decrease of arc, are in no case greater than one fourth of one per cent of the computed time, and are here neglected. Since the copper wire does not touch each of the armatures in a single point, the arc of contact will obviously not be exactly equal to the angle of overlap, but its value may be easily determined by direct observation. By throwing the switch at H to the right, the circuit through the bell and battery, J, is made complete, except for the break at the disks. The pendulum is then lowered, and the readings on the divided arc E of the microscope K are noted when the bell begins and stops ringing, as the pendulum is moved through its ascending arc ; the former must nearly correspond with the reading when the pendulum is in its position of rest. To facilitate OF ARTS AND SCIENCE- 151 I this latter adjustment the wire / is made movable in the direction of its length. For releasing the pendulum and catching it at the end of its spr the contrivance shown at D is used. The latch h is firmlv fastened to the spring i, which serves the double purpose of giving the up- ward force upon the latch-bar to cause it to ensa^e with the catch upou the pendulum bob, and also of lessening the shock produced upon the whole apparatus by the arrest oi the pendulum. The sprint i is fixed inside the tube k, which, sliding inside the sleeve /, serves as guide and stop for the motion of the latch. To operate the mech- anism, the tube k is drawn out by the cord attached, and the pen- dulum drawn with it by the latch ; at a certain point, however, the pin m, which passes through the latch, is brought against the wed^e n, and a slight further motion trips the latch, and the pendulum is released. The point at which the pendulum is released is so adjusted, by sliding the wedge >t. that the arc through which the bob is lifted - slightly greater than the loss of the arc through friction, etc. in a complete vibration. The latch is drawn up by a cord passing around an axis. L. which is turned by a lever and cord pulled by the observer at the galvanometer. This is to insure that the pendulum is dropped from nearly the same height at each observation, the multiplying arrangement serving to decrease the velocity with which the peudu- lum is raised, so that it rises an exceedingly small distance beyond the point where the latch is tripped. As soon as the pendulum tails, the latch, being at once released by the observer, is drawn back to its lowest position by a spring, not shown in the figure, and the pendulum returning is caught by the latch, and thus, having made a complete swing, is left in its original position ready for the next observation. Attached to the frame in which the pendulum swings is a balanced rocking kev. /'. with two adjustable screws making contact in mercury cups. When the pendulum hang- by the latch, the key r- sts in contact with the left-hand mercury cup q. through the k fi-hand bo but as the pendulum completes its half-vibration, the pin .«. attached to the " fixed " ebonite disk for this purpose, throws the lever over upon the right-hand contact, r. where it remains during the second half-vibration of the pendulum, being replaced in its original position by the pin t, as the pendulum is caught by the latch. The cycle of operations performed by the pendulum is explained bv the diagram below, which shows the connections as made for the three different kinds of observation : — 152 PROCEEDINGS OF THE AMERICAN ACADEMY (1.) Charge of the condenser for a short measurable interval followed by discharge through the galvanometer, the discharge occurring about 0.6 sec. after the commencement of the charge, and the contact between condenser and galvanometer lasting abuut 1.2 sec. (2.) Charge of the condenser through the galvanometer for a short measurable interval; discharge (not measured) about 1.8 sec. after commeucement of charge, the condenser remaining short-circuited 1.2 sec. This is the arrangement shown in Fig. 1. (3.) Current flowing directly through the galvanometer for a short measurable interval of time. The switch H is always turned to the left except when the arc of contact is to be measured as before described. For all the observations on condensers referred to in this paper, the first figure is applicable ; the action is then as follows. When the pendulum rests in the latch, one terminal of the con- denser, C, attached to the binding screw 3, is in connection, through the rocking key, with the mercury cup, q, and therefore with one pole of the battery, B, at 4. When the pendulum is released, contact is made between the disks during a certain arc of swing, and the current then flows from the binding screw 5, through the disks and switch H, to the other terminal of the condenser at 2. On the pendulum's arriving at the end of its swing, the key is shifted from contact with 4 to contact with 1, causing the condenser to be discharged through the galvanometer ; returning, the pendulum returns the rocking key to its initial position, ready for the next observation. It may be noted that the battery is permanently con- nected with one pole of the condenser except during the return swing OF ARTS AND SCIENCES. 153 of the pendulum, but we have found no trouble from leakage in these experiments. The action in cases (2) and (3) will be sufficiently evident from the above description. The weight of the pendulum rod being considerable, we found that it was somewhat bent by its own weight when the pendulum bob was supported by the latch, and when released a vibration was set up in the rod on its own account, which caused a rapid vibration of the disks in addition to the motion due to the pendulum. The result of this was to produce an uncertainty in the beginning and end of con- tact, depending upon the relative phase of the two vibrations at the beginning and end of the arc of contact ; the amount of this uncer- tainty was less than 0.0005 sec, and was greatly lessened by adding steel wire stays to the rod when it became desirable to use the pen- dulum for times approaching 0.001 sec. in magnitude. A similar effect, probably attributable to the same cause, was noticed as producing a considerable error in a much larger pendulum of similar construction, when used for times approaching 0.001 sec, although the rod was of wood 1£ inches square in section, the bob weighing 40 lb. and the time of swing being 1.8 sec, with an initial displacement of 26°. We have used a more simple apparatus, shown in Fig. 3, in cases where it was desired to charge a condenser for a definite interval of time, the absolute value of which is required to be known with a higher degree of accuracy. With the pendulum already described, the time is liable to considerable error when determined by an arc of contact nearly equal to the half arc of swing ; that is, when the time of contact is in the neighborhood of 0.5 sec. Where different times are not to be experimented upon, a greater degree of accuracy may be attained if the contact existing through the upward swing be maintained through the downward swing as well, beginning and ceasing nearly at the lowest point of the swing. The time of contact is then equal to the time of vibration, affected by a very small correction, which depends upon the departure of the beginning and end of contact from the lowest point, and which may be determined with considerable accuracy. The pendulum bob is of iron, and is held displaced from its position of rest by one pole of a horseshoe magnet b, in contact with it at its middle point; this magnet is attached to the plate c, which turns on the screw d, so that the magnet maybe moved in the plane of vi- bration of the pendulum by a cord leading to the observer al the galvanometer. The pin e acts as a stop limiting this motion of the 154 PROCEEDINGS OF THE AMERICAN ACADEMY Fig. 3. magnet towards the left. If the magnet is pulled out a certain distance toward the right, the pendulum bob is brought against the stop /, and any further motion of the magnet detaches the pendulum ; the magnet is at once released by the observer, and falls back to a point fixed by the stop e, so as to arrest the pendulum at the completion of its first swing. The pendulum rod is screwed into the edge of an eb- onite disk, g, three eighths of an inch thick and one inch in diameter, through the centre of which passes the pin h, which forms the axis of suspension. Attached to the disk g are two copper strips, j, of which one is shown in the figure, and which, as the pendulum swings, rub lightly upon the edge of the fixed disk k. Inserted in the latter are four pieces of copper m, n. In the ordinary position of the pendulum as shown in the figure, the copper strips j j, which are connected with the condenser by the binding screws at p, rest upon the opposite copper pieces m ?», and through them are in circuit with the binding screws at q, which are connected with the galvanometer. The condenser is thus short circuited through the latter. When the pendulum swings, the strips ^y make contact at the lowest point of the swing with n n, which are connected through the binding screws at r with the battery ; and this connection is maintained until the pendulum reaches its lowest point on the return swing, when the strips j j pass to the copper pieces, and the condenser is discharged OF ARTS AND SCIENCES. 155 through the galvanometer. It is hardly necessary to say, that the width between the pieces m and n is made slightly greater than the width of j, to prevent a direct current from the battery through the galvanometer. The method above described has been found very satisfactory for the purpose of obtaining a single swing of a not too heavy pendulum; it is essential that the stop e should be somewhat elastic ; a short piece of soft rubber tubing slipped over the pin answers well. The upper pole of the magnet is brought quite near the upper part of the pendulum bob to strengthen the induction. The motion of the magnet is so slight, that its direct effect upon the galvanometer is negligible. No great care is necessary in the release, as, even if the bob is brought up against the stop f, so as to rebound, the time of describing the second and third quarters of the complete vibration is altered by an inappreciable amount. With the apparatus described a great many measurements were made, and these all gave concordant results. The following tables give, in microcoulombs, the charges which variously arranged batteries of water cells gave, in the times named, to condensers of different capacities. Each number in the body of a table is the mean of a set of closely agreeing observations. In the cases of many of the com- binations of cells we have used a much greater number of different capacities than is indicated in the tables, but the results given below are representative. Whereas in studying certain other cells we have found it desirable to use times shorter than the ten-thousandth of a second, it is evident, from the results in Table L, that in the present instance it was not worth while to use charging times smaller than the hundredth of a second. 156 PROCEEDINGS OF THE AMERICAN ACADEMY TABLE I. Quantity of Electricity delivered in 0.01 seconds by different Batteries of Water-cells to Condensers of various Capacities. Battery. 0.1 Capacities of Condensers 03 0.5 1.0 in Microfarads. 1.87 3.06 9.58 mc. mc. mc. mc. mc. mc. mc. 20 cells in series .... ■1 parallel 20's .... 8 parallel 20's .... 12 parallel 20's .... 0.9 1.6 1.7 1.0 3.5 4.2 1.0 3.1 4.6 5.8 1.1 3.4 5.8 7.9 6.8 9.1 3.8 6.8 9.7 1.1 4.0 7.9 10.8 6 parallel 40's .... 2.6 4.6 5.2 5.3 5.5 5.5 5.8 60 cells in series .... 4 parallel 00's .... 1.1 1.2 3.6 3.5 1.3 3.8 4.1 4.4 1.8 4.4 3 parallel 80's .... 3.0 .... 3.3 o.o 3.6 2 parallel 120's .... 2.4 26 2.7 2.8 3.2* 240 cells in series . . . 2.4 2.7 2.7 2.8 TABLE II. Quantity of Electricity delivered in 0.19 seconds by different Batteries of Water-cells to Condensers of various Capacities. Battery. Capacities of Condensers in Microfarads. 0.5 1.0 1.87 3.06 C.82 10.70 20 cells in series . . 3 parallel 20's . . 12 parallel 20's . . mc. 5.4 7.2 8.2 mc. 7.3 12.3 15.9 mc. 8.7 17.1 28.7 mc. 8.9 20.1 42.7 mc. 9.6 23.8 69.6 mc 9.0 25.3 82.5 40 cells in series . . 6 parallel 40's . .' 7.1 14.2 8.4 25.5 8.8 37.1 9.6 44.1 53.6 9.8 55.9 00 cells in series . . 4 parallel 60's . . 7.0 18.5 89 26.6 9.1 31.0 9.0 35.7 38.5 9.6 40.1 3 parallel 80's . . 18.7 24.6 26.7 29.7 30.3 31.0 2 parallel 120's . . 17.3 19.0 20.1 20.7 21.5 240 cells in series 10.9 11.2 11.3 11.3 11.8 OF ARTS AND SCIENCES. 157 TABLE in. Quantity of Electricity delivered in 0.37 seconds by different Batteries of Water-cells to Condensers of various Capacities. Capacities of Conden sers in Microfarads. Battery. 0.5 1.0 1.138 3.07 6.86 10.85 mc. mc. mc. mc. mc. mc. 20 cells in series . . 7.1 10.9 13.0 15.1 17.4 17.4 2 parallel 20's . . 8.0 140 20.6 26.0 31.8 33.9 3 parallel 20's . . 8.1 146 24.1 31.7 42.3 46.8 4 parallel 20's . . 8.1 15.5 • . • • 38.0 55.6 64.5 6 parallel 20's . . 8.6 16.6 .... 43.6 70.5 83.0 8 parallel 20's . . 9.0 16.7 30.3 46.8 80.4 98.9 12 parallel 20's . . 17.0 31.7 50.3 94.8 119.3 40 cells in series . . 10.8 13.3 16.4 17 5 18.9 20.0 2 parallel 40's . . 14.6 22.4 29.2 32 9 37.0 39.2 3 parallel 40's . . 15.0 25.1 36.2 43 2 50.3 62.6 4 parallel 40's . . 16.4 28 1 42.4 52.1 66.7 71.0 5 parallel 40's .... 29.6 46.4 60.3 78.2 85.5 6 parallel 40's . . 16.6 31.6 51.5 68.2 91.3 100.2 60 cells in series . . 12.0 14 9 19.2 2 parallel 60's . . 18.5 26.2 • ■ * • ■ • > • • . . . 38.4 3 parallel 60's . . 20.8 32.9 • . . • 49.3 54.4 57.5 4 parallel 60's . . 22.8 38.3 52.9 63.2 73.0 77.0 80 cells in series . . 14.1 16.6 18.7 19.8 20.0 20.7 2 parallel 80's . . 22.1 29.0 33.9 3i-,.2 38.9 39.5 3 parallel 80's . . 26.1 39.1 47.4 53.5 ,>.i; 62.1 120 cells in series . 16.4 17.8 19.1 20.2 20.4 20.7 2 parallel 120's . . 26.2 33.6 37.3 38.8 41.0 42.4 240 cells in series . 18.9 20.2 21.9 21.7 158 PROCEEDINGS OF THE AMERICAN ACADEMY TABLE IV. Quantity of Electricity delivered in 0.93 seconds by different Batteries of Water-cells to Condensers of various Capacities. Battery. 0.5 Capacities of Condensers iu Microfarads. 1.0 1 89 3.11 7 18 11.41 mc. mc. mc. mc. mc. mc. 20 cells in series 8 parallel 20's . . 0 parallel 20's . . 12 parallel 20's . . 7.2 73 7.6 13.0 14.2 16. i 19.2 24.6 38.6 46.3 51.0 29 6 61.8 89 7 103.9 32 2 72.8 40 cells in series . . 6 parallel 40's . . 14.4 16.0 21.5 81.1 26.2 56.8 28 9 84.6 32.9 80 cells in series . . 3 parallel 80's . . 210 29.7 27.6 50.7 32.9 717 35 1 85.3 36.5 37.0 120 cells in series 2 parallel 120's . . 24.3 35.(3 30.0 61.1 33.5 61.9 34.1 68.2 72.3 36.3 74.1 240 cells in series 31.6 34.9 37.2 37.9 39.0 TABLE V. Quantity of Electricity delivered in 2.0 seconds by different Batteries of Water-Cells to Condensers of various Capacities. Battery. Capacities of Condensers in Microfarads. 0.5 1.0 1.89 3.11 7.19 11.74 mc. mc. mc mc. mc. mc. 20 cells in series . . 7.3 14.4 24.9 35.1 52.9 57.7 2 parallel 20's . . .... 14.3 26.8 42.3 75.5 93.8 4 parallel 20's . . 15.2 48.8 96.1 40 cells in series . . 14.8 26.2 40.0 50.1 59.3 64.1 2 parallel 40's . . .... 30.1 514 72.6 4 parallel 40's . . . 31.0 567 87.6 60 cells in series . . 20 0 33.1 53.6 62.3 65.0 3 parallel 00's . ■ . 44.5 77.1 80 cells in series . 25 8 40.8 53.6 59.8 68.5 69.8 2 parallel 80's . . 28 5 53.0 78.7 97.4 3 parallel 80's . . 30.4 58.2 94.2 120 cells in series 33.8 474 57.8 63.9 71.9 75.6 2 parallel 120's . . 73.5 100.0 240 cells in series 49.8 63.6 71.0 78.0 83.8 OP ARTS AND SCIENCES. 159 The results given in Tables II., III., IV., and V. have been used in plotting the subjoined curves. In each curve the ordinates rep- resent the charges on a scale of 10 microcoulombs to a division, and the abscissas represent the capacities of the charged condensers in microfarads. Attached to each curve is a number (m), and at the upper left-hand corner of the square in which the curve is drawn is another number («). These denote that a battery made up of m parallel groups, each consisting of n cells in series, was used in obtaining the results from which the curve has been plotted. Fig. 4. J ■ ■ ' h ) a y / j^ / h / / 3 — / / / '' *—. : / 1 1 1 ' , Y st i: £ 2V I 1 ^ t ■ f : > . — Time of charge, 0.19 sec. Unit of abscissas, 1 raf. Unit of ordinates, 10 mc. Fig 5. -'. i :.,, ■„ ',. 1 ■ ^r 6C ' i A' . >< t / • ■ >, - -' ', / ■. A t _i i / ^ i I A ; ■ ' l / £ £ i ! V . / 1 k i I — \ si ]• p r 0 l / : i t— — - * - — 7 '- 1 p - i I - ( ' , _ Time of charge, 0.37 sec. Unit of abscissas, 1 mf. Unit of ordinates, 10 mc. 160 PROCEEDINGS OF THE AMERICAN ACADEMY Fig. G. .' * ♦1 It / * ' V / 3 1 / / , 1 >, 1 / (. / y 1 1 ' i 1 1 1 r / § ' / 1 , A 1 ' n 9 2. 0 2 ' -1 1 " ' , Time of charge, 0.93 sec. Unit of abcissas, 1 mf. Unit of ordinates, 10 ma Fig. 7. :t K < -40 i 1 / u- 4 S s 1 / J / J- 4 -~ • ' / , • / r~ , '4 ■ - 1 ■ t / »i 1 { !Z "1 ti i f /■ (» j [/ 1 _j_ \ • x / / / t , / 1 / 1 / 1 Time of charge, 2 sec. Unit of abscissas, 1 mf. Unit of ordinates, 10 mc. It will be noticed that all the curves in all those squares which have any one number in their upper left-hand corners, have the same slope at the origin. This slope is numerically equal to one tenth* of the electromotive force in volts of the charging batteries, as computed from measurements of such cells in open circuit made with a Quadrant Electrometer. * Each vertical unit corresponds to ten microcoulombs. ' OF ARTS AND SCIENCES. 161 So far as we can judge from our observations with limited ca- pacities, each curve has as an asymptote a line parallel to the axis of a?, and at a distance from it which represents the quantity of elec- tricity which the charging battery would yield if joined up for the time given in simple circuit with a trifling outside resistance. Direct experiment shows that this quantity is almost exactly proportional to the number of cells joined up parallel to each other. The general effect of interposing a large resistance wound bifilar between the battery and the condenser which it is charging is shown by the following diagram, in which the curves are drawn in the same way as in Figures 4, 5, 6, and 7. The two upper curves represent observations taken with a battery of twelve parallel groups of 20 water cells each, first with no interposed resistance and then with Fig. 8. 247,000 ohms inserted. The two lower curves represent similar observations made with a single group of 20 cells joined up in series. For purposes of comparison with the numbers in Tables I., II., III., IV., and V., we give some results obtained with a battery consisting of 20 water cells arranged in series. The poles of this battery were connected together, through various outside resistances, for given short intervals of time, and the quantities of electricity which traversed the circuit during these intervals were measured. The three curves of Fig. 9 were plotted by using as abscissas the times * during which the battery circuit was closed, and as ordinatea the quantities of electricity which passed through the circuit in these times. The observations represented by points in the upper curve were made when the resistance in the circuit outside the battery was 3,000 ohms. The corresponding resistances for the Other two curves were 102,000 ohms and 250,000 ohms respectively. It will be * Each vertical unit corresponds to 1 microcoulomb. Each horizontal unit corresponds to 0.01 sec. vol. xxiv. (n. s. xvi.; 11 162 PROCEEDINGS OF THE AMERICAN ACADEMY noticed that the curvature near the origin is considerable, but that after about one tenth of a second each line becomes nearly, though not quite, straight. If the internal resistance of the battery is assumed to be 24,000 ohms, the effective electromotive forces in the circuit after one tenth of a second are about 1.2 volts, 4.5 volts, and 7.4 volts, respectively. The electromotive force of the open battery was a little over 16 volts. 0.1 sec. 0.2 sec. 0.3 sec. Fig. 9. The results in Table VI. were obtained with another battery of 20 water cells which had been resting for one month. The numbers in the body of the table give in microcoulombs the quantity of elec- tricity which passes through the circuit when the poles of the battery were connected for the times named through various external re- sistances. TABLE VI. Duration of Current. Resistance of Outside Circuit in Ohms. 3,000 102,000 250,000 sec. mc. mc. mc. .0025 0.34 0.21 0.12 .011 0.94 0.59 0.41 .034 2.50 1.73 1.22 .077 4.94 3.59 2.52 .1033 6.43 4.64 3.34 After the poles of a battery of these water cells joined up in series have been connected together for a short interval only (say for one OP ARTS AND SCIENCES. 163 second or less), the battery seems to regain almost instantly its origi- nal electromotive force. Indeed, it is evident from the numbers given in Tables L, II., III., IV., and V., that the polarization — which, as is well known, increases and diminishes in the case of any given simple element with the intensity of the currents which pass through the cell — must almost instantly respond to any decrease in the density of the current. Of course, if a battery of water cells is short-circuited for a number of seconds or minutes, the polarization slowly increases, and the battery becomes " tired," and after the circuit is broken it must be allowed to rest for a number of minutes, or even hours, before it gets back its lost power. From the fact that the lines in Fig. 9 are not straight, it appears that the sudden falling off in the electromotive force of the cells when the circuit is closed is not wholly due to a polarization, which is at every instant simply proportional to the density of the current then flowing. AVe shall not discuss further the subject of polarization in water cells until we have published the results of some observations made with other kinds of battery. Jefferson Physical Laboratory, Cambridge. 1G4 PROCEEDINGS OP THE AMERICAN ACADEMY XIV. CLASSIFICATION OF THE ATOMIC WEIGHTS IX TWO ASCENDING SERIES, CORRESPONDING TO THE GROUPS OF ARTIADS AND PERISSADS. By W. R. Livermore, Major of Engineers, U. S. Army. Presented by the Corresponding Secretary, April 10, 1889. If the atomic weights of all chemical elements are arranged in a single ascending series, it will take the following form if expressed in whole numbers : 1,-7, 9, 11, 12, 14, 16, 19,-23, 24, 27, 28, 31,32, 35,-39, 40, 44, 48, 51, 52, 55, 56, 59, etc. ; corresponding to the elements, H, — Li, Be, B, C, N, O, F, — Na, Mg, Al, Si, P, S, CI, — K, Ca, Sc, Ti, V, Cr, Mn, Fe, Co, etc. The well known " Law of Octaves " calls attention to the fact that each element bears a strong resemblance to that seven places from it in this series, and the " Periodic Law " states that the properties of elements stand in periodic relation to their atomic weights. These laws have been enunciated and illustrated by Newlands, Mendeleeff, Lothar Meyer, and others, and are now familiar to all students of chemistry. Referring to these laws, Wurtz in his "Atomic Theory " says : " Though it may be generally true that the properties of bodies are subject to periodic modifications with the increase of their atomic weights, the law of these modifications escapes our observation, and seems to be of a complicated nature ; for, on the one hand, the atomic weights of successive elements vary within considerable limits without displaying any regularity in these variations ; on the other hand, we must confess that the gradations of properties, in other words the greater or less divergencies between properties of successive elements, do not appear to depend upon the degree of the differences between the atomic weights. These are real difficulties."* * The Atomic Theory, 1881, p. 162. OF ARTS AND SCIENCES. 1G5 Lothar Meyer on the same general subject says, " There cau be no doubt as to the fact that these differences are subject to law";* and, " There is still much work for the hands and mind ; but it will be thoroughly rewarded. The prize is a systematic inorganic chemistry which will bear comparison with the thoroughly developed system of organic chemistry." f The object of this paper is to contribute to the removal of these difficulties, by showing that the increase in the atomic weights of the elements follows a law of the utmost simplicity in its general form, and identical with that of the series of organic compounds. Let us take the series above mentioned and consider whether any of its terms can be classed in a series of constant increase. Beginning with 2 as a modulus, we find that it applies to 7, 9, and 11, with no recurrence of this difference except for the terms 12, 14, 16 • 3 applies only to 9, 12, — 24,27, — 48, 51, and to 16, 19 * * 28, 31 **** * 52, 55; 4 however applies to 7, 11 * 19, 23, 27, 31, 35, 39 * * 51, 55, 59, and to 12, 16 * 24, 28, 32 * 40, 44, 48, 52, 56; thus embracing in two parallel series all the terms of the first three periods of New- lands and Mendeleeff, with the exception of 9 and 14, i. e. 22 out of 24. The probability that these numbers would so far coincide with the regular series from the result of chance, is too slight to be enter- tained. If now, in addition to this coincidence, any points of resem- blance can be discovered among several of the elements in each series, such resemblances are significant; but when it appears that all or nearly all in each series fall into a distinct group that has already been recognized as such by chemists, there is scarcely room for doubt that the regularity of the series is connected with the intrinsic nature of the elements. Those of the first series are all Perissads and those of the secm.d Artiads, or elements of uneven aud even quantivalence respectively, with the single exception in one case of scandium, a newly discovert 1 element whose atomic weight has never been so accurately determin< d as to throw it outof its group, and cobalt and nickel, which apparently belong to another group. For the present, therefore, the law of regu- lar increase in the atomic weight of the parallel series is spoken of as the Law of Artiad and Perissad Increase, or more briefly aa the Pkrissad Law. By similar methods, we find that the numbers between 70 and 100 * Modern Theories of Chemistry, English Translation, L888, p. 100. * Ibid., p. 170. 166 PROCEEDINGS OF THE AMERICAN ACADEMY fall naturally into two series, with the common difference of 5 for the perissads and perhaps 4 for the artiads. The latter series, however, is somewhat indefinite. Between ICO and 150 the perissads increase regularly, with a com- mon difference of about G|, and the artiads less regularly, with the same difference, as shown in Tables I. and II. Too little is known of the atomic weights between 150 and 190, and of those above 210, to justify their classification. Between 1 90 and 210, we find that 4 applies to 195, 199 * 207, and to 196, 200, 204, 208. All of the first series are artiads, and in the second all except 200, or II g, are recognized as perissads, and this element is so similar in many respects to Cu, Ag, and Au that for the present it is allowed to remain in its place. There only remain unclassified 9, 14, 59, 104, and 193. Of these numbers, 9 is the atomic weight of Be and ap- pears to differ too much from 8, the serial number of this element, to be recognized in its natural place. The remaining numbers, 14, 59, 104 * 193, form a series by them- selves, with a difference of a little less than 45. Ni and Co correspond to 59, Ru and Rh to 104, and Ir to 193. These elements are always classified together, and this regularity of increase has often been noticed. But perhaps 14, or N, falls into this series accidentally. In Tables I. and II. the first column shows the symbols for the ele- ments ; the second column, the serial numbers derived from the for- mula; the third column, the observed atomic weights; and the fourth column, the deviations from the serial numbers. The next columns show the specific gravity, the atomic volume, the fusibility, mallea- bility, and place in an electro-chemical series for each element, and the last column the group in the classification of Newlands and Mende- leeff to which the element has been assigned. The horizontal lines divide the series and periods of this system. The observed atomic weights are taken from the lists of Clarke,* L. Meyer,f and Van der Plaats,$ and in most cases by selecting for each element that one of the values that differs least from the mean, taking oxygen at 1G for a standard, and expressing but one place of decimal fractions. The data for the next four columns are taken from Meyer's " Modern Theories." To express their fusibility, the elements are divided into seven classes, that represented by 1 being the most fusible. The brittle and malleable elements are distinguished * The Constants of Nature. A Recalculation of Atomic Weights, 1882. t Modern Theories of Chemistry, English Translation, 1888. t Verification of the Atomic Weights of M. Stas. OF ARTS AND SCIENCES. ll'.T by the initial letters B and M. In the electro-chemical series taken from Barker's " Text-Book of Chemistry," * 1 is the most electro-posi- tive in an acid solution, and 63 the most negative. It appears from these tables that none of the deviations from the serial numbers exceed 0.6 excepting that for Cb among the perissads, and Zn and Mo among the artiads ; Zn differs by just a unit, and 6eems to foim an exception to the regularity. In his account of the Discovery of the Periodic Law,f Newlands points out the irregularity of the single series, illustrating it by several tables, and the data are clearly set forth and tabulated in a recent paper by Venable, on the Recalculation of the Atomic Weights.! In the artiad grand group no atomic weight corresponds to 20, 36, 83, or 131, and a reference to the electro-chemical series will show that these are the points at which the elements change from a negative to a positive maximum, corresponding also to the maximum atomic volumes, and to the end of the Mendeleeff periods. These points are marked with asterisks in the table. Analogy points to the possibility of elements with atomic weights of 15, 43 or 44, 47, 60, and perhaps of 99, 100, and 143.5. The newly discovered philippium and praseodymium may perhaps correspond to 47 and 143.5, respectively, but there appears to be no place in either series for neodymium or 140.3. In each of the grand groups, perissads and artiads, the breaks be- tween the minor groups of common difference occur at or near the minimum points of the series of atomic volumes, and therefore mid- way between the dividing lines above mentioned. The first term of each of the groups of common difference, except the first, viz. Ga, Ag, Au, Ge, Pd, and Pt, appears to be a heavy malleable metal, electrically neutral, and with an atomic volume a little above 9 in the artiad, and 10 in the perissad groups. With the increase of atomic volume is generally associated an in- crease in electro-negative properties, and, as a rule, the elements be- come fusible, brittle, and diamagnetic. With the maximum atomic volume, the elements change from the extreme of negative to positive, from diamagnetic to magnetic, from brittle to malleable ; and with the decrease of volume, they lose their electro-positive properties, and, as a rule, become at last brittle and infusible. * Text-Book of Chemistry, p. 16. t The Periodic Law, p. 27. 1 Journal of Analytical Chemistry, January, 1889, p. 48. 1G8 PROCEEDINGS OF THE AMERICAN ACADEMY TABLE I. — Perissads. Atomic Weights. Physical Properties. El. Gr. Ser. Obs. Dev. Sp. Gr. At. Vol. Fus. Mai. Elec. H 1 1.0 0.0 •• •• I Li 7 7.0 0.0 0.59 11.9 1 JV1 5 I B 11 11.0 0.0 15 ? 2.68 4.0 6 B 49 III F 19 100 0.0 1 B 60 VII Na 23 231 +0.1 0.97 23.7 1 M 4 I Al 27 27.1 +0.1 2.56 10.6 3 M 13 III P 31 31.0 0.0 2.30 13.5 2 B 55 V CI 35 35.5 +0.5 1.38 25.6 1 B 59 VII K 39 39 1 +0.1 0 80 45.4 1 M 3 I Sc 43 44. ? .... 47 1 •• III V 51 51.3 +0.3 5.50 9.3 7 B 52 V Mn 55 55.0 0.0 8.00 6.9 5 B 19 VII Co? Cu 59 (59.0 0 0 8.50 6.9 5 M 23) 63 63.5 +0.5 8.80 7.2 3 M 31 I + 7 + n X 5 Ga 70.0 70.0 0.0 5.96 11.7 1 -2 ? III As 75.0 75.0 0.0 5.67 13.2 2 B 54 V Br 80.0 80.0 0.0 2.97 26.9 1 B 58 VII Kb 85 0 85.4 +0 4 1.52 56 1 1 M 2 I Y 90.0 89.8 —0.2 * * • • , t 11 III Cb 95.0 94.2 —0.8 100.0 + 7 5 + n X 6.25 G.27 15.0 7 B 44 V Ag 107.5 107.9 +0.4 10.50 10.2 3 M 32 I In 113.7 113.7 0.0 7.43 15.3 1 M 27 III Sb 120.0 120.1 +0.1 6.70 17.9 2 B 47 V I 126.3 126.8 +0.5 4.94 25.6 1 B 57 VII Cs 132.5 132.9 +0.3 1.88 706 1 M 1 I La 138 8 138.8 0.0 6.20 22.3 3? 18 III Di 145.0 145.0 0.0 ? + n X 4 6.50 22.3 3? 17 V Au 190.0 196.6 +0.6 19.30 10.2 3 M 40 I Hg 200.0 200.2 +0.2 13.59 14.7 1 M 33 II Tl 204.0 204 2 +0 2 11. si; 18.1 2 M 24 III Bi 208.0 208.0 0.0 9 82 21 1 2 B 29 V OF ARTS AND SCIENCES. 1G9 TABLE II. — Artiads. El. Atomic Weights. Physical Properties. Gr. Ser. Obs. Dev. Sp. Gr. A.t. Vol. Fus. Mai. Elec. 12 +n X4 C 0 2 12.0 12.0 0.0 16.0 16.0 0.0 20.0 * 0.33 3.6 7 1 B B 54 63 IV VI Mg Si S 24.0 24.0 0.0 28.0 28.1 +0.1 32.0 32.1 +0.1 36.0 * 1.74 2.49 2.04 13.8 11.2 15.7 3 6 1 M B B 9 42 62 II IV VI Ca Ti Cr Fe 40.0 40.0 0.0 44.0 ? 48.0 48.1 +0.1 52.0 52.3 +0.3 56.0 560 0.0 60.0 1 1.57 6.80 7.80 25.4 ' 7.7 7.2 2 *5 5 iM B B M 8 43 53 21 II IV VI VIII Zn Ge As Se 64.0 65.0 +1.0 + 7 + n X4 71.0 ? 75.0 75.0 0.0 70.0 79.0 +0.0 83.0 * 7.15 i 5.07 4 60 9.1 13.2 17.1 2 i 2 1 M B B 20 i 54 56 II IV V VI Sr Zr Mo Pd 87.0 87.5 +0.5 91.0 90 6 —0.4 95.0 95.9 +0.9 99.0 ? + 7 + n X 6.25 106.0 1060 0.0 2.50 4.15 8.60 11.50 34.9 21.7 11.1 9.2 2 6 6 4 M B B M 7 14 51 34 II IV VI VIII Cd Sn Te 112.2 112.2 0.0 118.5 118.0 +0.5 124.8 125.0 —0.2 131.0 * 8.65 7.29 6.25 12.9 16.1 20.2 2 2 2 M M B 25 28 46 II IV VI Ba Ce? Pt Os 137.2 137.1 —0.1 143.5 ? ? ? + n X 4 195.0 194.9 —0.1 199 0 198.9 -0.1 3.75 6.70 21.50 22.50 36.5 21.0 9.1 87 2 3? 5 5 M M B (i 16 37 39 11 IV VIII VIII Pb 203.0 ? •_!n7.0 206.9 —0.1 11.38 18.1 2 M 26 IV Ni Co Ru Rh Ir 14 + n X 44.8 58.8 58.7 —01 58 8 59.0 +0.2 103.6 104.0 +0.4 103.6 104.2 +0.6 148.4 1 193.2 193.0 —0.2 8.80 8.50 12.26 12.10 22.46 6.7 6.9 8.4 8.6 8.6 4 5 5 6 5 M M B M B 22 23 85 86 38 VIII \ III VIII VIII VIII 170 PROCEEDINGS OP THE AMERICAN ACADEMY The 'study of the periodic law has directed attention to the relations between the atomic weights and these properties, many of which were previously treated as functions of the electro-chemical order. When the exact atomic weights are all determined with sufficient accuracy, it is natural to infer that the deviations from the regular increase will show a law as significant as the approximate coinci- dence with the serial numbers, and even now we see clear evidences of this law. To make it more apparent, it will first be necessary so to adjust the formula as to reduce these differences to a minimum, and in the low atomic weights to take account of smaller fractions. The formula a -\- n d then has the following values for the sev- eral groups of common difference : — 6.99 + «X 4.02 12.00 + nx 4.01 70.25 + n X 4.85 74.88 + n X 4.12 107.85 + w x 6.20 105.98 + n X 6.22 Table III. shows the deviations, arranged in the groups and series of the periodic law ; the lower division shows the electro-chemical numbers in the same form. Neglecting insignificant deviations, we find the positive results, or those where the atomic weight is slightly in excess of the serial num- ber, either near the extremes of the electric series, in elements of maximum atomic volume, etc., or in the very centre of this series. The negative results occur half-way between the centre and the ex- tremes. Of the perissads, 1, 2, — 31, 32, — 57, 59, are positive, and 17, 18, 19, 21, — 44, 47, 54, 55, are negative; of the artiads, 7, — 46, 51, 53, are positive, and 8, 14, 21, 23, 28, are negative. In the periodic arrangement, the first and second groups show posi- tive deviations in the high series of this arrangement; the third, fourth, and fifth, negative in the high series ; the sixth, positive in the high series ; and the seventh, positive in two terms, and insignificant in two. The seventh and eighth groups are negative in the third series. The deviation of Zn is not included in these calculations, nor is the cause of its deviation yet apparent. Perhaps the perissads of the second group are formed from an artiad nucleus, and the artiads of the second group from a perissad nucleus, thus : * G5, 70, 75, 80, etc., and 63 * 71, 75, 79, etc. The last line shows the algebraic mean of the deviations in each group, which, as might be expected, corre- sponds nearly to the relative atomic volumes. To do justice to the bearing of these results on the physical ques- tion of the ultimate nature of "atoms" would involve a mathematical OF ARTS AND SCIENCES. 171 TABLE III. — Deviations. Gr. I. II. III. IV. v. VI. VII. VIII. Ser. 1 —.03 i —.03 .00 ? —.01 —.03 2 —.02 —.02 .00 + .02 —.08 +.01 +.32 3 —.02 —.08 ? .00 +.05 + .10 (-.26) —.11 4 +.06 ■? —.30 ? —.06 + .03 + .01 5 + .64 +.28 + .01 —.80 —.30 + .47 +.02 6 + .08 +.03 —.36 —.42 —.14 +.31 +.41 7 +.25 + .02 —.18 ? —.05 +.14 +.05 —.14 —.25 —.09 + .17 + 18 —.05 Electro-chemical Order. 1 5 i 49 48 i 63 00 2 4 9 13 42 55 02 59 3 3 8 ■? 43 52 53 (19) 21 4 31 20 ? 1 54 56 58 5 2 7 11 14 44 51 34 6 32 24 27 28 47 46 57 7 1 6 18 16 17 discussion too prolonged for this paper ; but the subject cannot be com- pleted without a brief statement of its relation to well known systems and theories of Chemistry. A few extracts will serve as a basis to show what the perissad law is intended to contribute to the solution of the all-important problem. In 1854, in a paper read before the American Academy on " The Numerical Relation between the Atomic Weights," Professor Cooke announced the character of the problem as follows : — " Numerical relations between the atomic weights of the chemical elements have been very frequently noticed by chemists. One of the fullest expositions of these relations was that given by M. Dumas, of Paris, before the British Association for the Advancement of Science, at the meeting of 1851. This distinguished chemist at thai time pointed out the fact, that many of the elements might be grouped in triads, in which the atomic weight of one was the arithmetical mean of those of the other two. Thus the atomic weight of Bromine is the mean between those of Chlorine and Iodine; that of Selenium i- the mean between those of Sulphur and Tellurium ; and thai of Solium, the mean between those of Lithium and Potassium. "M. Dumas also spoke of the remarkable analogies between the 172 PROCEEDINGS OF THE AMERICAN ACADEMY properties of the members of these triads, comparing them with sim- ilar analogies observed in Organic Chemistry, and drew, as is well known, from these facts arguments to support the hypothesis of the compound nature of many of the now received elements. Similar views to those of Dumas have been advanced by other chemists. "The doctrine of triads is, however, as I hope to be able to show in the present memoir, a partial view of this subject, since these triads are only parts of series similar in all respects to the series of homo- logues of Organic Chemistry, in which the differences between the atomic weights of the members is a multiple of some whole number. All the elements may be classified into six series, in each of which this number is different, and may be said to characterize its series. In the first it is 9, in the second 8, in the third G, in the fourth 5, in the fifth 4, and in the last 3." (See Table IV.) The paper speaks of the properties of the elements which are func- tions of the atomic weights, and says that it does not seem bold the- orizing to suppose that the atoms of the members of the same series are formed of a common nucleus, to which has been added one or more groups of atoms, or perhaps one or more single atoms, to which the corresponding element has not been discovered. Referring to this subject in 1857,* M. Dumas said : "I have often tried, as Mr. Josiah Cooke has on his part, to compare them, to com- bine them, and to discuss them, with the hope of drawing some conclu- sion from them with certainty, but I have been unable to draw from them anything but doubt. The formula deduced from the above simple progression" (a+?id) "would not account for the generation of simple bodies, as Cooke had supposed, but organic radicles are not always formed by addition, they are also produced by substitution, as we see in the compound ammoniums." Dumas proposed to substitute a formula like n a -f- n' d-\- n" d' ; a being the nucleus; d and d\ the common differences ; and n, n', n", whole numbers. Table IV. shows the series of Cooke aud Dumas. Following in their footsteps, Professor Newlancls extended their prin- ciples to include newly discovered elements. Employing Cannizzaro's atomic weights instead of those of the old system, and collating his own results and all discovered up to 1864, he arranged the groups in hori- zontal lines instead of vertical columns, and then discovered the " Law of Octaves," as shown in Table IV. The coincidence of the ordinal numbers led him, in 18G5, to express the following opinion: "I will * Comptes Rendus, 1857, p. 709. OF ARTS AND SCIENCES. 173 TABLE IV. Cooke, 1854. Ser. Gr. in. 3. 2. 1. IV 3, 2. 1. v. VI. VIII. IX. IV. 2. 1. 3. H Li Na K Ag CaMg Sr Zn Ba Cd Pb Al Ti Cr Pd Mn Sn Fe Pt Co Ir Ni Os U Au Cu Hg C B Si 0 N P As Sb Bi 0 s Se M Te V W Ta 0 F Cy 3 CI Br I Al Ti Cu Cr Pd Hg MnSn Fe Pt Coir Ni Os U Au Cu Mn Ti Cr V As Mn Cr Mn Os Au Dumas, 1857. Form. 7 + n .8 12 + n 8 25+ nSi 6 + ?i5 14 + n 17 8 + ?i8 19 + m 16.5 + «'28 L Na K Mg Ca Sr Ba Pb Ti Sn Ta C B Si Zr N P As Sb Bi Cr 0 Mo S V Se W Te F CI Br I Mendeleeff, 1869. Or. -S..-r_ 1 2 .3 4 5 6 7 8 9 10 11 12 I. II. III. IV. v. VI. VII. \ in. H Li Na K (Cu) Rb (Ag) Cs (-) (Au) Be Mg Ca Zn Sr Cd Ba Hg B Al Sc Ga ?Y In ?Di ?Er Ti C Si Ti Zr Sn ?Ce ?La Pb Th N P V As Nb Sb Ta Bi 0 s Cr Se Mo Te W u F CI Mn Br I IV Co Ni Cu RuRhPdAg Oa Ir Pt Au 174 PROCEEDINGS OP THE AMERICAN ACADEMY TABLE IV. — Continued. Newlands, 1865. No. No No. No. No. No. No. No. H 1 F 8 CI 15 Co&N 22 Br 29 Pd 36 I 42 Pt&I ^50 Li 2 Na 9 K 1(5 Cu 23 Rb 30 Ag37 Cs 44 Tl 53 G 3 MglO Ca 17 Zn 25 Sr 31 Cd 38 Ba&V45 Pb 54 Bo 4 Al 11 Cr 19 Y 24 Ce & La 33 U 40 Ta 46 Tb 56 C 5 Si 12 Ti 18 In 26 Zr 32 Sn 39 W 47 HS 52 N 6 P 13 Mn20 As 27 Di&Mo34 Sb 41 Nb 48 Bi 55 0 7 i S 14 Fe 21 Se 28 Ro&Ru35 Te43 Au 49 Os 51 endeavor to show that all the numerical relations among the equivalents pointed out by M. Dumas and others, including the well known triads, are merely arithmetical results flowing from the existence of the 'law of octaves,' taken in connection with the fact of the equivalents forming a series of numbers approaching to the natural order." And in 1866 : " The fact that such a simple relation exists now, affords a strong presumptive proof that it will always continue to exist, even should hundreds of new elements be discovered. For, although the differ- ence in the numbers of analogous elements might, in that case, be altered from 7, or a multiple of 7, to 8, 9, 10, 20, or any conceiv- able figure, the existence of a simple relation among the number of analogous elements would be none the less evident." * The law of regular increase, however, points to a relationship far more significant than the identity of their ordinal numbers. Working independently of Newlands, Mendeleeff discovered the pe- riodic law in 1869. It has offered a grand incentive to new discov- eries and received well merited recognition throughout the world. The extracts from Wurtz and Meyer, at the beginning of this paper, show what it left to be desired. A paper by Rev. Dr. Haughton, and an abstract of one by Mr. Stoney, have recently appeared in " The Chemical News." Each gives a clear enunciation of the nature of the problem. Dr. Haugh- ton discovers some of the regular intervals noticed here. Unfortu- nately, the paper of Stoney, on " The Logarithmic Law of Atomic Weights " f is so abridged, that it is hard to determine how his results may compare with those herein discussed. The abstract states, that, in plotting the atomic volumes as ordinates of a diagram, the effort to * The Periodic Law, p. 20. t The Chemical News, vol. lvii. p. 163. OF ARTS AND SCIENCES. 175 extract information from the resulting curves was a failure ; iu plot- ting their cube roots, however, he found a logarithmic curve with per- turbations which showed a distinct law of increase for perissads and aitiads. The abstract was not discovered until most of this paper was written, and, from its indefinite statements, it would require much time to construct the curves and divine the inferences. At the close of his paper of 1854, Professor Cooke said : " To my conceptions Chemistry will then have become a perfect science, when all substances have been classed in series of homologues, and when we can make a table which shall contain, not only every known substance, but also every possible one, and when by means of a few general formula? we shall be able to express all the properties of matter, so that, when the series of a substance and its place in the series are given, we shall be able to calculate, nay predict, its properties with absolute certainty. . . . Then the dreams of the ancient alchemist will be realized, for the problem of the transmutation of metals will have been theoretically, if not practically, solved." 176 PROCEEDINGS OP THE AMERICAN ACADEMY XV. CONTRIBUTIONS FROM THE JEFFERSON PHYSICAL LABORATORY, HARVARD UNIVERSITY. NEUTRALIZATION OF INDUCTION. By John Trowbridge and Samuel Sheldon. Presented May 28, 1889 The invention of the telephone drew attention to the extraordinary sensitiveness of Faraday's electrotonic state, and immediate attempts were made to construct induction balances, so called, which might serve for quantitative measurements. Thus we have Hughes's induction balance, which had its prototype in the balance described in Max- well's " Electricity and Magnetism," Vol. II. § 636, due to Felici,* and which differs from Hughes's balance merely in the employment of a galvanometer instead of a telephone. By substituting the lat- ter instrument, Hughes showed that great sensitiveness could be obtained, and even proposed to adopt an instrument for measuring minute amounts of impurities in coins arising from alloys. The great difficulty, however, in the employment of Hughes's induc- tion balance in quantitative work arises from the difficulty of getting a good minimum of tone in the telephone. The method that Hughes employed was, briefly, to employ four coils, — two in a circuit through which an alternating current or an interrupted current was passed, and two other coils placed contiguous to the coils which were in the interrupted circuit, but in another circuit.' By interposing a telephone in the last mentioned circuit, and by properly placing the coils in this circuit with reference to those in the circuit through which the inter- rupted current was passed, a balance could be obtained, or an imperfect minimum of sound in the telephone, when the induction between the sets of coils was neutralized. In order 'to obtain a standard, Hughes employed a wedge of zinc, which was thrust between one of the coils in the interrupted circuit and one of the coils in the telephone circuit, in order that the mutual induction between these coils might balance * Nuovo Cimento, vol. ix. p. 345, 1859. OP ARTS AND SCIENCES. 177 that arising between the other two similarly placed coils whin a coin or sheet of metal was placed between these last mentioned coils. Other devices have also been employed by various investigators who have endeavored to use the apparatus for quantitative measurement. Alexander Graham Bell employed a modification of Hughes's induc- tion balance for the detection of the presence of a bullet in the human body. In the form employed by him, one coil, which was a closely wound flat copper band, was made to slide over a similar one by means of a screw, one coil being placed in the telephone circuit and the other in a circuit containing a current-breaker. The induction arising from a similar pair of coils moved over a mass of metal like a bullet could thus be neutralized by this sliding coil arrangement. In no form, however, of Hughes's induction apparatus can one obtain a satisfactory minimum of tone in the telephone. There is never abso- lute silence, and no two observers can obtain the same point at which the sound seems to be a minimum. The failure to obtain this min- imum is thus a radical defect in the instrument. It is doubtless very sensitive, but it cannot be called a quantitative instrument. To remedy this defect, A. Overbeck and J. Bergmann * substituted an electro-dynamometer for the telephone, and worked out a method of obtaining the resistances of metals when they are in the form of thin circular plates. The standard of comparison they employed was a thin layer of mercury between disks of glass in a cylindrical reser- voir. Preliminary investigations had shown the authors that a cer- tain relation existed between the thickness and specific resistance and coefficient of induction of metals in the form of thin disks, which were placed between the coils of the induction balance. In a subsequent paper,f A. Overbeck gives the mathematical theory of the induction balance, which in the main is Maxwell's theory of current sheets applied to Arago's disk.$ In employing the instrument to measure the effect of change of temperature on induction in copper plates, or, in other words, temperature coefficients, in which we found thai Messrs. Overbeck and Bergmann had anticipated us,§ we were led to adopt the following form of the instrument, which differed entirely from that of these authors. Four coils were employed, as in the Hughes lorn. of instrument. One of the coils in the telephone circuit was fixed upon a horizontal axis which was at right angles to the axis of the * Annalen der Physik, xxxi., 1887, p. 792. t Ibid., p. 812. | Maxwell's Electricity and Magnetism, vol. ii. § 668 et seq. § Annalen der Physik, xxxvi., 1880, p. 783. vol. xxiv. (h. s. xvi.) 12 178 PROCEEDINGS OP THE AMERICAN ACADEMY coil. The coil could therefore be moved through all positions, from perfect parallelism to its. neighboring coil in the interrupted circuit to a position at right angles to this coil. The horizontal axis was pro- vided wiih an index arm which moved over a graduated circle. Call- ino- 6 the anjrle of inclination of the axis of the movable coil with the axis of the fixed coil in the interrupted circuit, and N the strength of the induction current in the movable coil, we have evidently, on the supposition that the strength of the alternating current remains constant, N = constant X cosine 6. When the axes of the coils are at right angles, cosine 6 = 0, and we should have silence in the telephone. Since adopting this arrange- ment we have discovered that Dr. Bowditch, of the Harvard Medical School,* has employed this arrangement of a movable coil placed in front of a fixed coil as a modification of Du Bois Reymond's appa- ratus for controlling induction currents so that they may be admin- istered by known amounts for physiological purposes. In Du Bois Reymond's apparatus one induction coil was simply moved away from a fixed coil through which an interrupted current was passed, much in the same manner as the coils in Wiedemann's form of galvanometer are moved. Here no minimum could be obtained. In Dr. Bowditch's form of this apparatus, theoretically a minimum should be obtained, that is, when cosine 8 = 0, or when the axes of the coils were at right angles. An indication of an electrical current is obtained even when the axes of the coils are at right angles, on account of the windings of the coil not being perfectly at right angles to those of the stationary coil. That no minimum should be obtained when the axes of the coils are at right angles, and when induction arises from all parts of the circuit, is evident upon an elementary consideration of the subject. We have to deal in this form of instrument with the mutual induction which arises between the fixed coil and the movable one, and also with the self-induction which arises between the spires of the movable coil in the telephone circuit. The mutual induction can be reduced theo- retically to zero by placing the movable coil of the telephone circuit at right angles to the fixed coil. The self-induction can be estimated as follows. Taking Maxwell's discussion for the induction between parallel circuits of radii A and a, we have the coefficient of mutual induction, cos e ds dsf M -ff- * Proc. Am. Acad., vol. xi. p. 281. OP ARTS AND SCIENCES. 179 Projecting one circle upon the plane of the circle of greater radius, A, we have M _ C2n C2n A a cos (ft — 0') dcf> ' Jo J> V^M-o2 -R>2 — *- Waco's (ft — ft') ' Making 6 the distance between the planes of the circles = 0, we pass from the case of mutual induction to that of self-induction between two spires of a coil which may be considered approximately circular. The form of M adapted for calculation is then M= 4tt \/Aa j(c — -) F+ ?.#]•, where c = -—-. — -, and F and E are complete elliptic integrals to (A-\-a) i t- s> modulus c. If we make A — a = B, or A = D + a, in which D is the distance between the spires at which the self-induction becomes insensible, the most perfect minimum can be attained. We have found that copper wire of 2 mm. diameter, wound in a flat loose spiral, the spires of which from centre to centre of the wire are 4 mm. apart, gives no sensible self-induction for spirals of eight to ten spires. On turning a movable coil of this form so that its axis may be perpendicular to the axis of the fixed coil, a perfect minimum can be obtained. A slight movement to the right or left of this position is quickly made evident by the note of the interrupted circuit which is heard in the telephone. It is evident that, if four coils are employed, as in Hughes's form of induction balance, the two coils in the telephone circuit should be wound in the manner we have indicated, to avoid self-induction. On placing a plate of metal between one set of the coils of this balance, the movable coil no longer gives ;i minimum at the position where its axis is at right angles to that of the fixed coil, but at some point removed a few degrees from this. By placing a mirror upon the movable coil, and by observing its deflection with a telescope, a greater refinement of reading is possible. This instrument in its modified form suggests the possibility of neutralizing induction upon telephone circuits. The extension of the various systems for transmitting power by electricity, especially the electric car system, has led to great disturbances in the telephone circuits. These disturbances are due both to leakage from the power circuit into the telephone circuit, since the earth is used partially by the electric power companies in their return circuits, and to actual induction. The best remedy for these disturbances is doubtless the 180 PROCEEDINGS OF THE AMERICAN ACADEMY adoption by either the power companies or the telephone companies of entire metallic circuits, in which the earth plays no part. If this is not possible, a system of neutralization for the inductive disturbances might be adopted as follows. Let a shunt circuit from the electric light wire or the wire carrying the current for motors be led into a station through which also passes the telephone wire. The resist- ance of this shunt or derived circuit can be made suitable for the pur- pose. In all cases it reduces the resistance of the main line, and is therefore not prejudicial. On this shunt can be arranged a fixed coil, and on a neighboring telephone wire a movable coil of no self-induc- tion. Let this movable coil be placed in front of the fixed coil in the motor circuit, and let it be turned until the. mutual induction between it and the fixed coil neutralizes the induction produced at all points along the telephone circuit. Each telephone wire would need its movable coil, and to every movable coil would correspond a fixed coil in the shunt of the motor circuit. The operator at the central sta- tion could adjust the movable coils until the disturbances arising from induction at various points along the line are neutralized. OF ARTS AND SCIENCES. 181 XVI. THE MAGNETISM OF NICKEL AND TUNGSTEN ALLOYS. By John Trowbridge and Samuel Sheldon. Presented May 28, 1889. Introductory. The fact that different kinds of steel, alloyed in small proportions with Tungsten or Wolfram, and magnetized to saturation, increase in spe- cific magnetism * has long been known. Whether the same effect would result from the use of Nickel alloyed with Tungsten has never been investigated. This paper has for its object a partial answer to the query. It was instigated by Mr. Wharton, proprietor of the American Nickel Works, whose chemist, Mr. Riddle, kindly prepared the alloys which have been employed. These alloys were in two groups. The first, received in November, 1888, consisted of three bars of the same shape, one being of pure nickel and the other two having respectively 3 and 4 per cent of tungsten in alloy. These bars were rolled from cast ingots, which were toughened by the addition of magnesium after Fleitmann's method, the magnesium being added just before pouring. They were hot when rolled. The one of pure nickel was afterwards planed into regular shape. Those containing tungsten were too brittle to allow of this manipulation. They were, however, of sufficient regularity to permit accurate measurements. This group contained also an octagonally shaped bar with 8 per cent of tungsten, which was prepared like the others, and was afterwards ground into shape. The second group, received in May, 1889, contained bara which were simple castings, m;ule without the addition of magnesium, and consisted of pure nickel and alloys with 1, 2, 3, and G per cent of tungsten. All the bars in this group were extremely hard and brittle. In making them, tungsten oxide, of weight calculated to yield the de- sired percentage of tungsten in the resulting alloy, was placed with * Jour. Chem. Soc, 1868, xxi. 284, says 300 per cent. 182 PROCEEDINGS OP THE AMERICAN ACADEMY adequate carbon in the bottom of a graphite crucible and covered by the proper weight of pure grain nickel. All was then covered with borax, the lid of the crucible was placed on, and the crucible was heated until reduction and fusion wrere completed. Method. As the suspected influence of the tungsten would be to affect the magnetic moment of the bars, these were magnetized to saturation and their specific magnetism then determined, i. e. the magnetic moment for each gram of metal. The magnetization was effected by placing the bars separately in a hollow coil whose length was 15 cm. and outside and inside diameters respectively 6 and 3 cm. It consisted of 6 layers of wire having 63 turns each. A dynamo current of 40 amperes was then sent through the coil for one minute, and the circuit then broken and the bars removed. For the determination of the magnetic moment, use wTas made of a reflecting magnetometer, and deflections were observed with a telescope and scale at a scale-distance of 100 cm. Measurements of the hori- zontal intensity, H, of the earth's magnetism were first made. The results from these determinations by means of the first and second Gauss arrangements were, respectively, H= 0.1724 cm. g. s. H= 0.1720 The freshly magnetized bars were then placed in the second Gause position relative to the magnetometer, and the angular deflection de- termined. The specific magnetism, S, was then calculated by the formula c rz H tan £) = - — 111 where r = distance from bar to magnetometer = 72.68 cm. H = earth's horizontal intensity = 0.1722. m = mass of the bar. — angular deflection of magnetometer. Results. The mean results of two sets of observations on Group I., and also upon a similar bar of soft tool steel are given in the following table. OP ARTS AND SCIENCES. 183 GROUP I. Composition. Size in cms. Mass in grams. /S[cm.sg.-J sec.-']. Pure Nickel 18 X 2.7 X 0.65 284.5 1.23 Ni + 3%W it tt u 286.5 10.60 Ni + 4%W it (i u 283.5 10.40 Tool Steel 15 X 2.5 X 05 159.5 7.46 Ni + 8%W / Octagonal \ U3 X 1.5/ 144.0 5.25 Group II., of cast bars, gave the following results. GROUP II. Composition. Size in cms. Mass in grams. S [cm. 5 g ~i sec.-1]. Pure Nickel 18 X 1.8 X 1.6 459 1.05 Ni + 1 % W it tt tt 455 1.92 Ni + 2 % W tt tt tt 454 1.70 Ni + 3%W tt It tt 463 1.75 Ni + 6%W tt tt tt 465 1.15 The bars of both groups were, subsequent to the above observations, completely demagnetized, and then freshly magnetized. New deter- minations save the same results as before. The demagnetization was accomplished by placing the bars inside two coils, which were traversed by currents from an alternating dynamo. The coils were then slowly drawn apart, and the bars maintained at a position central between them. After treatment in this manner, they showed no appreciable deflection when placed in position relative to the magnetometer. The results tabulated indicate that tungsten greatly increases the magnetic moment of nickel, if the alloy he forged and rolled, bul on the other hand has but small influence if they be simply east. Fur- thermore, changes in the amount of tungsten do not appear to cause corresponding changes in the magnetic properties. To see whether the remarkable effect in bars 2 and 3, aa compared with bar 1, of Group I. was owing to some molecular condition oi their 184 PROCEEDINGS OF THE AMERICAN ACADEMY surfaces induced by rolling, two bars from the same steel, one rolled and the other pressed, were magnetized and then measured. The ratio of the specific magnetism of pressed to rolled was as 9 to 5, the rolled having the smaller amount. The existing difference, in this case, is probably owing to a difference in hardness, rather than to any molecular condition of the surfaces. The specific magnetisms of all the bars are small when compared with good steel magnets. Kohlrausch says that good magnets, of common form, should have S = 40. The bar of ordinary tool steel, however, retained but 7.46. Still it was soft, and by tempering would doubtless have doubled this value. If forged nickel and tungsten can be made to maintain a specific magnetism of 10, it will form a useful addition to the resources of physical laboratories. From the high polish of which it is suscepti- ble and its freedom from damaging atmospheric influences, it will be most happily suited for the manufacture of mirror magnets where magnetic damping is to be employed. Jefferson Physical Laboratory. OF ARTS AND SCIENCES. 185 XVII. THE MECANIQUE CELESTE OF LAPLACE, AND ITS TRANSLATION WITH A COMMENTARY BY BOW- DITCH. By Joseph Lovering. Presented June 8, 1889. Laplace was born in Beaumont-en-Auge on March 28, 1749. The early years of his life are hidden in the obscurity of his humble origin. It is only known that he was the son of a small farmer. He first gained distinction in a theological controversy. After attend- ing some of the classes in a military school in Beaumont, he taught mathematics there. At the age of eighteen, he approached the great D'Alembert with the hope of finding some career in Paris, and was rebuffed. Afterwards, Laplace sent to him a letter on the Principles of Mechanics. D'Alembert wrote back : " You see that I make little enough of the matter of recommendations. You have no need of them. You have done better : to know. This is enough for me : my support is your due." Thus he mounted at once to the position of Mathematical Professor in the Military School at Paris. Before en- tering the Paris Academy, at the age of twenty -four, he began his career of investigation by which he won the title of the Newton of France, having made a capital discovery relating to the mean distances of the planets from the sun. Laplace was also an investigator in phys- ics and chemistry, working with Lavoisier and Berthollet. Only fifteen days before his last sickness, he communicated to the Memoirs of the Academy a paper on the oscillations of the garth's atmosphere, which was printed in the same volume which contained Poisson's funeral oration. Of his three great works, the five volumes of the Micanique Celeste were published between 1799 and 1827 ; the Exposition du Systeme dn Monde in 1796; and the Theorie analytiqne des Proba- Mites in 1812. Arago reported, in 1842, that not a copy of the last work was in the libraries of Paris, although three editions had been published, and that the two other works were almost out of 186 PROCEEDINGS OF THE AMERICAN ACADEMY print, so that he feared that it would be necessary to order from America Bowditch's translation. In this emergency Madame de Laplace, always devoted to the reputation and memory of her dead husband, was negotiating for the sale of a small farm in order to pro- vide tbe means of republishing his works, when the government of Louis Philippe took the matter in hand and appropriated forty thou- sand francs for a new edition. This appeared, in seven quarto vol- umes, between 1843 aud 1847. At a later period, when this edition was nearly exhausted, General Laplace, the distinguished son of the mathematician, and his granddaughter, the Marquise de Colbert, ex- pended seventy thousand francs on a third edition, which appeared between 1878 and 1886. Laplace was the friend of young mathematicians and physicists, such as Arago, Poisson, and Biot, who were called " the adopted children of bis thought." At an early age, while still a pupil in the Polytechnic School, Arago was attached to the Paris Observatory as secretary. He has given in his Autobiography the following inter- esting sketch of Laplace. He says : " I entered this establishment, then, on the nomination of Poisson, my friend, and through the inter- vention of Laplace. The latter loaded me with civilities. I was happy and proud when I dined in the Rue de Tournon with the great geometer. My mind and my heart were much disposed to admire all, to respect all, that was associated with one who had discovered the cause of the secular acceleration of the moon, had found in the move- ment of this satellite the means of calculating the ellipticity of the earth, had traced to the laws of gravitation the long inequality of Jupiter and Saturn, etc., etc. But what was my disenchantment when, one day, I heard Madame de Laplace approach her husband, and say to him, 'Will you intrust to me the key of the sugar ?': Another anecdote told by Arago is not so complimentary to La- place. Delambre, the Perpetual Secretary of the Academy of Paris, died on the 19th of August, 1822. A committee was appointed to present candidates for the succession. The choice lay between Fou- rier and Biot. The election was always by secret ballot, — Arago frankly saying that no one wished to incur the disaffection of a suc- cessful candidate against whom he had voted. Laplace wrote the same name upon two ballots, put them in his hat, and shook them up. He took one out and tore it, and put the other in the urn, pretend- ing not to know for whom he had voted, though an indiscreet neighbor did. No calculus of probabilities, Arago says, was needed for this problem. OF ARTS AND SCIENCES. 187 Twenty-three years after the death of Laplace, Biot confided to the Academy of Paris these interesting reminiscences of him. " Every one," he says, " will understand how valuable to a young man were these familiar and intimate interviews with a genius so powerful and so comprehensive. But what he might not imagine were the senti- ments of affectionate and paternal delicacy which attended them, unless he himself had been the object of them. Shortly after I was permitted to approach him, I had the good fortune to take a step, which seemed to me new and unexpected, in a field of mathematics hitherto scarcely invaded. In 1766, Euler had treated a peculiar class of geometrical questions by an indirect method in a paper entitled JJe inslgni promotione methodi tangentium inversce.* Subsequently, he attacked a more difficult problem of the same kind, to which he re- peatedly returned with different solutions, but always indirect. The singularity of the problem originated in the nature of the curve, the geometrical characters being of different orders, — some belonging to points infinitely near, others to distant points separated by finite differences. I succeeded in rendering a complete statement of the problem in analytical language, applying to each part appropriate symbols. The realization of this idea surpassed my expectations. f " After I had found the key to a solution of the problem, I spoke to Laplace about it. He listened with attention and with some surprise, and then said, ' It seems all very well ; come to-morrow morning and bring your memoir ; I shall be glad to see it.' After hearing it, discussing it, and suggesting certain omissions, he told me to present it to the Academy the next day, and, after the session, come and dine with him. 'Now,' said he, 'let us lunch.'" Biot communicated his paper to the Academy in the presence of Monge, Lagrange, Laplace, and of Bonaparte who had just returned from Egypt. Bonaparte pretended to recognize the diagrams, though no one had ever seen them before except Laplace. " I had more fear of Lagrange," said Biot, "than of Bonaparte, with all his military glory." After Biot had read his paper, and received the congratulations of the Academicians, he accompanied Laplace home. As soon as they had entered the house, Laplace took Biot into his study, unlocked a closet, took out a copy-book, yellow with age, and showed him all * Nov. Comment. Petrop., x. t Considerations sur les equations aux differences mdlfes j Mem. Saratlta Etrangeres, i 296-328. 188 PROCEEDINGS OF THE AMERICAN ACADEMY the problems resolved by the method which Biot had supposed to be original with himself. When Biot read his paper to Laplace he was cautioned against certain inferences at the end which Laplace thought too remote. " Go not," he said, "beyond the results which you have actually obtained. You will probably meet difficulties more serious than you suppose : the actual state of analysis cannot furnish you the means of surmounting them." And Biot struck out his hazardous inferences. It now appeared that Laplace had been arrested by the same obstacle which he had signalized to Biot. Hoping to surmount it later, he had said nothing about it to any one, not even to Biot, when he came to bring him his own work as if it were a novelty. Biot does homage to the abnegation of Laplace in allowing him to make his communication without the consciousness of having been anticipated. Laplace would allow no allusion to be made to the trans- action when Biot's paper was printed. No mention of it appears in the records of the Academy. Not until after fifty years did Biot feel at liberty to mention it. " This discovery, the first I had made, was everything for me. It was little for him who had made so many. Would he always have been so just? Would he be so generous to a rival ? I have no occasion to examine that here. He was all this for me, and for many others who began their career in this way." Biot has described the country-seat of Laplace in Arcueil, adjoin- ing that of the eminent chemist, Berthollet. " It was acquired by him in 1806, two years after the Emperor, Bonaparte, had promoted him to the first dignities of the Senate. He bought it without having seen it, on the report of Madame Laplace, being contented to know that it was adjacent to that of his friend Berthollet. A simple garden wall separated them. Berthollet had cut an opening in it and placed a gate there before Laplace arrived. Then he came to receive him with ceremony at the boundary of their domains, bringing the keys which would give them free access to each other. It was in this de- licious retreat that Laplace spent every day, every moment, of liberty that his business left to him, — not to give himself to indolent repose, but to continue, with unwearied passion, his great labors on mathe- matical physics and the system of the world, emerging from these meditations only to converse with his friend on physics and chemistry. Here he also welcomed a retinue of zealous young men, whom he condescended afterwards to call his colleagues, and who always were proud of this association. Around him, in a more elevated sphere, were seen continually Berthollet, Lagrange, Cuvier, etc., to whom he introduced his vouug proteges. Here Laplace died, on March 5, 1827. OF ARTS AND SCIENCES. 189 His last words were, ' Ce que nous connaissons est peu de chose ; ce que nous ignorous est immense.' This sanctuary of sciences has been preserved, with a religious respect, by Madame Laplace, to whom it belongs to-day (1850). The house, the gardens where he walked, are as they were then. The study in which he composed so many noble works remains untouched, with the same furniture and books that served him iu the state in which he left them. He alone is wan tin sr, to the profound regret of those who knew him and will never see his equal." If we turn from this attractive picture of the domestic and scientific life of Laplace to his public career, the contrast is not pleasant. Liv- ing in the most disturbed period of France, he managed to keep him- self always iu the ascendency. After the coup d'etat of Napoleon, in 1799, his republican ardor was replaced by devotion to the First Consul. But his incapacity as Minister of the Interior led to his re- moval in six weeks. It was charged against him that he brought into his administration the principles of the infinitesimals. As a consola- tion, he was given a place in the Senate, of which he was made Chan- cellor in 1803. He was also Grand Officer of the Legion of Honor. On the erection of the Imperial throne, in 1804, he was made a Count. In 1814, he gave his voice for the Provisional Government, the deposition of Napoleon, and the restoration of the Bourbons. Louis XVIII. rewarded him by a seat in the Chamber of Peers, and in 1817 by a Marquisate. The first edition of the Exposition du Sjjsteme da Monde was in- scribed to the Council of Five Hundred. The third volume of the Mecanique Celeste, published in 1802, was a tribute to the Pacificator of Europe. In the edition of the Theorie analytique des Probabiliies, published after the restoration, the dedication to the Emperor in an earlier edition was suppressed. Bonaparte recognized the splendor which the great intellect of Laplace shed upon his administration. On October 19, 1801, ha\ received a volume of the Mecanique Celeste, he wrote to the author: "The first six months at my disposal will be employed on your beauti- ful work." On November 26, 1802, after reading some chapters <>f a new volume dedicated to himself, he refers to "the new occasion for regret that the force of circumstances had directed him to a career which led him away from that of science. At least, he added, I de- sire ardently that future generations, reading the Mecanique Celeste, should not forget the esteem and friendship I have borne to the au- thor." On June G, 1805, the General having become Kmperor. he 190 PROCEEDINGS OF THE AMERICAN ACADEMY wrote from Milan : " The Mecanique Celeste seems to me called to give a new splendor to the age in which we live." On August 12, 1812, he wrote from Witepsk: "There was a time when I should have read with interest your Traite da Calcul des Probabilites. To- day, I must limit myself to testifying to you the satisfaction I experi- ence every time I see you communicate new works which perfect and extend the first of the sciences and contribute to the glory of the nation. The advancement and perfectionatiou of mathematics are bound to the prosperity of the state." Arago did not imitate the political subserviency of Laplace, much as he admired his genius. In early life he went to Spain with Biot, to complete a geodesic operation. This expedition, though full of adven- ture and danger, had a successful issue, by giving a more precise value to the magnitude of the earth. On his return he was made a member of the Paris Academy when scarcely twenty-three years old. His sci- entific career was brilliant, and in 1830 he replaced Fourier as Perpet- ual Secretary. In 1 848 he espoused the cause of the second republic, with Louis Bonaparte as President. After the second coup d'etat, he refused to take the oath of allegiance to the new government, required of all officials. Nevertheless, he was allowed to retain the post of as- tronomer in the Bureau de Longitude, the new Emperor " making an exception in favor of a savant whose works had thrown lustre on France, and whose life his government would regret to embitter." As Minister of the Marine, Arago had originated and carried an act for abolishing slavery in the French colonies. Being urged to delay the change and make it gradually, he declared, " I will not postpone till to-morrow an act which sets free the oppressed." Poisson was of humble origin, but rose to be Peer of France. He befriended Arago, who was five years younger, and who describes him in his youth as of delicate complexion, slight figure, and childish man- ner. At the age of eighteen, he submitted to his teacher, Lagrauge, some amelioration in the method of demonstrating the binomial the- orem, which his teacher read publicly in his lectures, and said he should adopt. Laplace wished to know a geometer who had made such a beginning. Poisson was one of the earliest and the most powerful in applying Fourier's definite integrals and periodic series to physical problems. He extended the conclusions of Lagrange and Laplace on the stability of the solar system, adding millions of years to its probable duration. As there was no vacancy in the French Academy in his proper section, he was placed in that of Physics. Afterwards much of his work was upon physical problems, such as OP ARTS AND SCIENCES. 191 electricity, magnetism, and capillarity. By common consent, he stood at the head of European analysts, after the death of Laplace, whom he succeeded as geometer in the Bureau de Longitude. The publication of Dr. Bowditch's great work, a translation of four volumes of Laplace's Mecanique Celeste, with an ample commentary, was heralded by an article which he wrote for the North American Review in 1820. After describing the works of Olbers and Gauss in mathematical astronomy, the three principal publications of Laplace, and especially his discovery of the great equation in the motions of Jupiter and Saturn, with its long period of 917 years, and the neglect by men of science in Great Britain of the vigorous science upon the Continent, he thus expresses his admiration of Laplace: "These dis- coveries, together with a multitude of improvements in analysis and in every branch of mathematical knowledge, place this immortal man far above any of his contemporaries in the walks of science."* Fourier had called Laplace's works the Almagest of the eighteenth century. Professor John Playfair, having alluded to the absence of diagrams and geometrical figures in the writings of the great mathematicians of France, says : " If we come to works of still greater difficulty, such as the Mecanique Celeste, we will venture to say that the number of those in this island who can read that work with any tolerable facility is small indeed. If we reckon two or three in London and the mili- tary schools in its vicinity, the same number at each of the two English Universities, and perhaps four in Scotland, we shall not hardly exceed a dozen : and yet we are fully persuaded that our reckoning is beyond the truth." t On the appearance of the first volume of Bowditch's translation, a writer in the London Quarterly Review expresses his admiration in these words : " The idea of undertaking a translation of the whole Mecanique Celeste, accompanied throughout with a copious running commentary, is one which savors, at first sight, of gigantesque, and is certainly one which, from what we have had hitherto reason to con- ceive of the popularity and diffusion of mathematical knowledge on the opposite shores of the Atlantic, we should never have expected to have found originated, or at least carried into execution, in that quarter. Meanwhile, the part actually completed (which contains the first two books of Laplace's work) is, with few and slight excep- tions, just what we could have wished to see, — an exact and careful * North American Review, 1820, vol. x. pp. 200-272. t Edinburgh Review, 1808, vol. xi. p. 281. 192 PROCEEDINGS OF THE AMERICAN ACADEMY translation into very good English, — exceedingly well printed, and accompanied with notes appended to each page which leave no step in the text, of moment, unsupplied, and hardly any material difficulty of conception or reasoning unelucidated." Referring to the continu- ance of the work, the writer adds : " Should this unfortunately not be the case, we shall deeply lament that the liberal offer of the Ameri- can Academy of Arts and Sciences to print the whole at their expense, was not accepted.." * In 1888, after three volumes of the translation and commentary had been published, a writer in the London Athenaeum expresses himself in these words : " Dr. Bowditch rose, like Franklin, from humble life, and had much to struggle with, and did struggle man- fully, and did succeed. He was, iu other words, an illustrious instance of a self-educated man. . . . No matter what a man's facilities may be, without this (the possession and use of the appropriating and in- corporating power) he can never be educated, any more than he can be healthy without sound bodily organs. " The lack of facilities is not, however, to be spoken of lightly, though it must not be confounded, nor yet compared, with the lack of the power that uses them: nor must it be supposed that such a thing as an absolute lack of facilities can exist. Nature herself has provided facilities, food for education, materials for self-making men to rise up, in times and places when and where no other facilities may be had. She opens the great school-room of creation for them. She gives them homes, society, the world at large. Above all, she gives them eyes to see, and ears to hear, and an all-availing and available spirit within them : the intellectual, immortal instinct, the thirst for knowledge, and the faculty of finding it, in earth, and air, and sea. No loads of appliances can surfeit such a mind on the one hand ; no lack of them can starve it on the other. " Let us not be supposed, then, to use the words as abusing them, when we call Dr. Bowditch an illustrious instance of a self-educated man. He was, in other words, as we understand it, an educated man : his intellect informed and trained, his character seasoned and consummated, and this under those circumstances of extraordinary self-dependence, which, it is well known, are so admirably suited to bring out and give their finest play to minds of a high order, on the very same principle that they prove fatal to weaker ones. . . . " Dr. Bowditch's great scientific work — the one on which his * Quarterly Review, vol. xlvii., 18o2, pp. 558, 559. OP ARTS AND SCIENCES. 193 European reputation rests and will rest — was a translation of the Mjfanique Celeste of Laplace, accompanied with an extensive explan- atory commentary, making a work, which existed uue may say in mere abstraction before, as accessible to all public and popular pur- poses as its essential nature would permit." * Dr. Bowditch's work was not that of a mere translator and com- mentator. The subject was brought down to the date of publication, and was illustrated by the labors of geometers and astronomers who had succeeded Laplace. Such mathematicians as Lacroix, Legendre, Bessel, and Puissant recognized the great value of these additions. 3Ir. Babbage, in a letter to Dr. Bowditeh, under date of August 5, 1832, wrote: "It is a proud circumstance for America that she has preceded her parent country in such an undertaking ; and we in Eng- land must be content that our language is made the vehicle of the sublimest portion of human knowledge, and be grateful to you for rendering it more accessible." Letters of similar import were received by Dr. Bowditeh from Airy, Francis Baily, Herschel, the Bishop of Cloyne (Dr. Brinkley), and Cacciatore. The Council of the Royal Astronomical Society of London, f in noticing Dr. Bowditch's commentary and notes upon Laplace, ex- presses its appreciation in these terms : " An expert mathematician would find most of them {the notes) useless ; but to the student who has sufficient knowledge to understand, without the habit of previous investigation which the reading of Laplace always requires, the work of Dr. Bowditeh is invaluable. We see in it, not the performance of a practised analyst, but the record of the steps by which the trans- lator became one ; and a person more familiar with the most modern form of analysis than he appears to have been at the time when he wrote would probably have filled his commentary with difficulties of the same order as those of his author. This, however, was not done ; and the work, as it stands, is most unquestionably fitted to bring the Mtcaniqne Celeste within the grasp of a number of students exceed- ing five times, at least, that of those who could master Laplace by themselves. "The name of Dr. Bowditeh must be long remembered in tin' United States by the impulse which such a work as his commentary cannot fail to give to analysis in that country. The undertaking re- quired sound knowledge, power of combining brevity and clearness, * London Athenaeum, 1838, pp. 451, 452. t Memoir?, vol. xi. pp. 300, 301. vol. xxiv. (k. s. xvi.) 13 194 PROCEEDINGS OF THE AMERICAN ACADEMY an accurate remembrance of the nature of a beginner's difficulties, and determined perseverance. The congratulations which this soci- ety would so cordially have offered to the performer of this strikingly useful task can now only be forwarded, with expressions of sympathy and condolence, to his surviving relatives and friends ; with the hope that astronomy, theoretical and practical, will flourish in the country which has produced so remarkable a facilitation of the study of the former, and so sound an example of the union of both." In a note to the memoir of Dr. Bowditch by his son, it is stated that in America two, and perhaps three persons, besides Dr. Bow- ditch, were able to read the original work critically; but a compe- tent judge has doubted whether the whole of it had been so read even by one. It is also known, on the authority of his son, that Dr. Bowditch was gratified whenever he received assurances that his work had made Laplace accessible to young students. — more even than he was by the approbation of his peers. Benjamin Peirce, who was born in Salem, Mass., in 1809, and died at Cambridge in 1880, and who was Professor of Mathematics or Astronomy for forty-seven years, enjoyed the most intimate social and scientific relations with Dr. Bowditch. How these relations originated we are told by the writer of his obituary notice prepared for the American Academy of Arts and Sciences.* " In his early years he had the good fortune to come under the influence of Dr. Nathaniel Bowditch. It is said that their first ac- quaintance was made while Dr. Bowditch's son, Ingersoll, and young Peirce were schoolmates. Ingersoll showed his comrade a solution which his father had prepared of a problem that the boys had been at work upon. Some error, real or conceived, was pointed out in the work, which was reported by Ingersoll to his father. ' Bring me that boy who corrects my mathematics ! ' was the invitation to an acquaint- ance, the importance of which, in Professor Pierce's own estimation, is told in the dedication, more than thirty years later, of his Analytic Mechanics : ' To the cherished and revered memory of my Master in Science, Nathaniel Bowditch, the father of American Geometry.' "Peirce entered Harvard College in 1825. As Dr. Bowditch was now in Boston, having removed from Salem in 1823, and was pre- paring the first volume of his translation of Laplace's Mecanique Celeste for the press, it followed almost as a matter of course that the college student was more influenced in his studies by him than by * Proceedings, vol. xvi. pp. 443, 444. OF ARTS AND SCIENCES. 195 the college course. Dr. Bowditch's first volume was completed, and the second entered for copyright, in 1829, the year of Peirce's gradu- ation ; and the proof-sheets were regularly read hy him." * That it should have been left to this country to open a way to English- speaking nations for the study of the transcendental mathe- matics of France and Germany may be explained by the following lamentation of the younger Herschel, printed as late as 1845. f After acknowledging the celerity with which everything valuable in British journals is republished, examined, and criticised in those on the Conti- nent, he writes : — " This ought to encourage our men of science. They have a larger audience, and a wider sympathy than they are, perhaps, aware of; and however disheartening the general diffusion of smatterings of a number of subjects, and the almost equally general indillerence to profound knowledge in any, among their own countrymen, may be, they may rest assured that not a fact they may discover, nor a good experiment they may make, but is instantly repeated, verified, and commented upon in Germany, and we may add too in Italy. We wish the obligation were mutual. Here, whole branches of Conti- nental discovery are unstudied, and indeed almost unknown even by name. It is in vain to conceal the melancholy truth. We are fast dropping behind. In mathematics we have long since drawn the rein, and given over a hopeless race. In chemistry the case is not much better." At the present day Great Britain no longer lies under this sev reproach. In pure mathematics there have been Boole, Hamilton, Cayley, H. J. S. Smith, Clifford, and Sylvester; and in applied mathematics, Adams, Stokes, Sir William Thomson, Lord Rayleigh, Challis, and Powell. But the highest mathematical faculty will be always the prerogative of the few. Not many can say with Lagrange, " I found chemistry as easy as algebra ! " The contrast is not less striking in this country between the pre* condition of mathematical taste and acquirement and what they were at the time of Bowditch's translation. This change has been lai * In the memoir of Dr. Bo wd itch by his son it is said : " Whenever hundred and twenty pages were printed, Dr. Bowditch had them bound in a pamphlet form, and sent them to Professor Peine, who, in this manner, the work for the first time. lie returned the pages with the list of errata, which were then corrected with a pen or otherwise in every copy of the whole edition." t On Sound. Encyclo Metropolitan a, vol. iv. p. 810 196 PROCEEDINGS OF THE AMERICAN ACADEMY due to the example and inspiration of Peirce. Though he was a poor teacher for indifferent students, he was the best for superior intellects. He simply led, and charmed them into following him as far and as fast as they could. While his text-books were an enigma to those who had little mathematical capacity, they fascinated minds of the highest order in this direction. Hence, in every class in college, a very few were found competent to read Bowditch's version of Laplace, and obtain glimpses of the meaning of Peirce's ideal algebras. Observa- tories, the United States Coast Survey, the Nautical Almanac, the Smithsonian Institution, and schools of science exist, partly as cau!-e and partly as effect of this new development. Bowditch's Practical Navigator, first published in 1802, has carried his name, long ago, over every ocean and into every port in the civilized world, and his scientific reputation, as the earliest American expounder of the higher geometry, is slowly following after. The four volumes of Dr. Bowditch's Translation and Commentary were published successively, in 1829, 1832, 1834, and 1839, at the sacrifice of one quarter of hi whole property. The expense was largely increased by the \ oluminous commentary. This was really of the nature of an original work, and was rendered necessary by the frequent ^aps which Laplace had left in his own publication. Mr. N. I. Bowditch says, in his biography of his father, that Dr. Bowditch himself was accustomed to remark, " Whenever I meet in Laplace with the words, Thus it plainly appears, I am sure that hours, and perhaps days, of hard study will alone enable me to discover how it plainly appears." The attention of Mr. James B. Francis of Lowell was attracted by the following passage in a recent work of W. W. R. Ball of London : " The Mecaniqne Celeste is by no means easy reading. Biot, who assisted Laplace in revising it for the press, says that Laplace him- self was frequently unable to recover the details in the chain of reason- incr, ai d. if satisfied that the conclusions were correct, he was content to insert the constantly recurring formula, 11 est aise a voir." * Mr. Ball refers to the Journal des Savants, February, 1850. Mr. Francis has found the volume in the Boston Public Library. The title of the paper, translated, is, " An anecdote relating to Laplace : read to the French Academy at its special session, on February 5, 1850, by Mr. J. B. Biot." I find that Biot reprinted the paper in 1858, in his Melanges Scientijiques et Litteraires. As Mr. Francis * A Short Account of the History of Mathematics. London, 1388, p. 387. OF ARTS AND SCIENCES. 197 has been at the pains of obtaining a translation of the paper by a lad v. I shall adopt that with a few trifling changes. " When a man of order prepares to depart on a long journey, he arranges his affairs, and is careful to discharge all the debts he may have contracted. This is why I am going to tell you how, some fifty years ago, one of our scientists, the most distinguished, received and encouraged a young debutant who had come to show him his first attempts. " This young debutant was myself, with your leave. Notice, to excuse the epithet, that this goes back to the month Brumaire of the year VIII. of the French republic, first edition.* Some months later, they did me the signal honor of electing me an associate of the Na- tional Institute ; but at that date, and especially at the little earlier period when my story begins, I found myself completely unknown. I was then quite a small professor of mathematics in the Central School of Beauvais. Having recently left the Polytechnic School. I had much zeal and less science. At that time, little was demanded of young men but zeal. I was impassioned for geometry and many other things. Fortune rather than reason saved me from yielding to tastes too diverse. Bound from that time by the sweetest ties to the interior of the family which had adopted me, happy in the present and counting on the future, I only thought of following with delight the bent of my mind towards all kinds of scientific studies, and of doing for pleasure what the interest of my career would have prescribed to me as a duty. I had, above all, an unbounded ambition to penetrate into the high regions of mathematics, where men discover the laws of the universe. But these grand theories, still scattered in the collections of academies, were almost unapproachable, except to a small number of superior men who had co-operated in establishing them; and to launch into them without a guide over their footsteps, this would be an enterprise in which one would have every chance of wandering for a long time before rejoining them. I knew that Laplace had labor* A in unifying this magnificent ensemble of discoveries in the work which he has very justly called the Mecanique Celeste. The fust volume was in press ; the others would follow, at long intervals, agreeably t ■< my desires. A step which might appear very hazardous opened t.i me a privileged entrance into this ?anctuary of genius. I ventured 10 write directly to the illustrious author, ami beg him to permit liis * Brumaire began in 1790 on October 23: Biot was then twenty-five .years ol 1. 198 PROCEEDINGS OP THE AMERICAN ACADEMY publisher to send me the sheets of his book as they were printed. Laplace replied to me with no less ceremony than if I had been a real savant. However, as the end of the story, he refused my request ; uot wishing, he said, that his work should be presented to the public 1 efore it was completed, that it might be judged as a whole. This polite refusal was doubtless very obliging in its form ; but, at bottom, it badly suited my business. I was not willing to accept it without appeal. I immediately wrote again to Laplace to represent to him that he did me more honor than I merited, and than I desired. I am not, I said to him, of the public who judge, but of the public who study. I added, that, wishing to follow and make again all the calcu- lations throughout, for my own instruction, I might, if he yielded to my request, discover and indicate the errors of press which may have slipped into them. My respectful persistence disarmed his reserve. He sent to me all the sheets already printed, adding thereto a charm- ing letter ; this time not at all ceremonious, but filled with the most lively and precious encouragements. I need not say with what ardor I devoured this treasure. I could well apply to myself the maxim, Violenti rapiunt Mud. " After this, every time I went to Paris, I carried my work of typo- graphical revision, and presented it in person to M. Laplace. He re- ceived it always with kindness, examined it, discussed it ; and that gave me an opportunity to submit to him the difficulties which too frequently baffled my weakness. His condescension to remove them was without bounds. But he himself could not always do it, with- out giving attention to them ; sometimes pretty long. That happened usually in places where, to save himself from the details of a too ex- panded exposition, he had employed the expeditious formula, // est aise de voir. The thing, in fact, had appeared at the moment very clear to his eyes. But it was not so always, even for him, some time after- wards. Then, if you asked him the explanation of it. he sought it patiently, by different ways, on his own account as well as yours ; and there was, without doubt, the most instructive of commentaries. Once I saw him pass almost an hour trying to seize again the chain of rea- soning which he had concealed under this mysterious symbol, 11 est aise de voir. It must be said, for his acquittal, that if he had wished to be completely explicit, his work would have required eight or ten quarto volumes instead of five ; and perhaps he would not have lived long enough to finish it." These minute details relating to the intellectual life of Laplace, so sacredly preserved by Biot, the eminent mathematician and physicist, OF ARTS AND SCIENCES. 199 were not published until twenty-three years after the death of Laplace, and twelve years after the death of Bowditch. Tliey must be taken into account when the mathematical powers of the author of the Me- canique Celeste and of its translator and commentator are compared. There can be no doubt that a higher order of mind is demanded for originating a profound analysis, than for understanding it when it is once made. Dr. Bowditch said to one of his sons : " My order of talent is very different from that of Laplace. Laplace originates things which it would have been impossible for me to have originated. Laplace was of the Newton class ; and there is the same difference between Laplace and myself as between Archimedes and Euclid." This confession, taken in connection with Bowditch's estimate of Euclid, erred on the side of excessive modesty. Eor he was able not only to detect and point out to Laplace accidental errors in his work, but to provide an original commentary upon it more volumi- nous than the work itself. If this required a great expenditure of time and thought, it was no easy matter for Laplace himself. It was, in fact, so hard, that Laplace was not willing to undertake it a second time, after the subject had passed out of his mind ; and he left the abyss open, with no stronger bridge to cross it than the simple for- mula, 11 est aise de voir. The circumstances under which Laplace and Bowditch did their work are in striking contrast. Laplace was a favored child of for- tune. He was able to give his long life of seventy-eight years to his noble task, breathing an intensely intellectual atmosphere, and surrounded by men of science only a little less distinguished than himself. Bowditch's knowledge of affairs was as remarkable as his science. He was weighted all his life with heavy cares and trusts, and could spare only his hard-earned leisure for scientific work, dying at the age of sixty-five. His intellect worked on a solitary height, admired but not fully comprehended by those about him. For example, instruction, and inspiration, he did as much for science in America, and wherever the English language is read, as Lapli did for that of France. It would be unjust to his memory, and to his own great modesty, to make any other comparison. No names more illustrious adorn the two original branches ol membership in this Academy than those of Laplace and Bowditch. Laplace was elected a Foreign Honorary Member in 1822, when he had published only four volumes of the Mecanique I 'eleste. Bowditch became a Resident Fellow in 1799, fifteen years before he had begun his translation of Laplace's greatest work. He contributed twenty- » 200 PROCEEDINGS OF THE AMERICAN ACADEMY three valuable papers to the Memoirs, chiefly on Astronomy and the Physics of the Globe. Having succeeded John Quincy Adams as President of the Academy in 1829, he died in office, in 1838. An elaborate eulogy was pronounced before the Academy, May 29, 1838, by Mr. John Pickering, the Corresponding Secretary. After the death of Laplace, his widow recognized the value of Rowditch's labors, in extending the usefulness and enlarging the fame of her husband's greatest work, by presenting to his translator and commentator his marble bust. In the fourth volume of the last edi- tion of Laplace's work, fifty-two corrections are specified as having been made by Dr. Bowditch. Dr. Bowditch's strength held out until he had corrected the proof- sheet of the thousandth page of the fourth volume of his translation. That was the last page his eye was to rest on. Eighteen more pa^es remained. The incident has its parallel in the death of Copernicus. He had spent twenty-three years in writing his book De Orbium Ccelestium Revolutionibus, but delayed its publication for fear of a popular outcry against his scientific doctrines. The book had been printed at Nuremberg under the care of his disciple, Rheticus. A few hours before he died, a copy arrived which was placed in his hands. He touched it, and seemed to recognize it, and then relapsed into unconsciousness. No less suggestive was the death-bed of Lagrange. Though of French extraction, he was born in Turin in 1736. His father lost his property in speculation, — an event which the son did not regret. " Had 1 been rich," he said, " I might never have known mathemat- ics." At the age of twenty-six, Lagrange had reached the summit of fame, though at the sacrifice of his health. In 1766, he was brought to Berlin by Frederick the Great, " the greatest king in Europe wishing to have the greatest mathematician at his court." After- wards, various other courts competed for him. In 1787, he selected Paris. He was patronized by Marie Antoinette, and lodged in the Louvre. In the Revolution, when other scientific men were victims, his name commanded respect. In reply to a petition in favor of Lavoisier it was said, " The republic has no need of savants." Bona- parte called Lagrange " La haute pyramide des sciences mathema- tiques," and loaded him with offices and distinction. The first edition of his Mecanique Analytique appeared in 178S. In 1811, he pub- lished the first volume of another edition. The second volume, which was on Dynamics, required more serious changes, and its preparation was too much for his failing strength. On April 8, he had a conver- OP ARTS AND SCIENCES. 201 sation with Monge and other friends, and looked forward to another early interview, when he would complete some autobiographical de- tails. But what he intended to say was never spoken. He died two days afterwards, and was buried in the Pantheon. Only one Fellow of this Academy is now living who was elected before the death of Dr. Bowditch ; and there must be very few in its present membership who knew him or ever saw him. But his work and his reputation are their common inheritance. To keep alive his memory, and do justice to his gigantic undertaking, is the loving ser- vice of one who, in early life, was welcomed to the hospitality of his thoughts and his books. 202 PROCEEDINGS OF THE AMERICAN ACADEMY XVIII. CONTRIBUTIONS FROM THE CHEMICAL LABORATORY OF HARVARD COLLEGE. ON A NEW METHOD OF DETERMINING GAS DENSITIES. By Josiah Parsons Cooke. Presented June 12, 1889. In the well known method employed by Regnault for determining the density or specific gravity of air, oxygen, nitrogen, hydrogen, and carbonic acid, we deal primarily with tares, of which the weights to be determined are the differences. The glass balloon which holds the gas is tared by a similar balloon of exactly the same volume and of nearly equal weight, suspended from the opposite pan of the balance. The small difference of weight required to establish perfect equilibrium is alone measured with standard brass or platinum weights. What- ever may be the form of the subsequent calculation, the primary ob- ject is to obtain the tare of the empty balloon when absolutely vacuous. This known, the differences between such tare and the tare of the balloon filled with various aeriform substances, gives the weights of equal volumes of these substances under the temperatures and pres- sures at which the balloon was filled. The volume of the counter- poise is exactly adjusted to that of the balloon by the aid of a small subsidiary glass bulb (Plate II.) ; and by sealing up more or less mer- cury in this bulb it is easy to make the difference of weight such that the standard weights required to complete the equilibrium will measure tlie differences of tare to be determined, and no more. In the method of Regnault the tare of the empty balloon, or what was equivalent to it, was found by exhausting the balloon with an air-pump and weighing it after measuring the tension of the residual gas while the glass was surrounded by ice. But it has been shown by Agamennone * and Lord Rayleigh ,f that the results thus obtained are * Atti (Rendiconti) d. R. Accad. dei Lincei, 1885. i Proceedings of the Royal Society, vol. xliii. p. 362. 1888. OF ARTS AND SCIENCES. 203 vitiated to a small extent by the circumstance that when the balloon is exhausted the pressure of the atmosphere determines a slight shrink- age of the external volume, which naturally disturbs the exactness of the compensation between the buoyancy of the air on the balloon and on its counterpoise. Although this shrinkage can be readily meas- ured, as was done by Dr. T. W. Richards under my direction,* and still more recently by Professor Crafts, t who experimented on the balloon used by Reguault, which fortunately has been preserved, it seemed de- sirable to develop a method by which this correction could be avoided. For even if the new method should lead to no more accurate results than before obtained, it might serve to confirm the validity of the cor- rection iu question, and at least would gi\e additional data towards establishing the value of important physical constants. The new method we have devised for the purpose consists in first taring the balloon when filled with carbonic acid gas, and then drawing the gas through absorption tubes and determining its weight, as in the well known method of organic analysis. This weight known, the tare of the empty balloon is obviously the difference between the first tare and the weight in question. The practical problem here presented is, however, far more difficult than that of organic analysis. In the last, we expect to determine the weight of only a few decigrams of car- bonic acid within a few tenths of a milligram, while in the problem now before us we must weigh at least nine or ten grams of carbonic acid, not simply to a proportional, hut to an equal, degree of accuracy. We only succeeded in securing such accuracy after many trials and a careful study of all the conditions involved, and our primary object in this paper will be to describe the precautions which are essential to the success of the new experimental method. Incidentally it will appear that our results confirm in a most striking manner the high value of the specific gravity of hydrogen found by Lord Rayleigh,± and the low value of the atomic weight of oxygen found by ourselves. The Balance and Weights. The balance and weights were the same as those used by us in our previous work.§ The disposition of the apparatus whirl., after many trials, we have found most suitable for accurate work, is shown in * The.-e Proceedings, vol. xxiii. p. 177. 1888. t Comptes Rend us, vol. cvi. p. 16G'2. 188b. j Proceedings of the Royal Society, vol. xlv. p. 426. 1889 § These Proceedings, vol. xxiii. p. 159. 1* 204 PROCEEDINGS OF THE AMERICAN ACADEMY Plate II. The balance rests on the plank shelf of a wooden case, whose glazed doors are shown open in the drawing ; and as this shelf is firmly secured to a thick brick partition wall behind, great steadiness is secured for the instrument. Around the iuside of the wooden case are hung folds of drapery, which surround the balance case and protect the beam from radiations, while a curtain rolling on a spring fixture enables the experimenter to uncover the front as necessary. Fastened by flanges and screws to the under side of the same shelf is a box, made of tinned sheet iron, of somewhat larger dimensions than the balance case. The front of this box can be almost wholly uncovered by means of two large doors made of the same metal sheet, and se- cured when closed by turning buttons, but shown open in the draw- ing. In the metal top are two circular holes about half an inch in diameter, corresponding to holes through the shelf and the base of the balance case, and directly under the centres of the balance pans. From hooks soldered to the under side of the pans the globe and its counterpoise are suspended by means of brass wires, and the lengths of the wires are so adjusted that the two glass vessels shall hang mid- way in the metal box. The globe is hung from a wire stirrup, Plate I., which swings from an eye at the end of one wire; while on the neck of the counterpoise is cemented a brass cap and hook, and both it and the small subsidiary bulb are hung on an eye at the end of the other wire. Of course these details might be varied. It is only important that the whole system should swing freely, with as little friction as possible, and that the balloon should be easily removed and replaced. Through a third hole in the top of the metal box and shelf, placed just in front of the balance case, passes a thermometer (not shown in the drawiug) by which the temperature may be watched, and the in- side of the box is painted with lamp-black so as to secure a uniform temperature throughout the interior. In our previous paper we spoke of the disturbance sometimes caused by currents of air within the box, but we found on further experience that these currents could be pre- vented by keeping the interior of the box as nearly as possible at the temperature of the external air. For this purpose it is important that the air of the room should circulate as freely as possible around the box, and the required condition is more easily secured if the box is made of thin metal sheet. It is also important that the temperature of the room should not be constantly changing, and that all circum- stances should be avoided which would cause a flow of heat either into or out from the box. Sitting in front of the box in the process of weighing immediately causes a disturbance, and hence the division of OF ARTS AND SCIENCES. 205 the outer wooden case below the shelf is provided with wooden doors, which should be shut in front of the metal box before approaching the balance. When the thermometer hanging with its bulb inside the box indicates the same temperature as one hanging from the balance case outside within one tenth of a centigrade degree, the conditions are most favorable for accurate weighing. In order to maintain the atmosphere within the box in a constant hygrometric condition, we placed in it four large open dishes of sul- phuric acid, two on the bottum of the box and two on a shelf near the top, as described in our previous paper. The acid was first boiled with a fraction of a gram of amnionic sulphate, to remove the last traces of nitrous fumes, and renewed as occasion required. ■ We have found that we can most accurately estimate slight differ- ences of weight with a balance thus loaded by observing the amplitude of the first swing of the pointer when the pans are relieved. With the balances of Becker, after the beam has been set on its bearings by the usual cam motion, the pans are still supported by two delicate arms, which are held by a weighted lever against the under side of the pans, but which can be pressed down by pushing against the button shown in the drawing on the front of the balance case. Such a mechanical arrangement is peculiarly adapted to this method of weighing, as it relieves the pans suddenly and under the same conditions, so that the amplitude of the subsequent swing is an accurate measure of the differ- ence of weight acting at the two ends of the balance beam ; and in this case the inertia of the heavy load renders the effects surprisingly uniform. We give these details, not because they involve any new principles, but because the results have been reached after a long se- ries of experiments, and our experience may save others much loss of time. With the apparatus arranged as we have described it, a dif- ference of weight amounting only to one tenth of a milligram was distinctly indicated, although the load exceeded half a kilogram on each pan, and the compensation was made so perfect that the equilibrium was not perceptibly altered by any ordinary changes of atmospheric conditions. In order to reach such compensation, a counterpoise is first select" . 182. 208. PROCEEDINGS OP THE AMERICAN ACADEMY inside a second cylindrical vessel of the same material, leaving an an- nular space about two inches wide and an equal space between the bottoms of the two vessels, all of which is filled with water. In addi- tion, the water vessel is further protected by a layer of felt one inch thick kept in place by an outer covering of the same sheet metal. When in use, the top is covered by a cap made also of thick felting, and in the crown of the cap is a slit, through which a thermometer may be inserted or the hand passed to turn the stop-cocks. The gas to be used is conducted into the calorimeter through a very small lead tube, which is connected with the lower tubulature of the stop-cock by a rubber connection, and the balloon is so placed that the current shall enter either at the top or at the bottom of the vessel, according as the gas is lighter or heavier than the atmosphere. The calorimeter case stands about four feet high, and the balloon rests in it on a down cush- ion, with the connecting tube's fully six inches below the surface of the water in the annular space above mentioned. "With this apparatus it was possible to keep the temperature of the balloon constant within the one hundredth of a centigrade degree for an hour at a time, unless the temperature of the laboratory suddenly and greatly changed. The general arrangement for filling the balloon was then as follows. The gas delivered from the drying tubes of one of the generators here- after to be described passed through the lead tube of which we have spoken to one or the other, as the case might be, of the tubulatures of the balloon standing in the calorimeter. Passing out by the opposite tubulature, the current was conducted by a similar lead tube to a second but much larger balloon serving as a gasometer, and from the last vessel through a gas wash-bottle to the atmosphere. The bottom of the wash-bottle was covered with strong sulphuric acid to dry any returning air, but not deep enough for the inlet tube to dip under the liquid. The current was continued until the proper test showed that the gas issuing from the end of the apparatus was perfectly pure. Then the inlet cock of the balloon was turned, and the temperature of the calorimeter case watched until constant, and a sufficient time had elapsed to establish a perfect equilibrium with the atmosphere through the connecting tubes and vessels. This, as we found by experience, often requires longer time than we were led to anticipate, and when experimenting with carbonic acid gas it is not safe to allow less than twenty or thirty minutes ; and now the large balloon and wash-bottle come into play to prevent air diffusing into the balloon, or being drawn back in consequence of changing pressure. When all the conditions seemed to be satisfactory, the temperature OF ARTS AND SCIENCES. 209 of the calorimeter and the height of the barometer were accurately observed, the first to the hundredth of a centigrade degree and the last to the twentieth of a millimeter, noting always the height of the attached thermometer. The hand was then quickly thrust into the calorimeter, aud the outlet cock at once closed. The balloon was now removed, dusted with a large camel's-hair brush, and hung in its place on the balance. When, however, the atmosphere is very dry, as it often is in this climate during the winter months, it may happen that the surface of the glass acquires a charge of electricity from the fric- tion of the cushion in the calorimeter or of the brush just mentioued ; and if there is auy suspicion of such an effect, the best way to dissipate the charge is to stand the balloon for a few minutes in its metal case (shown in Plate III.), after covering the bottom of the case with a thin layer of water. If the balloon is hung on the balance with a charge of electricity on its surface, however small, it will be unequally attracted by the surrounding metallic walls, and most confusing anomalies ot weight will be noticed. Moreover, in the very dry atmosphere of the case the charge will last for days, or even weeks, as on the insulated vanes of an electrometer. Thermometers and Barometers, and their Correction. The thermometers on whose indications we have relied in this investigation are two of small range, but divided into fiftieths of a centigrade degree and made by the house of the late Dr. H. Geissler of Bonn. We were obliged to use the two, for our investigation was continued into summer weather, which exceeded the range of the ther- mometer first selected. As should always be the case with such in- struments, the zero point is given in each case on a short subsidiary scale, separated from the main scale by an enlargement of the tube. Careful observation showed that the zero point of the instrument we will designate as No. 1, was depressed 0.02 of a centigrade degree, while the zero point of No. 2 was raised 0.28 of a degree. Making the correction thus indicated, to be added to all temperatures observed with No. 1, and subtracted from all observed with No. 2, the two in- struments were found to agree exactly through all portions of the scale common to both. Obviously, therefore, the differences of tem- perature observed are perfectly trustworthy to the one hundredth of a degree, but how far the absolute values — counting from the freezing point of water — can be relied on when compared with the observa- tions of other experimenters, we have no means of determining. Of course, it will be understood that all temperatures hereafter given VOL. XXIV. (n. S. XVI.) 14 210 PROCEEDINGS OF THE AMERICAN ACADEMY have been corrected for the variation of the zero point. At the close of the investigation the zero points were again tested and found to be unchanged. The barometer used was a large standard instrument of the familiar mountain form, made by Greene of New York. Hanging at the side of it was a smaller instrument of the same maker, whose indications agreed with the first within the tenth of a millimeter. Here again, as in the case of the thermometer, there can be no question as to the ac- curacy of the differences of tension observed within moderate limits ; but how far the absolute heights can be compared with those observed by Regnault and others is also a problem that cannot be readily solved, and one not within the means of a single experimenter to determine. All heights of barometer given hereafter have been reduced to 0° by the tables of Guyot.* Tare op the Empty Balloon by Regnault's Method. In the method of experimenting devised by Regnault the tare of the empty glass globe used, although not explicitly given, was implicitly determined. His arrangement for filling the globe, shown by Figure 1, has already been referred to, and his general method of experimenting consisted in taking the tare of the globe when filled with the same gas at the temperature of melting ice under as different tensions as possible. The ten- sions were found by measuring with a cathetometer the difference of height, a ft (see Fig. 1), under each condition, and the tares were found by means of the balance by the system of compensation already de- scribed. The difference of tare gives the weight of gas which the globe contains at 0° at the tension H — h, and from this may readily be deduced the weight at any other tension ; as, for example, at the stand- ard tension of 7 GO mm. The calculated weight at either of the tensions H or h, deducted from the corre- sponding tare, gives what we have called the tare of the empty globe ; but obviously with Regnault's method this value is not needed in the calculations of specific gravity or density. Fig. 1. Published by the Smithsonian Institution, Washington. OF ARTS AND SCIENCES. 2 1 1 When the globe is filled by displacement it conduces to greater ac- curacy to determine independently the tare in question ; and as soon as the details of the new method had been worked out, we began our final determinations by taking according to the old method the tare of the balloon abovre described when empty, so as to obtain a definite standard of comparison for further results. We however varied the method of Regnault in so far that we always filled the globe with hy- drogen before exhausting the interior. As with this exceedingly light, material the weight of the residual gas seldom exceeded one half a milligram, an error as great as one fifth in the capacity of the bal- loon or in the tension of the residual gas would cause no appreciable difference in the value of the small weight we sought to estimate. The details of a single example will be sufficient to illustrate the procedure. Determination No. 1. A current of hydrogen gas from the electrolytic generator described in our previous paper * was run through the balloon from Saturday, May 25th, at 4 o'clock p. m., to Monday, May 29th, at 10 o'clock A. M., 1889, the balloon standing in calorimeter case connected with larger balloon to receive overflow. At moment of closing, the height of barometer and temperature of the case were observed, but these data are not required for the present determination, and will be given hereafter when used for calculating the specific gravity of hydrogen. The balloon was exhausted with an excellent mechanical air-pump, f and the tension of the residual gas measured by means of a siphon manometer interposed between the balloon and the pump. The form of manometer used is shown by Figure 2. It was made in the labo- ratory, and in filling it with mercury the liquid metal, purified by repeated distillation, was boiled in the tube with the greatest care. For convenience, the difference of level of the mercury in the two arms was measured with a cathetometer constructed by the Societe Genevoise, but it might have been estimated with sufficient accuracy by the millimeter scale of the instrument. Tension in balloon after exhaustion 456.95 — 455.55 = 1.40 mm. Assuming 0.4164 as the approximate value of the weight of hydro- gen gas filling the balloon at 763.10 mm. and 21°.08 C. (p. 227), the ht of the residual gas at 1.4 mm. and same temperature would be weig * These Proceedings, vol. xxiii. p. 1G8. t Author's Chemical Physics, p- 881. 212 PROCEEDINGS OF THE AMERICAN ACADEMY 0.00076 gram or 0.76 m.g. No exact observation of the temperature of the balloon was necessary ; for a difference of 4° C. would not alter the above value more than T£o m.g., and we may therefore assume that the temperature of the balloon was the same as that of the laboratory, Fig. 2. which at the time was 21° C. The correction for lessened buoyancy (increased weight) on account of the contraction of the balloon by atmospheric pressure amounts, as has been shown, to 1.98 m.g.,* and this added to 0.76 makes the total correction 2.74 m.g. When the balloon was hung on the balance, the weight required to complete the tare was 2.5600 grams. Hence we have, — Weight of balloon exhausted 2.5600 grams. Correction for residual gas . . . 0.76 m.g. " " lessened buoyancy . 1.98 " 27 " Tare of empty balloon 2.5573 " Two other determinations were made in the same way, and the three results are united iu the following table. * These Proceedings, vol. xxiii. p. 184. OF ARTS AND SCIENCES. 213 Summary. Tare of empty balloon, 1st value 2.5573 grams. " " " 2d " 2.5572 " « u 3d " 2.5574 " Mean value, 2.5573 " Take op the Empty Balloon by Chemical Method. The general theory of this method has already been stated. The balloon is filled with carbonic acid gas by displacement, and the tare taken. The gas is then drawn through a series of absorption tubes, as in the process of organic analysis, and the sum of the increased weights of these tubes gives the weight of the total contents of the balloon at the time the tare was taken. The weight of the balloon filled with carbonic acid gas less the weight of the carbonic acid thus determined is obviously the tare of the empty balloon required. In attempting to perfect this apparently simple experimental method we met with unexpected difficulties, arising from several circumstances. In the first place, in order to wash out from the balloon the last traces of carbonic acid, it was necessary to draw through the apparatus a very large volume of air, and the system of purifiers and desiccators needed absolutely to free the atmospheric air from the least admixture of carbonic acid or aqueous vapor was found to be far more extensive than we anticipated. In the second place, since the globe held, at the ordinary temperature of the laboratory and at the average pres- sure of the atmosphere, no less than nine grams of gas, the common potash bulbs used in organic analysis were wholly inadequate for our requirements, and we only succeeded after many trials in finding ;i form of apparatus by which so great an amount of carbonic acid could be determined with the necessary accuracy, that is, within a few tenths of a milligram. The arrangement finally adopted is shown in Plate III. The balloon is represented standing in its covered metallic case, in which it is placed the moment it is taken from the balance. On the right of the balloon and below it is a system of tubes tor purifying and drying the atmospheric air which enters from outside the laboratory by the flexible tube on the extreme right. On the left of the globe is a system of tubes for absorbing the carbonic acid. The flexible tube on the left is connected with a Bunsen pump through 214 PROCEEDINGS OF THE AMERICAN ACADEMY a form of Mariotte's flask,* and by this means a current is maintained through the whole system, under constant pressure. Purifying and Drying Apparatus. The air entering as we have described passed first through a wash- bottle of familiar construction containing a solution of potassic hydrate, Sp. Gr. = 1.44, and then through a similar wash-bottle containing a concentrated solution of baric hydrate ; and if the rapidity of the cur- rent was not greater than two bubbles a second, this double washing was found sufficient to remove the last traces of carbonic acid. Indeed, as soon as the baryta water showed the least indications of cloudiness, the solutions were renewed. It was not so easy to remove the last traces of moisture. After the air had passed the washing flasks it entered a system of desiccators, shown in the lower half of the plate, where in small bubbles it travelled up first one tube, and then a second tube, both 5t feet long, and filled with concentrated sulphuric acid previously boiled with a small amount of ammonic sulphate to remove all nitrous fumes. Leav- ing the second of these tubes it entered an elongated bulb four inches long by two inches in diameter filled with phosphoric anhydride ; and the fact that prolonged contact with sulphuric acid is not sufficient to remove the last traces of moisture was shown by the circumstance that after the current has passed for several days the dry white powder at the opening of the bulb showed signs of deliquescence. Our phosphoric anhydride was prepared by burning common yellow phosphorus in a large sheet iron drum, through which a current of dry air was drawn with sufficient rapidity to maintain the phosphorus in rapid combustion, and the bottom of the drum was made tunnel- shaped so that the anhydride could be shaken down into a self-sealing fruit jar as fast as it formed. As thus prepared the anhydride has a slight odor, which it loses after a prolonged current of dry air has been drawn through the powder ; and after our drying tubes had been filled their contents were submitted to a preliminary treatment of this sort, and not until long after all perceptible odor had disappeared were they used in our work. We noticed that after the anhydride had been used for some time it appeared more granular and lost in part its hygroscopic power. In order to make sure of this point, the apparatus as far as described having been in use for several weeks, we connected with the first phosphoric anhydride tube a weighed tube * These Proceedings, vol. xxiii. p. 163. OF ARTS AND SCIENCES. 215 containing fresh anhydride. After drawing air through the system at the same rate and during the same time as in a carbonic acid determination, we reweighed this second tube and found that it had gained 5.5 m.g. We next added to our system the U tube filled with phosphoric anhydride, which is shown in Plate III. immediately before the balloon, and repeated the experiment. There was then no gain in weight perceptible. The observations were as follows. Before interposing the U Tube. ■ ii ipO R 1st weight P205 tube 25.9212 grams 295.7 20.0 302.7 2d " " 25.9267 " 295.2 20.8 301.4 0.0055 " 1.4 After interposing the U Tube. 1st weight P2Os tube 25.9268 grams 299.3 19.6 306.7 2d " " 25.9268 " 299.2 21.6 304.6 2.1 In this table the column headed H contains the barometric pressure at time of weighing in tenths of an inch ; that headed T° gives the corresponding temperatures of the balance case in centigrade degrees. By adding to the values H the quantities (27 — T)° we obtain the values R, and these are the barometric heights which would give an atmosphere of the same density, and therefore exerting the same buoy- ancy, as the atmosphere at the time of weighing if the temperature were uniformly 27° C. The correction that should be made for differ- ences of temperature and pressure at successive weighings can at once be calculated from these values. We found by experiment that for the phosphoric anhydride tube used in these and in subsequent deter- minations the correction amounted to 0.04 m.g. for each tenth of an inch change of pressure, and hence in the above weighings the correc- tion is too small to be appreciable. This simple method of correcting weights for changes in the buoyancy of the atmosphere has been de- scribed in a previous paper in these Proceedings.* In order to apply it readily, the barometric heights, although usually read in millimeters, were often also noted, as here, in tenths of inches, and the instrument we used was provided with both scales. * Vol. xviii p. 55. 216 PROCEEDINGS OF THE AMERICAN ACADEMY It is obvious from the above experiments that the hygroscopic power of phosphoric anhydride becomes impaired before the powder actually deliquesces, and we have dwelt on the point because the ex- perience was of great importance in our investigation by leading us to add the second anhydride tube to our system, and also to watch carefully the condition of its contents and to replace the tube as soon as the least change was perceptible. We attribute the change to a glazing of the amorphous grains due to the forming of a coating of glacial phosphoric acid, but the effect is one that would not be noticed except under such extreme conditions as existed in our work. We now pass to the system of absorption tubes on the other side of the balloon. Absorption Apparatus. The apparatus for the absorption of the carbonic acid gas must meet very opposite requisitions. In the first place, it must offer a sufficiently large mass of absorbent to the pure gas which first comes to prevent overheating from the rapid chemical combination. In the next place, it must be capable of removing the last traces of carbonic acid from the air which is afterwards drawn through the tubes. Lastly, it must not be so heavy or so complicated that it cannot be promptly and sharply weighed, and the correction for changes of temperature and pressure between successive weighings accurately estimated. After trying in various ways to enlarge and modify the different forms of potash bulbs and spiral tubes in general use, (and in these attempts we had the aid of a skilful glass-blower,) we found that we could reach a more accurate result with a system of separate tubes, in spite of the number of weighings they involved. To absorb the great mass of the carbonic acid we used the simplest form of gas washer, shown in Plate III. at A. The bulb had a capacity of 200 c.c., and in this we placed 75 c.c. of a solution of potassic hydrate having Sp. Gr. = 1.443. When empty the bulb weighed only 57 grams, and when filled about 165 grams. Assuming that the potash was fully neutralized, less than one half of this amount would be sufficient to combine with nine grams of carbonic acid ; but to insure prompt action and avoid excessive heating the amount given is required. The potash tube was followed by a small U tube, four inches long, with ground caps filled with finely granulated soda lime, and weighing when full about 40 grams. (See B, Plate III.) To. this was united a similar U tube containing phosphoric anhydride to hold the aqueous vapor, which is brought over by the gas current in no inconsiderable OF ARTS AND SCIENCES. 217 amount from the potash solution and the soda lime, in consequence of the heat set free by the absorption. The anhydride tube weighed when full about 25 grams, and is shown at C. Next was a third l' tube filled with glass beads and having a few drops of strong sulphuric acid at the bend. This tube, D, was not weighed, but was necessary in order to indicate any sucking back of the air and to prevent any vapor from thus reaching the phosphoric anhydride. The double bulb forming the end of the system, shown at E, was made by melting together the usual inlet tubes of two gas washers like A. In this we placed 50 c.c. of a standard solution of baric hydrate, and the peculiar construction was necessary in order to provide against regurgitation in consequence of back pressure. The solution is easily washed out of the bulbs, and wdien retitrated at the end of the process gives the amount of carbonic acid, if any, which escaped the other absorbents. All of these tubes were united into one system by rubber connections carefully lubricated both inside and out with vaseline, a soft parafline which had previously been melted and heated to remove every trace of moisture. The manipulation of this apparatus was an interesting experiment. When all had been set up as shown in Plate III., the globe being full of carbonic acid, the Bunsen pump was first started, and after a con- stant suction (regulated by the Mariotte's flask before described) had been established, we cautiously opened the cock of the balloon, which connected with the potash bulb, closely watching the flow of gas. As soon as this flow began to slacken, we as cautiously opened the farther cock, by which air was admitted to the balloon through the line of purifiers, still closely watching and regulating the flow. We then noticed a striking phenomenon. As pure carbonic acid was now passing into the potash bulb, the air mixing but slowly with the heavy gas at the surface of contact as the level sunk in the balloon, the absorption at first was complete. If the air supply from behind was not sufficient, a partial vacuum formed in A, and air was drawn back through the tubes in front, as indicated at once by the bubbles at the bend of D; but if the supply was carefully regulated, a perfect equilibrium could be maintained in the tubes beyond, and we have seen the carbonic acid flow into the potash bull) fur half an hour without more than a few bubbles of air passing through the sulphuric acid at the bend of I) in either direction. After a while, however, when the great mass of the carbonic a. -id has been absorbed, bubbles of air begin to pass through D, and also bubble through the baryta water beyond, and soon a steady current 218 PROCEEDINGS OP THE AMERICAN ACADEMY is established throughout the whole apparatus, which may then be left to take care of itself. If the current does not exceed in rapidity two bubbles a second, it may be allowed to flow for twenty-four hours without risk, and in that time every trace of carbonic acid will have been washed out of the 'balloon. The suction should now be stopped, and the cocks of the balloon closed. The tubes A, B, and C may then be disconnected, and after they have come to equilibrium in the balance case reweighed. The double bulb E must also be discon- nected, the baryta washed out into a suitable bottle, and the solution retitrated with oxalic acid. As the weights of the tubes A, B, and C must be corrected for the buoyancy of the air, it is essential to note the temperature of the balance case and the height of the barometer at the time of each weighing. The corrections in question may be considered under two heads ; first, that made necessary by a change of temperature or pressure between successive weighings ; secondly, that required to eliminate the effect of atmospheric buoyancy on the total weight of carbonic acid absorbed. The first correction is best made by the method already described, and the application of this method was greatly facilitated in the present investigation by the circumstance that the same tubes, wiih the "same weights of contents, were used in all the carbonic acid determinations made. We were able to determine once for all for each tube the correction required for a variation of one tenth of an inch in the barometric height reduced to 27° C.,* and then the cor- rection in any case could be found by a simple multiplication. Thus we estimated that the correction for one tenth of an inch in the barometric height reduced to 27° C. was, — For the potash bulb before absorption, . . . 0.306 milligram. « " after " ... 0.321 " " soda lime tube 0.067 " " phosphoric anhydride tube .... 0.040 " * That is, reduced to the height which would be required to give at the temperature of 27°, an atmosphere of the same density and buoyancy as that at the temperature of the balance case when the tube was weighed. These Proceedings, vol. xix. p. 55. OP ARTS AND SCIENCES. 219 Calculation of Correction for Potash Bulb. Before After Absorption. Absorption. "Weight of glass 57.45 grams. 57.45 grams. Volume of glass = 57.45 -r- 2.5 . . 23 c. c. 23 c. c. « KOH solution .... 75 " 80 98 103 " brass weights, 164 -f- 8.2 20 " " '• " 173 ~ 8.2 21 « Uncompensated volume 78 " 82 " Air displaced at 27° C. and 300 tenths of an inch. 1.176 x 78 91.928 m.g. 1.176x82 96.332 m.g. Variation for ^ 0.306 " 0.321 " The correction of the total weight of carbonic acid for the buoyancy of the atmosphere was not so simple a problem ; but by using the same bulb and nearly the same volume of the same solution of potassic hydrate in every case, it was sensibly the same for all the determina- tions. The specific gravity of the solution of potassic hydrate before the absorption was 1.443, and tested in two separate determinations after absorption it was found to be 1.464 in each case. Using now the arithmetical means of the weights of the potash bulb in the three determinations under consideration, it was easy to find an average value for the correction thus. Average weight of potash bulb before absorption 165.02 gr. Weight of glass 57.45 " solution of KOII 107.57 " Volume of solution of KOH = 107.57 -h 1.443 . 74.55 c. c. Average weight of potash bulb after absorption . 173.57 gr. Weight of glass 57.45 u 116.12 - Volume of solution of KOIT = 1 16.12 -4- 1.464 . 79.32 c. <■. Difference of volume = 79.32 -- 74.55 .... 4.77 - Weight of C02 absorbed in potash bulb = 173.57 — 165.02 8.55 gr. 220 PROCEEDINGS OP THE AMERICAN ACADEMY Volume of brass weights = 8.55 4- 8.2 1.04 c. c. Uncompensated volume = 4.77 — 1.04 3.73 " Weight of 3.73 c. c. of air at 300 tenths inch and 27° C. = 1.176 X 3.73 = corr. required . . 4.39 m.g. In this calculation we have necessarily left out of the account both the small amount of carbonic acid absorbed by the soda lime and the water carried by the current from the potash bulb to the connecting tubes ; for the increased weight of these tubes results from both these causes, whose relative effects or whose influence on the correction we canuot estimate! That they wuuld tend to raise slightly the value of the correction is obvious ; and if we assume, as we have in the following calculations, that the value is 4.5 milligrams we shall ap- proximate as nearly to the precise amount as circumstances will per- mit. For all these corrections the data are only known within certain narrow limits ; but the total uncertainty thus arising does not exceed two or three tenths of a milligram in the final result. In weighing the potash bulb and U tubes it is of course essential that they should be left in the balance case until a perfect equilibrium of temperature has been reached, and then they must be weighed when open so that a perfect equilibrium of pressure on the inside and outside of the glass may be secured. And since we were here aiming at very great accuracy, we felt it important to inquire further whether any gain of weight from hygroscopic moisture was possible during the time necessary to verify the weight while the tubes remained open on the scale pan. We therefore carefully investigated this point. The air in the balance case was kept as dry as possible by an open dish of sulphuric acid, aud the experiments were made under such conditions. It was found that the weight both of the potash bulb and of the soda lime tube remained absolutely constant, hour and hour together, except so far as they were influenced by changes of temperature and pressure, but the weight of the phosphoric anhy- dride tube slowly but uniformly increased at the rate of 0.025 m.g. per hour. We followed the change on one occasion from I0h- 45m- a. m. to 6h< 15m- p. m., and during these seven hours and a half the gain was 19 m.g., while the changes of temperature and pressure meanwhile were not enough to cause a sensible difference in the atmospheric buoyancy. Such experiments were continued for a sufficient length of time to enable us to confirm the values of the corrections above given, and they gave us great confidence in our weights. They showed that the only precaution necessary for accuracy was to close OF ARTS AND SCIENCES. 221 the tubes as soon as they were disconnected, and to leave each of them closed in the balance case until it was time to take the weight. The U-shaped tubes with perforated ground stoppers, by which connection with the lateral tubes can be instantly opened or closed, are admirably adapted to this work. As an example, we give next the details of one determination of carbonic acid by the method we have described. Details of a Determination of Carbonic Acid. The gas was generated from statuary marble and dilute hydro- chloric acid in an apparatus precisely similar to that described and figured by us in a previous paper.* It was first washed by a solution of potassic bicarbonate, and then, having passed in succession over Fig. 3. calcic chloride, sulphuric acid, and phosphoric anhydride, il was con- ducted into the balloon and overflow in tlie manner already described. The gas was tested by leading the current from the overflow into a familiar form of nitrogen apparatus filled with a solution of p<>t * These Proceedings, vol. xxiii. p. 160. 222 PROCEEDINGS OP THE AMERICAN ACADEMY hydrate (Fig. 3), and not until no measurable residue was left by a full liter of gas was its condition regarded as satisfactory. The balloon stood in the calorimeter case, and when the cocks were closed with the precautions already described the temperature of the case and the height of the barometer were observed, and although these values are not needed for determining the tare of the empty balloon, they will be used for determining the density of carbonic acid here- after. The balloon was then disconnected and hung on the balance, and its tare found to be W = 11.5907 grams. The balloon was then transferred to its metal case, and, having been mounted ;ts shown in Plate III., the determination of the weight of its contents proceeded as just described. Potash Bulb. Grams. H TO 1st weight of potash bulb 165.3388 299.99 25.8 2d " " " 174.0132 299.83 27.0 8.6744 Correction* for change of H and T 4 8.6740 * Since the volume and density of the potash solution used were closely the same in all the determinations, whether compared before or after the absorp- tion, the value of the correction may be assumed to be the same in all cases, and, as has been shown at page 218, amounts to 0.306 m.g. before absorption and 0.321 m.g. after absorption for every change of one tenth of an inch pres- sure or 1° centigrade temperature from the standard of 300 tenths inch and 27° C. or 300° absolute temperature. The correct mode of calculating the correction in any case is to reduce both weights to what they would appear to be at II = 300 and T0° = 300 = 27° C. before taking their difference, using the value 0.30G for the smaller of the two, and 0.321 for the larger. 290.89 at 25° .8 corresponds in buoyancy to 301.09 at 27° 299.83 at 27° " " " 299.83 " 301.09—300 = 1.09 and 1.09 X 0.306 = 0.33 addative. 299.83 — 300 = —0.17 and —0.17 X 0.321 = —0.05 subtractive. Then 165.3388 + 0.33 = 165.33913 174.0132 — 0.05 = 174 01315 8.67402 as before. As regards the sign of the correction, notice that, when reduced to H = 300, the buoyancy becomes less and the apparent weight greater if the previous pressure was above 300, and vice versa. Grams. H T° 42.8731 299.54 26.6 43.1857 299.87 27.4 OF ARTS AND SCIENCES. 223 Soda Lime Tube, 1st weight of soda lime tube 2(1 '< " it U Correction insensible 0.3126 Phosphoric Anhydride Tube. 1st weight of anhydride tube 39.5196 299.50 27.0 2d " " " « 39.5493 300.00 27.2 Correction insensible 0.0297 Standard Solution of Baric Hydrate. Before absorption, 50 c. c. required 46.60 c. c. solution of oxalic acid. After " " " 43.65 « « " 2.95 One c. c. of decinormal solution of oxalic acid contains 0.0126 cram of H2C204 . 2 H20, corresponding to 0.0044 gram of C02. 2.95 X 0.0044 = 0.0130 gram of CO,. Total Weight of Carbonic Acid. Grams. From potash bulb 8.67 10 " soda lime tube 0.3126 " anhydride tube 0.0297 " titration 0.0130 9.0293 Reduction to vacuum 45 9.0338 Tare of balloon and gas 11.5907 Tare of empty balloon 2.5569 Value by Regnault's method 2.')-'n'-'> The value of the tare of the empty balloon found by the new chemi- cal method is directly comparable with that obtained by the Regnaull method, since there was no change in the balloon meanwhile. But after this determination was finished, the balloon, as it remained stand- ing in its case, having been exposed to the direct sunshine of an un- usually hot June day, some of the cerate lubricating the stop-cocks melted and ran down into the tubulatures below, from which ii bad t" be removed. Thus the tare was lessened by nearly a centigram, fl 224 PROCEEDINGS OF THE AMERICAN ACADEMY was easy, however, to determine the exact loss, and as in a like inves- tigation, even when using the greatest care, one must ever be liable to accidents of this sort, it is important to dwell on this point. In losing the tare we had apparently lost the thread of our inves- tigation, but we were readily able to recover this thread without inter- rupting the general course of the work. It must be borne in mind that our immediate object was to obtain by the chemical method a series of results for the tare of the empty globe which could be com- pared with the mean value 2.5573 obtained by the method of Regnault. Here had come a change of tare, and we could obviously find a new standard of comparison by redetermining the new value by the old method. But this was not necessary. In the first determination by the chemical method, we had observed with great precision the pres- sure and temperature at which the balloon was filled. We do the same in the second determination, to which we next proceed, although these values are not needed in this determination, by itself considered, any more than they were in the first. If now from the tare of bal- loon and gas in the first determination (11.5907) we deduct 2.5573, we have the weight of carbonic acid which the balloon contains at a known temperature and pressure as found by the method of Regnault. If we deduct the same quantity from the tare found in the second de- termination, we have the weight of gas which the balloon holds at another temperature and pressure by the same method. If now there has been no change of tare, these two weights ought to agree exactly when one is reduced to what it would have been under the conditions at which the other was taken ; and if there has been a change of tare, the difference of the weights thus reduced will give the exact amount of the loss, on the basis solely, let it be noticed, of results obtained after the method of Regnault. Thus we have, — Grams. By No. 1, weight of C02 at 763.85 mm. and 25°.08 9.0273 " No. 2, " " 756.73 " " 22°.40 9.0334 Weight No. 1 reduced at " " " " 9.0241 Loss of tare 9.3 m. g. Obviously the accuracy of this result depends upon the accuracy with which the observations of temperature and pressure were made, and upon the correctness of the data on which the reductions are based. That the accuracy is extreme will appear from a comparison of the values of the specific gravity of carbonic acid, given on page 229, which were deduced from the same elements. And although in such work as this there is an obvious liability to error from just such a change of OF ARTS AND SCIENCES. 225 tare as we have been discussing, yet the loss or gain thus resulting is usually of such a magnitude that it cannot be overlooked. Besides the one of which the details have been given, we made by the chemical method two other determinations of the tare of the empty globe in precisely the same manner as before described, and obtained the values 2.5481 and 2.5475 respectively. In order to bring these results into comparison with that obtained by the first determination, or those obtained by the method of Reguault, we must add 9.3 m.g. to each value. We then have for Tare of Empty Balloon. Regnault's Method. Chemical Method. No. 1 2.5573 2.5569 No. 2 2.5572 2.5574 No. 3 2.5574 2.55G8 Average 2.55730 2.55703 o These results are essentially identical, and the two methods confirm each other. But having reached this important conclusion, which was the main object of our investigation, we freely concede the preference to Regnault's method. The difference between the results of the two methods, as here exhibited, is insignificant ; but so long as the validity and value of the correction for the contraction of the balloon on exhaustion has been thus established, Regnault's method will be preferred because it is practically more simple, and hence the results are more accordant than those obtained by the chemical method first described in this paper. • During the course of our investigation there were two marked changes in the tare of our balloon. One of these has been de- scribed. The other arose from the circumstance that the thin paraf- fine (vaseline) which was most suitable for lubricating the stop-cocks during the winter no longer kept the joints tight when the heat of approaching summer rendered the material more liquid ; and it became necessary to remove the stoppers and relubricate them, and it was the excess of cerate then used which melted and ran into the tubulaturea subsequently. There are then three separate values of the tare of the empty bal- loon to be used in our further calculations, all determined by or de- pendent upon Regnault's method, and all known with equal accuracy. These values we shall distinguish by the letters A, B, and C, and we shall designate by the same letters the experimental data or calculated results into which these values enter as elements. VOL. xxiv. (n. s. xvi.) 15 226 PROCEEDINGS OP THE AMERICAN ACADEMY Tare of Empty Balloon. Values. A 2.5098 grams. B 2.5573 " C 2.5480 " Density of Air freed from Moisture and Carbonic Acid. In these determinations the balloon was placed in the calorimeter case and connected with the Bunsen pump through an overflow jar. Air was then drawn into it through the purifiers we have described, and the reflux current which followed for a moment when the inlet cock was closed was supplied from the previous overflow. In other respects the determinations were made as before described, and we obtained the following data for the weight of air held in the balloon at different temperatures and pressures. Summary of Air Weights. A No. 1, weight of air at 762.63 mm. and 18°.52 = 6.0347 grams. A No. 2, " " 758.71 " " 19°.96 = 5.9745 " B No. 1, " " 750.30 " " 23°.32 = 5.8411 " Reducing now these weights to what they would have been at the temperatures and pressures we have assumed as standards, we obtain the following comparable values. , Reduced Air Weights for H == 761.99 mm. = 300 d. in* and T = 27° C. = 300° absolute temperature. A No. 1 5.8584 grams. A No. 2 5.8588 " B No. 1 5.8586 " Average value 5.8586 grams, t * We shall use the abbreviation d. in. for tenths of an inch, after the analogy of d. m. for tenths of a meter. t In the calculations of density and specific gravity, a still further, although wholly unimportant, correction has been made for the buoyancy of the air on the brass weights used to complete the tare in weighing the balloon, and in this connection it must be borne in mind that the platinum or aluminum fractions of a gram in a set of weights have always been adjusted to the larger brass weights in the air, and are therefore the equivalent of brass weights of the same denomi- OP ARTS AND SCIENCES. JlIT Density of Hydrogen. We have for the weight of hydrogen held hy the balloon the following data. B No. 1, weight of hydrogen at 763.10 mm. and 21°.08 = 0.41 G4 gr. B No. 2, " " 764.92 " » 20°.52 = 0.4178 " B No. 3, " " 758.96 « « 22°. 75 = 0.4123 " nations. The volume of the counterpoise was adjusted when the balloon was full of air; but although the compensation may be perfect through all ordinary changes of temperature and pressure, it cannot be regarded as absolute. In a laboratory, such changes seldom amount in the aggregate to more than the equivalent of one twentieth of the normal atmospheric pressure ; and although such a variation might not produce a sensible effect on the apparent weight of the small amount of brass used in our weighings, twenty times this effect, which we should have if the brass weights were wholly uncompensated, might be an appreciable quantity. In weighing the balloon the largest amount of brass weights used was about 11.5 grams, which at 300 d. in. and 27° C. displace 1.6 m.g. of air. One twentieth of this value would be barely, if at all, percep- tible, but the whole quantity might cause a serious error in our results. The tare of the empty balloon as first found by Regnault's method was 2.5573 grams ; and we must assume that in the system consisting of balloon counterpoise and weights there may be outstanding a very small uncompen- sated volume, so that the true tare would be represented by WR = 2.5573 ± w. We next find the weight of the balloon filled with hydrogen gas, and it is ob- vious that under standard conditions the true weight, or W = 2.5573 ± w + 0.4076 - w', where w' represents the buoyancy of air on 0.4076 gram of brass. So the true weight of the balloon filled with air must he W" = 2.5573 ± w + 5.8594 - w", where w" represents the buoyancy of air on 5 8594 grams of brass. In like manner, the true weight of the balloon filled with carbonic acid gas is W" = 2.5573 ± w + 8.9564 - w'"f where w'" is the buoyancy of air on 8.9564 grams of brass. Taking 1.176 m.g. as the weight of 1 c.c. of air at 300 d. in. and 27° C, the standard conditions to which the weights have been reduced, we have w' = 0.05 m.g., w" = 0.84 m.g., w'" = 1.28 m. g. ; and further, W — WR = 0 4076 - 0 00005 gram. True weight of hydrogen. W" - Wi: = 5.8594 - 0.00084 " *' " air. W'"-WK = 8.9564 -0.00128 " " " carbonic acid. These corrections should be applied to the weights before calculating the specific gravities, although they only alter the last values one or two unit- in 228 PROCEEDINGS OF THE AMERICAN ACADEMY Reduced Weights. H = 300 d. in. T = 27° C, B No. 1 0.4076 B No. 2 0.4072 BNo. 3 0.4081 •age 0.4076 Specific Gravity of Hydrogen. Air = 1. The values were obtained by dividing each of the weights of hydro- gen above given by the average weight of air (5.8586), after reduction for the temperatures and pressures at which the hydrogen weights were observed. The calculations were verified by dividing each of the reduced weights of hydrogen by the average reduced weight of air as above, and the same figures were obtained in both ways. B No. 1 0.06957 B No. 2 0.06951 B No. 3 0.06966 Average 0.06958 Average using values of tare by chemical method 0.06962 Specific Gravity of Oxygen. Hydrogen = 1. In this investigation we have not made an additional determination of the specific gravity of oxygen gas referred to air, for the causes of error which are serious in the case of hydrogen are not appreciable when working with the heavier gas, and we cannot expect to improvu the last decimal place ; and in this paper, as is usual, the decimals are carried out one figure beyond tlie limits of accuracy. In the chemical method we also took the weight of the balloon filled with carbonic acid gas, and, as before, we have W" = 2.5573 ± w + 8.9564 - w'". Then by chemical means we determined the absolute weight (tfi vacuo) of the carbonic acid which the vessel held, that is, the quantity represented by 8 9564 — w"'. Subtracting this value from the total weight, we obtained the tare of the empty balloon by the chemical method, and this obviously is Wc = 2.5573 ± w. Thus, the buoyancy of the air on the weights is eliminated, and "Wc is directly comparable in all its relations with WR. OF ARTS AND SCIENCES. 220 on the results of Regnault. Assuming, then, for the specific gravity of oxygen gas referred to air the value 1.10562, as obtained by Re«- nault and corrected by Crafts, and dividing this value by each of the values for the specific gravity of hydrogen gas given above, we have the following values for the specific gravity of oxygen referred to hydrogen. BNo.l B No. 2 BiNo.3 Average Average of chemical method Value found by Lord Rayleigh 15.892 15.907 15.873 15.891 15.882 15.884 Density of Carbonic Acid. For the weight of carbonic acid gas held in the balloon at different temperatures and pressures we have the following data. B No. 1, weight of C02 at 756.73 mm. and 22°.40 9.0334 gr. C No. 1, " « 760.50 " " 25°.56 8.9821 « C No. 2, " « 759.13 " " 26°.60 8.9348 " Taking now the average value of the weight of air held in the bal- loon at 300 d. in. = 761.99 mm. and 27° (viz. 5.8586 grams), and re- ducing this weight to what it would have been under the condition at which each of the four weights just given was observed, and then divid- ing each of these weights (corrected as by previous note) by the weight of air under the same conditions, we obtain the following results. Specific Gravity of Carbonic Acid. Air = 1. Wt. of CO,. Wt. of Air. n T Sp. Gr. B No. 1 9.0321 5.9088 756.73 22°.40 1.52858 CNo. 1 8.9808 5.8753 7C0.50 25°.56 1.52855 CNo. 2 8.9335 5.8445 759.13 26°.60 1.52855 Average value L.52856 Aver age value b\ ' chemical r irocess 1..-.2854 Taking lastly the average value of the weight of hydrogen held in the balloon at 761.99 mm. and 27° (viz. 0.4076 gram), and dividing the several weights of carbonic acid by this weight reduced to the same conditions, we have, — 230 PROCEEDINGS OF THE AMERICAN ACADEMY Specific Gravity of Carbonic Acid. Hydrogen = 1. Wt. of C02. Wt. of H2. H T Sp. Gr. B No. 1 9.0321 0.4111 756.73 22°.40 21.971 C No. 1 8.9808 0.4088 760.50 25°.56 21.971 C No. 2 8.9335 0.4066 759.13 26°.60 21.971 Average value 21.971 Average value by chemical process 21.957 The close agreement, indeed the essential identity, of these results should be noticed, as this fully substantiates the extreme accuracy of the method of recovering the lost tare of the empty balloon described on page 224. It is true that, as the values of the specific gravity of carbonic acid have been calculated with an average value of the sev- eral reduced weights of hydrogen or air, an error in these data would not affect the results ; but any error in the observed weights of car- bonic acid would appear to its full extent. Moreover, the striking fact should not be overlooked that the specific gravity of carbonic acid gas referred to hydrogen approaches much more nearly 22, the half molecular weight of carbonic acid gas as generally assumed, than does that of oxygen gas when referred to the same standard, the corresponding whole number 16, and the signifi- cance of the circumstance is obvious. If we assume that the atomic weight of oxygen as determined by Dr. Richards under my direc- tion is 15.87,* then the corresponding atomic weight of carbon would be 11.90, and the half molecular weight of carbonic acid 21.82. Theoretically, this number ought also to define the specific gravity of carbonic acid gas referred to hydrogen gas, if the two gases were com- pared under the same conditions of high temperature and indefinite expansion. But under the great pressure of our atmosphere the molecular volume of carbonic acid gas is known to be condensed to a measurably greater degree than the potentially equal molecular vol- ume of hydrogen gas, and the result must be a proportionally increased density ; and, moreover, the inequality in the condensation of the two gases must be increased by the circumstance that at the ordinary tem- perature of the air carbonic acid gas is below the critical point, while hydrogen gas is very far above it. If, however, this is true in the case of carbonic acid gas, our knowledge of the deviations from Mariotte's law compels us to infer that the same must be true in some small measure, although in a much less degree, in the case of oxygen gas ; * These Proceedings, vol. xxiii. p. 185. OF ARTS AND SCIENCES. 231 and it would lead us to expect that the specific gravity of oxygen gas referred to hydrogen gas would be slightly greater, certainly not I than the corresponding half molecular weight. Now we have from the results published in this and our preceding paper, — Half molecular weight of carbonic acid gas 21.82 Sp. Gr. of carbonic acid gas (referred to hydrogen gas) . 21.96 Half molecular or atomic weight of oxygen gas . . . 15.87 Sp. Gr. of oxygen gas (referred to hydrogen gas) . . . 15.88 It has been thought to discredit the low value of the atomic weight of oxygen we have found by the very easy but wholly gratuitous as- sumption that the hydrogen gas on which we experimented was im- pure, and we had intended in this investigation to demonstrate the identity of the gas from the several sources employed by a comparison of their specific gravities. We are under great obligations to Lord Kayleigh, who has relieved us from this necessity by anticipating the work. He has experimented on hydrogen gas, not only from all the sources we used, but also on gas which had been occluded by palla- dium, and has obtained the same result in all cases ; namely, the value 1-3.S84,* essentially identical with that which we have found in this investigation with the hydrogen gas from our electrolytic apparatus.! This point, however, had not been overlooked in the previous paper. It was there shown that the results obtained, in three distinct series of experiments, with hydrogen gas prepared by three different processes and with three different forms of apparatus, were essentially identical, t On the doctrine of chances, such an agreement would have been prac- * tically impossible had there been an appreciable amount of accidental impurities, in the gas from either of the sources. We say accidental impurities, for there may be inherent impurities common to the from all sources, of which we as yet know nothing; and, as we wrote before, " The question still remains, Is the hydrogen gas thus prepared the typical hydrogen element? But this is the same question which must arise in regard to any one of the elementary substances ; and :ill that we can say is, that the evidence in regard to the purity of the hydrogen we have used is as good as any that can be adduced in regard to any one of the elementary substances whose atomic weight has been most accurately determined." § * Proceedings of the Royal Society, vol. xlv. p. 426. t These Proceedings, vol. xxiii. p. 108. t See table, these Proceedings, vol. xxiii. p. 173. § These Proceedings, vol. xxiii. p. 171 232 PROCEEDINGS OF THE AMERICAN ACADEMY It is not to be expected that our results, or those of our contempo- raries, are final. The most that has beeu accomplished by recent in- vestigation is to show that the ratio of the atomic weight of oxygen to that of hydrogen, deduced from the elementary substances, as we know them in their purest condition, is decidedly less than that of 10 to 1. The evidence as to the exact value of this ratio is still conflicting, and although after our experience we cannot see how greater accuracy could be gained by any variation of our process, we are far from claim- ing that our results have not been vitiated by unknown constant errors. Fortunately, an exact knowledge of the ratio is at present of no practical importance in chemical analysis. The only question on which the actual small indefiniteness has a bearing is the unit of atomic weights, a question that has been much discussed of late ; but here, as it seems to us. one consideration should be conclusive. Every one who has worked on the oxygen and hydrogen ratio knows that the resources of experimental science have been taxed to the utmost in these investigations. Greater accuracy is not to be i x- pected with our present appliances, and yet there is an outstanding uncertainty amounting to more than one half of one per cent of the value. This corresponds to a variation of more than one unit in many of the higher atomic weights ; and unless we are willing that these chemical constants should fluctuate to this extent with every new de- termination of the fundamental ratio, we must seek a more invariable basis. The most natural and stable unit is the atomic weio-ht of oxygen, not only on account of the wonderful combining power of this element, but also because the ratio of the combining weights of most of the elements to that of oxygen are known with great precision ; and many cogent reasons could be urged for returning to the system of Berzelius, which referred all the other weights to that of oxvsren, assumed to be 100. But this system would not exhibit to advantage the numerical ratios ou which modern chemical classification is based. Hence for a provisional system we most warmly approve of that which assumes 0 = 16 as its basis, and of the best known atomic weights leaves only the value of H to vary with our changing knowledge. This system has all the stability it is possible at present to secure, and exhibits to advantage the relations which are important in classifica- tion. Moreover, it is no small recommendation to this system that a large number of the weights are whole numbers, within the limits of error of ordinary analytical work, and for this reason can be easily remembered. In conclusion, I would express my obligations to my nephew, Dr. PLATE I. PLATE II. OP ARTS AND SCIENCES. 233 Oliver W. Huntington, for the great aid he has given throughout this investigation. With the help of his skill in glass-blowing I have been able to secure all the connections of my gas generators with melted or cement joints, except the direct connections with the globe, where india- rubber could not be avoided. He has also constantly assisted my im- paired eyesight in the observations with barometer and thermometer on which the accuracy of the work greatly depended. I have likewise been indebted to Dr. Arthur M. Comey for making the titrations required, and to Mr. W. W. Bosworth for the drawings with which this paper is illustrated. 234 PROCEEDINGS OF THE AMERICAN ACADEMY XIX. CONTRIBUTIONS FROM THE CHEMICAL LABORATORY OF HARVARD COLLEGE. ON THE ACTION OF SODIUM MALONIC ESTER ON TRIBROMDINITROBENZOL. SECOND PAPER. By C. Loring Jackson and W. S. Robinson. Presented May 28, 1889. In a previous paper * on this subject we were obliged to publish sev- eral results in an unfinished condition, because at the time we saw no chance of being able to continue the work together. Since then, how- ever, unforeseen circumstances have allowed us to go on with the re- search, and in this paper we describe work which fills up most of the gaps in our former publication. The most important results contained in this paper may be stated briefly as follows. The reactions by which the bromdinitrophenyl- malonic ester is formed have been made out to be the following : — I. C6HBr3(N02)2 + CHNa(COOC2H5)2 = NaBr + CGHBr2(N02)2CH(COO"C2H5)2. II. C,HBr2(N02)2CH(COOC2H5)2 + CHNa(COOC2H6)2 = C6HBr2(N02)2CNa(COOC2H5)2 + CH2(COOC2Hs)2. III. C6HBr2(N02)2CNa(COOC2H5)2 + CH2(COOC2H.)2 = C6H2Br(NO,)2CNa(COOC2H5)2 + CHBr(COOC2H6)2. IV. CHNa(COOC2H.)2 + H20 = NaOH + CH2(COOC2H,)2. V. CHBr(COOC2H5)2 + NaOH = NaBr + CHOH(COOC2H.)2. The proof of these reactions consisted in the isolation of tartronic acid from the mixture obtained by the saponification of the oily secondary product with hydrochloric acid. The action of concentrated hydrochloric acid, or, better, sulphuric acid of specific gravity 1.44, upon the bromdinitrophenylmalonic ester * These Proceedings, xxiv. 1. OP ARTS AND SCIENCES. » has been studied, and we are able to correct some of the preliminary statements made on this subject in our first paper. The product is the bromdiuitrophenylacetic acid C6H2Br (N02) 2CH2COOH, which melts at 177°, and is formed, when hydrochloric acid is used, by the following reactions : — C6H2Br(N02)2CH(COOC8H5)2 + 2 HC1 = 2 C.,H.C1 + C6H2Br(NOs)2CH(COOH)2 = 2 C2H.C1 + C02 + C6H2Br(N02)2CH2COOH. The crystalline silver salt of this acid was analyzed, and proved to have the formula C6H2Br(N02)2CH2COOAg. H20. With sodic hydrate a deep Prussian green or with an excess a yellow- ish brown solution is formed, from which acids throw down a pale crimson precipitate, or a white one which becomes pale crimson when moistened with alcohol ; none of these substances could be brought into a state fit for analysis, but we found that bromine was removed in their formation. The bromdiuitrophenylacetic acid is broken up when boiled with alcohol into bromdiuitrotoluol and carbonic dioxide ; boiling with water produces the same effect, but much more slowly. A few drops of sulphuric acid prevent the decomposition by boiling water. This conversion into bromdiuitrotoluol gave us the means of determining the constitution of the bromdinitrophenylmalonic ester and its deriva- tives; as Messrs. W. B. Bentley and \V. II. Warren have, at our re- quest, worked out the constitution of the substituted toluol, and found that it is as follows : CH8.Br.N02.N02.1.3. 4.G. It follows, therefore, that all the substances mentioned in this and our former paper must have a similar constitution, and thai in making the bromdinitrophenylmalonic ester from bromdinitrobenzol the bromine atom replaced by the malonic radical is one of those which is at the same time para and ortho to the nitro groups, the one replaced by hy- drogen is ortho to the two nitro groups, while the third atom of bro- mine, which remains unaltered, occupies exactly the same position as that replaced by the malonic ester radical, — certainly a curious result. 286 PROCEEDINGS OP THE AMERICAN ACADEMY Preparation of Bromdinitrophenylmalonic Ester. Our longer experience in the preparation of bromdinitrophenyl- malonic ester has led us to introduce several improvements into the process, which now we carry on as follows. A strong benzol solu- tion of 20 grs. of tribromdinitrobenzol (benzol is to be preferred to the ether used formerly, because the tribromdinitrobenzol is more soluble in it) is mixed with 16 grs. of malonic ester previously con- verted into sodium malonic ester by treatment with the sodic ethylate from 2.3 grs. of sodium and about 100 to 125 c.c. of alcohol, and the mixture allowed to stand over night at ordinary temperatures. The red solution thus obtained is treated with water, which separates it into two layers, a dark red aqueous solution containing the sodium salt of bromdinitrophenylmalonic ester and sodic bromide, and a ben- zol solution of the unaltered tribromdinitrobenzol with the oily product of the reaction. The two layers are separated with a drop-funnel, and the lower aqueous one acidified with dilute sulphuric acid ; this throws down a yellowish white precipitate of the bromdinitrophenyl- malonic ester, which is purified by crystallization from hot alcohol, until it shows the constant melting point 70°. In this way 20 grs. of tribromdinitrobenzol gave 7.9 grs. of the bromdinitrophenylmalonic ester,* and 5.1 grs. of tribromdinitrobenzol were recovered from the benzol solution. Subtracting this from the 20 grs. there are left 1-4.9 grs. of tribromdinitrobenzol, which entered into the reaction, and should have given the same weight, 14.9 grs., of the product, so that the yield was 53 per cent of the theory, or about the same as that obtained by the process as given in our first paper, which calculated in the same way becomes 50 per cent. In the course of some other experiments the curious observation was made that it is not necessary to use sodic ethylate to bring about the action of malonic ester on the tribromdinitrobenzol, as a little of the red salt of bromdinitrophenylmalonic ester was formed when aqueous sodic hydrate was added to a mixture of the two organic * Dr. G. D. Moore, in his work with me on the action of sodium acetacetic ester on tribromdinitrobenzol, has found that a much better yield is obtained if the mixture is boiled for an hour under a return condenser. This observation was not made until the work described in this paper was finished and Mr. Robinson had left Cambridge, so that it was not convenient to try the experi- ment of boiling the solution of sodium malonic ester and tribromdinitrobenzol, nor did it seem very desirable to do so, as when we first took up the subject such an experiment was tried, and seemed to yield very unfavorable results. I propose, however, to repeat the experiment next year, if I return to the study of these compounds. C. L. J. OF ARTS AND SCIENCES. 237 substances. This recalls the observation of Victor Meyer,* that hom- ologues can be obtained from benzylcyauide by using the alkylhaloid with powdered solid sodic hydrate instead of sodic ethylate, or from desoxy benzoin by the use of an alcoholic solution of an alkaline hydrate. Study of the Reactions hj which the Bromdinitrophenylmalonic Ester is formed. One of the most important points, which want of time prevented us from considering in our first paper, was the mechanism of the reac- tions by which the bromdinitrophenylmalonic ester was formed from the tribromdinitrobenzol, and accordingly this was one of the first points to which we turned our attention in taking up the subject again. The reaction consists essentially, as our aiwyses of the pro- duct showed, in the replacement of one of the bromine atoms in the tribromdinitrobenzol by the malouic ester radical C1I(C00C2II5)2, and of a second by hydrogen forming CcH2Br(N02)2CH(COOC,H.)a, and the obscure part of it is the manner in which this second atom of bromine is replaced by hydrogen. The first step toward clearing up this obscurity was obviously to make out whether this atom of bro- mine was eliminated in the form of some organic compound, or as sodic bromide, which was done by the following quantitative deter- minations of the amount of sodic bromide formed in the reaction. I. 20 grs. of tribromdinitrobenzol were treated with the sodium malonic ester from 16 grs. of malonic ester in the way already de- scribed, and, after precipitating the bromdinitrophenylmalonic ester from the aqueous solution with dilute nitric acid, and filtering it out, the amount of sodic bromide was determined by precipitation of argen- tic bromide from an aliquot part of the filtrate, and calculating the amount in the entire solution. In this way the whole solution was found to yield 13.81 grs. of argentic bromide, corresponding to 5.88 grs. of bromine. The benzol solution on evaporation yielded 5.1 gr>. of tribromdinitrobenzol, which had not taken part in the reaction, leaving 14.9 grs. which had acted, and which would yield 5.89 grs. of bromine, if two of the atoms of bromine had been removed from each molecule as sodic bromide. II. 20 grs. of tribromdinitrobenzol gave under the same conditions 13.8 grs. of argentic bromide corresponding to 5.87 grs. of bromine, but only 4.9 grs. of tribromdinitrobenzol were recovered unaltered. * Ber. d. cli. G. 1888, p. 1201. 238 PROCEEDINGS OF THE AMERICAN ACADEMY The 15.1 grs. of tribromdinitrobenzol which entered into the reaction should have lost 5.96 grs. of bromine. Percentage of the theoretical amount of bromine removed from tri- bromdinitrobenzol in the form of sodic bromide : — I. ii. 99.86 98.49 These numbers agree as closely as could be expected, when the necessary sources of error in the process are considered, and prove that all the bromine removed by the reaction is converted into sodic bromide. The second point to be determined was from what source the atom of hydrogen was obtained which replaced the atom of bromine. For this purpose we investigated the oily product of the reaction, and, after we had found that nothing definite could be obtained from it by distillation under ordinary pressures, or with steam, and that sodic hydrate or other alkaline saponifying agents gave most unpromising results, we tried heating it with strong hydrochloric acid in a sealed tube to 130° for 20 hours, as the bromdinitropheuylmalonic ester which was dissolved in the oil would be converted by this treatment into the corresponding phenylacetic acid, with the properties of which we were familiar, and which therefore we thought could be removed easily from the other products of the reaction. The tubes after heat- ing contained an aqueous solution and a small amount of viscous matter, which gradually changed into an amorphous solid. These were separated by filtration, and the filtrate evaporated to dryness on the water bath, leaving a crystalline residue, which was extracted with cold water to leave behind the bromdinitrophenylacetic acid present. The extract after being evaporated again on the water bath gave crys- tals, which made up about one half the amount of the residue from the first evaporation. They were freely soluble in water or alcohol, nearly insoluble in ether, and could be sublimed at temperatures below their melting point forming glassy white thick needles or prisms, which melted at 185°. These properties prove that the crystals are tartronic acid, as they are identical with those given by Conrad and Bischoff for that substance.* We tried also to confirm this inference by an analysis, but the small amount of the acid which after some unsuccessful experiments remained at our disposal, little more than 0.1 gr., prevented us from purifying it thoroughly, as sublimation, * Ann. Cliem., ccix. 222. OP ARTS AND SCIENCES. 289 which had given the substance melting at 185°, turned out to be too wasteful a process for working up large amounts ; we were not sur- prised, therefore, that our analysis of the silver salt gave 62.82 per cent of silver, instead of the 64. G9 per cent calculated for argentic tartio- nate. This result, however, bad as it is, comes nearer to that for argen- tic tartronate than to that for any other substance which could well be formed, and therefore gives us the desired confirmation.* The small amount of tartronic acid obtained, less than 0.5 gr. from about 10 grs. of the oil, may be accounted for on the supposition that the larger part of the tartronic acid was decomposed by the strong hydrochloric acid used in the saponification of the oil, as Conrad and Bischoff f have observed that tartronic acid is decomposed very easily by hydrochloric acid, and we also were unable to obtain a trace of the acid from the filtrate after argentic chloride had been precipitated from the silver salt by a slight excess of hydrochloric acid. In fact, we should not have thought it worth while to try to obtain tartronic acid by the ac- tion of hydrochloric acid on our oil, if it had not been for the fact that tartronic ester has been made from calcic tartronate by the action of hydrochloric acid gas and alcohol, \ which would seem to show that the tartronic acid is more stable in presence of strong than of dilute hydrochloric acid, improbable as this sounds. This view is in harmony with our observations detailed above, and Conrad and Bischoff state that even very dilute acid decomposes it readily ; but even granting this, a large proportion of the tartronic acid must have been decom- posed during the treatment with hydrochloric acid, and this seems to us sufficient to make it more than probable that the tartronic acid is the product of the principal reaction, and not formed in a secondary one taking place only to a limited extent. If this is admitted, the fol- lowing reactions would give the most probable explanation of what takes place. I. C6HBr„(N02)2 + NaCII(COOC2H/)2 = C6HBr2(N02)2CH(COOC2H5)2 + NaBr. II. C6HBr2(N02)2CH(COOC2H5)2 + NaCH(COOC2H5)2 = CcIIBr2(N02)2CNa(COOC2H.)2 + CH2(COOC2H5)2. * No attempt was made to obtain a better analysis of the tartronic acid, because the work upon, the corresponding trinitro compound described in an- other paper furnished a complete confirmation of the theory of the reactions given here. t Ann. Chem., ccix. 223. J Freund, Ber. d. eh. G., xvii. 786. Pinner, Ibid., xviii. 757. 240 PROCEEDINGS OP THE AMERICAN ACADEMY III. C6HBr2(N02)2CNa(COOC2Hs)2 + CH2(COOCaH5)2 = CeH2Br(N02)2CNa(COOC2H5)2 + CHBr(COOC2H5)2. IV.. NaCH(COOC2H5)2 + H20 = NaOH + CH2(COOC2H5)2. V. CHBr(COOC2H5)2 + NaOH = CHOH(COOC2H5)2 + NaBr. Of these reactions, I., II., and III. take place before, IV. and V. after, the addition of the water used in working up the product. That Reaction III. takes place we infer from our discovery of tartronic i cid among the products of saponification of the oil, as Conrad and Bischoff * have proved that brommalonic ester is decomposed by sodic hydrate, according to Reaction V.f The experiments of one of us with G. D. Moore upon the action of sodium malonic ester on tribromtrinitrobenzol have shown that these reactions take place in a way analogous to that just worked out. For the details we would refer to the paper on this subject. The objection which might be raised against these reactions, that the yield of bromdinitrophenylmalonic ester is at best only about 50 per cent of that required by theory, and therefore that some other substance may be formed from the tribromdinitrobenzol in addition to it, is disposed of by the fact that on making the dibromdinitrophenyl- malonic ester from tetrabromdinitrobenzol by exactly analogous re- actions, the yield rose to 80 per cent of the theoretical. t It follows, therefore, that the 47 to 50 per cent unaccounted for in our preparations remained dissolved in the oily secondary product ; but although we have made many attempts to recover it, none of them have been crowned with success. The absence of malonic acid in the product of the action of hydro- chloric acid on the oil seems to us extraordinary, as we purposely kept the temperature of the saponification at 130°, in order to avoid decom- posing the malonic acid, which we expected from the excess of malonic ester undoubtedly present in the oil. We can account for this only by supposing that malonic acid is decomposed in presence of strong hydrochloric acid at a lower temperature than when heated alone. Saponification of Bromdinitrophenylmalonic Ester- In our previous paper we stated that strong hydrochloric acid de- composed bromdinitrophenylmalonic ester, when the two substances * Ann. Chetn., ccix. 222. t A fuller discussion of these reactions will be found in the general paper at the end of this series. t These Proceedings, xxiv. 295. OP ARTS AND SCIENCES. 241 were heated together to 140°-145° in a sealed tuhe, and described the product formed, stating, however, that all our results up to that time must be regarded as preliminary. Upon taking up the subject again, we studied in the first place the gas evolved when the tube was opened, and found that, in addition to the gas already mentioned burn- ing with a green-bordered flame (which is undoubtedly ethylchloride), carbonic dioxide was given off, as was proved by the precipitate formed when the gas was passed through lime-water. It is to be observed, however, that if the temperature to which the tubes were heated was 140°, or a little lower, very little, if any, carbonic dioxide was given off, and the product insoluble in the hydrochloric acid was oily ; on the other hand, when a crystalline product was obtained at a some- what higher temperature, carbonic dioxide was given off freely. "VVe next attempted to prepare the substance in open vessels by substitut- ing for strong hydrochloric acid dilute sulphuric acid boiling at about the temperature to which we heated the tubes, and found that not only did we obtain the product in this way, but that it was much purer than that made in the sealed tubes with hydrochloric acid. We have ar- rived accordinslv at the following method as the most convenient for saponifying the bromdinitrophenylmalonic ester. 2 grs. of the ester are mixed with about 100 c.c. of dilute sulphuric acid, specific gravity 1.44 and boiling point 132°, and the mixture boiled in a flask with a return condenser, until the oily drops of melted bromdinitrophenyl- malonic ester have all gone into solution, which usually takes about an hour and a half. After this the solution, as it cools, deposits long, pale yellow needles of the new substance, which, if the preparation has succeeded well, melt at 177° at once. If, however, the action has not run so well, and the melting point is somewhat lower than this, the substance can be easily purified by crystallization from boiling water acidified with a few drops of dilute sulphuric acid, but in no case should it be crystallized from pure water, or alcohol, as these solvents decompose it in the curious way described later in this paper, when we consider its properties. Metabromdinitrophenylacetic Acid, C0II2Br(N02)oClI,COOII. The substance prepared in the manner just described, and showing the constant melting point 177°, was dried at 100°, and analyzed with the following results : — I. 0.2106 gr. of the substance gave on combustion 0.2426 gr. of carbonic dioxide, and 0.0420 gr. of water. vol. xxiv. (n. s. xvi.; 16 242 PROCEEDINGS OF THE AMERICAN ACADEMY II. 0.1933 gr. of the substance gave 15.6 c.c. of nitrogen at a tem- perature of 15°. 5, and a pressure of 759.2 mm. III. 0.1821 gr. of the substance gave, according to the method of Carius, 0.1152 gr. of argentic bromide. Found. in. Carbon Calculated for C6H2Br( NO, )2CH2C02H. 3L47" i. 31.43 Found. II. Hydrogen Nitrogen 1.64 9.18 2.21 9.42 Bromine 26.23 26.93 These analyses supersede those already published,* which were made with a substance prepared by crystallization from dilute alcohol, before we had found that this solvent decomposed the compound ; it was therefore decidedly impure, as indeed was shown by its melting point, which was 170° instead of 177°. The yield of the bromdinitrophenylacetic acid is essentially quanti- tative, as 2 grs. of the bromdinitrophenylmalouic ester gave, after treatment with dilute sulphuric acid, 1.4 grs. of bromdinitrophenylacetic acid melting at 177°, instead of the calculated amount, 1.56 grs., that is, 90 per cent of the theory; the missing 10 per cent without doubt remained dissolved in the dilute sulphuric acid, in which the substi- tuted acetic acid is not wholly insoluble, as the 1.4 grs. were obtained by simple filtration, no attempt being made to recover the organic substance from the filtrate. In view of the observations described above, there can be no doubt that the following reactions take place when bromdinitrophenylmalonic •ester is saponified by heating it with hydrochloric acid at temperatures in the neighborhood of 145° : CcH2Br(N02),CH(COOC,H,)2 + 2 HC1 = CGH2Br(X02)2CH(COOH)2 + 2 C2H.C1 = CJI2Br(N02)2CH2COOH + C02+ 2 C2H5C1. And there can be no question that a similar reaction takes place when dilute sulphuric acid is substituted for strong hydrochloric acid. In fact, this was so obvious that we have not thought it worth while to try to isolate the sulphovinic acid which must be formed in this case instead of the ethylchloride. Properties. — The metabromdinitrophenylacetic acid crystallizes from an aqueous solution containing a little sulphuric acid in yellowish * These Proceedings, xxiv. 11. OF ARTS AND SCIENCES. 243 white needles, often one to two centimeters long, which appear under the microscope as tolerably thick prisms frequently tapering owing to modification by the planes of a pyramid with, a very acute angle, but almost always, even in addition to this tapering, terminated bluntly by the planes of another very obtuse pyramid. Occasionally the ter- mination is a single plane at a moderately acute angle to the sides, but this looked as if it were due to cleavage. The crystals are generally very well developed, but if they are small, a tendency to twin longi- tudinally is observed. If the substance is crystallized from alcohol, the forms like feathers, or half-feathers, described in our previous paper, and groups of branching needles looking like certain feathery seaweeds, appear ; but as the alcohol decomposes the substance, these forms can hardly be ascribed to the substituted acetic acid itself. It melts at 177° ; and is essentially insoluble in ligroine or carbonic disulphide ; very slightly soluble in chloroform, slightly in benzol, more soluble in both of these solvents when hot ; tolerably soluble in ether, separating from the solution in a liquid form, which solidifies on stirring ; easily soluble in acetone or glacial acetic acid ; soluble in cold alcohol, more freely in hot, but the alcohol decomposes it, as is indicated by the change in the appearance of the crystals, the long yellowish prisms of unaltered bromdinitrophenylacetic acid becoming roughly studded with fine needles of another substance, and by the lowering of tke melting point, when the substance is crystallized from alcohol ; evaporation to dryness of the alcoholic solution, if repeated three times, reducing the melting point from 177° to 147° ; while after two more evaporations, making five in all, the melting point had sunk to 103°— 104°, at which point it remained constant after repeated crystallization. The substance obtained in this way crystallized in rectangular prisms, or plates, was not acted on by alkalies, and was recognized as Grete's metabromdinitrotoluol.* For greater certainty it was analyzed, with the following results : — I. 0.1690 gr. of the substance gave by the method of Carius 0.1210 gr. of argentic bromide. II. 0.2185 gr. of the substance gave 20.3 c.c. of nitrogen at a temperature of 22°. 5 and a pressure of 773.3 mm. Bromine Nitrogen Calculated for C6H2Br(N02)2CH3. 30.65 10.73 Found. I. II. 30.47 10.69 * Ann. Cliem., clxxvii. 258. 244 PROCEEDINGS OP THE AMERICAN ACADEMY This conversion of the metabronidinitrophenylacetic acid into the corresponding toluol by boiling with alcohol, when it is so stable in presence of boiling dilute sulphuric acid, seemed to us so interesting that we have examined it more carefully. Having in the first place determined that the alcohol was neutral to test papers, to prove that the reaction could not be due to a trace of alkali, or acid in it, a quantity of the substance melting at 177° was boiled in a flask under a return condenser with a little alcohol for three hours, and pure air occasionally drawn through the apparatus to sweep out its contents into a set of absorption bulbs filled with lime-water ; in this way a heavy precipitate was obtained, which consisted in great part of calcic hydrate precipitated by the alcohol vapor, but also contained calcic carbonate, as was shown by effervescence when it was dissolved in an acid, thus proving that carbonic dioxide had been given off. The alcoholic solution, after it had been boiled for an hour and a half longer, gave crystals, melting at 103° to 104°. It seems evident, therefore, that the reaction runs as follows, CeH2Br(N02)aCH2COOH = C6H2Br(N02)2CH3+C02, and the alcohol seems to take no part in it. Methyl alcohol, in which the substance is more soluble than in ethyl alcohol, brings about a similar decomposition, but more slowly. In boiling water the meta- bromdinitrophenylacetic acid is tolerably soluble, but nearly insoluble in cold water. The decomposition produced by alcohol also takes place when the aqueous solution is boiled, but very slowly, so that long boiling is necessary to convert the substance completely into the substituted toluol ; nevertheless, after distilling with steam for several hours, the whole of the substance had passed over into the receiver as metabromdinitrotoluol, since none of the substituted acetic acid, which does not distil with steam, was left in the flask. The presence of a very small amount of sulphuric acid (two or three drops of the dilute acid to 100 c.c. of water) is sufficient to prevent this decomposi- tion entirely, as a specimen of the substituted acetic acid showed no signs of decomposition, even after having been distilled with steam for three hours with only the amount of dilute sulphuric acid which remained adhering to it after the excess of acid used in its preparation had been removed by filtration. The best solvent for the bromdini- trophenylacetic acid therefore is boiling water containing a few drops of sulphuric acid. If the substance has become contaminated with the substituted toluol, it can be purified conveniently by distilla- tion with steam in presence of a few drops of sulphuric acid, when OF ARTS AND SCIENCES. 2-15 the toluol passes over, and the acetic acid remains behind in the flask. Amnionic hydrate dissolves the metabromdinitrophenylacetic acid, forming a colorless solution if the acid is in excess ; but if the amnio- nic hydrate is added in slight excess, a green solution is obtained, which turns dark brown if a large excess of ammonic hydrate is added, but regains its green color on dilution with water. Both the colorless and green solutions smell of ammonia, and this smell could not be removed by gentle boiling, or by allowing the solution to stand over sulphuric acid, from which we infer that the ammonium salt is a decidedly unstable substance. When either solution is warmed on the water bath for some time it is partially decomposed with formation of a precipitate of metabromdinitrotoluol, and the green solution turns yellow even when allowed to evaporate spontaneously. Hydrochloric acid threw down from the solution a precipitate of metabromdini- trophenylacetic acid. The ammoniacal solution, prepared with an excess of the acid and freed as completely as possible from an excess of ammonia, gave no precipitate with baric, strontic, or calcic chloride, but with the salts of many of the heavy metals it gave precipitates, of which the following were the most characteristic: — Aluminic chloride, heavy, white. Ferric chloride, heavy, very pale bluff. Cupric sulphate, heavy, pale blue. Mercuric nitrate, heavy, yellowish white. Mercuric chloride, a very slight precipitate, probably white precipi- tate from the slight excess of ammonic hydrate. Mercvrous nitrate, heavy, white. Plumbic acetate, heavy, white. Argentic nitrate, heavy, white. The behavior with argentic nitrate is especially characteristic ; if the solutions are strong, the mixture becomes nearly solid from the formation of a white flocculent precipitate, which frequently swells up, forming a little heap or pyramid, and after standing for some hours becomes converted into good-sized crystals. The analysis and proper- ties of this salt are described more in detail below. With sodic hydrate a solution of the acid turns a deep Prussian green color, which passes in time into a yellowish brown, this latter color appearing at once when an excess of sodic hydrate is added. If the green solution is acidified, a precipitate is obtained, which, although nearly colorless when dry, becomes purple when moistened with alco- hol. This precipitate was oily at first, and, although it solidified later. 246 PROCEEDINGS OF THE AMERICAN ACADEMY we did not succeed in finding any solvent from which it could be crys- tallized. That the sodic hydrate had acted on the bromine was shown by an actual experiment, which gave the following results. 0.67 gr. of the acid yielded by treatment with sodic hydrate so as to form the green salt 0.1136 gr. of argentic bromide, which corre- sponds to 0.0483 gr. of bromine instead of the 0.1757 gr. contained in the amount of acid taken ; that is, 27.5 per cent of the whole had been removed. The yellowish brown solution obtained, when a large excess of sodic hydrate was used, or the mixture of sodic hydrate and metabromdi- nitrophenylacetic acid was boiled for some time, gave on addition of an acid a viscous red substance, which was exceedingly unmanageable. That bromine was removed in quantity in this way is shown by the following determination. 0.2412 gr. of the metahromdinitrophenylacetic acid was boiled with sodic hydrate for three quarters of an hour ; the product, after acidify- ing with nitric acid, and filtering out the precipitate, gave 0.1180 gr. of argentic bromide, corresponding to 0.0502 gr. of bromine instead of the 0.0632 gr. contained in the weight of acid taken ; that is, 79.4 per cent of the whole. It is evident, therefore, that the original compound has undergone a deep-seated alteration, and the new crimson substance is probably a phenol. This view of its nature receives some confirmation from the fact that it is decomposed with the greatest ease by even somewhat dilute nitric acid. We have not yet succeeded in bringing either of the products derived from sodic hydrate into a state fit for analysis, although the slight solubility of the barium salt of the crimson acid awakened hopes of success ; but these ended in disappointment, as the salt proved quite as viscous as the free acid. Potassic carbonate gives with the metahromdinitrophenylacetic acid results similar to those obtained with sodic hydrate, but less marked. We hoped to be able to throw some light on this action of alkalies on the metahromdinitrophenylacetic acid by the study of the correspond- ing anilido compound, but have not succeeded as yet in preparing it, as aniline converts the free acid direct into metanilidodinitrotoluol,* C6H2CH8(C6H6NH)(N02)2, melting point 142°, and the saponification of anilidodinitrophenylmalonic ester with sulphuric acid yielded only uninviting viscous products. * Hepp, Ann. Chem., ccxv. 371. OF ARTS AND SCIENCES. 247 Radziszewski,* Gabriel and R. Meyer,f and Heckmann,^ have pre- pared a dinitrophenylacetic acid which differs from that just described only in containing no bromine. This substance also loses carbonic dioxide easily, passing into diuitrotoluol, but none of the chemists who have worked with it describe a decomposition by solvents similar to that observed by us ; in fact, they crystallized it for analysis from boiling water, but, as in all their methods of preparation acids were used, it is possible that a sufficient amount of sulphuric acid was pres- ent during the crystallization to prevent the decomposition. It ap- pears that none of them tried to crystallize it from alcohol. The statement is made, however, that the sodium or potassium salt of the acid decomposes slowly on standing, instantly on boiling giving car- bonate and diuitrotoluol ; from this it would seem probable that our bromine acid was more stable than that containing no bromine, as our ammonium salt (the sodium or potassium salt could not be obtained) stood unaltered for many days, and even could be warmed on the water bath for some minutes with only slight decomposition. The curious change of color with sodic hydrate observed by us did not occur with the dinitro body, confirming our conclusion that this action was due to the removal of bromine by the sodic hydrate. A rgentic Metabromdinitrophenylacetatey C6H2Br(N02)2CH2COOAg . H20. This substance was prepared by adding a solution of argentic nitrate to a solution of the acid in amnionic hydrate, which had been freed from the excess of ammonia as completely as possible, best by using an excess of the acid in preparing the salt. The heavy flocculent precipitate, which, if the solutions were strong, entirely filled the liquid, and even piled up above its surface, became crystalline on standing, and was purified by washing with cold water. Some of the salt is also formed when argentic nitrate is added to an aqueous solution of the free metabromdinitrophenylacetic acid. The analysis of the salt gave the following results. 0.3530 gr. of the air-dried salt lost, when heated to 100°, 0.0149 gr. Calculated for C6H2Br(N02)2CH,C02Ag . H20. Found. Water 4.19 4.22 * Ber. d. ch. G., ii. 210. J Ann. Chem., ccxx. 134 t Ibid., xiv. 823. 248 PROCEEDINGS OF THE AMERICAN ACADEMY I. 0.1674 gr. of the salt dried at 100° gave, after being heated with fuming nitric acid in a sealed tube * and precipitated with potassic bromide, 0.0761 gr. of argentic bromide. II. 0.1556 gr. of the salt treated in the same way gave 0.0707 gr. of argentic bromide. Calculated for Found. C6H2Br(N02)2CH2CO,Ag. I. II. Silver 26.21 26.11 26.10 Properties. — The argentic bromdinitrophenylacetate forms white flat prisms terminated by a single plane at an oblique angle ; the ter- minated end is somewhat broader than the other, so that the crystals look like a flattened base-ball bat. They have also a tendency to twin longitudinally. When put in the flame of a Bunsen lamp, they burn with a sparkling flame, but when heated carefully on a piece of porcelain, decompose quietly leaving a residue of silver. The sub- stance is very slightly soluble in cold water, so that it can be washed without too great loss ; more soluble in hot water, from which it crys- tallizes apparently without decomposition ; insoluble in cold alcohol, but slowly decomposed, if heated with it. Constitution of Bromdinitrophenylmalonic Ester. The formation of metabromdinitrotoluol from bromdinitrophenyl- malonic ester by a series of reactions giving essentially a quantitative yield and taking place at temperatures not above 150°, throws a great deal of light on the nature of this substance. In the first place, its conversion into a toluol derivative is a welcome confirmation of the formula which we have given it, and which did not rest on the most secure experimental foundations. In our first paper it was stated that the analysis left the choice open between the following formulas, I. C,H,Br(N02),CH(COOC,H5)2, II. C6HBr(N02)2C(COOC2H5)2, and we decided in favor of the first on account of the analyses of the sodium salt, an amorphous substance for the purity of which we had no guaranty, and also on account of the ease with which this salt was formed and decomposed, the product of the decomposition being the original ester. Against this formula stood only our inability at the * We had hoped in this way to determine both the silver and bromine in one operation, but found that the filtrate gave a precipitate with potassic bromide. It would seem, therefore, that the presence of an excess of argentic nitrate is necessary to retain all the bromine. * OF ARTS AND SCIENCES. 249 time to explain the reactions by which it was formed, an objection which is removed by this paper. The easy conversion of a substance having Formula I. into a toluol compound is to be expected, whereas with one having Formula II. it would be necessary to add two atoms of hydrogen, an action which could hardly take place quantitatively by boiling with dilute sulphuric acid, or distillation with steam, the two processes employed in converting the bromdinitrophenylmalonic ester into the bromdinitrotoluol. This formation of the substituted toluol therefore establishes Formula I. beyond question. In the second place, the way is opened to the determination of the position of the substituting radicals upon the benzol ring in all these compounds, as their position must be the same as in the bromdinitro- toluol. Messrs. W. B. Bentley and W. H. Warren have accordingly, at our request, determined the constitution of the bromdiuitrotoluol by replacing its bromine successively by the amido group and by hydro- gen, and have found in this way that its constitution is CH3 . Br . NOa . N02 .1.3.4.6. For the details of their work we would refer to their paper, which fol- lows immediately after this. It follows from this that in the tribrom- dinitrobenzol Br . H . Br . N0.2 . Br . N02 . 1 . 2 . 3 . 4 . 5 . 6, the bromine numbered 1, which stands in the ortho position to one nitro group and the hydrogen, in the para position to the other nitro group, has been replaced by the malonic ester radical CH(COOC2H5)2 ; that the bro- mine replaced by hydrogen is the one between the two nitro groups ; and that the third bromine, which is in exactly the same relation to the nitro groups as the one replaced by the malonic ester radical, is left entirely unaltered. This last fact seems very strange to us. The constitution of our bromdinitrophenylmalonic ester is therefore repre- sented by the following graphical formula : — CH(COOC2H5)2 250 PROCEEDINGS OF THE AMERICAN ACADEMY XX. CONTRIBUTIONS FROM THE CHEMICAL LABORATORY OF HARVARD COLLEGE. ON SOME NITRO DERIVATIVES OF METABROMTOLUOL, By W. B. Bentley and W. H. Warren. Presented May 28, 1889. Determination of the Constitution of Metabromdinitrotoluol, C6II2CH3Br(N02)2. Our attention was first called to this subject by Prof. C. Loring Jackson, who, having with W. S. Robinson* obtained the metabrom- dinitro toluol by the decomposition of their bromdinitrophenylmalonic ester, asked us to determine its constitution. This metabromdinitrotoluol, melting point 103°-104°, was discovered by Grete,f who made it by the action of fuming nitric acid on meta- bromtoluol, or metabrommononitro toluol, and assigned to it the con- stitution CH3, N02, Br, N02, 1, 2, 3, 4, although he was very doubtful about the position of the second nitro group, giving it the para posi- tion without any experimental reason for doing so. His proof that one of the nitro groups was in the ortho position consisted in estab- lishing the identity of the bromtoluidine made by the reduction of his bromnitrotoluol with that obtained by the action of bromine on ortho- acettoluid ; % but this obviously leaves it doubtful whether this nitro group stands in the position 2 or 6 to the methyl of the toluol, and in fact later work has shown that Grete was wrong in ascribing to it the position 2, as his mononitro compound really has the constitution CH3, Br, N02, 1, 3, 6. The proof of this was given by Nevile and Winther,§ who, by replacing the amido group in the metabromor- thotoluidine (melting point 55°-56°) already mentioned by bromine, * See preceding paper. t Ann. Chem., clxxvii. 258. X YVroblewsky, Ann. Chem., clxviii. 1G1. § Ber. d. eh. G., xiii. 962. OF ARTS AND SCIENCES. £51 obtained a liquid dibrotntoluol, which on oxidation with nitric acid yielded the dibrombenzoic acid melting at 151°-153° previously made by Von Richter* from paradibrombenzol. The only point therefore not settled in regard to the constitution of Grete's metabromdinitrotoluol was the position of the second nitro group, which might be either para or ortho to the methyl. To deter- mine this the metabromdinitrotoluol was heated with alcoholic ammo- nia f in sealed tubes to 100° for 12 hours, when it was found to be converted into a yellow substance, which had partly separated in the solid state, and partly remained in solution in the alcohol, from which it was obtained by evaporation. The product was purified by wash- ing with water to remove the amnionic bromide, and crystallization from hot glacial acetic acid, until it showed a constant melting point (193°-194°), when it was dried at 135°, and the following analysis showed that a diaitrometatoluidine had been formed. 0.2658 gr. of the substance gave 51.2 c.c. of nitrogen at a temper- ature of 24° and a pressure of 767.5 mm. Calculated for C6H2CH3NH,(N02)2. Found. 21.31 21.71 Nitrogen The melting point showed that this substance is identical with the dinitrotoluidine made by Heppl by the action of alcoholic ammonia on his y trinitrotoluol, but the constitution of this trinitrotoluol had not been determined. Staedel § has also announced recently that one of his students, Herr Adalbert Kolb, has prepared a dinitrotoluidine from dinitrokresolether and determined its constitution as CH3, NH„ NO.,, N02, 1, 3, 4, 6 ; but, as he neglected to give the melting point, we were unable to tell whether it was identical with ours or not, and have been forced to work out the constitution of our dinitrotoluidine by the replacement of the amido group by hydrogen. In doing this some difficulty was encountered because of the very slight solubility of the dinitrotoluidine in alcohol, but we found on experiment that the Griess reaction would take place satisfactorily in a mixture of acetone and alcohol, and accordingly proceeded as follows. 2 grs. of the dinitro- * Ber. d. ch. G., vii. 1146. t When metabromdinitrotoluol was allowed to stand with alcoholic ammonia in the cold, a dark blue solution was formed at first, but the color gradually changed to reddish brown. J Ann. Chem., ccxv. 371. § Ber. d. ch. G , xxii. 21-3. 252 PROCEEDINGS OF THE AMERICAN ACADEMY toluidine were dissolved in about 12 c.c. of acetone, 8 c.c. of common alcohol added, and the mixture acidified with strong sulphuric acid, after which 1.5 grs. of sodic nitrite, about twice the calculated amount, was added in small portions at a time, and the liquid warmed gently until the evolution of nitrogen ceased, when the larger part of the acetone and alcohol was distilled off at first on the water bath, finally on the sand bath, and the residue distilled with steam ; the dinitrotoluol passed over into the receiver in small white crystals, which were removed by filtration, and crystallized from hot alcohol until they showed the constant melting point 71°. It was not worth while to' dilute the distillate of acetone and alcohol, as no precipitate was ob- tained in that way. For greater certainty the product was analyzed, with the following results : — 0.2456 gr. of the substance gave 33.1 c.c. of nitrogen at a tempera- ture of 22° and a pressure of 764.2 mm. Calculated for CoILjCHaCNOj;);,. Found. Nitrogen 21.31 21.71 There is no question therefore that the substance is the orthopara- dinitrotoluol, CH3, NO.,, NO.„ 1, 2, 4, and the bromdinitrotoluol accord- ingly has the following constitution: CH3, Br, N02, N0.2, 1, 3, 4, 6. It follows also that our dinitrotoluidine is identical with that described by Kolb, and, if Staedel had given its melting point, it would not have been necessary for us to determine its constitution. As has been already stated, this dinitrotoluidine melts at the same point as that made by Hepp from alcoholic ammonia and his y trinitrotoluol. To establish the relation between these substances more firmly, we made the dinitrophenyltoluidine by treating our dinitrobromtoluol with ani- line, and found that the product showed the same melting point, 142°, as that of the compound made by Hepp from y trinitrotoluol and aniline. The y trinitrotoluol of Hepp therefore has the following constitution : CII.,, N0.2, NCX, N02, 1, 3, 4, 6 ; which is in harmony with Laubenheimer's rule,* that a nitro group is removed by the action of alcoholic ammonia only when it is in the ortho position to another nitro group. Metabromtrinitrotoluol, CcHCII3Br(N02) ,. In preparing the metabromdinitrotoluol, we found, if a mixture of fuming nitric acid and sulphuric acid was used, that a new substance * Ber. d. oh. G., ix. 7G6, 1828. OF ARTS AND SCIENCES. 253 melting above 104° was obtained, which turned out to be the as yet undescribed metabromtriuitrotoluol. This compound is most easily prepared from the metabromdinitrotoluol, when it is convenient to proceed as follows. 5 to 10 grs. of metabromdinitrotoluol were placed in a flask, and 10 to 20 c.c. of a mixture of two volumes of fuminf 9 c* nitric acid and one of strong sulphuric acid added. The whole was then boiled until the evolution of red fumes had nearly ceased, when, after it was cool, it was poured in a fine stream into a beaker of cold water, stirring the liquid vigorously during the addition of the acid solution, as in this way the product is precipitated in a granular form much more easy to manage than the large compact lumps obtained if the stirring is neglected. The product was then washed with cold water till free from acid, and purified by crystallization from alcohol, until it showed the constant melting point 143°. The residue from the mother liquors, consisting of a mixture of metabrom trinitrotoluol and the corresponding dinitro compound, can be advantageously used for preparing a fresh quantity of the trinitro body. The pure sub- stance was dried at 120°, and analyzed with the following results: — I. 0.3372 gr. of. the substance gave on combustion 0.3356 gr. of carbonic dioxide and 0.0453 gr. of water. II. 0.2651 gr. of the substance gave 32.9 c.c. of nitrogen at a tem- perature of 21° and a pressure of 761.5 mm. III. 0.1830 gr. of the substance gave, by the method of Carius, 0.1120 gr. of argentic bromide. Found. III. Carbon Calculated for CGHCH3Br(X02)3. 27.46 i. 27.14 Found II. Hydrogen 1.31 1.49 Nitrogen 26.14 26.0' Bromine 13.73 14.09 The yield was about 60 per cent of the theoretical. Properties. — The metabromtrinitrotoluol crystallizes from alcohol in small white needles, which melt at 143°. They are insoluble in water, or ligroiue ; nearly insoluble in cold alcohol, only sparingly soluble in hot ; slightly soluble in carbonic disulphide ; soluble in ether, methyl alcohol, benzol, chloroform, glacial acetic acid, or acetone. Boiling alcohol we found the best solvent for it, although it is so slightly soluble in it. Aqueous sodic hydrate seemed to have no action upon it, nor was it affected by the strong acids. The bromine is removed easily, which we proved by the action of alcoholic ammonia or aniline on it, as will be described later in this paper. 254 PROCEEDINGS OF THE AMERICAN ACADEMY Constitution of Metabromtrinitrotoluol. As the metabromtrinitrotoluol is made from the raetabromdinitro- toluol, the only point to be determined is the position of the third nitro group ; for this purpose we converted it into the corresponding trini- trotoluidine by treatment with alcoholic ammonia in the cold. The mixture was allowed to stand in a corked flask for about twelve hours ; at first a dark blue color appeared in the liquid, but on longer stand- ing this turned to a deep reddish brown, and a precipitate was de- posited, which with the supernatant liquid at the end of the twelve hours was poured into a dish, and the solvent allowed to evaporate spontaneously. The residue, which was red and yellow, was washed till free from ammonic bromide, and then purified by crystallization from hot glacial acetic acid, until it showed the constant melting point 136°, when it was dried at 120°, and analyzed with the following result : — 0.1144 gr. of the substance gave 24.2 c.c. of nitrogen at a tempera- ture of 23° and a pressure of 754.7 mm. Calculated for C6HCH3NH,(N02)3. Found. Nitrogen 23.14 23.51' The melting point of this trinitrotoluidine shows that it is identical with that prepared by Nolting and Salis* by the action of alcoholic ammonia on trinitrometakresolethylether, to which they assign the constitution CTI3, N02, NH2, N02, N02, 1, 2, 3, 4, 6, on the ground that the alcoholic ammonia did not remove any of the nitro groups, and therefore, according to Lauhenheimer,| no two of them could be in the ortho position to each other, and this is the only possible ar- rangement in which no two nitro groups are in the ortho position. Our metabromtrinitrotoluol must consequently have the constitution CH3, N02, Br, N02, N02, 1, 2, 3, 4, 6 ; and this conclusion is confirmed by the fact recently discovered in this laboratory,! that the bromtrini- trophenylmalonic ester is converted by boiling with sulphuric acid of specific gravity 1.44 into this metabromtrinitrotoluol melting at 143°. As the bromtrinitrophenylmalonic ester is made from the symmetrical tribromtrinitrobenzol, Br, N02, Br, N02, Br, N02, 1, 2, 3, 4, 5, 6, it can have only the constitution CH(COOC2tL)„, N02, Br, N02, N02, * Ber d. ch. G., xv. 1864. t Ber. d. cli. G., ix. 766, 1828. % C. Loring Jackson and G. D. Moore. These Proceedings, xxiv. 268. OF ARTS AND SCIENCES. 255 1, 2, 3, 4, 6, which leads to the constitution of our metabromtrinitro- toluol given above. Anilidotrimtrotoluol, C6HCH3(CGH3NH) (N02)3. This substance was prepared by treating metabromtrinitrotoluol with aniline in the proportion of two molecules of the base to one of the nitro compound ; the action is violent, accompanied with consider- able evolution of heat, and the product was easily purified by crystal- lization from a mixture of alcohol and benzol, until it showed the constant melting point 151°, when it was dried at 120°, and analyzed with the following results : — I. 0.2804 gr. of the substance gave on combustion 0.5031 gr. of carbonic dioxide and 0.0936 gr. of water. II. 0.2777 gr. of the substance gave 43.2 c.c. of nitrogen at a tem- perature of 27°. 5 and a pressure of 772 mm. Found. II. Carbon Calculated for C6HCH3(CcHflNH)(N02)3. 49.06 i. 49.03 Hydrogen Nitrogen 3.14 17.61 3.71 17.41 Properties. — The metanilidotrinitrotoluol crystallizes from a mix- ture of alcohol and benzol in well developed shining yellow plate's, which melt at 151°. The substance is insoluble in water or ligroine ; sparingly soluble in ethyl or methyl alcohol ; soluble in ether, chloro- form, benzol, carbonic disulphide, glacial acetic acid, or acetone. The most convenient solvent for it is a mixture of five parts of alcohol with one of benzol. Aqueous sodic hydrate dissolves it with a red color, and hydrochloric acid throws down from this solution the original sub- stance apparently unaltered. Strong sulphuric or strong nitric acid dissolves it, but strong hydrochloric acid does not. The constitution of this substance is CH3, N02, C6HSNII, NO,,, N02, 1, 2, 3, 4, 6, as is shown by its preparation from the metabromtrinitro- toluol, the constitution of which has been determined, as given earlier in this paper. 256 PROCEEDINGS OF THE AMERICAN ACADEMY XXI. CONTRIBUTIONS FROM THE CHEMICAL LABORATORY OF HARVARD COLLEGE. ON THE ACTION OF SODIUM MALONIC ESTER UPON TRIBROMTRINITROBENZOL. By C. Loring Jackson and George Dunning Moore. Presented May 28, 1889. In a previous paper * one of us with J. F. Wing described the prepa- ration of tribromtrinitrohenzol, and announced that its action with sodium malonic ester would be studied. This work promised to be of especial interest, because we hoped that each of the bromine atoms would be replaced by the radical CH(COOC2EL)2, and that by the reduction of the substance thus formed a compound might be obtained consisting of three pyrrol molecules united to form a central benzol ring, a sort of triple indol. Our first experiments, however, showed that the reaction did not run in the way we had expected, but instead of the removal of all three of the bromine atoms only two were re- placed, one by the radical CH(COOC2H5)2, the other by hydrogen giving a product with the following formula, C6HBr(N02)3CH(COOC2H5)2, that is, bromtrinitropheuylmalonic ester. After we had established the composition of this substance, we decided that it was unwise to undertake a complete study of this trinitro compound, which can be obtained only with a very considerable outlay of time and material, when the corresponding dinitro compound can be made much more easily, and resembles it closely in most respects. "We have accord- ingly confined our work principally to those properties of the trinitro componnd in which we have observed marked differences from the corresponding ones of the dinitro body, and for a fuller discussion of those properties which the two substances have in common would * These Proceeding, xxiii. 138. OF ARTS AND SCIENCES. 257 refer the reader to a paper " On the Action of Sodium Malonic Ester on Tribromdiuitrobenzol " by one of us and W. S. Robinson.* The results described in this paper can be briefly stated as follows. Sodium malonic ester forms in the cold with tribromtrinitrobenzol bromtrinitrophenylmalonic ester, C6HBr(N02)3CH(COOC2H.)2, melting point 104°-105°, which has acid properties forming salts even with aqueous solutions of the alkaline carbonates. Of these the red soluble sodium salt has been studied, and its analysis led to the formula C6HBr(N02)3CNa(COOC2H5)2. The yellow insoluble copper salt, on the other hand, gave no con- stant result on analysis, but on several occasions, in trying to make it from a solution of cupric chloride in alcohol and the sodium salt, a crystalline substance free from copper was obtained melting in the neighborhood of 75°. Unfortunately the end of the term has pre- vented us from studying this substance, which is the more interesting because no similar compound has been obtained from the correspond- ing dinitro body. The reactions by which the bromtrinitrophenylmalonic ester is derived from tribromtrinitrobenzol have been made out as follows: — C6Br3(NO.,)3 + 3 CIINa(COOC2H3)2 = NaBr + CGBr.,(N02)3CH(COOC2H5)2 + 2 CHNa(COOC2H.)2 = CGBr2(N02)3CNa(c60C2H5)., + CH2(COOC2H5)2 ' + CHNa(COOC2rL)2 + NaBr = C6HBr(N02)3CNa(COOC2IL)2 + CIIBr(COOC2H5)2 " + CHNa(COOC2H5)2 + NaBr = C6HBr(N02)3CNa(COOC2H5)2 + 2NaBr + C2H2(COOC2II,)4. The acetylentetracarbonic ester formed according to the last re- action was obtained from the oily secondary product of the action by distillation under diminished pressure, and identified by its melting point and analysis. Perhaps the most striking difference between the dinitro and trini- tro compounds consisted in the fact that the trinitro ester, or its salts, when heated with an excess of common strong nitric acid, turned bright blood-red, whereas no such action could be obtained from the dinitro compound. The red product, on crystallization from alcohol, * These Proceeding, xxiv. 1. vol. xxiv. (s. s. xvi ) 17 258 PROCEEDINGS OP THE AMERICAN ACADEMY was converted into colorless crystals melting at 125°, and as they melted becoming blood-red and increasing very much in volume. The study of this curious substance is still unfinished : we have only established the fact that it is an ester. If the action of the nitric acid is long continued, another body is formed melting at 156° to a color- less liquid, and dissolving in aqueous sodic hydrate with a red color. Sulphuric acid of specific gravity 1.44 converts the ester into the metabromtrinitrotoluol melting at 143°-144°, recently discovered in this laboratory by Bentley and Warren. The trinitrophenylendimalonic ester (melting point 123°), C6H(N02)3[CH(COOC2H5)2]2, was also obtained by the further action of sodium malonic ester on bromtrinitrophenylmalonic ester ; strangely enough, it has less marked acid properties than the bromine compound, from which it is derived. Preparation of Bromtrinitrophenylmalonic Ester. The tribromtrinitrobenzol used for this purpose was prepared according to the method already given by one of us and J. F. Wing;* we have found, however, that if the proportion of fuming sulphuric acid is increased, a better yield is obtained. The proportions finally used were, 20 grs. of tribromdinitrobenzol, 500 c.c. of the nitric acid of 1.52 specific gravity, and 200 c.c. of fuming sulphuric acid, instead of one third the volume of the nitric acid as previously recommended. The yield obtained from the new proportions was in the neighborhood of 40 per cent of the theory, running in one case as high as 45 per cent, whereas the proportions recommended by one of us and Wing gave on the average from 15 to 20 per cent, and only in a single instance ran as high as 40 per cent. To convert the tribromtrinitrobenzol into bromtrinitrophenylmalonic ester, one molecule of it must be treated with about three molecules of sodium malonic ester. In practice we found it convenient to pro- ceed as follows. 10 grs. of tribromtrinitrobenzol were dissolved in about 200 c.c. of benzol with the aid of heat, mixed, while the solu- tion was still moderately warm, with 10.6 grs. of malonic ester pre- viously converted into the sodium compound by treatment with the sodic ethylate from 1.7 grs. of sodium (a slight excess over the calcu- lated amount) and about 15 c.c. of absolute alcohol, and the mixture * These Proceedings, xxiii. 139. OP ARTS AND SCIENCES. 259 allowed to stand 40 to 60 hours in a corked flask at ordinary tem- peratures. As soon as the sodium malonic ester was added, the liquid became dark blood-red, and on standing this color gradually increased in intensity, while at the same time a precipitate of sodic bromide was thrown down. The product of the reaction was mixed with about three quarters of a litre of water, and acidified with dilute sulphuric acid,* which decomposed the red salt, setting free the ester. Ether was then added, and, after shaking thoroughly, the ethereal and benzol solution separated from the aqueous liquid, which was ex- tracted once more with ether. On distilling off the ether and benzol from the extract, a dark oily residue was left, which was mixed with a little alcohol, when, upon stirring, it solidified to a mass of prismatic crystals. These were sucked out on the pump, washed with a little cold alcohol to remove the adhering oil, and purified by crystallization from hot alcohol, till they showed the constant melting point 104°- 105°. The oil which was sucked out from the crystals, or removed from them by alcohol, upon standing, deposited an additional amount of the substance, which was purified in the same way as the main portion. The substance, after being dried in vacuo, was analyzed with the following results : — I. 0.2235 gr. of the substance gave on combustion 0.28G0 gr. of carbonic dioxide, and 0.0629 gr. of water. II. 0.1930 gr. of the substance gave 16.2 c.c. of nitrogen at a tem- perature of 21°, and under a pressure of 775.9 mm. III. 0.2548 gr. gave 20.1 c.c. of nitrogen at 18°.5, and 784 mm. pressure. IV. 0.2080 gr. gave by the method of Carius 0.0870 gr. of argentic bromide. V. 0.2512 gr. gave 0.1034 gr. of argentic bromide. Calculated for Found. CfiHBr(N02)3CH(C00C2H5)2. I. II. III. IV. V. Carbon 34.67 34.89 Hydrogen 2.67 3.13 Nitrogen 9.33 9.75 9.38 Bromine 17.78 17.80 17.52 The yield was good, when compared to that obtained in similar preparations from other substances ; the best result was as follows : * Dilute nitric acid, which was used in some of the earlier preparations, seemed to diminish the yield. 260 PROCEEDINGS OP THE AMERICAN ACADEMY 10 grs. of tribromtrinitrobenzol, treated as described above with 10.6 grs. of nialonic ester, gave 6.4 grs. of bromtrinitropbenyloialonic ester. The amount required by theory, if all the tribromtriuitrobenzol had been converted into bromtrinitrophenyl malonic ester, is 10 grs. ; there- fore the yield is 64 per cent of the theoretical. The average yield was between 50 and 60 per cent of the theoretical. Properties. — The bromtrinitrophenylmalonic ester crystallizes in white slender needles arranged in radiating groups, which, when ex- amined with the microscope, are seen to be flat needles, or long plates terminated by one plane, or, as commonly, by two at an obtuse angle to each other. The crystals seem to belong to the monoclinic system. The melting point is 104° to 105°, and if heated to 160° the substance becomes dark red, and gives off gas. It is essentially insoluble in cold water, very slightly soluble in hot ; insoluble in ligroine ; slightly soluble in ether ; not very soluble in cold, freely in hot ethyl or methyl alcohol ; freely in benzol, carbonic disulphide, or glacial acetic acid ; very freely in chloroform or acetone. Hot alcohol is the best solvent for it. Strong hydrochloric acid has no action upon it, even when the substances are warmed together in open vessels ; it is prob- able, however, that in sealed tubes the same decomposition would take place as that observed with the corresponding dinitro body. Strong sulphuric acid dissolves a little in the cold, more when hot, forming a colorless solution. Strong nitric acid has little or no action in the cold, but, if warmed with it, converts it into an intensely red viscous substance swimming in the red acid liquid, which by further action of strong nitric acid becomes solid and crystalline. A fuller discussion of the action of strong nitric acid and that of dilute sulphuric acid will be found later in this paper. As was to be expected from the position of one of its hydrogen atoms on a carbon surrounded by two carboxylester radicals and a trinitrophenyl group, the substance possesses marked acid properties. Sodic hydrate in excess gives only a pale red color with the solid ester, owing to the very slight solubility of the sodium salt in sodic hydrate, but upon adding water the coloration increases, and the addi- tion of a few drops of alcohol produces a very dark red solution. Potassic carbonate in aqueous solution gives a slight red color, on the addition of a little alcohol a dark red solution ; acid sodic carbonate acts in much the same way. but the color produced by the aqueous solution is paler than that given with potassic carbonate. Amnionic hydrate gives a red color at once, but this cannot be obtained free from ammonia by evaporation on the water bath, or by using an excess OF ARTS AND SCIENCES. 261 of the ester. The behavior of such a solution made by using an ex- cess of the ester with amnionic hydrate was studied nevertheless, and the following are the more characteristic precipitates which were obtained : — Magnesium salt, pale rust-colored. Calcium salt, pale red flocks. Strontium salt, like that obtained from calcium, but not so heavy a precipitate. Barium salt, an even less heavy precipitate than that obtained with strontium, also less flocculent. Manganese salt, yellowish brown. Zinc salt, pale red. Cobalt or Nickel salts, yellowish. Ferric salt, rust-colored. Capric salt, a rusty red to orange. Mercuric chloride, yellowish brown. Mercuric nitrate, rust-colored. Mercurous salt, rusty precipitate mixed with the black product from the excess of amnionic hydrate. Cadmium salt, yellowish red. Lead salt, brilliant rust-color. Silver salt, vivid brown (" Bismarck brown"). The most characteristic point in its behavior with reagents is that the magnesium and calcium salts are less soluble than the strontium and barium salts, the order of solubility being magnesium and calcium least soluble, strontium more soluble, barium the most soluble. A similar observation has been made by Bischoff * in regard to the salts of orthonitrobenzoylmalonic ester, and the bromdinitrophenylacetacetic ester also exhibits the same peculiarity, as we mention in detail in the next paper of this series. Salts of Bromtrinitmphenylmalonic Ester. "We had intended at first to make a ra;her thorough study of the salts of the bromtrinitrophenylmalonic ester, but after a few experi- ments became convinced that this would be a waste of time, as, owing to the ease with which the atom of bromine can be removed, no very satisfactory analytical results could be obtained ; and we were the more ready to give up this part of the work, because our investigation of the secondary oily product of the reaction, by which the bromtrini- * Ann. Chem., ccli. 3G2. 262 PROCEEDINGS OF THE AMERICAN ACADEMY trophenylmalonic ester is formed, had settled beyond a doubt the com- position of the ester, which before this and the similar investigation made by one of us and W. S. Robinson had rested principally on the analyses of its salts (see these Proceedings, xxiv. 4). We have confined ourselves therefore to a single analysis of the sodium salt, and a preliminary study of the copper salt, the results of which are given below. Sodium Salt, C6HBr(N02)3CNa(COOC2H5)2. — This substance was made in two ways. First, by digesting solid pure sodic carbonate with a solution of bromtrinitrophenylmalonic ester in absolute alcohol. The red solution was filtered from the excess of sodic carbonate, evaporated to dryness on the water bath, and dried at 100°, when it gave the following result on analysis : — 0.2373 gr. of the salt gave after being heated with sulphuric acid 0.0418 gr. of sodic sulphate. Calculated for C6HBr(N02)3CNa(C02C2H5)a. Found. Sodium 4.87 5.71 The bad result is probably due to a slight excess of sodic carbonate, which dissolved in the alcohol. The salt looked black and somewhat decomposed. The second and better method was that used for making the salt of the corresponding dinitro compound, that is, by the action of an alco- holic solution of sodic hydrate or ethylate on an alcoholic solution of the ester, taking care that the ester is in excess. For the necessary precautions see these Proceedings, xxiv. 7. No analysis was made of this preparation, as from our experience with the acetacetic com- pound we were sure that no accurate analytical results would be obtained. Properties. — The sodium salt forms an amorphous blackish red mass, soluble in ethyl or methyl alcohol, water, or acetone ; tolerably soluble in ether; slightly in chloroform ; insoluble in benzol or ligroine. All the solutions have a deep blood-red color. When the salt is treated with an excess of strong nitric acid (of specific gravity 1.36), it is at first decolorized, but almost immediately turns vivid red owing to the formation of the substance produced by warming the free ester with nitric acid. This behavior is characteristic, as it appears with none of the similar substances which we have studied. Copper Salt. — We took up the study of this salt in the hope of throwing light on the composition of the ester, but after analyzing OF ARTS AND SCIENCES. 263 several samples were convinced that the precipitate had a varying composition, and therefore describe our work only because of a curious observation made in the course of it. The salt was made by adding a solution of cupric sulphate to an alcoholic solution of the sodium salt, which need not be free from sodic hydrate ; the copper salt was ex- tracted with ether, and obtained on evaporating the ethereal eolutiou as an orange mass, which when heated exploded with a blue flame. It was insoluble in water, nearly insoluble in cold alcohol, soluble in hot, and the yellow solution deposited the salt in rhombic crystals ; very soluble in benzol or chloroform ; insoluble in ligroine. AVe next substituted an alcoholic solution of cupric chloride for the cupric sulphate, in hopes of getting a better result, when to our sur- prise a product was obtained crystallizing from alcohol in long white prisms, and melting in the crude state at 75°. This product was ob- tained more than once, but as frequent crystallization was necessary to purify it, we did not at first have enough to bring it into a state fit for analysis ; and, on returning to the subject after some mouths, we obtained under the same conditions nothing but the orange explosive copper salt. .Unfortunately, we had postponed work on this subject till so near the end of the term that we were unable to give it the careful study it seems to deserve, but its investigation will be continued in this laboratory next year. Study of the Reactions by which Bromtrinitrophenylmalonic Ester is formed. The reactions by which the bromtrinitrophenylmalonic ester is formed from the tribromtrinitrobenzol must consist in the replace- ment of one of the atoms of bromine by the nialonic ester radical CH(COOC2IL)2, and of another by hydrogen. The first of these pro- cesses needs no explanation, but the mechanism of the second, the replacement of the bromine by hydrogen, could be made out only by experiment. Obviously, the first point to be settled was the form in which the bromine was eliminated ; that is, whether as sodic bromide alone, or partly as sodic bromide and partly as an organic com- pound. For this purpose the following quantitative determinations were made : — I. 10 grs. of tribromtrinitrobenzol, treated with the sodium malonic ester from 15 grs. of malonic ester, gave after standing two davs and a half 8.83 grs. of argentic bromide, corresponding to 3.76 grs. of bromine. 264 PROCEEDINGS OF THE AMERICAN ACADEMY II. The same weights under the same conditions gave 9.08 grs. of argentic bromide, corresponding to o.SG grs. of bromine. If two atoms of bromine had been removed, the amount of bromine should have been 3.55 grs. Therefore the percentages of the theo- retical bromine removed as sodic bromide were, — I. ii. 105.9 108.8 It appears, therefore, that a little more than the amount calculated for two atoms of bromine has been removed as sodic bromide, and this is easily explained by the observation described later in this paper, that sodium malonic ester can act on the bromtrinitrophenylmalonic ester even in the cold to form the trinitrophenylendimalonic ester, a small quantity of which was undoubtedly formed in these two experi- ments by the large excess of sodium malonic ester present. At any rate, there can be no question that all the bromine was removed in the form of sodic bromide. The next step consisted in determining the nature of the organic secondary product. For this purpose, the oil, separated from the bromtrinitrophenylmalonic ester by sucking out the crude product on the pump and treatment with alcohol, was allowed to stand till it ceased to deposit crystals of the ester, and then submitted to distilla- tion under diminished pressure. The pressure varied from 22 to 25 mm., and a distillate began to appear when the thermometer inside the flask stood at 98°, and was collected until the temperature had reached 1G0°, when about one third of the total volume had passed over. In this way a clear yellow liquid was obtained, which distilled unaltered at ordinary pressure between 197° and 206°. We there- fore inferred it was mostly malonic ester, boiling point 197°. 7, a view of its nature which was confirmed by its smell. As the whole of the distillate passed over below 206°, there could be no large amount ot tartronic ester (boiling point 220°) present, which we had expected after the work of one of us and W. S. Robinson on the corresponding dinitro compound, and the secondary product of the reaction must be looked for in the residue which had been left behind in the flask after the distillation under diminished pressure. This was a thick blackish brown oil, which on standing for about a week deposited crystals all over its surface ; these were removed and allowed to stand on filter paper until a large part of the oil had been sucked out, when they were purified by washing with a small quantity of cold alcohol, and then crystallizing from boiling alcohol, until they showed the constant Carbon Calculated for C2H2( C02C2H6)4. 52.83 Hydrogen 6.92 OF ARTS AND SCIENCES. 265 melting point 76°. The substance formed long glittering colorless needles or prisms, and contained no bromine ; we decided accordingly that it was the acetylentetracarbonic ester (melting point 76°), and this conclusion was confirmed by the following analysis : — 0.2270 gr. of the substance gave on combusion 0.4384 gr. of carbonic dioxide, and 0.1506 gr. of water. Found. 52.67 7.36 The amount of acetylentetracarbonic ester was so considerable, that there can be no doubt it was a principal product of the reactions by which the bromtrinkrophenylmalonic ester is formed, and these must therefore be written thus : — C6Br3(NO.v)3 + 3 CHNa(COOC2H5)2 = C6Br,(XO,)3CH(COOC2H5)2 + NaBr + 2 CHNa(COOC2H5)2 = C6Br2(N02)3CNa(COOC2Hs)2 + CH2(COOC2H.)2 + CHNa(COOC,H5)9 + NaBr = C6HBr(N02)3CNa(COOC2H5)2 + CHBr(COOC2H5)2 " + CHNa(COOC2H5)2 + NaBr = C6HBr(N02)3CNa(COOC2H5)2 + C2H2(COOC2H5)4 + 2 NaBr. The only objection which could be urged against this series of re- actions is that the yield of bromtrinitrophenylmalonic ester is only 64 per cent of the theoretical, from which it might be argued that nearly half of the tribromtrinitrobenzol may have undergone some different transformation. This objection is disposed of, however, by the fact that W. D. Bancroft and one of us * have succeeded in getting a yield of 80 per cent of the dibromdinitrophenylmalonic ester from tetrabromdinitrobenzol by a series of reactions exactly analogous to those just given. The missing 36 per cent of the bromtrinitrophenyl- malonic ester must therefore have remained dissolved in the oil, and have been destroyed by the distillation even under the diminished pressure used by us. Action of Nitric Acid. The intense red color produced by the action of nitric acid of spe- cific gravity 1.36 on the sodium, or copper salt of the bromtrinitrophe- nylmalonic ester in the cold, or on the ester itself at 100°, seemed to * These Proceedings, xxiv. 295. 266 PROCEEDINGS OP THE AMERICAN ACADEMY us of great interest, and we laid out what we thought would be time enough for its investigation ; unfortunately, however, this was not the case, since, after the work had been going on for some time, we found that at least two substances were formed by this reaction, and conse- quently the end of the term surprised us before we had reached any definite results. We have decided, however, to publish here what results we have obtained, as we are unable to go on with this work together, but wish it to be understood that all these statements are to be taken as preliminary. If about 1 gr. of bromtrinitrophenylmalonic ester was mixed with 2-3 c.c. of strong nitric acid (specific gravity 1.36), no change took place in the cold ; but if the mixture was warmed gently on the water bath for less than five minutes, an intense vivid red color appeared in both the acid liquid and the organic substance, which melted and became converted into a viscous mass. If now the acid was poured off, a fresh quantity added, and the gentle warming repeated, the vis- cous drop became converted into a red crystalline mass, and by con- tinuing* this treatment with successive portions of nitric acid the red color could be removed partially, so that the product had a spotted red and white appearance. This frequent treatment with nitric acid was, however, unnecessary, as the red crystalline product after the second warming with nitric acid gave, when crystallized from alcohol, well formed white prisms, and a reddish mother liquor. The red nitric acid poured off from the principal part of the product gave with water a red precipitate, but a better mode of treatment seemed to be to evapo- rate this red acid to dryness on the water bath. The residue, or pre- cipitate obtained with water, was partly viscous, partly crystalline, and by treating it again with warm strong nitric acid a new quantity of the red crystalline substance was obtained, but the amount recov- ered in this way was so small that it hardly paid for the trouble. The white crystals, after purification by crystallization from alcohol, showed the constant melting point 125°, and their behavior in melting was very characteristic, as they turned from white to bright red, and swelled to many times their original volume. They were not affected by sodic hydrate in aqueous solution. Supposing that the substance was homogeneous because of its constant melting point, we analyzed it, but on studying its properties more carefully we began to doubt its purity for the following reasons : — First. Although the microscopic examination showed that the substance consisted principally of white, short, rather thick monoclinic prisms, usually with both terminations well developed and made up of two planes, there were mixed with OP ARTS AND SCIENCES. 2G7 these longer prisms, and we could not decide whether these latter were a different substance or merely a different habit of the same. Second. When the crystals were treated with sodic hydrate and alco- hol a little of a soluble red salt was formed around each crystal, but we could not convert the whole of the crystals into this salt. This seemed to point to the presence of an impurity, from which the salt was formed. Third. We found almost at the very end of the term, that by warming the bromtrinitrophenylmalonic ester with strong ni- tric acid for three hours, instead of a few minutes, a red substance was obtained, which crystallized from alcohol, became white, and melted at 156° instead of 125°, and, what was as distinctive as the different melting point, fused to a colorless liquid, and gave a red solution with aqueous sodic hydrate. This substance was discovered so late that we had no time to investigate it, but some of it seemed to be formed even on shorter heating (15 minutes) with the nitric acid. For these reasons, we have decided that it is wiser to postpone the publication of our analyses of the substance melting at 125° until the work has been repeated with samples in regard to the purity of which there can be no doubt. We add such results of our work as are established with certainty. The analyses made by us showed that there were three atoms of nitrogen to one of bromine in the substance, and there- fore the action of the nitric acid did not consist in the introduction of another nitro, or nitroso group. The fact that it is insoluble in aqueous sodic hydrate shows that it is not a free acid, and its action with hydrochloric acid would indicate that it was an ester, as, when heated to 135°-140° with this acid in a sealed tube for 36 hours, a gas was given off burning with a green-bordered flame, and giving a white precipitate with lime-water, which therefore must have contained ethyl chloride and carbonic dioxide. The solid product of this action was partly viscous and partly crystalline ; the latter melted in the crude state above 180°. It has been stated already that the substance melting at 125° turns red aud increases in volume when it melts; this change, which takes place to a limited extent even when it is kept at 100° for some time, is accompanied by loss of weight, as a sample kept at its melting point for some days lost at least 17 per cent, and gave a residue consisting of two or more substances, one white and crystalline, the other red and viscous. 268 PROCEEDINGS OP THE AMERICAN ACADEMY Action of Sulphuric Acid. — Constitution of the Bromtrinitrophenyl- malonic Ester. The action of dilute sulphuric acid upon the bromtrinitrophenyl- malonic ester was studied in the hope of obtaining the as yet un- known bromtriuitrophenylacetic acid, as it had been found by one of us and W, S. Robinson f that the corresponding dinitro compound was decomposed in this way. For this purpose, about 2 grs. of the ester were boiled in a flask under a return condenser with sulphuric acid of specific gravity 1.44 and boiling point 132° until the ester had dis- solved ; the liquid was then allowed to cool, when it deposited crystals, which, after recrystallization from alcohol, were recognized by their melting point 143°-144°, their appearance, and the absence of acid properties, as the metabromtrinitrotoluol discovered in this laboratory by Bentley and Warren. It is evident therefore that the bromtrinitrophenylacetic acid is less stable than the corresponding dinitro compound, as indeed was to be expected, and was broken up as soon as formed into the substituted toluol and carbonic dioxide according to the following reaction : CGHBr(N02)3CH2COOH = C6HBr(N02)3CH3 + CO,. The formation of this substance would settle the constitution of the bromtrinitrophenylmalonic ester, if that were necessary, but the preparation of the ester from symmetrical tribromtrinitrobenzol leaves no doubt as to its constitution, which must be as follows, CH(COOaH-).,, N02, Br, NO,, H, NO,, I, 2, 3, 4, 5, 6, and Bentley and Warren have established the corresponding constitution for their substituted toluol. Trinitrophernjlendimalonic Ester, CcH(N02),[CH (COOC2H5),]2. This substance was formed by the further action of sodium malonic ester on bromtrinitrophenylmalonic ester. For this purpose, 1 gr. of bromtrinitrophenylmalonic ester dissolved in ether was mixed with 1.5 grs. of malonic ester previously converted into sodium malonic ester and dissolved in much absolute alcohol, and the mixture boiled in a flask with a return condenser for an hour. The product, which was very dark brown, almost black, was treated with water, acidified with dilute sulphuric acid avoiding a large excess, the ether removed with a drop funnel, and the aqueous liquid shaken out twice with ether. The extract, after distilling off the ether and allowing it to t These Proceedings, xxiv. 240. OF ARTS AND SCIENCES. 269 get perfectly cool, was treated with a little alcohol, when crystals separated on standing, which were purified by recrystallization from alcohol, until they showed the constant melting point 123°. They gave no test for bromine when heated on a copper wire, and, after drying in vacuo, were analyzed with the following results : — I. 0.3004 gr. of the substance gave on combustion 0.5043 gr. of carbonic dioxide, and 0.1230 gr. of water. II. 0.2392 gr. of the substance gave 1 6.8 c.c. of nitrogen at a tem- perature of 25° and a pressure of 768 mm. Calculated for Found. CeHlNO^^CIKCOOC.IIs).,]^ I. II. Garbon 45.37 45.78 Hydrogen 4.35 4.55 Nitrogen 7.94 7.92 A small quantity of this substance can also be formed in the cold, and more than once some of it has been obtained in making the bromtrinitrophenylmalonic ester by the process described earlier in this paper (compare pages 258 and 264). Properties. — The trinitrophenylendimalonic ester crystallizes from alcohol in long colorless prisms, terminated by a single rhombic plane at a tolerably sharp angle to the sides ; less frequently, the termination consists of two planes at an obtuse angle to each other, so that the general effect is as if the prisms had rounded ends. They are fre- quently grouped, or twinned, parallel to their long axes, so that often there are two or more terminations at one end of a group. The sub- stance melts at 123°; and is very nearly, if not quite, insoluble in water, whether cold or boiling; essentially insoluble in ligroine ; not very soluble in cold ethyl or methyl alcohol, freely in either of these solvents when hot ; very slightly soluble in carbonic disulphide ; soluble in ether or glacial acetic acid ; and freely soluble in benzol, chloroform, or acetone. Its acid properties are not so strongly de- veloped as we expected. An aqueous solution of soilic hydrate turns the solid pale red, but does not dissolve it to any extent ; if, however, sodic hydrate is added to its alcoholic solution, it at once takes on a dark brownish red color, much browner than any of the similar salts which we have studied. — in fact it would be possible to recognize the salt by this color. An aqueous solution of potassic car- bonate gives a very faint red color with it, which is increased, but not to a great extent, by adding alcohol to the aqueous solution. The action was incomplete at best ; acid sodic carbonate had no action on 270 PROCEEDINGS OP THE AMERICAN ACADEMY it in aqueous solution, but on the addition of alcohol a barely per- ceptible red color appeared. Amnionic hydrate even in dilute aqueous solution dissolved it easily with a brown color ; the solution turned blacker when the attempt was made to drive off the excess of ammo- nia on the water bath, and a white scum formed on the surface, probably the original substance. The behavior of this solution was studied with some of the commoner reagents ; but, as it showed such evident signs of decomposition, we did not think it worth while to extend this work to salts of all the basic radicals. Ferric salt, cupric salt, silver salt, and lead salt all gave brown ilocculent precipitates. Calcium salt gave no precipitate. Barium salt, a very slight dirty brown precipitate, but none if the solution had not been warmed on the water bath in the vain attempt to drive off the excess of ammonia. Strong sulphuric acid dissolved the dimalonic ester, giving a color- less solution. Strong hydrochloric acid had no action upon it, whether hot or cold. Strong nitric acid dissolved it partially in the cold, giving a yellowish solution, which when warmed became darker yellow ; but if the warming on the water bath was continued for some time, the acid liquid became red, and a red viscous substance was also obtained, which, after washing with water and crystallization from alcohol, was converted into yellow plates melting at 104°-105° in the crude state. It is evident that the action here is similar to that of bromtrinitrophenylmalonic ester with strong nitric acid, but the end of the term has prevented us from continuing the study of this sub- stance at present. OF ARTS AND SCIENCES. 271 XXII. CONTRIBUTIONS FROM THE CHEMICAL LABORATORY OF HARVARD COLLEGE. ON THE ACTION OF SODIUM ACETACETIC ESTER UPON TRIBROMDINITROBENZOL. By C. Loring Jackson asd George Dunning Moore. Presented May 28, 1889. After the action of sodium malonic ester ou tribromtrinitrobenzol and on tribromdinitrobenzol had been studied, it seemed of interest to determine whether sodium acetacetic ester acted in the same way, and the following paper contains the results of experiments undertaken with this intention upon the tribromdinitrobenzol, which was selected because it can be prepared so much more easily than the correspond- ing trinitro compound. These results can be summarized briefly as follows. Tribromdinitrobenzol behaves with sodium acetacetic ester in the same way that it does with sodium malonic ester ; that is, one atom of its bromine is replaced by the acetacetic radical CH3COCHCOOC2H5, and a second by hydrogen, while the third remains unaltered ; so that the product of the action is the bromdinitrophenylacetacetic ester, C6H2Br(N02)3CH3COCIICOOC8Ha, or to speak more accurately its sodium salt, CTI2Br(NO,)2CH3COCNaCOOC2H5, The bromdinitrophenylacetacetic ester melts at 96°, and possesses marked acid properties, forming the sodium salt whose formula has just been given, even with acid sodic carbonate in aqueous solution. The salt has a red color, and is soluble in water ; in fact, it resem- bles the sodium salt of the corresponding malonic compound most closely. 272 PROCEEDINGS OP THE AMERICAN ACADEMY The broradiuitrophenylacetacetic ester is saponified and decomposed by heating with sulphuric acid of specific gravity 1.44, giving the bromdinitrobenzylmethylketone, C6H2Br(N02)2CH2COCH3, but no trace of the corresponding acetic acid. This ketone melts at 112°— 1 13°, and also possesses acid properties, giving a purplish red salt soluble in alcohol, but decomposed almost completely by water. The acid properties of the ketone are less marked than those of the acetacetic ester, as was to be expected, since the hydrogen, which is replaced by basic radicals, is subject to the influence of an acetyl, a carboxylester, and a dinitro phenyl group in the acetacetic compound, only to those of an acetyl and a dinitro phenyl group in the ketone. The bromine of the ketone can be replaced easily by the aniline radical C6H.NH, forming anilidodinitrobenzylmethylketone, C6H2(C6H5NH)(N02)2CH2COCH8, which melts at 131°, and has not lost all acid properties, although they have been much weakened by replacing the bromine atom by the basic radical CCH.NH. It cannot form an ammonium salt, but the sodium salt can be easily obtained in alcoholic solution, and on analysis gave a number corresponding to the formula CJIJ(CtiH5NH)(NO,),CHNaCOCH3. It is completely decomposed by water, but dissolves in alcohol with a brown color. Both these ketones, therefore, show stronger acid properties than desoxybenzoine C6H.COCH2C6H5, the metallic compounds of which, according to Victor Meyer,* could not be isolated ; we are inclined to ascribe this to the presence of the nitro groups in the phenyl, which would heighten its acid-producing power, but it may also be due in part to the fact that those ketones contain the acetyl group, which, as Claisen and Ehrhardtf have pointed out, has a greater influence in producing acidity than the benzoyl radical contained in desoxy- benzoine. The hydrazone of the anilirlodinitrobenzylmethylketone, C6II.2(C6tI5NII)(N02)2CII2C(NNHC6H5)CH3, was also prepared, and melted at 140°. The full details of the work will be found in the remainder of the paper. * Ber. d. ch. G. 1888, p. 1291. t Ber. d. ch. G. 1889, p. 1019. OF ARTS AND SCIENCES. 273 Preparation of Tribromdinitrobenzol. The method used by us for preparing tribromdiuitrobenzol differs from that formerly, in use only in certaiu details, but, as careful atten- tion to these details insures a purer product at much less expense of time and labor, we have thought it best to give a full account of our mode of procedure. To make the tribromaniliue, GO grs. of aniline were dissolved in dilute hydrochloric acid, and, the solution having been made up to a volume of about 3 litres, a rapid stream of air saturated with bromine vapor was sucked through it by means of a Bunsen pump, until the liquid assumed a distinct yellow color. The precipitate of tribrom- aniliue was then removed by straining through cheese-cloth, and washed with a stream of common water, until free from acid, when the greater part of the water was squeezed out with a screw press, and the product thoroughly dried on a steam radiator. In this way a quantitative yield of the tribromaniliue was obtained, and it was free from colored by-products. In order to convert the tribromaniline into tribrombenzol, 50 grs. of it, after being pulverized, were dissolved with the aid of heat in about 300 c.c. of common alcohol, and a concentrated aqueous solution of 21 grs. of sodic nitrite poured in slowly, but not in successive portions. The hot mixture was then acidified with dilute sulphuric acid, and allowed to stand over night, when it was filtered, and the precipitate washed with hot water to remove the sodic sulphate and leave the tribrombenzol. An additional quantity of this was obtained by con- centrating the alcoholic filtrate, when it separated as an oil, that solidi- fied on standing, and was then crystallized from alcohol. The yield was nearly quantitative, as 45.50 grs. of tribrombenzol were obtained instead of the 47.77 required by the theory, that is 95 per cent. When made by this method, the tribrombenzol was usually pure enough to be nitrired directly in spite of its brownish color.* * The amount of sodic nitrite used in the process described above (two mole- cules of nitrite to one of the base) is twice that required by the theory, but we have found that this larg-e excess was necessary to bring all the tribromaniline into the reaction. When a smaller amount of nitrite was used, the product was much less pure, as shown by its lower melting point ; it was necessary in this case to distil it from a little retort, and crystallize several times from alcohol, to obtain pure tribrombenzol. The crystals obtained on evaporating the alcoholic mother liquors, which made up about two thirds of the entire amount, were dis- tilled with steam, pushing the distillation as rapidly as possible, when tribrom- benzol passed over, and tribromaniline was left in the retort ; but all this tedious purification can be avoided by using the excess of nitrite recommended above, vor.. xxiv. (y. s. xvi.) 18 274 PROCEEDINGS OP THE AMERICAN ACADEMY To convert the tribrombenzol into the dinitro compound, 25 grs. of it were added to 100-120 grs. of nitric acid* of specific gravity 1.52, (made from potassic nitrate and sulphuric acid in the laboratory.) warmed gently until the solid had dissolved, and allowed to stand about two hours, when tbe tribromdinitrobenzol crystallized out in large white prisms. The yield was essentially quantitative. Bromdinitroph enylacetacetic Ester, C6H2Br(N02)2CH3COCHCOOC.2Hs. Preparation. — This substance was made by the action of an alco- holic solution of sodium acetacetic ester on a benzol solution of the tribromdinitrobenzol in the proportion of about four molecules of the former to one of the latter. For this purpose 15 grs. of tribromdini- trobenzol were dissolved in about 200 c.c. of benzol, and mixed with 20 grs. of acetacetic ester previously treated with 3 grs. of sodium dissolved in about 20 c.c. of absolute alcohol. At first there was very little change of color, but on standing at ordinary temperatures the liquid turned first yellow and then red (whereas with malonic ester the red color appeared instantaneously). In order to complete the reaction, the mixture was heated on the steam bath for about one hour, at the end of which time it had become nearly black, and a con- siderable precipitate of sodic bromide had formed. It was then mixed with from one and a half to two litres of water, and the reddish benzol solution, which was precipitated, removed from the dark red aqueous liquid ; the latter was then acidified with dilute sulphuric acid,- taking care to avoid a large excess ; this decomposed the red sodium salt of the new substance, which was set free in the form of a yellowish oil, and extracted by shaking the liquid with ether twice. On distilling off the ether a dark reddish brown oil was left, which, when cold, was treated with very little alcohol, and upon stirring became filled with crystals, the quantity of which increased on standing for twelve or more hours. When the quantity of the crystals did not increase further, the pasty mass was sucked out on the pump, first adding a little alcohol, if necessary, and by washing with a small quantity of cold alcohol all the very soluble red oil was removed from the crys- tals, which were nearly or quite insoluble in cold alcohol, and were next purified by crystallization from hot alcohol until they showed the constant melting point 96°. An additional quantity of the substance can be obtained from the benzol solution by distilling off the benzol * These Proceedings, xxii. 374. OP ARTS AND SCIENCES. 275 and treating the residue with sodic hydrate and a little alcohol, which convert the new substance into its sodium salt, and this can be re- moved from the unaltered tribromdinitrobenzol by washing with water ; when the wash-waters were acidified, and the precipitate puri- fied in the same way as the maiu portion, the substance was dried in vacuo, and analyzed with the following results : — I. 0.2683 gr. of the substance gave on combustion 0.3788 gr. of carbonic dioxide, and 0.0748 gr. of water. II. 0.2512 gr. of the substance gave 16.7 c.c. of nitrogen at a tem- perature of 22° and a pressure of 759.7 mm. III. 0.2067 gr. of the substance gave, according to the method of Carius, 0.1041 gr. of argentic bromide. IV. 0.2141 gr. of the substance gave 0.1059 gr. of argentic bromide. Calculated for Found. C6H„Br(N02),CH3COOHCO,C,H5. I. II. III. IV. Carbon 38.41 38.50 Hydrogen 2.93 3.09 Nitrogen 7.47 7.33 Bromine 21.33 21.43 21.05 The yield of bromdinitrophenylacetacetic ester, prepared by the method described above, is satisfactory on the whole, the best result being as follows : — 15 grs. of the tribromdinitrobenzol yielded 6.5 grs. of the ester, and 3.1 grs. of unaltered tribromdinitrobenzol were recovered, leaving 11.9 grs. which had entered into the reaction. 11.9 grs. of tribromdinitro- benzol should yield 11.0 grs- of bromdinitrophenylacetacetic ester. The actual yield, therefore, was 59 per cent of the theoretical. In other preparations the yield varied from 54 to 34 per cent, the lowest which was obtained from this process. The yield was not improved by increasing or by diminishing the proportion of acetacetic ester to the tribromdinitrobenzol. In our first preparations the reaction was allowed to run in the cold, as an experiment, in which the mixture had been heated less than one hour, seemed to give a very unmanageable product; in this case, however, the yield was very much less than that obtained by the process described above, in which the mixture was heated one hour. In order to throw light on the way in which the reaction runs, we determined the amount of bromide of sodium formed in two prepara- tions as follows : — I. 12 grs. of tribromdinitrobenzol yielded 4.43 grs. of bromine in the form of sodic bromide. 27G PROCEEDINGS OP THE AMERICAN ACADEMY II. 12 grs. of tribromdinitrobenzol yielded 4.40 grs. of bromine in tbe form of sodic bromide. If two atoms of bromine are removed from each molecule by this re- action, 12 grs. of tribromdinitrobenzol would lose 4.74 grs. of bromine. Percentage of bromine removed as sodic bromide, — i. ii. 93.5 93.0 From this it appears that all the bromine removed from the tribrom- dinitrobenzol is finally in the state of sodic bromide, as the sligbt loss of 7 to 6.5 per cent is not greater than wonld be expected when it is considered that the aqueous solution containing the sodic bromide was shaken out twice with ether. These determinations show also that in these cases the whole of the tribromdinitrobenzol entered into the re- action, and in fact none of it could be found unaltered in the products of these two preparations ; but this was not always the case, as, for in- stance, in the preparation described on page 275. The full explanation of the reaction, however, was to be found in the study of its secondary product, the red oil removed from the crys- tals by washing with cold alcohol. This, upon long standing exposed to the air, threw down a few more crystals of bromdinitrophenyl- acetacetic ester, which would raise the yield a little above that given, but the amount obtained in this way was very small. The oil, after no more crystals could be obtained from it, was distilled under di- minished pressure and yielded some acetacetic ester, leaving in the flask a tarry mass which has shown no signs of giving crystals even after long standing. This part of the work therefore was not carried fur- ther, as from the formula of the ester and the removal of all the bro- mine as sodic bromide there can be no doubt that the reaction with acetacetic ester runs in the same way as that with malonic ester, and in this latter case the reaction has been fully explained.* Reasoning on this analogy, the following reactions may be taken as expressing what takes place in the formation of the bromdinitrophenylacetacetic ester. C6HBr3(N02)2 + 2 CH3COCHNaCOOC2H. = ' C6HBr2(Na),CH„COCHCOOC2H5 + NaBr + CH,COCHNaCOOC2H5 = CsIIBr„(N02)2CII3COCNaCOOC2H5 + CH3COCII2COOC2H5 + NaBr = C6n2Br(N02)2CII!COCNaCOOC2II5 + CH,COCIIBrCOOC2H5 + NaBr. * These Proceedings, xxiv. 238, 265. OF ARTS AND SCIENCES. ' 277 The broraacetacetic ester being afterward attacked either by a molecule of sodium acetacetic ester or by sodic hydrate. The only question with regard to these reactions, which might arise would be due to the fact that only a little over 50 per cent (59 per cent) of the ester was obtained, which might lead to the hypothesis that nearly half of the tribromdinitrobeuzol went to form another substance ; but this objection is removed by the fact that in another analogous case as much as 80 per cent of a corresponding ester has been found. We consider, therefore, that the missing 41 per cent of the ester remained dissolved in the oily secondary product, but should state, on the other hand, that upon treating the oil with sulphuric acid of specific gravity 1.44 in hopes of decomposing the secondary products and converting the bromdinitrophenylacetacetic ester into bromdinitro- benzylmethylketone, we obtained nothing but black tarry substances, from which no substance fit for analysis could be obtained. Properties. — The bromdinitrophenylacetacetic ester crystallizes well, usually in forms looking like a rhombohedron with a very acute angle, less frequently in prismatic forms, which are twinned on a cen- tral line parallel to their longer axis, the termination being in shape either like a simple gable, or one with a notch in its point. The crys- tals show a great tendency to twin, or group, often in forms like those of frost, and are sometimes from 2 to 3 mm. long. The sub- stance has a yellow color of about the shade of potassic chromate, which is characteristic, as the corresponding malonic compound is nearly white. Heckmann * has observed a similar deep yellow color in the orthoparadinitrophenylacetacetic ester. It melts at 9G° ; is very slightly soluble in water, rather more so in hot than in cold ; essen- tially insoluble in ligroine ; not very soluble in cold alcohol, but freely in hot ; if anything less soluble in methyl than in common alcohol both cold and hot, but the solubility is much greater in the hot methyl alco- hol than in the same solvent when cold ; tolerably soluble in carbonic disulphide, or ether; soluble in glacial acetic acid; and freely in ben- zol, chloroform, or acetone ; from ether, benzol, or chloroform it is deposited as an oil. The best solvent for it is hot alcohol. Strong sulphuric acid does not act upon it in the cold, but when warm dia solves it, forming a slightly yellowish solution. Strong hydrochloric acid has no action with it in open vessels, even if heated. The de- composition of the substance by these two acids under proper condi- tions is described later in this paper. Strong nitric acid has no action * Ann < hem., ccxx. 133. 278 PROCEEDINGS OF THE AMERICAN ACADEMY on it in the cold, but dissolves it when warm ; there is, however, no marked change of color in which respect this substance shows a strik- ing difference from the bromtrinitrophenylmalonic ester, but resembles the broindinitrophenylmalonic ester. The bromdinitrophenylacetacetic ester shows marked acid proper- ties, as was to be expected from the position of one of its hydrogen atoms upon a carbon adjacent to an acetyl, a enrboxylester. and a phenyl group, the hater rendered still more efficient by the presence of two oitro groups, and also from the acid properties of the corre- sponding malonic compound. Aqueous sodic, or amnionic hydrate dis- solves i: forming a red solution of the corresponding salt ; an aqueous solution of potassie carbonate acts upou it in the same way giving, however, a somewhat fainter color, but, if alcohol is added to the solution, it turns at once dark red; acid sodic carbonate in aqueous solution gives a very faint red color which is much intensified by addition of alcohol to the solution. The red solution of the ester in amnionic hydrate is decomposed by heating, or even by exposure to the air at ordinary temperatures, anil we were uot able to obtain a solution, which did not smell of ammonia, even when a large excess of the ester was used, it is evident therefore that its ammonium salt i- very unstable. We have, however, tried the action of a solution prepared from an excess of the ester and amnionic hydrate with vari- ous reagents, and found the following characteristic reactions. Magnesium or Calcium suit, heavy flocculent precipitate of the color of chrome yellow. Strontium salt, a less heavy precipitate of a redder color. Barium salt, a still smaller precipitate, also reddish. Zinc salt, a pale yellow precipitate. Cupric salt, a pale yellow precipitate. Lead salt, a dark yellow precipitate. Silver salt, a yellowish white precipitate. The most striking thing about these salts is that the calcium salt is i ^ soluble than that oi strontium, and this less soluble than the barium salt. Bischoff* has observed a similar peculiarity in the salts of orthonitrobenzoylmalonic ester, and we have found it in the salts oi' bromtrinitrophenylmalonic ester. With aniline the bromdinitrophenylacetacetic ester gave only a waxy yellow mass, from which there seemed little chance of obtaining a substance in a state tit for analysis. We have, therefore, abandoned * Ann. Chem., ecli. OF ARTS AND SCIENCES. 279 the further study of this reaction, in which undoubtedly the aniline acted on the acetacetic ester radical as well as on the bromine in the benzol ring. That this bromine had been removed we proved by de- tecting aniline bromide among the products of the reaction. Sodium Salt, C0H2Br(NO2)2CH3COCNaCOOC2H5. In the earlier portions of our work on the bromdinitrophenylacet- acetic ester and allied bodies tbe determination of the composition of the salts was of the greatest importance, as this was the only ex- perimental method which we had found for deciding between the formulas, I. C(;H,Br ( N02) 2CH,CO CH COOGH., II. C HI]] ND2)2CH8COCCOOC2H3. This, at present, is no longer the case, as the discovery of acetylen- tetracarbonic ester or tartronic acid as a secondary product in the for- mation of the corresponding malonic compounds can be explained only if a formula similar to I. is adopted, and the easy conversion of bromdi- (or tri-) nitrophenylmalonic ester into the corresponding toluol compound also could hardly be brought into harmony with a formula like II. No similar proof has been applied to the acetacetic com- pound, it is true: but when the close resemblance between this and the malonic compounds is considered, there can be no doubt that they are similarly constituted. The composition of the sodium salt there- fore becomes of secondary importance, and this is fortunate, as we have not succeeded in preparing it in a state of purity sufficient to decide between the salts derived from formulas I. and II., although our analyses leave no doubt as to its composition, if the first formula i> adopted as correct. The salt was prepared by adding to a solution of the bromdiui- trophenylacetacetic ester in absolute alcohol a solution of sodic hy- drate or ethylate also in absolute alcohol, taking care that the ester was in decided excess. The deep red alcoholic solution thus obtained was evaporated rapidly to dryness in a narrow beaker sunk throughout its whole height in a water bath, some ether having been added pre- viously in order that its vapor might protect the solution from the carbonic dioxide of the air until the alcohol began to boil. The excess of ester was washed out of the dry residue with benzol, and the salt dried at 100°, and analyzed with the following results : — I. 0.2102 gr. of the salt gave after treatment with sulphuric ;i 0.0361 gr. of sodic sulphate. 280 PROCEEDINGS OF THE AMERICAN ACADEMY II. 0.2056 gr. of the salt gave 0.0407 gr. of sodic sulphate. III. 0.2531 gr. of the salt gave 0.0390 gr. of sodic sulphate. Calculated for Fouod. C6H2Br(N02)2CH3COUNaC02C,H5. I. IJ. III. Sodium 5.79 5.56 6.41 4.99 It is evident from these results that the method of preparation is unsatisfactory, and we ascribe this to the action of the sodic hydrate (or ethylate) on the bromine, and perhaps also on the acetacetic radi- cal, as, when these two sources of error were removed by using the anilidodinitrobenzylmethylketoue, an excellent result was obtaineii. Bad as these analytical results are, they show that the salt contains but one atom of sodium, and therefore must have the formula which we have ascribed to it. Properties. — The sodium saltof the bromdinitrophenylacetaceiiv- ester forms a brick-red amorphous mass, easily soluble in water, al- cohol, or ether, but insoluble in benzol. Much less freely soluble in a solution of sodic hydrate than in water. Strong nitric acid decom- poses it, giving apparently the unaltered ester. Bromdinitrobenzyhnethylketone (Bromdim'trophenylacetone), C6II2Br(N02)2CH2COCH3. This substance can be made from the bromdinitrophenylacetacetic ester by the action of dilute sulphuric acid in open vessels, or of strong hydrochloric acid in sealed tubes. The method of preparation which gave us the best results was as follows : 2 to 2.5 grs. of bromdinitro- phenylacetacetic ester were boiled with about 200 c.c. of sulphuric acid of specific gravity 1.44, boiling point 132°, in a flask with a return condenser, until all the solid was dissolved, which took usually from one hour to an hour and a half. The yellow solution was then allowed to cool, when it deposited a heavy white flocculent precipitate, which was increased in quantity by diluting largely with water; it was filtered out, and after thorough washing with water was purified by crystallization from alcohol until it showed the constant melting point 112°-113°, when it was dried at 100° for analysis. If the ester used in this process was not perfectly pure, a tarry impurity was formed which could be removed only with great difficulty ; the best plau in such a case was to wash the product with a small quantity (20-30 c.c.) of benzol, which dissolved the ketone more readily than its impurity, but even after this treatment tedious crystallization from alcohol was necessary to obtain a pure substance. OF ARTS AND SCIENCES. 281 The formation of this substance by heating the bromdinitrophenyl- acetacetic ester with hydrochloric acid is not a good method of prepar- ing it, because the process must be carried on in sealed tubes, and also because the product is apt to be contaminated with the tarry impurity just mentioned; but as it throws light on the reaction which takes place, we will describe it briefly: 1 gr. to 1.5 grs. of the ester were sealed in a tube with 20-30 c.c. of pure strong hydrochloric acid, and heated from 130°-150° for two or three hours. Upon opening the tube a gas was evolved, which burnt with a smoky green-bordered flame (ethylchloride), aud also contained carbonic dioxide, as shown by its giving a precipitate with lime-water. The contents of the tubes consisting, in addition to the acid liquid, either of tufts of brown- ish acicular crystals, or a brown oily semi-solid mass, were poured into a large volume of cold water, and the insoluble portions purified as already described. The following analyses were made in part with substance prepared by the hydrochloric acid process, and in part with that made with sulphuric acid : — L 0.2312 gr. of the substance gave on combustion 0.3005 gr. of carbonic dioxide, and 0.0546 gr. of water. II. 0.1638 gr. of the substance gave 14 c.c. of nitrogen at a tempera- ture of 23° and a pressure of 755 mm. III. 0.1862 gr. of the substance gave, according to the method of Carius, 0.1173 gr. of argentic bromide. Carbon ' Calculated for CGH2Br(XO,),< H,UOCH3. 35.64 r. 35.44 Found. II. Hydrogen 2.31 2.62 Nitrogen 9.24 9.57 Bromine 26.40 III. 26.81 It is evident from the analyses and observations given above that the reaction with hydrochloric acid runs as follows: — CGH2Br(N02)2CH3COCHC02CJL + HC1 = C2H3C1 + C02+ C6H2Br(N02)2CH3COCH8; and that the reaction with sulphuric acid must be similar. We had expected that bromdinitrophenylacetic acid would be formed also by these processes, but after a most careful search for it not a trace could be detected; and as its properties are so striking that we could not have overlooked it, the conclusion is forced upon us that the reaction 282 PROCEEDINGS OF THE AMERICAN ACADEMY consisted only in the formation of the ketone. This result is the more remarkable because Ileckmaun * obtained from the orthoparadinitro- phenylacetacetic ester by treatment with sulphuric acid of about 10 per cent exclusively the dinitrophenylacetic acid without a trace of the corresponding ketone. As the presence of bromine in our compound could hardly have caused such a great difference in the action of the sulphuric acid, we infer that it must have been caused by the difference iu strength of the sulphuric acid, Heckmann's containing about 10 per cent of H2S04, while ours contained 54 per cent. This inference will be tested by experiment in the ooming year. Properties. — The bromdinitrobenzylmethylketone crystallizes from hot alcohol by cooling in white rectangular plates, often with a right- angled notch in one corner, sometimes also in plates with parallel sides and a deep notch in each end, which makes them look like reels. If crystallized by the evaporation of its alcoholic solution, it forms cylin- drical tufts of needles looking like spires of moss, or much branched forms resembling certain seaweeds. Both the plates and the branch- ing needles commonly occur together. It melts at 112°-113° and is essentially insoluble in ligroine ; nearly insoluble in cold water, more soluble in hot, but still very sparingly ; slightly soluble in ether, car- bonic disulphide, benzol, or methyl alcohol, its solubility in the last two solvents is increased by heat ; tolerably soluble in ethyl alcohol iu the cold, freely when hot ; ethyl alcohol dissolves it more freely than methyl alcohol ; tolerably soluble in glacial acetic acid ; soluble in chloroform ; aud freely soluble in acetone. Hot alcohol is the best solvent for it. Strong sulphuric acid has no action on it in the cold, but when warmed dissolves it, forming a colorless solution from which water precipitates the ketone essentially unaltered, although it appears at first in spheri- cal groups of thickly set radiating needles, a form in which it is also obtained sometimes when prepared by the action of sulphuric acid on bromdinitrophenylacetacetic ester, but these crystals are converted by crystallization from alcohol into the rectangular plates described above. Strong nitric acid acts like strong sulphuric acid. The bromdinitrobenzylmethylketone has well marked acid proper- ties, and in this respect far surpasses the desoxybenzoine from which according to Victor Meyer f no sodium compound could be isolated. In alcoholic solution the ketone gives a dark purplish red color with sodic hydrate or ethylate. Aqueous amnionic hydrate gives only a slight red color with it, which is increased by warming for a short * Ann. Chem., ccxx 134. t Ber. d. ch. G. 1888, p. 1291. OF ARTS AND SCIENCES. 283 time, and still more by the addition of alcohol, but the color disappears if the heating is long continued. Aqueous potassic carbonate gave no action, but on the addition of alcohol a very dark purplish red solution of the salt. Acid sodic carbonate had no action in aqueous solution, and only very slight on addition of alcohol. The dark red alcoholic solution of the ammonium or sodium salt, if made with an excess of the ketone, is decomposed by water, giving a white precipitate of the ketone. The decomposition is not complete, however, as the liquid retains a pale red color. In the presence of an excess of sodic hydrate, the salt is much more stable. An attempt was made to study the action of the pale red aqueous solution of the ammonium salt with various reagents, but no characteristic precipitates were obtained, probably on account of the small amount of salt left in solution. We tried also to prepare and analyze the sodium salt, the method being that adopted for the sodium salt of the bromdinitrophenylaceta- cetic ester; but the results of the analyses came much too high, 9.73 and 8.64 per cent of sodium, instead of the 7.07 per cent required by the formula. The reason for this difference is that the sodic hydrate or ethylate removed a portion of the bromine from the ketone, and the benzol, dissolving the organic product, left the sodic bromide formed with the salt of the ketone, as was proved by dissolving the salt in water, and acidifying with nitric acid, when, after removing the pre- cipitate by filtration, argentic nitrate gave a heavy precipitate of argen- tic bromide in the filtrate. We accordingly turned our attention to the anilidoketone, our work on which is described later in this paper. We add here the properties of the sodium salt of bromdinitrobenzyl- metltylketone. It is a purplish black amorphous substance, very easily soluble in alcohol forming a dark claret-red solution, the color of which is so much more purple than that of the salt of the corresponding acetaoetic ester, that the two substances can be easily distinguished in this way ; it is decomposed almost, but not quite, completely by water, and is insoluble in benzol. The ketone is a decidedly reactive substance. When treated with aniline, it and analyzed with the following result : — 0.2003 gr. of the substance gave 14.85 c.c. of nitrogen at a tem- perature of 20°. 5 and a pressure of 762 mm. Calculated for C6HBr(CGH5XII)i X02)2CH(C02C2H5)2. Found. Nitrogen 8.47 8.49 Properties. — The bromanilidodinitrophenylmalonic ester crystal- lizes from alcohol in bright red needles, which under the microscope are seen to be slender prisms terminated usually by two planes, less com- monly by one, and seeming to belong to the monoclinic system. The substance melts at 127° ; and is essentially insoluble in cold water, very sparingly soluble in boiling water, as shown by the faint yellow color imparted to the liquid ; insoluble in ligroine ; very slightly solu- ble in cold ethyl or methyl alcohol, more freely in either of these solvents when hot; slightly soluble in ether; soluble in benzol or glacial acetic%acid; freely soluble in chloroform, carbonic disulphide, or acetone. Strong sulphuric acid dissolves it slightly, forming a yellowish solution ; the solubility did not seem to be increased by heat. Strong nitric acid dissolved it rather more freely than sul- phuric acid, and the solubility was increased by heat. Strong hydro- chloric acid had no action upon it, although it is probable that long heating in a sealed tube with this acid would have decomposed it in the way described * under the bromdinitropbenylmalonic ester. * These Proceedings, xxiv. 240. OF ARTS AND SCIENCES. 299 The acid properties of this substance have been much weakened by the replacement of bromine by the basic aniline radical CtiH.NH, but that they still exist is shown by the following observations. Sodic hydrate in aqueous solution has no action on the solid, but on the addition of a little alcohol a dark red solution of the salt is formed ; sodic carbonate in aqueous solution produces no effect, but on the addition of alcohol a very slight red coloration appears ; acid sodic carbonate produces no effect even in presence of alcohol. Ammonic hydrate in aqueous solution does not dissolve the solid substance, and, t^en if alcohol is added, the action is very slight ; if, however, the mix- ture of aqueous ammonic hydrate, alcohol, and the solid is warmed on the water bath, a dark red solution is obtained, which smells of ammo- nia, even if a large excess of the ester is used. The behavior of such a solution with various reagents was studied with the following results : — Salts of magnesium, calcium, strontium, or barium gave rusty brown precipitates. The salts of the heavy metals gave yellow precipitates, except where the color was modified by the excess of ammonia which could not be removed from the solution of the salt. Reduction of Dibromdinitrophenylmalonic Ester. The investigation of this subject interested us especially, because it seemed probable that the diamidophenylmalonic or acetic acid, which would be the first product of the reaction, would lose water and be- come converted into an amidooxindol, especially since Bischoff* ob- tained from the reduction of his orthonitrobenzoylmalonic ester a-y- diliyclroxychinoline. As with zinc and alcoholic hydrochloric acid, or with zinc dust and acetic acid, he obtained more complex products, some of which it was almost impossible to purify, we decided to try first the action of tin and hydrochloric acid with alcohol upon our dibromdinitrophenylmalonic ester, and for this purpose proceeded as follows. 2 grs. of the dibromdinitrophenylmalonic ester were mixed with alcohol, strong hydrochloric acid, and tin, a piece of platinum foil being used to accelerate the action, and the mixture was kept upon a steam radiator at a temperature of from 50°-70° until the whole of the malonic compound had disappeared, which usually happened in an hour and a half. The clear solution was poured off from the excess of tin, and, after evaporation to dryness, dissolved again in water, and * Ann. Chem., ccli. 364. 300 PROCEEDINGS OP THE AMERICAN ACADEMY freed from tin with sulphuretted hydrogen ; upon concentrating the filtrate, long needles separated, which varied in color from brown to nearly white. By further concentration of the mother liquors a fresh crop of crystals was obtained, and the precipitate of sulphide of tin must be boiled out several times with water, as the reduction-product is but slightly soluble. As the substance seemed to be decomposed to a certain extent by our attempts to purify it by crystallization, we analyzed some of it without further purification, while other samples were crystallized once more from hot water, allowing the solution to cool in vacuo to avoid oxidation by the air. It was dried in vacuo, and analyzed with the following results : — I. 0.0977 gr. of the substance gave on combustion 0.1224 gr. of car- bonic dioxide and 0.0434 gr. of water. II. 0.3108 gr. gave on combustion 0.3869 gr. of carbonic dioxide ami 0.1128 gr. of water. III. 0.1113 gr. of the substance gave 9.8 c.c. of nitrogen at a temper- ature of 25°. 5 and a pressure of 763 mm. IV. 0.1010 gr. of the substance treated with argentic nitrate and the precipitate washed with nitric acid and water gave 0.0498 gr. of argentic chloride. V. 0.4762 gr. gave 0.2461 gr. of argentic chloride. Found. I. II. III. IV. V. Carbon 34.17 33.93 Hydrogen 4.93 4.03 "Nitrogen 9.84 Chlorine 12.19 12.77 The free base corresponding to this chloride was next prepared by adding amnionic hydrate to a strong solution of it, when a white precipitate swimming in a dark green liquid was obtained. It was purified by washing with cold water, in wdiich it is as good as insolu- ble, until the wash water gave no test for a chloride, then dried in vacuo, and analyzed with the following results : — I. 0.1690 gr. of the substance gave on combustion 0.2587 gr. of carbonic dioxide and 0.0580 gr. of water. II. 0.2021 gr. of the substance gave 23.7 c.c. of nitrogen at a tem- perature of 24°. 5 and a pressure of 768.5 mm. Found. I. II. Carbon 41.75 Hydrogen 3.81 Nitrogen 13.28 OF ARTS AND SCIENCES. 801 The following comparison shows that the numbers obtained from the analyses of the chloride correspond to those calculated for the formula CsHfJBrN.202HCl (with the exception of the hydrogen,* which was undoubtedly brought too high by the passing over of a part of the halogen into the sulphuric acid bulbs). Calculated for CgU9BrN202H01. Found. Carbon 34.12 34.17 33.93 Hydrogen 3.55 4.93 4.03 Nitrogen 9.95 9.84 Chlorine 12.61 12.19 12.77 On the other hand, the numbers given by the analyses of the free base indicate a substance containing one molecule less of water. Calculated for Calculated for C8H7BrN20. Found. C8H9BrN202. Carbon 42.30 41.75 39.17 " Hydrogen 3.08 3.81 3.67 Nitrogen 12.34 13.28 11.43 The want of agreement between the percentages of hydrogen f is ex- plained in the same way as in the analyses of the chloride. Other- wise the numbers come as near as could be expected, when it is remembered that the free base was so unstable that we did not dare to purify it except by washing, and that it gradually turned brown even when dry. In order to harmonize these results and determine the nature of the substances we have found only three hypotheses. First, and most obvious. The two substances belong to different classes, i. e. one is the chloride of the bromdiamidophenylacetic, acid C^HoBrNHgClNIIoCHjCOOH; the other is free bromamidooxindol, CflH2BrNH2(CH2CONH). If, on the other hand, the substances belong to the same class, — Second. They are the bromamidooxindol and its chloride. In this case the chloride must contain one molecule of water of crystallization. Third. Tliey are bromdiamidophenylacetic acid and its chloride. In this case our analyses of the free base are incorrect. * The formula C8HnBrN.202HCl requires 4.23 per cent of hydrogen, and is therefore distinctly too high for Analysis II., and the analysis of the " chloride of the free base " given later. The small amount of substance used in Analysis I. makes the per cent of hydrogen in it of no value. t The formula C8II9I3rNoO requires 3.93 per cent of hydrogen. 302 PROCEEDINGS OF THE AMERICAN ACADEMY If the first of these explanations is the true one, the chloride made by adding hydrochloric acid to the free base would be the chloride of the bromamidooxindol, and therefore different from the original chloride of the bromdiamidophenylacetic acid. To settle this point, we set free the base with amnionic hydrate from a quantity of the original chloride, and, after washing until free from ammonic chloride, dissolved it in dilute hydrochloric acid and crystallized it from the slightly acid solution. The general habit of the crystals of the two chlorides (the original one and that made from the free base) was the same, but there were differences in the modifications on the ends of the prisms which made the identity of the two somewhat doubtful ; we accordingly analyzed the chloride made from the free base, with the following results : — 0.1853 gr. of the substance gave on combustion 0.2328 gr. of car- bonic dioxide and 0.0678 gr. of water. Calculated for Calculated for Found. Analyses of C8H713rN20IICl. C8H0BrN202HCl. Original Chloride. Carbon 36.43 34.12 34.26 34.17 33.93 Hydrogen 3.04 3.55 4.06 4.93 4.03 There can be no doubt, therefore, of the identity of the two chlo- rides, and the first explanation must be abandoned. The second explanation requires that the chloride should contain one molecule of water of crystallization. This point was tested by heating the chloride with the following result : — 0.2517 gr. of the chloride heated for 6 hours at first at 110°, later to 135°, lost 0.0024 gr. Calculated for C8H,BrN,OHClH20. Found. Water 6.42 0.95 From this it appears that, if the chloride contains water of crystalli- zation, it does uot lose it at 135°. The slight loss of only 2.4 mgrs. could be sufficiently accounted for by the decomposition of the salt, which had turned dark gray on the surface, and for this reason too the heating could not be repeated at a higher temperature. This result, unfavorable to the second explanation, necessitates the discussion of the third, — that the free base is bromdiamidophenylacetic acid, — which otherwise we should not have thought worthy of consid- eration. As has been already stated, the analyses of the free base do not agree with this explanation, and in order to adopt it we must assume that the substance had undergone a decomposition sufficient to OF ARTS AND SCIENCES. 303 raise the carbon 2.58 per cent, an assumption improbable in itself, and not supported by the appearance of the preparation, which had only a slight dirty pink color. This we think is enough to condemn this third explanation, but we add the following considerations, all of which tell strongly in favor of the second, and against the third ex- planation. (1.) Gabriel and R. Meyer* by the reduction of diui- trophenylacetic acid with tin and hydrochloric acid obtained the paramidooxindol direct, and it does not seem possible that our brom- diamidophenylacetic acid, which differs from theirs only in containing an atom of bromine, should be so much more stable. (2.) Our free base agrees fairly well in properties with the paramidooxindol of Gabriel and R. Meyer. Both are easily oxidized, soluble in hot water or in alcohol, slightly soluble in benzol or carbonic disulphide, the only difference being that our base is nearly insoluble in ether, whereas theirs is soluble in it. The melting points also stand about where we should expect, amidooxindol about 200°, our bromamidooxindol about 212°; in both cases there was so much blackening that the melting point could not be accurately determined. (3.) Our base (or its chlo- ride) gives the indol reaction, turning a piece of pine wood red if boiled with it and dilute sulphuric acid, or if the wood, after being satu- rated with a solution of the base, is soaked in strong hydrochloric acid. This seems to us conclusive. The color is rather dull, and appears only after some time ; but the objection which might be urged against this argument on this account, that the bromdiamidophenylacetic acid was converted into the bromamidooxindol by treatment with the acids, has no weight, as in the preparation of the original chloride it was most thoroughly exposed to the action of strong hydrochloric acid, both hot and cold ; and yet this chloride, as we have shown by the analyses, contained two atoms of hydrogen and one of oxygen more than is re- quired by the chloride of the bromamidooxindol. These arguments seem to us to prove conclusively that the two substances are bromamidooxindol CGH2BrNH2(CILCONH), and its chloride CGH2BrNH,(CH2CONH)HCl.H20, in spite of the fact that we could not drive off the water of crystallization from the chloride even at 135°. Properties of Bromamidooxindol, CGH2BrNH2(CH.,CONiI). As precipitated from its chloride it forms a heavy flocculent white precipitate, which, when examined with the microscope, is seen to be * Ber. d. ch. G., xiv. 832. 304 PROCEEDINGS OF THE AMERICAN ACADEMY a felt of small white needles, often arranged in fagots or groups like an hour-glass ; it is not very stable, changing to a dirty pink on ex- posure to the air, even when dry. The substance analyzed melted at 212° with a good deal of blackening, but we do not place much reli- ance on this melting point, as the sample used was a good deal colored. It is almost insoluble in cold, soluble in hot water ; soluble in hot alcohol ; insoluble or nearly so in ether or chloroform ; not freely soluble in benzol or carbonic disulphide, even when hot ; freely soluble in hot glacial acetic acid. Sodic hydrate dissolves it, giving a pinkish or pale magenta solution ; ammonic hydrate at first seems to have no action, but on standing the liquid and solid turn dark bluish green ; potassic carbonate in aqueous solution does not dissolve it. It seems therefore to have the properties of a phenol. Neither picric acid in henzol solution, nor ferric chloride with an alcoholic solution of the base, produced any change of color. If some of the free base was boiled with dilute sulphuric acid and a piece of pine, the wood was turned a dull orange-red. As to the constitution of this base, it has been determined by work* done in this laboratory on the bromdinitrophenylmalonic ester that the nitro group, from which the amido group is formed, is in the para position to the carbon side chain. The bromine is probably in the ortho position, since all our work with the tetrabromdinitrobenzol has shown that only three of its atoms of bromine can be replaced easily ; and, as the compounds made from this substance are so closely analo- gous to those prepared from the tribromdinitrobenzol, it is fair to infer that the three symmetrical (meta) atoms of bromine are those which can be removed, and that the fourth more stable atom of bromine is the one in the unsymmetrical (ortho) position ; the atom of bromine, therefore, which reduction takes away from the dibrom- dinitrophenylmalonic ester, would be that in the meta position, and the base would be accordingly orthobromparamidooxindol. Properties of the Chloride of Bromamidooxindol, CGH2BrNH2(CH2CONH)HClH20. When crystallized from water, the substance forms needles, or prisms, sometimes as much as a centimeter long and a millimeter thick, which seem to belong to the monoclinic system, and usually have a yellowish color; we think, however, that this color is due to partial oxidation, and that the substance is white when pure. When * These Proceedings, xxiv. 249, 250. OF ARTS AND SCIENCES. 30" • > examined with the microscope, the prisms are found to be arranged in globular radiating groups, and are terminated usually by a single rhombic plane at a not very oblique angle to the long sides of the prism ; sometimes a number of other modifying planes are observed, giving a sharp end to the prism. From alcohol it crystallizes in branching ueedles set at a very acute angle to each other. It melts only at a very high temperature, probably above the range of the mercury thermometer. It is slightly soluble in cold water, freely in hot; soluble in alcohol; slightly soluble in cold benzol, chloroform, or glacial acetic acid, freely soluble in these solvents, when hot; almost insoluble in ether; very soluble in carbonic disulphide. The best sol- vent for the substance is boiling water. An excess of amnionic hy- drate throws down from a concentrated solution a heavy precipitate of the free base, which is white, but the liquid turns dark green ; potassic carbonate gives a similar precipitate, not soluble in an excess ; sodic hydrate in small quantity gives a similar precipitate, but dis- solves it when added ho larger quantity, giving a reddish solution. It gives a dull orange-red indol reaction with pine wood. vol. xxiv. (n. s. xvi.) 20 306 PKOCEEDINGS OF THE AMERICAN ACADEMY XXIV. CONTRIBUTIONS FROM THE CHEMICAL LABORATORY OF HARVARD COLLEGE. GENERAL CONSIDERATIONS IN REGARD TO CER- TAIN COMPOUNDS PREPARED FROM BROMNITROBENZOLS. By C. Loring Jackson. Presented May 28, 1889. Several compounds derived from various bromnitrobenzols have been described recently by me in conjunction with other chemists in a number of papers* from this laboratory, but in the course of the work certain general observations were made in regard to them which could not conveniently be introduced in the separate papers, and are therefore collected here. . The Action of Sodium Malonic {or Acetacetic) Ester on certain Bromnitrobenzols. The actions studied were the following : — Sodium Malonic Ester on Tribromtrinitrobenzol, C6Br3(N02)3, melting point 285°. Tribromdinitrobenzol, C6HBr.,(N02)2, melting point 192°. Tetrabromdinitrobenzol, CtiBr4(N02)2, melting point 227°. Sodium Acetacetic Ester on Tribromdinitrobenzol, C6HBr3(N02)2, melting point 192°. In all these cases the action was essentially the same, and may be represented by the following reactions for tribromtrinitrobenzol : — I. C6Br8(N0.2)8+ CHNa(COOC2H5)2 = NaBr+ CGBr2(N02)3CH(COOC2H5)2. II. C6Br2(NO,),CH(COOC.,H.)2 + CHNa(COOC2EL),= C6Br2(N02)3CNa(CObC2II5)2 + CH2(COOC2H5)2- III. C0Br2(NO2)3CNa(COOC2H5)2 + CH2(COOC2H5)2 = C,HBr(N02)3CNa(COOC2H5)2 + CHBr(COOC2H5)2. * These Proceedings, xxiii. 138; xxiv. 1, 105, 234, 256, 271, 288. OF ARTS AND SCIENCES. 307 The formation of brommalonic ester in III., the only point in these reactions about which there was any doubt, was proved by the isola- tion of acetylentetracarbonic ester* or of tartronic acid J from the oily secondary product, as these substances could hardly have been formed otherwise than by the following reactions, — CHBr(COOC2IL), + CHNa(COOC2H5)2 = CHCfI((JOOC2lL)4 + NaBr. CHBr(UOOG,H5)2 + NaOM = CHOII(COOC2H.)2 + NaBr. Reactions I.— III. are given because they show more clearly what has taken place, but the discussion which follows does not depend on them alone, since the analyses of the products are sufficient to prove that in all the cases studied the action has consisted in the re- placement of one atom of bromine by the malonic ester radical, and of the second by hydrogen, while the third (and fourth) has remained unaltered.! This difference in the behavior of the three atoms of bromine is certainly very curious, and, so far as I can find, no case analogous to it has been described as yet. The strangeness of the replacement of bromine by hydrogen becomes especially evident when it is remembered that in every case there was a large excess of sodium malonic ester present, and that this second atom of bromine has there- fore combined with the carbon of malonic ester (see Reaction III.) in preference to the sodium of sodium malonic ester, so that the tendency to introduce hydrogen rather than the malonic ester radical has been strong enough in this case to overcome the attraction of the bromine for the sodium, and to cause it to combine with carbon instead. I have not succeeded in finding any explanation of these curious observations which satisfies me, but hope to be led to one by further experiment. It can be stated at present, however, that the difference of behavior in the three bromine atoms is not due to differences in their position on the benzol ring. This is shown easily in the case of the tribromtrinitrobenzol, as here the three atoms of bromine occupy exactly similar positions, each being ortho to two nitro groups and para to the third. In the tribromdinitrobenzol.§ also, the first ami * These Proceedings, xxiv. "2G5. t Ibid., xxiv. 238. J Ih the trinitro compound the third atom of bromine is replaced by the ma- lonic ester radical to a limited extent even in the cold, but it is acted on much less easily than the first. § In the tetrabromdinitrobenzol the fourth atom of bromine seems to have no influence on the reaction, and therefore all I say about the tribromdinitro- benzol also applies to this substance. 808 PROCEEDINGS OF THE AMERICAN ACADEMY third atoms of bromine are similarly placed (ortho to one, para to the other nitro group), but the second (that replaced by hydrogen) is pe- culiar in being ortho to both nitro groups. It is evident, then, that in these reactions both similarly placed bromine atoms are not replaced by the malonic ester radical ; but it is also to be observed that the bromine which is replaced by hydrogen has in every case stood in the ortho position to two nitro groups, and this suggested to me that perhaps an atom of bromine in this position might be especially susceptible to the action of free malonic ester. To test this hypothesis I mixed some tribromdinitrobenzol dissolved in benzol with malonic ester, and, after the mixture had stood for some time in the cold, warmed it for about an hour on the water bath, but even after this treatment no action * had taken place, as the tribromdinitrobenzol melted unaltered at 192°. This result was confirmed by a similar experiment with acetacetic ester, which stood with tribromdinitrobenzol for six mouths without any action. It is evident, therefore, that this atom of bromine is not attached in an especially loose way to the molecule, and that its re- placement by hydrogen does not depend only on its position with reference to the nitro groups, but is due also to the presence of the malonic ester radical. On the Relative Ease vrith which the Reactions take Place. This subject will I hope prove susceptible of quantitative treatment, and I propose next year to try some experiments of this sort ; I shall therefore at present confine myself to two qualitative observations, which were so marked that a quantitative confirmation of them seems unnecessary. The tribromtriuitrobenzol is distinctly more reactive than the tri- bromdinitro- or tetrabromdinitrobenzol,as it acts on alcoholic ammonia in the cold, whereas the other two must be heated to 100° in sealed vessels to bring about this reaction. The sodium acetacetic ester acts much less energetically than sodium malonic ester upon tribromdinitrobenzol, since the red color of the product appears instantaneously with the malonic ester, but only after some time with acetacetic ester, and the yield of the acetacetic com- pound is much smaller than that of the malonic derivative, if the reactions are carried on under the same conditions. * The addition of a little aqueous sodic hydrate was enough to cause action at once, as shown by the appearance of the red color of the sodium salt. OF ARTS AND SCIENCES. 809 On the Acidity of the substituted Malonic Esters, Acetacetic Ester, and Ketones described in the preceding Papers. In order to determine the relative acidity of these substance*, their action with the following reagents was studied: acid sodic carbonate, sodic carbonate, amnionic hydrate, sodic hydrate. Each reagent was added in aqueous solution to the solid organic substance, and, after observing what took place, alcohol was added, and any change in the behavior of the substauce noted. All these experiments were tried at the same time, great care being used to make the conditions as nearly the same as possible. The results can be divided into those which were perfectly definite, that is, where the differences consisted in the fact that one compound formed a salt with the reagent, and another did not ; and those depending to a certain extent upon my judgment, in which the differences were only in the amount of salt formed, as shown by the depth of color, or in the cpuantity of alcohol necessary to produce the salt. The differences of the first class can be described most clearly and succinctly by the following table, in which the sub- stances are arranged in the order of their acidity, beginning with the most acid. The columns correspond to the reagents, and the word " Salt " indicates that a salt was formed, as shown by the color imparted to the solution, or solid. NaHC03 Na2C03 NH,OH NaOH 0Q = O 0? S < Salt ._ c Salt w 2 O D C < Salt So w S o 0) s < "5 So DO s o 3 < "3 _ & . - o ,1. CuH^BrtNO.JA^sOCHoCOa^Hs Salt Salt Salt Salt Salt II. C6HBr(NO.J3CH(C02C2H5)2 Salt Salt Salt Salt Salt Salt Salt Salt III. C6H„Br(N02)oCH(COoC.2H5)2 Salt Salt Salt Sr.lt Salt Salt Salt IV. C6H2Br(XOo)oCII2COCri3 •• Salt * Salt Salt Salt Salt Salt V. C,HBro(N02)2CH(C02C2H;;)2 •• Salt Salt Salt Salt Salt Salt Salt VI. C6H2CBH,NH(N02)2CH(C02C.2H5)2 Salt •• Salt Salt Salt VII. (VnBrC,Hr,NH(NO,)2CH(C02C2H5), :: Salt Salt Salt Salt VIII. C„H2C0H5NH(NO2)2CH2COCII3 * No salt was obtained from IV. with aqueous sodic carbonate, but I ascribe this to a mistaken observation, probably due to the difficulty in moistening the ketone with the aqueous solution. •310 PROCEEDINGS OF THE AMERICAN ACADEMY The observations recorded in this table divide these substances into the following groups (indicated by the lines): — I. and II., most acid ; III., IV., and V., less acid ; VI.. less acid ; VII., less acid ; VIII., least acid. The relative acidity of I. and II. was determined by data of the second sort mentioned above, since I. gave a much stronger coloration than II. with aqueous sodic carbonate, amnionic hydrate, or sodic hy- drate. The order of III., IV., and V. was determined by the following observations. With acid sodic carbonate and dilute alcohol, III. and IV. gave a stronger red color than V. With aqueous sodic carbonate, III. gave a pale red, V. a much paler, in fact barely perceptible color. With aqueous amnionic hydrate, III. gave a pale red, V. a very pale barely perceptible red, and IV. stood between III. and V. in color. With aqueous sodic hydrate, the color was confined to the crystals of the organic substance, owing to the slight solubility of the salt in a solution of sodic hydrate, and III. turned dark red, IV. pale red, while V. showed a mixture of pale red particles of the salt and white ones of the ester. Upon adding alcohol to the mixture of the substance and either aqueous sodic carbonate or amnionic hydrate, a dark red color was obtained from all three, but much more alcohol was neces- sary to produce this color with V. than with III. or IV. My obser- vations on the intensity of the color with different reagents confirm the order of compounds VI., VII., and VIII., but I do not think it worth while to give the details. I should add, also, to show that the personal equation did not enter to auy great extent into these obser- vations, that the substances during the experiments were arranged in an order different from that of their acidity, and that the order of acidity given above derived from these experiments was a surprise to me in many particulars. These experimental results justify the following inferences in re- gard to the effect of differences in conijx>sition upon the acidity of these substances. (a.) The introduction of an additional nitro group (in the ortho position) increases the acidity, since II. is more acid than III. (b.) The replacement of hydrogen (in the ortho position) by bro- mine diminishes the acidity, since V. is less acid than III. (c.) The replacement of bromine (in the meta position) by the aniline radical C'(,1LNTI reduces the acidity very considerably, since III., IV., and V. are much more acid than VI., VIII., and VII. respectively. In all these cases the differences occur in the benzol ring, and the effects are very marked (especially in c) when it is considered that OF ARTS AND SCIENCES. 311 the hydrogen affected is attached to the side chain, and therefore more removed from the influence of the acid radicals than in most of the similar cases previously described, in which the element influenced was attached to the benzol ring. These observations recall some made by me several years ago, when 1 showed * that the ring bromine in the three brombenzylbromides had a marked influence in diminishing the ease with which the side-chain bromine was removed, varying with its position on the benzol ring, the para bromine having less influence than the meta, the meta than the ortho. (d.) The nature of the side-chain also has a marked influence on the acidity ; thus the substituted acetacetic ester I. is much more acid than the corresponding malouic ester III., a result in harmony with Claisen and Ehrhardt's f classification of the radicals according to their acid-producing power, since they give the following list beginning with that which has the least influence, "phenyl, carboxyl, benzoyl, acetyl, formyl." An approximate measure of the relative acid-producing power of carboxyl and acetyl is given by the comparison of III. and IV., which possess nearly the same degree of acidity, and therefore it follows that one acetyl has nearly, although not quite, the same effect as two carboxyls. (e.) The comparison of a dimalonic with the corresponding mono- malonic compound in this respect is of interest. Unfortunately I had none of the trinitrophenylendimalonic ester when the comparison de- scribed above was made, so that this substance does not appear in the table; but by comparing the observations made on it when its prop- erties were studied with those on the bromtrinitrophenylmalonic ester, I have found that the dimalonic compound is much less acid than the brommonomalonic ester, since acid sodic carbonate in aqueous solution has no action upon it, and even aqueous sodic carbonate gives only a very faint red color.J This weaker acidity can be accounted for by the hypothesis, that the influence of the three nitro groups being di- vided between two malonic ester radicals, each will have the acidifying influence of only one and a half nitro groups, instead of the three, which act on the acid hydrogen in the monomalonic compound. The stability of the salts of all these compounds is remarkable, the * Those Proceedings, xvi. 241. t Ber. d. ch. G. 1889, p. 1019. i I should he inclined to place the trinitrophenylendimalonic ester between III. and V., although from the absence of comparative work ita exact place cun- not be determined with certainty ; this, however, is of little importance, as the comparison of it with II. is the only one of especial interest. 312 PROCEEDINGS OF THE AMERICAN ACADEMY sodium salt even of the anilidodinitrobenzylmethylketone (the least acid of all these substances) having been prepared and analyzed with no especial difficulty ; it shows therefore a marked difference in this respect from desoxybenzoine (CgFLG'OCHgCytL), the sodium com- pound of which, according to Victor Meyer,* has not been isolated. In fact, he thinks it probable that it may not exist in the free state, and leaves it doubtful whether the syntheses of homologues of desoxy- benzoine are preceded by the formation of a sodium compound, as with malonic or acetacetic ester, or whether the homologue is formed direct by the removal of hydrogen and the halogen by sodic hydrate, according to this reaction : C6H.COCHCuH. + CH3 + NaOH = Nal + Ho0 + C6H.COCHCcH.. [H~ ~T\ CH3. The reason for this striking difference in acidity between the sub- stituted benzylmethyl ketones and desoxybenzoine can hardly be due to the fact that the former contain the more active acetyl instead of the benzoyl contained in the latter, although this may have some influ- ence, but in my opinion is rather to be ascribed to the heightening of the acid-producing power of the phenyl by the nitro groups which it contains. The salts of the acetacetic or malonic esters are much more stable than those of the ketones, as was to be expected, since in these cases the hydrogen is exposed to the acidifying power of three radicals (nitrophenyl and two carboxyls, or one carboxyl and an acetyl), and their stability almost equals that of the salts of BischofF's f orthonitro- beuzoylmalonic ester, in which the nitrophenyl of my compounds is replaced by the even more acid nitrobenzoyl. * Ber. (1. ch. G. 1888, p. 1291. t Ann. Chem., ccli. 364. OF ARTS AND SCIENCES. 313 XXV. FEATURES OF CRYSTALLINE GROWTH. By Oliver Whipple Huntington. Presented June 12, 1889. Variations in the Butcher Irons. In a former paper * the author discussed in some detail the crystal- line structure of iron meteorites, and in a second f described the cleavage exhibited by various specimens of the Coahuila group of irons, which are generally supposed to have come from the same original mass. It was then shown that in this group of irons the Butcher specimens differed so markedly from those of Saltillo (Santa Rosa) that the cleavage seemed to offer a conclusive means for separat- ing the two falls, though the appearance of the etched surfaces failed to distinguish them. As several very large individual masses of these irons are now in the Harvard Cabinet, under the general name of " The Butcher Irons," we were interested to see whether any peculiarity of structure would further distinguish them as independent meteorites, or whether on the contrary they could be identified as having unquestionably come from the same original body. A careful examination of the exterior of these irons showed that they had begun to break up since becoming the property of Harvard College, but this alteration had only taken place in certain parts of the specimens. The largest specimen seemed to have a zone running through the thickest part from which could be detached with little difficulty octahedral fragments of iron made up of distinct plates, showing a cleavage very similar to the well known Put- nam County iron, while the rest of the mass was compact and un- altered. Thus certain parts of the Butcher specimens appeared to have an entirely different structure from what we are accustomed to associate with these irons. They have heretofore been known as typical " cubic irons," and, though it has been shown that all the twin * Proceedings of the American Academy, vol. xxi. p. 478, May, 1886. t Ibid., vol. xxiv. p. 30, October, 1888. 314 PROCEEDINGS OF THE AMERICAN ACADEMY members of the regular octahedron cube and dodecahedron appear on the surface of fracture, still the cube gives character to the iron, and, together with the etched surface, serves to connect it closely with the Brauuau (Hauptmannsdorf) and other so called cubic irons. In seeking to explain this apparent variation in the structure of the Butcher specimens, a number of large masses were polished and etched. The most striking result was obtained on a specimen which formed one end of a large mass originally cut up by Ward and Howell for the late J. Lawrence Smith. This surface as it appeared after etching is shown, one third the natural size, in Plate I., which was made directly from a photographic negative. The figure, although so much reduced, shows clearly a zone passing through the thickest part of the mass characterized by a very different crystallization from the rest of the piece. The greater portion of the etched surface is cov- ered only with Neumann lines so characteristic of the Coahuila irons. These lines, although not well shown in the photograph, are plainly exhibited by the print from an etched plate previously published.* This last feature is characteristic of the outside of the mass, where the cooling must have been quicker and the crystallization more rapid and disturbed, though following, nevertheless, the fundamental forms of the regular system. In the central zone, however, corresponding to the thickest part of the specimen, the iron appears to have crystallized more slowly, and exhibits all the characters of Widmanstattian figures resulting from well marked crystal plates ; and here the octahedron appears to predominate, though the presence or absence of the cube and dodecahedron cannot be established by the examination of only a single etched surface cut at random. The etched surface of another portion of the same mass seemed to explain this contrast of coarse and fine grained crystallization. There is in the Harvard collection the largest slab ever cut from the Coa- huila specimens, being a full section of the large mass which we have been discussing. The etched surface of this slab was fully as striking as that shown in Plate L, but exhibited more uniformity in the. distri- bution of the figures. Unfortunately, the slab was too large to allow of its reproduction on paper within the limits of this publication, but the figures can be best described by their resemblance to the mark- ings of frost on a large window-pane. Around the edge the crystals were so compact as to show no details, but these compact masses joined the inner portion on a curved outline, looking like cloud masses * Proceedings of the American Academy, vol. xxiii., Plate I. OP ARTS AND SCIENCES. 315 which had floated in to the distance of from ten to one hundred millimeters from the crust, and on the inner edge of these cloudy por- tions the crystals became more distinct, and finally shot out in crystal- line plates (which were seen of course only in section) some of them from fifty to one hundred millimeters in extent. These again were met and intersected by similar crystalline plates radiating from numer- ous centres through the mass, these centres being spots of more com- pact crystallization, like the cloudy masses around the edge, forming in the interior a network of plates producing skeleton crystals. Thus the entire surface presented exactly the appearance that one might expect in a mass of iron which had slowly cooled. In such a mass, the surface cooling first would become compact, and exhibit only confused crystallization, while the interior, cooling more slowly, would allow time for isolated crystal plates to form ; and at the same time local causes would start a simultaneous crystallization from other points in the interior, determined probably by the presence of nuclei of foreign matter. The possible variation in the character of the figures brought out by etching different portions of the same iron, has been mentioned in a former paper,* but at that time no such striking example had been noticed as that now exhibited by the Coahuila irons. Specimens might be cut from the iron shown in Plate I. so selected that one piece when etched would give well marked Widmanstattian figures, with all the characteristic features which have commonly been associated with the so called typical octahedral irons, while another would show equally typical Neumann lines, and still a third piece would appear perfectly amorphous or made up of irregular grains. Widmanstattian Figures on " Spiegel Eisex." Hitherto Widmanstattian figures and Neumann lines have been considered the strongest characteristic of meteoric irons ; but since it is merely the evidence of slow crystallization attended by the exclu- sion of foreign matter, one would expect that any impure iron, pro- vided that it had cooled slowly from a state of fusion, would exhibit similar characters. From depending too much upon these features the Greenland iron was originally considered to be of meteoric origin, as some of the masses show very good Widmanstattian figures. Since specimens of cast iron have been frequently described as meteoric, and * Proceedings of the American Academy, vol. xxi. p. 478, May, 1880. 316 PROCEEDINGS OF THE AMERICAN ACADEMY Fig. 1. are to be found in all the large museums of the world, I was inter- ested in examining specimens of " Spiegel Eisen," which contains so large an impurity of manganese, and is at the same time so strikingly crystalline. In the first place, the fracture somewhat resembles that of the Mexican irons which we have been discussing, as it shows cube faces, although the octahedron is dominant. Moreover, thin plates of " Spiegel Eisen " can in some cases be detached from the mass which would make it appear still more like meteoric iron, were it not for its great hardness. On a polished surface, however, the resemblance is far more striking, since etching or tempering brings out well de- fined Widmanstattian figures. These figures are shown of natural size in Figure 1, which is an exact sketch of the etched surface on a piece of this iron. OF ARTS AND SCIENCES. 317 Crystalline Plates in Galena. In this connection it may be of interest to describe some specimens of galena which appeared among the minerals used for blowpipe analysis by the class in mineralogy at Harvard College, but whose origin is unknown. Fig. 2. There were found three crystals very much alike, one of which is shown considerably enlarged in the accompanying sketch. On one side it showed the perfect cubic cleavage of ordinary galena, but the mass of the crystal consisted of a network of plates about 1 mm. thick, in- tersecting each other for the most part at right angles, and thus form- ing a skeleton cube. But that which makes the specimens of unusual interest is the fact that there are certain additional plates, following the direction of the faces of an octahedron, and thus running diago- nally through the entire thickness of the crystals. Such a plate is shown at A B in the sketch (Fig. 2). Moreover, the cleavage of the galena appeared to be due to some other cause than the form of the crystal, since the octahedral plates were as well marked and nearly as abundant as the cubic ones, while the cleavage was distinctly cubic. Thus it appears that when galena crystallizes, just as when iron crystallizes, plates form through the mass following the directions of both the cube and octahedron till 318 PROCEEDINGS OF THE AMERICAN ACADEMY the mass becomes solid, but that subsequently either cleavage may become so dominant as to wholly cover up all other crystalline structure. Crystalline Concretions of Mica. Some time ago I received from Dr. D. F. Lincoln of Boston some remarkable specimens of curved mica, one of which is shown of natu- ral size in Figure 3. This crystal had its cleavage face very much Fig. 3. curved, while the successive layers tapered back to an apex at the centre of curvature, the whole having the appearance of forming a portion of a sphere. The occurrence of these micas is very well de- scrihed in a letter from Dr. Lincoln : — " The specimens of mica were procured by me in 1885, from Mt. Apatite in Auburn, Maine. The rock of that locality resembles that V x X ■^ ^> *!= V -. OP ARTS AND SCIENCES. 319 of Mt. Mica, being a granite, with all its components (quartz, ortho- clase, clevelandite, muscovite, black tourmaline, etc.), in very lar^e masses. At the eastern end of the ridge there are several places where a very pure quartz is quarried in immense quantities. The peculiar mica is found at one of these quarries at points on the border of the quartz deposit. The coarser and less well formed specimens are imbedded in quartz and feldspar ; the finer and well formed are usually enclosed in feldspar alone. One vertical face of the quarry presented a most interesting exposure. Here the mica stood out in bosses, or huge breasts, looking like broken spheres developed from numerous centres, and grouped very irregularly. The spherical sur- faces, on analysis, consisted of groups of rhombic figures, each repre- senting a crystal of mica, with curved cleavage and tapering to the centre of the sphere.'' Thus it appears as if these crystals were the result of two distinct tendencies acting together, one concretionary, exerted to make the mass solidify from centres, and the other the crystallizing force, tend- ing to form at the same time the rhombic prism of 60° and 120° so characteristic of the mineral. 320 PROCEEDINGS OF THE AMERICAN ACADEMY XXVI. CONTRIBUTIONS FROM THE CHEMICAL LABORATORY OF HARVARD COLLEGE. I. ON CHLORPYROMUCIC ACIDS* By Henry B. Hill and Louis L. Jackson. Presented May 28, 1889. Many years ago Malaguti f found that dry chlorine gas was quickly absorbed by ethyl pyromucate, and that a thick viscous liquid was formed, the composition of which showed that four atoms of chlorine had been taken up. The oil was carbonized on distillation, and yielded with potassic hydrate decomposition products which were not further studied. Although Schmelz and Beilstein $ later found that chlorine converted pyromucic acid in aqueous solution into muco- chloric acid, and this reaction was afterwards further studied by Hill and Bennett,§ no further experiments, as far as we could learn, had ever been made with dry chlorine on pyromucic acid or its ethers. In 1884, after it had been shown by investigations carried on in this laboratory that substitution products could readily be formed from pyromucic acid by the action of dry bromine, Mr. J. N. Garratt, at that time an assistant in the laboratory, undertook the investigation of the action of dry chlorine under similar conditions. Although he succeeded in isolating a dichlorpyromucic acid melting at 1G7-1G80 in a state of purity, he found that the reaction differed in many re- spects from the corresponding reaction with bromine, and that the matter deserved a more careful study than he was then able to bestow upon it. Mr. Garratt relinquished his investigation of this subject in order to continue his studies in Zurich, and in the following winter * A part of the work described in the following paper was pre«ented in the form of a thesis to the Academic Council of Harvard University in May, 1888, by Louis L. Jackson, then candidate for the degree of Doctor of Philosophy. t Ann. Chim. Phys., Ixiv. 282; lxx. 371. t Ann. Chem. u. Pharm., Suppl., iii. 276. § Berichte d. deutsch. chem. Gesellsch., xii. 655. OP ARTS AND SCIENCES. 821 met with the fatal accident which so sadly ended his promising career. The observations which already had been made interested us so much that in 1886 we undertook a more thorough study of the sub- ject. We had already collected a great deal of material which we did not think it necessary to publish in a preliminary form, when Denaro * published in the Gazzetta Chimica a brief notice of a dichlorpyromucic acid melting at 167-168°, which was evidently identical with that pre- pared by Garratt. The paper contained a description of the acid and two of its salts, but the analyses of the latter did not agree with those which we had already obtained, and moreover contained such serious misprints or arithmetical errors, or both, as to be wholly without value. In consequence of the appearance of that paper, we thought it best to publish a preliminary account f of our work, so far as that one acid was concerned, more especially since our study of it was then essentially completed. In repeating the experiments of Garratt, we had no difficulty iD isolating the dichlorpyromucic acid which he had prepared, but we found that the reaction was still more complex than we had supposed. At ordinary temperatures chlorine was rapidly absorbed, but the pyro- mucic acid was soon so coated with the viscous addition product that a homogeneous product could not be obtained. On heating, the reaction could easily be pushed to the end, and the gain in weight closely cor- responded with the addition of four atoms of chlorine. At the same time hydrochloric acid and carbonic dioxide were given off, and the resulting product contained a percentage of chlorine much larger than that demanded by any simple addition product. Under these circum- stances it seemed advisable to return to the ethyl pyromucic tetrachlo- ride of Malaguti, which, from his description and analyses, appeared to be homogeneous ; and to take up the study of the more complex ac- tion of chlorine upon the acid itself after this investigation had made us better acquainted with some of the products likely to be formed. Although we were unable to prepare a perfectly homogeneous product by following the directions of Malaguti, we found no difficulty in so modifying the conditions that the resulting compound should give us pure fiy dichlorpyromucic acid melting at 168-169°, S chlorpyro- mucic acid melting at 176-177°, or trichlorpyromucic acid melting at 172-173°. The (38 dichlorpyromucic acid we were unable to prepare by direct substitution, or by saponification of ethyl pyromucic tetra- * Gazz. Chim., xvi. 333. t Berichte d. deutsch. chem. Gesellsch., xx. 252. vol. xxiv. (n. s. xvi.) 21 322 PROCEEDINGS OF THE AMERICAN ACADEMY chloride ; but by distillation of ethyl pyromucic tetrachloride, of the tetrachloride of pyromucyl chloride, or of ethyl 8 chlorpyroniucic tetra- chloride, the ySS dichlorpyromucic acid melting at 155-156° may be obtained, and in the first two cases a third dichlorpyromucic acid melt- ing at 197-198° is also formed. By careful reduction of the j38 or the /3y dichlorpyromucic acids, the /3 chlorpyromucic acid melting at 145-146° is formed. Ethyl Pyromucic Tetrachloride. The ethyl pyromucate which we have used in the course of our investigations we have made by warming a solution of pyromucic acid (3 parts) in absolute alcohol (5 parts) with concentrated sulphuric acid (3 parts acid, Sp. Gr. 1.84). After heating for four hours on the water bath, the mixture was allowed to cool, precipitated with water, and the ether washed with a dilute solution of sodic carbonate. The crude ether was then dried by exposure to the air and distilled. The yield of pure distilled ether which is thus obtained amounts to about 85 per cent of the weight of the acid taken. This is somewhat less than that which may be obtained by means of hydrochloric acid, but the method is much more expeditious and convenient. When dry chlorine is passed over ethyl pyromucate we found that the ether was rapidly liquefied with the evolution of heat, and that the formation of the addition product proceeds as described by Malaguti until the ether has increased in weight very nearly the amount re- quired by the addition of four atoms of chlorine. We soon found, however, that, no matter how carefully the chlorine was dried, hydro- chloric acid escaped, showing the formation of a substitution product, and that the amount of hydrochloric acid formed depended largely upon the rapidity of the stream of chlorine and the consequent eleva- tion of temperature. Even when the ether was carefully cooled to 0° during the whole of the treatment with chlorine, the formation of hydrochloric acid could not wholly be avoided. In this respect our experience agrees with that of Hill and Sanger,* who were unable to form the ethyl pyromucic tetrabromide without the simultaneous for- mation of substitution products. While the statements of Malaguti seemed to leave no room for doubt that the ethyl pyromucic tetrachlo- ride was completely carbonized by heat, experiments made with bro- mine in this laboratory had shown that substitution products could readily be formed from the ethyl pyromucic tetrabromide by heat, * These Proceedings, xxi. 155. OF ARTS AND SCIENCES. 323 and it seemed to us hardly conceivable that complete carbonization should ensue. A preliminary trial showed so much less charring under ordinary pressure than we had anticipated, that we were en- couraged to hope that the ethyl pyromucic tetrachloride itself might be distilled under diminished pressure without essential decomposition. Ethyl pyromucate was therefore carefully treated with chlorine at 0° until it ceased to gain in weight. Hydrochloric acid was given off in small quantity, and the total gain in weight was 94 per cent of the weight of ethyl pyromucate taken, instead of the theoretical gain of 101 per cent. The product was then fractionally distilled under a pressure of 15 mm. and showed its complex nature by the wide range of its boiling point, 104-160°. Above 160° there remained a residue which even under 15 mm. pressure could not be distilled without decomposition. None of the fractions showed any tendency to solidify in a freezing mixture. After several distillations, it became evident that the greater portion boiled without essential decomposition between 150-160°, and that a smaller portion boiled below 110°. In order to determine the nature of the several products, the follow- ing analyses were made. Each fraction was collected under 15 mm. pressure. A. Boiling point 104-110° ; weight = 2.6 grm. 0.2235 grm. substance gave 0.2139 grm. AgCl. Calculated for C6H2C103C2US. Found. CI 20.34 23.63 B. Boiling point 145-150° ; weight = 3.2 grm. 0.2334 grm. substance gave 0.4418 grm. Ag. CI. C Boiling point 152-153° ; weight = 7.7 grm. I. 0.1678 grm. substance gave 0.3431 grm. AgCl. II. 0.1415 grm. substance gave 0.2889 grm. AgCl. D. Boiling point 153-157° ; weight = 12.0 grm. 0.1502 grm. substance gave 0.3094 grm. AgCl. Found. Calculated for B. C. D. C5H30,C2II5C14. I. n. CI 50.36 46.77 50.55 50.49 50.97 From these analyses it was evident that the fraction C consisted of pure ethyl pyromucic tetrachloride ; the fraction D contained a slight 324 PROCEEDINGS OF THE AMERICAN ACADEMY admixture of a product containing a higher percentage of chlorine ; the fraction A approached in composition the ethyl chlorpyromucate ; while the fraction B was a mixture. In order to be quite sure of the correctness of our conclusions, we treated these successive fractions with an alcoholic solution of sodic hydrate, and obtained acids in each case confirming the results of our analyses. From fraction A we obtained an acid crystallizing from hot water in irregular leafy plates which melted at 176-177°. The physical properties and melting point were sufficient to identify this acid as the 8 chlorpyromucic acid later described, and to prove that the lower boiling fraction consisted chiefly of ethyl 8 chlorpyromucate. Fraction C yielded us without difficulty, and in nearly theoretical quantity, an acid which when re- crystallized twice from benzol melted sharply at 168-1G9°, and in other respects proved to be identical with the /3y dichlorpyromucic acid which we shall hereafter fully describe. The formation of this acid in nearly theoretical quantity and without recognizable admixture proves that the fraction C consisted of pure ethyl pyromucic tetrachloride. Fraction D yielded us a somewhat less pure j3y dichlorpyromucic acid, as did also fraction B. In the latter case, however, we were able to isolate a small quantity of a sparingly soluble acid, crystal- lizing from water in minute needles which closely resembled trichlor- pyromucic acid. It was therefore evident that the main product formed by the action of chlorine at 0° upon ethyl pyromucate was the tetra- chloride and this might be distilled under diminished pressure without essential decomposition. At the same time, it was shown that substi- tution was effected even in the cold, and that the product contained ethyl 8 chlorpyromucate and very possibly its tetrachloride. 8 Chlorpyromucic Acid. Since substitution had taken place at low temperatures, it seemed not unlikely that at 100° the substitution might be so rapid as to offer a convenient mode for the preparation of chlorpyromucic acids. Ethyl pyromucate when treated with bromine at 100° yields 8 brompyro- mucic and y3S brompyromucic acids still more readily than pyromucic acid itself. We accordingly passed dry chlorine through ethyl pyromu- cate heated to 100°, but found that a higher temperature was necessary in order that substitution might promptly be effected. At 145° the action was sufficiently rapid, and the chlorine was passed through the melted ether at this temperature until a gain in weight was noted which corresponded to the substitution of one hydrogen atom by chlo- rine. The viscous liquid which was thus obtained was then slowly OF ARTS AND SCIENCES. 325 added to an excess of a concentrated alcoholic solution of sodic hydrate, care being taken to avoid any great elevation of temperature. "When the action was completed the sparingly soluble sodium salt was re- moved by filtration and dried. The alcoholic filtrate contained small quantities of this sodium salt in solution, and contained further a small amount of some volatile furfuran compouud. We converted the excess of sodic hydrate into carbonate with carbonic dioxide, removed the sodic carbonate by filtration, and distilled the alcoholic filtrate. The distillate when mixed with water threw down a minute quantity of a colorless oil of peculiar aromatic odor, which we have as yet been unable to identify through lack of material. The small amount of sodium salt obtained from the alcoholic mother liquors was then added to the main portion. The sodium salt when dissolved in water and acidified with hydrochloric acid then yielded the crude 8 chlorpyro- mucic acid, which not infrequently needed no other purification than recrystallization from benzol. If, however, the treatment with chlorine had been too long continued, or the action had taken place at too low a temperature, the product contained dichlorpyromucic and trichlorpy- romucic acids which could not be removed by simple recrystallization. Whenever the crude acid failed on trial to crystallize from hot water in shining irregular plates, it was necessary to resort to chemical means for its purification. The acid was suspended in twenty times its weight of cold water, ammonia added in slight excess, and then baric chloride in quantity sufficient to precipitate the sparingly soluble barium salts of the admixed acids. After the separation of these salts is complete, the filtered solution gives on acidification an acid which crystallizes from water in leafy plates, and which may further be puri- fied by recrystallization from .benzol. The yield of chlorpyromucic acid thus obtained amounts to about 40 per cent of the weight of ether taken, or 38 per cent of the theoretical amount. I. 0.2761 grm. substance gave 0.4145 grm. CO., and 0.0494 grm. II20. II. 0.2G67 grm. substance gave 0.2642 grm. AgCl. III. 0.2990 'grm. substance gave 0.2950 grm. AgCl. Calculated for Found. cysjCio,. i. ii. in. C 40.96 40.94 H 2.05 1.99 CI 24.23 24.49 24.39 The 8 chlorpyromucic acid is readdy soluble in hot water, sparingly in cold water, and crystallizes in large irregular leafy plates, which 326 PROCEEDINGS OF THE AMERICAN ACADEMY closely resemble the corresponding bromine derivative. It dissolves readily in alcohol, ether, or hot benzol, but sparingly in cold benzol. The acid recrystallized from benzol melted at 176-177°, and a prepa- ration made from the pure etbyl ether melted at the same point. Its solubility in cold water was determined according to the method of V. Meyer. A weighed portion of the solution saturated at 19°. 5 was boiled with baric carbonate, and the barium dissolved determined by precipitation with sulphuric acid. I. 37.8458 grm. solution saturated at 19°.5 gave 0.0833 grm. BaS04. II. 33.5216 grm. solution saturated at 19°.5 gave 0.0742 grm. BaS04. According to these determinations, the solution saturated at 19°. 5 contained the following percentages of acid. i. n. 0.28 0.28 Baric S Chlorpyromucate, Ba(C5H2C10„)2 . H20. — The barium salt was prepared by boiling the acid with an excess of baric carbonate. The salt is quite readily soluble even in cold water, still more readily soluble in hot water, and separates from a hot concentrated solution in thin leafy plates, usually aggregated in globular form. The air- dried salt contains one molecule of water, which it loses rapidly at 100°. I. 1.2193 grm. air-dried salt lost at 100° 0.0491 grm. H20. II. 0.5932 grm. air-dried salt gave 0.3094 grm. BaS04. Calculated for Found. Ba(C5H2C103)2 . H20. I. II H20 4.04 4.04 Ba 30.72 30.67 0.6909 grm. salt dried at 100° gave 0.3763 grm. BaS04. Calculated for Ba(C5II2C103)2. Found. Ba 32.01 32.02 The solubility of the salt in cold water was determined according to the method of V. Meyer. I. 9.3523 grm. solution saturated at 19°.5 gave 0.2932 grm. BaS04. II. 8.3395 grm. solution saturated at 19°.5 gave 0.2534 grm. BaS04. The solution saturated at 19.5° therefore contained the following percentages of anhydrous salt. I. n. 5.76 5.58 OF ARTS AND SCIENCES. 327 Calcic o Chlorpyro?nucatei Ca(C5H2Cl(X)2 . 3 H20. — The calcium salt was prepared by boiling the acid with an excess of calcic car- bonate. It is readily soluble in hot water, rather sparingly soluble in cold water, and separates from a hot concentrated solution in clustered prisms with rectangular terminations. The air-dried salt contains three molecules of water. It effloresces slowly over sulphuric acid, and loses all its water readily at 100°. I. 1.0814 grm. air-dried salt lost at 100° 0.1480 grm. H,0. II. 1.2247 grm. air-dried salt lost at 100° 0.1689 grm. H20. Calculated for Found. Ca(C5H2C103)2 . 3 H20. I. II. H20 14.03 13.70 13.79 I. 0.6236 grm. salt dried at 100° gave 0.2564 grm. CaS04. II. 0.5509 grm. salt dried at 100° gave 0.2244 grm. CaS04. Calculated for Found. Ca(C6II2C103)2. i. II. 12.09 12.09 11.98 Ca The solubility of the salt in cold water was determined according to the method of V. Meyer. The calcium was precipitated as oxalate, and the oxalate ignited with sulphuric acid. I. 21.6494 grm. solution saturated at 19°. 5 gave 0.1002 grm. CaS04. II. 17.7467 grm. solution saturated at 19°.5 gave 0.0809 grm. CaS04. The solution saturated at 19°. 5 contained therefore the following percentages of anhydrous salt. i. n. 1.13 1.11 Potasstc 8 Chlorpyromucate, KC5H2C103. — The potassium salt is readily soluble even in cold water, and separates from a hot concen- trated solution on rapid cooling in fine branching needles ; on slower cooling, in small thin oblique plates. The salt lost nothing in weight when dried at 120°, and analysis showed it to be anhydrous. I. 0.6543 grm. salt dried at 120° gave 0.3100 grm. K2S04. II. 0.6390 grm. salt dried at 120° gave 0.3018 grm. K2S04. Calculated for Found. KC5H,C103. I. II. 21.18 21.27 21.20 K Argentic S Chlorpyromucate, AgC5H2C103. — The silver salt may best be prepared by precipitating a solution of the barium salt with argentic nitrate. 328 PROCEEDINGS OF THE AMERICAN ACADEMY For analysis the precipitated salt was well washed, recrystallized from hot water, and dried in vacuo over sulphuric acid. It is spar- ingly soluble even in hot water, and separates from a hot concentrated solution in irregularly branching flattened needles. I. 0.4843 grm. substance gave 0.2730 grm. AgCl. II. 0.3948 grm. substance gave 0.2220 grm. AgCl. Calculated for Found. AgC3H2C103. I. II. Ag 42.60 42.44 42.34 Ethyl 8 C/tlorpyromucate, C5H2C103C2H5. — The ethyl ether was pre- pared by heating at 100° a solution of 5 parts of 8 chlorpyromucic acid in 10 parts of absolute alcohol, with the addition of 5 parts of concentrated sulphuric acid (Sp. Gr. 1.84). After heating for three hours, the ether was precipitated by the addition of water, washed first with dilute sodic carbonate, then with water, and finally dried with calcic chloride. The ether is a colorless heavy oil boiling at 216-218° (column completely in vapor) under a pressure of 76.8 mm., solidifying at 1-2°, and melting at the same point. I. 0.2740 grm. substance gave 0.2219 grm. AgCl. II. 0.2918 grm. substance gave 0.2402 grm. AgCl. Calculated for Found. C6H2C103C2H5. I. II. CI 20.34 20.02 20.35 8 Chlorpyromucamide, C5H2C10.,NH2. — 8 chlorpyromucic ether is but slowly attacked by concentrated ammonia in the cold, and the amide may more readily be prepared from the acid chloride by means of solid ammonic carbonate. The amide is readily soluble in hot water, sparingly soluble in cold water and separates from a hot concentrated solution in fine branching needles, which melt at 154-155°. For analysis, the amide was dried over sulphuric acid. I. 0.1696 grm. substance gave 0.1677 grm. AgCl. II. 0.2933 grm. substance gave 25.7 c.c. moist N at 25° and under a pressure of 764 mm. Found. II. 9.82 Preparation I. was made from the ether, and II. from the acid chloride. CI Calculated for CEU2C102NH2. 24.40 I. 24.44 N 9.62 OF ARTS AND SCIENCES. 329 There seemed no room for doubt that the chlorpyromucic acid thus formed by the direct replacement of hydrogen by chlorine, like the 8 brompyromucic acid obtained in a similar way, contained its chlorine in the 8 position. We considered it necessary, however, to establish this point by direct experiment. Action of Bromine and Water. Although the action of bromine on 8 brompyromucic acid suspended in water varied greatly with the conditions, Hill and Sanger* found that, when the oxidation was carefully conducted, fumaric acid alone was formed. We therefore suspended the 8 chlorpyromucic acid in about twenty-five times its weight of water, and passed in bromine vapor slowly with a current of air. The acid gradually dissolved, and but little more than two molecules of bromine were needed to com- plete the oxidation. After standing for some time in the cold, the solution was evaporated to a small volume, and the crystalline acid which appeared as the solution cooled recrystallized from hot water. In this way we obtained a white crystalline acid which contained neither chlorine nor bromine, which was sparingly soluble in cold water, more readily in hot water, and which remained unchanged when heated to 200°. Although the acid was thus sufficiently char- acterized as fumaric acid, we further analyzed its silver salt. 0.4943 grm. substance dried at 120° gave 0.5591 grm. AgBr. Calculated for Ag,C4H204. Found. Ag 65.46 64.97 In the oxidation of the 8 chlorpyromucic acid by bromine water, fumaric acid, had therefore been formed according to the equation : C5H3C103 + 2 Br2 + 3 H20 = C4H404 + COa + 4 II Br + IIC1. Action of Nitric Acid. 8 chlorpyromucic acid is not as readily attacked by nitric acid as the 8 brompyromucic acid, and for its complete oxidation we found it neces- sary to heat one part of the acid with three parts of strong nitric acid (Sp. Gr. 1.42) diluted with twice its weight of water. After heat- ing for three hours the oxidation was completed, and on evaporation fumaric acid was obtained, which was recognized by its sufficiently characteristic physical properties. * These Proceedings, xxi. 144. 330 PROCEEDINGS OP THE AMERICAN ACADEMY (3 Chlorpyromucic Acid. Hill and Sanger* found no difficulty in preparing ft brompyro- mucic acid by the reduction of either of the two dibrornpyroniucic acids described by them. The corresponding dichlorpyromucic acida we found to be much more refractory, and we succeeded in preparing the j3 chlorpyromucic acid only after many unsuccessful attempts. The fSy dicblorpyromucic acid, which was the more accessible, proved to be the more difficult of reduction, so that almost the whole of the material for this investigation was made from the y8S dichlorpyromucic acid. When zinc dust is added to a cold ammoniacal solution of this acid, no perceptible reaction takes place, and even after long standing no essential change can be detected. Even when the ammoniacal solution is boiled with a large excess of zinc dust the reduction is but slowly effected, and long continued heating is necessary to complete the reaction. We have fouud it advantageous to dissolve the acid in about twenty times its weight of dilute amnionic hydrate, to add an equal weight of zinc dust, and to boil for eight or ten hours, taking care to keep the solution strongly ammoniacal. The filtered solution is then cooled and acidified with dilute sulphuric acid, the acid which separates removed by filtration, the filtrate extracted with ether, and the residue left upon the evaporation of the ether added to the main product. The crude acid thus obtained melted at about 130°, and evidently contained unaltered /38 dicblorpyromucic acid. We there- fore dissolved it in dilute amnionic hydrate, and added to the ammoni- acal solution calcic chloride as long as a sparingly soluble calcium salt was promptly precipitated. The filtered solution then gave, when acidified with hydrochloric acid, a crystalline acid, which after recrys- tallization from hot water melted at 145-146°, and proved upon analysis to be a chlorpyromucic acid. From the sparingly soluble calcium salt, which had been removed by filtration, we obtained only unaltered fi& dichlorpyromucic acid, which in its turn was treated with zinc dust. In this way we found it possible to obtain from the /?S di- chlorpyromucic acid at least 80 per cent of the theoretical amount of pure /3 chlorpyromucic acid. Zinc dust, even after long boiling, seems to have but little action upon /3y dichlorpyromucic acid in ammoniacal solution, but sodium amalgam slowly reduces it at 100°. In order to effect complete reduction, it proved to be necessary to use a large ex- cess of sodium in the form of a one per cent amalgam, and the reaction was then completed after heating for three hours on the water bath. * These Proceedings, xxi. 147. OF ARTS AND SCIENCES. 831 The acid obtained by acidification melted at 145-146°, contained the percentage of chlorine required by a chlorpyromucic acid, and appeared to be in all respects identical with the acid obtained from the /38 dichlor- pyromucic acid. While the yield of pure acid was in this case but 50 per cent of the theoretical amount, it is possible that it might be somewhat increased by further experiments. From the third iso- meric dichlorpyromucic acid, subsequently described, we have as yet been able to obtain no definite reduction product. The {3 chlorpyromucic acid dried over sulphuric acid gave on analy- sis the following results : — I. 0.2710 grm. substance gave 0.4073 grm. C02 and 0.0513 grm. H20. II. 0.1385 grm. substance gave 0.1355 grm. AgCl. III. 0.1736 grm. substance gave 0.1692 grm. AgCl. i. in. c Calculated for C6HaC103. 40.96 i. 40.99 Found. II. H 2.05 2.10 CI 24.23 24.18 24.10 Analysis III. was made with material prepared from the fiy dichlor- pyromucic acid. /3 chlorpyromucic acid is readily soluble in hot water, sparingly sol- uble in cold water, and crystallizes from hot aqueous solution in thin irregular striated plates or flattened prisms. It is readily soluble in alcohol, ether, hot benzol or hot chloroform, and is but sparingly sol- uble in cold benzol or cold chloroform. "When repeatedly crystallized from hot water it melted at 145-146°, and recrystallization from other solvents failed to raise this melting point. In order to determine the solubility of the acid in cold water, a weighed quantity of a solution of the acid saturated at 19°.8 was boiled with baric carbonate, and the barium taken into solution precipitated as sulphate. I. 31.6300 grm. solution saturated at 19°.8 gave 0.201 9 grm. BaS04. II. 34.0328 grm. solution saturated at 19.°8 gave 0.2176 grm. BaS04. The solution saturated at 19°.8 therefore contained the following percentages of the acid : — i. n. 0.80 0.80 For the further characterization of the acid we prepared certain of its salts. 332 PROCEEDINGS OP THE AMERICAN ACADEMY Baric ft Chlorjvjromucate, Ba(C5H2C103)2 . H20. — The barium salt was prepared by boiling a solution of the acid with an excess of baric carbonate. The filtered solution was evaporated, and the salt which separated on cooling recrystallized from hot water. It proved to be readily soluble in hot water, more sparingly soluble in cold water, and crystallized in long obliquely terminated prisms, which contained one molecule of water. The salt is permanent in the air or over sulphuric acid, but loses its water readily at 100°. I. 0.6092 grm. of the air-dried salt gave 0.3180 grm. BaS04. II. 1.3540 grm. of the air-dried salt lost at 100° 0.0576 grm. H20. Calculated for Found. Ba(C5H2C103)2.H20. I. II. Ba 30.72 30.69 H20 4.04 4.25 0.4749 grm. of the salt dried at 100° gave 0.2587 grm. BaS04. Calculated for Ba(C5H2C103).,. Found. Ba 32.01 32.03 The solubility of the salt in cold water was determined in the usual way. I. 10.2683 grm. solution saturated at 1 9°.l gave 0.1 1 49 grm. BaS04. II. 6.8737 grm. solution saturated at 19°. 1 gave 0.0747 grm. BaSQ.. According to these determinations, the aqueous solution saturated at 19°. 1 contained the following percentages of the anhydrous salt: — i. II. 2.06 2.00 Calcic /? Chlorpyromucate, Ca(C5H2C10„)2 . 3 H20. — This salt was prepared by neutralizing with calcic carbonate a boiling solution of the acid. If the solution thus obtained is evaporated upon the water bath clustered, pointed prisms of an anhydrous salt are formed when the solution becomes highly concentrated. By evaporation in vacuo over sulphuric acid at ordinary temperatures, tufts of fine branching prisms are obtained which contain three molecules of water. The latter salt is permanent in the air, effloresces over sulphuric acid, and loses its water readily at 105°. I. 0.4226 grm. of the air-dried salt gave 0.1490 grm. CaS04. II. 1.3627 grm. of the air-dried salt lost at 105° 0.1902 grm. H20. Calculated for Found. Ca(C6lI2C10.,),.3H20. I. II. Ca 10.39 10.37 H20 14.03 13.95 OP ARTS AND SCIENCES. 333 0.5160 grm. of the salt dried at 105° gave 0.2111 grm. CaS04. Calculated for Ca(C5H2C103)3. Found. Ca 12.09 12.03 The pointed prisms obtained by evaporating the solution at 100° gave the following results. 0.4433 grm. of the air-dried salt gave 0.1796 grm. CaSOr Calculated for Cu(,C5II,C103)?. Found. Ca 12.09 11.92 The solubility of the calcium salt in cold water was determined in the usual manner. The calcium was precipitated as oxalate, and con- verted into the sulphate before weighing. I. 5.0960 grm. solution saturated at 19°. 5 gave 0.0653 grm. CaS04. II. 5.8981 grm. solution saturated at 19°. 5 gave 0.0752 grm. CaS04. According to these determinations, the aqueous solution saturated at 19°.5 contained the following percentages of the anhydrous salt: — i. ii. 3.12 3.10 Ethyl (3 Chlorpyromucate, C.H2C103. C2H5. — The ethyl ether was prepared by heating at 100° for four hours a mixture of 2 parts of the acid. 3 parts of absolute alcohol, and 2 parts of sulphuric acid (Sp.Gr. 1.84). On dilution with water the ether separated as an oil, which was thoroughly washed and dried over calcic chloride. It then dis- tilled without essential decomposition at 217° (mercury column com- pletely in vapor) under a pressure of 764 mm. The liquid distillate solidified on cooling, with the formation of concentrically grouped prisms, which, after repeated recrystallization by cooling the melted ether, showed the constant melting point of 29-30°. 0.1864 grm. of substance gave 0.1523 grm. AgCl. Calculated for C6H2C103 . C2H6. Found. CI 20.34 20.19 Action of Nitric Acid. /3 chlorpyromucic acid is readily attacked by dilute nitric acid, but the oxidation is not smoothly effected, and the yield of chlorfumaric acid is comparatively small. The best results were obtained when the acid was boiled with 2 parts of nitric acid (Sp. Gr. 1.42) diluted with 334 PROCEEDINGS OF THE AMERICAN ACADEMY 5 parts of water. After the lapse of two hours, the action appeared to be completed, although a few drops of oil were still suspended in the clear solution. The products of the reaction were then extracted from the diluted solution with ether, the residue obtained by the evaporation of the ether pressed thoroughly with filter-paper and dried at 100°. The dry residue was then repeatedly washed with benzol in which chlorfumaric acid is but sparingly soluble. The product thus obtained was readily soluble in water, almost insoluble in benzol, melted at 188°, and contained the percentage of chlorine required by chlorfumaric acid.* 0.1089 grm. substance dried over H2S04 gave 0.1027 grm. AgCl. Calculated for C4H3C104. Found. CI 23.59 23.31 The reaction may therefore be represented, in part at least, by the equation C5H3C103 + 30 = C4TI3C104 + C02. Action of Bromine and Water. Since j3 brompyromucic acid in aqueous solution is readily con- verted by an excess of bromine into mucobromic acid,f it seemed to us of interest to study the behavior of the (3 chlorpyromucic acid under the same conditions, since a product containing bromine and chlorine might then be formed. The acid was therefore suspended in five times its weight of water, and an excess of bromine at once added. After heating for a short time a clear nearly colorless solution was obtained, which was concentrated by evaporation on the water bath. On cooling, the solution deposited a crystalline acid which was readily soluble in hot water or hot benzol, and but sparingly soluble in these solvents in the cold. The acid recrystallized from water formed thin rhombic plates which melted at 120-121°, but this melting point could easily be raised to 121-122° by recrystallization from benzol. An analysis of the substance dried over sulphuric acid showed that it was the mucochlorbromic acid whose formation we had been led to expect. 0.2871 grm. substance gave 0.4486 grm. AgCl + AgBr. Calculated for C4U2BrC103. Found. Br+Cl 54.11 54.45 * Kauder (Journ. f. prakt. Chem., [2], xxxi. 28) gives the' melting point of chlorfumaric acid as 191°. t These Proceedings, xxi. 152. OP ARTS AND SCIENCES. 335 The reaction was then precisely analogous to that by means of which mucobromic acid was formed from (3 brompyromucic acid : C5HX103 + 3 Br2 + 2 H20 = C4H2BrC103 + Co2 + 5 HBr. With the material which for the moment was at our disposal, we were unable to study the decomposition of the mucochlorbromic acid by alkalies. We shall hope in the future to prepare in this way a chlor- bromacrylic acid, and compare it with the acid of the same composi- tion already described by Mabery and Loyd.* (3y DlCHLORPYROMUCIC ACID. Hill and Sanger f had shown that in the decomposition of pyromu- cic tetrabromide or of ethyl pyromucic tetrabromide by alcoholic sodic hydrate, two isomeric dibrompyromucic acids are formed in not widely unequal quantities. There was, therefore, every reason to expect that two isomeric dichlorpyromucic acids could be found in the product formed in a similar way from ethyl pyromucic tetrachloride. Since we had found that a low temperature was essential to the preparation of a pure product, we allowed the ethyl pyromucate to absorb chlorine at 0° until a constant weight was reached, expelled the excess of chlo- rine by a current of dry air, and decomposed the product at once with an excess of an alcoholic solution of sodic hydrate. The best results were obtained when the tetrachloride was slowly added to a concen- trated sodic hydrate solution, taking care to keep the mixture cold. The sodium salts formed are sparingly soluble in alcohol, and after a short time can be removed by filtration. The alcoholic solution was freed from the excess of sodic hydrate by means of carbonic dioxide, and, after removing the sodic carbonate by filtration, distilled. The sodium salts left on distillation appeared to be identical with those already obtained and were therefore added to the main portion. The alcoholic distillate grew turbid when mixed with water, and gradually deposited a small quantity of a colorless oil which had a peculiar aro- matic odor. The quantity of this oil was so small that no investiga- tion of it has as yet been made. The sodium salt which was obtained from the tetrachloride was dried, dissolved in hot water, and acidified with hydrochloric acid. In this way an acid was obtained which crystallized in finely felted needles which usually melted at 155°. After two recrystallizations from benzol the acid melted at 108-169°, and further recrystalliza- * These Proceedings, xvi. 238. t These Proceedings, xxi. 150. 336 PROCEEDINGS OP THE AMERICAN ACADEMY tions failed to raise this melting point. Analysis showed this acid to be a dichlorpyromucic acid. I. 0.4235 grm. substance gave 0.51 35 grm. C02 and 0.0455 grm. H20. II. 0.2332 grm. substance gave 0.3695 grm. AgCl. III. 0.2195 grm. substance gave 0.3490 grm. AgCl. Calculated for Found. CSH2C1,03. I. II. III. C 33.15 33.07 H 1.10 1.19 CI 39.22 39.16 39.31 The acid, which proved on subsequent investigation to be the (3y dichlorpyromucic acid, is sparingly soluble in cold water, readily in hot, and crystallizes as the solution cools in finely felted needles. It is readily soluble in alcohol, ether, or in hot benzol ; in cold benzol it is sparingly soluble and crystallizes from it in short prisms. In hot chloroform it is also readily soluble, sparingly soluble in the cold. The ready purification of this acid by recrystallization rendered it improbable that any sensible amount of an isomeric acid was formed with it. The most patient search has failed to show the formation of such a product in appreciable quantity, and from pure ethyl pyromucic tetrachloride almost pure /3y dichlorpyromucic acid is obtained at once. The yield of pure acid ordinarily obtained from pyromucic ether is not wholly satisfactory, since it amounts to about 50 per cent of the weight of ether taken, or about 39 per cent of the theoretical amount. The solubility of the acid in cold water we determined as usual. A weighed quantity of a solution of the acid saturated at 19.5° was boiled with baric carbonate and the barium dissolved precipitated by sulphuric acid. I. 36.2505 grm. solution saturated at 19°.5 gave 0.0619 grm. BaS04. II. 35.6546 grm. solution saturated at 19°.5 gave 0.0615 grm. BaS04. According to these determinations, the solution saturated at 19°. 5 contains the following percentages of acid : — i. ii. ■ 0.27 0.27 Baric fiy Dichlorpyromiicate, Ba(C5HCl203) . 3 H20.* — The barium salt may be most conveniently prepared by precipitating a solution of the * We have already referred to the brief description of the &y dichlorpyro- mucic acid published by Denaro in the Gazzetta Chimica (xvi. 333), and have asserted that the analyses of the two salts which he describes are not worthy of confidence. In support of our assertion we append his results in full, together OF ARTS AND SCIENCES. 337 ammonium salt with baric chloride. It is rather sparingly soluble even in hot water, and still less soluble in cold water. It separates from a hot concentrated solution in fine clustered needles which contain three molecules of water. The crystals are permanent in the air, but lose their water readily at 100°. I. 1.2048 grm. air-dried salt lost at 100° 0.1170 grm. H20. II. 1.2118 grm. air-dried salt lost at 100° 0.1132 grm. H20. III. 0.5694 grm. air-dried salt gave 0.2393 grm. BaS04. IV. 0.3783 grm. air-dried salt gave 0.1593 grm. BaS04. Calculated for Found. Ba(C5HCl203)2 . 3 H20. I. II. IH. IV. H20 9.80 9.71 9.34 Ba 24.86 24.71 24.76 I. 0.4828 grm. salt dried at 100° gave 0.2250 grm. BaSOv II. 0.5540 grm. salt dried at 100° gave 0.2579 grm. BaS04. Calculated for Found. Ba(C5HCl2Os)2. I. II. Ba 27.56 ' 27.40 27.36 The solubility of the salt in water at 19°.5 was determined accord- ing to the method of V. Meyer. with the analytical data upon which they depend. The errors in the calculated percentages are corrected in parenthesis. Barium salt : 0.4480 grm. of the salt lost at 110° 0.00204 grm. H20. Calculated for Ba(C6HCl203)2 . 3 H20. Found. H.20 9.80 8.30 (0.445) 0.1939 grm. of the dry salt gave 0.0769 grm. BaS04. Calculated for Ba(C5HCl,03)2. Found Ba 23.54 (27.56) 23.32 Calcium salt: 0.6942 grm. of the salt lost at 110° 0.0300 grm. H20. Calculated for Ca(C5HClo03), . 3£ H20. Found. H20 13.60 14.45 (4.32) 0.3024 grm. of the salt gave 0.1072 grm. CaS04. Calculated for Ca(C5HCl20,)2. Found. Ca 10.00 10-42 These results can hardly be explained unless it is assumed that they con- tain both typographical arid arithmetical errors. The two remaining analyses contained in Denaro's paper, two chlorine determinations in the free acid are correctly calculated, and agree well with the theory. vol. xxiv. (n. s. xvi. ) 22 338 PROCEEDINGS OP THE AMERICAN ACADEMY I. 23.0222 grm. solution saturated at 19°.5 gave 0.0503 grm. BaS04. II. 22.4890 grm. solution saturated at 19°.5 gave 0.0487 grm. BaS04. The solution saturated at 19.5° therefore contained the following per- centages of anhydrous salt. i. n. 0.46 0.46 Calcic /3y Dichlorpyromucate, Ca(C5HCl203)2 . 4 H20. — The calcium salt was prepared by boiling a solution of the acid with an excess of calcic carbonate. It is readily soluble in hot water, less soluble in cold, and crystallizes from a hot concentrated solution in long clustered needles which contain four molecules of water. The crystallized salt is permanent in the air, effloresces slowly over sulphuric acid, and loses all its water readily at 110°. I. 2.7640 grm. air-dried salt lost at 11"0° 0.4160 grm. H20. II. 3.1275 grm. air-dried salt lost at 113° 0.4707 grm. H20. Calculated for Found. Ca(C6HCK03)2 . 4 H20. I. II. H20 15.26 15.05 15.05 I. 0.6595 grm. salt dried at 110° gave 0.2227 grm. CaS04. II. 0.7004 grm. salt dried at 113° gave 0.2366 grm. CaS04. Calculated for Found. Ca(C6HCl.,03)2. I. II. Ca 10.00 9.93 9.94 The solubility of the salt in water at 19.5° was determined as usual. The calcium was precipitated as oxalate and the oxalate ignited with sulphuric acid. I. 22.8797 grm. solution saturated at 19°. 5 gave 0.0944 grm. CaS04. II. 21.5915 grm. solution saturated at 19°. 5 gave 0.0891 grm. CaS04. The solution saturated at 19°. 5 therefore contained the following percentages of anhydrous salt: i. n. 1.21 1.21 Potassic fiy Dichlorpyromucate, KC5HC1208. — The potassium salt is readily soluble in hot water, but rather sparingly soluble in cold water, and separates from a hot concentrated solution in small prisms which are anhydrous. I. 0.6130 grm. substance dried at 120° gave 0.2435 grm. K2S04. II. 0.8200 grm. substance dried at 120° gave 0.3265 grm. K2S04. Calculated for Found. KCr>HCUOs. I. II. K 17.84 17.83 17.87 OP ARTS AND SCIENCES. 339 Argentic fty Dichlorpyromucate, AgC5HCl203. — If argentic nitrate is added to a cold aqueous solution of the acid, the silver salt is pre- cipitated in the form of fine needles. For analysis 'we prepared the salt by precipitating a dilute neutral solution of the ammonium salt with argentic nitrate, and recrystallizing the precipitated salt from hot water. It is sparingly soluble even in hot water, and separates on cooling the hot saturated solution in fine needles. I. 0.3230 grm. substance dried over H2S04 gave 0.1612 grm. Ao-Cl. II. 0.2580 grm. substance dried over H2S04 gave 0.1282 grm. AgCl. Calculated for Found. AgC5HCl2Os. I. II. Ag 37.50 37.57 37.41 Ethyl /3y Dichlorpyromucate, C5IIC1203C2H5. — The ethyl ether was prepared by heating at 100° for three hours a mixture of 5 parts of acid, 8 parts of absolute alcohol, and 5 parts of concentrated sulphuric acid (Sp. Gr. 1.84). It was precipitated with water, washed with dilute sodic carbonate, and then with water. It is readily soluble in hot alcohol, more sparingly in cold, and crystallizes in large needles which melt at 63-64°. I. 0.2645 grm. substance dried over H2S04gave 0.3640 grm. AgCl. II. 0.1933 grm. substance dried over H2S04 gave 0.2673 grm. AgCl. Calculated for Found. CfiHCljO^Hs. I. II. CI 33.98" 34.02 34.18 fiy Dichlorpyrmucamide, C5HC1202NII2. — The ethyl ether of /?y dichlorpyromucic acid is readily attacked by strong aqueous ammonia even in the cold, and in a short time is converted into the amide. The amide is sparingly soluble even in hot water, and crystallizes in long slender needles which melt at 176-177°. 0.4015 grm. substance dried over II2S04 gave 28.5 c.c. moist N at 23° under a pressure of 767 mm. Calculated for C3nCU02NII2. Fcund. N 778 8.03 The formation of but one dichlorpyromucic acid in the decomposi- tion of the ethyl pyromucic tetrachloride by alkalies, while two iso- meric acids are always obtained under the same circumstances from the corresponding bromine compound, made it impossible to predict its constitution from the method of formation. Still, its comparatively high melting point, its physical properties, and the ready solubility of 340 PROCEEDINGS OF THE AMERICAN ACADEMY its calcium salt, in which it closely resembled the /?y dibrompyromucic acid, gave fair ground for the conjecture that it had a similar struc- ture. A study of its oxidation products showed that such was the case, since we easily obtained from it mucochloric and dichlormaleic acids. Action of Bromine and Water. If bromine is added to f3y dichlorpyromucic acid suspended in six or eight times its weight of cold water, oxidation rapidly ensues, with the escape of carbonic dioxide. A slight excess of bromine was added, and the reaction completed by the aid of heat. On cooling, the solution solidified with the separation of colorless crystals, which when recrystallized from water and finally from benzol melted at 124—125°, and had the characteristic form of mucochloric acid. Analysis also gave the proper percentage of chlorine. I. 0.2015 grm. substance dried over H2S04 gave 0.3408 grm. AgCl. II. 0.2320 grm. substance dried over H2S04 gave 0.3922 grm. AgCl. Calculated for Found. C4H2C1203. I. II. CI 42.01 41.81 41.79 In this case the reaction may be represented by the equation C6H2C1203 + 2Br2 + 2 H20 = C4H2C1203 + C02 + 4 HBr. Action of Nitric Acid. Nitric acid acts but slowly upon the fty dichlorpyromucic acid, and for its complete oxidation we have found it necessary to take for one part of the acid 3 parts of concentrated nitric acid (Sp. Gr. 1.42) diluted with twice its weight of water. After boiling for five hours the action appeared to be complete, and as the clear solution deposited nothing on cooling we extracted it with ether. The ether left upon evaporation a colorless crystalline mass, which proved to be a mixture of two substances, one readily soluble, the other but sparingly soluble in cold water. The sparingly soluble substance when recrystallized from hot water was recognized by its crystalline form and by its melting point, 124-125°, as mucochloric acid. The acid, which was readily soluble in cold water, was neutralized with baric carbonate, the barium salt precipitated from its aqueous solution by alcohol, and the acid liberated from this purified barium salt again extracted with ether. The crystalline acid left by the evaporation of the ether was then dissolved in a small amount of water, and on standing well OF ARTS AND SCIENCES. 341 formed rhombic plates separated which were dried over sulphuric acid for analysis. 0.2233 grm. substance gave 0.3433 grm. AgCl. Calculated for C4U2C1204. FouDd. CI 38.38 38.01 The identity of this acid with dichlormaleic acid was further de- termined by the melting point of the anhydride prepared by sublima- tion, which we found to be 119-120°, in agreement with the statement of Ciamician and Silber.* The oxidation therefore took place in accordance with the following reactions, C5H2C1208 +20= C4H2CI208 -f C02, C5H2C1203 +30 = C4H2C1204 + C02, and the dichlorpyromucic acid in question is thus conclusively shown to have its chlorine atoms in the j3 and y positions. Preparation of Isomeric Dichlorpyromucic Acids. Although we had been unable to find the (38 dichlorpyromucic acid among the products formed by the action of alkalies upon ethyl pyromucic tetrachloride, it seemed to us probable that it might be formed under the proper conditions by the direct action of chlorine upon ethyl pyromucate, or by the decomposition of its tetrachloride by heat alone. Tunnies f had already shown that 8 brompyromucic acid could be formed by heating pyromucic tetrabromide, and Hill and Sanger $ had further shown that 8 brompyromucic acid and /38 dibrompyromucic acid could conveniently be made by the action of bromine upon pyro- mucic acid at high temperature. As subsequent experiments in this laboratory had shown that these two acids could more advantageously be made by substituting the ethyl ether for the acid, and our own experiments had shown that the S chlorpyromucic acid could readily be made in this way, we proceeded to study the action of chlorine upon ethyl pyromucate at high temperature. It seems hardly neces- sary to describe in detail the numerous experiments which we made under widely varying conditions, each one of which yielded us purely negative results. Ethyl pyromucate was treated with chlorine at * Berichte d. deutsch. chem. Gesellscb., xvi. 2390. t Ibid., xi. 1088. | These Proceedings, xxi. 130, 100. 342 PROCEEDINGS OP THE AMERICAN ACADEMY temperatures ranging from 145° to its boiling point, both by itself and after the addition of iodine or aluminic chloride, but in no case was the desired product obtained. Pyromucic acid and 8 chlorpyroniucic acid also failed to give such a product when treated at high tempera- tures with chlorine, and we were equally unsuccessful when we used the chloranhydrides of these acids either with or without an excess of phosphoric pentachloride. We then studied the action of heat upon the tetrachloride of pyromucic acid itself, of its chloranhydride and ethyl ether, and of the ethyl ether of S chlorpyromucic acid, and found in each case that small quantities of a dichlorpyromucic acid were formed which closely resembled the (38 dibrompyromucic. A more careful investigation further proved that in the decomposition of the ethyl pyromucic tetrachloride a second new dichlorpyromucic acid was formed concerning whose constitution we are not yet able to speak definitely. This acid we propose to call the ^ dichlorpyromucic acid until its structure is established. The amount of the dichlorpyromucic acids which we have been able to obtain is but small, and we have made many unsuccessful attempts to increase the yield by varying the temperature or the mode of heating, or by adding iodine, or aluminic or ferric chloride, before heating. We first obtained the (38 dichlorpyromucic acid by distilling under ordinary pressure the product formed by treating pyromucic acid with chlorine at 100°. Hydrochloric acid is given off in quantity, and, although a large carbonaceous residue is left in the retort, a liquid distillate is obtained which, after repeated distillation through a Hempel's column, amounts to about 85 per cent of the weight of the pyromucic acid taken and then distils leaving but an insignificant carbonaceous residue. This distillate is extremely complex in its nature and we have as yet made no thorough study of its constituents. We found, however, that the portions which boiled between 196° and 220° gave considerable quantities of (38 dichlorpyromucic acid when treated with cold water. They therefore contained the corresponding chloranhydride of the acid. The yield thus obtained amounted to but about 4 per cent of the pyromucic acid taken. From ethyl pyromucic tetrachloride we succeeded in obtaining a somewhat better yield. We found it advantageous to purify the tetrachloride by one distillation in vacuo, and to distil the product thus obtained under ordinary pressure. More or less carbonization ensued, and on frac- tional distillation in vacuo through a Hempel's column * the distillate * For fractional distillation under diminished pressure we used the extremely convenient apparatus of Anschiitz. We found that the ease of separation could OF ARTS AND SCIENCES. 343 was found to contain considerable unaltered tetrachloride. That portion which boiled above 140° under 16 ram. pressure was there- fore redistilled under ordinary pressure and the distillate again frac- tioned in vacuo. After repeated distillations we found that the portion which boiled between 118° and 123° under 16 mm. pressure partially solidified on cooling, and that a few crystals were also formed in the next lower fraction. These fractions were therefore strongly cooled and the crystalline solid removed by filtration and the liquid portions further distilled. The solid thus obtained proved to be the ethyl ether of the new x dichlorpyromucic acid melting at 197-198°, which we shall presently describe. When no more of this crystalline ether could be obtained by cooling, the liquid fractions were saponified by alcoholic sodic hydrate, the acids liberated by hydrochloric acid and separated through their calcium and barium salts. From the fraction boiling below 110° (16 mm.) we obtained chiefly 8 chlorpyromucic acid melting at 176-177°, although it yielded also a small quantity of (38 dichlorpyromucic acid, which was readily isolated by means of its sparingly soluble barium salt. The fractions 110-118° and 118-123° apparently consisted chiefly of the ethyl ether of j3d dichlorpyromucic acid, but the latter necessarily contained also a small amount of the crystalline ethyl % dichlorpyromucate held in solution. The two dichlorpyromucic acids could readily be separated through the differ- ent solubilities of their calcium salts, the calcic (38 dichlorpyromucate like the calcium salt of the corresponding bromine derivative being very sparingly soluble in water. From 123° to 130° but an insignifi- cant fraction was collected and the fraction 130°-153° consisted in part at least of unaltered ethyl pyromucic tetrachloride, from which j3y dichlorpyromucic acid was obtained. 100 grin, of ethyl pyromucate yielded us 197 grm. of the tetrachlo- ride and from this we obtained the following weights of pure products : be materially increased by filling a few inches of the stem of the distilling flask with glass beads, and thus combining the Hempel's column with the vacuum distillation. The beads were supported upon a perforated disk of platinum foil slipped over the capillary air tube and held in place by a slight enlargement of the tube. The thermometer was then raised to the proper line by a short bit of small glass tubing dropped into the air tube. Ilantzsch (Ann. Chem. u. Pharm., ccxlix. 57) has used with advantage for distillation under ordinary pressure a long necked boiling flask whose stem is partially filled with beads supported upon a platinum foil forced into the neck. We have for a long time used such a Hempel's column, but have supported the beads conveniently upon a glass bulb which nearly fills the stem and whose sealed neck is long enough to rest upon the bottom of the flask. 344 PROCEEDINGS OP THE AMERICAN ACADEMY 5.0 grm. 8 chlorpyromucic acid. 12.2 grm. /38 dichlorpyromucic acid. 2.7 grm. x dichlorpyromucic acid. 16.1 grm. ethyl x dichlorpyromucate. If pyromucyl chloride is treated with chlorine at 0°, the chlorine is absorbed very slowly, but the gain in weight finally approximately cor- responds with that required for the formation of a tetrachloride. If the tetrachloride is distilled under ordinary pressure, only an inconsid- erable carbonaceous residue is left in the retort, and after repeated distillations through a Hempel's columu under ordinary pressure a product is obtained which, when treated with water, yields the /J8 dichlorpyromucic acid and the x dichlorpyromucic acid. While the yield of the /SS dichlorpyromucic acid thus obtained is somewhat greater than that obtained from the ethyl pyromucic tetrachloride, the yield of the x dichlorpyromucic acid is much smaller. By treating ethyl 8 chlorpyromucate in the cold with chlorine, and distilling the addition product thus formed under ordinary pressure, we also obtained the (38 dichlorpyromucic acid. While the yield was somewhat larger than that obtained from the ethyl pyromucic tetra- chloride, it did not repay us for the loss of time and material involved in making the 8 chlorpyromucic acid. Moreover, to our surprise, we could obtain in this way none of the crystalline ethyl x dichlorpyro- mucate. /38 Dichlorpyromucic Acid. The acid whose preparation has just been described can most readily be purified by repeated precipitation from ammoniacal solution with calcic chloride, and recrystallization from chloroform. The acid thus purified gave on analysis the following results : I. 0.2577 grm. substance gave 0.3129 grm. C0.2 and 0.0259 grm. H20. II. 0.1933 grm. substance gave 0.3053 grm. AgCl. Calculated for Found. C5U2C103. I. II. C 33.15 33.11 H 1.10 1.12 CI 39.22 39.04 /3S dichlorpyromucic acid is readily soluble in ether or alcohol. It dissolves readily in hot water, benzol, or chloroform, and the greater part of the acid is in each case deposited on cooling in oblique prisms, which are frequently twinned in forms which can hardly be distin- OF ARTS AND SCIENCES. 345 guished from those of the (38 dibrompyromucic acid. The acid melts sharply at 155-156°, and sublimes unaltered at a higher temperature. The solubility of the acid in water at 19°. 5 was determined in the usual manner. A weighed quantity of a solution of the acid saturated at 19°. 5 was boiled with baric carbonate, and the barium dissolved determined by precipitation with sulphuric acid : I. 42.8007 grm. solution saturated at 19°.5 gave 0.0724 grm. BaS04. II. 51.4109 grm. solution saturated at 19°.5 gave 0.0907 grm. BaS04. According to these determinations, the solution saturated at 19°. 5 contained the following percentages of acid : I. II. 0.26 0.27 Baric (38 Dichlorpyromucate, Ba(C5HCl.203)2. 4 H20. — The barium salt was prepared by precipitating a dilute solution of the ammonium salt with baric chloride, and recrystallizing the product thus obtained from water. The salt is sparingly soluble in hot water, still less solu- ble in cold water, and crystallizes from a hot concentrated solution in long irregular flat prisms which contain four molecules of water. The salt is permanent in the air, effloresces over sulphuric acid, and loses its water readily at 100°. I. 1.4513 grm. air-dried salt lost at 100° 0.1795 grm. H20. II. 0.4908 grm. air-dried salt gave 0.1981 grm. BaS04. Calculated for Found. Ba(C5HCl203)2 .4H20. I. II. H20 12.66 12.37 Ba 24.07 23.73 0.4751 grm. salt dried at 100° gave 0.2205 grm. BaS04. Calculated for Ba(C5HCl203)j. Found. Ba 27.56 27.29 The solubility of the salt in water at 19.5° was determined in the usual manner. I. 28.4671 grm. solution saturated at 19°.5 gave 0.0561 grm. BaS04. II. 28.6844 grm. solution saturated at 19°.5 gave 0.0573 grm.BaS04. The solution saturated at 19°.5 therefore contained the following percentages of anhydrous salt : I. ii. 0.42 0.43 346 PROCEEDINGS OF THE AMERICAN ACADEMY Calcic /38 Dichlorpyromucate, Ca(C5HCl.203)2 . 3 H20. — Tlie cal- cium salt was prepared by precipitating a dilute solution of the ammo- nium salt with calcic chloride, and recrystallizing the product from hot water. It is but sparingly soluble in hot water, still less soluble in cold water, and separates from a hot concentrated solution in flattened prisms with rectangular terminations. The crystallized salt is perma- nent in the air, effloresces slowly over sulphuric acid and loses all its water at 125°. I. 1.5490 grm. air-dried salt lost at 125° 0.1820 grm. H20. II. 0.4067 grm. air-dried salt gave 0.1219 grm. CaS04. Calculated for Found. Ca(C5HCl,03)2 . 3 H20. I. II. H,0 11.90 11.75 Ca 8.81 8.81 0.6899 grm. salt dried at 125° gave 0.2332 grm. CaS04. Calculated for Ca(C6HCl203)2. Found. Ca 10.00 9.94 The solubility of the salt in water at 19°. 5 was determined in the usual manner. The calcium was precipitated as oxalate and ignited with sulphuric acid. I. 32.1733 grm. solution saturated at 19°. 5 gave 0.0244 grin. CaS04. II. 36.7555 grm. solution saturated at 19°.5 gave 0.0289 grm. CaS04. The solution saturated at 19°. 5 therefore contained the following percentages of anhydrous salt : I. IT. 0.22 0.23 Ethyl /3S Dichlorpyromucate, C5HC1203C2H5. — The ethyl ether was prepared by the action of ethyl iodide on the silver salt, and is a heavy liquid of pleasant odor. It melts at 2-3° and distils at 116-118° under a pressure of 16 mm., the oil bath being at 165-175°. An analysis of the distilled ether gave the following result. 0.2157 grm. substance gave 0.2957 grm. AgCl. Calculated for Found. C6HC1203C2H5. CI 33.98 33.89 /3S Dichlorpyromucamide, CSHC1202NH2. — The ethyl ether is but slowly attacked by concentrated ammonia in the cold, but at 100° it is readily converted to the amide. The amide is sparingly soluble in OF ARTS AND SCIENCES. 347 cold water, more readily in hot, and separates from a hot concentrated solution in long needles which on standing are converted into oblique prisms which melt at 153-154°. 0.2781 grm. substance dried over H2S04 gave 20.0 c.c. moist N at 25.5° under a pressure of 766 m.m. Calculated for C5HC1302NH2. Found. N 7.78 8.06 Although the melting point, the crystalline form, and the insolubility of its calcium salt showed that this acid closely resembled the (38 dibrompyromucic acid, it was evidently necessary to establish the posi- tion of the chlorine atoms by means of its oxidation products. Action of Bromine and Water. Hill and Sanger* found that the (38 dibrompyromucic acid was readily. attacked by aqueous bromine in the cold with the formation of monobrommaleyl bromide. The (38 dichlorpyromucic acid is but slowly attacked by aqueous bromine in the cold, and we therefore sus- pended it in five times its weight of water, added at once somewhat more than four atoms of bromine, heated until the oil which was first formed had almost all disappeared, and evaporated the solution at a gentle heat. The crystalline mass thus obtained was readily soluble even in cold water, and very sparingly soluble even in hot chloroform or benzol. The product was dissolved in cold water, filtered, and evaporated nearly to dryness. The crystals which separated were pressed dry with filter paper, washed carefully with hot benzol, and recrystallized from a little hot water. The acid thus prepared crys- tallized in microscopic crystals, which melted at 189-1 90°,t and proved on analysis to contain the percentage of chlorine required by mono- chlorfumaric acid. 0.1288 grm. substance dried over H2S04 gave 0.1227 grm. AgCl. Calculated for C4H,C104. Found. CI 23.59 23.55 The oxidation with bromine and water therefore takes place in accordance with the following equation : CLBLCLO, + 2Br2 + 3H.20 = C4II,C104 + C02 + HC1 + 4 HBr. * These Proceedings, xxi. 165. t Kauder (Journal fur prakt. Cheinie, [2], xxxi. 28) gives the melting point as lfJl°. 348 PROCEEDINGS OP THE AMERICAN ACADEMY Since the (38 dichlorpyromucic is but slowly attacked even by concentrated nitric acid, it was not thought worth while to study the reaction in detail. X Dichlorpyromucic Acid. The formation of the ethyl ether of this acid by the decomposition of ethyl pyromucic tetrachloride has already been described. The ether was recrystallized from hot alcohol, and saponified by alcoholic sodic hydrate. On the addition of hydrochloric acid to the aqueous solution of the sodium salt, a sparingly soluble acid separates, which may easily be purified by recrystallization from hot water. The acid dried over sulphuric acid gave on analysis the following results : — I. 0.2196 grm.substance gave 0.2672 grm. C02 and 0.0237 grm. H20. II. 0.2212 grm. substance gave 0.3492 grm. AgCl. Found. II. c Calculated for C5II2C1203. 33.15 I. 33.18 H 1.10 1.20 CI 39.22 39.03 X dichlorpyromucic acid is readily soluble in ether or alcohol, and but sparingly soluble in cold water. In hot water it is freely soluble, and crystallizes as the solution cools in long needles which melt at 197-198°. The acid readily sublimes unchanged below its melting point. Sodium amalgam slowly reduces it to pyromucic acid melting at 129-130°. The solubility of the acid in water at 19°. 5 was determined in the usual manner. A solution of the acid saturated at 19°. 5 was boiled with baric carbonate, and the barium dissolved determined by precipitation with sulphuric acid. I. 38.2670 grm. solution saturated at 19°.5 gave 0.0322 grm. BaS04. II. 37.5125 grm. solution saturated at 19°. 5 gave 0.0301 grm. BaS04. The solution saturated at 19°. 5 therefore contained the following percentages of acid : — i. n. 0.13 0.12 Baric x Dichlorpyromucate, Ba(C5HCl203)2 . 4 H20. — The barium salt may most readily be prepared by boiling the acid with baric car- bonate. The salt is quite readily soluble in cold water, more soluble in hot water, and crystallizes in columnar aggregations of prisms which OF ARTS AND SCIENCES. 349 contain four molecules of water. The crystallized salt is stable in the air, effloresces over sulphuric acid, and loses all its water at 100°. I. 1.0471 grm. air-dried salt lost at 100° 0.1285 grra. H20. II. 0.5464 grm. air-dried salt gave 0.2235 grm. BaS04. Calculated for Found. Ba(C5HCl203)2 . 4 H20. I. II. H20 12.66 12.27 Ba 24.07 24.05 0.4495 grm. salt dried at 100° gave 0.2091 grm. BaS04. Calculated for Ba(C5IICl203)2. Found. Ba 27.56 27.35 The solubility of the salt in water at 19°.5 was determined in the usual manner. I. 11.1910 grm. solution saturated at 19°.5 gave 0.0820 grm. BaS04. II. 8.6544 grm. solution saturated at 19°. 5 gave 0.0644 grm. BaS04. According to these determinations, the solution saturated at 20° contained the following percentages of anhydrous salt: — I. ii. 1.56 1.59 Calcic x Dichlorpyromucate, Ca(C5HCl203)2. 4 H20. — The calcium salt was prepared by boiling the acid with calcic carbonate. The fil- tered solution was then concentrated on the water bath to a small vol- ume, and the salt which separated was filtered out and washed with a little water. Since the salt appeared to be about as soluble in cold water as in hot, it was dissolved in water and the solution concen- trated in vacuo over sulphuric acid. The salt which separated was then pressed dry with filter paper. It is quite readily soluble in water, and crystallizes in prisms vhich contain four molecules of water. The crystallized salt is permanent in the air, effloresces slowly over sul- phuric acid, and loses all its water at 117°. I. 0.9075 grm. air-dried salt lost at 117° 0.1380 grm. H20. II. 0.6080 grm. air-dried salt gave 0.1746 grm. CaSOv Calculated for Found. Ca(C5HClo03), . 4 HjO. I. n. H20 15.25 15.21 Ca 8.48 8.44 0.3377 grm. salt dried at 117° gave 0.1152 grm. CaSOv Calculated for Ca (C5HCU03),. Found. Ca 10.00 10.02 350 PROCEEDINGS OF THE AMERICAN ACADEMY The solubility of the salt in water at 19°. 5 was determined in the usual manuer. The calcium was precipitated as oxalate and iguited with sulphuric acid. I. 6.5743 grm. solution saturated at 19°.5 gave 0.1522 grm. CaS04. II. 7.2115 grm. solution saturated at 19*°. 5 gave 0.1689 grm. CaS04. The solution saturated at 19°. 5 therefore contained the following percentages of anhydrous salt: i. ii. 6.81 6.89 Ethyl x Dichlorpyromucate, C5HC1203C2H.. — The process by which the ethyl ether was obtained has already been described. It is readily soluble in hot alcohol, sparingly soluble in cold alcohol, and crystallizes in clustered prisms with rectangular truncations which melt at 72-73°. A sample of the ether melting at 72-73° was distilled under a pressure of 16 mm. and boiled constant at 12 2°. 5, temperature of bath 170-175°. For analysis the ether was dried over sulphuric acid. I. 0.2034 grm. substance gave 0.2790 grm. AgCl. II. 0.2302 grm. substance gave 0.3160 grm. AgCl. Calculated for Found. C6HC1203C2H6. I. n. CI 33.98 33.91 33.94 In order to determine the constitution of this dichlorpyromucic acid we studied its oxidation products with aqueous bromine. Action of Bromine and Water. As it was desirable to compare the oxidation product obtained from this acid with that obtained from the fih dichlorpyromucic acid under the same conditions, the acid was suspended in five times its weight of water, somewhat more than four atoms of bromine added as rapidly as possible, and the solution boiled until the oil which was at first formed had nearly disappeared. The filtered solution was evaporated to dry- ness at a gentle heat, the crystalline residue dissolved in a little cold water, filtered, and again evaporated nearly to dryness. The acid which separated was readily soluble even in cold water, almost insolu- ble in hot chloroform or benzol. It was therefore pressed dry with filter paper and carefully extracted with hot benzol. The acid as thus prepared crystallized in microscopic crystals which melted at 188-189°, and moreover gave on analysis the percentage of chlorine required by monochlorfumaric acid.* * KauJer, loc. cit. OF ARTS AND SCIENCES. 351 0.1441 grm. substance dried over H2S04 gave 0.1377 grm. AgCl. Calculated for C4H3C104. Found. CI 23.59 23.62 The x dichlorpyromucic acid, like the (38 dichlorpyromucic acid, therefore gives with aqueous bromine as tbe chief product chlorfumaric acid according to the equation C5H2C1203 + 2 Br2 + 3 H20 = C4H3C104 + C02 + HC1 + 4 HBr. Since the oxidation with bromine had shown with sufficient precision that one of the chlorine atoms of the x dichlorpyromucic acid occupied the 8 position, we thought it unnecessary for our purposes to study also the action of nitric acid. Action of Fuming Sulphuric Acid. The two isomeric dibrompyromucic acids had shown marked differ- ences in their behavior toward fuming sulphuric acid.* While the /Sy acid had rapidly been converted into the corresponding sulphonic acid, brommaleic acid in nearly theoretical quantity had been formed from the (38 dibrompyromucic acid, and no trace of a sulphonic acid could be detected. Preliminary experiments proved that the /?y and /8S dichlorpyromucic acids showed a similar difference in their behavior toward fuming sulphuric acid. While the formation of chlormaleic acid in the latter case could not definitely be pi'oved, certainly no sulphonic had been formed, and it seemed to us of interest to study also the behavior of the third isomeric dichlorpyromucic acid under the same conditions, x dichlorpyromucic acid dissolves readily in fuming sulphuric acid, and if care be taken to prevent any marked elevation of temperature no very essential decomposition ensues, although a slight effervescence is noticeable. After the solution of the acid in four times its weight of fuming sulphuric acid had stood for thirty-six hours, it was poured into a large amount of cold water, the solution cooled, and thoroughly extracted with ether. The ethereal extract left on evaporation a small quantity of a colorless oil which reduced silver oxide, and whose vapor vigorously attacked the eyes and nose. The amount of oil thus obtained was wholly insufficient for further study. On standing, it deposited a few clustered needles, which probably were unaltered acid, although they may possibly hive been the decomposition product subsequently described. From the aqueous solution the barium salt was prepared in the usual way, and, * These Proceedings, xxiii. 218. 352 PROCEEDINGS OF THE AMERICAN ACADEMY since the properties of the neutral salt were unfavorable to purifica- tion, it was converted into the acid salt, and this recrystallized from hot water. The acid salt was readily soluble in hot water, more spar- ingly soluble in cold water and crystallized in triclinic (?) prisms which effloresced on exposure to the air. It gave an excellent qualitative reaction for sulphur, and when dried over sulphuric acid* gave the percentage of barium required by the formula Ba(C.HCl2SOc)2. 0.3886 grm. of the salt dried over sulphuric acid gave 0.1338 grm. BaS04. Calculated for Ba(C5HCl2S06)2. Found. Ba 20.84 20.24 Baric x Dichlorsulphopyromucate, BaC5Cl2S06 . 2 H20. — From the acid barium salt we prepared the neutral salt by neutralizing its aque- ous solution with baric carbonate. Since the hot saturated solution deposited little or nothing on cooling, it was evaporated in vacuo over sulphuric acid. The salt then crystallized in sheaves of prisms which appeared to be triclinic. It was permanent in the air, effloresced over 6ulphuric acid, and lost its water completely at 160°. 1.4159 grm. of the air-dried salt lost at 160° 0.1277 grm. H20. Calculated for BaC5Cl2S06 . 2 H20. Found. H20 8.33 9.02 0.5296 grm. of the salt dried at 160° gave 0.3126 grm. BaS04. Calculated for BaC5Cl2S06. Found. Ba 34.59 34.69 The formation of a dichlorsulphopyromucic acid by the action of fuming sulphuric acid upon the x dichlorpyromucic acid is thus suffi- ciently established. The bromsulphop3Tomucic acids are so readily reduced in alkaline solution that we hoped to be able to prepare from this dichlorsulphopyromucic acid the corresponding sulphopyromucic acid, and thus establish the position of the two chlorine atoms. We soon found, however, that the chlorine was held with unusual persist- ence, and with the material at our disposal we have as yet been unable to reach decisive results. * The single determination of the water of crystallization was unfortunately defective. It gave 13.34 per cent of water in the salt dried by short exposure to the air, while a salt crystallizing with 2£ molecules of water should contain 13.70 per cent. OF ARTS AND SCIENCES. 353 Decomposition by Hydrochloric Acid. If the x dichlorpyromucic acid is heated with water in a sealed tube to 170°, no change is effected, but a reaction which we had in no way anticipated takes place if it is heated upon the water bath in an open flask with concentrated hydrochloric acid. Carbonic acid is evolved, and in a short time the acid is completely decomposed with the forma- tion of a neutral body which volatilizes when the solution is boiled, and which can be extracted, although with difficulty, from the distil- late, or from the original solution with ether. The ethereal solution left on evaporation a white crystalline solid which was sparingly soluble in water, readily soluble in cold chloroform or benzol, and but sparingly soluble in ligroin. When recrystallized from ligroin it formed long slender lustrous prisms, which melted at 52-53°, and sublimed rapidly at ordinary temperatures. It reduced argentic oxide on warming, and dissolved in aqueous alkalies, forming a yellow solution. The physical properties and the behavior of this substance at once recalled to our minds the crystalline body melting at 77° which Hill and Sanger* had obtained in small quantity from the by-products of the decompo- sition of pyromucic tetrabromide by alcoholic sodic hydrate. The formula of this body had been shown to be C4H3Br02 and an analysis of the new substance left no doubt of its similar composition. 0.1045 grm. substance gave 0.1261 grm. AgCl. Calculated for C4H3C102. Found. CI 29.95 29.84 This interesting body is probably formed according to the reaction C5H2C1203 + H20 = C4H3C102 + C02 + HC1. And since we found little difficulty in obtaining 40 per cent of the yield which this equation demands, it will be possible to study it more in detail. Unfortunately, it was discovered so late in our work as to make it impossible to present the results of such a study in this paper. While it would be easy for us to venture a conjecture as to its struc- ture, we prefer to await the results of a future investigation. Trichlorpyromucic Acid. For the preparation of the trichlorpyromucic acid it was evidently most convenient to decompose with alkalies the tetrachloride of the & chlorpyromucic acid. It did not seem necessary, however, to pre- * These Troceerfings, xxi. 158. vol. xxiv. (n. s. xvi.) 23 354 PROCEEDINGS OF THE AMERICAN ACADEMY pare this tetrachloride in a pure condition, and indeed we first obtained the trichlorpyromucic acid from one of the earlier preparations of the ethyl pyromucic tetrachloride in which an unusually great spontaneous elevation of temperature had taken place through the rapid absorption of chlorine. For its preparation we heated the ethyl pyroinucate to 145°, and passed in chlorine at this temperature until the gain in weight showed that one atom of hydrogen had been replaced by chlorine. We then allowed the temperature to fall to about 120°. and continued the chlorination to saturation. The total train iu weight then corresponded approximately to that required by the formation of the tetrachloride of the ethyl chlorpyromucate. On decomposing this product as usual with a cold concentrated alcoholic solution of sodic hydrate, the alcoholic solution filtered from the insoluble sodium salts contained, as in the previous cases, small quan- tities of liquid furfuran derivatives, but the amount was so minute that no separate study of them was made. The sodium salts dissolved iu hot water gave with hydrochloric acid an impure trichlorpyromucic acid as a more or less colored oil, which solidified as the solution cooled. For the purification of the acid we have found it convenient to take advantage of the slight solubility of the ammonium salt in cold water. The crude acid was suspended in about thirty times its weight of water, ammonic hydrate added in excess, and the hot solution treated with bone-black. The filtered solution deposits on cooling the greater part of the trichlorpyromucic acid as the ammonium salt from which the pure acid can readily be obtained. The small amount of trichlorpy- romucic acid remaining in the ammoniacal solution may be recovered, although at the expense of considerable trouble, by precipitation with calcic chloride and repeated recrystallization from water and dilute alcohol of the acid obtained from the insoluble calcium salt. The yield of pure trichlorpyromucic acid was far from satisfactory, as we could obtain only 30 per cent of the weight of the ethyl pyromu- cate taken, but 15 per cent of the theoretical amount. For analysis the acid was dried over sulphuric acid. I. 0.3214 grm. substance gave 0.3248 grm.C02 and 0.021 1 grm. H20. II. 0.2107 grm. substance gave 0.4192 grm. AgCl. III. 0.2135 grm. substance gave 0.4255 grm. AgCl. i in. 49.27 c Calculated for CfiIICl303. 27.85 i. 27.56 Found II. II 0.46 0.73 CI 49.43 49.U OP ARTS AND SCIENCES. 355 Trichlorpyromucic acid is readily soluble in alcohol or ether, quite readily soluble in boiling benzol, and but sparingly soluble in cold benzol. Hot water dissolves it but sparingly, and as the solution cools most of the acid is deposited in microscopic needles which melt at 172-173°. This melting point was so much below that which we had been led to expect from analogy to the known acid containing bromine that we felt some doubt of its correctness, more especially since the crude acid was so far from pure. A sample of the acid melting at 172-173° was therefore recrystallized twice from water and then three times from benzol without perceptibly changing the melting point. The acid was then converted into the calcium salt, and this separated by crystallization into three successive fractions. The acid from these three fractions melted simultaneously and sharply at 172-173°. Finally, the ethyl ether was made, and the acid prepared from the repeatedly recrystallized pure ether melted at the same point. The solubility of the acid in water at 19°. 5 was determined by boil- ing with baric carbonate a weighed quantity of a solution of the acid saturated at that temperature, and determining the barium dissolved as sulphate. I. 49.1742 grm. solution saturated at 19°.5 gave 0.0344 grm. BaS04. II. 47.0228 grm. solution saturated at 19°.5 gave 0.0331 grm. BaSo4. The solution saturated at 19.5° therefore contained the following percentages of acid : i. ii. 0.13 0.13 Baric Trichlorpyromucate, Ba(C5Cl.,03)2 . 4 H20. — The barium salt was prepared by precipitating a dilute solution of the ammonium salt with baric chloride, and recrystallizing the sparingly soluble salt thus thrown down from hot water. The salt proved to be but sparingly soluble even in hot water, and still less soluble in cold water. It sep- arates from a hot concentrated solution in needles which apparently contain four molecules of water. The salt is permanent in the air, but loses three molecules of its crystal water over sulphuric acid. When dried at 120°, it still retains a half-molecule of water which cannot be expelled without essential decomposition. I. 0.6847 grm. air-dried salt gave 0.2511 grm. BaS04. II. 0.6205 grm. air-dried salt gave 0.2273 grm. BaS04. III. 0.5672 grm. air-dried salt gave 0.2076 grm. BaS< \. IV. 1.3625 grm. air-dried salt lost over II2S04 0.1148 grm. H.,0 and at 120° 0.1338 grm. II20. Found. I. II. iii. 23.86 23.72 23.84 356 PROCEEDINGS OP THE AMERICAN ACADEMY V. 1.1645 grm. air-dried salt lost over H2S04 0.1003 grm. H20 and at 100° 0.1124 grm. H20. VI. 1.3000 grm. air-dried salt lost over H2S04 0.1124 grm. H20 and at 100° 0.1256 grm. H20. Calculated for Found. BaJCjCLjOa).; . 4 H,0. I. II. III. IV. V. VI. Ba 21.47 21.56 21.54 21.52 3H20 8.46 8.43 8.61 8.65 3£H20 9.87 9.83 9.65 9.66 I. 0.7484 grm. substance dried at 120° gave 0.3038 grm. BaS04. IT. 0.6247 grm. substance dried at 100° gave 0.2521 grm. BaS04. III. 0.6497 grm. substance dried at 100° gave 0.2634 grm. BaS04. Calculated for i Ba(C5CI303)2.^n20. Ba 23.83 The solubility of the salt in water at 19°. 5 was determined in the usual way. I. 41.4499 grm. solution saturated at 19°.5 gave 0.0470 grm. BaS04. II. 44.9822 grm. solution saturated at 19°.5 gave 0.0500 grm. BaS04. The solution saturated at 19°. 5 therefore contained the following percentages of anhydrous salt : — i. ii. 0.27 0.27 Calcic Trichlorpyromucate, Ca(C5Cl303)2 . 4 H.,0. — The calcium salt was prepared by precipitating a dilute solution of the ammonium salt with calcic chloride. The precipitated salt was then crystallized from hot water, and proved to be sparingly soluble in hot water, still less soluble in cold water, and separated from a hot solution in irreg- ular aggregations of small leafy plates. The salt is permanent in the air, effloresces over sulphuric acid, and loses all its water at 110°. I. 1.3008 grm. air-dried salt lost at 110° 0.1697 grm. H20. II. 1.8389 grm. air-dried salt lost at 110° 0.2417 grm. H20. Calculated for Found. (C6Cl303),Ca . 4 11,0. I. II. H20 13.30 13.05 13.14 I. 0.6399 grm. salt dried at 110° gave 0.1855 grm. CaS04. II. 0.6974 grm. salt dried at 110° gave 0.2019 grm. CaS04. Calculated for Found. Ca(CBCl303)2. I. n. Ca 8.53 8.53 8.51 OF ARTS AND SCIENCES. S57 The solubility of the salt in water at 19°. 5 was determined in the usual manner. The calcium was precipitated as oxalate, and the oxalate ignited with sulphuric acid. I. 18.1457 grm. solution saturated at 19°.5 gave 0.0342 grm. CaS04. II. 14.6806 grm. solution saturated at 19°. 5 gave 0.0265 grm. CaS04. The solution saturated at 19°. 5 therefore contained the following percentages of anhydrous salt : — i. ii. 0.65 0.62 Potassic Trichlorpyromucate, KC5C1303. — The potassium salt was prepared by boiling the acid with a slight excess of potassic carbonate. The solution was then concentrated until the salt began to separate, and on cooling it solidified to a mass of crystals, which were filtered off on the pump and pressed dry with filter paper. The salt is readily soluble even in cold water, and separates from a hot concentrated solution in sheaves of fine needles, which lose nothing in weight when heated to 120°. Analyses of the salt dried at this temperature proved it to be anhydrous. I. 0.5338 grm. salt dried at 120° gave 0.1851 grm. K2S04. II. 4425 grm. salt dried at 120° gave 0.1532 grm. K2S04. Calculated for Found. KC5C1303. I. II. K 15.42 15.57 15.54 Argentic Trichlorpyromucate, AgC5Cl,03. — The silver salt may best be prepared by precipitating a hot solution of the calcium salt with argentic nitrate. For analysis the precipitated salt was well washed, and then recrystallized from hot water. It is sparingly solu- ble even in hot water, less soluble in cold water, and crystallizes from a hot concentrated solution in moss-like aggregations of fine needles. The aii-dried salt gave on analysis much too low a percentage of silver, and although the sample analyzed was free from calcium salt and free acid, it failed to give perfectly satisfactory results even when dried in vacuo over sulphuric acid or at 100°. I. 0.5142 grm. salt dried in vacuo over H2S04 gave 0.2254 grm. AgCl. II. 0.4545 grm. salt dried at 100° gave 0.1998 grm. AgCl. Calculated for Found. C5Cl,0,Ag. i. a Ag 33.48 33.00 33.10 358 PROCEEDINGS OP THE AMERICAN ACADEMY Ethyl Trichlorpyromucate, C5C1803C2H5. — The ethyl ether was prepared in the usual manner, by warming an alcoholic solution of the acid with concentrated sulphuric acid. 5 parts of the acid, 10 parts of absolute alcohol, and 5 parts of concentrated sulphuric acid (Sp. Gr. 1.84) were heated together for three hours at 100°. The ether was then precipitated with water, washed with warm dilute sodic car- bonate, and finally with water. The ether is readily soluble in hot alcohol, more sparingly in cold alcohol, and crystallizes in flat prisms which melt at 62-63°. I. 0.2142 grm. substance dried over H2S04 gave 0.3793 grm. AgCl. II. 0.2536 grm. substance dried over H2S04 gave 0.4476 grm. AgCl. Calculated for Found. C6C1303C2H0. I. ii. 43.74 43.77 43.64 CI Trichlorpyromucamide, C5Cla02NH2. — Concentrated aqueous am- monia attacks the trichlorpyromucic ether but slightly at ordinary tem- peratures. Even after three hours' heating in a sealed tube at 100° most of the ether was found to be unaltered, and we were obliged to prepare the amide from the acid chloride by the action of solid am- nionic carbonate. The amide is but sparingly soluble even in hot water and crystallizes in long slender needles, which melt at 160-161°. 0.3804 grm. substance dried over H2S04 gave 23.2 c.c. moist N at 21° under a pressure of 765 mm. Calculated for C6C1302NH2. Found. N 6.53 6.95 Although there could be no doubt as to the constitution of the trichlorpyromucic acid it seemed better for the sake of completeness to study its behavior with oxidizing agents. Action of Bromine and Water. Trichlorpyromucic acid was suspended in ten times its weight of cold water, and a little more than one molecule of bromine was added. Carbonic dioxide was evolved and the color of the bromine rapidly disappeared. When the reaction had been completed, a white insolu- ble substance remained, which was removed by filtration and washed with a dilute solution of sodic carbonate. The alkaline solution gave on acidification a copious precipitate of unaltered trichlorpyromucic acid, whose identity was established by the melting point 172-173°. The substance which remained undissolved by the alkaline solution OP ARTS AND SCIENCES. 359 had the characteristic odor of the tetrabromfurfuran, and crystallized from hot alcohol in irregular plates, which melted at 75-76°. Analy- sis showed this substance to be a trichlorbromfurfuran. I. 0.1749 grm. substance dried over H2S04 gave 0.4269 grm. AgCl and AorBr. II. 0.1411 grm. substance dried over H2S04 gave 0.3447 grm. AgCl and AgBr. Calculated for Found. C4Cl3Br0. I. ii. Cl3 + Br 74.45 73.60 73.67 The strongly acid filtrate from the trichlorbromfurfuran and unal- tered trichlorpyromucic acid yielded on extraction with ether a crys- talline acid which was readily soluble in water. The amount of this acid was too small for analysis, but it was easily identified as dichlor- maleic acid by the melting point of its anhydride, 119-120°.* The reaction had therefore taken place in accordance with the following equations : C5HC1303 4- Br2 = C4CLBrO + C02 + HBr. C5HC1,03 + 2 Br2 + 3 H20 = C4H2C1204 + C02 + HC1 + 4 HBr. Action of Nitric Acid. Trichlorpyromucic acid is but slowly attacked by nitric acid, and prolonged heating with moderately strong nitric acid is needed for complete oxidation. Even after heating the acid for six hours with six times its weight of nitric acid (Sp. Gr. 1.42) diluted with an equal weight of water, a portion of the trichlorpyromucic acid escaped oxi- dation. Carbonic dioxide was slowly given off, and a small quantity of an insoluble oil was formed, which had a peculiar penetrating odor not unlike that of substituted furfuran derivatives. Its quantity was too small to admit of its identification. In solution we were able to find nothing but dichlormaleic acid, which we purified through the barium salt and identified by the melting point of its anhydride and by analysis. 0.1997 grm. substance dried over H2S04 gave 0.3086 grm. AgCl. Calculated for C4H2C1204- Found. CI 38.38 38.20 The reaction had therefore taken place in accordance with the fol- lowing equation : C5IIC130; + 2 O + H20 = C4H2CL04 + CO, + IIC1. * Ciamiciau and Silber, he. cit. 360 PROCEEDINGS OP THE AMERICAN ACADEMY We have also prepared several other trisubstituted pyromucic acids, which may conveniently be described here. /3y-DlCHLOR-S-BROJIPYROMDCIC ACID. Hill and Sanger * found that fiy dibrompyromucic acid was easily converted into tribrompyromucic acid by the action of bromine at ordinary temperatures. If /3y dichlorpyromucic acid is exposed to the vapors of bromine at ordinary temperatures, bromine is rapidly absorbed, hydrobromic acid is evolved, and the gain in weight approaches that required by the dis- placement of hydrogen by bromine. The product was treated with small quantities of boiling water to remove unaltered dichlorpyromucic acid, and then recrystallized from dilute alcohol, and finally from water. The acid is readily soluble in alcohol or ether, dissolves freely in boil- ing benzol, more sparingly in cold benzol. Even in boiling water it is very sparingly soluble. It crystallizes in short clustered prisms, which melt at 185-186°. 0.3189 grm. substance dried over II.2S04 gave 0.5817 grm. AgCl and AgBr. Calculated for C0HCl2Br03. Found. Cl2 + Br 58.08 57.99 /?y-DlBROM-S-CHLORPYROMUCIC ACID. This acid we made by treating the ethyl fiy dibrompyromucate with chlorine and decomposing the product with alcoholic sodic hy- drate. On acidifying the aqueous solution of the sodium salts thus obtained, a crystalline acid was precipitated, which after one recrystal- lization from dilute alcohol melted at 192-193°. After recrystalliza- tion from benzol the melting point rose to 193-194°. The acid was readily soluble in alcohol, ether, or hot benzol ; sparingly soluble in cold benzol, or even in boiling water. 0.2315 grm. substance dried over H2S04 gave 0.39G0 grm. AgCl and AgBr. Calculated for C5UClBr,03. Found. CI + Br2 64.19 64.37 We have attempted to prepare these acids also by the decomposition with alcoholic sodic hydrate of products formed by the addition of * These Proceedings, xxi. 172. OF ARTS AND SCIENCES. 861 bromine to 8 chlorpyromucic acid and of chlorine to ethyl 8 brompyro- mucate. Although we readily prepared in this way trisubstituted acids, the products in neither case were homogeneous, tribrom- or trichlorpyromucic acids being formed together with the acid containing both halogens. /3y-DiCHLOR-8-NiTROPYito:\iucic Acid. Hill and Palmer* have shown that /3y dibrompyromucic acid is easily converted into a sulphonic acid by means of sulphuric acid, and that the sulpho group in this acid may readily be replaced by the nitro group. /3y dichlorpyromucic acid was dissolved in fuming sulphuric acid, and the barium salt of the sulphonic acid isolated in the usual way. Since a more complete study of the salt did not fall within the plan of our work, we precipitated the barium exactly with sulphuric acid, and evaporated the dilute solution of the acid first at 100° and afterwards in vacuo over sulphuric acid. The crystalline somewhat deliquescent acid thus obtained was dissolved in several times its weight of fuming nitric acid, to which half its volume of concentrated sulphuric acid had been added. After the action was finished, the nitric acid was partially expelled, the residue diluted with water, and extracted with ether. The ether, was then shaken with a dilute solu- tion of soclic carbonate, and the acid precipitated from this alkaline solution by the addition of hydrochloric acid. The ethereal solution proved to contain no substance which invited further investigation. The /3y-dichlor-S-nitropyromucic acid is readily soluble in alcohol, ether, or hot benzol. Hot water dissolves it freely, and on cooling the greater part of the acid is deposited in flattened leafy prisms which melt at 189-190°. 0.2168 grm. substance dried over H2S04 gave 0.2756 grm. Ag. CI. Calculated for C6HC12N06. Found. CI 31.42 31.42 "We have as yet made no further study of this acid. Theoretical Considerations. The acids melting at 168-169° and 155-156°, which in the pre- ceding pages we have called the (3y and /3S dichlorpyromucic acids, are without doubt identical in structure with the two dibrompyromucic acids described by Hill and Sanger. | Their physical properties and * Tliese Proceedings, xxiii. 201, 205. t These Proceedings, xxi. 137. 362 PROCEEDINGS OP THE AMERICAN ACADEMY the solubility of their salts show their close relationship to these bro- mine derivatives, while the products formed from them by oxidation conclusively jjrove that they are structurally isomeric, and that the chlorine atoms occupy the same relative position that the bromine atoms hold in the dibrompyromucic acids. On reduction these two acids both yield the same chlorpyromucic acid, which in its turn closely resembles the j3 brompyromucic acid in its jmysical properties, although its melting point, 145-146°, is comparatively high. It is to be noted, however, that the f3y dichlorpyromucic acid alone is formed by the action of alkalies upon the ethyl pyromucic tetrachloride, while the two isomeric dibrompyromucic acids are simultaneously formed under sim- ilar conditions. This simultaneous formation of the two structurally isomeric acids from pyromucic tetrabromide to which the formula Br Br H--C-C- COOH \ 0 / HC - C - H Br Br may be assigned led Hill and Sanger * to the conclusion that these acids must have their bromine atoms in the /?y and ft8 positions respectively, and that pyromucic acid itself probably had the formula HC = C - COOH O / HC = CH. The structure of the fSy and /?S dichlorpyromucic acids seems to us to be thus sufficiently established. As to the third isomeric form, which for the present we have called the x dichlorpyromucic acid, since it gives chlorfumaric acid by oxida- tion, it is evident that it must either have its chlorine atoms in the y and 8 position, or that it must be a geometrically isomeric form of the (38 acid. Unfortunately, we have been able to obtain as yet no evidence which conclusively proves either view to be correct. A dichlorpyromucic acid having its chlorine atoms in the y and 8 posi- tions could not well be formed from ethyl pyromucic tetrachloride by the simple loss of hydrochloric acid. Tonniesf had shown that 8 brom- * These Proceedings, xxi. 182. \ t Berichte de deutsch. chem. Gesellsch. OP ARTS AND SCIENCES. 863 pyroinucic acid could be formed by tbe action of heat upon pyromucic tetrabrornide, when bromine must be eliminated as well as hydrobromic acid. Since we had noticed that hydrochloric acid invariably was evolved in the preparation of ethyl pyromucic tetrachloride, it seemed to us not improbable that the ^ dichlorpyromucic acid was in fact the yd acid which had been formed in a similar way from the tetrachloride of the 8 chlorpyromucic ether necessarily contained in the crude product. CI CI HC - C - COOH \ 0 / Cl( : cci I I Cl We found, however, that no x dichlorpyromucic acid was formed on heating ethyl 8 chlorpyromucic tetrachloride, and that our product in this case contained the /?8 acid alone, so that the molecule of chlorine, which had been eliminated in the reaction, had taken its chlorine atoms from the y and 8 positions. We hoped also to get further evidence as to the structure of the ^ dichlorpyromucic acid by reducing it to a chlorpyromucic acid, or by substituting the chlorine of the x dichlorsulphopyromucic acid by hydrogen; but in neither case have we yet succeeded in obtaining well characterized products. While it seems to us probable that the % dichlor pyromucic acid is geometrically isomeric with the /38 acid, we have as yet been unable to convert one acid into the other. Both acids volatilize unchanged when heated, and the ordinary reagents which usually effect conver- sion in such cases have failed to bring abont any perceptible isomeri- zation. While lack of material has to a great degree limited our work with the x acid, we have studied the behavior of the fi8 acid under a variety of conditions with purely negative results. If tlie two acids are in fact geometrically isomeric, the simultaneous appearance of both forms in the distillation of ethyl pyromucic tetrachloride with the escape of large quantities of hydrochloric acid shows that the conver- sion of one acid into the other is effected with difficulty, while the formation of the (3d acid alone from the ethyl 8 chlorpyromucic tetra- chloride under similar conditions is especially worthy of note. Since pyromucic acid apparently contained two pairs of carbon atoms doubly 364 • PROCEEDINGS OF THE AMERICAN ACADEMY tied, the existence of geometrically isomeric forms of its derivatives seemed at the outset more thau prohable, and during the progress of the investigations which for many years have been carried on in this laboratory careful search had been made for such bodies, but hitherto only the two isomeric dibromfurfuran tetrabromides of Hill and Harts- horn * had been discovered. Since the discovery of the ^ dichlorpyro- mucic acid, which we made toward the close of our work, we have attempted to prepare the corresponding bromine derivative, but as yet without success. The isolation of the body C4H3Br02, which Hill and Sanger f found among the products of the decomposition of pyromucic tetrabromide by alkalies, certainly is an indication of the previous existence of such an acid, although it is by no means clear in what stage of the process the decomposition of the acid was effected, nor how the decomposition product itself escaped further alteration. Any detailed consideration of the geometrical structure of pyromucic acid we' feel obliged to postpone until more facts bearing upon the question are at our disposal. II. — ON CERTAIN DERIVATIVES OF FURFUR- ACRYLIC ACID. By H. B. Gibson and C. F. Kahnweiler. < Presented May 28, 1889. The preparation of furfuracrylic acid was described by v. Baeyer t 1877. At that time, however, the investigation of the acid was pushed in but one direction, and the successive steps by which it could be converted into a pimelic acid were alone described in detail. It seemed that a further study of the acid in other directions also could hardly fail to yield interesting results. The ready decomposition of furfuracrylic acid by mineral acids compelled us to relinquish the line of work we originally had pro- posed to follow, and we consequently began an investigation into the nature of this decomposition. The study of the action of hydrochloric acid upon an alcoholic solution of furfuracrylic acid was just beginning * Berichte der deutsch. chem. Gesellsch., xviii. 450. t These Proceedings, xxi. 158. t Ber. d. deutsch. chem. Gesellsch., x. 355. OF ARTS AND SCIENCES. 365 to yield us results when the paper o'f Markwald * upon the same sub- ject reached us, and we were therefore obliged to abandon our work in this direction, and turned our attention to the products formed by the action of bromine, which promised to repay investigation. We felt ourselves quite at liberty to continue our study of furfuracrylic acid in this direction, since Markwald had declared himself unable to obtaiu well defined crystalline products in this way. Furfuracrylic Acid. In the preparation of furfuracrylic acid we have found it to our advantage to modify slightly the proportions given by v. Baeyer, and in this respect our experience agrees more closely with that of Mark- wald. We have heated 2 parts of furfurol with 3 parts of fused sodic acetate and 3 parts of acetic anhydride with reverse cooler at 160-170° for about ten hours, extracted the acid with a dilute solution of sodic carbonate, precipitated with hydrochloric acid, and recrystallized the product thus obtained from boiling water. Although the yield varied somewhat in successive preparations, we frequently obtained an amount equal to the weight of furfurol employed. The melting point of the pure acid we found to be 140°, in agreement with the observations of Jaffe and Cohn,f instead of 136° as given by v. Baeyer. From the acid we made the methyl ether and the amide, which we may describe a little more in detail, since no description of them has yet been published. Methyl Furfuracrylate, C.H.CX . CH3. — By precipitating with ar- gentic nitrate a solution of ammonic furfuracrylate the silver salt was obtained as a heavy curdy precipitate. This was carefully dried and treated with an excess of methyl iodide. When the decomposition was complete the product of the reaction was extracted with ether, and purified by distillation under diminished pressure. Under a pressure of 15 mm. the methyl furfuracrylate distils unchanged at 112°, and the distillate solidifies in beautiful rhombic crystals which melt at 27°. Under a pressure of 774 mm. we found that the ether distilled without apparent decomposition at 227-228°. It possessed an agreeable characteristic odor, and dissolved readily in alcohol, ether, ligroin, or benzol. An analysis gave the following results : — 0.2224 grm. substance gave 0.5157 grm. C02 and 0.1084 grm. H20. Calculated for C8H9Oa. Found. C 63.17 63.23 H 5.26 5.42 * Ber. d. deutsch. chem. Gesellsch., xx. 2811. t Ibid., xx. 2315. 366 PROCEEDINGS OP THE AMERICAN ACADEMY Furfur acrylamide, C-H.02. NH2. — Concentrated aqueous amnionic hydrate acted but slowly upon methyl furfuracrylate in the cold, but at 100° in sealed tube the decomposition was readily effected. The amide was sparingly soluble in cold water, more readily in hot water, and crystallized in pearly scales which melted at 168-1G90. I. 0.4076 ffrm. substance gave 35.5 c.c. moist nitrogen at 21°. 4 and under a pressure of 766 mm. II. 0.4590 grm. substance gave 41.9 c.c. moist nitrogen at 21°. 7 and under a pressure of 767 mm. Calculated for Found. C7II7X0,. I. II. N 10.22 9.98 10.45 Action of Bromine. It had already been observed by v. Baeyer that furfuracrylic acid was readily attacked by aqueous bromine, but he had made no careful study of the products formed. Since the product formed in this way was un- inviting, and the reaction undoubtedly complicated, it seemed advisable to study instead the action of dry bromine, which might yield well char- acterized addition products. We soon found, however, that with dry bromine even in the cold substitution was readily effected, so that the simplest well defined product contained three atoms of bromine. Sub- sequent study showed that this product was a saturated compound iu which one atom of bromine had taken its place in the furfuran ring. Bromfurfurdibrompropionic Acid, C7H.Br303. — If furfuracrylic acid is suspended in ten times its weight of carbonic disulphide and two molecules of dry bromine added, a clear deep red solution is at once obtained, from which hydrobromic acid is soon evolved in quantity. Although the reaction progresses steadily at ordinary temperatures, it may be greatly hastened by heat, and we usually have heated the mixture upon the water bath soon after the addition of the bromine. When the evolution of the hydrobromic acid slackens, and a crystalline substance has separated in quantity, the solution is well cooled, filtered, and the crystalline solid well washed with cold carbonic disulphide. The substance then gives on analysis percentages which closely agree with those required by the formula C7H5Br303 ; but it may still further be recrystallized from hot benzol or carbonic disulphide. I. 0.2080 grm. substance gave 0.3117 grm. AgBr. II. 0.3798 grm. of substance recrystallized from carbonic disulphide gave 0.3099 grm. C02 and 0.0502 grm. H20. OP ARTS AND SCIENCES. 867 III. 0.2005 grm. substance recrystallized from benzol gave 0.2998 grm. AgBr. IV. 0.2003 grm. substance recrystallized from benzol gave 0.2993 grm. AgBr. Calculated for C7H5Br303. c 22.28 H 1.33 Br 63.66 Found II. III. IV. 2.26 1.47 63.65 63.60 63.78 Bromfurfurdibrompropionic acid crystallizes in small flat oblique prisms, which are sparingly soluble iu cold benzol or carbonic disul- phide, more readily in hot. It is readily soluble in alcohol or ether, insoluble in water, although slowly decomposed by it. On heating, the acid is gradually decomposed, with the evolution of hydrobromic acid and slight carbonization. As might be expected, we found it im- possible to prepare salts, or even ethers, of the acid. The action of cold water upon the acid was so well marked, that we proceeded to determine the products formed. When bromfurfurdi- brompropionic acid is suspended in water, carbonic dioxide soon begins to escape, and after long standing the crystalline solid is com- pletely converted into a colorless oil. The aqueous solution then contains hydrobromic acid in abundance. As the decomposition was greatly facilitated by gentle heat, we usually have allowed the reaction to proceed at about 40°. When the decomposition was complete, we distilled with steam, and dried the heavy colorless oil thus obtained with calcic chloride. Ou distilllation under diminished pressure, we found that this oil began to boil at 108° under a pressure of 14 mm., and that the thermometer gradually rose to 112° the pressure remain- ing constant. The distillate was at first nearly colorless, and of high refractive power, but on standing it quite rapidly became dark- colored. Analyses of the freshly distilled substance showed it to be a bromfurfurbromethylen. I. 0.3173 grm. substance gave 0 3350grm. C02 and 0.0476 grm. ILO. II. 0.1928 grm. substance gave 0 2883 grm. AgBr. III. 0.2045 grm. substance gave 0.3056 grm. AgBr. and. III. 63.60 Calculated for Found CcII4Br20. i. II. c 28.57 28.79 H 1.59 1.67 Br 63.49 63.65 368 PROCEEDINGS OF THE AMERICAN ACADEMY The reaction is then strictly analogous to that by which /? brom- styrol may be made from phenyldibrompropionic acid : C7H5Br303 = C6H4Br20 + C02 + HBr. The aqueous solution left in the retort after distillation with steam deposited on long standing a small quantity of a crystalline acid. The quantity of this acid was so insignificant that we were able to iden- tify it only after uniting the products obtained in many successive preparations. Two determinations of the percentage of bromine showed the acid to be the bromfurfuracrylic acid subsequently de- scribed. Lack of material made it impossible to prove with precision the identity of the two acids, and we can therefore only assert their close resemblance. I. 0.1262 grm. substance gave 0.1091 grin. AgBr. II. 0.1956 grm. substance gave 0.1700 grm. AgBr. Calculated for Found. C7II,Br03. I. II. Br 36.86 36.79 36.99 We have hitherto been unable to find other definite products of the reaction. By the action of bromine upon bromfurfurbromethylen we could obtain no products which invited further study. On the other hand, alcoholic potassic hydrate gave us the corresponding acetylen deriva- tive, although we have not yet isolated it in a pure condition. The oil obtained as the direct product of the reaction contained much too large a percentage of bromine, and prolonged action at a higher temperature gave no more satisfactory results. That the oil con- tained the acetylen derivative was readily shown by its behavior with an ammoniacal solution of silver or copper. The silver compound was white, the copper compound a greenish yellow. The latter was made in larger quantity, carefully washed by decantation, and dried over sulphuric acid. It then exploded violently by heat or on contact with fuming nitric acid, and contained the required percentage of copper. I. 0.6479 grm. substance gave by electrolysis 0.1748 grm. Cu. II. 0.6178 grm. substance gave 0.1681 grm. Cu. Calculated for Found. [CgHjBrOJjCuj. I. II. Cu 27.16 26.98 27.20 From the copper compound we attempted to prepare the bromfurfur- acetylen in a pure condition. By decomposing with acid, extracting OP ARTS AND SCIEiNCES. 369 with ether, and distilling the well dried extract under diminished pressure, we obtained a colorless oil which boiled at 65-68° under a pressure of 19 mm. This oil contained a percentage of bromine, which left no doubt as to its identity, but showed at the same time that it was still impure. We have as yet made no further attempt at its complete purification. It seemed to us of interest to prepare by oxidation the diacetylen derivative also, analogous to the diacetenylphenyl of Glaser,* which was afterward more fully studied by v. Baeyer and Landsberg.| In its preparation we followed closely the method of v. Baeyer. To the copper compound was added one molecule of potassic ferricyanide in aqueous solution. When the oxidation was complete, the precipitate formed was collected on a filter, dried, and extracted with hot alcohol. On cooling the alcohol deposited the new compound in small iridescent plates which melted at 126°. It was readily soluble in hot alcohol, sparingly in cold alcohol, and dissolved freely in ether, chloroform, benzol, or ligroin. Analysis showed the substance to be dibromdifur- furdiacetylen (diacetenylbromfurfuryl) : C4H2BrO -C=C-C=C- C4H2BrO. I. 0.2476 grm. substance gave 0.3888 grm C02 and 0.0383 grm. H20. II. 0.1538 grm. substance gave 0.1696 grm. AgBr. III. 0.1548 grm. substance gave 0.1702 grm. AgBr. d. in. c Calculated for CjoH^Br-jC^. 42.36 i. 42.82 Found, II. H 1.18 1.72 Br 47.06 46.93 46.79 Bromfurfuracrylic Acid. The behavior of the acid containing three atoms of bromine which was obtained by the direct action of bromine upon furfuracrylic acid left little doubt that it was a bromfurfurdibrompropionic acid. If this view were correct, it seemed not improbable that the bromine attached to the the side-chain might be removed without disturbing the bromine in the furfuran ring, and that a bromfurfuracrylic acid would thus be formed. After a kw preliminary experiments it was found that zinc dust added to an alcoholic solution of the bronifnrftirdibrom- propionic acid brought about the desired result. The reaction is vig- * Ann. Chem. u. Pharm., cliv. 159. t Ber. d. deutsch. chem. Gesellsch., xv. 57. vol. xxiv. (n. s. xvi.) 24 870 PROCEEDINGS OP THE AMERICAN ACADEMY orous, and the boiling point of the alcohol soon reached. When the reaction is over, water is added to the filtered solution, and the acid which is thus precipitated is purified by conversion iuto its sodium salt, reprecipitation with hydrochloric acid, and recrystallization from dilute alcohol or boiling water. The yield of the new acid thus ob- tained was between 80 and 90 per cent of the theoretical amount, and analysis showed that it had the desired composition. I. 0.2645 grm. substance gave 0.3768 grm. C02 and 0.0566 grm. H20. II. 0.2511 grm. substance gave 0.2161 grm. AgBr. III. 0.2223 grm. substance gave 0.1920 grm. AgBr. IV. 0.1490 grm. substance gave 0.1288 grm. AgBr. Found. II. III. IV. c Calculated for C7H0Br03. 38.71 i. 38.86 H 2.30 2.38 Br 36.86 36.63 36.76 36.80 Bromfurfuracrylic acid crystallizes in long slender prisms, which are sparingly soluble in cold water, more readily in hot water. The acid dissolves readily in alcohol, ether, hot benzol, or hot chloroform, in cold benzol or cold chloroform it is but sparingly soluble, and it is nearly insoluble in ligroin. It melts sharply at 176-177°, but since it is somewhat decomposed and blackened by long continued heating above 150°, the bath must first be heated to within a few degrees of the melting point. Small quantities of the acid may readily be sublimed between watch-glasses. The sublimed product also melts at 176—177°, and darkens upon long heating. With bromine the acid unites readily, and forms the original substituted propionic acid. We have made many attempts to convert the acid into the corresponding substituted pyromucic acid, or to obtain from it by oxidation a product which should enable us to fix the position of the bromine atom, but hitherto without success. We can, therefore, at present only conjecture that the bromine in this case, as with the pyromucic acid, enters first the 8 position. For the further characterization of the acid we have prepared a few of its salts. Baric Br omfurfaracrylate, Ba(C7.II4Br03)2 . H20. — The barium salt is sparingly soluble in cold water, somewhat more readily in hot water, and crystallizes in clustered needles. When air-dried it loses nothing over sulphuric acid, gives up one molecule of water slowly at 100°, and is decomposed at a somewhat higher temperature. I. 1.1830 grm. of the air-dried salt lost at 100° 0.0380 grm. II20. Calculated for Ba(C,Il4Br03)2 . H20. H20 3.07 Ba 23.34 OF ARTS AND SCIENCES. 371 II. 0.7064 grm. of the air-dried salt lost at 100° 0.0227 grm. H20. III. 0.4898 grm. of the air-dried salt gave 0.1951 grm. BaS04. Found. I. 11. III. 3.21 3.21 23.42 I. 0.5258 grm. of the salt dried at 100° gave 0.2149 grm. BaS04. II. 0.4787 grm. of the salt dried at 100° gave 0.1955 grm. BaS04. Calculated for Found. Ba(C7lI4Br03)2. I. II. Ba 24.07 24.02 24.01 Calcic Bromfurfuracrylate, Ca(C-H4Br03)2. 3 H20. — This salt crys- tallizes in columnar aggregations of plates, and is sparingly soluble in cold water, more readily in hot water. The air-dried salt effloresces over sulphuric acid, and is gradually decomposed at 100°, but may be dried without difficulty at 80-85°. I. 1.1639 grm. of the air-dried salt lost at 82° 0.1184 grm. H20. II. 0.7362 grm. of the air-dried salt lost at 83-85° 0.0740 grm. H20. III. 0.6331 grm. of the air-dried salt gave 0.1648 grm. CaS04. IV. 0.5287 grm. of the air-dried salt gave 0.1375 grm. CaS04. Calculated for Found. Ca(C7H4Br03)2 . 3 H20. I. II. III. IV. H20 10.07 10.17 10.05 Ca 7.61 7.65 7.65 0.6123 grm. of the salt dried at 82° gave 0.1774 grm. CaS04. Calculated for Ca(C7H4Br03)2. Found. Ca 8.47 8.52 Sodic Bromfurfuracrylate, NaC7H4Br03. — This salt is readily soluble even in cold water, and crystallizes in anhydrous nodular aggregations. I. 0.7612 grm. of the salt gave 0.2228 grm. Na2S04. II. 0.7589 grm. of the salt gave 0.2206 grm. Na2S04. Calculated for Found. NaC7H4Br03. I- H. Na 9.62 9.48 9.42 Argentic Bromfurfuracrylate, AgCrII4BrOr — The silver salt, formed by the addition of argentic nitrate to a neutral solution of the ammo- nium salt, proved to be nearly insoluble in water, and was apparently amorphous. I. 0.3919 grm. of the salt gave 0.2261 grm. AgP»r. II. 0.4065 grm. of the salt gave 0.2347 grm. AgBr. 372 PROCEEDINGS OF THE AMERICAN ACADEMY Calculated for Found. AgC7H4Br03. I. rr. Ag 33.34 33.13 33.16 Ethyl Bromfurfuracrylate, C7H4Br03 . C2H5. — To a solution of the acid (5 parts) in somewhat more than its own weight of absolute alco- hol (6.5 parts) was added concentrated .sulphuric acid (3 parts), and the mixture heated upon the water bath for two or three hours. "We found that too long heating should be avoided since decomposition then ensued, and a product was formed which undoubtedly was analo- gous to that obtained by Markwald.* We have, however, made no careful study of it. As soon as the etherification appeared to be com- plete, the ether was precipitated with water, dried with calcic chloride, and distilled uuder diminished pressure. The greater part of the product distilled at 151-152° under a pressure of 14 mm., and on cooling this distillate completely solidified. From ligroin the ether could be obtained in large flat prisms, which melted at 42°. It was readily soluble in alcohol, ether, chloroform, benzol, or ligroin and had a faint aromatic odor. I. 0.1968 grm. substance gave 0.31 68 grm. C02 and 0.0673 grm. H20. II. 0.2251 grm. substance gave 0.1722 grm. AgBr. III. 0.2545 grm. substance gave 0.1943 grm. AgBr. m. c Calculated for C9H9Br03. 44.08 i. 43.88 Found. II. H 3.67 3.80 Br 32.65 32.55 32.49 We further attempted to make the amide, but found that the ether was hardly attacked by concentrated ammonic hydrate at 100°, and that at a much higher temperature (215°) most of the ether employed also remained unchanged. Bromfurfurbromacrylic Acid. It already has been mentioned that bromfurfurdibrompropionic acid is decomposed by heat with the evolution of hydrobromic acid, and the simultaneous formation of a disubstituted furfuracrylic acid might be inferred. We have made many attempts to bring about this loss of one molecule of hydrobromic acid by more convenient and more economical methods, but without success. In alcoholic solution potas- sic hydrate gave chiefly the ethylen derivative and potassic carbonate. * Loc. cit. OP ARTS AND SCIENCES. 373 no matter how the conditions of the reaction were varied. A number of high boiling neutral solvents gave no better results than those ob- tained by heating the acid by itself. The bromfurfurdibrompropionic acid was therefore carefully heated in shallow crystallizing dishes im- mersed in a sulphuric acid bath. The hydrobroinic acid thus escaped without blackening the product to any great extent. The tempera- ture was slowly raised to 130°, and when at this point the formation of hydrobromic acid was no longer noticeable the residue was boiled with dilute ammonic hydrate filtered, heated with bone-black, and the filtered solution concentrated by evaporation. In this way sparingly soluble finely felted needles of ammonic bromfurfurbromacrylate were obtained, which yielded the acid in a state of purity. I. 0.2246 grm. substance gave 0.2328 grm. C02 and 0.031 7 grm. H20. II. 0.2290 grm. substance gave 0.2373 grm. C02 and 0.03H grm. H20. III. 0.2059 grm. substance gave 0.2G15 grm. AgBr. IV. 0.2025 grm. substance gave 0.2571 grm. AgBr. Calculated for Found. C7H4Br20s. I. II. HI. IV. C 28.38 28.27 28.26 H 1.35 1.57 1.53 Br 54.05 54.04 54.03 Bromfurfurbromacrylic acid is almost insoluble even in hot water. It dissolves freely in ether or alcohol, and when precipitated by water from a hot alcoholic solution is obtained in fine clustered needles. At ordinary temperatures it is very sparingly soluble in chloroform or carbonic disulphide, but dissolves somewhat more freely on heating. The acid melts at 178-179° and small quantities of it may easily be sublimed without essential decomposition. In spite of many attempts, we have been unable to obtain experi- mental evidence as to the position of the bromine atoms. We have also been unable to prepare definite products by the addition of bro- mine to the acid, or to form from it bromfurfurpropiolic by the elimi- nation of hydrobromic acid. The following salts may serve for the better characterization of the acid. Baric Bromfurfnrbromacrylate, Ba(C7H3Br20..)2 . 2 ILO. — This salt was prepared by adding baric chloride to a solution of the ammo- nium salt. It is very sparingly soluble even in boiling water, and crystallizes in lustrous scales. The air-dried salt contain-, two mole- cules of water, which it does not lose over sulphuric acid. I. 1.4911 grm. of the air-dried salt lost at 120° 0.0674 grm. 11,0. II. 0.8824 grm. of the air-dried salt lost at 120° 0.0399 gnu. 11./). 374 PROCEEDINGS OF THE AMERICAN ACADEMY Calculated for Found. Ba(C7H3Br203)2.2Ha0. I. II. 4.72 4.52 4.52 H20 I. 0.2130 grin, of the anhydrous salt gave 0.0684 grm. BaS04. II. 0.2229 grm. of the anhydrous salt gave 0.0712 grm. BaS04. III. 0.4376 grm. of the anhydrous salt gave 0.1398 grm. BaS04. Calculated for Found. Ba(C7H3Br203)2. I. II. III. Ba 18.85 18.88 18.78 18.78 Argentic Bromfurfurbromacrylate, AgC7H3Br203. — The silver salt made by precipitation is very sparingly soluble even in boiling water, and is apparently amorphous. I. 0.2052 grm. of the salt dried over sulphuric acid gave 0.0951 grm. AgBr. II. 0.2101 grm. of the salt dried over sulphuric acid gave 0.0977 grm. AgBr. Calculated for Found. AgC,H3Br20j. I. II. Ag 26.80 26.62 26.71 Potassic Bromfurfurhromacrylate, KC7H3Br203. — The potassium salt is sparingly soluble in cold water, more readily soluble iu hot water, and crystallizes in slender clustered needles which are anhydrous. I. 0.2275 grm. of the salt gave 0.0589 grm. K2S04. II. 0.5386 grm. of the salt gave 0.1407 grm. K2S04. Calculated for Found. KC7HsBr20,. I. n. K 11.70 11.62 11.72 Ethyl Bromfurfurbromacrylate, C7H3Br203 . C2Hj. — The ethyl ether was made by heating for three hours on the water bath a solution of the acid (4 parts) in absolute alcohol (40 parts), with the addition of a small amount (3 parts) of concentrated sulphuric acid. The ether was then precipitated with water, washed with a dilute solution of sodic carbonate, and recrystallized from ligroin. It crystallized easily in radiated needles which melted at 55-56° and dissolved readily in alcohol, ether, chloroform, benzol, ligroin, or carbonic disulphide. I. 0.3774 grm. of substance gave 0.4592 grm. C02 and 0.0849 grm. H20. II. 0.2125 grm. substance gave 0.2464 grm. AgBr. III. 0.2179 grm. substance gave 0.2525 grm. AgBr. OF ARTS AND SCIENCES. 375 Calculated for Found C9H815r203. i. II. c 33.34 33.19 H 2.47 2.50 Br 49.39 49.3, III. 49.32 While we have been unable to establish with precision the constitu- tion of the foregoing derivatives of furfuracrylic acid, the analogies offered by the derivatives of pyromucic and cinnamic acids naturally suggest the following formulas for the substances in question : — HC = C - CHBr - CHBr - COOH \ O / IIC = C \ Br Bromfurfurdibrompropicmic Acid. HC = C - CH = CHBr \ O / HC = C \ Br Bromfurfurethylen. HC = C - CH = CBr - COOH \ O / HC = C \ Br HC = C - CH = CH - COOH \ O / HC = C \ Br Bromfurfurbromacrylic Acid. Bromfurfuracrylic Acid. 376 PROCEEDINGS OF THE AMERICAN ACADEMY III. ON THE SO CALLED DIOXYMALEIC ACID. By W. S. Hendrixson. Presented May 28, 1889. Several years ago Bourgoin * announced the discovery of two new acids which he had obtained by replacing the bromine of brommaleic and dibrommaleic acid by hydroxyl, and which he therefore called oxy- maleic and dioxymaleic acid. Although the experimental evidence as to the existence of these acids was very slight, and their assumed struc- ture wholly anomalous, they soon found place in many text-books. In 1886, at the suggestion of Fittig, the work of Bourgoin upon oxymaleic acid was repeated by Scherks,f who found that his state- ments were without foundation, and that brommaleic acid in aqueous solution was not in the least attacked by argentic oxide, even at 100°. Scherks further concluded that Bourgoin's statements concerning his dioxymaleic acid must also be incorrect, because the dibrommaleic acid which he used he claimed to have made from his tribromsuccinic acid, an acid which could not be formed under the given conditions, as shown by Fittig and Petri,:? or if formed would at once be decomposed into dibromacrylic acid and carbonic dioxide. This conclusion of Scherks seems hardly justified by Bourgoin's statements. The dibrommaleic acid which he used undoubtedly was made by the action of aqueous bromine upon succinic acid, and, while his material may have been far from pure, the question of its identity is in no way affected by his erro- neous assumption that it had been formed by the decomposition of tribromsuccinic acid. In any case the subject seemed to demand a more careful investigation. At the suggestion of Prof. H. B. Hill, I have, therefore, repeated Bourgoin's work upon dioxymaleic acid, and find that decomposition is in this case readily effected, but that the product formed is not dioxymaleic acid. The dibrommaleic acid needed for this investigation was made by the oxidation of mucobromic acid with cold fuming nitric acid, a method which had already been found in this laboratory to be much more advantageous than the methods previously described. Muco- * Bull, de la Soc. Chim.,xix. 482; xxii. 443. t Ann. d. Chem. u. Pharm., ccvii. 223. } Ibid., cxcv. 70. OF ARTS AND SCIENCES. 377 bromic acid was dissolved in cold fuming nitric acid, and the nearly saturated solution allowed to stand for several days at ordinary tem- peratures. When the mixture had completely solidified, the nitric acid was expelled by gectle heat, and the dry residue distilled from a small retort. In order to obtain a perfectly pure product, the distil- late was dissolved in water, neutralized with baric carbonate, and the baric dibrommaleate precipitated by the addition of alcohol. The barium salt was then converted into the sodium salt, and from this the silver salt was made by precipitation with argentic nitrate. According to Bourgoin, dioxymaleic acid is formed by heating ar- gentic dibrommaleate with water to 150°. On opening the tubes after heating for five hours he found that carbonic dioxide escaped, that argentic bromide had been formed, and that the liquid in the tubes was distinctly acid. On the addition of argentic nitrate to this acid solution carefully neutralized with ammouic hydrate he obtained a white insoluble silver salt, which gave on ignition a residue closely agreeing with the weight of metallic silver required by the formula Ag2C4H206. He found tbe acid to be a white crystalline solid, which was readily soluble in water and alcohol, and barely soluble in ether. With tbe alkalies and alkaline earths it formed readily soluble salts, and showed itself to be non-saturated in that it was capable of fixing hy- drogen aud bromine. Bourgoin gives, however, no analytical results whatsoever except the one already mentioned. On following closely the directions of Bourgoin, I found that the argentic dibrommaleate had been almost completely decomposed, and that at least 95 per cent of the theoretical amount of argentic bromide had been formed. The liquid in the tubes was strongly acid, but the carbonic dioxide which escaped was by no means insignificant in quan- tity. Although the aqueous solution gave a crystalline precipitate with argentic nitrate after careful neutralization with amnionic hydrate, it was thought advisable to distil the liquid with steam before preparing salts for analysis, since it was found that the acid volatilized readily under these conditions. The acid distillate was neutralized with calcic carbonate, the silver salt precipitated by the addition of argentic nitrate to the concentrated solution, and recrystallized from hot water. The silver salt thus obtained closely resembled argentic acetate, and its identity was established by analysis. I. 0.4677 grm. of the air-dried salt gave 0.5249 grm. A^Br. II. 0.2263 grm. of the air-dried salt gave 0.1465 grm. Ag. III. 0.2056 grm. of the salt dried over sulphuric acid gave 0.1082 grm. C02, 0.0330 grm. H20, and 0.1327 grm. Ag. Calculated for AgC2H302. 64.67 i. 64.46 Found. II. 64.73 m. 64.54 14.37 14.35 1.80 1.78 378 PROCEEDINGS OF THE AMERICAN ACADEMY H c H The barium salt was also made by neutralizing the acid distillate with baric carbonate. The salt obtained on evaporation was either recrystallized from water, or precipitated from a concentrated aqueous solution by alcohol. I failed to find any definite statements as to the composition of the salt thus precipitated by alcohol, but experiments of my own showed that it contained one molecule of water like the salt crystallized from water. I. 1.1456 grm. of the air-dried salt lost at 150° 0.0780 grm. H20. II. 0.9187 grm. of the air-dried salt lost at 125° 0.0609 grm. H20. III. 0.4561 grm. of the air-dried salt gave 0.3899 grm. BaS04. IV. 0.6868 grm. of the air-dried salt gave 0.5841 grm. BaS04. Calculated for Found. Ba(C2H302)2 . H20. I. II. IH. IV. H20 6.59 6.80 6.62 Ba 50.18 50.25 50.02 0.8554 grm. of the salt dried at 125° gave 0.7811 grm. BaS04. Calculated for Ba^HA)* Found. Ba 53.73 53.69 It thus appears that acetic acid is formed in the decomposition of argentic dibrommaleate by water at 150° and the reaction may be expressed by the equation : Ag2C4Br204 + 2 H20 = 2 AgBr + C02 + C2H402. The weight of baric acetate which was obtained from the distilled liquid amounted to about 60 per cent of the theoretical yield required by this equation, while 85 per cent of the theoretical amount of free acid, calculated as acetic acid, was found by direct titration of the con- tents of the tubes. The higher result in the latter case may in part have been due to incomplete expulsion of the carbonic dioxide, but the most careful search failed to show that any well defined organic acid except acetic acid had been formed in the reaction. Dibrommaleic acid therefore yields, under the conditions prescribed by Bourgoin for its conversion into dioxymaleic acid, carbonic dioxide and acetic acid. The facts observed give no certain information as to the mechanism of the reaction. If it is assumed that the body OF ARTS AND SCIENCES. 379 C H OH is first formed, it would pass at once into the aldehyde alcohol H OH from which acetic acid would then be formed, precisely in the same way that tartronic acid is formed from dibrompyruric acid,* or from dioxytartaric acid.f It is more probable, however, that the ketone acid COOH I CO Ih ?OH COOH is the first product, and that this passes into acetic acid in a similar way through the loss of carbonic dioxide. * Griniaux, Bull, de la Soc. China., xxvii. 440. t Kekule, Ann. Chem. u. Pharm., ccxxi. 230. 880 PROCEEDINGS OP THE AMERICAN ACADEMY XXVII. AN ADDRESS DELIVERED AT THE MEETING OF APRIL 10, WHEN THE RUM- FORD MEDALS WERE PRESENTED TO PROFESSOR A. A. MICHELSON. By Joseph Lovering. For many generations it was assumed that no sensible time was taken by light in moving over the largest distances. The velocity of sound was found by noting the time which elapsed between seeing the flash and hearing the report of an explosion. It was only in the vast spaces of astronomy that distances existed large enough to un- mask the finite velocity of light, and, in extreme cases, to make it seem even to loiter on its way. The satellites of Jupiter were discovered by Galileo in 1610; and the eclipses of these satellites by the shadow of Jupiter became an interesting subject of observation. It was soon noticed that the in- terval between successive eclipses of the same satellite was shorter when the earth was approaching Jupiter, and longer when the earth was receding from Jupiter. The change of pitch in the whistle of a locomotive, under similar motions, would suggest to the modern mind an easy explanation. A Danish astronomer, Romer, without the help of this analogy, deciphered the problem in astronomy. The eclipse was telegraphed to the observer by a ray of light, and the news was hastened or delayed in proportion to the distance from which it came. In this way it was discovered that light took about 18 minutes to run over the diameter of the earth's orbit. This discovery was published by Romer in the Memoirs of the French Academy in 1675. The mathematical astronomer Delambre, from a discussion of one thou- sand of these eclipses observed between 1662 and 1802, found for the velocity of light 193,350 miles a second. Meanwhile Rbmer's method, after fifty years of waiting, had been substantially confirmed in an unexpected quarter. Dr. Bradley of the Greenwich Observatory, the greatest astronomical observer of his day, was perplexed by certain periodical fluctuations, of small amount, OF ARTS AND SCIENCES. 381 in the position of the stars. Suddenly the explanation was flashed upon him by something he observed while yachting on the River Thames. He noticed that, whenever the boat turned about, the direction of the vane altered. He asked the sailors, Why ? All they could say was, that it always did. Reflecting upon the matter, Brad- ley concluded that the motion of the boat was compounded with the velocity of the wind, and that the vane represented the resultant direc- tion. He was not slow in seeing the application of this homely illus- tration of the parallelogram of motion to his astronomical puzzle. The velocity of light was compounded with the velocity of the earth in its orbit, so that its apparent direction differed by a small angle from its true direction, and the difference was called aberration. In spearing a fish or shooting a bird, the sportsman does not aim at them, but ahead of them. This inclination from the true direction is similar, in angular measure, to what the astronomer calls aberration. Struve's measurement of aberration combined with the velocity of the earth in its orbit gave for the velocity of light 191,513 miles a second. Both of the two methods described for obtaining the velocity of light depend for their accuracy upon the assumed distance of the earth from the sun. The distance adopted was the one found by the transits of Venus in 1761 and 1769, viz. 95,360,000 miles. During the last forty years, the opinion has been gaining ground amon