)jn.
These equations ought to give the same values of A~! what-
ever the strength of the solution may be; and herein lies a
first test of the truth of the principles involved.
The following values of cA for NaCl are calculated from
Volkmann’s data (Wied. Ann. xvii.) for its solution in water
at 20°; w is taken as 18, although we consider the water
molecule to be complex, but this does not affect the purely
relative comparison being made :—
ait ahs "105 084 "052 (35 ‘017
cA! . ° 1°34 1°38 1°47 1°46 4:42
Considering that the solutions range from saturation down
to considerable dilution, the approach to constancy is satis-
factory; but it will be noticed that, on the whole, there is a
tendency for the value of cA—! to increase with diminishing
concentration, and this same phenomenon is to be seen in
the case of almost all Volkmann’s solutions, most pronoun-
cedly in that of CaCl, :—
eT Se eee ‘O91 "068 ‘O41 ‘O21 ‘O11
GRE) fe PeN 2A 2 op ZG 2°95 Ae &
This case shows us that there is a certain amount of incom-
pleteness in our theory of the capillarity of solutions, as indeed
we ought to be surprised if there were not, when we try to
apply our arbitrary definition of the molecular mass of a solu-
tion to one which contains 56 parts by weight of CaCl, to 100
of H,O as the solution for which n=*091 does, and also when
we assume that the concentration in the surface-layer is the same
as in the body-fluid at all strengths up to saturation. If our
object were an exhaustive representation of the connexion
between the surface-tension of a solution and its concentration,
it would be easy to introduce a slight empirical alteration into
the above equations to make them exhaustive. For instance,
ae
Laws of Moleculur Force. 279
we might imagine that the effective value of W in a solution
experiences a small change proportional to the concentration ;
but the equations as they stand will prove to be sufficient for
our purpose if, in comparing solutions of different substances,
we calculate cA! for the same value of 2 throughout.
In all. subsequent calculations n=18/1000. The experi-
mental data for surface-tensions of solutions are abundant, the
chief that I know of and have used being those of Valson
(Compt. Rend. \xx., lxxiv.), Volkmann (Wied. Ann. xvii.),
Réntgen and Schneider (Wied. Ann. xxix.), and Traube
(Journ. fiir Chem. cxxxix.).
The following Table contains the values of cA! for a certain
namber of compounds, the surface-tension being measured in
‘rammes weight per linear metre and the half molecules of the
salts of the bibasic acids being regarded as molecules.
TABLE XX XI.—Values of cA.
ior Br pcCk NO. POH: sO, 400,
ib. S Gaetan 4°15 | 2°46 "83 | 161 83 | 161
Sich, oe SO0e p22 tr) 670), |, ode | 2. | 145
oe 4°74 | 3:06 | 1:45 | 2:30 | 1:37 | 2:30 | 1-95
ik ae 4:99 | 3:31 | 1-78 | 2:55 | 1-71 | 2-72 | 2-21
The study of this table brings out the fact that the differences
of the numbers in any two rows or in any two columns are
constant: thus the differences for the iodide and chloride of
the four bases are in order 3°32, 3°29, 3°29, and 3:21, while
the differences of cA—! for the Na and Li salts of the mono-
basic acids are in order *59, °60,°62,°69, and °54. Accordingly
each atom contributes a certain definite part to the value of
cA for the molecule in which it occurs, and that part is
independent of the other atoms in the molecule. I shall call
this part the parameter-reciprocal modulus of the atom ; we
have not at present sufficient data to get its absolute value in
any case, but if we make Li our standard positive radical, and
Cl the standard negative, we can calculate the average values
of the difference between the parameter-reciprocal modulus of
a radical and its standard,—thus in the case of iodine this
difference is 3°28, and in the case of Na ‘61, and so on.
Before tabulating these mean values I will give the values
calculated for the salts of some other metals with the values
for the same salts of Li subtracted.
280 Mr. William Sutherland on the
TABLE XXXII.
I Br Cl NO,. | 480,
ob een ne Re 39 35 53
MGe ai... 632: 44 73 67 DD s
ar Gi ce ¥ 1-67. | Smt
Ba tae Vee 249 | 2:52
I7n j= liad. 1-35 2 1:33
10d ab bes 224 | 242 | 215 2:29
Min = lui c...s 1:17 93 | 12
To these we may add the following values, cbtained from
the sulphates 3Fe—Li 1:27, 3Ni—Li 1:19, $Co—li 1:15,
4Cu—Li 1:49, JAI—Li *6, Fe, —Li *5, and 4Cr,,— Li 1:0;
and the two following from the nitrates Ag—lLi 3°91, and
4Pb—Li 4°51.
The following Table contains the values of the parameter-
reciprocal moduluses of the different metals minus that for
Li and of the negative radicals minus that for Cl.
Tapia XXL.
Mean Values of Parameter-reciprocal Modulus for the Metals
with that for Li subtracted.
|
Na. K. NH. | 3Mg.| $Ca. | 4Sr. | 4Ba.
6L | 90 |—15] 42 | 6 Rhy a ae
{
1:33 | 2:3 12
]
Pree
. | $Ni. | 4Co.
us |
Ag. | 4Pb. | 2Al.
ee ere 2 Ail
|
|
1:27 | 1:2 Hy 1:5
39 | 45 | 6
The same for negative radicals with that for Cl subtracted :—
ie Br. NO,. On. / 380/59 apes
3°28 1°56 “81 ‘04 “86 “46
It may be worth mentioning that these differences show a
pretty close parallelism to the corresponding differences of
the atomic refraction given by Gladstone (Phil. Trans. 1870)
but not close enough to be worth dwelling on.
In the case of the organic bodies studied there was nothing
analogous to this singular property possessed by these inorganic¢
compounds of having the reciprocal of the parameter A of
molecular force separable into a constant and definite parts
~ Laws of Molecular Force. — 281
contributed by each constituent of the molecule. Thus we
have characteristic of inorganic bodies in solution another of
those properties called by Valson modular, who discovered
that the density, capillary elevation, and refraction of normal
solutions (gramme-equivalent dissolved in a litre of water)
could all be obtained from the values for a standard solution
such as that of LiCl by the addition of certain numbers or
moduluses representing invariable differences for the metals
and Li and for the negative radicals and Cl. Other properties
of solutions have since been proved to be modular, as for
instance their heats of formation from their elements and
their electric conductivities. I think the modular nature of
some of these properties of solutions is the outcome of this
modular property in the parameter reciprocal of molecular
force along with the additive property in mass. To prove
this in the case of density would require a special investiga-
tion, but if we assume the property for density we can easily
deduce Valson’s result that the property applies to capillary
elevation. Let h be the height to which a normal solution of
any salt RQ rises in a tube of radius 1 millim., then
hy poke HDR
h=2a/p=2Xpi( ats Je.
Let r and g be the density moduluses of the radicals R, and
Q, being small fractions, then p=d+r+q where d is a con-
stant nearly 1 ; also
X1=(Wt+nA)/1+n),
so that
l+n (wknp\?
n= 2( way naa )atr+ gyi ro |.
Remembering that in the case of a normal solution n is small,
being 18/1000, we can develop the last expression in powers
of n as far as the first ; and it is evident that as p the mole-
cular mass possesses the additive property and A~! possesses
the modular property, then 4 must also possess the modular
property, which is Valson’s result.
16. Second method of finding the virial constant for inorganic
bodies or solid bodies in general from the properties of their
solutcons.—In this method the compressibility of solutions is
used. Ifa solution could be treated as an ordinary liquid we
might attempt to apply the equation of our second method for
liquids, namely,
PyeG: AOi a
a= 3(%% + gg rel 3
but as the solutions to be dealt with are all aqueous, and as a
Phil. Mag. 8. 5. Vol. 35. No. 214. March 1893. U
982 | Mr. William Sutherland on the
for water at ordinary temperatures is quite abnormal, it would
be useless to attempt to apply this equation to them; but
from the “ dimensions” of the physical quantities involved in
it we may make it yield a correct form of empirical equation
for solutions. If we neglect the small term 25R/26, and also
the difference between v and v, at ordinary temperatures, the
equation above suggests the simple form / varies as 1/up?, that is
X-! varies as wp”, say KX~1=yp*, where K is a constant,
and for water KW-!=y,, the compressibility of water, and
as before we have X-t=(W-!+nA7})/(l+n). But on
account of the rapid alteration of the compressibility of water
with pressure, and its anomalous variation with temperature,
we must be prepared to admit that the part of the com-
pressibility of a solution due to the water in it is altered from
its value in pure water, and is more altered the more the
water is compressed in the process of dissolving the salt. Let
this compression be measured roughly by the total amount of
shrinkage that ensues when 1 molecule of salt is dissolved in
1000 grms. of water, call the shrinkage A, and let us amend
the equation given above to KX~!=ypp?+/(A): Let suffixes
aand 6 attached to symbols refer them to two different bodies,
then
, KX —KXs*=1,p2— Papi +F(A,) —7(4,);
ut
KX7!—KX1=Kn(A7!—A;,1)/A +n),
oe Kn(Apt— As*)/(L +2) = ape— Hops thAa) — F(A»).
Hence selecting pairs of bodies for which A,=A, approxi-
mately, we ought to get “,p7— @,p; proportional to cA7*—cA;*,
the values of the last expression being obtainable from
Table XX XI.
To facilitate the comparison I furnish the following broad
statements about A founded on the study of data as to the
molecular volumes of salts, both solid and in solution, given
by Favre and Valson (Comp. Rend. Ixxvii.) Long (Wied.
Ann. 1ix.),and Nicol (Phil. Mag. xvi. and xviii.). The modular
property applies approximately to shrinkage on solution ; the
shrinkage of a gramme molecule of LiCl is 2, and the shrinkage
for : gramme molecule is increased when for Li is substi-
tute
K. Na. NH; _ 30a, 38r, $Ba.
by-o' ‘i —d 10 {h 127s
and when for Cl is substituted
Br. i NO,. - 180, 2oe"
by 0 0 0 8 14,
Laws of Molecular Force. 283
After giving the values of up? in the next table we can pro-
ceed with the comparison.
TaBLE XX XIV.—Values of 10"pp?.
cna) aa i We ENO gl SO ACOs
Ms. | Soc ciae- 432 484 541 457 433
Witte he oe ..| 441 496 550 468 444 498
LC 454 507 557 480 450 437
ELS 443 493 544 466 449,
Or ian 464
Soe ae 497
so 521
Lhe experimental data used are those of Rontgen and
Schneider (Wied. Ann. xxix.), and those of M. Schumann
(Wied. Ann. xxxi.) for CaCl, SrCl,, and BaCl,, in the case
of which I calculated the compressibility for the half-gramme
molecule according to his result that w—p,,=cp where p is
percentage of salt, using a value of ¢ got from the more con-
centrated solutions.
An inspection of this table shows that 10’yp? possesses the
modular property; it gives for instance the following dif-
ferences for Na and Li, 9, 12,9, 11,11, with a mean value 10,
and so on for the other metals; the mean values for the metals
minus that for Li are :—
Na. K. NH,,. Ca, iS8r. Ba.
10 20 8 32 65 89 ;
and for the negative radicals minus that for Cl :—
Br. L NO, 380, 300,.
52 105 25 0 —15.
We can now select pairs of bodies for which A, =A, and test
if {1,07 —[,0; is proportional to cA '—cA>1.
The following are pairs of elements ands acterized by nearly
equal shrinkage on solution with the values of the differences
of 10’up? and of cA~ and also their ratio.
TABLE XXXV.
HKqual shrinkage pair...| K,Na. | Sr, $Ca.| 3 Ba, $Ca. | Br, Cl.| I, Cl.
—_—_~—- -
Mean diff. of 107up?...| 10 33 57 52 105
Mean diff. of cA~?...] 29 1:05 1:85 | 1:56 | 3:28
Ratio of differences ...} 34 3l 31 33 32
984 Mr. William Sutherland on the
The agreement here is excellent, as will be seen more clearly
if we compare bodies not having equal shrinkage, as K and
Li, for which we get the 10"up? difference 20, the cA~* diffe-
rence ‘90 with a ratio 22, or K and NH,, for which the two
differences are 12 and 1:05 with a ratio 11.
The agreement above is a verification of the theory of the
compressibility of solutions, here barely outlined, and the
equation
10°(4,p2—Myp;) =32 (cAZ!—cA;")
when A,=A, nearly constitutes a second method of getting
values of cA~1; but we will not use it, as it adds no bodies to
our list. It suffices to have partly verified the principles on
which the first method is founded by their application to quite
another physical phenomenon, and especially the principle
involved in the remarkable equation
X—1=(W-!+nA)/(1+72).
With the values in Table XXXITI. and that for LiCl, namely,
83, we can obtain the value of cA—! for any salt whose con-
stituents are to be found in the table, or we can if we like use
the actual values in Tables XXX. and XX XI1.; we can then cal-
culate M?/cA—, which is proportional to M*/, or M77=CM*/cA—,
where C is a constant. To connect the values of M?/ thus
found with those previously given absolutely in Table XXV.,
we must find the value of C/c, which we can proceed to do in
the following manner :—
We have seen (Section 14) that we had better regard the
molecule of water as doubled relatively to that of ordinary
liquids, and as we have shown that the molecules are paired
in ordinary liquids the molecules are doubly paired in water ;
but it was suggested that the second pairing of the pairs was not
attended with any alteration in the parameter of molecular
force, and that the only effect of the second pairing was to make
the radius of the molecular domain of water 2? as large as if
water were an ordinary liquid. And, again, in the case of
solutions the surface-tensions have been measured at about
15°C , whereas for comparison with our previous work they
ought to have been measured at 2T,/3, which for water is about
150°C. At this temperature the value of the surface-tension
of water reduces, according to Hitvés, to about °6 of its value
at 15°C. Hence the equation, which treating water as an
ordinary liquid and at 15° we wrote a, = Wwi/c, ought for
double pairing and at 150° to become ‘6a,—=W23w#/c, and
similar statements hold for the equation for «; so that values
Laws of Molecular Force. — 285
of W, X,and A, as deduced from measurements at 15°, ought
to be reduced by the factor ‘6/23, or 1/2, to give the desired
values. Now in the case of homogeneous liquids in the
equation l=cav*/m? giving 1 in terms of the megadyne we
found a value 5930 for c/2, with the megamegadyne as unit
of force c/2=00593; and we can use this same value in the
case of solutions after we have halved our values of A, or
doubled those of cA—! so far given ; hence using the values
of cA so far given we get M*/=:00593M?/cA—1.
Fortunately, a test of this argument is made possible by
means of Traube’s data for the surface-tension of solutions of
certain organic acids and sugars, for which the values of
‘00593M?/cA— are given in the following Table, as well as
values of S found by the relation M?/=6S (the term ‘668?
being omitted), and also values of S calculated from the
dynic equivalents in Table XX VI.
TaBLeE XXXVI.
Oxalic Acid.) Citric Acid. Glycerine. | Mannite.
(COOH),. |C,H,OH(COOH),.) C,H,(OH),.) C,H,(OH),.
We ae es hove on gelo ds 19-4 43°5 33°5 63-0
Sa MPYIG. oa cees ss Be "2 56 10°5
S from dynic equiv. 4:2 9°7 5:0 10°0
Tartaric Acid. Dextrose. | Saccharose.
C,H,(OH),(COOH),. | C.H,.05. | Ci.H»,0)).
-| JU U) nee 6c eget On ee eee 389 721 112°5
IME OP eae retshi sa.ceeses ss 65 12:0 188
S from dynic equivalents 74 9-6 18:1
The agreement between the two sets of numbers is not all
that could be desired, but it is good enough to show that the
only part of M?/ effective in a solution is the linear term in
M*%=6S+°66S?; and we have already seen that when the
molecules of ordinary liquids pair during liquefaction the term
‘66S? is inoperative in the process, so that there is a certain
resemblance in the relations of two paired molecules and those
of solvent to those of substance dissolved.
Returning to the inorganic compounds we can now tabulate
the absolute values of M2l, calculated according to the rela-
tion M7/=:00593M?/cA—. The manner of calculation is best
illustrated by an example, say for KBr; first °83 is taken as
the value for LiCl, and to it are added -90 and 1°56, taken
from Table XX XITI., as the differences for K and Li and for
286 Mr. William Sutherland on the
Br and Ol; the square of the molecular weight of KBr is
divided by this sum and multiplied by -00593 to give the
tabulated value of M2/ in terms of the megamegadyne. From
the value of M2/ thus found the dynic equivalent S is caleu-
lated by the relation M2/=6S, which has been seen to be
appropriate to values of M?/ obtained from solutions.
TABLE XXX V1I1I.—Values of M?/ and 8.
Cl. Br. i NO,. 180n S)e 260.
M7. S. | Mz. S. | M% S.|M¥%. S. | MW S. (Mz S
Li...) 125 29 | 167 3-1) 257 43 171-28 qOGeees
Na. ...| 13:7 23 | 208 35 | 28:0 4-7 1.188 3 1)) deems
K ...| 185 $1 | 283° 4:7 | 82:4 5-4 | 235 39 | 1725 aaa
NH, | 23:0 3:8'| 27-0 4:5) 81:0 52 | 25:0 427) 170m@e
iMg | 104 1-7 | 17-7 80] 251 42 | 156 26) toa
4Ca...| 120 2:0 | 19-4 3:2 | 267 451173 29
ASr ...| 142 2-4 | 21:8 3:6 | 293 49] 195 32
3Ba...| 18:8 3:1 | 264 44 | 339 56 | 240 40
Ae Oa Dold gece ote eee? et tn jock: ieee 21 |
40d... 15°7 26 | 23:2 3:9°| 305 51 | 21:0 35 | 162527
4 11° 9G in | 168 eee Sie
AgNO,. |3Pb(NO,),.| 3CuSO,. 4FeSO,. | 3NiSO,.
IM 30°6 26°3 lS 11°4 12°3 oa
Risentisece Bri 4:4 ied) 1-9 20
3CoSO,. sAl,(SO,);. | ¢Fe,(SO,)3. | 4Cr.(SO,),.
IMEI bcccsnaen 12°7 89 12°6 9°6
iad Bs aakuree 21 1-5 21 16
The additive principle holds amongst both sets of numbers
except in the case of NH,; see for instance the following list
of the differences of S for the iodides and chlorides :—2°2, 2:4,
2°3, 2°D, 2°, 2°8, 2°59, 2°5. Now we have already seen that
the modular principle applies to cA— (the modular principle
applies when a quantity is given by the addition of moduluses
to a constant, the additive principle is a special case of the
modular in which the constant is zero) ; the additive principle
apples to M the molecular weight: hence it would appear
Laws of Molecular Force. 287
to be a mathematical impossibility that the modular or additive
principle should apply also to M?/cA—!, rigorously ; or, more
accurately, if the modular principle applies rigorously to one
of the quantities cA~! and M?/cA—! it cannot apply rigorously
to the other: but practically we find such relations amongst
the numbers that both are approximately obedient to the
modular principle. The case of NH, casts some light on the
question, for with it cA—! shows the same differences in the
values of the chloride, bromide, iodide, and nitrate as with
the other positive radicals, while M?/cA—! does not do so:
this case would make it appear that the modular principle
applies rigorously to cA}, but not so rigorously to M?/cA—}.
But leaving out of the count this case of NH,, significant as
it is, we can find mean values for the differences of the dynic
equivalents of all the metals and Li, and of all the negative
radicals and Cl; if we can obtain the absolute value of the
dynic equivalent of Li and of Cl, we shall have those for all
the metals and radicals. Now from the organic compounds
we have already got a value 1°3 for the dynic equivalent of
Cl, and hence from the value for LiCl we could obtain that
for Li. The value tabulated for LiCl is 2:1, but we can
obtain a mean value fairer to all the other bodies by sub-
tracting, for example, from the value for KI the mean difference
for K and Li, and for I and Cl; in this way we arrive at a
mean value 1:9 for LiCl, from which, taking the value 1°3 for
Cl, weshould get °6 for Li. But the refraction-equivalents of
the halogens are supposed by Gladstone to be a little larger
in inorganic than organic compounds ; so that in the light of
our previous knowledge of a close parallelism between dynic
equivalents and refraction-equivalents it might be safer to
assume that the dynic equivalents of Li and Cl in LiCl are in
the ratio of their refraction-equivalents in that compound,
namely, 3°8 and 10:7. According to this assumption the values
for Li and Cl come out ‘5 and 1:4, which we will adopt as
true and use in the calculation of the dynic equivalents of the
elements given in the following Table. These are measured
of course as before in terms of that for CH, as unity, and,
again, for comparison there are written along with the dynic
equivalents the refraction-equivalents in terms of that for CH,
as unity, calculated from Gladstone’s values (Phil. Trans.
1870).
288 Mr. William Sutherland on the
TABLE X XXVIII.
Li. | Na. | K. | $Mg.| 3Ca. | 2S
Pete ee | | |
|
Dynic equivalent ...... te 3D ‘Sh AGG ‘3 | 758 ‘9 | 4)
Refraction-equivalent.. °5 63| 1:06] -46-| -68 | ‘90 | 1:04 ‘674
|
= i i
Ag. | 4Pb. | 3Cu.| $Mn. | 3Fe.
|
Dynic equivalent ...... 2°70 | 20 6 "5 6 xf 8 >| 8
76) 8 | +80 1) 5690 aga eayaeetoos
Refraction-equivalent .. 2:06 1-63
4Cr.| Cl | Br. | ZL | NO, | 480,|400,.|4Cr0,.
Dynic equivalent ...... 3 | 141 27 | 88 | 23 | 135
Refraction-equivalent.| °7 14 | 90°71 3:6" | 9-6 eee
| | i
Again we see a remarkable parallelism between the dynic
and refraction-equivalents of the elements and radicals. Of
course there are refinements which will yet have to be made
in the calculation of the dynic equivalents, but it is not likely
that they will make the parallelism seriously closer.
17. Meaning of the Parallelism between Dynic and Refraction
Equivalents, and general speculations as to the volumes of the
atoms and their relation to ionic speeds—We are now called
upon to consider the meaning of this parallelism which has
been demonstrated both for organic and inorganic compounds,
and we shall be helped thereto by the very simple theory which
I have given of the Gladstone refraction-equivalent (Phil. Mag.
Feb. 1889), showing that to a first approximation
(n—1l)u = T(N—1)U,
where n is the index of refraction and w the molecular domain
of a substance, N the index of the matter of an atom, and U
its volume in the molecule. Hence the refraction-equivalent
of an element is the product of the refractivity (Sir W. Thom-
son’s name for index minus unity) of the substance of its atom
and the volume of the atom (the volume of the atom being
measured in terms of the unit in which the molecular domain,
usually called molecular volume, is measured); so that the re-
Laws of Molecular Force. 289
fraction-equivalent is a function of the two variables only,
namely, the volume of the atom and the velocity of light
through it. Now we have seen that the expression M/, as a
whole, in one aspect appears to be not dependent directly on
the molecular mass M, seeing that M?/ can be represented in
terms of certain quantities which we have called dynic equi-
valents. Hence, as / is proportional to A in our expression
3Am?/r* for molecular force, we see that in one aspect mole-
cular force seems to be not directly dependent on the mass of
the attracting molecules; and yet, on the other hand, in con-
sidering solutions we found that the quantity A asserted its
individuality as separate from the whole expression Am?, so
that in another aspect there does appear to be a mass action
in the attraction of two molecules. However, regarding
M?/ or Am? as a whole, the simplest hypothesis we can make
about the mutual action of molecules is that it depends most
on the size of the molecules. This would make Am? a simple
function of U; so that the dynic and refraction equivalents
would have this in common, that they are both simple functions
of U. Suppose, now, that the velocity of light through all
matter in the chemically combined state is approximately the
same, or that N is approximately the same for all atoms as
constituents of compound molecules, then the refraction-equi-
valents given by Gladstone are directly proportional to the
volumes of the atoms in the combined state, and then the
parallelism between dynic and refraction equivalents would
mean that 8 is nearly proportional to the volume. It is very
interesting, therefore, to inquire briefly whether there is any
evidence to prove that Gladstone’s refraction-equivalents are
proportional to the volumes of the atoms; and I think that
in Kohlrausch’s velocities of the ions in electrolysis we have
such evidence. If different solutions, such as those of KCl,
NaCl, or 4BaCl, ere electrolysed under identical cireum-
stances, then we know, according to Faraday’s law, that
each atom of K and of Na, and each half-atom of Ba, may be
considered to receive the same charge, so that they acquire
their ionic speeds under the action of the same accelerating
force. Accordingly, the ionic speed characteristic of an atom is
reached when the “ frictional” resistance to its motion is equal
to this accelerating force ; hence the “ frictional ”’ resistance is
the same for all atoms, or rather for all electrochemical equi-
valents. Now the “ frictional ” resistance will be a function
of the velocity of the atom and of its domain (atomic volume)
and of its actual volume as well as of the domain and actual
volume of the molecule of the solvent; but if water is the
solvent in all cases, the only quantities which vary from body
290 Mr. William Sutherland on the
to body are the velocity and the domain and volume of the
ions, so that we can say
“ frictional” resistance = $(V, u, U),
v V = F(u, U).
Now the simplest connexion that one can imagine between
the velocity and the domain and volume of the ion is that
the velocity will be greatest when the free domain or the
difference between the domain and the volume is greatest,
or, to be more general, when the difference between the
domain and some multiple of the volume is greatest; but
if N is the same for all combined atoms, then U is proportional
to the refraction-equivalent g. Hence the form of F is such
that it contains w—ag, where a is a constant. On studying
the experimental data I found that a might be considered
unity, and that V is a linear function of w—q. There is a
little difficulty in determining with accuracy the domain of an
ionic atom in a solution. Nicol, in his work (Phil. Mag. xvi.,
xviii.) on the molecular domains of inorganic compounds in
solution, has confined his attention almost entirely to differ-
ences of domains, making the assumption suitable to his purpose
that the inolecular domain of water is unaltered in solutions,
whereas we should expect that the greater part of the shrinkage
occurring on solution of an inorganic crystal happens in the
water, which is far more compressible than the crystal.
Accordingly I take the molecular domains of salts in the
solid state, as given by Long in his paper on diffusion of
solutions (Wied. Ann. ix.), as nearer to the true domain when
they are in solution than Nicol’s values ; but to allow to a
certain extent for the change of state on solution, I have assumed
that in each case the water experiences four fifths of the total
shrinkage and the dissolved salt one fifth. This is an arbitrary
adjustment, and is of no material importance to the comparison
to be made except as showing that the point has not been over-
looked. In the following Table are given under wu the mole-
cular domains, under g the molecular refractions (Gladstone’s),
in the next column their differences, under & the specific mole-
cular conductivities determined in highly dilute solution by
Kohlrausch and shown by him to be equal to the sum of the
velocities of the ions in each case. These are taken from his
paper (Wied. Ann. xxvi.), with a few additions from an
earlier one (Wied. Ann. vi.). Under & (calculated) are given
values of the conductivity calculated from the equation
k = 684+2°2 (w—g),
7
Laws of Molecular Force. 291
expressing the linear relation between conductivity or sum of
ionic velocities and u—gq.
TABLE XX XIX.
U. q. uUu—q. k. X (cale.).
AU een tees» 3 =i 53°5 39°3 18 107 108
ERE fi. esses 44 25 19 107 110
Lh a oee eee 36 18°8 iby 105 105
Shoe 41 32 9 87 88
1 (C151? deen poeR ee 32 21°7 10 87 90
ite OW ee roe 24 155 8:5 87 87
BG ine 55.2 5000 20°5 145 6 78 81
£MgCl, .....005. 20 14 6 80 81
2 02) 0: Lear 22 16 6 81 81
He 0] Ree 24 17-5 6:5 83 82
PCL, wowosina' 24 186 D4 86 80
22/710 Ul ule paeeeee 23 15°8 7 17 83
The agreement is here such as to prove a true connexion
between conductivity and u—q, the more striking as no relation
can be seen between conductivity and wu or q taken separately.
The only bodies I have omitted from Kohlrausch’s latter list
are the nitrates of some of the above metals and of silver, the
hydrogen compounds of the halogens, and the ammonium
compounds. These do not give results in harmony with
those in the last table, and, indeed, we should hardly expect a
compound radical like NO; to experience frictional resistance
in the same manner as a single atom like Cl, and as to the
hydrogen compounds they form a class by themselves with
respect to many physical properties. It will be as well to
show the amount of departure in these cases in the following
Table :-—
U. q. u—4. k. K (eale.).
ASS ists’ pss 56 26 30 327 134
Teg) ere anaes 50 16 34 327 142
RG 2? earee snes 42 11 dl 324 136
KEN 53 72. as 47 22 25 98 123
NINO N 8 oat se 36 19 17 82 LOD
INIEMINO Do Buccs 475 25°5 22 98 L116
iis L(G) ie areas 35°95 22-2 13 104 97
Kohlrausch has pointed out that there is some difticulty in
determining the true connexion between ionic velocities and
conductivities in the case of the bibasic acids SO, and COs, so
that we must leave them out of the count for the present.
292 Mr. William Sutherland on the
18. An Attempt to Determine the Velocity of Light through
the substance of the water-molecule.-—In spite of the excep-
tions, the relation demonstrated in Table XX XIX. is suffi-
ciently striking. To explain it, let us replace g by its value
(N—1)U ; then, in interpreting the expression u—(N—1)U
as occurring in our expression for the conductivity of a solu-
tion, there are two methods of procedure: first, we can assume
that w—U, the free or unoccupied part of the domain, is the
most likely to occur, in which case N=2; second, that w—cU
occurs in the expression for conductivity, and that ¢ happens
to have the same value as N —1, on which supposition it would
be desirable to determine N. .At present I know of only one
way of attempting to find N or v/V, the ratio of the velocity
of light through free ether to its velocity through the matter
of an atom, namely by means of Fizeau’s experiment, repeated
by Michelson and Morley, on the fraction of its motion com-
municated by flowing water to light passing through it.
Exactly in the manner of my paper (Phil. Mag. Feb. 1889,
p- 148) we can estimate the effect of the motion of matter on
the light passing through it. Let s be the distance travelled
by light in water flowing through the ether at rest with
a velocity 6 in the same direction as the light, v the mean
velocity of light through the flowing water, v' the mean
velocity through still water, v its velocity through free ether,
V through a molecule of water, J the mean distance through
a molecule, and a its mean sectional area ; then the total loss
of time experienced by a wave of unit area of front or a tube
of parallel rays, or, briefly, a ray of unit section in passing
through the matter-strewn path s instead of a clear path in free
zether, will be equal to its loss in a molecule multiplied by the
number of molecules passed through in the path. This
number, when the matter is at rest, is proportional to s, to a,
and to p/M, or it varies as sap/M ; but when the matter is in
motion it is reduced in the ratio 1—6/v": 1. The loss of time
in each molecule is found thus: J/V is the time taken to pass
through a molecule, and in this time the molecule moves
a distauce 1/6/V and the unit wave-front moves a distance
(1 + 6/V), which in free ether would take a time /(1+6/V)/v ;
so that the loss of time in a molecule is 1/V—/(1+8/V)/2.
Hence, the total loss of time in the path s may be written
)
ksalp (1 Lea 1 3)
abe) ge
But the loss of time is also s/v!—s/v; equating the two ex-
Laws of Molecular Force. 293
pressions and putting M/p=u and al=U, v/v"=n", o/ V=N
we get |
u(n!’—1) =U(N-1 _ “x )(1— en
as k& is equal to 1, seeing that if 6=0 and U=w, then N must
be equalto x. This equation is the companion to that for
still matter, namely,
u(n—1)=U(N—1).
But to allow for deformation of the wave-front in passing
through molecules it was shown (Phil. Mag. Feb. 1889,
p- 150) that this first approximation might be altered to the
form
u(n—1)=U(N—1) +09,
where ¢ is a constant, and this form was verified, so that we
may write
u(n!!—1) =U(N-1- °N) de ° nt + cp
5S & N Of,
neglecting the term in 6? ;
; ws N
as u(nl!—n) = —" U(N—1)(x oa +n")
een UCN!) nee ON
pee ed N"
i os Ou(n—)) in ay) +n}.
Now
Mice Ted =U; vd xO
MUR ah Galareaiue approximately,
where z is the fraction of the water’s velocity imparted to the
velocity v’ to change it to v’. Fizeau (Ann. de Ch. et de Phys.
sér. 3, t. lvii.) found a value °5 for 2, while Michelson and Morley
(Amer. Journ. Se. ser. 3, vol. cxxxi.), ina more extended and
accurate series of experiments, found a value e="43+:02,
which we will adopt. U(N—1)is equal to w(n—1) measured
in the vapour of water, for which Lorenz (Wied. Ann. xi.)
gives the value 5°6; the value for water at 20° C., according
to his data is 6, and n is 1:333, which may also be taken as the
value for n” where it occurs ; all these values being substituted
in the equation
ING) edt odie 4») 6 (i= ht)
Noten, Und), -
) i!
294 Mr. William Sutherland on the
give the value N=9. Hence the velocity of light through
the water molecule appears to be one ninth of that through
free ether. But before we could ascribe any degree of
accuracy to this estimate we should need to be surer of the
value of 2, whose measurement is attended with great experi-
mental difficulties. It is much to be desired that we had
similar measurements for other bodies than water, both liquid
and solid, to permit of other estimates of N, so as to see if it
is the same for all compound bodies, and also to decide be-
tween the theory here sketched and Fresnel’s hypothesis,
that matter carries its own excess of ether with it, so that
a= (n?—1)/n?, which in the case of water is ‘437, in excellent
agreement with Michelson and Morley’s experimental number ;
but one such agreement is not sufficient to establish an
hypothesis founded on such artificial grounds. However, if
N=9 then N—1=8, and we have the electrical specific mole-
cular conductivity k=68+2°2 (u—8U). Itis only a coinci-
dence that this agrees so exactly in form with Clausius’s
calculation that the number of encounters experienced per
second by a molecule of volume U moving amongst a number
of others of volume U is greater than that experienced by an
ideal particle moving under the same circumstances in the
ratio w:u—8U. Further experiment must elucidate the
subject-matter of these speculations.
19. Suggested relation between the change in the volume of an
atom on combination and the change in its chemical energy.
—Returning to the idea that the dynic equivalent furnishes
a measure of the volume of its atom, we can get a suggestive
glimpse into the relation between the volume of an atom and
its chemical energy. Kundt has recently (Phil. Mag. July
1888) shown that the velocities of light through the metals
(uncombined) are as their electrical conductivities, being in
the case of silver, gold, and copper greater than through free
ether, and as in this case both n—1 and N—1 are negative,
we see that (n—1)u or (N—1)U for the metals changes
greatly when the metals pass from the combined to the free
state. Now this is in strong contrast to the behaviour of the
non-metallic elements, which have been shown in the case of
O, N, C, 8, P, Cl, Br, and I to possess nearly the same values
of (n—1)u in the combined and free states, and the same may
perhaps be said of H. Again, in contrast to this approximate
inalterability of (n—1)w for these non-metals we have the
fact, already pointed out, that the dynic equivalents of H, O,
and N are much smaller in the free than the combined state.
If, then, the dynic equivalents give a measure of the volumes
Laws of Molecular Foree. 295
of the atoms in both states, we must consider the volumes of
free H, O, and N to be smaller than when they are combined,
the change of volume corresponding to the change of energy
on combination. [f this is true, then the elasticity and density
of the non-metallic atoms (or the equivalents of these proper-
ties in the electromagnetic or any other theory of light) are
so related that although the density changes (N—1)U re-
mains constant, whereas in the metallic atoms the relation
between density and elasticity must be quite different, because,
as we have seen, (N —1) U actually changes sign in some cases.
It would be possible to determine approximate values for
the dynic equivalents of the uncombined metals from Quincke’s
data for the surface-tension of melted metals, and also to get
some light on the constitution of salts from his measurements
of the surface-tension of melted salts, but these would be
most appropriately discussed in connexion with a general
study of the elastic properties of solids. I have, however,
satisfied myself that the dynic equivalents of the uncombined
metals are different from their values in the combined state.
To show the existence of an intimate relation between dynic
equivalents and chemical energy we can enumerate the follow-
ing propositions :—That in the great majority of inorganic
compounds the evolution of heat accompanying the passage
of an atom from the uncombined to the combined state is
almost independent of the nature of the atoms it combines
with, similarly the change of dynic equivalent of an atom on
combination is almost independent of the nature of the atom
it combines with ; that in organic compounds with the excep-
tion of the simpler typical forms the same proposition as this
applies both as regards heat and dynic equivalent.
These general remarks are intended to indicate the most
hopeful direction for the continuation of these researches to
open up new fields ; and yet in old fields there is abundance
of scope for the application ef the law of molecular force
towards the acquisition of a knowledge of the structure of
molecules, in the elasticity of solids, in the viscosity of gases
and of liquids, in the kinetics of solutions, and many kindred
subjects.
Melbourne, February 1890.
i996]
XXVIII. The Fusion-Constants of Igneous Rock. — Part III.
The Thermal Capacity of Igneous Rock, considered in its
Bearing on the Relation of Melting-point to Pressure. By
CaRL BarRus*.
[Plate VI.]
1. FNTRODUCTORY.—tThe present experiments are in
series with the volume-measurements of my last paper,
and the same typical diabase was operated upon. Since it is
my chief purpose to study the fusion behaviour of silicates,
more particularly the relation of melting-point to pressure,
the observations are restricted to a temperature-intervyal
(700° to 1400°) of a few hundred degrees on both sides of
the region of fusiont (§ 11).
2. Literature—LHxperiments similar to the present, but
made with basalt, were published quite recentlyt by Profs.
Roberts-Austen and Riicker§. The irregularities obtained
by these gentlemen with different methods of treatment
(heating in an oxidizing or a reducing atmosphere, repeated
heating, sudden cooling), the anomalously large specific heat
between 750° and 880°, where basalt is certainly solid, and the
absence of true evidences of latent heat||, contrast strangely
with the uniformly normal behaviour occurring throughout
my own results. Basalt is chemically and lithologically so
near akin to diabase (particularly after melting) that I anti-
cipated a close physical similarity in the two cases. Unfor-
tunately the account given of the basalt work is meagre.
Detailed comparisons are therefore impossible.
The elaborate measurements of Hhrhardt (1885) and of
Pionchon (1886-7) are less closely related to the present work.
APPARATUS.
3. The Rock to be tested About 30 grammes of diabase
were fused in the small platinum crucible together with which
they were to be dropped into the calorimeter. Two such
charged crucibles were in hand, to be used alternately. ‘The
molten magma, after sudden cooling, shows a smooth, appa-
rently unfissured surface, glossy and greenish black. After
* Communicated by the Author.
T The geological account of the present work is begun by Mr. Clarence
King, in the January number of the American Journal.
{ This was written some time ago. See American Journal, December
1891 and January 1892, A forthcoming Bulletin, No. 96, U.S. Geological
Survey, contains the work in full,
§ Roberts-Austen and Ricker: this Magazine, xxxii. p. 855(1891).
| Supposing basalt to solidify (§ 18) below 1200°,
The Fusion Constants of Igneous Rock. 297
drying and weighing, the mass is often found to have gained
5 per cent. in weight. I was at first inclined to believe that
this was attributable to water chemically absorbed by the
viscous magma; but the water is only mechanically retained,
for it passes off after 24 hours of exposure to the atmosphere,
or by drying at 200° C. for, say, 30 minutes. Hence I
weighed my crucibles at the beginning of each measurement,
having previously dried them at 200°. The solid glass, sud-
denly cooled from red heat, soon shows a rough and tissured
surface, and its colour changes from black to brown, possibly
from the oxidation of proto- to sesquisalt of iron, possibly from
mere changes in the optical character of the surface (§ 2).
Throughout the course of the work the charge of the
crucibles was neither changed nor replenished.
4. Thermal Capacty of Platinum.—Data sufficient for the
computation of the heat given out by the crucibles were
published in 1877 by Violle*, whose datum for the high
temperature (t) specific heat of platinum is ‘0317 + °000012¢.
Hence the increase of thermal capacity from zero Centigrade
to the same temperature is ¢(°0317 + -000006¢), which is the
allowance to be made per gramme of platinum crucible.
5. Lurnace.—Inasmuch as heat is rapidly radiated from the
white-hot slag, iit is necessary to transfer the crucible from
the furnace into the calorimeter swiftly. I discarded trap-
door, false bottom, and other arrangements for this purpose,
because the mechanism clogs the furnace, interferes with con-
stant temperature, and is too liable to get out of order. The
plan adopted is shown in figs. 1 and 2 (Plate VI.), in sectional
elevation and plan. ‘The body of the furnace consists of two
similar but independent bottomed half-cylinders, A A and
BB, of fire-clay properly jacketed, which come apart along
the vertical plane cece. The lid, LL, however, is a
single piece, and fixed in position by an adjustable arm (not
shown). Hach of the halves of the furnace is protected by a
thick coating of asbestos, CC, DD, and by a rigid case of
iron, HH, FF. Set ser ews, 9999, pass through the edges
of this in sucha way as to hold the fire-clay and asbestos in
place. The horizontal base or plate of the casing H F is bent
partially around the two iron slides, GG, along which the
two halves of the furnace may therefore be ‘moved at pleasure
while the lid is stationary ; as is also the blast-burner, H,
clamped on the outside (not shown), and entering the furnace
by a hole left for that purpose.
* Violle’s calorimetric work will be found in C. &. Ixxxv. p. 5483 (1877),
Ixxxvii. p. 981 (1878), Ixxxix. p. 702 (1879); Phil. Mag. [4] p. 818 (1877)
Phil. Mag. 8. 5. Vol. 35. No. 214. March 1893. X
298 - Mr. Carl Barus on the Fusion
The charged crucible is shown at K (figs. 1, 2, and 3), and
is held in position by two crutch-shaped radial arms, N,N, of
fire-clay, the cylindrical shafts of which fit the iron tubes
P, P, snugly, and are actuated by two screws, R, R. More-
over P, P are covered with asbestos (not shown), and thus
subserve the purpose of handles, by grasping which the two
halves of the furnace may be rapidly jerked apart. It is by
this means that the crucible is suddenly dropped out of the
furnace into the calorimeter immediately below (not shown).
Care must be taken to have the arms N, N free from slag. ~
6. Temperature.—As in the former work, the temperature
of the furnace is regulated by forcing the same quantity of
air swiftly through it at all times, but lading this air with
more or less illuminating-gas, supplied by a graduated stop-
cock. The amount of gas necessary in any case is determined
by trial, and observations are never to be taken except after 19
or 20 minutes’ waiting, when the distribution of temperature
is found to be nearly stationary. Nevertheless the tempera-
ture of the crucible is never quite constant from point to
‘point. I therefore measured this datum at three levels—near
the bottom, the middle, and the top of the charge, after the
stationary thermal distribution had set in (see Tables, § 10).
For this purpose the fire-clay insulator*, ¢¢, of the thermo-
couple, ab, passing through a hole in the lid, is adjustable
along the vertical. Before dropping the crucibie the thermo-
couple is withdrawn from the charge and suspended above it.
The cold junction is submerged in petroleum and measure-
ments made by the zero method. . -
When the charge is solid, a small platinum tube previously
sunk axially into the mass (see fig. 3) enables the observer to
make the three measurements for temperature as before. In
my later work I also encased the insulator of the thermocouple
in a platinum tube closed below (see fig. 1) when making
these measurements for the molten charge. Slag being a
good conductor at high temperatures, hydroelectric distor-
tions of the thermoelectric data may not otherwise be absent.
I state, in conclusion, that when constancy of temperature
is approached the hole in the lid is closed with asbestos, and
the products of combustion escape by the narrow seam in the
side of the furnace, through which, moreover, crucible and
appurtenances are partially visible.
* These are cylindrical stems, 0°5 centim. thick, 25 centim. long, with
two parallel canals running from end to end, through which the platinum
ee are threaded. Cf. Bulletin U.S. Geolog. Survey, No. 54, p- 95
Constants of Igneous Rock. — 299
7. Calorimeter.—A hollow cylindrical box, provided witha
hollow hinged lid, through both of which a current of cold
water at constant temperature continually circulated, sur-
rounded the calorimeter on all sides. Thus the temperature
of the environment was sharply given, and the correction for
cooling could be found and applied with accuracy. :
The calorimeter was a vessel of thin tinned sheet iron,
28 centim. long, 8 centim. in diameter, having a water-value
of 19 gramme-calories, and holding a charge of about 1200
grammes of water. The inside of the vessel was provided with
a fixed helical strip running nearly from top to bottom, and
was supported on a hard rubber stem. This could be actuated
on the outside of the outer case from below, and served as
a vertical axle around which the calorimeter could be rotated.
In this way the water within the vessel was churned, and
three small hard rubber rowels near the top gave steadiness
to the rotation. I pass the description of this apparatus
rapidly here, but shall recur to it in connexion with other.
calorimetric work.
The box or outer vessel of the calorimeter, with its pro-
jecting stem, was movable on a small tramway, the. tracks of
which lay at right angles to the slides G, G (figs. 1 and 2).
Thus at the proper time the lid of the box was opened and the
calorimeter rolled directly under the furnace. After receiving
the crucible the calorimeter was again rolled away and the box
closed, whereupon the temperature-measurements were made
by a sensitive thermometer inserted through a hole in the lid.
Were I to continue work like the present I should make the
crucible bullet-shaped, and provided with a permanent central
tube much like fig. 8. The splashing of water by the drop-
ping crucible (an annoyance which is sometimes serious)
would then be to a great extent obviated.
RESULTS.
8. Method of Work.—While waiting for stationary furnace
temperature I made the initial measurements for the cooling
of the calorimeter in time series. Knowing, therefore, the
time at which the body was dropped I also knew the tempe-
rature of the water into which it was dropped, accurately:
Similarly the three measurements for the temperature of the
charge had just before this been made in time series.
The experiments showed that ten minutes after submer-
gence the crucible and charge might safely be considered
cold, for the maximum temperature of the calorimeter was
X 2
300 Mr. Carl Barus on the Fusion
reached after 5 minutes. Hence the time from 10 to 15
minutes was available for making the final measurements for
cooling ; knowing the extremes, I found the intermediate
rates in accordance with the law of cooling. Thus, while the
calorimeter was being constantly stirred, its temperature was
measured at the end of each minute. Hence I knew the mean
excess of its temperature above its environment during the
course of every minute, and was able to add the corresponding
allowance for elation and evaporation at once. How im-
portant this correction is the Tables (§ 10) fully show. The
only drawback against sharp values is the lag error of the
thermometer ; but this is eliminated in a long series.
I have bated that both the calorimeter aa the eaeible.
were weighed before and after each measurement. The latter
data were taken.
9. Arrangement of the Tables——The two crucibles (§ 3)
and tubes (fig. 3) are designated I. and II. In all cases m
is the mass of the charge, M the calorimetric value of the
calorimeter (corrected for temperature), 7 the temperature of
the environment. © is the temperature at the top, the
middle, and the bottom of the charge at the time of submer-
gence. The mean value is also given. The temperature of
the calorimeter at the time specified is given under @, and a
parallel column shows the correction of @ for radiation.
Finally, the computed thermal capacity of the platinum cru-
cible and appurtenances (correction fh), and the thermal
capacity * h of the charge computed up to each of the con-
secutive times, are found in the last columns. A few obvious
remarks follow. Note that h reaches its true (constant) value
in proportion as the body is cold.
To avoid prolixity I have only given full examples of the
data here defined at the head of each table. The remainder
is abbreviated.
10. Tables——In the data of the first series (Table I.) only
one value of ® is in hand for the liquid state. Moreover the
construction of the furnace was somewhat faulty, not being
flat-bottomed. Hence these results are of inferior accuracy
as compared with Series II. (Table I1.), which are the best
obtained.
* The constant / is really the increase of thermal capacity above zero
degrees Centigrade.
Constants of Igneous Rock.
301
Tasie I.—Thermal Capacity of Diabase. First Series.
Platinum crucible, I., 11:169 g.; Platinum tube, L[., -985 g.
Platinum crucible, II., 11°271 g.; Platinum tube, IL., -654 g.
. | |
: | Mean 6. 'Correc- | Correc-
ae meeetme., | OQ... | ME) 6. tion tion h.
; | | ho, Ue | re h.
i———-| | ee |: ape? ee ee on eee ance Sees nee |
| °C. | Minutes.; °C. | 2. °C. | g.-cal. | g.-cal. |
eS ‘Dai esta NBO See ORAS Bape Ge daey: eases Immersion |
. ee 12022. | 22:30) +02) | 179 | 967 | Taquid. |
2 ih oa 33:36 g.| 25:20) -06 355 |
3 | | 25°50) -11 367
| 5 | 25°58| -20 372 | |
| 8 | 2540| -33 370 an |
11 25:25| 46 370 |
14 | 25:12] +60 370
iy Cee ee TBOGeHN5- OO ly eae || Sela Immersion |
ernie) 2.2... 1145 g. | 36-04} 1:10 | 166 | 364 | Liquid.
MMSE reir | ses... 33°75 g.
Bagh ge |. 1378° | 99-16] ...... Ce REA ee Tare ceou
| pie | 1202 g. | 30-97] 1:11 | 20°77 | 385] Liquid.
Peas 29°32 g.
| I} ia 1397 PCIe oe eee ae ee ae eeeiereion
| La EAE tls Bios 1196 g. | 2440; 69 18-0 373 Liquid.
OEE eg ere 32°22 g.
a Se. eee eee yee) Dice ey mean es. iitverten
fee | Ales, 1196 ¢g. | 29-98} 1:10 | 17-1 358 | Liquid.
Bosse 29°16 ¢.
| sel ee O | 1199 | 1166° PAs NPAs tail a eee |) See Immersion
14 1163 | 1195 ¢. | 22-98) -81 | 167 311 | Solid.
1138 | 82:22 ¢.
ete O- | L 100) | LOT8S | | NOTIG | Si ee Immersion
14 1074 | 1196 g. | 27:25] -74 | 164 | 263] Solid.
1060 | 29:16 ¢.
—- ce |S oe ———$————— —_—_—— =——_——___| __.___ Se
ete | tt 0 LOR | PLOOWC 4 SOh = ees ee emia ah Immersion
iu 998 | 1196 ¢. | 21°31] -47 | 139 | 242/ Solid,
| 983 | 32-23 ¢.
II. | 11 0 1035 | 1025° OG) SOONER De erate eet hee Immersion
14 1025 | 1195¢. | 25:55) -73 | 15:5 | 253] Solid.
1015 | 29:16 ¢. |
oe | ee ee | ee ee | ee
ef. 0 889 880° TGAHOUM Ah eeu a lvere meee Nt g eet ae Immersion
| 11 880 | 1198 g. | 21:59} 41 | 120 | 204] Solid |
872 | 32:24 pg.
Se eee eee Cea Eee
iC a ) B27 | WSO9Cm 0-07 ues] one Lt eee Immersion |
14 | 827 | 1192g. | 2439) 65 | 121 191 | Solid.
hee) | 833 | 29°16 g.| | |
{ | ; i |
302
Mr. Carl Barus on the Fusion
TasLe [1.—Thermal Capacity of Diabase. Second Series.
— =
10
10 |
PALER
10
997
995
987
1260
1251
1243
| 1354
1333
948
949
| 1364
| 1854 —
| 1339
877
873
870
| 1176
1164
1158
1215
1191
| 1186
782
780
780
| 1204
| -1195°
| 1183
Mean 0.
1319
| 954
1
993°
26:27 g.
i
M.
Mm.
1251°
1189 g.
26°39 g.
1192 ¢.
32°22 g.
1251°
1190 g.
26°07 g. |
1334°
1190 ¢. |
948°
1186 g.
32°22 g.
1352? >, |
1194 g. |
26°05 g. |
873°
| 1191 g. |
32°20 g. |
11GG2 |
LISis. |
25°97 g.
197°
1192 ¢.
25°95 g.
781°
1189 g.
3219 g.
1194°
1195 g.
25°90 g.
(mecca
1
| Correc-| Correc-. |
Time. 0. tion tion | Coe =
6. hee |
Minutes. °C. | °C. | g.-cal. | g-cal. : yh
fe) 18°94). o.0) =e Immersion
1 24-60; -04 206 | 236 Liquid.
2 26:°05| -10 305
3 26:52) -16 329 |
9) 26:61| -30 339
8. | 2645] -50 341
11 | 2625) -69 au) Gyo
14 26:08; -88 341
OF AAT. cence ee =. Immersion
igi 20°61) -22 13:38 | 2383) Solid.
0 1934) \.c2%.) | 22 eee TS See:
4, 2649) _. 80 20°38 | 842°5| Liquid.
0 13°78) <2... | 2.28 Immersion
14 | 21°79| °84. | 224 | Sirah Ss nguid:
0 | 20-24) ...... eee Immersion |
14 | 2581, -94 | 18:0 | 2266) Solid.
hues ae! Lose FV ee Sess
0 AAS) eee [gees tae | Immersion
14 24:82| °87 | 23:1 (| 3660) aiid:
0.) 14°83 sce ee eee Immersion
14 .| 20:13|- 46. | 2:9 9202 Salad:
Os] 17-40, vezi | eae ee: | Immersion |
14 | 24-21) 77 | 19:2 | 3095) Liquid.
0 | (4488) <2) hee Immersion
ea | 2113; 62 199 | 3185; Liquid.
0 19°36 Petes. Immersion
yaa Be 23:61) -94 104 | 179-7 Solid.
pot tl et : nod
0. 114:54|" cect | eee Immersion
145 | 21:22) -66 19:99 | 3179 Liguid.
|
|
Constants of Igneous Rock. — 303
Table LI. (contznued).
| Cone Mean 9. | Corree-| Correc-
N pins é. M. Time. Q. tion LOMey yas
fae |
Mm. | 0
ser OC, | Minutes.| °C. °C. | g-cal. | g.-cal.
era ibis | Li71° Y) TO S8i ee eee a AOE aot Immersion
BETO |) 1192 ¢- 14 27°30 2 VAD | 16°7 | 301°6 Solid.
1166 | 32:20 g. |
E |) 11 | 1106 | 1096°-| 0 - | 16-28! ...... | Behe Immersion
1094 | 1195¢: 14 | 23°24 “OL Lar 268°2 Solid.
1088 | 32-21 g. | |
mene 95) 4ge 0, TSF) | ea... Immersion
1244] 1191v.| 14 | 2655; -89 | 21-1 | 3888] Liquid.
1238 | 25°49 g.
MINIS | 1216201 0 81 13°67) ee ee Seasee Immersion
1216 | 1188¢.| 14 - | 21-60| “69 |-17-7 | 3303| Liquid.
/ 1202 | 29-43 ¢.
ee ae = pe a, es aah CEES
He ebie 1924)" 1215° 0 oS a 0 Wa C3, nega Peon See Ls Immersion
1216 | 1185 ¢. 14 26°27 ‘95 20°4 326°6 Liquid.
1205 | 25°57 g.
For brevity the later observations were averaged per
3 minutes, and under / the mean value for the last 11 minutes
is usually given.
In Series I. the increase of temperature from top to bottom of
the crucible is as large as 60° at 1200°, usually much smaller,
however, and falling off pretty regularly to 6° at 829°. In
Series II. the corresponding mean difference is about 25° at
1300°, 14° at 1000°, 10° at 800°. ‘The errors thus involved
cannot be greater than 2 per cent. in the extreme case ; but
since the distribution of temperature 1s measured, it is probably
negligible except at very high temperatures. I am inclined
to infer that the greater constancy of the solid distribution
as compared with the liquid is due to greater thermal con-
ductivity in the former case (solid), convection being neces-
sarily absent in both.
Considering the observational work as a whole, the data
are satisfactory, seeing that an error of 0°1°C. in the calori-
metric temperatures, initial or final, must distort the results
at least 1 per cent. But the real source of error is probably
accidental, and is encountered when the hot body falls through
the surface of the cold water.
INFERENCES.
11. Digest and Charts—In Tables III. and IV. I have
summarized the chief results on a seale of temperature. The
304
Mr. Carl Barus on the Fusion
results of the latter (Series II.) are graphically shown in the
chart (fig. 4), in which thermal capacity in gramme-calories
is constructed as a function of temperature *.
are drawn through the points, showing the mean specific
heats for the intervals of observations, solid and liquid. The
letter a marks the region of fusion.
TasiE III.—Thermal Capacity of Diabase.
Mean specific heat, solid, 800° to i100°
liquid, 1200° to 1400° .
Latent heat of fusion, at 1200°, 24 g.-cal.; at 1100°, 16 g.-cal.
99
Solid.
‘romp Teena | 2
| 829 | 191. |} 1025
| 80 | 204 || 1078
1001 | 242 | H1166
| |
Digest, of. § 15.
| Thermal
‘| capacity.
253
263
all
Straight lines
“304.
350.
Series I.
Liquid.
Thermal
‘| capacity.
358
Taste [V.—Thermal Capacity of Diabase.
Digest, ef. § 15.
Mean specific heat, solid, 800° to 1100° f
liquid, 1100° to 1400° .
Latent hea of fusion, at 1200°, 24 g.-cal.; at 1100°, 16 ¢.-cal.
29
Solid.
Temp. ee Temp.
oO te)
781 180 1096
873 202 (i171
948 227
993 238
|
|
Thermal
capacity.
Thermal
‘| capacity.
———
370
385
|
|
|
Series II.
290.
360.
| 1352
Liquid.
| |
Temp,| capacity. | T%P+ capacity
evinaeiel. - é
1166 | 310 || 1248] 339
1194 | 318 || 1251 | 340
1197] 319 || 1251] 342
1215 | 327 || 1334] 377
1218 | 330 367
* The corresponding chart for Table III. is almost identical with this.
+ Incipient fusion (?) at the base of the crucible.
Constants of Igneous Rock. 305
In both the tables, III. and IV., the solid points lie on lines
which, if reasonably curved, would be nicely tangent to an
initial specific heat of about 0°2 at °C. The grouping, in
other words, is so regular as to exclude the probability of
anomalous features, either in the observed or the unobserved
parts of the loci. The solid point near a (fig. 4, a similar point
occurs in Table III.) alone lies markedly above the curve ; but
inasmuch as in my volume work | found solidification to set in
at 1100°, it is altogether probable that the occurrence at 1170°
is incipient fusion (¢ 13).
The regularity of the liquid loci (Tables III. and IV.) is
slightly less favourable; but the discrepancies which occur
are above 1300°, and obviously accidental (§ 10, end).
12. Specific Heat.—As regards the mean specific heats be-
tween 800° and 1100° in Tables III. and IV., it will be seen
that the intermediate datum would satisfy both groups of
points about as well as the individual data given. A tracing
made of the first group practically covers the other. The
same remarks may be made for the liquid state. I have not
attempted any elaborate reductions, since the equations of
the necessarily curved loci would have to be arbitrarily
chosen, and since values for specific heat are of no immediate
bearing on the present inquiry.
13. Hysteresis.—Recurring to the suggestion of the pre-
ceding paragraph, it appears that the fusion behaviour of rocks
must be accompanied by hysteresis* of the same nature as
that which I observed with naphthalene and other substances:
for, whereas in my volume work with diabase I was able to
cool the rock down to 1095° without solidifying it, evidences
of fusion (at a, figs. 4 and 5) do not occur in the present
work until 1170° is reached. The magnitude of the lag is
thus of the order of (say) 50°, and its pressure-equivalent
may be estimated as 500 atmospheres.
14. Latent Heat.—In virtue of the fact that the (upper) end
of the solid locus (Tables II]. and IV.) may be carried so
near the beginning of the liquid locus, the datum for latent
heat is determinable with some accuracy, in spite of its sur-
prisingly small (relative) value. Difficulties, however, present
themselves in the determination of the true melting-point, a
datum which can only be sharply defined when the tempera-
ture of the crucible is quite constant throughout. I have,
therefore, considered it preferable to state the conditions at
1200° and at 1100°, the former being nearer fusion and the
latter very near solidification. The latent heats for these
* Am, Journal, xlil. p. 140 (1891); of ibid., xxxvili. p. 408 (1889).
306 The Fusion Constants of Igneous Rock.
temperatures are 24 and 16 respectively. The coincidence of
results in both of the independent constructions (Tables ILL.
IV.) is in a measure accidental. :
15. The Relation of Melting-point to Pressure.—The first and
second laws of thermodynamics leid to the equivalent of
James Thomson’s fusion equation, which in the notation of
Clausius* is dT/dp=T(o—7)/Hr’ ; where T is the absolute
melting-point, c—7 the difference of specific volumes solid
and liquid at T, 7’ the latent heat of fusion, and EK Joule’s.
equivalent. *
Combining the present Series I. of thermal measurements
with the former Series III. of volume measurements, I ob-
tain at 1200°, since T= 1470°, co—r="0394/2°72 (where 2°72,
is the density of the solid magma at zero), and 7’=24. |
dT
== == (ile
ak
and-at 1100°, since T=1370°, c—rT='0385/2°72, and 7 =16,
—,
—— 7 oe
(a 1100
Similarly, combining the present (heat) Series IJ. with the
former (volume) Series IV., at 1200°, since o—T='0352/2°72,
and 7’ = 24,
dT
—— =°()19 ;
dp pe
and at 1100°, since o —7T=°0341/2°72, and te 16,
([) ~-026
dp 1100
Hence the probable silicate valuet of dT/dp falls within the
margin (‘020 to ‘036) of corresponding data for organic sub-
stances (wax, spermaceti, paraffin, naphthalene, thymol). I
may, therefore, justifiably infer that the relation of melting-
point to pressure in case of the normal type of fusion is
nearly constant irrespective of the substance operated on, and
in spite of the enormous differences of thermal expansibility
and (probably) of compressibility. And in the measure in
which this is nearly true on passing from the carbon com-
pounds to the thoroughly different silicon compounds, is it
* Warmetheorre, i. p. 172 (1876). 2
+ For reasons to be stated elsewhere, 6m =a+'025p (where On is the
melting-point in °C. at the pressure p atmospheres) will be assumed in
making geological application of the above data.
Notices respecting New Books. 307
more probably true for the same substance changed only as
to temperature and pressure. In other words, the relation
of melting-point to pressure is presumably linear. « In my
work on the continuity of solid and liquid * these relations
are corroborated for naphthalene within an interval of 2000
atmospheres.
XXIX. Notices respecting New Bowes.
Treatise on Thermodynamics. By Purer ALEXANDmR, M.A.
London: Longmans, Green, and Co. 1892.
rom the preface it appears that this book is ambitious: it
claims to have elevated the science of Thermodynamics into
an organic unity from being a mere collection of detached propo-
sitions, to exhibit the thermodynamic relations as the outcome of
physical, as opposed to mathematical, considerations, to have
cleared away the fog that has enw rapped the subject of irreversi-
bility, and, by an enlarged definition of entropy, to have opened
up a mode of dealing with this subject, and, finally, to have
dissipated the haziness that has overlain the subjects of Motivity
and Dissipation of Energy.
The idea is to be deprecated, however, that, as hitherto treated,
the science of Thermodynamics has consisted of any more detached
propositions than the two, representing the two laws, which are
the necessary basis of this as of every other treatise on the sub-
ject, viz. that of the conservation of energy and that of the perfec-
tion of a reversible engine or its equivalent, together with their
consequences ; and indeed a set of relations, which are the expres-
sions in different forms of the same fact and which are all deducible
from each other by simple transformations, does not constitute
different but identical propositions. What the author has really
done is to express the two laws, 7. e. practically the values of the
dynamical equivalent and of Carnot’s function, in a manner even
more general than that worked out (though not otherwise employed)
by Clausius, viz. in terms of two general variables with any scale
of temperature whatever, and then from these expressions to deduce
particular thermodynamic relations by the substitution of particular
variables : and it is these relations, which are necessarily identical,
that constitute the “ detached propositions” above mentioned.
Eyen if this method does not really tend to promote the organic
unity of the science, it has without doubt its advantages and, by
reason of its generality, should find place in some form or other
in every formal text-book : it is certainly convenient if only as a
simple mode of demonstrating certain identities and even of bringing
to light identities, unimportant enough it may be, that might
otherwise escape recognition. At the same time it is unlikely that
general resort will be made to it for obtaining the really important
* Am. Journ, xlii p, 144 (1891).
303 Notices respecting New Books.
forms of the thermodynamic relations, each of which is patent on a
glance at the corresponding infinitesimal cycle.
In his investigation of these general expressions, the author
prefers not to avail himself directly of the fact that infinitesimal
changes of entropy and intrinsic energy are perfect differentials,
and so, according to Lord Kelvin’s simple plan, to apply the corre-
sponding criteria forthwith, this method savouring of mathematics
only: he follows Clausius’ original lead instead, without, however,
Clausius’ elaboration, and, taking an infinitesimal cycle composed
of two pairs of thermal lines of any different types, he sums up the
heat absorbed all round the cycle and also the changes of entropy,
and equates the former sum to the area of the cycle and the latter
to zero, this lengthier process being chosen as being of a more
distinctly physical character than the other. In the second of
these calculations the criterion of a perfect differential 1s of course
necessarily arrived at, since the process of determining the eri-
terion is essentially that of the method pursued ; attention might
therefcre with advantage have been called to the mathematical
character of this resulting equation, more especially as after
reading Chap. XV., wherein is given Lord Kelvin’s method, a
student will not be likely to have recourse to the other. Advan-
tageous, too, would be the omission in this calculation of the signs
of integration, which are finally discarded as quite unnecessary
and are not even introduced into the other calculation on p. 42.
With respect to irreversibility, itis pointed out that there may
be processes which, though not actually reversible, are, so far as the
working substance is concerned, in one direction equivalent to pro-
cesses that are reversible, in which case the changes of entropy
that occur in the working substance itself during such processes
(termed conditionally irreversible, in contradistinction to zintrinsi-
cally irreversible processes which have no such equivalents) depend
only on its initial and final states. But we are not really helped
by these considerations—which are not new—since it is the actual
sources &c. and the actual variations of entropy with which we
are really concerned.
The proposed enlargement of the definition of entropy which is
to help with the treatment of irreversibility greatly needs defence.
It is ushered in with an objection to the definition of the entropy
of a body or system as the sum of the entropies of its parts,
‘‘ which seems to me as unwarrantable as to define the temperature
of a body or system as the sum of the temperatures of its parts,” so
that to speak of entropy per unit mass “‘seems to me as un-
warrantable as to speak of temperature per unit mass”; though no
reason whatever is given or even hinted for likening entropy to
temperature rather than to such another physical property as
energy or volume. Such a definition of entropy is then desired
as will make the entropy of any system whatever invariable when
no heat passes into or out of it; and the author considers that he
has obtained such a definition—which satisfies also his previous
objection—in the formula X.rmg/S.7m, where m is the mass
Notices respecting New Books. 309
of a portion of the system of which the entropy and absolute
temperature are ¢ and r.
Assuming, however, the formula for a single mass, consider a
system of two masses m,, m, of the same substance with entropies
¢,, ¢, and at absolute temperatures 7,,7, respectively; and let
these masses be respectively expanded and compressed adiabati-
cally to the temperature - and then respectively compressed and
expanded isothermally to the pressure p: the system is now in
equilibrium, and, if vis taken such that no energy is lost or gained
by the system and that the heat lost by the one mass is equal
to that gained by the other, it is in that state of equilibrium
which the system would finally attain in isolation. If, then, ¢ is
the final entropy of the system, the heats lost and gained are
m,t (¢,—¢) and m,7 (¢—@,), whence ¢=(m,¢,+m,9,) /(m,+m,),
which does not satisfy the proposed formula except for r,=r, or
ce ao, being thus considered a debatable subject, it is surpri-
sing to see it postulated in the Introduction as an evident property
of a substance and to find it treated as such without debate or
explanation till the last chapter. In Maxwell’s opinion, “ itis to be
feared that we shall have to be taught thermodynamics for several
generations before we can expect beginners to receive as axiomatic
the theory of entropy.”
The account given of thermodynamic mnctivity and dissipation of
energy is good and clear, and it is properly remarked that Clausius’
theorem of the tendency of the entropy of the universe to a maxi-
mum is only a restatement in terms of entropy of Lord Kelvin’s
dissipation theorem published thirteen years earlier.
Though the book, therefore, does not seem quite to fulfil the pro-
mise of the Preface, it will doubtless prove a useful mathematical
introduction to the subject, which it does not pretend to treat
experimentally, the few experiments that are referred to being
mentioned only briefly and without detail.
Its arrangement seems capable of improvement. Thus, it is not
broken up into articles and its equations zre numbered consecu-
tively from first to last, so that references are tedious: the theorem
of the dependence on pressure of the temperature of the maximum
density of water is placed where it seems to be dependent on
thermodynamical considerations, while that of the equality of the
ratios of the principal specific heats and of the principal elasti-
cities is actually proved by such considerations, of which it is
absolutely independent—as is obvious, since it was known to
Laplace: and two general equations of very great importance,
(216) and (217), are deduced only incidentally to prove that the
principal specifie heats of superheated vapours are approximately
functions of temperature only.
There is some looseness of expression: thus the word perfect
is used as equivalent to efficient, which leads to the solecisms
more perfect and equally perfect ; the dyne, centimetre, and erg are
called French units: the dynamical equivalent of heat is said to be
B10 Notices respecting New Books.
-* 772 on the Fahrenheit scale”; Mayer is credited with an experi-
ment which was repeated by J oule, whose object in experimenting
-is-rather made to appear as the justification of Mayer's hypothesis.
Technical terms, too, are used without definition: thus the idea of
efficiency 1s introduced on p- 26 without any explanation though
-its quantitative measurement is concerned, and, indeed, when an
-tmplicit definition is finally given on p. 35 in connexion witha
Carnot cycle, it is in terms which are neither general nor such as
Carnot could have accepted. it may also-be pointed out that
in Chaps. XVI. and XVII. there is no Wee symbol for
absolute temperature, though everywhere else the letter 7 is used ;
that in Chapter XV. the muiceeieal specitic ation of entropy Abas
from that adopted elsewhere; and that in (151) only a particular
integral is given of the partial differential equation (150), the
general solution of which is K=7* f(;*—3Ar,"p) corresponding to
the characteristic v/7= U(p)+Ard\de 7—*f(7°--3Ar,"p).
The notation is not all that can be desired; that of partial
difterential coefficients is specially abused, after Clausius’ example,
_In being applied to denote thermal capacities, and in Chap. XI.
‘the differential coefficients of p and A with respect to ¢ are con-
tinually enclosed in brackets armed with some such subscript as 4,
which is entirely incorrect, as these are not partial differential
coefficients at all except with respect to the state of saturation ;
elsewhere, too, occurs repeatedly the meaningless form (dr/dt)g,
wherein 7 is an acknowledged function of ¢ only.
These are, however, blemishes which do not impair the value of
the book, but might be considered in view of a second edition.
_Among its good points must specially be mentioned the stress that
is laid on the proper definition of absolute temperature, though
on p. 168 the author himself uses the definition to which he objects ;
and there is an in‘eresting modification of Rankine’s characteristic
for gases suggested w hich deserves discussion. It is further well
remarked that even on the caloric theory Clapeyron’s version of
-Carnot’s operations (which is that adopted in the book) would be
improved by the adoption of Clausius’ modification,—which, by the
way, is ascribed to J. Thomson, though contained in that memoir
of Clausius which first set the subject on its new basis. It may
_be here remarked that Carnot’s own version of his cycle requires
no modification whatever, even from the new point of view.
Die physikalische Behandlung und die Messung hoher Temperaturen.
By Dr. Cart Barus. Leipzig: Barth, 1892.
THE subject of pyrometry, although forming an important
application of physics to manufactures, has not received from
physicists the attention which it deserves. One reason for this is
undoubtedly the difficulty of maintaining a constant high tempera-
‘ture, and another is to be found in the fact that the subject neces-
-sitates a detailed study of the alterations produced in the properties
-of matter by excessive heating. In order to measure any tempera-
Notices respecting New Pooks. 311
ture absolutely, we must assume that some property of a substance
remains constant at that temperature and at other known tempe-
ratures. If this is not the case, the same temperature will have
different values according tc the method by which it is measured,
and its true value will most probably be that found by a majority
of the methods. The author in his present volume has criticized
the different methods of determining temperatures, and has given
the results of experiments by himself and other workers in the
same field, from which it appears that only three properties remain
constant over wide ranges of temperature. These are the expan-
sion of gases, the change of their viscosity with temperature, and
the thermoelectric properties of certain wnetals, All these methods
yield consistent results for the value of a given high temperature. .
The second part of the volume is a discussion of the applicability
of these three methods, and Dr. Barus pronounces in favour of the
thermoelectric method. He then goes on to discuss the various
forms of apparatus which might be used in applying this method ;
from which it appears that a junction of platinum with an alloy of
platinum and iridium or rhodium gives the best results.
The book is the outcome of several years of difficult experi-
menting, and it is to be hoped that it will encourage a closer study
ot the properties of bodies, and especially of metals, at high tem-
peratures. James L. Howarp.
Hilfsbuch fur die Ausfuhrung elektrischer Messungen. By Dr. AD.
HEYDWEILLER. Leipzig: Barth, 1892.
Txis volume is not intended to serve as a text-book, but merely as
an epitome of the various processes of electrical measurement. It
gives in a collected form the different methods available for any
particular kind of measurement, together with a short description
of each; the formule necessary in order to calculate the results
being likewise quoted, but not proved. In the majority of cases,
however, the original papers and treatises are referred to for more
complete information on this latter pomt. Under each experiment
the author mentions the sources of error to which it is liable, and
the devices for avoiding or eliminating them are stated, when such
exist. This portion of the work has been carefully written, and
will be found useful when the choice of a suitable method of
measurement has to be made. At the end of the volume the
various electrical constants have been tabulated, and four-figure
logarithm and trigonometrical tables are also to be found there.
Although the title of the book refers to electricity only descriptions
of magnetic observations have also been given; but, as the author
tells us im his preface, these are treated more briefly, and only
those which are necessary in electrical measurements have been
described. JamEsS L. Howarp.
XXX. Proceedings of Learned Societies.
GEOLOGICAL SOCIETY.
(Continued from p. 150. }
December 21st, 1892.—Prof. J. W. Judd, F.R.S., Vice-President,
in the Chair.
Sheet following communications were read :—
1. “On a Sauropodous Dinosaurian Vertebra from the Wealden
of Hastings.” By R. Lydekker, Esq., B.A., F.G.S.
2. “On some additional Remains of Cestraciont and other Fishes
in the Green Gritty Marls, immediately overlying the Red Marls of
the Upper Keuper in Warwickshire.” By the Rey. P. B. Brodie,
MAS, EeG:S:
3. “ Calamostachys Binneyana, Schimp.” By Thomas Hick, Esq.,
B.A., B.Sc.
4. “Notes on some Pennsylvanian Calamites.” By W. S.
Gresley, Esq., F.G.S.
5. “Scandinavian Boulders at Cromer.” By Herr Victor Madsen,
of the Danish Geological Survey.
During a visit to Cromer in 1891 the author devoted much
attention to a search for Scandinavian boulders, and obtained three
specimens; one (a violet felspar-porphyry) was from the shore, and
the other two were from the collection of Mr. Savin. ‘The first was
considered to come from S.E. Norway, and indeed Mr. K. O. Bjorlykke,
to whom it was submitted, refers it to the environs of Christiania.
The author considered that the two specimens presented to him
by Mr. Savin, who had taken them out of Boulder Clay between
Cromer and Overstrand, were from Dalecarlia; and these were
submitted to Mr. E. Svedmark, who compared one of them (a brown
felspar-hornblende-porphyry) with the Gronklitt porphyry in the
parish of Orsa, and declared that the other (a blackish felsite-
porphyry) might also be from Dalecarlia.
January llth, 1893.—W. H. Hudleston, Esq., M.A., F.R.S.,
President, in the Chair.
The following communications were read :—
1. “ Variolite of the Lleyn, and associated Volcanic Rocks.” By
Catherine A. Raisin, B.Sc.
The district in which these rocks occur is the south-western part
of the Lleyn peninsula, marked on the Geological Survey map as
‘ metamorphosed Cambrian.’
_ Some of the holocrystalline rocks are probably later intrusions.
The igneous rocks, which are described in detail in the present paper,
belong to the class of rather basic andesites or not very basic basalts ;
they show two extreme types, which were probably formed by
ee
Intelligence and Miscellaneous Articles. 313
differentiation from an originally homogeneous magma. Corre-
sponding to the two types of rock are two forms of variolite.
These are fully described, and their mode of development is dis-
cussed.
The variolites occur near Aberdaron and at places along the coast.
Their spherulitie structure often is developed towards the exterior
of contraction-spheroids, and in this and in other particulars they
correspond with those of the Fichtelgebirge and of the Durance.
The volcanic rocks include lava-flows and fragmental masses, both
fine ash and coarse agglomerate. They are associated with lime-
stones, quartzose, and other rocks, which are possibly sedimentary,
but which give no trustworthy evidence of the age of the variolites.
2. “ On the Petrography of the Island of Capraja.” By Hamilton
Emmons, Esq.
The rocks of Capraja consist generally of andesitic outflows resting
on andesitic breccias and conglomerates. ‘The southern end seems
to have formed a distinct centre of volcanic activity, whose products
are younger in age and more basic in character than the rocks of the
rest of the island, and may be termed ‘ anamesites.’ The lavas
appear to have flowed from a vent at some distance from the cone
which probably occurred here and gave out highly scoriaceous
fragments. In the other parts of the island andesite is almost
everywhere found, with patches of the underlying breccias here
and there in the valley bottoms. The chief centre of activity prob-
ably lay west of the centre of the island.
Petrographical details of the andesites and anamesites, descrip-
tions of the groundmass and included minerals of each, and chemical
analyses are given. As regards the age of the constituents, the
author arranges them in the following order, commencing with the
oldest :—magnetite, olivine, augite, mica, felspar, nepheline.
XXXI. Intelligence and Miscellaneous Articles.
ON A NEW ELECTRICAL FURNACE. BY M. HENRI MOISSAN.
HIS new furnace is made of two carefully plane pieces of quick-
lime one placed under the other. In the lower one is a longi-
tudinal groove for the two electrodes, and in the middle is a small
cavity more or less deep acting as a crucible; it contains a layer
ot a few centimetres of the substance to be acted upon by the are.
A small carbon crucible may also be placed in it containing the
substance to be calcined. In the reduction of oxides and the
fusion of metals, larger crucibles are used, and through a cylin-
drical aperture in the upper brick small] cartridges of the compressed
oxide and carbon can from time to time be added. The diameter
of the carbons which act as conductors will of course vary with the
strength of the current; after each experiment the end of the
carbon is changed into graphite.
The current most frequently used was one of 30 amperes and
Phil. Mag. 8. &. Vol, 35. No. 214. March 1893. iy,
314 Intelligence and Miscellaneous Artzcles.
55 volts; the temperature did not much exceed 2250°. A current
furnished by a gas-engine of 8 horse-power was 100 amperes and
45 volts produced a temperature of about 2500°. Finally, thanks
to the courtesy of M. Violle, we had at our disposal 50 horse-
power ; the are in these cunditions measured 450 amperes and
70 volts, the temperature was about 3000°.
With high-tension experiments certain precautions must be
taken and the conductors be carefully insulated. Even with
currents of 30 amperes and 50 volts, like those used at the
beginning of the investigation, the face must not be exposed to a
prolonged action of the electrical light, and the eyes must always
be protected by means of very dark glasses. Electrical sun-strokes
were very frequent at the outset of these researches, and the
irritation produced by the are on the eyes may produce very painful
congestion.
The temperatures given are only approximate; they will be
especially determined by M. Violle by methods to be afterwards
described. A certain number of the results obtained are briefly
enumerated.
When the temperature is near 2500°, lime, strontia, and magnesia
crystallize in a few minutes. If the temperature reaches 3000° the
substance of the furnace itself—quick-lime—melts and runs like
water. At this same temperature carbon rapidly reduces calcic
oxide, and the metal is liberated freely ; it unites readily with the
carbon of the electrodes, forming a calcic carbide, liquid at a red
heat, and which can be easily collected. Chromic oxide and magnetic
oxide of iron are melted rapidly at a temperature of 2250°.
Uranium oxide when heated alone is reduced to protoxide, erystal-
lizing in long prisms. Uranium oxide, which cannot be reduced
by carbon at the highest temperature of our furnaces, is reduced
at once at the temperature of 8000°. In ten minutes it is easy to
obtain a regulus of 120 grains of uranium.
The oxides of nickel, cobalt, manganese, and chromium are
reduced by carbon in a few minutes at 2500°. This is a regular
lecture experiment not requiring more than a quarter of an hour.
By this method we have been able to cause boron and silicon to
act on metals, and thus obtain borides and silicides in very
beautiful crystals.
This investigation is being continued.—Comptus Rendus, Dec. 12,
1892,
ON THE DAILY VARIATIONS OF GRAVITY. BY M. MASCART.
I have on former occasions used under the name of a gravity
barometer an instrument by which the variation of gravity between
different stations may be determined. The apparatus has the
drawback of being very fragile, but the same arrangement haa
great advantages in examining whether there are temporary Varia-
tions in one and the same place.
For some years past I have arranged a barometric tube contain-
ing a column of mercury four metres and a half in length, which
Intelligence and Miscellaneous Articles. 315
counterbalances the pressure of a mass of hydrogen contained in a
lateral vessel. The whole apparatus is sunk in the ground with
the exception of a short column of mercury at the top. The level
of the liquid is compared with a lateral division, the image of which is
formed in the axis of the tube, and the points may be fixed to
within the ;4, of a millimetre.
Direct observations at different times of day only showed a
continuous course, the greater part of which was due to inevitable
changes of temperature ; certain results can only be obtained by
photographic registration.
In the proofs submitted the differences of level are multiplied
by 20; they correspond to the variations which are directly ob-
served on a column 90 metres in length.
The curves ordinarily present a very regular and slow course
which is especially due to changes of temperature; but for some
days sudden accidents are seen, the duration of which is from
fifteen minutes to an hour, and which do not seem to be explicable
otherwise than by correlated variations of gravity. These accidents
may attain and even exceed 5), of a millimetre, which corresponds
to so¢yp OF One second per day, supposing that they lasted the
whole day.
In order to have a term of comparison, it is sufficient to observe
that if the difference between high and low water is 10 metres,
the liquid layer would produce a variation of spy of the level
value of gravity, that is one fifth of the preceding,
The existence of these temporary variations of gravity appears
undoubted and deserves attention. I intend to organize at the
Observatory of the Parc Saint Maur an apparatus constructed
with more care, from which all casual trepidation of the ground is
excluded, and the indications of which can be continuously followed.
Observations of this kind will no doubt present a peculiar interest
in voleanic districts if the changes are due to displacements of
masses in the interior.—Comptes Rendus, January 30, 1893.
PRELIMINARY NOTE ON THE COLOURS OF CLOUDY
CONDENSATION. BY C. BARUS.
By allowing saturated steam to pass suddenly from a higher to
a lower temperature (jet) in uniformly temperatured, uniformly
dusty air, the following succession of colours is seen by transmitted
white light, if the difference of temperature in question continually
increases :—F aint green, faint blue, pale violet, pale violet-purple,
pale purple, muddy brown-orange, straw-yellow, greenish yellow ;
green, blue-green, grey-blue, intense blue, indigo, intense dark
violet, black (opaque); intense brown, intense orange, yellow,
white.
Seen by reflected white light, the same mass of steam is always
dull neutral white.
If the colours enumerated be taken in the inverse order, be-
ginning with white, they are absolutely identical with the inter-
ference-colours of thin plates (Newton’s rings) of the first and
316 Intelligence and Miscellaneous Articles.
second order, seen by transmitted white light under normal inci-
dence. ‘Thus it is worth inquiring whether small globules of water,
when white light is normally transmitted, affect it like thin plates.
For a given homogeneous colour, if I be the intensity of the incident
licht and & ( 04 to -05) the reflexion-coefficient, then after a single
transmission the interference maxima and minima are
(1-k)(1+)1 and (1—ky(1—-2 1;
they differ only very slightly. But if there be an indefinite number
of particles all of the same size available, then this process is in-
definitely repeated in such a way that while the coloured light is
not extinguished, the admixed white lght becomes continually
more coloured. Hence, after a sufficiently great number of trans-
missions, the emergent ray will show intense colour. Seen by
reflected light, the case is almost the converse of this. For a single
particle the masses which interfere are (Kl and k(1—<)?1) weaker,
but nearly equal, and the interference is therefore very perfect.
It is not, however, capable of indefinite repetition, for after each
interference the direction is reversed. The light which emerges in
a direction opposite to the incident ray must therefore have passed
through the particles, 7. e. it has been brought to interference both
by reflexion and by transmission, and its colour is thus virtually
extinguished.
The final point to be considered is the occurrence of black between
brown and dark violet of the first order. Here, however, for
relatively very small increase of the thickness of the plate, the
colours run rapidly from brown through red, carmine, dark red-
brown to violet. Hence these interferences are apt to occur to-
gether and an opaque effect is to be anticipated. Particularly is
this presumable, because the opaque field is coincident with the
breakdown of the steady motion * of the jet.
Thus it seems that the colours of cloudy condensation may,
without serious error, be interpreted as a case of Newton’s inter-
ferences by transmitted light. In so far as this is true, one may
pass at once from the colour of the field to the size of the particles
producing it; and the dimensions so obtained agree well with R.
v. Helmholtz’s estimate made in accordance with Kelvin’s equation
for the increase of vaponr-tension at a convex surface. In the
study of the condensation phenomena vapour-liquid, the experi-
mental power of a method, which is adapted for instantancous
observation, and which, for a certain range of dimensions, not only
discriminates between vapour and a collection of indefinitely small
suspended water-globules, but actually defines their size, cannot
be overestimated. An account of my work, together with other
allied observations, will be given in the March number of the
‘American Meteorological Journal.’—Silliman’s Journal, February
1893. |
* IT refer here to Osborne Reynolds’ work (Phil. Trans. iii. p. 935, 1883)
with liquid jets, according to which, after a certain critical velocity is
surpassed, the uniformly steady motion breaks up into eddying motion.
I am also searching for Reynolds’ lag phenomenon (J. ¢. p. 957).
THE
‘LONDON, EDINBURGH, ano DUBLIN
PHILOSOPHICAL MAGAZINE
AND
JOURNAL OF SCIENCE.
[FIFTH SERIES.]
APREL 1893.
XXXIL, On Plane and Spherical Sound-Waves of Finite
Amplitude. By Cuaries V. Burton, D.Sc.*
Part I.— PLANE WAVES.
1. HE subject of plane waves of finite amplitude has
been considered by Riemann{; and so long as we
confine our attention to the case where velocity and density
are everywhere continuous, his investigation, as is well known,
leaves little to be desired. It will not, therefore, be necessary
here to make further reference to this aspect of the subject ;
but there is one part of Riemann’s work which Lord Rayleigh
has clearly shown to be unsatisfactory, and it is this point
which we have now especially to consider. Lord Rayleigh
says t:— | |
a It has been held that a state of motion is possible
in which the fluid is divided into two parts by a surface of
discontinuity propagating itself with constant velocity, all
the fluid on one side of the surface of discontinuity being in
one uniform condition as to density and velocity, and on the
other side in a second uniform condition in the same respects.
Now, if this motion were possible, a motion of the same kind
in which the surface of discontinuity is at rest would also be
possible, as we may see by supposing a velocity equal and
* Communicated by the Physical Society: read February 24, 1898,
¥ “Ueber die Fortpflanzung ebener Luftwellen von endlicher Schwing-
ungsweite,” Gott. Abhandi. t. viii. (1860); reprinted in Werke, p. 145.
{ Theory of Sound, vol. ii. § 253, p. 41.
Phil. Mag. 8. 5. Vol. 35. No. 215. April 1893. Z
318 Dr. C. Burton on Plane and Spherical
opposite to that with which the surface of discontinuity at
first moves, to be impressed upon the whole mass of fluid. In
order to find the relations which must subsist between the
velocity and density on the one side (w, p,) and the velocity
and density on the other side (wz, p,), we notice in the first
place that by the principle of the conservation of matter
Polg=pity. Again, if we consider the momentum of a slice
bounded by parallel planes and including the surface of dis-
continuity, we see that the momentum leaving the slice in the
unit of time is for each unit of area (p9v.=p1u1)Ue, while the
momentum entering it is p;u,”. The difference of momentum
must be balanced by the pressures acting at the boundaries of
the slice, so that
Pilly (U2— Uy) =p — Po = a(p1— po),
=an/(@), m=an/(%)
U,=a Un =A 5
: We Sosy P2
The motion thus determined is, however, not possible; it
satisfies indeed the conditions of mass and momentum, but it
violates the condition of energy expressed by the equation
whence
Won Lap AS 2 99
3 Ug 7 Uy =a log pi—a log po.
2. The assumed motion here criticised is one in which
density and velocity are constant for all points on the same
side of the surface of discontinuity, while this surface itself is
propagated through the fluid with constant velocity. It is
easily shown, however, that the same objection applies when,
on either side of the surface, velocity and density vary con-
tinuously in the direction of propagation, while the velocity
of propagation of the surface is also allowed to vary. For
let 8 (fig. 1) be a surface of discontinuity which
is being propagated through the fluid, while the Fig. 1.
planes A, B, parallel to S and lying on either |
side of it, are fixed in the fluid. At a given
instant let
distance of S from A = m,
ry) BB, S=n;
density and velocity of fluid just to the left
of Po U4,
density and velocity of fluid just to the right
of S=Ppo, w 5
velocity with which § is travelling = V.
Sound- Waves of Fimte Amplitude. 319
Then, since A and B are fixed in the fluid, they are ap-
proximately moving with the respective velocities uw, ug; m
and n being taken sufficiently small. On the same under-
standing, the mass of fluid between A and B (referred to
unit surface) =mp,+mnp,; and since this mass must remain
constant,
d
ap (mpi + Mpa) =93
2. e. in the limit, when m and n are infinitesimal,
dm dn
Bae aa Pee =0,
or
pi( V —2) =p.(V—w,). ni ir AC a Sabor 5 te
Similarly, if p, and p. are the pressures corresponding to
p; and pe, the principle of momentum gives:—
p\—po= rate of change of momentum between A and B
d
= oF (u3p1m + Upon)
= um pi(V—u)—Uaps(V—ue). » 2 - - + « (2)
If the energy per unit volume corresponding to density p
(in the absence of bodily motion) is called y(p), the principle
of energy would further give
Pi1—Poo= rate of change of energy between A and B
= 3m( spin? + x(01)) + m(4 par +x(02) )}
= feprs’ +x (Pr) (V —1) — faparle’ +x (92) t (Vue). (8)
Since (1), (2), and (3) involve only the instantaneous values
of w, Pi, U2, P2, and V, together with explicit functions of such
values, while the space- and time-variations of all these quan-
tities are absent from the equations, it is evident that the
conditions to be satisfied at the surface S are the same as if
Ur) Pi) U2) P2, V were absolute constants. We conclude then,
that, with our assunvptions, a surface of discontinuity cannot
be propagated through a fluid with any: velocity, uniform of
variable, except under that special law of pressure for which
progressive waves are of accurately permanent type.
3. What, then, becomes of waves of finite amplitude after
discontinuity has set in? We may emphasize this difficulty,
and at the same time obtain a clue to its solution, by con-
sidering the following case (fig. 2):—-A is a piston fitting a
Z 2
320 Dr. C. Burton on Plane and Spherical
cylindrical tube (or, if we Fig. 2.
please, is a portion of an un-
limited rigid plane). All the
air to the right of A is initially
at rest and of uniform density,
and then A is impulsively set in
motion, and kept moving to the right with uniform velocity v.
Consider the speed with which the disturbance generated by
A advances into the still air to the right; it is evident that
in all cases the front of the disturbance must advance faster
than A. ‘Take, then, the case in which
U> a,
where a is the propagation-velocity of infinitesimal disturb-
ances. Two alternatives present themselves :—
(i.) If velocity and density are always either constant or
continuously variable in the direction of propagation, the rate
of propagation at any point will, in accordance with known
principles, be =
d
/ Ere
and therefore at the front of the disturbance, where w=0 and
p = the “undisturbed” density, the velocity of propagation
will be simply =a; that is, less than the velocity with which
A is advancing. Obviously this will not do.
(ii.) If velocity and density are not always either constant
or continuously variable, that is, if one or more surfaces of
discontinuity are being propagated through the air, we are
met by the difficulty explained in the last section.
4, A simple mechanical analogy will help to indicate the
actual motion. A number of equal spheres, of the same
material throughout, are capable of sliding without friction
Fig. 3.
{iHO—0—0—0=0=0-
=1]}@=O=0=—0=—0=O=
— 71 DO©=02 0-0
along a straight bar (fig. 3), and are connected together by a
number of very weak and exactly similar springs (not shown),
so that. when there is equilibrium they are equally spaced
Sound- Waves of Finite Amplitude. 321
along the bar. If one of the spheres were moved backwards
and forwards through a small range, a disturbance would
travel through the whole system, but owing to the weakness
of the connecting springs it would travel very slowly. Sup-
pose, now, that the last sphere on the left hand is connected to
a movable piston by a spring half the length of the others,
but otherwise similar to them; and let this piston be suddenly
moved to the right with a considerable velocity which is kept
constant, and which we may call unity. The weak connecting
spring between the piston and the first sphere produces no
sensible effect until the two are almost in contact, when the
sphere rebounds with velocity 2. This first sphere then
strikes the second, imparting to it the velocity 2, and at the
same time coming to rest. The positions of the spheres after
successive equal intervals of time are represented in fig. 3,
where the number written on any sphere represents its velo-
city just after the impact which it is suffering. No number
is written on those spheres which have not so far been affected
by the motion. From this it will be evident that when the
piston moves to the right with a constant velocity which is
very great compared with the propagation-velocity of infini-
tesimal vibrations of the system, the disturbance advances to
the right with twice the velocity of the piston, provided that
the diameters of the spheres are excluded from the reckoning.
Now suppose that the spheres are too small and too close
together to be individually distinguished; then, at any instant,
the system will appear to be divisible into two parts, in one
of which the velocity is unity, while in the other it is zero;
and in the moving part the spheres will appear to be twice as
thickly condensed as in the still part. That the constant
velocity of the piston is very great compared with the propa-
gation-velocity of small vibrations is of course only a sup-
position introduced for the sake of simplicity. If, on the
other hand, these two velocities are comparable, two adjacent
spheres will always remain finitely separated from one another,
and the velocity of any individual sphere within the disturbed
stretch will never be as small as zero, or as great as twice the
velocity of the piston ; the mean velocity within the disturbed
stretch being equal to that of the piston. When the spheres
are very small and very close together, we shall still have
apparently an abrupt transition frem finite velocity and greater
density to zero velocity and smaller density; and the energy,
which is apparently lost.as the spheres pass from the latter
condition to the former, exists as energy of relative motion
and unequal relative displacement amongst the spheres in the
disturbed stretch. :
5. Let us now compare the case just considered with the
322 Dr. C. Burton on Plane and Spherical
case of § 3 (fig. 2): and first, concerning the nature of the
analogy, it should be noticed that the individual spheres are
not the analogues of the separate gaseous molecules, but that
when both spheres and molecules are very small and very
numerous, the apparently continuous properties of the system
of spheres correspond to similar properties of the gas. The
connecting springs represent the elasticity of the gas, iso-
thermal or adiabatic as the case may be, and the energy of
relative motion and unequal relative displacement amongst
the disturbed spheres suggests that there is a production of
heat over and above that which would be due to the (iso-
thermal or adiabatic) change of density ; that is, a diss¢pative
production of heat. The motion considered in the last section
properly corresponds to the case where there is no conduction
of heat, so that the connecting springs are the representatives
of adiabatic elasticity, and the additional heat generated
remains wholly within the more condensed part of the air.
If we make the somewhat violent assumption that the tempe-
rature of the air remains constant throughout, the additional
heat generated will be conducted away isothermally, and the
equivalent energy will be, for our purposes, entirely lost.
To represent this case by means of our spheres we should
have to regard the connecting springs as representing iso-
thermal elasticity, while the energy of relative motion and
unequal relative displacement among the disturbed spheres,
as fast as it is produced, is to be consumed in doing work
against suitable internal forces.
6. The mechanical system of spheres and springs, having
suggested a solution, has served its purpose, and it now
remains for us more closely to consider the aerial problem in
the light of this suggestion. We may take, first, the case
where the temperature is supposed to be invariable; for
although such a supposition is necessarily far removed from
the truth, it leads to very simple results, which indicate well
enough the general character of the motion. Let the piston
A (fig. 4) be moving to the
right with constant velocity Fig. 4,
v (which may be either less
or greater than a, the velo-
city of feeble sounds in air).
Assume all the air between
A and a parallel plane sur-
face B to have the velocity v
and density p,, while all the air to the right of B is at rest
and has the density pp». Let the plane B move to the right
with velocity V. Then the invariability of mass between A
Sound- Waves of Finite Amplitude. 323
and a plane C fixed in the still air gives
pi(V—v)—pyv=0; . . .. . 4)
while from the principle of momentum,
Pi (V— v) Olam 0's .=, hans Sosy tee (5)
the pressure p being a function of p only, since the tempera-
ture is supposed to be constant throughout. If we assume
for this case the truth of Boyle’s law, so that p=a’p always,
(5) becomes
py(a? — Vv + v7) =pya”, SRR thea (6)
which together with (4) is sufficient to determine V and p;
when v and py are given. Taking all these quantities to
remain constant throughout the motion, we see that at each
instant the following conditions are satisfied :-—
(i) Every necessary condition between A and B, since
density and velocity are there constant with respect
to space and time ;
(1) Every necessary condition to the right of B, since the
air there is at rest and in a constant uniform state ;
(iii) Equality between the velocity of A and that of the
air in contact with it ;
(iv) At B, the conservation of mass and momentum, which
are necessary conditions, and which, together with
our supposition that the temperature is somehow
maintained uniform, are sufficeent to determine what
takes place at B*.
Moreover, if at a time ¢ (reckoned from the instant when
A was impulsively started into motion) we take the distance
of B from A to be (V—v)t, so that initially B coincides with
A, the initial conditions are satisfied.
‘Thus the assumed motion satisfies all the necessary con-
ditions ; it is therefore the actual motion.
7. Let us now examine what occurs when no heat is
allowed to pass by conduction or radiation ; a state of things
much more nearly realized in practice. Suppose the motion
of A and the condition of the undisturbed air to be the same
as in the last section, while the (constant) velocity of B is
now called V’, and the density and pressure of the air between
A and B (called p’, p’ respectively) are also taken to be uni-
form and constant. At each instant, in place of (4) and (5),
we shall now have
AANg= ©) gests hy. se ya nae)
pruCV =v) = pi. ay. ew 6) (8)
* Energy appears to be lost, because dissipatively produced heat is
conducted away isothermally,
324 Dr. ©. Burton on Plane and Spherical
Since we assume that there is no transference of heat by
conduction or radiation, the rate at which the total energy of
the system increases must be equal to the rate at which work
is being done upon it by the piston A. Let @ be the abso-
lute temperature to the right of B, that between A and B
being 0’, and let us further assume for simplicity that
P a const. :
pe
while y, the ratio of the two specific heats, is also supposed
constant. It can then be shown without difficulty that the
total energy per unit mass between A and B exceeds that to
the right of B by
Po O —O% fe es
(y—1)po % 2°
and multiplying this by p,V’, the mass of air which crosses
one unit of the surface B in each unit of time, we obtain the
rate (referred to unit area) at which the system is gaining
energy. Again, the rate at which unit area of the piston does
work on the system
als
Ee ges a ae
Tet a ed eeiae
and equating this to the rate of gain of energy, we obtain
po mes wv PoV'! pe
PO 505 V=PyV 5) + (y—1)0, (0 ,). a ° (9)
We may also write equation (8) in the form
plo(W'—v) = $F (p'6'—pr)s - ~~ (10)
Po%
and (7), (9), and (10) will then serve to determine V’, p',
when ¥, po, 9 are given. Since we have taken all these
quantities to remain constant throughout the motion, we see,
as before, that at each instant all the necessary conditions are
satisfied ; the principles of mass and momentum, together
with our supposition that there is no exchange of heat, being
sufficient to determine what takes place at B. Again, if ata
time t from the commencement of the motion we take the
distance of B from A to be (V’—v)é, so that initially B coin-
cides with A, the initial conditions are satisfied. The assumed
motion thus satisfies all the necessary conditions, and is there-
fore the actual motion.
8. If we compare the results of the last two sections with
Sound- Waves of Finite Amplitude. 325
those given by Riemann*, we shall find complete accordance
so far as §6 is concerned, though with §7 the case is dif-
ferent ; and this may be easily explained. We cannot in
general investigate the motion of a (frictionless) compres-
sible fluid by means of the equations of continuity and
momentum, without further making some supposition as to
the exchange or non-exchange of heat, and so we usually
assume either that the temperature remains constant, or that
there is no exchange of heat: in either case (provided the
motion is continuous), the pressure is a function of the
density only. Ata surface of discontinuity there is not only
the ordinary heating effect due to compression, but also, as
we have seen, a dissipative generation of heat, and so, when
applying the equations of continuity and momentum at such
a surface, we must know what becomes of this additional
heat. Now in all cases Riemann makes the assumption that
the pressure is a function of the density only, and this is
necessarily equivalent to an assumption concerning the trans-
ference of heat. Throughout most of his treatment of waves
of discontinuity Riemann assumes that temperature is
constant and that Boyle’s law holds good; accordingly our
§ 6 is entirely in harmony with his conclusions, in fact (4)
and (5) are only particular forms of equations given by
Riemann. Of course the hypothesis that a portion of gas
can be instantaneously compressed to a finite extent without
any appreciable change of temperature, is not in accord-
ance with experience, but provided we accept the assump-
tion that the temperature remains constant throughout, all that
Riemann says concerning the propagation of waves of discon-
tinuity under Boyle’s law will hold good.
The assumption made in § 7, that there is no appreciable
transference of heat, is probably much nearer the truth; but
this is not in accordance with any assumption made by
Riemann. When pressure is assumed to be a function of
density only, and to vary with it according to the adiabatic
law, 2t 2s wrtually assumed that at the discontinuity just so
much heat remains in the gas as would be due to slow adiabatic
compression, while the further amount of heat which is dissipa-
twely produced 7s completely and instantaneously removed by
conductzon. But though Riemann’s results may thus be
justified by impossible assumptions concerning the diffusion
of heat, we may more reasonably, following Lord Rayleigh,
regard them as involving a destruction of energy. The real
source of error lies in Riemann’s fundamental hypothesis.
At the outset he supposes the expansion and contraction of
* Loc, cit,
326 Dr. C. Burton on Plane and Spherical
the air to be either purely isothermal or purely adiabatic, and
thenceforward he treats the air as a frictionless and mathe-
matically continuous fluid, in which pressure and density are
connected by an invariable law. But in general the existence
of such a fluid is contrary to the conservation of energy ;
for as soon as discontinuity arises, energy will be destroyed.
9. It may not be out of place to conclude this portion of
the subject by a short reference to a paper by Dr. O. Tum-
lirz *. This author starts, as Riemann did, with the assump-
tion that the pressure is a function of the density only, the
law of pressure being further assumed to be the adiabatic
law; and in order to avoid Riemann’s error, he explicitly
uses the principle of energy applicable to continuous motion,
in place of the principle of momentum. But the foregoing
discussion will have made it clear, I think, that the solution
of the difficulty is not to be sought for in this direction. In
addition to the assumptions common to his own work and te
that of Tumlirz, Riemann uses only the principle of mass
and the principle of momentum ; and since by their aid alone
he arrives at a completely determinate motion, it follows
that any other motion consistent with the same arbitrary
assumptions, and with the condition of mass, must violate
the condition of momentum. We have seen, in fact, that
there is dissipation of energy at a surface of discontinuity, so
that the condition of energy applicable to continuous motion
ceases to hold good. We are acquainted, too, with other
instances where loss of continuity involves dissipation of
energy ; for example, there is the case of one hard body
rolling over another.
As the result of his investigation, Dr. Tumlirz concludes
that as soon as a discontinuity is formed it immediately dis-
appears again, this effect being accompanied by a lengthening
of the wave and a more rapid advance of the disturbance.
In this way, therefore, he seeks to explain the increased
velocity of very intense sounds, such as the sounds of
electric sparks investigated by Macht. But it has already been
pointed out [§ 3 (i.) |, that when density and velocity are every-
where continuous functions of the coordinates, the front of a dis-
turbance advancing into still air must travel forward with the
velocity of infinitely feeble sounds. A greater velocity can
only ensue when the motion has become discontinuous.
* “Ueber die Fortpflanzung ebener Luftwellen endlicher Schwing-
ungsweite,” Sitzungsb. der Wien. Akad. xcv. pp. 367-887 (1887).
T Sttzungsb. der Wien. Akad, \xxv., Ixxvii., lxxyiii. Cf. also W.
W. Jacques |On Sounds of Cannon], Amer. Journ. Sci, 3rd ser. xvii.
p. 116 (1879).
Sound- Waves of Finite Amplitude. 327
Part I].—SPpHERICAL WAVES.
10. When plane waves of finite amplitude are propagated
through a frictionless compressible fluid, discontinuity must
always occur sooner or later, and a moment’s consideration
will show that there are at least some cases when the motion
in spherical waves becomes discontinuous ; the question arises
whether in any case it is possible (in the absence of viscosity)
for divergent spherical waves to travel outward indefinitely
without arriving at a discontinuous state. This question was
suggested to me by Mr. Bryan, who at the same time kindly
handed me notes of his manner of attacking the problem.
His method was to write down the exact kinematical equation
for spherical sound-waves, and then to obtain successive
approximations to the integral of this equation. If it appears
that after any number of approximations the integral would
remain convergent for large values of the radius, we may con-
clude that our equation holds good throughout, and hence that
no discontinuity arises. If, on the other hand, the second or
any higher approximation becomes divergent for large values
of the radius, it is probable that the motion becomes some-
where discontinuous. This method I have not followed out;
but by another method which is, I hope, sufficiently con-
elusive, I shall now endeavour to show that discontinuity
must always arise.
The case in which the motion loses its continuity compara-
tively early requires no further consideration here ; we have
only to concern ourselves with the case in which the initial
disturbance has spread out into a spherical shell of very small
disturbance whose mean radius is very great compared with
the difference between its extreme radii. The equations
applicable to the disturbance are then, very approximately,
8
te eee
u or oP ec - for a given part of the wave, . (12)
where p is the mean density, p+ép the actual density at a
point where the velocity is wu, and a 1s the velocity of infinitely
feeble sounds in air of density p; 7 is as usual the distance of
a point from the centre of symmetry. Let us consider two
neighbouring points M and N, on the same radius, each being
fined in a definite part of the wave, the point M being behind
N (.e. nearer to the origin), and the air-velocity at M ex-
ceeding that at N by Au. Then, as the wave advances, each
328 Dr. C. Burton on Plane and Spherical
part of it will be instantaneously moving forward with (very
approximately) the velocity _
dp
-£ +u
dp
determined by the corresponding values of p and w; so that
M will be gaining on N at the rate
’]
Aut! , [2 &xa 2
dp dp du
approximately. We may admit then that the rate at which
M gains on N is
never < BAu,
where B is a constant suitably chosen.
Again, if Aju is the difference between the air-velocities at
M and N at the time ¢=0, and 7g is the corresponding co-
ordinate of M, we may admit that
Ary
19 + at
where A is a constant not very different from unity. Thus
M gains on N ata rate which is
Au,
Aw is never <
a
7 LESS =
never < a Ser Ayu;
and between the times t=0 and t=¢, the distance gained by
M relatively to N will be
at least ABAon|
0
4 pdt
To + at :
io salen ABAu”log °F“, : aR)
0
If B is finite and positive this expression increases indefinitely
with the time, so long as the laws of continuous motion hold
good. If Apr was the distance between M and N at time
t=0, the time required for M to overtake* N will be not
greater than the value of t, given by
ie a
—Ayr=ABAw log foie
Yo
or, when M and N are taken indefinitely close together at
starting, by
Tor Opps Ou
log nt = a { AB( se oe
1.€., we have t =" en Gera. D) — 1) (15)
; ae
* Cf. Lord Rayleigh, ‘Theory of Sound) vol. ii. p. 36.
Sound- Waves of Finite Amplitude. 329
which gives us a finite upper limit to the time required for
discontinuity to set in, provided B is finite. As our assump-
tions only remain approximately true so long as the motion is
continuous, (15) will only give an approximation to the time
when discontinuity first commences, and accordingly the
relation must be taken to refer to that part of the wave for
which its right-hand side is a minimum. If B is negative
(which is not the case for any known substance), the appro-
priate part of the disturbance will be such that Qu/dr is
positive.
To determine approximately the value of B, we may refer
to (13) and the inequality immediately following. If we
assume Boyle’s law of pressure, so that / (dp/dp)=const., we
have evidently
B=1 very nearly.
If we assume that the changes of density take place adia-
batically, so that p ocp’ and y is nearly constant, the approxi-
mate value of B becomes
dap ee fd
ie = oP.
dp V dp : dp
by means of (11) ;
Date
9 e
If, then, viscosity be neglected, we must conclude that under
any practically possible law of pressure the motion in spherical
sound-waves always becomes discontinuous, and a fortiori the
same will be true of cylindrical waves. But inasmuch as
our result for spherical waves depends on the existence of an
infinite logarithm in (14) when ¢, is increased without limit,
we may conclude that for waves diverging in four dimensions
(or, more generally, in any number of dimensions finitely
greater than three) there would be some cases where the
motion remained always continuous.
11. The general question of spherical sound-waves of finite
amplitude is by no means an easy one. In the case of plane
waves we can write down at once from Riemann’s equations
the condition that the disturbance may be propagated wholly
in the positive or wholly in the negative direction. The
respective conditions are* :— .
wat |'a/P dose,
Po dp
where pp is the density of that part of the fluid whose velocity
* Cf. also Lord Rayleigh, ‘Theory of Sound,’ vol. ii. p. 35 (8).
330 Dr. C. Burton on Plane and Spherical
is reckoned as zero. No such simple criterion can be given
for the existence of a purely convergent or purely divergent
spherical disturbance ; a fact which may be readily seen from
the equations for waves of infinitesimal amplitude. If ¢ is
the potential of a purely divergent system of waves, we have
rh=f(at—7), . te)
where / is a function whose form is unrestricted. Let p be
the ordinary density of the air, and p+6p the actual density
at a point where the coordinate is r and velocity u. We
have, then, on differentiating (16) the well-known relations
200 2) ) [Ga _ f(at—r)
haan —_— ype y tea ° ° e (17)
and 5 ;
ogee *90— LAA"), Bees ees
Pp
From (17) and (18),
(a2 —u)e=f(at—n),
whence differentiating with respect to 7, and neglecting small
quantities beyond the first order,
neo —_ 8) 4 2r( a? —u)= —f'(at—?)
by (18) ; therefore
por 7 >; 2 ae (19)
If, then, an infinitesimal spherical disturbance is to be purely
divergent, this equation must be satisfied for every value of
r. But since the left-hand side involves 6p/p as well as u,
du/dr, and 9 (log p)/d”, it is evident that the question whether
or not the equation is satisfied for some particular value of r
does not depend solely on the state of things in the immediate
neighbourhood of this value, but is influenced also by the
value of p corresponding to the undisturbed air. We must
not therefore seek to characterize a purely divergent dis-
turbance by a differential equation expressing that, with
respect to the air at each point, the disturbance is wholly
propagated in the positive direction of r.
12. Not recognizing this, I had attempted to discover such
an equation, and one step of the inquiry is reproduced here,
for the sake of any interest which it may have.
- Sound-Waves of Finite Amplitude. 331
Tt is required to write down the differential equation of an
infinitesimal spherical disturbance, which is superposed on a
purely radial steady motion.
Though a steady motion extending inward to the pole
would involve a violation of the principle of continuity, we
may suppose that throughout a shell of finite thickness the
distribution of density and velocity is such as would be con-
sistent with steady motion ; the motion within such a shell
would then continue steady, provided that its spherical
boundaries were constrained to expand or contract in a
suitable manner. In the absence of constraints the shell of
steady motion would be invaded from without and from
within by disturbances emanating from adjoining parts of the
fluid, but, at points well within the shell, the character of the
steady motion would necessarily be maintained for a finite
time.
Let ¢ be the potential of the steady motion.
Let $+ be the potential of the actual motion so that
and its derivatives are small.
_Let p, p be the pressure and density in the steady motion.
Let p +p, p+6p be the pressure and density in the actual
motion, and assume that the pressure is a function of
the density only. From the ordinary equations for the
motion of compressible fluids we obtain
= 3 (Sf), es (740)
(rie 1 (SP +g oy)
spk . ae ey GO)
when small quantities of the second order are neglected.
Subtracting (20) from (21)
op - oOpow
ee Ae (22)
Now
op _ dp op.
pe dp pie
therefore
0 op _ dp 10.o, ae
Sieieds : Re ee (23)
and the equations of continuity tor the steady motion and the
332 On Plane and Spherical Sound- Waves.
actual motion may be written
Op. _ 0¢ dp
Cae °° See
dp) 6
OP HPP) — — (p+ Bo) V°(h+H)— (SE + SHOR,
whence by subtraction
Oop Opdv dopded
Sp PV PV b= 5 a, = 5 eee
SG ) 3
was (2 (-+- SPS) fs
expanding this and ee in (24) we get
00 ; __0¢0 eyes)
BEM -o(Z) (45h)
dp\— ,__ oP ov
“Dot? (as) Fs ore
dp\\/_ Od _ Hd _ I'GdW 79S
eye Or Or Of Ores Nes
Now differentiate (22) with respect to ¢ and we have, remem-
bering (23),
_ 4 243% _ lap 8p
Or or rode: Ot!
In this equation we have to substitute the value of Qép/dé
from (25), and if we then put y= Wr, and perform the
necessary reductions, we finally obtain as the differential
equation satisfied By br,
OX — (ew) SK + mw Ok 4 USK + v(S¥—%)=
where
a’=the variable 2 (in the steady iota
Be a __ constant
aie or pr?
ie) 2u da __ 2u 2u oa
ra ton2 (2) Ome.
Vx 2au 2 (7) ; ae
On a new and handy Focometer. 333
if the steady motion in question is a state of rest, «=O and
p 1s a constant, so that U=0, V =0, and our equation reduces
to the ordinary form for small spherical disturbances,
If, on the other hand, y=, the motion may, through any
finite distance, be treated as linear. We shall then have wu and
p both constant, as well as a, and as before U=0, V=0. In
that case
Ovo Oh» OY
7 (?— ne =()
YE (a?—wu Jan BE 5
and this, by a change of independent variables, is easily seen
to be the appropriate form for small plane disturbances of a
fluid whose motion is otherwise uniform.
XXXII. On a new and handy Focometer.
By Protessor J. D. Everett, /.R.S.*
| ae focometer is designed to permit the distance of the
_ “object”? from the screen to be varied, while the lens
which is to throw on the screen an image of the “ object” is
automatically kept midway between the two. This position,
as is well known, gives both the sharpest definition and the
simplest calculation.
The instrument is constructed on the principle of the well-
known toy~called lazy-tongs. A number of flat bars (fig. 1),
OOOO
all exactly alike, are jointed together in such a way that half
of them are in one plane and the other half in a superposed |
plane. With the exception of the end bars, each bar in either
plane is jointed to three of the bars in the other plane, one
joint being in the middle and one at each end. The end bars
are jointed at the middle and one end only. All the bars in
the same plane are parallel, and the two sets together form a
single row of rhombuses all equal and similar, a side of a
rhombus being half the length of a bar. The system has only
* Communicated by the Physical Society: read February 24, 1893.
Phil. Mag. 8. 5. Vol. 85. No. 215. April 1893. 2A
334 Professor J. D. Everett on a
one degree of freedom, and its length is a definite multiple of
the longitudinal diagonal of a rhombus.
The joints are arranged in three rows, one down the middle
and one along each edge, and the distance from joint to joint
in any row is equal to this longitudinal diagonal. This
common distance can be varied between very wide limits by
pulling out or pushing in the frame, and we have thus a means
of dividing an arbitrary Jength into any number of equal
parts. I utilize only the middle row for this purpose, and
utilize it only or chiefly for bisecting a variable distance.
The pins on which the middle joints turn are continued
upwards, as shown in fig. 2, to serve as supports for clips
holding the object, the lens, and the screen. The lens is
Fig. 2.
Elevation.
mounted on the centre pin, and the object and screen usually
on the two end pins, as in fig. 2. In order to avoid flexi-
bility, the clips are made short, and the pins, on which they
are held by screws, rise only 14 inch above the frame. The
base of each pin is a substantial disk (see fig. 3) which rests
upon the table ; all the pins, not only in the middle row, but
also in the two outside rows, terminate in such disks, which
serve as the feet of the instrument, and slide upon the table
when the frame is expanded or contracted. ‘The pins are
of brass 4+ inch in diameter, and the bars are of +-inch
mahogany, ? inch wide, and 13 inches in gross length.
There are 18 of them, as shown in fig. 1. There are 9
pins in the middle row ; and when the object and screen
are on the two end pins, the distance between them is
divided by the other pins into 8 equal parts, any two of
which should together make up the focal length. The
unused pins are the most convenient handles for manipulating
the frame.
The screen may converiently be a piece of white card a
little larger than a post-card, and a square of wire-gauze
about half as big may be used as the object ; but a still
better ‘ object’ is a cross of threads stretched across a square
hole in a card. The light which passes through the square
hole is very conspicuous on the screen before the correct
distance is approached, whereas the shadow of the wire
new and handy Focometer. 335 |
gauze is almost invisible. Two thin cards about the size of
post-cards should be taken, a hole a centimetre square should
be cut through both of them, and they should be gummed
together with the cross threads between them, the threads
being in the first instance long enough to project beyond the
eards to facilitate adjustment while the gum is wet. Waxed
carpet-thread, or any very stout thread with smooth edges, is
Fig. 3.
A supporting pin.
the best for giving a conspicuous and at the same time a
sharp image. As the cross will sometimes have to be raised
or lowered, the hole should be much nearer to one end of
the card than to the other, in order to give a greater range
of adjustment in mounting on theclip. One thread should be
vertical and the other horizontal, in order that their simul-
taneous focussing may serve as a check on the correct
orientation of the lens.
The instrument is intended to be used by placing it on a
table of length not less than four times the focal distance
which is to be measured. A lamp is to be placed either on
one end of the table or on a stand opposite the end, at such
aheight that its flame is about level with the tops of the
clips. The clips should be fixed as low as possible on their
supporting pins, unless it is necessary to raise them to suit
the height of the lamp. In default of a lamp at the proper
height, an adjustable mirror may be used instead, and made
to reflect a beam of light from any large gas-flame in the
room so that the beam shall pass along the tops of the clips.
2 A 2
336 Professor J. D. Everett on a
When the lamp or mirror has once been adjusted to throw
its light in the proper direction, it should not be disturbed,
as all necessary adjustments can be better made by moving
the instrument.
The lens and screen may conveniently be mounted first,
and the adjustments made so that the light collected by the
lens falls on the screen as a horizontal beam. The cross is
then to be mounted in such a position that a bright patch
corresponding to the square hole is seen on the screen, sur-
rounded by the shadow of the card. The frame must now be
extended or compressed till the image of the cross appears in
the bright patch ; and the lens, object, and screen should then
be carefully set square by hand before the final adjustment.
If the vertical and horizontal lines of the cross do not focus
simultaneously, it is a sign that the lens needs setting square.
The focussing having been completed, the distance of the
object from the image is to be measured and divided by four.
This will give the focal length ; and the calculation can be
checked by measuring one or more of the four equal parts
into which the distance is divided by alternate pins. Owing
to slight play in some of the joints, or other mechanical
imperfections, the theoretically equal distances may exhibit
sensible differences, especially when the frame is nearly
closed up; but the method of observation is so well con-
ditioned that these inequalities do not practically affect the
correctness of the result.
In fact, if the distances of the lens from the object and
image, instead of being exactly equal, are a+ and a—2,
2
2a
fourth of the whole distance we are simply neglecting 2? in
comparison with a?. Suppose the two distances a+a and
a—x to measure 203 and 194 inches, which is a larger
inequality than is likely to occur, the ratio of 2? to a? is 1 to
1600 ; and this error is negligible, in view of the fact that
the doubt as to when the image is sharpest involves an un-
certainty in the focal length to the extent usually of more
than one per cent. :
When the focal length does not exceed 10 or 12 inches,
the instrument may be supported with the two hands and.
pointed towards a gas-flame, which need not be at the same
level, but may be at any height. A fairly good measure-
ment can thus be made by one person, if there is opportunity
for setting the instrument down on a table or floor when the
lens needs setting square, and when the final measurement
of distance is to be made. The friction at the joints of the
2
the true focal length is rs , and in taking it to be one
new and handy Focometer. Boe
frame is just sufficient to keep them from working while the
instrument is being carefully set down. The chief difficulty
is from flexure.
Instead of receiving the image on a screen, it can be viewed
in mid air. For this purpose I mount the cross on one of
the two end clips, and a piece of wire gauze about the size of
the palm of my hand on the other, setting the wires at a
slope of 45° by way of contrast with the upright cross. The
end which carries the cross should be turned towards the
strongest light; as this renders the cross more visible to an
observer behind the gauze, and also renders the glistening
wires of the gauze more visible when the observer stations
himself behind the cross. The adjustment for focus is made
by lengthening or shortening the frame till parallax is re-
moved. This is a very convenient way of establishing
experimentally the fact of the interchangeableness of object
and image.
The instrument can also be employed to illustrate the
general law of variation of conjugate focal distances, the lens
being for this purpose shifted from the central pin to any one
of the other pins, and the frame being then extended till the
image is correctly focussed. Regarded as an optical bench,
the instrument is remarkably light and handy. Its weight,
including screen, cross, wire-gauze, and lens, is 2 lb. 10 oz. ;
and a lecturer can carry it through the streets of a town
without inconvenience.
The dimensions and number of bars of the instrument as
exhibited are recommended as the most convenient for general
purposes. Ten bars only were constructed for the first trials,
and any number included in the formula 4n+2 might theo-
retically be employed.
In order to prevent looseness at the joints, it would be well
to make the holes in the bars bear against a cone below and
another cone above, with a very slightly tapering wedge for
adjustment, as indicated in fig. 3.
If the instrument were to be set up permanently in one
place, guides might be used for compelling the middle row of
pins to travel without rotation, or the pin on which the lens
is mounted might be a fixture; but as long as portability is
to be preserved, | do not think that any arrangements for
automatically preventing rotation would be practically bene-
ficial. It is only in the large movements which precede the
final adjustment that rotation occurs to any injurious extent.
The instrument has been constructed from my drawings by
Messrs. Yeates of Dublin, and the cost is trifling.
[ 388 ]
XXXIV. A Hydrodynamical Proof of the Equations of Motion
of a Perforated Solid, with Applications to the Motion of a
Fine Rigid Framework im Circulating Liquid. By G. H.
Bryan”.
Introduction.
iE 1 the whole range of hydrodynamics, there is probably
no investigation which presents so many difficulties
as that which deals with the equations of motion of a per-
forated solid in liquid. The object of the present paper is to
show how these equations may be deduced directly from the
pressure-equation of hydrodynamics, without having recourse
to the laborious method of ignoration of coordinates. ‘The
possibility of doing this is mentioned by Prof. Lamb in his
‘Treatise on the Motion of Fluids’ (pp. 119, 120), but he
dismisses the method with the brief remark that in most cases
it would prove exceedingly tedious. I think, however, that
it will be admitted that the following investigation is more
straightforward and simple than that given by Basset in his
‘ Hydrodynamics,’ vol. i. pp. 167-178.
The usual method presents little difficulty when the motion
of the liquid is acyclic, because the whole motion could in
such cases be set up from rest by suitable impulses applied to
the solids alone; anda consideration of Routh’s modified
Lagrangian function shows that in this case the equations of
motion can be obtained by expressing the total kinetic energy
as a quadratic function of the velocity-components of the solid
alone, and applying the generalized equations of motion re-
ferred to moving axes.
If, however, the solid is perforated, and the liquid is cireu-
lating through the perforations, this method presents several
difficulties. If the solid were reduced to rest by the applica-
tion of suitable impulses, the liquid would still continue to
circulate through the perforations, the “ circulation ” in any
circuit remaining unaltered. From this and other circum-
stances we are led to infer that these circulations are not
generalized velocity-components, but rather that the quan-
tities xp are generalized momenta. Now the kinetic energy
of the system is naturally calculated as a function of the
velocity-components of the solid and of these constant circu-
lations (or the corresponding momenta) ; a form unsuited for
obtaining the equations of motion. We ought either to have
the kinetic energy expressed in terms of generalized velocity-
components alone, or to know the “ modified Lagrangian
* Communicated by the Physical Society: read February 24, 1893.
Equations of Motion of a Perforated Solid. 339
function ” obtained by “ignoring” the velocity-components
corresponding to the constant momenta or circulations. Hither
of these expressions involves constants which cannot be deter-
mined from the ordinary expression for the energy alone, and
to determine them in the usual way it is necessary to resort
to arguments based on a consideration of the “impulse” by
which the motion might be set up from rest.
In the following investigation the equations of motion are
deduced from purely hydrodynamical considerations, and from
them the modified function is found. In §§ 12-16 the equa-
tions of motion are interpreted for the case in which the solid
is a light rigid framework and the inertia is entirely due to
the circulation of the liquid, and the results are applied to
interpret the effective forces of the cyclic motion for a per-
forated solid in general.
General Hydrodynamical Equations.
2. Let a perforated solid bounded by the surface 8 be
moving through an infinite mass of liquid (density p) with
translational and rotational velocity-components wu, v,w, Pp, J, 7,
referred to axes fixed in the solid, and let «,, «2, K3...Km be
the circulations in circuits drawn through the various aper-
tures. Then we know that ¢@ the velocity-potential of the
fluid motion may be expressed as a linear function of the
velocities and circulations in the form
p=udut vpyt whut phy t Why t?hrt Zk. + (1)
where evidently ¢,=0¢/du &c., and the coefficients dy...
depend only on the form of the solid.
If dy denotes the element of the normal to S measured
from the solid into the liquid, (/, m, n) its direction-cosines,
then, in the usual way, we have
oe =I1(u—ry +92) +m(v—pzt+re)+n(w—getpy). . (2)
The six coefficients gy... are single-valued functions of
the coordinates, while the coefficients ¢, which determine the
part of the velocity-potential due to the circulations are cyclic
functions making Q¢,/Qv=O0 at the surface of the solid; these
coefficients are supposed known for each form of solid, although
their determination in any given case is generally beyond the
range of mathematical analysis.
3. Let oj, o2,...0, be barriers drawn across the perfora-
tions ; then, in the usual way, the kinetic energy of the liquid
340 -Mr. G. H. Bryan on the Equations of
is found to be J, where
; 3
t= 1p |\p2% a+ 4px ||P do=B.+K. B3)
Here J, is a quadratic function of the velocity-components of
the solid, and is the kinetic energy when the motion is acyclic,
and K is a quadratic function of the circulations.
If the axes were fixed in space, the pressure equation
(supposing no forces to act on the liquid) would be
Pi , of
pot
(where p; = pressure, g, = resultant velocity of liquid).
Owing to the motion of the axes, however, O¢/Q¢ must be
replaced by the rate of change of ¢ at a fixed point, that is by —
+3$9,)’=const.,
dp aan ee op an) O° o¢
a. Uo te) a — sep tet) a ee
whence the pressure equation becomes — |
Pi, Uh ae OG _ pede OF _ = we
me ee) (wv RUS, (5 2
+39°= const. eae 5 | st.)
The Mutual Reactions between the Solid and Liquid.
4, Let X,, Y;, Z;, L,, M,, N, be the component forces and
couples which the solid exerts on the liquid ; then we have
evidently
Seas L, = \\ (ny—mz) p, dS. 21s GD)
_ To reduce these expressions to the required form, we shall
have to resort to repeated applications of Green’s formula.
Since the velocity-potential @ is a multiple-valued function,
it follows that in transforming volume integrals involving }
we shall obtain surface integrals over the barriers 01, dg,... Om
as well as over 8S the surface of the solid. On the other hand,
the pressure p, and the velocity-components 04/02, 0¢/dy,
0¢/02 are single-valued and do not contribute barrier terms
to the surface integrals. Moreover, since the circulations «
are independent of the time,
OF = Ub, +E, FI, + D4, +98, 476,
and 0¢/0¢ is therefore a single-valued function of the velocity-
components of the solid satisfying Laplace’s equation.
Motion of a Perforated Solid in Liquid. B41
We also notice that
Ody feke)
l= a Ye ao ate mare tts (6)
as may be at once seen by differentiating (2) with respect
to w and p respectively.
Substituting for p, in (5) in terms of the velocities, we
have
=e sale ds
p :
+ {lf (u—yr + . + (two similar) F1US
—al|{ (Sey y+ (38) ] pee
The first line of a expression is, from (6), equal to
ee Ou
a eerar rome
by Green’s transformation. os. that @, is inde-
pendent of the time, this integral, taken throughout the liquid,
becomes
=523 2 al|i{ (S*) ey (82) } ans -
pot OL ILS) esa
~ pdtou pot ou —
By Green’s transformation the second line is equal to
={\\3 { (u—yr + 2q) oF + (two similar) \ dx dy dz
= ~ {{\(-22 ¢ at a) dx dy dz
-\\\f (u—yr + 2q) 2 + (two similar) ae dy dz,
which by a second application of Green’s transformation
becomes
Oo
49 Mr. G. H. Bryan on the Hquations of
=\| (mr—ng) dS —Zx\\(mr—ng) do
+ (V{2(u —yr+2q) + m(v—eptar)+n(w—agt+ yp) $ Seas
0p oe
=(\(mr —ngq)odS— Sxc\\(m —ny)do +\| ae ds
by (2).
Lastly, the third line of (7) is, by Green’s transformation,
"(Bb9% , 96 B'S , BH dS
={\\{8 Seo SRORRUN e serps p aedyde
“(£29247
Ov 02 a
Hence, adding the several terms together, we have
The
~ dt Ou
1p {p\\modS = S«p\\mdo} — qip\\nodS _ Sxp\\ndo} 8)
Now by (6),
p\\mddS=p Obe 478
i {| Ov
-e|\| OPIS: , BHIb. , BHO»
a Ode
=Sep| Be Sane AF an aie ~~ \da dy dz
~sl] ie Zaof NG) + REF) Jere
= ao | 2 eee
Therefore
ie = g2_, £2 , aaa we a ”) da}
+9 { S= oe " Cia
6. In like manner we have
— ae-{f (ny —mz) as
+]| | (u~yr+ - a (two similar) (ny—mz)dS
Motion gi 6,08 Solid in Liquid. 343
LO +B“ 08) Jom
“Hboe Yas) (v5! - so) du dy dz
— ||) fy { e-yrte0) 2 + (tro. similar)? 9%
=z} (w—yr+ 2q) o + (two similar) a dx dy dz
On
060 , Of 0 , 060)/(,0b_,0¢
oe By t Bebe) Uae: 0 y Naadyde
eee 02
pdt op
Bs (two sim.) poste ve - $98
—\\\[o(9s 5 eave “(P5o
fol ‘ oe)
Shey yp eee Se Gye 9) — \da dy dz.
(v—zp+2r) e + Cw “g+yp) By c dy
Remembering that in this expression one factor of the
surface integral is zero at every point of S, we have, by
again applying Green’s transformation to the volume integral,
ar
made Op
+w{ p\\m dds —Zxp\\mdo} —vf p\\npdS —Sxp\\ndos
+r{p\\(l (le—nx) dds — —Xxp\\( (lz—na)do}
—qip\\ (ma—ly) ddS — — xp \\ (ma—ly\do$ . . (10)
Now, just as before,
(le—mn)bdS= p || Pega
all = =Sxp || 2 , da
2, (ieee 388, feb Od, 738 08, \ zi a:
alll oe
= Seo (( 0% gq ©
=3ep [|Site 0g’
344 Mr. G. H. Bryan on the Equations of
Therefore,
d OL
1 = dt Op
—w foe + Sep ||(m — oP de \
tne) ge a eo {| (n— =) da |
7 1 oe + xp | (t: —nw— ee da \
+g = == Sap || (may eae} Beene ul
Application to the Equations of Motion.
7. The equations of motion of the solid may now be written
down at once. Let 3! be the kinetic energy of the solid, T
the total kinetic energy =%+ ‘3! ; and suppose that the motion
takes place under the action of a system of external impressed
forces and couples designated by X, Y, Z, L, M,N. Then
the effective forces and couples to which the motion of the
solid itself is due are X—X,..., L—L,..., respectively, and
the six equations of motion of the solid referred to the moving
axes are of the form
dIOS LOS! Hawes! ,
dau "90 ' 230 ~~ 9 ne
AS) SSG Sole Se
tn Se ; q
dt Op Ov w OY or
Hence, on substitution, we see that the required equations
of motion are found by writing T tor J and X, Y, Z, L, M,N
for X,, Y;, Z;, L;, My, N, in equations (9) (11). The resulting
equations may be written :
x= 55, -"(85 +7) +{& +5) yr (14)
t= ae = 0(S +0) 40o(& +6)
=L—1L,. e (13)
where &, 7, &, d, “, v are defined by the equations
Motion of a Perforated Solid in Liquid. 345
g = 2xp|| (I 2 ada, de, ee (16)
N= sep || (x (ny— mz— 928 \do, ewe te ce El)
As Lamb has pointed out (‘ Motion of Fluids,’ p. 140), the
six quantities (&, 4, ¢, A, w, v) are “the components of the
impulse of the cyclic fluid motion which remains when the
_ solid is (by forces applied to it alone) brought to rest” *. They
are linear functions of the circulations and their form depends
on the form of the solid. If there is only one aperture they -
are all proportional to the circulation «.
The Modified Lagrangian Function.
8. We shall now show that the motion of the solid can be
determined in terms of Routh’s modified Lagrangian function,
and shall find the form of this function for the system.
Putting.
H=T+éEu+nvt+Gwt+rAptpqtvr+F (kp), . . (18)
where F'(«p) denotes any function whatever of the quantities
Kp, we see that the equations of motion reduce to the standard
form
@ lel oat lal
ir iu eae (iey
OE ele! OH “Olt. @ils! :
The function H, therefore, plays the same part in deter-
mining the equations of motion of the solid as the kinetic
energy T in the case of an imperforated solid (or any solid
when the motion of the liquid is acyclic). It remains (i.) to
determine what quantities are to be regarded as the generalized
velocities if the quantities xp are regarded as generalized
momenta ; (ii.) to find the form of the function F(«p) in order
that H may represent the modified Lagrangian function.
9. Let y,, be the generalized velocity-component corre-
sponding to the ignored momentum «,p. Then, as Routh has
shown (‘ Rigid Dynamics, vol. 1. § 420), the modified La-
grangian function H is of the form
Ev > in PNR Oe hal F<. ce ts. E28)
* Our & 7, 6, A, w, v are the same as the &, no, fo, A 0) Hoy Yo Of Lamb, or
the’ X,Y), 3, &, Mi, "I of Basset’s § Hydrodynamics.’
346 ‘Mr. G. H. Bryan on the Equations of
and therefore by equating the two expressions for H we must
have
Eutnutfotrptpqtwr+F (x) =—ZKpy. . ~ (22)
Since y,, is the generalized velocity-component corre-
sponding to the momentum kmp, therefore
oH
0. Kp = Xm ° . ° ° e (23)
Now H is a homogeneous quadratic function of the six
velocities (u...,0...) and the momenta xp; therefore
| oH oH oH
2H =2u s- + Sxp sae == 7 —Xkpy. . (24)
Hence, from (21), .
H H H
2139 + Sepy = Sud Sapo AS 5)
The portions of T and H which involve only the momenta xp,
and are independent of the six velocities (u..., p...), must
arise from the terms 2«py in the above expressions (24) (25),
and must therefore be equal and of opposite sign in the ex-
pressions T and H respectively. Hence, since from (8)
T=2'+3,+K,
the portion of H which is independent of the six velocities
(@..., p...) must be —K, so that,
H=2/4+ 31+ (ut nut Gwt+rApt+pyqtvr) —K
=T +(Eutnvtcwt+rAptuqtvr)—2K, . . (26)
and therefore F(ep)=—2K. ..
The function F'(«p) does not enter into the six equations of
motion of the solid, but its form requires to be determined if
we wish to reduce the equations of motion of the whole
system to the canonical or Hamiltonian form.
The Generalized Velocities and Momenta.
10. Comparing (21) with (27), we see that
LKpX=2K—(Eu+ nu+lwt+rApt+puyqt+vr). . (28)
Now equation (3) may be written in the form
Bigg ih) malas +...tp,+...+2«,)d8
+24 2 (ug, + 1 tpbyt...+ 2kde)do. (29)
Motion of a Perforated Solid in Liquid. B47
~ But by § 2, 0¢,/0v=0 all over the surface 8 of the solid.
Hence, equating the terms independent of the six velocities
(w...,p...) on the two sides of (29), we have
79 C= , », v being integrals taken over the
finite surfaces of barriers are in general finite.
If we choose as our axis of wx the Poinsot’s central axis of
the impulse whose six components are &, 7, £ Ar, @, v, the
modified function will reduce to the form
H=ButAp—Ki eee
If there is only one aperture, &,7,¢, 2, u,v are all pro-
portional to the circulation « and the central axis of the
impulse is fixed in position relative to the solid: if there are
several apertures the position of the axis depends on the
ratios of the circulations through the various apertures, but
throughout the motion it in every case remains fixed rela-
tively to the solid.
The six equations of notion (19) (20) now reduce to
rl); 0, )
Nears, M=wE+rA, " 54.) ee
)
Motion of a Perforated Solid in Liquid. 349
Since these equations do not involve w or p, we see that
no forces will have to act on the solid in order to maintain a
screw motion whose axis coincides with the central axis of the
umpulse.
13. To interpret the equations still further, let us suppose
that w and p are both zero, since they do not enter into the
equations of motion. ‘Then the motion whose components are
(0, v, w, 0, g,7) consists of two screws whose axes are the axes
oi y and z respectively, and, by the theory of screws, these
are equivalent to a single screw whose axis is a certain
straight line intersecting the axis of # and perpendicular to
it. We may take this straight line as our axis of ¢, for
hitherto we have only fixed the position of the axis of «.
We have then
v=0, g=0.
The equations (34) therefore reduce to
4
xXx—(; L=0,
Y=7e, M=we +a} eee too)
Zi=), N=0:
Hence the solid is acted on by a wrench (Y, M) whose axis
is the axis of y. Thus the axis of the impressed wrench is
perpendicular to the central axis of the impulse of the
fluid motion, and to the axis of the screw motion of the body.
Let II be the pitch of the impulse, w the pitch of the
screw motion of the solid, P the pitch of the impressed
wrench, then |
A w M
N=5, ee Pay
and therefore by (35), |
Pesan LL fae Aisa ok: 1a (Gl)
is the relation connecting the three pitches.
In particular, if » = 0 the equations of motion give
Z=0, M=wé#,
showing that a couple M about the axis of y will produce
translational motion with velocity M/E along the axis of z.
14. More generally, let the motion be a screw motion
about an axis whose inclination to the axis of w is @ and
whose shortest distance from that axis is a. Take this
shortest distance as the axis of y, and let the screw motion
consist of a linear velocity V combined with an angular
velocity ©, the pitch V/O being denoted, as besore, by a.
Phil. Mag. 8. 5. Vol. 35. No. 215. April 1893. 2B
350 Mr. G. H. Bryan on the Equations of
It will be readily found that the six components of the
screw motion are
u=Vcosd+QOasiné, p=Ocosé,
v=0, q=9, 3 - (87)
w=VsinOd—Qacosé, r=Qsin 8,
so that the equations (34) now give
A=0, 1;=0,
Y=02siné, M=VEsin@—Oaz cos 0+0A sin | (38)
=: N=0,
The impressed wrench therefore has for its axis the shortest
distance between the axis of the screw motion of the solid
and the axis of the impulse of the cyclic fluid motion. To
find the pitch of the wrench, we have, by division,
= = 5 —a.cot 0+ =
that is,
P= e—acot@+Il. .. 7) yee
15. In the case of a fine massless circular ring A vanishes,
or the impulse of the cyclic motion is purely translational.
For it is clear that the axis of the ring is the axis of this
impulse (the above axis of z), also the fluid motion will
evidently be unaffected by rotating the ring about its axis;
and therefore the modified function is independent of the
angular velocity p.
The equations (34) now become
K—0; L=0,
Se), M=we, | (40)
ZL=—q2, N=—vée.
Hence a constant force Y along the axis of y causes
uniform rotation with angular velocity Y/E about the axis
of z, and a constant couple M about the axis of y causes
uniform translational velocity M/E along the axis of z.
It is to be noticed that the impressed wrench never does
work in the resulting screw motion, in accordance with the
principle of Conservation of Energy.
16. The above results show the effective forces produced by
circulation of the fluid on any perforated solid whatever. In
the general case the modified function contains the quadratic
terms 2+, in addition to the terms of the first degree con-
sidered in the above investigation. If we suppose that the
solid is moving in any given manner, the six equations of
motion (19, 20) determine the components of the impressed
wrench (X, Y,-Z, L, M, N) necessary to maintain the given
Moton of a Perforated Solid in Liquid. 351
motion. This impressed wrench may be divided into two
parts, one being due to the terms 3/+2Z, in the modified
function, the other being due to the terms
Eutnvt+ GwotrAp+pg+yr.
The first portion is the same as if the motion were acyclic,
and represents, therefore, the wrench which would have to be
impressed on the solid in order to maintain the given motion
if there were no circulation. The second part represents the
additional wrench which must be applied on account of the
circulations, and the equations to determine it are of the forms
found above.
We notice, in particular, that if the solid has any screw
motion whose axis coincides with the axis of the impulse of
the cyclic fluid motion, the latter wrench vanishes; so that
the forces required to maintain the motion are unaffected by
the circulations. In other cases the additional wrench is
about an axis perpendicular to the axis of the impulse. This
is true whatever be the form of the solid and the number of
the circulations ; but, as has already been pointed out, the
position of the axis of the impulse relative to the solid is not
in general independent of the circulations unless the solid has
. but a single aperture.
It is probable that these results might be made to furnish
mechanical illustrations of certain physical phenomena ; but
with these we are not concerned in the present paper.
Note on the foregoing Paper.
Concerning the proper measurement of the impulse of the
eyclic motion, a difficulty arises ; for, as Mr. Bryan remarks,
this motion cannot be set up from rest by impulses applied to
the solid alone. Suppose, however, that we close each perfora-
tion by a barrier in the usual way, and let the barriers be acted
on by the impulsive pressures xp, K.p,... respectively. And
instead of these impulsive pressures being due to external
forces, suppose that they are due to some immaterial mechanism
attached to the solid. In general, an impulsive wrench must
act on the solid to keep it at rest, and this wrench ts the
required impulse of the cyclic motion; for the only other
impulses acting on the system are due to the mutual reactions
of the solid and fluid, exerted partly over the surface of the
solid and partly through the barriers and attached mechanism,
and such mutual reactions cannot affect the impulse. The
wrench thus found is of course the same as would be
obtained by supposing the impulses on the barriers to be due
to external impulsive forces, and compounding with these the
2B2
352 Mr. G. H. Bryan on the Equations of
impulse then necessary to hold the solid at rest. This is in
agreement with Prof. Lamb’s investigation, which Mr. Bryan
has quoted.
More generally, if the solid is in motion, and the liquid is
also circulating, we may suppose the instantaneous motion to
have been set up from rest by an immaterial mechanism con-
necting the barriers with the solid at the same time that the
requisite external impulses act on the solid. The resultant of
these last is, as before, the impulse of the whole motion, and
is identical with that found by supposing the barriers actuated
by impulses from without, and compounding with these the
impulse then necessary to give to the solid its instantaneous
motion.
The same point may be further illustrated by supposing the
circulations « to vary continuously during the motion. To
effect this variation we may suppose finite uniform pressures,
P,...P,,, to be exerted over certain ideal surfaces which
occupy the positions of barriers. The rate of variation x of
any circulation is given by P=xp, and in order that it may
take place without the direct operation of external forces and
couples we may conceive the pressure P to be due, as before,
to some highly idealized mechanism attached to the solid. As
before, the only forces capable of modifying the impulse are
the external forces acting on the solid ; and the equations of
motion are therefore still to be found by equating the
impressed force- and couple-components to the corresponding
variations of the ‘‘ impulse.” Since we know the expressions
for the impulse-components corresponding to a given instan-
taneous motion of the solid and given circulations, we have
only to remember that in these expressions the «’s are
functions of the time, and, just as before, the equations
of motion are directly deducible from Hayward’s formule.
Hquations (19) (20) of Mr. Bryan’s paper will thus be
applicable to the present case, provided that in the value of H
given by (27) the «’s are allowed to vary. 7
An investigation proceeding from a consideration of the
impulse of the whole motion is not so entirely satisfactory, I
think, as the direct method given by Mr. Bryan ; but, at the
same time, this brief attempt to interpret the impulse of the
cyclic motion may not be without interest.—C. V. Burton.
—
Note added by the Author.
Dr. Burton’s note is of much value as showing more
exactly what is meant by the “ impulse ” of the motion in the
Motion of a Perforated Solid in Liquid. 353
ordinary investigations given by Prof. Lamb, and, in a less
intelligible form, by Basset.
The equations of motion under finite forces may be deduced
by equating the change of momentum in a small time-interval
d¢ to the impulse of the impressed forces, taking into account
the fact that in the interval 6¢ the origin has a displacement
of translation (wdz, vdé, wot) and the axes have rotational dis-
placements ( pdt, g6t, 76¢), so that the final momenta are referred
to a different set of axes to the original momenta.
The mode of forming the equations of motion is given by
Prof. Greenhill (Encyclopedia Britannica, art. “ Hydro-
mechanics ’’) for the case of acyclic motion, but it is hardly so
obvious why in thus forming the equations of motion of a
perforated solid, it is necessary to include in the “impulse”
terms representing the components of the wrench applied to
the barriers as well as to the solid. We may, however, sup-
pose the changes which actually occur in the time o¢ to have
been produced as follows :—
1st. Let the solid and fluid be reduced to rest by an impul-
sive wrench applied to the solid, and transmitted to a series of
barriers crossing the perforations. The components of this
~wrench will be found to be
ot or
au + &, SCT ap +r, &c. ...
2nd. The barriers being rigidly connected with the solid, let
the latter receive small displacements whose translational and
rotational components are (wot, vdé, wot, pdt, godt, rdt) and let
the solid come to rest in its new position. The fluid will
evidently also come to rest, and therefore no impulse will be
impressed on the system by this change (as may be otherwise
seen by supposing the change to take place very slowly).
3rd. Let the solid be set in motion with velocity-compo-
nents (w+ Qu/dt.dt,... ptdop/dt.dt...) referred to the
new positions of the axes, and let the circulations « be started
in the new position of the solid by a suitable impulsive wrench
applied to the solid and transmitted from it to the barriers.
Then the impulse of the impressed forces (components
Xdt..., Ldt...) is the resultant of the wrenches required to
stop the whole system in the first process and to start it again
in the third.
It is, therefore, that impulse which must be compounded
with the total impulse in the initial position in order to
obtain the total impulse in the final position.
Whence Hayward’s equations of motion follow at once (as
or
354 Prof. G. M. Minchin on the Magnetic
shown in Greenhill’s article above referred to), and they take
the form of the above equations (14), (15).
If we were merely to stop the solid in the first process
without stopping the liquid, the cyclic motion would cause
the liquid to exert a pressure on the solid in the second pro-
cess, and the impulse of this pressure would not be zero, but
would have to be taken into account in forming the equations
of motion. It would be wrong, therefore, to deduce the
equations of motion from the impulse applied to the solid
alone, as is evident in the analogous case of a solid containing
one or more gyrostats.
XXXV. The Magnetic Field of a Circular Current.
By Professor G. M. Mrycuty, 1.A.*
LERK MAXWELL gives a method of drawing the
lines of magnetic force due to a circular current
(‘ Hlectricity and Magnetism,’ Art. 702) by means of a series
of circles and a series of parallel lines. ‘The object of the
following paper is to show how these curves can be described
by a slightly different method, and to exhibit the geometrical
connexion of the series of circles.
Let AQBQ' be the circular current whose sense is indicated
by the arrows, the plane of the circle being that of the paper;
Fig. 1.
ene,
~
2 fee es Se et ee
let P be any point in space, PN the perpendicular from P on
the plane of the circle, and NAOB the diameter of the circle
drawn through N. We shall calculate the vector potential of
the current at P.
Draw any ordinate, QQ!, of the circle perpendicular to BA;
and consider two equal elements of length of the circle, each
equal to ds, at Q and Q!. Resolving each of these along and
perpendicular to QQ!, we see that the latter components are in
opposite senses, and hence their vector potentials at P cancel
* Communicated by the Physical Society: read March 10, 1893.
Field of a Circular Current. 355
each other, since PQ = PQ’. If Ww is the angle QOA,
a=radius of circle, 1=current strength, the components
of ids along Q’Q being equal and in the same sense, the two
elements of current at Q’ and Q conspire in giving a vector
22 cos
PQ
Hence the total vector potential at P is perpendicular to
the plane PON. -If, therefore, OA is the axis of «x, the
perpendicular at O to the plane of the circle the axis of z,
and the diameter at O perpendicular to AB the axis of y,
the components of the vector potential being, as usual, denoted
by F, G, H, the only component existing is G; but, by
taking the components of the vector potential at a point
indefinitely close to P in the direction of the axis of y, we
easily find that
potential .ds perpendicular to the plane PON.
ae _G
| dy = a"
Hence if X, Y, Z are the components of the force of the
current per unit magnetic pole at P, since this force is the
curl of the vector potential, we have
dG dG G
Sa aa, Yi = (): L=— + oe?
where 2(=ON) and y (=NP) are the coordinates of P.
If along the line of force at P the increments of the co-
ordinates are Aw, Ay, we have
ae
GE VA
Hence along this line we have
AG dG G
Tn At + a + — Aas 0,
i.€., G.e= constant along the line of force.
We shall therefore calculate the vector potential, G, at P.
Hvidently
G = 2i| SON 5
0
PQ
a nd
9 VMat+a+y*?—2aecos p
e 2 "e+e pty?
avian : D —D) dp,
356 Prof. -G. M. Minchin on the Magnetic
denoting the denominator by D. Now let ~p=a—o, and
let p?=(a+a)?+9’, p?=(a—a)?+¥4”’, so that p=PB, p'=PA.
Then
ay o wT p> +p? ie, t
G= 2a‘, 1 ihe 2pA ¢ do,
[2 =
A=A/ 1—(1-§) sin? $.
7
Let o=2¢, and Bal — Gs: then, finally,
where
hia
(res <2 {pK-8)-K},
where K and E are the complete elliptic integrals of the first
and second kinds with modulus &; so that the quantity in
brackets is a function of the ratio — simply. |
27,2
Also, since p?— p”=4aa, we have a= ee
G .« which is constant along the line of force is given by the
equation
,and the quantity
G .a=ip{2(K—E) —#’K}.
It is thus seen that at every point in space G is of the
!
form . if. c ) ; so that at all points on the surface for which
: is a constant, the value of G will vary inversely as p. The
I
surface for which © is constant is a sphere having its centre
on the line BA produced and cutting the sphere having BA
for diameter orthogonally. If we assign a series of values to
!
the ratio f. we obtain a series of spheres having their centres
on BA and cutting the given sphere orthogonally, the radius
of each sphere of the series being, therefore, the length of a
tangent from its centre to the sphere described on BA; for,
given the base, BA, of a triangle, and the ratio of the sides,
the locus of the vertex is a circle whose diameter is the join
of the points which divide BA internally and externally in the
given ratio. The surface locus of the vertex is the sphere
generated by the revolution of this circle. >
Field of a Circular Current. 357
On account of the symmetry of the current round its
axis through O, the lines of force and those of constant
vector potential are the same inall planes through the axis.
We may, then, confine our attention to the plane PON,
and suppose fig. 2 to be in this plane, the current being
Fig, 2.
in this figure represented in projection by the line BA.
Describe a series of circles having their centres on BA pro-
duced and cutting the circle described on BA as diameter
orthogonally. Along each of these circles, then, the ratio ee
es e e e PB
is constant, P being any point on the circle.
Consider first the lines of constant vector potential. For
each of the circles let the value of the quantity 2 (K—E)—K
be calculated. Denote this quantity by Q for any one circle ;
then
Q — AQea
p
so that if we wish to trace out the line of constant vector
potential for which G has any given value, we can find the
point, P,in which it cuts any circle of the series by measuring
358 Prof. G. M. Minchin on the Magnetic
the length PB such that
4
_ 4Q
PB=-G. 4.
Let PT be any circle of the co-orthogonal series cutting BA
at nand m. Then for this circle
i
p Bn mB’
and if this ratio is denoted by s, it is well known that
Or Ue
Cam
where C is the centre of the circle. Now the modulus, &, of
the elliptic integrals which belongs to the circle mPn is
Ag
1 Pe) he Ba1—sts hence
AB
2 AD
a BC’
or the square of the modulus is inversely proportional to the
distance, BC, of the centre of the circle from B.
The circles employed by Clerk Maxwell in drawing the
lines of force can be easily shown to be this co-orthogonal
system whose centres are ranged along BA produced. For,
his rule is to assign a series of values to @, and construct
a series of circles whose centres lie on BA, the radius of
each being 5 (cosec 6—sin @), while the distance of its centre
from O is 5 (cosec 9+sin @) ; the modulus belonging to this
circle is sin 8. For the series of circles he then calculates
the values of the expression (constant for each circle)
sin 6
(K—H)
assigned line of force is found by drawing a certain right
line perpendicular to BA. It is at once found that this
series of circles is precisely the co-orthogonal system above
described ; but Clerk Maxwell’s modulus is not the same
, and the point on each circle which lies on any
!
function of the ratio = or of the radius of the circle selected,
Pp
as that adopted above; for, with Clerk Maxwell, if r is the
radius of any circle of the series and & the corresponding
modulus,
es (z— k),
2 \k
Field of a Circular Current. 359
whereas above we have
_2V71-#
f= je eo.
Of course (as stated in a note by Clerk Maxwell) the elliptic
integrals depending on the one modulus can be transformed
into elliptic integrals depending on the other ; and in this
case the transformation is the well-known one of Lagrange.
But the constructions for the points in which any given line
of force cuts the series of circles will not be the same in both
cases—those of Clerk Maxwell depending on a series of right
lines perpendicular to BA, and those above indicated de-
pending on a series of radial distances from B.
When we propose to draw the line of constant vector
potential through any point, P, which lies on a circle whose
constant is Q,, let PB be p); then the point, R, in which this
line meets any other circle, whose constant is Q,is found from
the relation
men
he Ge
where p= BR.
This latter method has a certain advantage for the eye,
inasmuch as it enables us to see readily those circles of the
series outside which the line of constant vector potential
through any proposed point lies.
Consider now the lines of force. With the above value of ©
Q, the quantity which is constant along a line of force is
p.k’Q, so that on each of the above circles in fig. 2 we must now
mark the number £?Q. Denote this by Q’. Then the above
relation for points on the same line of constant vector potential
becomes for the lines of force
/
p=
and the construction proceeds in the same way. The con-
stants, Q’, for the above series of circles, beginning at the
innermost, are :—
"A841; :4301 ; °3775; °3396; °2782 ; °2376; :1954; °1727.
. The values of the Q’s diminish outwards for the circles; so
that if we consider the line of vector potential at any point,
S, suppose, which is such that SB is greater than the distance
from B of the point along AC in which any circle interior to
that passing through 8 cuts the line BAC, it is at once obvious
that the line of vector potential which belongs to 8 is wholly
outside all such circles. The numerical values of Q for the
360 Prof. G. M. Minchin on the Magnetic
circles in fig. 2 are marked at the circumferences, and as much
of the line of potential belonging to P is drawn as is justified
by the number of circles represented in the figure.
The fundamental proposition of electromagnetism is that
the intensity of magnetic force produced at any point in
presence of electric currents is the curl of the vector potential
Fig. 3.
A P Q B
P
0
at the point. But if in the field there is a current in an in-
finitely long straight wire, AB, we find that at every point in
the field the vector potential due to this current is infinite.
Hence it seems impossible to deduce the magnetic force, and
the lines of magnetic force, from the above fundamental pro-
position. This result is unsatisfactory, and it manifestly points
to some defect in our definition of the vector potential.
We are presented with a similar unsatisfactory result in the
general theory of gravitation potential. Thus, taking the
common definition of gravitation potential, if AB is a limited
uniform bar attracting according to the law of inverse square,
we know that the potential which it produces at any point,
P, is proportional to log (cot > cot =) where A= 7 PAB;
B=ZPBA. Now, if the rod extends to infinity, this ex-
pression becomes infinite. I have shown (‘ Statics,’ vol. ii.
Art. 332) how this difficulty arises, and how it is to be
remedied by mending the definition of potential. The diffi-
culty is avoided in a similar manner with regard to the vector
potential.
Thus, since we are concerned only with differential co-
efficients of the vector potential, the ordinary components,
F, G, H of this vector may have added to them any constant
quantities whatever. This amounts to saying that the vector
potential at any variable point, P, in the field is the vector
potential at any fixed point, O, plus the vector difference
between P and O. It does not matter whether the vector
at O is infinite or not: it is a constant in the field. As in
the general gravitation field we are concerned with dzjerences
Field of a Circular Current. 361
of potential only, so in the electromagnetic field we are
concerned with vector differences only.
Let us, then, calculate for the infinite straight current AB
the vector difference between P and a point O on the per-
pendicular, Pp, at a constant distance Op=a from the line.
Let Pp=r, and let an element, ds, of the line AB be taken
at any point, Q; let 2pPQ=0. Then the vector difference,
Ea hdis ds
due to this element, at P is OP —Q07™
M7 + (a—2") cos’OS * cos 6"
Double the integral of this from 0=0 to 0= 5 is the vector
difference at P due to unit currentin AB. LHxpanding the
Py poe
ge )s we have the
radical in ascending powers of » Cc 3
vector equal to
0. ee ee Lac
2f {an 7g 008 Ot oe ate COW 6 oo Palen)
=—4$n? +40? —FAt+ sirens
and this=log,(1 +) =2 log- . Thus, then, the vector dif-
ference at any point, P, is measured by
C—2 log»,
where C is a constant; and this gives the known value of
the magnetic force at P, viz., — a (where G is the vector
potential), perpendicular to the plane PAB, i.e. where &
i
isa constant. In this way, then, the inconvenience of deal-
ing with an infinite vector potential in presence of an infinitely
long (or very long) straight current is avoided.
e lines of constant magnetic potential, or the loci of
points, P, at which the given circular current subtends a
constant conical (“solid”) angle, are the orthogonal trajec-
tories of the lines of force, and can be drawn when these
lines are drawn.
It is not easy to draw these equipotential curves independ-
ently, or even to deduce their typical equation from that of
362 Prof, G. M. Minchin on the Magnetic
the lines of force by the mathematics of orthogonal trajec-
tories.
The magnitude of the conical angle subtended at any point
by a given circle can be expressed in finite terms by means
of complete elliptic integrals of the third kind. The para-
meter involved in these integrals will depend on the way in
which they are taken.
If a sphere of unit radius is described round P as centre,
and lines are drawn from P to the points on the circum-
ference of the given circle, BMAI, fig. 4, these lines will
intercept on the sphere a spherical ellipse, bmat, whose area
is the conical angle subtended by the circle at P. The minor
axis of this ellipse is the great circular are ab determined by
the lines PA, PB, while the major axis, mi, is determined by
the chord, MI, of the circle which subtends a maximum angle,
MPI, at P. This line is determined by drawing the bisector,
Fig. 4.
PC, of the angle BPA, meeting BA in O; then MI is the
chord through C perpendicular to the plane BAP. The
point cin which PC meets the surface of the sphere is the
centre of the spherical ellipse.
Now, given any curve, mpi, fig. 5, on a sphere of unit
Fig. 5.
radius, its area is ja cos #)dg, where, if o is any point on
the sphere inside the area, @ is the circular measure of the
Field of a Circular Current. 363
spherical radius vector op drawn to any point, p, of the curve,
and ¢ is the angle between the radius op and any fixed arc,
oa, drawn ato. If, as said, the pole o is inside the area,
goes from o to 27; but if o is outsede the curve, the area has
a different expression, viz.:—
if cos Odd,
the longitude angle ¢ obviously starting and ending with a
zero value. If o is on the curve, the expression for the area
is again different.
In calculating the area of the above ellipse it would be
natural to choose for pole (0) the point n in which the sphere
is cut by the line PN; but this leads to difficulties when the
position of P is such that n falls on the ellipse. This will
happen when P is on any perpendicular to the plane of the
circle of the current drawn at any point on its circumference;
and, moreover, the choosing of n for pole will lead to expres-
sions for the conical angle which present its values in forms
which are apparently discontinuous for points P which project
inside and outside the area of the given circle BMAI. Such
discontinuity must not exist, and to get rid of it from the
expressions requires troublesome transformations of elliptic
integrals of the third kind.
We must, then, choose for pole a point which is always
inside the spherical ellipse. The simplest point is the point
o (fig. 4), in which the sphere is cut by the line PO which
joins P to the centre, O, of the given circle. This point is,
of course, always inside the ellipse.
Let, then, Q be any point on the given circuit, and p the
point in which PQ cuts the ellipse. Taking for the fixed
plane of longitude through o the plane baP, or BAP, and
denoting the angle poa by ¢@, the area of the ellipse is
(7d —cos op)dd, i. e., 2a —{ "cos op .dd.
Denoting, as before, the position of Q by. the angle , or
QOA, we easily find, if PN=z, PO=r, ON=a,
v2
d = 6 ° © e d
vo) 27 + at gin” ap Vr,
— —ax cos
cos 00 = aaa
Pr / y+ a — Que COS yp?
Hence
ar ty 2
7” — AL COS
cos op -dp=2e | be CONN Gs EY
0 0 Vp +a’—2arcosy 2 +2° sin“
364 The Magnetic Field of a Circular Current.
Putting ~~=7—y, this becomes
dy ?
2e| Jea/1—Psi?§ — Hsin? X + 75 Paap bs STi aang SPOOR
sin
[2
where, as before, p=PB, p'=PA, and ?=1— ie . If we put
¥=2e, this becomes
if A ; ye — a? da
| naga? pA / 2? +2’ sin? 20’
where A= V 1—F?’ sin’ o.
To reduce this to elliptic integrals, we must resolve the
fraction 1/2? + 2? sin? 2 into two fractions. It is easily found
that
xo)
2+2" sin’ 20=2 +42’ (sin? o—sin* o)
=(V72+0?+a—24 sin? o)(V 2 +2?—a2+4+ 22 sin’ @).
Let v denote the sine of the angle between PO anu
the axis of the current (or PN); then the expression, after
resolution into partial fractions, becomes
vad =D i 1
akc ASN oS eee i itv iyawe)
The aia of this expression which has A in the deno-
minator is at once the sum of two complete elliptic integrals
of the third kind; and the portion which has A in the nume-
rator is easily reduced to the same form. The result is
eae a 0
where N=1—v+ > sin’w, and N! is the value of N when v
is changed to —v. Hence we have two elliptic integrals of
the third kind, one with (= ae , k) for parameter and mo-
dulus, and the other with (—
1l+y
then, we have for the oe expression of the conical
angle subtended by the circuit at P the value
ae crs aha
, #). In the usual notation,
eee eae
pr =
On Hydrolysis in Aqueous Salt-Solutions. 365
Of course it is not pretended that this expression is the
most convenient for the purposes of calculation: the approxi-
mate value of the conical angle which is given by a series of
spherical harmonics is that which should be employed; but
it may be well to give the complete expression in the above
form, which I have not seen published anywhere.
XXXVI. On Hydrolysis in Aqueous Salt-Solutions.
By Joun SHE Ds, B.Sce., Ph.D.*
e)* dissolving potassium cyanide in water it is partially
decomposed into potassium hydrate and hydrogen cya-
nide. This action of the water in producing decomposition is
ealled hydrolysis. Probably all salts are hydrolysed in aqueous
solution to a certain extent, but in the majority of cases the
amount of hydrolysis is so excessively small that the means
which we have at our command are not sufficiently delicate to
enable us to detect it. Besides the salts there is another im-
portant class of compounds, namely the esters, which are sus-
ceptible to hydrolysis on being mixed with water. Methyl
and ethyl acetate, for example, are decomposed by water to a
considerable extent into acetic acid and the corresponding
alcohol. The extent to which hydrolysis takes place is regu-
lated by the law of mass action as enunciated by Guldberg and
Waage. In all cases we are dealing with a state of chemical
eden or balanced action which is usually represented
thus :—
KCN + HOH =— KOH+HCN,
or
CH;,COOC,H; + HOH =— C,H;0H + CH;,COOH,
the sign =—— being substituted for the ordinary sign of
equality as suggested by Van’t Hoff.
Now, a priori, we should expect a substance, for example
potassium cyanide, which is formed from chemically equivalent
quantities of acid and base to be neutral, and we have every
reason to believe potassium cyanide, as such, to be so. Its
solution in water, however, as is well known, has a strongly
alkaline reaction, and the above explanation of hydrolysis
furnishes us with no reason why the solution should react
alkaline rather than acid, since the hydrolysed fraction of the
potassium cyanide still exists in the solution as chemically
equivalent quantities of acid and base. Here Arrhenius’
theory of electrolytic dissociation comes to our aid, and shows
us that although we may have in the solution equivalent
* Read before the Swedish Academy of Science, Stockholm, 11th
January, 1893, Communicated by the Author.
Phil. Mag. 8. 5. Vol. 385. No. 215. April 1893. 2C
Pe ir,
ern dope? 2 TD
366 Dr. J. Shields on Hydrolysis
quantities of potassium hydrate and hydrogen cyanide, yet the
former is very largely dissociated into its ions, and, therefore,
in a particularily favourable state for entering into reaction
with the indicator, whilst the latter is not so. Accordmg to
the same theory, if we add other salts to a solution of hydro-
eyanic acid, which, per se, is only slightly electrolytically
dissociated, then the amount of dissociation is diminished
many thousand times, and this is practically what occurs in
the solution under consideration. The presence of the un-
hydrolysed potassium cyanide causes the dissociation ratio of
the hydrocyanic acid to be vastly decreased. |
‘There are salts, on the other hand, whose solutions have an
acid reaction. This is due to the fact that the acid, which is
one-of the products of hydrolysis, is more highly electrolyti-
eaily dissociated than the base which is formed at the same
time. Usually the above facts are expressed by saying that
the base is stronger than the acid, or vice versa.
if hydrocyanic acid were as nearly completely dissociated
as hydrochloric acid is, at the same dilution of course, then
probably a solution of potassium cyanide would be as nearly
neutral as one of potassium chloride, for Ostwald has pointed
out that all acids when completely dissociated are equally
strong.
In this memoir, salts of strong bases with weak acids only
have been considered. The investigation was undertaken at
the suggestion of Dr. Svante Arrhenius, in Stockholm, and
the main object in view was the determination of the amount
of free alkali in aqueous solutions of such salts as potassium
cyanide, sodium carbonate, &c.; that is, of salts whose solutions -
exhibit an alkaline reaction, or act as mild alkalies.
I should like to avail myself of this opportunity to express
to Dr. Arrhenius my warmest thanks for the help which he se
willingly gave me and for the interest which he all along took
in the work.
A research, “ Zur Affinitiitsbestimmung organischer Basen”
(Zeits. f. physikal. Chemie, vol. iv. p. 19,1889), on somewhat
- similar lines, has already been carried. out by Dr. James
Walker. In it the relative strengths of different organic
bases were measured ; but one of the experimental methods
which he adopted could have served equally well for the
determination of the amount of free acid in aqueous solutions
of salts of the bases.
As a general rule, it will be found that the determination of
the amount of free alkali in solutions of the above salts is
beyond the scope of ordinary analysis. A reaction which
enables us to do so, however, is known. The velocity with
which the salt-solutions saponify methyl or ethyl acetate gives
wn Aqueous Salt-Solutzons. 367
us a measure of the quantity of free alkali which they contain.
The essential condition for saponification to take place is the
presence of hydrogen or hydroxyl ions. Now Walker’s
method was based on the presence of hydrogen ions, whilst
in the experiments about to be described we are dealing with
hydroxylions. This places us, as it were, on vantage ground ;
for, since hydroxyl ions saponify much more rapidly than
hydrogen ions, it is thus possible to work with more dilute
solutions where perturbing influences are reduced to a
minimum.
To return once more to the typical example of the salts
under investigation, potassium cyanide, let us for a moment
consider what takes place when we dissolve this body in water.
+
Besides the undissociated KON we get a great number of K
and CN ions, the water itself, too, is slightly dissociated into
> - +
H and OH ions. Now the H ions coming into contact with
the CN ions unite with them to form HCN which is uncharged,
being practically undissociated, whilst the hydroxyl ions re-
main free and counterbalance the potassium ions.
The water goes on continually supplying hydrogen and
hydroxyl ions, which are disposed of in this way, until equili-
brium takes place. If we now make up a small inventory of
the principal constituents of the solution we get :—
+ a
1 and 2, K and ON ions.
3, KCN undissociated.
4, HOH undissociated (say).
5, po undissociated (say ), and, corresponding to this,
6 and 7, K and OH ions.
6 and.7 taken together represent the quantity of free potash
present in the solution. The task which now lies before us is
comparatively easy, but before proceeding to deduce formule
for the calculations it is as well to point out what will be
proved later on, namely, that potassium cyanide itself is not
an active agent of saponification. Attention may also be
directed to the fact that the dissociation of the hydrogen
cyanide is so excessively slight in presence of the salt, that it
cannot exercise any appreciable influence on the velocity of
saponification: the truth of this will be the more readily ad-
mitted if we bear in mind that hydrogen ions are much less
active than hydroxyl ions. What has already been said
regarding the influence of the salt on the dissociation of the
hydrogen cyanide applies equally well to the water.
When ethyl acetate is saponified by a solution of potassium
2C2
368 Dr. J. Shields on Hydrolysis
hydrate, the velocity of the reaction is represented at every
instant by the general equation
& =hO—n) (C2), « «+ = ee Q)
where k is the coefficient of velocity of reaction, C and C, the
concentrations of the ester and base respectively at the com-
mencement, and 2 the quantity of ester which has undergone
change during the time ¢. .
In the case of the salt-solutions we wish to determine the
concentration of the base, z.e., the amount of active free
alkali at the commencement, the coefficient of velocity for the
various bases being already known. On dissolving potassium
cyanide in water we get
KOH + HENg=— KCN Sale
(quantity KOH x diss. ratio) x (quantity HCN x diss. ratio)
= (quantity KCN x diss. ratio) x (quantity HOH x diss. ratio).
The dissociation ratios of potassium cyanide and potassium
hydrate, water and hydrogen cyanide, do not alter appreciably
with change of concentration in the solution, and may conse-
quently be regarded as constant. (Arrhenius, Zeits. f. physikal.
Chemie, vol. v. p. 17, 1890.)
The quantity of water as compared with the other substances
is supposed to be infinitely great and regarded as a constant
K. The saponification of ethyl acetate by means of aqueous
potash takes place according to the equation :—
CH;COOC,H; + KOH=CH;COOK + C,H;08 ;
and if we represent by C, the initial concentration of the
potassium cyanide, by A the concentration of the free
potassium hydrate, and by 2 that of the potassium acetate
formed, then C,—#2—A will represent the actual concentration
of the potassium cyanide, and A+w that of the hydrocyanic
acid; all of course being expressed in the same unit, namely,
gram-molecules per litre. From the equilibrium,
KOH +HCN =~ KON+ HOH
we now get, using our new symbols, the equation
A(A +a)=K(C,—2—A), ee
which represents what takes place at any stage of the reaction.
After the first few moments, however, when A becomes very
small compared with 2, we may write the equation thus :—
aa Kina), ‘
in Aqueous Salt-Solutions. 369
Now, in the general equation (1) C,;—w the concentration of
the base is what we now call A, so that we may re-write it in
the form
Cp a a
Be a e e e e ° . (4)
Combining (8) and (4) we get
de be K (Ci) (5)
dt °C—a k unis
which on integration gives the solution :
Cy . C,—2, C C—2
oe p= 0, log nat. pean C0 log nat. ae
of k(t,—to) - (6)
k, the specific coefficient of velocity, is known, and for potash
at 24°-2 C.is numerically equal to 6°22. Having got K froin
equation (6) all that remains to be done in order to know how
much free potash is present in the solution at the commence-
ment is the calculation of A from equation (2). At the
beginning, when «=0,
IR (Cpa Baan ie 8 elgg CG)
from which we get A in gram-molecules per litre.
The percentage amount of potassium cyanide which has
been decomposed by the water is therefore
100A
OF :
It is here unnecessary to describe in detail the apparatus
and method which I used to determine the velocity of the
saponification of ethyl acetate by the salt-solutions, as it was
precisely similar to that which has already been employed by
Ostwald (Journ. f. pr. Ch. [2] vol. xxxy. p. 112, 1887),
Arrhenius (Zerts. f. physikal. Chemie, vol. i. p. 110, 1887), and
others. Measured volumes of a known strength of salt-solu-
tion and of ethyl acetate were mixed at the temperature of the
thermostat. (For the construction of the thermostat, c.
see Zeits. f. physikal. Chemie, vol. ii. p. 564, 1888.) From
time to time small fractions of the mixture were withdrawn
by means of a pipette and titrated as expeditiously as possible.
In calculating the concentration of the salt at the com-
mencement, it has been assumed that the volume of the mixed
solutions of salt and ester is the sum of the volumes taken
separately. This is of course, strictly speaking, not true, but
the deviation from the truth is so small as to be entirely
negligible. I shall now proceed to give the experimental
370 Dr. J. Shields on Hydrolysis
results which I obtained. The first column in the tables
contains the time ¢ expressed in minutes since the beginning
of the reaction. The second and fourth columns C,—2 and
C—z contain the concentrations of the salt and ester re-
spectively in hundredths of a gram-molecule per litre. The
third column contains x the quantity of ester which has under-
gone change, also expressed in the same unit. In the last
column will be found the constant expressed in arbitrary units.
Here it may be noticed that the first few values have been
neglected in accordance with the derivation of the formula.
From the mean value of these the characteristic constant K
has been calculated. A represents the amount of free alkali
in gram-molecules per litre, and besides this will be found the
percentage amount of salt which has been hydrolysed in the
solution experimented on and at the temperature at which the
experiment was carried out. It is conceivable that the
addition of ethyl acetate to the solution of salt would disturb
the existing equilibrium, but a discussion of this question is
reserved for a later part of the memoir.
Potassium Cyanide.
Solutions of this salt of four different concentrations were
examined, namely, +, 4, 4, and ~, normal. The tempera-
ture at which the experiments were made was 24°20. The
value of k, the coefficient of velocity for potash at this temper-_
ature, is 6°22. Nitrophenol was found to be the most suitable
indicator, and enabled me when titrating with decinormal
= Potassium Cyanide.
t. O,—2. z. O—x.
0 94°74 0-00 39°34
4 93°40 1°34 38°00
16 92:28 2°46 36°88 (313) x 1077
| 39 91-40 3°34 36°00 324
90 88°72 6:02 33°32 385
210 86°40 8°34 31:00 337
353 84:20 10-54 28°80 342
580 81:20 13°54 25°80 378
-Mean=353 x 1077
K=0:000928.
A=0:00296, or 0°31 per cent. of salt hydrolysed.
hydrochloric acid to observe the end point pretty accurately. _
wn Aqueous Salt-Solutions. St
IN : d
—- Potassium ( vyanide.
4
: i
be | CLs | a. hy eK Cre
| etd ae eSeS INCE clue Aa
| |
0 | 2348 0:00 39:34
Go|. 222s | O96 i. esses 7).
re) 2198s) || 50, saree 1) (117) x 10s!
ef IO) | 1:9 S786 4 TBS
Sheet . 2012. | SOO at |, weonos: 4 219
2) Sd ok s ee 20 |. Bl 216
oem | 144 GO4> 7 ee3s30E" 4) 226
Bee | 1598 | 7:50 Sted, F206
1394 - |. 13°00 10-48 D886 1 | 225
2789 | 9:82 13°65 2568 |° 245
Mean=221 x 10-7)
K=0-00121.
A =0-:00168, or 0°72 per cent. of salt hydrolysed.
N ee:
— Potassium Uyanide.
10
t C,—2. ff C—x
0 9°52 0:00 48°70
2 9°23 0:29 48°41 |
6 8:87 0°65 48:05 (251-5) x 10-6
12°5 8:67 0-85 47°85 123°8
33 815 kes fae 47-33 12671
6Ooioin. 767 1:85 46:85 | 131-2
130 6°78 2°74 45°96 =|: 1451
209 6°25 3°27 45°43 Messy
319 5°56 3°96 44-74 J41°8
1372 | 2°93 6°59 42°11 | 1376
|
i
i
Mean=133'8 x 10-8
K=0:001204.
A =0°00107, or 1:12 per cent. of salt hydrolysed.
Sra
372 Dr. J. Shields on Hydrolysis
N Potassium Cyanide.
AQ)
t. C,—z. Pe | C—z. |
SS |
0 2:38 0:00 48°70
2 2:20 0-18 48°52
45 2-10 0:28 48-42 (449) x 10-6
8:5 2:00 0:38 48-32 782
22 1-83 0°55 48°15 602
44 1-59 0-79 47-91 683
112 117 1-21 47-49 759
191 100° “| “ps8 47°32 634
303 0-72 1-66 47-04 765
1351 0:16 2-22 46°48 742
| Mean=702'4 x 10-§
K =0:001336.
A =0:000557, or 2°34 per cent. of salt hydrolysed.
é
40 Potassium Cyanide (concentrations in 5}5 gram-
molecule per litre).
| t C,—2 | a C—x, |
|
| 0 4-73 0:00 97-40 |
| 2 4-42 031 97-09 |
5 411 0-62 96°78 | (1050) x 10-6
10 3°86 0:87 96:53 (893) |
23 3°57 1:16 96-24 728 |
36 3:26 1-47 95°93 728 |
60 |) 99204 1-79 95°61 686 |
122 2:30 2-43 94-97 720 |
180 2:02 271 94-69 653 |
Mean =703 x 10-5
K = 0-001328.
A =0°000553, or 2°35 per cent. of salt hydrolysed.
Sodium Carbonate.
Experiments were made with 1, +4, 94, and 2, mole-
cular normal solutions of sodium carbonate.
The titrations were made with the aid of phenol phthalein at
the ordinary temperature of the laboratory. In this way the
amount of standard acid added corresponded only to one half of
the real concentration of the salt in hundredths of a gram-mole-
cule per litre, as the solution becomes practically neutral when
the unaltered sodium carbonate has been converted into sodium
hydrogen carbonate. This would necessitate the doubling of
in Aqueous Salt-Solutions. 373
the apparent concentrations ; but since the exact point of
neutrality was difficult to observe, two series of experiments
were made to eliminate as much as possible the experimental
error and the sum of the apparent concentrations taken to
represent C,—2. Consequently, in the tables for sodium car-
bonate there are two extra columns (I. and II.) with the
sum of the numbers contained in them given under the
column C.—.. The temperature at which all the experiments
on sodium carbonate was made was 24°2C., and the co-
etlicient of velocity & for sodium hydrate at this temperature
is taken at 6°23.
_ (mol.) Sodium Carbonate.
t. fe IT. U,— 2. Le C—x.
0 19-00 19-00 38°00 0-00 48-70
2 18-15 18°10 36°25 1-75 46°95
4 17-40 17:27 34°67 33 45°37 | (150) x 10-6
8 16°55 16°65 33°20 4°80 43°90 | 129
2 15°95 15°99 31°94 6:06 42°64 | 138
20 15°15 15°15 30°30 7:70 41:00 | 135
30 14-72 14-74 29 46 854 40-16 | 112
50 13°23 13°26 26°49 11-51 37:19 | 136
85 11:80 11-95 23°75 14:25 34:45 | 136
155 10°10 9:97 20°07 17°93 30°77 | 141
Mean = 132°4 x 10-6
“ (mol.) Sodium Carbonate.
t. ih Ma Osea. | Aaa Coe.
0 9-40 9°40 18-80 0-00 48°70
2 9-07 9:05 18°12 0°68 48:02
4 8°85 8°10 16°95 1-85 46-85 | (625) x10-°
8 7°85 7:60 15°45 3°35 45°35 815
12 7:30 7:25 14°55 4°25 44°45 839
16 6°95 6:90 13°85 4°95 43°75 854
20 6°60 6:62 13°22 5°53 43°12 880
24 6°40 6°35 12°75 6°05 42°65 874
32 5°82 6-08 11:90 6:90 41°80 885
66 5:12 5:10 10°22 8°85 40°12 741
Mean =841 x 10-6
K=0:01954,
=0°00596, or 317 per cent. of salt hydrolysed,
374 Dr. J. Shields on Hydrolysis
ah (mol.) Sodium Carbonate.
Ree ere y ae 2...) Oa
z. : |
are Seals 7 one TA Tce Sia
0 | 477 | 477 | 954 | 0:00 | 48-70 :
2 | 430 | 433 | 863 | 091 | 47-79 |
4 3:84 | 3°90 T74 | 1:80 46:90 278 x 10-*
8 344 | 350 | 694 | 260 | 46:10 | > a7 |
12 0/2301. [83-18 |) 6492] 93-35 | 45-a5 ee |
|
|
16 290 | 2-96 5°86 3°68 | 45:02 255
32 247 | 2:25 4°72 4:82 | 43°88 243
40 209 | 207 4-12 542 | 43-28 266
62 152 | 160 a12 | G42 | 49:98 283
92 1-22 1:24 246° | 7-08 ..| 41-62 269
Mean= 265 x 10-5,
K=0-02383.
A =0°00465, or 4°87 per cent. of salt hydrolysed.
N
0 (mol.) Sodium Carbonate.
l l ; | | |
t, I Il | G,-2.| 2 | Cm~s
Sass eens | ==...
0 2°38 238 | 476 | 000 |) 458
2 | 195 | 225 | 420 | 056 | 4814
4h. STS 180 | 35d 1-21 47-49 634 x 10-5
8 1:35 153 | = 288 1-88 46°82 676
12 1°22 1:23 | 2-45 2°31 46°39 698
16 1:16 ay 2:27 2°49 | 46°21 613
20 1°02 1-07 2°09 267 | 4603 579
28 0-75 0°85 160° | SiG Maes 665
56 0°49 0°41 0-90 3°86 | 44-84 656 .
Mean=646 x 10-5
K=0-02586.
A =0:00838, or 7°10 per cent. of salt hydrolysed.
Potassium Phenate.
Carbolic acid or phenol is another well-known weak acid
which forms a crystalline salt with potash. As an experi-
ment with this salt seemed likely to be interesting, solutions
of it were prepared by mixing equivalent quantities of solu-
tions of potash and phenol of known strength and then diluting
until solutions of the salt of the required concentration were
obtained. Two sets of experiments were made; one with
in Aqueous Salt-Solutions. 375
zo and the other with =, normal solutions. The indicator
used for titration was nitrophenol.
The temperature of the thermostat was 24°1C., and the
coefficient of velocity for potash at this temperature was
taken as 6°19. Each set of experiments was done in duplicate,
the separate results being given in the columns I. and II.
The mean of these is contained in the column C,—wz. In the
case of the =, normal solution the concentrations are ex-
pressed in 5}, instead of ;}5 gram-molecule per litre, as
before.
N Potassium Phenate.
10
t 1 EE C,—2. a. C—xz.
0 9-62 9°62 9-62 0:00 48°70
2 8-80 8:80 8°80 0:82 47°88
4 8°30 8:20 8:25 1:37 47°33 | (1383) x10-5
6 8-03 8:00 8:01 161 47:09 107
8 781 CCT HEU 1°83 46°87 101
10 766 7-60 7°63 1:99 46°71 95
12 TAD 7:43 7:44 2°18 46°52 96
16 7:09 (US a es) 2°53 46:17 99
22 6°75 6°71 6:73 2°89 45°81 97
30 6°20 6:10 6°15 347 45:23 109
Mean=101x10-5
K=0:00925.
A =0:002936, or 3°05 per cent. of salt hydrolysed.
ny Potassium Phenate.
50
t aL II. C,—4 Ai C—z.
0 3°90 3°90 3°90 0:00 97°40
2 3°15 3:10 312 0-78 96°62
4 2°78 2°80 2°79 ei 96:29 | 567x10-5
i) 2°60 2°67 264 | 1:26 96°14 611
6 2°49 2°54 2°52 1-38 96°02 627
8 2:27 2:27 2°27 1:63 95°77 (704)
12 2°10 2°04 2:07 1°83 95°57 596
16 1:88 1-86 1:87 2°03 95°37 578
20 1-66 1-64 1:65 2°25 95°15 613
eR A hiasteee 1:46 1:46 2°44 94-96 616
OD Ue sends 1-29 1:29 2°61 94°79 629
Mean=605 x 10-5
K=0-00939.
A =0°001305, or 6°69 per cent. of salt hydrolysed.
376 Dr. J. Shields on Hydrolysis
Borax.
Several experiments were made with solutions of borax,
but the results were by no means as satisfactory as could be
desired. The chief difficulty seemed to be in the want of a
suitable indicator. After trying about twenty I finally selected
litmus as the one which gave the best results. Next to litmus
came rosolic acid. I first of all prepared a solution of litmus
of a certain purple tint to act as a guide or standard, and
then I added acid to the solution under examination until it
became of the snes tint. I shall only give one series of
experiments with a =4, molecular normal solution of borax, so
that some conception may be formed as to the amount of
hydrolysis in solutions of borax.
The temperature of experiment was 24°-2C., and the co-
efficient of velocity for sodium hydrate corresponding to this
temperature is 6°23,
N
39 (mol.) Borax.
|
t C,-2 L Ca
0 5°85 0.00 48°70
4 5°82 0:03 48°67
8 572 0-13 48-57 (30) x 10-6
30 5°55 0:30 48°40 (22)
188 4:10 1°75 46°95 120
1190 2°73 3°12 45°58 86
2885 1-40 4-45 45°25 95
4375 0-95 4°85 43°85 94 |
Mean = 99x 10-6
K =0:00050.
A =0:000738, or 0°92 per cent. of salt hydrolysed.
The Influence of Dilution on the Amount of Hydrolysis.
The table which follows contains the general results of the
foregoing experiments and shows the effect of dilution on the
amount of hydrolysis.
The first column gives the approximate concentration of
the solution, the second the amount of free alkali in the solu-
tion in gram-molecules per litre, and the last the percentage
amount of salt hydrolysed.
see
in Aqueous Salt-Solutions. 377
- Concentration. A. Hydrolysis.
N
z KON Be i onhee nee 0:00296 0:31 per cent.
2 mere 5 ak lp 0-00168 072 ,,
N
Pe laos Se 0-00107 ae
N : ‘
=. ae 0000557 Danes
B Gaol. )Na,00 0-00804 2-12
im (mo .)Na, Zot eees 0 wiz 9
N 00596
i0 5 Sh ae CR Ate 0:00596 317 a
N 00465
0 et eacties <<’ moe 0:00465 4°87 vs
0:00338 7-10
Fee c
N
BMOMIOR eeeesecee 0-00294 S0b)
N
Bp OMe 0:00131 669
a Gael N 0007 0:92
39 (mol.)Na,B,O, ... 0:00074 56
A glance at the table will show that among the four sub-
stances examined the greatest amount of hydrolysis occurs in
the case of sodium carbonate. The numbers cannot pretend
to a very high degree of accuracy, chiefly on account of the
difficulties in obtaining suitable indicators for the titration of
the solutions, but the following regularity is easily discernible.
The amount of free alkali contained in the salt-solutions is
proportional to the square root of the concentration of the salt.
This is, however, not strictly true, but more nearly expresses
the truth the greater the dilution of the solution. A rough
calculation on the numbers for the two most concentrated
solutions of potassium cyanide shows that there is a deviation
from the law of about 13 per cent., whilst for the less concen-
trated solutions the deviation is reduced to about 4 per cent.
If the dilutions be plotted as ordinates against the percentage
amount of salt hydrolysed as abscisse, curves are obtained.
Fig. 1 represents the curves for potassium cyanide and sodium
carbonate. ‘These curves enable us to see at a glance the per-
centage of salt hydrolysed at any given dilution. For example,
Dilution.
378 Dr. J. Shields on Hydrolysis
Fig. 1.
Percentage of Salt hydrolysed.
reading from the curve, there should be 1°65 per cent. of
the potassium cyanide decomposed in a 34, normal solution
of that salt. If calculated from the above law, the amount of
hydrolysis is 1°58 per cent.
Now if the salt itself were the cause of the saponification of
the ester, the velocity of the reaction which is proportional to
the amount of free base present would have been very nearly
directly proportional to the concentration of the salt; but it
has been found approximately proportional to the square root
of the concentration, consequently the view that the salt itself
produces the saponification is untenable.
The law which has just been enunciated is what we should
expect from the theory ; for if we again take the case of
potassium cyanide, we get, neglecting the dissociation ratios
as formerly, :
KOH+HCN ==> KCN+HOH,
0. Gee) Ne
where C, is the initial concentration of the potassium cyanide,
and the fraction of it which has been hydrolysed. When «
is very small compared with C,, the above equation becomes
C= V7 Cos
wn Aqueous Salt-Solutions. 379
that is to say, the amount of free potash is proportional to the
square root of the concentration of the potassium-cyanide
solution.
Tt has long been known that water decomposed certain salts,
with formation of free acid and free base, but the amount of
such decomposition has up to the present time only been
measured in a few cases. It is true some guesses at it have
occasionally been made, but they have proved rather unsatis-
factory. For example, it has been supposed (see Ostwald’s
Lehrbuch der allgem. Chemie, vol. ii. p. 187, 2nd edit.), from
measurements of the heat of neutralization of hydrocyanic
acid by caustic soda, that a solution of sodium cyanide con-
tains only one fifth of the salt as such, whilst the other four
fifths are decomposed into free acid and free base.
The experiments which I have made on the velocity of
reaction show that in a tenth-normal solution of potassium
cyanide only about one per cent. of the salt is decomposed in
the way indicated. The results which J. Thomsen (Thermo-
chemische Untersuchungen, vol. i. p. 161) obtained on neutra-
lizing one molecule of sodium hydrate with n molecules of
hydrogen cyanide are as follows :—
n. NaOH Aq, nHCN Aq.
i 13°68 heat units.
iL 27°66 i
2 27°92 =
These numbers indicate that the amount of heat which is
‘developed increases in the same proportion as the quantity of
hydrogen cyanide added, until there are equivalent quantities
of acid and base present. An excess of acid, then, produces
only a very slight alteration in the value of the heat of
neutralization.
Now manifestly this small increase in the heat of neutrali-
zation means that the first equivalent of hydrogen cyanide
has almost all combined with the sodium hydrate. The cause
of the incomplete combination is due of course to the mass
action of the water. Inshort, it would seem that only a small
fraction, presumably about one per cent., of the potassium
cyanide is decomposed by the water into free acid and free
base.
This corroborates the result which I have obtained by a
totally different method.
A guess which H. Rose (Jahresbericht, 1852, p. 311)
hazarded as to the amount of hydrolysis in an aqueous solu-
tion of borax is just as unsatisfactory. Rose supposed that
380 Dr. J. Shields on Hydrolysis
this substance in pretty dilute solution was almost entirely
decomposed into acid and base; but the preceding experi-
ments go to prove that in a =; molecular normal solution
rather less than one per cent. is decomposed by the water.
If the statement that the amount of free alkali in the solution
is proportional to the square root of the concentration holds
good for borax, then a solution in which the borax was com-
pletely hydrolysed would be almost infinitely dilute.
Rose has described a very interesting experiment which is
intended to show the decomposition of borax by water. A
tincture of litmus reddened with acetic acid is added to a
concentrated solution of borax until the red colour has almost
but not quite disappeared ; the whole is then diluted with
water, when the red colour changes to blue. I have repeated
this experiment, and find that a solution prepared in the way
Rose has indicated becomes distinctly blue on dilution. Joulin
(Bull. Soc. Chim. de Paris [2] vol. xix. p. 844, 1873), how-
ever, could not observe this change of colour, and moreover
has attempted to show that water exercises no decomposing
influence at all on salts; but there is little doubt that he has
been too hasty in coming to this conclusion, and that Rose,
at least qualitatively speaking, was right.
Trisodium Phosphate.
A preliminary experiment with a X solution of this salt
showed that the velocity of reaction, on saponifying ethyl
acetate, was singularly great when compared with what had
been observed in the case of the other salt-solutions, and in
fact closely approached that for a =, normal solution of
caustic soda itself. This seemed to indicate that the solution
under examination was almost entirely hydrolysed in the
sense of the equation 3
Na;PO,+ HOH =Na,HPO,+ NaOH.
The formulze which have hitherto been employed are of no
use in this case, for they depend on the condition that A
should be very small compared with 2 Here A can in no
case be neglected ; consequently the equation (3)
he K(C, — a)
is inapplicable. eae Ss
The general equation
dx
becomes d:
7G =KG—2)(C-0), 2... 8)
in Aqueous Salt-Solutions. | 381.
when we substitute for the concentration of the base that of
the sodium phosphate.
Instead of K we may write ky, where we is a factor which
expresses the ratio of the amount of free alkali present to’
what would be present if the hydrolysis of one sodium atom
was complete.
Hquation (8), on integration, gives the solution
. Cy—2
S20. log nat. (a G—0, °s nat. en =hu(t;—t),
Gag — log Gap = 04843 ku (—4)(C—C), + @)
from which we can calculate m at the time ¢,.
In order to determine pu at the commencement, the different
values of mw are plotted against the times, and the curve so
obtained prolonged. The point at which it cuts the axis for
the time t=0 gives the value of w at the commencement.
Hixperiments have been made which show that Na,H PQ, is
only slightly hydrolysed ; so if we neglect this and assume
that the equation
Na,PO,+ HOH=Na,HPO,+ NaOH
represents the posszble quantity of caustic soda which can be
formed in the solution, then 100 represents the percentage
amount of the caustic soda which actually eavsts in be solution.
The following experiments were made with a =, molecular
normal solution of trisodium phosphate at 24°-2 C., at which
temperature the coefficient of velocity of reaction for caustic
soda is 6°28. The concentrations are expressed in 3}5 of a
gram-molecule per litre, and the employment of phenol
_ phthalein enabled the titrations to be made pretty accurately.
i
a (mol.) in Phosphate.
t. I. II. C,—2. oR C—x. pe
0 3°81 J81 3°81 0:00 4°87
2 2°93 2°95 2°94 0:87 4:00 0:945
4 2°41 2°45 2°43 1:38 349 0882
6 2:06 2°03 2°04 1-77 3°10 0873
8 182 | 177 | 179 | 202 | 2:85 | 0-831
10 158 | 155 | 156 | 295 | 362 | 0-897
12 135 | 140 | 137 | 944 | 243 | 0-897
16 112 | 114 | 113 | O68 | 219 | o-788
20 091 | 094 | 093 | 288 | 1:99 | o-v780
4 079 | o8 | o7v9 | 302 | 185 | o-v64
| 30 063 | O66 | o64 | 317 | 170 | 0-738
Phil. Mag. 8. 5. Vol. 85. No. 215. April 1893. 2D~
Coefficient wu.
382 Dr. J. Shields on Hydrolysis
If the equation
Na;PO,+ HOH =Na,HPO,+ NaOH
represented accurately the amount of hydrolysis, then mw at
the commencement should be 1:00. A glance at the last
column of the table shows that the equation must be nearly
true. In order to find approximately the initial value of p,
a curve (fig. 2) has been drawn by plotting the values of w as
ordinates against the times ¢ as abscisse. .
Time, in minutes.
By referring to the curve it will be found that the initial
value of w is 0°98 at least ; that is to say, at least 98 per cent.
of one of the sodium atoms in Na;PO, exists as free caustic
soda in a = molecular normal solution of the salt at 24°-2 C.
In other words, although trisodium phosphate exists in the
sclid state, yet in dilute solution it is for the most part
decomposed into hydrogen disodium phosphate and sodium
hydrate. This result is in entire agreement with Berthelot’s
recent researches.
in Aqueous Salt-Solutions. 383
Allusion has already been made to the fact that hydrogen
disodium phosphate is only slightly hydrolysed when dissolved
in water. ‘This salt behaves rather differently from the others.
During the saponification the solution, which is at first
alkaline, becomes neutral and then acid.
For the sake of comparison with trisodium phosphate, the
following set of experiments was made witha 50 (mol.) solu-
tion of hydrogen disodium phosphate at 24°°2 C. The solution
was prepared from a sample of the salt obtained from Kahl-
baum, and had a slightly alkaline reaction.
The titre of the solution during saponification was as
follows :—
N setae
30 (mol.) Hydrogen Disodium Phosphate. |
ee ee
Time. Titre.
min. 7
0 0:06 ado g--mol. per litre (alkaline),
2 0-04 A; Er haes
5 0:00 Neutral.
32 0-06 zdo0 g.-mol. per litre (acid).
120 0-10 2
226 0-15 ” r
380 0°17 . ?
1380 0-30 a ‘
2815 0:41 ‘s x
4500 0-52 j 33
The titrations were made with phenol phthalein.
At the commencement the solution contained 0:0003 gram-
molecule of free soda per litre.
The case is a very complicated one, but possibly the bulk of
this alkalinity is due to the formation in the solution of tri-
sodium phosphate ; there is still, however, a minute amount
of free alkali in the solution, owing to the hydrolysis of
hydrogen disodium phosphate. The following attempt has
been made to measure it, but no stress must be laid on the
results. I give the calculations here merely for the sake of
comparison with trisodium phosphate, and to show that at the
best there is not much free alkali in the solution. The calcu-
lations were made with the help of equations (6) and (7). It
is evident, of course, that what we measure here is the quan-
tity «2. The initial concentrations of the salt and ester,
expressed in hundredths of a gram-molecule per litre, are
4°76 and 48°76.
2D2
384 Dr. J. Shields on Hydrolysis
If we start at the point where the mixture is neutral we
may construct the following table, from which we can calcu-
late the quantity of free alkali in the solution at the point of
apparent neutrality. This quantity, as has already been sug-
gested, is perhaps due to the hydrolysis of hydrogen disodium
phosphate ; whilst the quantity of free alkali determined by
direct titration is due to the presence of trisodium phosphate,
formed according to the equation
2Na,HPO,=Na;PO, + NaH,PQ,.
The influence of the dihydrogen sodium phosphate has been
neglected altogether. :
te C.—«. ap. C—x.
0 4:76 0:00 48°70
27 4-70 0:06 48-64
115 4-66 0:10 48°60 64x 10-8
221 4-61 0-15 48°55 (86)
375 4:59 0-17 48°53 65
1375 4°46 0:30 48°40 59
2810 4°35 0:41 48°29 55
4495 4:24 0:52 48:18 54
Mean = 59x107°
K=0-00000236.
A=0-:000038, or 0°07 per cent. of salt hydrolysed.
The amount of free alkali determined by direct titration is
0°63 per cent., whilst that determined from the velocity of
saponification, starting at the neutral point, is 0°07 per cent. ;
it is therefore evident that the total amount of free alkali in
the solution is very small when compared with what is present
in a solution of trisodium phosphate.
Sodium Acetate.
After having estimated the amount of hydrolysis in salts
of strong bases with some of the weakest acids, it was
thought desirable to extend the experiments a little and
determine the amount of hydrolysis in a salt of a stronger
acid, for example acetic acid. For this purpose a tenth
normal solution of sodium acetate was prepared and investi-
gated in the same manner as the salts of the weaker acids.
The calculation of the results, however, was in this case much
simplified, owing to the fact that the concentrations of the salt
and ester did not alter much during the reaction, consequently
in Aqueous Salt-Solutions. 385
the mean values have been employed in calculating the
rharacteristic constant.
If, in the equation (5),
de 1 1_ K(CG—z)
dig@en bes og be
we substitute for C.—a and C—w their mean values 9°316
and 48°49, which were obtained from a series of experiments
made at 24° 2 ©., where k=6'23, we get:
deel BI IGK
d 4849 623° 4%”
which on integration gives the solution
ay" — x67
6:23 x 48°49 x 9-316 K=
ty— to |
Having got the characteristic constant K, equation (7)
enables us to determine A, the amount of free soda in the
solution at the beginning, expressed in gram-molecules per
litre. The solution was titrated with the help of phenol
phthalein.
In this case of course a, which is expressed in hundredths
of a gram-molecule per litre, was measured directly. The
values of x in the following table are the means of two con-
cordant sets of experiments.
N et
i0 Sodium Acetate.
t. C,—<2. x. C—x2.
0 9-52 0-000 48°70
1224. 9-46 0-060 48-64
3952 9:455 0-065 48-635
6882 9 385 0-135 48:565 2:58 x 10-6
21252 9:20 0-320 48-380 4-98
25550 9:20 0-320 48-380 4-06
34160 9-165 0°355 48-345 3°72
41290 9:14 0380 48°320 3:51
Mean = 9°316. Mean=48'49. Mean=—3°76x10-°.
K=0:0000000668.
A=0:00000798, or 0°008 per cent. of salt hydrolysed.
According to these measurements and calculations, it will
be seen that in a tenth normal solution rather less than +4)
per cent, of sodium acetate is hydrolysed into free acid and
386 Dr. J. Shields on Hydrolysis
free base ; thus, |
- CH,COONa+ HOH === CH,COOH+NaOH.
Tt has already been stated that the presence of free weak
acids has no measurable influence on the velocity with which
the saponification takes place.
This is equally true in the case of sodium acetate, where
acetic acid is one of the products of hydrolysis, and is also
formed on the saponification of ethyl acetate. Arrhenius
(Zeits. f. phystkal. Chemie, vol. v. p. 2, 1890) has thoroughly
investigated the change of the dissociation ratio of acetic acid
on the addition of sodium acetate, and has shown that it may
be regarded as nil in presence of large quantities of its salts.
By referring to the table it will be seen that the experi-
ments on sodium acetate lasted for a considerable time, and it
is conceivable that the water itself may have played an im-
portant part in the saponification of the ester. In order to
test this a blank experiment was made with water and ethyl
acetate under the same conditions as the experiment with the —
sodium acetate, and after the lapse of nearly three weeks the
solution of the ester was only slightly acid. If, then, pure
water, in virtue of its being electrolytically dissociated to a
small extent, produces such an inappreciable effect, we can
easily conjecture how infinitely slight this effect will be in
presence of a strongly dissociated salt like sodium acetate.
The Influence of the Ester on the existing Equilibrium.
A]l the preceding deductions regarding the amount of
hydrolysis in aqueous solutions of salts of strong bases with
‘weak acids are based on the assumption that the equilibrium
in aqueous solutions,
KCN+HOH <> HCN+KOH,
is not disturbed by the presence of small quantities of ethyl
acetate. ‘To justify this assumption, I have made some expe-
riments in which the concentration of the ester was varied,
whilst the concentration of the salt remained nearly the same.
Now, if the presence of the ester produced any change in the
state of equilibrium, we should expect an alteration in the
concentration of the ester to be accompanied by a corre-
sponding variation in the amount of salt hydrolysed.
The following tables contain the results of experiments, on
an approximately 0-1 normal solution of potassium cyanide,
made at 25°-0 C., at which temperature 4=6°54.
in Aqueous Salt-Solutions. 387
I. Concentration of Ester = 0°4870 g.-mol. per litre.
s C,—2x. oD. C—x. |
2
0 10:08 0:00 48°70
2 9-70 0°38 48°32
6 9-46 0°62 48:08 (100) x 10-8
10 9-20 0:88 47°82 143
20 8:81 1:27 47°43 153
40 8:38 1:70 47:00 142
84 7°70 2°38 46°32 141
152 700 3°08 45°62 140
264 6:20 3°88 44°82 137
1484 2°90 718 41°52 139
Mean = 142x10-°
K=0:001305.
A=0-00114, or 1:13 per cent. KCN hydrolysed.
II. Concentration of Ester = 0°2005 g.-mol. per litre.
é C.—2. 2X. C—-x.
eee 1038 000 |. 20:05
2 10:20 0-18 19:87
6 9-99 0:39 19:66 (27) x 10-6
12 9°77 0-61 19:44 (36)
On 9-41 0-97 19:08 39
63 8:90 1-48 18°57 40
131 8:26 2-12 17-93 42
243 7-67 2-71 17°34 39
1463 4-85 553 1452 41
1683 4-56 582 14:23 49
Mean = 40x10-§
K=0:00151.
A =0:00124, or 1:20 per cent. KON hydrolysed.
III. Concentration of Ester =0°1013 g.-mol. per litre.
|
t. Ob hho x. C—x.
0 10-4902 Ae O00 1013
2 10°40 0-09 10-04
10 10:16 0:33 9:80 (103) x 10-8
37 9-66 0:83 9:30 130
104 9°19 1:30 8:83 143 |
215 8:57 1:92 8-21 160 |
1435 6-40 4-09 6-04 164 |
1655 6-26 4-93 5-90 150
Mean = 149x10-8
K — 0:00 148.
A=0:00124, or 1:18 per cent. KCN hydrolysed.
388 On Hydrolysis in Aqueous Salt-Solutions.
The next small table contains the collected results of these
experiments.
Cone. Ester. K. A. KCN hydrolysed.
0:4870 | 000131 0-00114 | 1:13 per cent.
0:2005 0:00151 000124 4 ae2inae
| ie
|
01013 000148 | 0°00124
The numbers show that the concentration of the ester has
no measurable influence on the amount of hydrolysis, since
the figures in the last column do not arrange themselves in a
series which is either gradually ascending or descending.
The differences between them are probably chiefly due to
experimental error. The mean value is 1°17, and the greatest
deviation from it is less than 5 per cent.
Résumé.—The general results of this investigation may
briefly be stated as follows :—
1st. It is shown how the velocity with which salt-solutions
saponify ethyl acetate may be utilized to determine the extent
to which hydrolysis has taken place in aqueous solutions of
salts of strong bases with weak acids.
2nd. The amount of hydrolysis has been measured in solu-
tions of the following salts; and in 4, molecular normal
solutions between 24°-25° C. the amount of salt which is
decomposed by the water is :—
Potassium cyanide 1:12 per cent.
Sodium carbonate . oa
Potassiam phenate ... . . s-Oa eae
Borax (about) ; 0-5 ss
Sodium acetate 0-008
7?
Ath. Trisodium phosphate can scarcely be said to exist in
a 345 molecular normal solution, as it is almost completely
hydrolysed in the sense of the equation ;
Na;PO,+ HOH=Na,HPO,+ NaOH.
5th. The presence of small quantities of ethyl acetate in the
solution does not materially disturb the equilibrium,
KCN + HOH 22— KOH + GR
University College, London,
[ 389 J
XXXVII. Suggestion as to a possible Source of the Energy
required for the Life of Bacilli, and as to the Cause of thew
small Size. By G. Jounstone Stoney, M.A., D.Sce.,
F.R.S., Vice-President, Royal Dublin Society *.
ie that part of the material universe which man’s position in
time and space, and the limitations of his senses, permit
him to investigate, the Dissipation of Energy is so prevalent
that instances of the reverse process can seldom be clearly
traced out, though many such can be dimly seen. Under
these circumstances, even possible instances, such as that dealt
with in this paper, are instructive if they are of a kind to be
fully understood. They are also important, for if the universe
is permanent, there must be, or have been, or be about to
be, parts of the universe where the Concentration of Hnergy
is as largely predominant as its dissipation is within our
experience.
Some bacilli, e. g. some of the nitrifying bacilli of the soil,
are said to be sustained by purely mineral food, while they
furnish ejecta which contain as much potential energy as the
food, or more. If this be the case, they must be supplied
with a considerable amount of energy to enable them to evolve
protoplasm and the other organic compounds of which they
consist, from these materials. Now many bacilli are so
situated that this energy is certainly not obtained from sun-
shine, and it is suggested that it may be derived from the
gases or liquids about them.
The average speed with which the molecules of air dart
about is known to be nearly 500 metres per second—the
velocity of a rifle-bullet ; and the velocity of some of the
molecules must be many times this, probably five, six, or
seven times as swift. We do not know so much about the
velocities of the molecules in liquids as of those in gases, but
the phenomenon of evaporation and some others indicate that
they are at least occasionally comparable with those of a gas.
Accordingly, whether the microbe derive a part of its oxygen
or other nourishment from the gases, or from the liquids about
it, it is conceivable that ONLY THE SWIFTER MOVING MOLECULES
can penetrate the microbe sufficiently far, or from some other
cause are either alone or predominantly fitted to be assimi-
lated by it.
Now if this be what is actually taking place, the adjoining
air or liquid must become cooler through the withdrawal from
* From the Scientific Proceedings of the Royal Dublin Society,
vol. yili, part i. Communicated by the Author,
390 Dr. G. J. Stoney on the Source of the
it of its swiftest molecules ; and, in compensation, an amount
of energy exactly equivalent to this loss of heat is imparted
to the microbes and available for the formation within them of
organic compounds.
It is further evident that if this be the source of energy
upon which bacilli and cocci have to draw, the minuteness of
their narrowest dimension will be of advantage—probably
essential—to them. Presumably it would only be limited by
such other necessary conditions as may forbid the diminution
of size being carried beyond a certain point. The diameter
of a bacillus is frequently as small as half or a third of a
micron, which brings it tolerably well into the neighbourhood
of some molecular magnitudes.
The transference of energy here suggested may be what
occurs notwithstanding that it does not comply with the
Second Law of Thermodynamics, which states that heat will
not pass from a cooler to a warmer body, unless some ade-
quate compensating-event occurs, or has occurred, in con-
nexion with the transference. This law represents what
happens when vast numbers of molecular events (which are
the real events of nature) admit of being treated statistically,
and furnish an average result. It, therefore, has its limits :
and the communication of energy from air to minute organ-
isms which is described above, is an example of a process
which is exempt from its operation ; since this transference
is supposed to be brought about by a discriminating treatment
of the molecules that impinge upon the bacillus of precisely
the same kind as that which Maxwell pictured as made by his
well-known demons. It therefore belongs to the recognized
exception to the Second Law of Thermodynamics, viz., that
which occurs in the few cases in which we can have under
observation the special consequences of selected molecular
events, instead of, as on all ordinary occasions, being only
able to measure an average outcome from all the molecular
events in the portion of matter we are examining.
If some bacilli—those which live on mineral food—obtain
their whole stock of energy in the way here indicated, it may
be presumed that all bacilli get at least a part of what they
require in the same way.
Should the reader have any doubt as to whether the pro-
cess here described is one of those that contradict the Second
Law of Thermodynamics, he may satisfy himself on this head
by the following considerations :— LTE
Imagine a perfect heat-engine within an adiabatic envelope
with some bacilli and an abundance of their mineral food, all
Energy requred for the Life of Bacilli. 391
‘being at one temperature. If events take place as supposed
above, the bacilli receive sufficient energy from the sur-
rounding medium to enable them to assimilate their mineral
food, and thereby to grow and multiply. Meanwhile the
medium becomes cooler. We may then suppose that the new
bacilli which have come into existence, and all the excreta,
are used as fuel in the heat-engine, and that its refrigerator is
as near as we please to being at the temperature to which the
medium has been reduced. The combustion of the fuel may
take the form of resolving the bacilli and excreta back into
the mineral substances from which they had been evolved,
except that these are now at the temperature of the combus-
tion. Let us next reduce this temperature in the heat-engine
to the temperature of the refrigerator. During this process
a portion of the heat may be converted into mechanical energy ;
and at the end of the process everything within the enclosure
is in the same state as at the beginning, with the sole excep-
tions that some of the bodies within the enclosure are now at
a lower temperature than at the beginning, and that the heat
which they have lost has been converted into mechanical
energy.
It thus appears that the contents of the adiabatic envelope
may be regarded asa heat-engine, all the parts of which start
at a certain temperature, and which yields mechanical energy,
while the only other change is that some of its parts are cooled
to a lower temperature. This contradicts the Second Law of
Thermodynamics as formulated by Lord Kelvin, if we leave
the word “inanimate” out of his enunciation. His state-
_ ment of the axiom is :—‘‘ It is impossible by means of inani-
mate material agency, to derive mechanical effect from any
portion of matter by cooling it below the temperature of the
coldest of surrounding objects.” It is legitimate here to
omit the word “inanimate,” as its insertion merely means
that cases of exception to the law may be met with in the
organic world ; and if this be stated it will need to be added
that cases of exception may also be found among inorganic
processes: the correct statement being that the law does not
apply to individual molecular events, and that therefore it
need not be obeyed in the cases, whether organic or inorganic,
in which any observable effect is the outcome of one-sided
molecular events.
- It should be borne in mind that the heat of a given portion
of matter is the energy * of motions of and within its molecules;
* The energy here spoken of may be partly potential: in fact while
motion is going on, the “energy of the motion,” or a part of it, usually
fluctuates between being kinetic and potential.
392 Intelligence and Miscellaneous Articles.
not necessarily of all such motions, but of those among them
which are capable of restoring energy to the parts of the
molecule carrying electra (see Stoney on “ Double Lines in
Spectra,” Scientific Transactions of the Royal Dublin Society,
vol. iv. part xi.) whenever the motion of the electron has
transferred energy from the molecule to the ether. As ful-
filling this criterion we are probably to include all irrotational
motions within the molecules, and we must also include rela-
tive motions of the molecules—all of them indeed if time
enough be allowed for turmoil within a fluid to subside. It
does not include any motion which the molecules have in
common, as in wind, or in the rotation of a wheel.
When these circumstances are taken into account, it is
obvious that the energy of the heat-motions of an individual
molecule undergoes rapid fluctuations, while there may be a
definite average of the energy of these motions, whether esti-
mated by what happens in an individual molecule over a
sufficiently long period of time, or when estimated by what
occurs simultaneously in all the molecules of a body. In
other words, the motions of an individual molecule do not
from instant to instant conform to the Second Law of Thermo-
dynamics, although the law may apply both to the average of
the motions of a single molecule taken over a long period of
time, and to the average of the simultaneous motions of vast
multitudes of associated molecules. As regards molecular
motions (the motions within a solid, or motions within a fluid
that do not produce currents in the fluid), the millionth of
one second is a long period.
XXXVIII. Intelligence and Miscellaneous Articles.
ON THE MAGNETIZATION OF IRON RINGS SLIT IN A RADIAL
DIRECTION. BY H. LEHMANN.
ee chief results of the present research may be summed up in
the following principles, which hold for an imperfectly closed
ferromagnetic ring, the radius of which is large in comparison
with the radius of the section :—
1. The demagnetizing factor, or the factor which, multiplied
by the mean magnetization, gives the mean factor of the demag-
netizing force, is constant up to about half the saturation.
2. The coefficient of dispersion (Strewungs-coefficient), the ratio
of the mean induction to that in the slit, is constant up to half
saturation.
3. The region of the dispersion of the lines of force is limited
essentially to the vicinity of the slit, and is narrower as the
magnetization increases.
4, The coefficient of dispersion is independent of the radius of
the ring; in regard to its constancy (2), it only depends on the
Intelligence and Miscellaneous Articles. 398
relative width of the ring d/r. The empirical expression for this
dependence is a linear one of the form
ete
7
where h is a constant which, for the Swedish iron investigated, has
the value 7, and will presumably have values differing but little
from this in the case of other ferromagnetic metals. This will
probably be the case more especially in the kinds of iron used in
technical processes.
5. When the empirical constant 2 is known, the factor of
demagnetization can be calculated from the geometrical dimensions
of the system by the formula
Ne 2d
d aN?
Pan = Earl
in which p is the radius of the ring, r that of the section, and d
the width of the slit. This formula holds with the same limitation
as (1), (2), and (4), that is, up to demisaturation. In general the
equation holds,
2d
medi 1
ayy
(p—z)
in which y is the factor of dispersion.
6. For high magnetizing values the factor of demagnetization
approaches the limiting value
Nope 5 are me a)
ee:
The previous results may find an approximate application even in
imperfect magnetic circuits of complicated shapes.—Wiedemann’s
Annalen, No. 3, 1893.
N=
THE SPECIFIC HEAT OF LIQUID AMMONIA.
BY C. LUDEKING AND J. E. STARR.
The specific heat of liquid ammonia, though it has often been the
subject of calculation in development of theory and practice, has
not yet been satisfactorily determined experimentally, if we except
the work of Regnault. His results, however, were unfortunately
lost during the Paris Commune. He assumed the specific heat to
be 0°799. Since then the interest in this constant has very
considerably increased through the rapid development of the
artificial ice industry. Generally the specific heat has been taken
at unity. Thus De Volson Wood in his ‘Thermodynamics,’
page 337, recommends this value “ until the experimental value is
determined.” |
It was our good fortune to have ready access to all the means
necessary for executing the somewhat laborious experiments
involved, and we take this opportunity to present briefly the
a94 Intelligence and Miscellaneous Articles.
results of our work. The liquid ammonia used in the experiments
was found on examination to contain 0°3 per cent. of moisture
and on spontaneous evaporation to leave only a trace of residue.
The impurities were therefore of no consequence in influencing the
result to the limit of accuracy intended.
Of this liquid ammonia 10°01 grams were introduced into a
small steel cylinder of 16:122 c.c. capacity, stoppered by a steel
screw. The mode of filling was quite simple. After cooling the
cylinder in a bath of the liquid ammonia itself and while still
immersed, it was possible to pour it brimful by means of a beaker.
The steel screw stopper, also previously cooled, was then inserted
and drawn almost tight. On then removing the cylinder from the
cooling bath, the liquid contents gradually expanded and escaped
in quantity proportional thereto, and besides a very small vapour
space was allowed to form as is indicated in the experimental data.
Then the stopper was driven tight. Thus the error in the result
due to the latent heat of condensation of vapour of ammonia in the
course of the experiments was reduced to a minimum and
rendered, as will be seen, almost inappreciable in its influence.
The cylinder was perfectly free from leakage and remained
constant in weight during each series of determinations. It was
suspended in the drum of a Regnault apparatus heated by the
vapour of carbon disulphide. The entire mode of procedure was
in all details that commonly used in the Regnault method. After
the cylinder had been heated for about six hours, it was dropped
into a brass calorimeter whose water value was 1°36 cal. and which
contained 150 grams of water. In each experiment it required
very nearly two minutes to raise the calorimeter to its maximum
temperature. The influence of loss by radiation was reduced
to a minimum by the Rumford manipulation. The thermometers
used were standardized, carefully compared, and read to hundredths
of a degree by means of a magnifying lens. The experiments were
conducted sufficiently far from the critical temperature, which
according to Vincent and Chappuis is 131° C.
The following are the data of Experiment 1 :—
Weight of steel cylinder and ammonia. .. 81-008 grams.
Weight of steel cylinder ............%. 70°998
9
Weicht of ammonia ..j.e0es52<. . AEG 10-01 25
The specific gravity of liquid ammonia being 0°656, the volume of
10°01 grams is 15:26 c.c.
Total water value of calorimeter, thermometer,
Bit WVAIeE ne. cs SEE A. ss 151°76 cal.
‘Water value of steel cylinder ............ 8°34 cal.
eMmEperavure OF di... eos. s 5 ts ee 25°4 C.
Temperature of steel cylinder ............ 46°51 C.
Temperature of calorimeter after immersion 26°69 C.
Temperature of calorimeter before immersion 24°44 C,
ftsse in temperaburers 1. Aa crew. ss. ys bot 2°25 C.
Intelligence and Miscellaneous Articles. 395
Thus 341:46 cal. were given off by the cylinder in cooling 19°82
or 17:23 cal. for one degree. Of this 8°34 cal. are due to the
steel cylinder itself, leaving 8°89 cal. for 10°01 grams of liquid
ammonia or 0°888 per gram=specific heat. In a second and third
experiment the values 0°897 and 0896 were obtained. The
determination of the specific heat of liquid ammonia would be
influenced, as stated, by the latent heat of condensation of part of
the small quantity of vapour present, when the cylinder cools in
the calorimeter. This would to a degree be neutralized by the
contraction of the liquid ammonia itself in the cooling and the
consequent formation of more vapour space.
It seemed desirable to ascertain the influence of these factors
collectively by experiment. or this purpose specific heat deter-
minations were made in a way somewhat different from the
ordinary. The steel cylinder was cooled in an iron shell in melting
ice, instead of being heated, and then introduced into the warm
calorimeter water. The mode of precedure was in detail similar to
that described above, and we will therefore only give our results.
In three experiments the values 0°878, 0°863, and 0-892 were
obtained. They are a trifle lower in their average than the results
obtained by the ordinary method. It.is reasonable to assume that
they are somewhat low, while as stated the other results are
presumably somewhat high ; and in order to arrive at the specific
heat of this substance nearest the true value from our experimental
evidence, we will take the average of our six values, viz. :
0-888 0-878
0-897 } 1st series, 0-863 $ 2nd series,
0-896 0:892
and state it as being=0°8857.
_ We beg herewith to acknowledge our obligations to Chancellor
W.S. Chaplin and Prof. Wm. B. Potter for kindly placing the
laboratories under their charges at our disposal.—Stlliman’s Journal,
March 1893.
ON THE OFFICIAL TESTING OF THERMOMETERS.
BY H. F. WIEBE.
In the year 1885 the Imperial Standards Commission undertook
on a large scale the official testing of thermometers which is of
such great importance both in science and in practice ; while pre-
viously only a few institutions, such as the Naval Office, had
occupied themselves to a limited extent with the investigation of
thermometers. These official testings were transferred to the
recently established Physical Technical Imperial Institute, to which
since then a great number of thermometers have every year been sent
for investigation. (In Ilmenau there is a branch for these testings.)
Through the great progress which has been made since Jena glass
has been used for thermometers, it has been possible to undertake
a permanent guarantee for the results obtained in such testing ;
and from the uniformity of this glass the thermometric constants,
once determined, may be universally adopted. The testing takes
396 Intelligence and Miscellaneous Articles.
place in two ways—either by comparison with a standard thermo-
meter at different temperatures, or by calibration and determina-
tion of the thermometric constants. The comparison of the thermo-
meters is made between 0° and 50° in water-baths; above 50°
in boiling-point apparatus with reversing condensers, in which
liquids of various boiling-points are used for the determinations.
The following liquids were found to be especially suitable :—
Boiling-point. Boiling-point.
Clvoroform “i262: .-- 60°6° Toluole \.. ..«s ptibuan i \ etbartny) dss
but - bf
BS sin eC
S2—] ptibuan — et? > ben :
e . bap
sin
Multiplying the disturbance by itself with —z in place of +1,
we have for the light intensity,
>= bapx?
sin ees
2
sin cs
The first term indicates spectral lines in positions given by
the equation :
a
7 = 3
with intensities given by the last integral. The intensity of
the spectral lines then depends on the form of the groove as
[ \ eBOz+uy) ds || ( etibrtuy ds].
sin
in Theory and Practice. . A401
given by the equation «=/(y) and upon the angles of inci-
dence and diffraction. The first factor has been often discussed,
and it is only necessary to call attention to a few of its pro-
perties.
When baw=27N, N being any whole number, the expres-
sion becomes n”?, On either side of this value the intensity
decreases until nbay'=2aN, when it becomes 0.
The spectral line then has a width represented by p/—w! = 2F
nearly ; on either side of this line smaller maxima exist too
faintly to be observed. When two spectral lines are nearer
together than half their width they blend and form one line.
The defining power of the spectroscope can be expressed in
terms of the quotient of the wave-length by the difference of
wave-length of two lines that can just be seen as divided,
The defining power is then
nN*=na 3
Now na is the width of the grating. Hence, using a
grating at a given angle, the defining power is independent
of the number of lines to the inch and only depends on the
width of the grating and the wave-length. According to this,
the only object of ruling many lines to the inch in a grating
is to separate the spectra so that, with a yiven angle, the
order of spectrum shall be less.
Practically the gratings with few lines to the inch are
much better than those with many, and hence have better
definition at a given angle than the latter except that the
spectra are more mixed up and more difficult to see.
It is also to be observed that the defining power increases
with shorter wave-lengths, so that it is three times as great in
the ultra-violet as in the red of the spectrum. This is of
course the same with all optical instruments such as telescopes
and microscopes. ,
The second term which determines the strength of the
spectral lines will, however, give us much that is new.
First let us study the effect of the shape of the groove on
the brightness. If N is the order of the spectrum and a the
grating-space, we have
e=Il(singd+sin py) = =~,
ba,
since sin —<" ==())
2
* An expression of Lord Rayleigh’s.
402 Prof. Henry A. Rowland on Gratings
and the intensity of the light becomes proportional to
[ iy il (F242) ds}[ (fe —ion(J2t Sy) ds}.
It is to be noted that this expression is not only a function
of N but also of lJ, the wave-length. This shows that the
intensity in general may vary throughout the spectrum ac-
cording to the wave-length, and that the sum of the light in
any one spectrum is not always white light.
This is a peculiarity often noticed in gratings. Thus one
spectrum may be almost wanting in the green, while another
may contain an excess of this colour; again, there may be
very little blue in one spectrum, while very often the similar
spectrum on the other side may have its own share and that
of the other one also. For this reason I have found it almost
impossible to predict what the ultra-red spectrum may be, for
it is often weak even where the visible spectrum is strong.
The integral may have almost any form, although it will
naturally tend to be such as to make the lower orders the
brightest when the diamond rules a single and simple groove.
When it rules several lines or a compound groove, the higher
orders may exceed the lower in brightness, and it is mathe-
matically possible to have the grooves of such a shape that,
for given angles, all the light may be thrown into one spectrum.
It is not uncommon, indeed very easy, to rule gratings with
immensely bright first spectra, and I have one grating where
it seems as if half the light were in the first spectrum on one
side. In this case there is no reflexion of any account from
the grating held perpendicularly: indeed, to see one’s face the
plate must be held at an angle, in which case the various
features of the face are seen reflected almost as brightly as in
a mirror but drawn out into spectra. In this case all the
other spectra and the central image itself are very weak.
In general it would be easy to prove from the equation
that want of symmetry in the grooves produces want of
symmetry in the spectra—a fact universally observed in all
gratings, and one which I generally utilize so that the light
may be concentrated in a few spectra only.
Example 1.—SQuaRE GROoVEs.
When the light falls nearly perpendicularly on the plate,
we need not take the sides into account but only sum up the
surface of the plate and the bottom of the groove. Let the
depth be X and the width equal to a
m
in Theory and Practice. 403
The intensity then becomes proportional to
ES sin? 7 sin? wy X,
This vanishes when
. N=m, 2m, 3m, &e. ;
l
The intensity of the central light, for which N=0, will be
Tes ho
7s (x7 x
This can be made to vanish for only one angle for a given
wave-length. Therefore, the central image will be coloured
and the colour will change with the angle, an effect often
observed in actual gratings. The colour ought to change,
also, on placing the grating in a liquid of different index of
refraction, since \ contains I, the index of refraction.
It will be instructive to take a special case, such as light
falling perpendicularly on the plate. For this case,
o=0, X=1(1 + cos), and p=lsinp=
Hence
=0, 1, 2, 3, &e.
rat{lea/i -(5 hb
The last term in the intensity will then be
‘ Small 1 N\2
2 as
sin 4X17 + ee,
As an example, let the green of the second order vanish.
In this case, /="00005. N=2. let a=-0002 centim.,.and
b=:
Then —_X[20000 + /(20000)?— (10000)"] =n.
Whence
pre i 8
37300"
where n is any whole number. Make it 1.
Then the intensity, as far as this term is concerned, will be
as follows :—
404 Prof. Henry A. Rowland on Gratings
Minima where Intensity is0.|| Maxima where Intensity is 1.
Wave-lengths. -Wave-lengths.
Ist spec....| *0000526 0000268 | 0001000 | 00003544 | -00002137
2nd ,, ...| °0000500 ‘0000266 0000833 | 00003463 | -00002119
ord ,, ...| *0000462 0000263 =| 0000651 | 00003333 | -00002089
4th ,, ...| °0000416 ‘0000259 | 0000499 | 00003169 | -00002050
thy oaere &e. &e. | &e. &e, &e.
The central light will contain the following wave-lengths as
a maximum :—
"0001072, :00003575, °0000214, &e.
Of course it would be impossible to find a diamond to rule
a rectangular groove as above, and the calculations can onl
be looked upon as a specimen of innumerable light distribu-
tions according to the shape of groove.
Every change in position of the diamond gives a different
light distribution, and hundreds of changes may be made
every day and yet the same distribution will never return,
although one may try for years.
Example 2.—TRIANGULAR GROOVE.
Let the space a be cut into a triangular groove, the
equations of the sides being e=—cy and w=c'(y—a), the
two cuttings coming together at the point y=u. Hence we
have —cu=c(u—a), and ds=dy-V/1+c?, or dyV¥1+c?.
Hence the intensity is proportional to
EN. 1 (Ee. ow 1
V(1+c¢?)(1+e¢?) . mu(u—cr) . m(a—u)(w+er)
aes UN) | sl a
cos [(H+eA)(a—u)—n(u—er)] t
pf 1+¢ ea Dg bam 2p—m+1
ey we sin ou : 7
2m 2
Now the first two terms have finite values only around the
points — =mNz, where mN is a whole number. But
2p—m-+1 is also a whole number, and hence the last term
is zero at these points. Hence the term vanishes and leaves
the intensity, omitting the groove factor,
sin? n a sin? n—/
x + (bv) 2
sin fee ‘ sin? bape
2m F 9
|
in Theory and Practice. 409
The first term gives the principal spectra as due to a grating-
space of < and number of lines nm as if the grating were
perfect. The last term gives entirely new spectra due to the
erating-space a, and with lines of breadth due to a grating of
n lines and intensities equal to (duv)?.
Hence, when the tangent-screw is used on my machine for
14,436 lines to the inch, there will still be present weak
spectra due to the 14,436 spacing, although I should rule,
say, 400 lines to the millim. This I have practically observed
also.
The same law holds as before that the relative intensity in
these subsidiary spectra varies as the square of the order of
the spectrum and the square of the deviation of the line or
lines from their true position. |
So sensitive is a dividing-engine to periodic disturbances,
that all the belts driving the machine must never revolve in
periods containing an aliquot number of lines of the grating ;
otherwise they are sure to make spectra due to their period.
As a particular case of this section we have also to consider
Periopic HRRors oF RuLING.—THEORY oF “ GHOSTS.”
In all dividing-engines the errors are apt to be periodic,
due to “drunken” screws, eccentric heads, imperfect bearings,
or other causes. We can then write
Y=Na+ a, sin (en) +a sin (en), + ke.
The quantities ¢,, ¢, &c. give the periods, and a, ay, Ke.
the amplitudes of the errors. We can then divide the integral
into two parts as before, an integral over the groove and
spaces and a summation with respect to the numbers.
UU
y" y"-y
s| e—BAt+Ky) ds = Set | e—tbAntny) ds,
y' 0
It is possible to perform these operations exactly ; but it is
less complicated to make an approximation, and take y!—y'=a,
a constant as it is very nearly in all gratings. Indeed the
error introduced is vanishingly small. The integral which
depends on the shape of the groove will then go outside the
summation sign, and we have to perform the summation
Se—ibu | aon+ a, sin er + asin eyn+ &e.
410 Prof. Henry A. Rowland on Gratings
Let J, be a Bessel’s function. Then
cos (usin 6) =Jo(u) +2[Jo(u) cose p+dy(u) cosyh+ &e.],
sin (usin 6) = 2fJy(w) sind +33(u) sing d+ Xe. |.
Bye e— usin? — cos (usin d) —2 sin (usin d).
Hence the summation becomes
( g-ibpagn
x [J o(buay) + 2(—23 ,(bua,) sin en + Jo(buay) cos 2e;n— Ke.)
Ss x [Jo(buae) + 2(—t3 (buy) sin egn + J 2( buy) cos 2en — Xe.)
x [Jo(buas) + &e.) |
Lx [ &e. ].
Case I.—Si1ncGLE PERIoDIC HRROR.
In this case only ap and a; exist. We have the formula
pine sin”
Seteimag a? 4
ae
sins
Hence the expression for the intensity becomes
2 2
\ sin n wal | sin n ts ot +]
Jo(bua,) ———— 7+ J," (bya
| Pens (+9 OH a |
2 2 2 4
ee 2
| sin pete ta |
4 ee, + &e.
om e1
| sin | J
As n is large, this represents various very narrow spectral
lines whose light does not overlap, and thus the different
terms are independent of each other. Indeed, in obtaining
this expression the products of quantities have been neglected
for this reason because one or the other is zero at all points.
These lines are all alike in relative distribution of light, and
their intensities and positions are given by the following
table :—
in Theory and Practice. 411
Places. Intensities. Designations.
= = ah J0°(bmay). Primary lines.
. 0 .
fe pe ca Jy?(bpey a1). Ghosts of 1st order.
2e
fg=bt a Jo°(bpya2). Ghosts of 2nd order.
p= Pe < J3°(bpras)- Ghosts of 3rd order.
&e. &c. ac.
Hence the light which would have gone into the primary
line now goes to making the ghosts, so that the total light in
the line and its ghosts is the same as in the original without
ghosts.
The relative intensities of the ghosts as compared with the
primary line is
. Jn’ (bya)
Jo” (bua)
This for very weak ghosts of the first, second, third, &c.
order becomes
2 4 6
Ay 2 Ag 6 Ag
The intensity of the ghosts of the first order varies as the
square of the order of the spectrum and as the square of the
relative displacement as compared with the grating-space ap.
This is the same law as we before found for other errors of
ruling; and it is easy to prove that it is general. Hence
The effect of small errors of ruling is to produce diffused
light around the spectral lines. This diffused light is subtracted
from the light of the primary line, and its comparative amount
varies as the square of the relative error of ruling and the
square of the order of the spectrum.
Thus the effect of the periodic error is to diminish the
intensity of the ordinary spectral lines (primary lines) from
the intensity I to Jo*(bua,), and surround it with a sym-
metrical system of lines called ghosts, whose intensities are
given above.
When the ghosts are very near the primary line, as they
nearly always are in ordinary gratings ruled on a dividing-
412 Prof. Henry A. Rowland on Gratings
engine with a large number of teeth in the head of the screw,
we shall have
2 LZ 2 A \ _ oe
J bay (u+ i )+d pha, (1 = 2J,°bayu nearly.
Hence the total light is by a known theorem,
Jo? + 2[J,?+J,.?+ &e. |=1.
Thus, in all gratings, the intensity of the ghosts as well as
the diffused light increases rapidly with the order of the
spectrum. This is often marked in gratings showing too
much crystalline structure. For the ruling brings out the
structure and causes local difference of ruling which is
equivalent to error of ruling as far as diffused light is con-
cerned.
For these reasons it is best to get defining power by using
broad gratings and a low order of spectra, although the
increased perfection of the smaller gratings makes up for this
effect in some respects.
There is seldom advantage in making both the angle of
incidence and diffraction more than 45°, but if the angle of
incidence is 0, the other angle may be 60°, or even 70°, as in
concave gratings. Both theory and practice agree in these
statements.
Ghosts are particularly objectionable in photographic
plates, especially when they are exposed very long. In this
case ghosts may be brought out which would be scarcely
visible to the eye.
As a special case, take the following numerical results :-—
N= 1. 2. 3.
@ gl 1.4. 11 22
a; 25 50? 100 25’ 50° 100, 2555p aumm
(xt) 4 td
TG) 63’ 252? 1008 16 63° 252° = 7? 28? 102"
In a grating with 20,000 lines to the inch, using the third
spectrum, we may suppose that the ghosts corresponding to
“ — = will be visible and those for i
1
a 50 very trouble-
0 25
in Theory and Practice. 413
some. ‘The first error is a;= zo9hp95 in. and the second
=spo000 m. Hence a periodic displacement of one
Set of an inch will produce visible ghosts and one five-
hundredth-thousandth of an inch will produce ghosts which
are seen in the second spectrum and are troublesome in the
third. With very bright spectra these might even be seen
in the first spectrum. Indeed an over-exposed photographic
plate would readily bring them out.
When the error is very great, the primary line may be
very faint or disappear altogether, the ghosts to the number
of twenty or fifty or more being often more prominent than
the original line. Thus, when
bya, = 2°405, 5°52, 8°65, &e. =2nN-,
0
the primary line disappears. When
bjs, =0, 3°83, 7:02, é&e. =20N-,
0
the ghosts of the first order will disappear. Indeed, we can
make any ghosts disappear by the proper amount of error.
Of course, in general
ics toet » Ji, He)
n—2°
Thus a table of ghosts can be formed readily and we can
always tell when the calculation is complete by taking the
sum of the light and finding unity (see p. 414).
This table shows how the primary line weakens and the
ghosts strengthen as the periodic error increases, becoming 0
at InN = 2-405. It then strengthens and weakens periodi-
0
cally, the greatest strength being transferred to one of the
ghosts of higher and higher order as the error increases.
Thus one may obtain an estimate of the error from the
appearance of the ghost.
Some of these wonderful effects with 20 to 50 ghosts
stronger than the primary line I have actually observed in a
grating ruled on one of my machines before the bearing end
of the screw had been smoothed. The effect was very similar
to these calculated results.
Phil, Mag. 8. 5. Vol. 35. No. 216. May 18938. 2F
414
Prof. Henry A. Rowland on Gratings
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in Theory and Practice. 415
DovusLE Pertopic ERROR.
Supposing as before that there is no overlapping of the
lines, we have the following :—
Places. Intensities.
= = [Jo(dyae) Jo(bazp) |?. Primary order.
0
e ‘
7 taee a [91 (a 41) JoC are) ]?. | Ghosts of Ist
Bs : r order.
M2 = et ba [Jo (basme) Ji (daefe) ]?. |
ete,
M3 = b+ = [Js (bays) J, (Daopes) ]?. 7
aa 2e 5 | hosts ef 2nd
fs, = eat Ta [Jo (ba,p4) Jo (Daopt4) |. G oe 2
; |
s= wtp — [Fo(bams) Fa(daqes)
+2
be = WETS, [Ty (Barge) Ta(Daaue) ). >
2
Pe ai [J o(Daypez) Ja (Deof47) |?.
“ Y \ Ghosts of 3rd
ps = B45 —— [Io(aypts) Js (Baus) }* | ae
Uy
3 :
Hy = wp [3 (betof49) Jp (batopte) ]?.
Ac. ae.
Each term in this table of ghosts simply expresses the fact
that each periodic error produces the same ghosts in the
same place as if it were the only error, while others are added
which are the ghosts of ghosts. The intensities, however,
are modified in the presence of these others.
Writing c,=ba,p and c.=bapy.
The total light is
2357(c,) Jo° (ce)
2517(e1) Jo?(co) 2071 2/., r
Jo (¢,) Jo’ (cg) + | + 2c.) J (co) } i Fone a0) oe
o (C1) Jo (C2
which we can prove to be equal to 1.
2F 2
416 Prof. Henry A. Rowland on Gratings
Hence the sum of all the light is still unity, a general pro-
position which applies to any number of errors.
The positions of the lines when there is any number of
periodic errors can always be found by calculating first the
ghosts due to each error separately; then the ghosts due to
these primary ghosts for it as if it were the primary line, and
so on ad infinitum.
In case the ghosts fall on top of each other the expression
for the intensity fails. Thus when e.=2e,, 3, = 3, uc., the
formula will need modification. The positions are in this
case only those due to a single periodic error, but the inten-
sities are very different.
Places.
2QaN 5
= [Jo(bayw)T y(basu) |.
0
= pt ap [J if (bap) J 0 (bap) —J 3(bayfy) JS 2 (Dae p11) = Ke. | 2
& ~~ bag + [Js (Gap) Ss (42p41) re 3(bayp5) 3; (baopey) + &e. ]?.
‘Ke eG
We have hitherto considered cases in which the error could
not be corrected by any change of focus in the objective. It
is to be noted, however, that for any given angle and focus
every error of ruling can be neutralized by a proper error of
the surface, and that all the results we have hitherto obtained
for errors of ruling can be produced by errors of surface, and
many of them by errors in size of groove cut by the diamond.
Thus ghosts are produced not only by periodic errors of
ruling but by periodic waves in the surface, or even by a
periodic variation in the depth of ruling, In general eee
ever, a given solution will apply only to one angle and
consequently, the several results will not be identical : -
some cases, however, they are perfectly so.
Let us now take up some cases in which change of focus
can occur. ‘The term «7? in the original formula must now
be retained. |
Let the lines of the grating be parallel to each other. We
can then neglect the terms in z and can write r2= 2 ver
nearly. Hence the general expression becomes ered
10(AZ+ py—Ky2
Se ees:
where « depends on the focal length. is i
very (ead aad hence « is small. ; vis 16 oppose
The integral can be divided into two parts—an integral over
the groove and the intervening space, and a summation for
all the grooves. The first integral will slightly vary with
in Theory and Practice. AIT
change in the distance of the grooves apart, but this effect
is vanishingly small compared with the effect on the summa-
tion, and can thus be neglected. ‘The displacement is thus
proportional to
DS eib(uy—Ky?)
Case I.—Lines at VARIABLE DISTANCES.
In this case we can write in general
y=an+a,n? + apn’ + &e.
AS K, %, a, &¢., are small, we have for the displacement,
neglecting the products of small quantities,
Dd etlelant ayn2+ agn3+ &e.)—Ka2n2]
Hence the term an? can be neutralized by a change of
forms expressed by wa,=«xa®. Thus a grating having such
an error will have a different focus according to the angle n,
and the change will be + on one side and — on the other.
This error often appears in gratings and, in fact, few are
without it.
A similar error is produced by the plate being concave,
but it can be distinguished from the above error by its having
the focus at the same angle on the two sides the same instead
of different.
According to this error, a,n?, the spaces between the lines
from one side to the other of the grating, increase uniformly
in the same manner as the lines in the B group of the solar
spectrum are distributed. Fortunately it is the easiest error
to make in ruling, and produces the least damage.
The expression to be summed can be put in the form
See" + tb( wa, — Ka?)n? + ibpagn? + ib [wag + 2b (wa, — Ka?)?] n4
+ &e. |
The summation of the different terms can be obtained as
shown below, but, in general, the best result is usually sought
by changing the focus. This amounts to the same as varying
« until wa,—Kxa?=0 as before. For the summation we can
obtain the following formula from the one already given.
Thus
n—1 1
. sm np .
3h e2tpn P pip(n—1),
in p
Hence
= 1: Ame Chine ae ™sin np
m2ipn — ip(n—1)f rane eA ee
a ane (inn? (z+éln 1)) Tar
418 On Gratings in Theory and Practice.
When 2 is very large, writing = =pn=aNn+q, we
have
a—1 Mon
> nine2tpr — —¢ (2 4 +4) S: Js
g @ dq q
Whence, writing
¢ = b(uay—xe),
i bpoag,
c" = bl pas + tb (pa,—xa’)’],
cl" = &e.,
the summation is
( n’
nti( SHES ee ) |
:
(a pes 1 94. |)
+ (2c0 + aoe + 4c 13+ ia |
ous yn ye & | salleeanen
i(e; + 363 + 6¢ Te a cng
q
_ (et n° )\S |
( Sag ae
5 4
5, ore
+2\ 6 a. |
+ &. }
dsnq_ eos si
dq q q
@ sing _ —2q cos g + (2—¢?) sing
dey q°
anes _ (69) cos g— (6—3¢') sing
dy’ g q |
&e. &e.
These equations serve to calculate the distribution of light
intensity in a grating with any error of line distribution
suitable to this method of expansion and at any focal length.
For this purpose the above summation must be multiplied by
itself with +2 in place of —2.
The result is for the light intensity
On the Differential Equation of Electrical Flow. 419
4
e 3 See
E+ (ach + 205 + ce aa
q t /dq q
n
8
4 5 3 ot Q
—_ (es ieee ke.) a wag + &e. \
{
8 16 dg q
n nt d’ sing
anes a sin g a
(oN + be. ee + &. ¢ -
As might have been anticipated, the effect of the additional
terms is to broaden out the line and convert it into a rather
complicated group of lines, as can sometimes be observed
with a bad grating. At any given angle the same effect can
be produced by variation of the plate from a perfect plane.
Likewise the effect of errors in the ruling may be neutralized
for a given angle by errors of the ruled surface, as noted in
the earlier portions of the paper.
XL. On the Differential Equation of Electrical Flow.
By T. H. Buaxestey, J/..4.*
apes object of this paper is to point out that the theory
of electrical discharge, as exemplified in the mathe-
matical expressions employed to represent the physical facts,
is incompetent to explain all the phenomena observed in
extreme cases; and to show that the admission of certain
properties of matter not usually recognized is the only way of
satisfactorily obviating the imperfection of the existing views.
In some of the investigations I shall not employ exclu-
sively algebraical symbolic methods, but, where it may more
advantageously be adopted, I shall avail inyselt of the geome-
trical method. Such cases most frequently arise where magni-
tudes under consideration are capable of having negative
values. All tidal effects, using the word in its most general
sense, involve such magnitudes.
Hlectrical currents in a given conductor may have all
possible values in one direction or in the opposite direction,
but are otherwise restricted.
The projection of the line joining two points in space
upon a fixed straight line is a geometrical magnitude of this
sort. With respect to the direction in space, sometimes one
of the projected points will be on one side of the other
* Communicated by the Physical Society: read March 24, 1893.
420 Mr. T. H. Blakesley on the Differential
projected point, sometimes on the other. So that sucha line
has all the properties necessary for representing another
magnitude of the same character. .
In this way I shall most generally make the projection
represent Hlectromotive Force, but occasionally Field of
Magnetism at a point. As to matter of nomenclature,
the only scientific term which | shall employ admitting of
any doubtful interpretation, is the Effective Electromotive
Force. By this term I intend to convey the idea of that
eleciromotive force which is numerically equal to the product
of the current and the resistance, at a point of time. Asa
department of State has recently employed the term in a
totally different sense, this statement has appeared to me to
be necessary in the interests of proper explanation. The
effective electromotive force is the algebraical sum of all the
impressed and induced electromotive forces, and is here
represented by E. If V is the sum of all the impressed
electromotive forces and F is the sum of all induced electro-
motive forces, then the equation among their quantities is
V+F=E universally. ?
Geometrically, if AB, BC are lines whose projections on
some one fixed straight line represent the sum of the im-.
pressed and the sum of the induced electromotive forces
respectively, then the projection of AC will represent the
effective electromotive force.
The three lines must form the sides of a triangle, those
corresponding to the impressed and induced electromotive
forces being taken the same way round the triangle, that
corresponding to E being taken in the opposite direction.
Now if the actual changes in the magnitudes are harmonic,
and of the same period, it is clear that the lines A B, BC,
AC must remain of constant length and the triangle must
rotate in its own plane at a uniform rate of such a value as
to perform a complete revolution in the period of the har-
monic change. ‘The triangle thus shows admirably the way
in which these magnitudes succeed one another in phase. It
also foliows from the properties of harmonic motion that if
two magnitudes have the same harmonic period, but differ
in phases by a quarter of the whole period, the corresponding
lines to be projected are at right angles with each other. And
hence the rate of variation of an harmonic magnitude differs
in phase from the magnitude itself by a quarter of the
period. But in the simplest case of a circuit being plied
with an harmonic electromotive force V, it is generally
considered that the induced electromotive force varies as the
Equation of Electrical Flow. 4AQ1
rate of change of the current ; that is
gC > Lidl eG
i> ie > eae for H=RC,
where C is the current, R the resistance, and L is the
coefficient of self-induction.
The equation already given then becomes
yee Lo? =n RC.
Multiplying through by C ee integrating through a com-
plete period,
VeanL foo? ari cat
The first term represents the work done by the source of
the disturbance.
The second term vanishes.
The third term represents work done in heating the
circuit.
Hence the whole work done has gone to heat the circuit.
Now it is admitted on all hands that when the period is
sufficiently short a radiation of energy into space takes place.
A portion of this radiated energy is sometimes caught by
means of a neighbouring circuit and converted into heat.
A coefficient of mutual induction and a corresponding
extra term is then introduced into the equation. But are
we to suppose that radiation would not proceed into space
were there no neighbouring conductor? Itis against proba-
bility, against the electromagnetic theory of light.
If electromagnetic waves are capable of being sent into
space, we can no longer look upon the operation of establish-
ing a current in a circuit as analogous to bending a stiff
spring or displacing rigid wheelwork. The wheelwork must
have indiarubber spokes or teeth.
The above equation takes no account of this radiation whieh j is
expended outside the wire, nor of any other work done else-
where than in the conductor ; and this latter the equation
states to be exactly equal to the ener gy expended in propa-
gating the electromotive force. Hven supposing a portion of
the field is occupied by some material whose passage through
a cycle of magnetization involves the loss of energy, in the
form of heat, this, equally with wave-propagation through
space occupied by perfectly elastic matter, will not be
accounted for by the equation.
Now of such phenomena as radiation of energy in electro-
magnetic waves, or absorption of energy in the field, there is
422 Mr. T. H. Blakesley on the Differential
ample evidence. Therefore an equation will not meet such
eases in which the induced electromotive force is taken as
entirely in quadrature with the current, or when F is wholly
of the form pee .
dt
Hence, in the geometrical representation it is clear that
the induced electromotive-force line must
not be exactly at right angles with that of =
the effective electromotive-force line; 7. e.
the angle BC A is not exactly a right angle;
and it is easy to see that it must be greater
than a right angle, for B C may be resolved
into BD.DC, where BDC is a right =
angle and A C D is one straight line. For C
then the whole work done is equal to
gD yal
7A cell
the conductor is
The work done in heating
J ° A
ea and the differ-
ence, or the work done in the field, is see
Hence, if D lies on the side of C neurer to A, A D would
be less than A C, and the work done by the discharge would
be less than that required to heat the conductor: in other
words, energy would have to be received from space.
Hence the induced electromotive forces may be represented
by two components—one A D in quadrature with the current,
and one D C in opposition to it,
dC
-L& -a¢,
where % may or may not be a constant, but is in kind a
resistance.
The equation among the electromotive forces may be
written
dC
V—L--—’AC=RC.
Multiplying through by Cdt and integrating through a
complete period,
{v Cdt—L jc - dt= R| Cae + facta,
The second term on the left vanishes as before, the first
term representing the whole work dove. On the right the
Equation of Electrical Flow. 423
first term heats the conductor and the second term gives
energy to space.
We may go somewhat further into the causes of such an in-
duced electromotive-force component if we
employ the geometrical mode of symboli- B
zing the electric quantities. BC,the induced
electromotive-force line, should be at right
angles to the induction through the circuit,
for it is the rate of increase of the latter D
which produces the former. Hence if A H
is a perpendicular let fall upon BC pro- C
duced, A E will represent the phase of the
magnetic induction. But AC being in E
phase with the current is in phase with the
field. Hence HAC, or CBD which is
equal to it, is a magnetic phase-lag, and A E may be said to
be in phase with the effectve field, and therefore with the
induction. This suggests that if we employ the lower lines of
the figure to represent fields, we may make up a triangle
A CE such that A Cis the impressed field,
C E an induced field, and A E an effective Cc
field, of course when, as usual, projected on
a fixed line ; C EH being perhaps, though by
no means certainly, at right angles to AE. E
However, whether CHE here has in any a
case two components perpendicular and
parallel respectively to A EK or not, it appears very certain that
the perpendicular component must exist. Assuming at first
that it alone exists,—
If we employ small letters :—
» for impressed field = AC,
f for induced field =CH,
e for effective fied =AH,
1 = coefficient of magnetic self-induction, so that
A
and yw for the permeability, I for the rate of magnetic induction,
1. @. per square centim., we have
To obtain an equation of energy from this we must multiply
(not by I, as analogy would at first sight perhaps dictate) by
dl y :
oe dt x cross section, for the formula for energy is
424 Mr. T. H. Blakesley on the Differential
[?e-*m | = [we ~2t— me || welt ?m? lt
= | Field | ane
ia
i a1 \(F) a = (Fo dt.
Here the term on the right hand oe necessarily,
and the work expended, if any, is equal to ( tan? B ~ sec? B—1’
and cos? B= : already obtained ;
1
Am tst 40° KL
therefore ea
2 te aa 2
te te 1 (a
therefore
IaV KL
ea
the form usually quoted if we neglect the second term of the
denominator.
I purpose to show that in a discharge of the sort here con-
templated (which has been shown to be the result of the
ordinary premisses given at page 425) there will be no work
done by any electromotive force which lags at an angle 6
behind the current, provided the initial condition is one of
zero-current. And, further, that the source of H.M.F., which
is represented by the side of the isosceles triangle in advance
by the angle 8, of the effective H.M.F., does all the work of
heating the circuit and no more. It will thus be seen that
there is no provision in the theory for expenditure of power in
the field, and hence that the theory does not explain the well
recognized phenomenon of radiation into space.
To establish the above-mentioned propositions, take the —
product of the projections of two lines undergoing variations
corresponding to the two radii vectores of two equiangular
spirals of the same characteristic angle 8 and period, and
differing in phase by the angle 2y.
One of these quantities may be expressed by
Equation of Electrical Flow. 431
EY ou
ae tam8sin O+y.
The other by
Ore
be nb sin @—y.
The product is
26
ab.e ™Bsin O+y SID @—y,
or
20
ab.e tamB (sin? @— sin’y),
This quantity, multiplied into an element of time dt, has to
be integrated through one period. Since = = = the
integral 1 becomes
abt
a e eer (cos 2y— cos 20) dd,
or
mem tanB cos Yy dO — a pp oraces 26 dé.
The first term of the integral is
abt
8a
The second term is
ae ——cos 2y tan Be — =r
20
abt pale DB orcs
3, sin 8 cos B +20 ‘ ee
and therefore the ce ig expressed :—
Abts | =
a Br °
This expression has to be taken between limits. If we con-
template one revolution only the limits will be ®,+27 and @,,
and the Definite Integral becomes
Abts 20,
3 1—sin 8 cos B+ 3+ 20, +tan B cos Qyte™ tus( 1—e ~ ane ).
If the limits are infinity and @, the integral becomes
_. 26,
us af ae Bcos2y—sinBcosB+203¢ me . (a)
aie {sin 8 cos 8 +20—tan @ cos 2y}.
Hither of these expressions becomes zero when
tan 8 cos 2y=sin 8 cosB+ 20;
2G 2
432 Mr. T. H. Blakesley on the Differential
or
cos 2y=cos 8 cos B+ 26,
showing that the condition that no work shall be done in the
electric problem depends on the initial circumstances, 7.e. 0;
-is involved. If 2y= the condition of no work becomes
cos 8+ 26, =1,
which is satisfied when
Hence if the initial condition be that of no current, the line
bisecting the angle between the line of effective H.M.F. and that
of the self-induced E.M.F. makes —§ with the line @=0, and
it is thus proved that on the whole no work
is done in the field.
If, on the other hand, we make
é,=+ B :
1 2 7
and start from a point where the current
is zero, we have in the above expression,
when proper substitutions are made for a and 3, the value of
the work done on the circuit by the discharging condenser.
The integral between infinity and @, becomes, when 6,= C and
ab. ty . F =e
— {1— cos 26} sin 8.e tanB;
or
id Ais ee ORME
? sin®Be tank,
; iD ELIE Eh ecw §
In this case 6= Rand ae tan sin Bis the potential difference
between the plates of the condenser at starting =Vj, say,
=Vsin8. Hence the expression becomes
My ager. fd
R:a,52 iS Ve
(E and V being now the full sides of the triangle, properly
E
interpreted), and Z.y =e B by the geometry of the triangle,
and further,
Equation of Electrical Flow. 433
tan game mad thereiore = =
ty Aq
and the work
pei’ ? i ty or ty sin? B
sR 2cos 6 2tan 6 [ae Ge
which is the expression we should obtain if we integrate the
square of the current multiplied by Rdt, seen as follows :—
In the general expression («) obtained above for the pro-
by
2 tan B’
sin? 8,
duct of the projections make a=H, b= = and 0,=0, y=0
the expression («) becomes
sa {tan 8 —sin B cos 8}
Pegee! an sin 6 cos f5,
or
EK? ty ;
aR a B—sin 8 cos P},
or
[Dee
in t, sin” B, as above.
Thus the whole of the work goes to heat the wire, and,
further, substituting in the equation for E in terms of V, it
may be shown to be entirely derived from the charged con-
denser.
The work may be written, eliminating E,
2V? cos B ty
R Aar
Ne ty O18)
Kae cos B sin’ 8.
sin’,
or
Now V/?=V’sin? @, and thus the work is
t
VR cos? B,
. ry t
or, since cos*B= a
1
V17ts KR
= and é = ——
Pree On oe
VK
— 5) 9
which is the ordinary expression for the energy stored in the
condenser ; and this appears from the investigation to he
434 On the Differential Equation of Electrical Flow.
entirely expended in heating the circuit, and there is no
margin for the exhibition of power elsewhere.
Suppose a line A B to represent (E) the line of effective
E.M.F. At the extremity A set off AC
as the direction of the line representing c
the P.D. of the condenser.
Then, as the condenser contains all
the energy that is going to be expended
on the circuit and on the ether, from
what has been said it is clear that A C
must be rather longer than the side of
the isosceles triangle; for, if not, the
energy stored will not do more than «a £ we
heat the circuit. If therefore a perpen-
dicular be dropped upon A B from GC, it will fall at a point
nearer B than A.
Join C B, and, further, draw C D to meet AB produced in
D, and so that C DA is an isosceles triangle on A D as base,
and therefore CDA=8. Now CB must be the line repre-
senting the resultant of the induced electromotive forces F,
and however complicated the case may be this line CB is
equivalent to two components CD, DB: of which CD results
in no expenditure of power because it is in a phase B behind
the current, and DB is in phase directly opposed to the
current, and therefore resulting in whatever expenditure of
energy takes place outside the circuit, and therefore in the
ether or in magnetic bodies, or in neighbouring or surround-
ing conductors. Asin the former case of sustained oscillations,
it may be shown that BCD isa magnetic lag necessary for
the exhibition of such phenomena.
The electromotive force DB may be expressed by —AC as
before, and the general equation
Vo E—s
takes the form
Vee be! nC
dt
and, as this may be written
V-L& =(R+2)C,
we see that the extra consideration required to express the
actual state of things is simply that the resistance of the
circuit is virtually increased. In the previous work it is
necessary to write (R+)) in all the equations.
Heat of Vaporization of Liquid Hydrochloric Acid. 435
The actual work done altogether is derived from the charged
condenser. This is divided between the circuit and the field
in the ratio R:X.
It may happen, therefore, that if the circumstances of the
discharge are such as to make X very large in comparison
with R, the ordinary heating-effect may be minimized. Among
such causes is frequency, and in this consideration is to be
found the true explanation of some of the experiments of
M. Nikola Tesla. The energy of the discharges which that
physicist encountered was expended in chief part in radiation
which his body did not check, and not in current through his
body. It is here suggested that the best way to measure
radiation would be to measure the defect in the heating of a
_ circuit, taking care to note the P.D. of the condenser at the
moment previous to discharge.
In ordinary sustained oscillations, as derived from a machine,
the alternations are not of sufficient frequency to make the
effect of X perceptible. Hlectromotive forces of induction in-
volve the period in their denominators, and it is reasonable
to suppose that induced magnetic fields do the same; and if
the period of the electromagnetic vibrations becomes com-
parable with that of light, it is conceivable that mere heating
might vanish, as in the solar spectrum light has less heating-
effect than radiation of smaller frequency from the same source.
XLI. Note on the Heat of Vaporization of Liquid Hydro-
chloric Acid. By K. Tsuruta, Rigakush, Tokio, Japan*.
| the thirtieth volume of the Proceedings of the Royal
Society of London Mr. Ansdell gave a full account of
a series of experiments on the condensation of hydrochloric
acid. At the end of the paper he promises another commu-
nication containing his considerations on some thermodyna-
mical quantities relating to that gas, but this, so far as I am
aware, has never appeared. Although his measurements
have often been referred to and used by other physicists, yet
some of the deductions that can be made from them appear
still left untouched, for instance the heat of vaporization,
which forms the subject of this note.
For the sake of convenience of reference I- here reproduce
those measurements as contained in the following Table given
by Ansdell :—
* Communicated by the Author.
436 K. Tsuruta on the Heat of Vaporization
eel B ea |. m E F
| a eS == | oe ip gee eee
1 | 4 [19781 | agp | (755 | Teme) eee
2, | 995 11896 | ges | 790 | 1505 | 939
3, | 188 |10350| soy | 885 | 1239 | 37°76
4 | 11 | or77 | sty | 874 | 1080 | 41-80
2 | eon 910 | 9892 | 45°75
6. | 2675 6969 | a5, 900)
7. | 38:4 | 55°75 }*t | 1019 | B50 loam |
g | 394 | 4485 | ais | 1068 | 419 | 66-95 |
9. | 448 | 3634 | aaa | 1196 | 308 | 520
10, | 48 | 8138) gem | 1200 | 261 | 8080
11. | 494 | 27-64 | arg | 1292 | 218 | 8475
12. | 5056 | 2670 |... 14:30 | 1-79 | 85:33
eon | 346 | |
The column A gives the temperature of the gas.
The column B gives the volume of the saturated vapour at
point of liquefaction.
The column © gives the fractional volume of the gas at
point of liquefaction in relation to the initial volume
under one atmospheric pressure.
The column D gives the volume of the condensed liquid. —
The column E gives the ratio of the volume of the gas
to that of the liquid.
The column F' gives the pressure in atmospheres.
These data alone are incomplete to enable us at once to
deduce by calculation the heat of vaporization in terms of
the usual units (metre and kilogramme). Here are given
only the relative volumes of the saturated vapour and con-
densed liquid, so that their specific volumes at different tem-
peratures, which are wanted, are unknown. it will, however,
be enough for our purpose if we know their densities. Now,
Ansdell gave as results of independent measurements the
densities of the condensed liquid at different temperatures.
An interpolation formula, obtained between those densities
of Liquid Hydrochloric Acid. 437
and those temperatures, when combined with the numbers
given in the second and fourth columns of the above Table,
will enable us to find the corresponding densities of the satu-
rated vapour. The results thus found were not very satis-
factory. Another way to overcome the difficulty is to make
use of the numbers in the third column, which give the
volumes of the saturated vapour just at the point of lique-
faction in relation to the volume occupied by the mass of the
gas at the temperature ¢° (column A*) and under the pressure
of one atmosphere. If the specific volume of the gas under
the normal circumstances be known in terms of the usual
units, this together with the coefficient of expansion under
that pressure will give us the specific volumes of the satu-
rated vapour at different temperatures. Now, Biot and
Arago{ give the density of hydrochloric acid under the
normal circumstances to be 1:2474 in reference toair. There-
fore, the specific volumes under consideration will be given
by the following :—
il i fractional
Bae 1998 1-247: | volume | ree
When a long time ago I began my calculation I was not able to
get any information with respect to the coefficient of expansion,
and I assumed it perhaps not far from the value 0:008665.
Quite recently, however, I have found that it was determined
by Regnault f as long ago as 1843 to be 0:003681, and so I
have proceeded to recalculate. Of course no great differences
were thus wrought in the final values of the heat of vaporiza-
tion. It is, moreover, to be remarked that Regnault himself
did not put much confidence in the accuracy of his value on
account of an unavoidable admixture of air, very small though
it was, with the gas he investigated.
The formula for the heat of vaporization (according to the
notation of Clausius) becomes :-—
—__ 10883 1 di fractional a\ dp ,
TE T393 ‘Toa7 | volume |* (+44) (1-2 au:
in which the ratio o/s is to be supplied by the numbers in
the second and fourth columns of the above Table.
* As it must have been, although it is not explicitly mentioned,
t+ Wiillner, Lehrbuch der Physik, iii. p. 150.
{ Ann. de Chimie et Physique, série 3, tome iv.
IN
438 Heat of Vaporization of Liquid Hydrochloric Acid.
o was calculated from the following interpolation formula
found by the method of least squares :—
p=28'451 + 0°4914 t+ 0:012463 #,
in the evaluation of whose constants the numbers in the
eleventh row in the above Table were omitted, because the
representative point in the p- and ¢-curve was much out of
the general course. p (calculated) in the following Table
are from the above interpolation formula, whose use is amply
justified by the numbers in the difference-column.
| |
}
|
| | iP P ; o P,P
| us || (observed). | (calculated). Tinie =e 5 |
j | atm. atm. calor. |
1. 4 29°8 |), a h061 +0°81 61-02
2. 9:25 | 33°9 34:10 +0°20 64-99 |
3. 138 37°75 3760 —O0°15 65°77
4, 18:1 | 41°8 41°45 —0°37 65°45
dD. 22 | 45°79 | 45°29 —046 || 63°51
Geo, Sen We pd 50°57 —043 | 60:02
7. 30-4 58°85 | 58:76 —009 | 5317 |
8. 39°4 | 66°95 67:15 +020 || 45-18
ae) ASS | 152 7547) | «= 4026 I ae
tO) as 80°8 80°75 | —005 | 30°08
a4 2 494 84:75 8914 | —161 | 20°49
1954) P5056.) || 85°33 85:22 0a
13. 51 |
i | H
| |
The manner of variation of these numbers for 7, as deduced
from the observations of Ansdell, is very remarkable. From
4° to about 14° the heat of vaporization increases, attains
there a maximum value, then decreases in a regular manner,
but from about 45° onwards it diminishes quite rapidly, as if
the gas were preparing for the critical point (51°25), at
which the heat of vaporization is to vanish.
Among those substances whose heat of vaporization was
investigated by MM. Cailletet and Mathias * we have no in-
stance like hydrochloric acid. It is much to be desired that
any one who has proper instruments in his possession will
take the trouble to decide whether the anomaly is real or
whether there were some mistakes in our data.
* Journ. de Physique, tom. v. 2° série, 1886. Also, zbid. tom. ix,
2e série, 1890.
[ 439 7
XLII. Note on the Flow of Water in a Straight Pipe.
By M. P. Rupsx1, Priv. Doe. in the University of Odessa *.
T is a known fact that the law of resistance to the motion
of a liquid in pipes and channels of great size differs much
from that in capillary tubes. It is also known that this differ-
ence is due to the presence of eddies in great pipes, while in
capillary tubes the liquid flows in straight lines. Prof. Osborne
Reynolds + has shown that there exists a certain critical mean
velocity, depending on the diameter of the pipe and on
the temperature (7. e. viscosity) at which the eddies must
appear. He thinks that the appearance of eddies is due to
the instability of rectilineal motion. But Lord Kelvin ¢ has
shown that at least for small disturbances the rectilineal
motion is stable provided the coefficient of viscosity is not zero.
Although Lord Rayleigh § thinks that Lord Kelvin’s proof is
not quite convincing, it seems to me to be so, because the
steady rectilineal motion with zero velocity at the walls
satisfies the condition that the loss of energy shall be the
least possible. This motion belongs to the type which was
shown by Helmholtz to have this property ||. Now itis known
that generally the motions, which in a certain manner satisfy
the minimum or maximum condition, are stable.
The same question was also treated by Mr. Basset 4]. He
has found the rectilineal motion unstable. As far as I can
understand him, from a short communication, it was only
after he had introduced in the expression of resistance a term
depending on the square of relative velocity. In doing so he
has anticipated the law of resistance proper to the eddying
motion. On the other hand, he finds that without this term
the steady rectilineal motion remains always stable. His
results also agree closely with the results of Lord Kelvin.
It seems to me that all this clearly agrees in showing
that it is not the question of stability or instability which
arises here, but another one. In speaking of stability we
mean ¢o ipso the tacit assumption that the eddying motion
may be also expressed with the help of functions satisfying
the common partial differential equations of viscous fluid
* Communicated by the Author.
+ Phil. Trans. 1885, p. 935.
{ Phil. Mag. 5 ser. xxiv. pp. 188 and 272.
§ Phil. Mag. 5 ser. xxxiv. p. 67,
|| Basset, Hydrodynamics, vol. ii. p. 356.
4] Proceedings Roy. Soe. vol. lii, no, 317, p. 273.
440) On the Flow of Water in a Straight Pipe.
motion. Our equations of disturbed motion serving to inves-
tigate the question of stability are the same hydrodynamical
equations with certain terms neglected. These equations, as
Lord Kelvin has proved, show that the undisturbed motion is
stable. But if we introduce something that is not contained
in the hydrodynamical equations, as Mr. Basset has done, we
find the sought instability.
In other words, our hydrodynamical equations, which we
know to be strictly true only for small relative velocities, are
now shown to be, in the case of water, of very limited im-
portance. They are not able to express the eddying motion.
In the motion which they are able to express, any surface
drawn within the liquid is supposed to be strained in a con-
tinuous manner. In the eddying motion these surfaces
are continually breaking and again reforming, an opinion
which seems not to be new to hydraulicians *.
The opinion that it is with a real breaking that we have to
do is strongly supported by a striking fact observed by Prof.
Reynolds. The eddies appear only at a certain distance from
the entrance of the pipe. This distance is diminishing when
the velocity increases, but diminishes asymptotically. Now
it is a known fact that the breaking of bodies, solid, plastic,
or plastico-viscous, depends not only on the amount of the
strain, but also on the velocity of straining. Even hard
bodies sustain a great strain when the straining is slow
enough ; on the other hand, fleazble bodies, when very rapidly
strained, Sreak down.
On the other hand, when the liquid enters the pipe tumul-
tuously, but with small mean velocity, the viscosity begins to
act at advantage, the breaking ceases, and the eddies die out.
Reynolds has shown that this reversal trom tumultuous to
quiet motion occurs at a critical mean velocity, which ceteris
paribus is about 6-3 times smaller than the other mean velocity
which renders the quie* motion impossible.
All other features of the phenomenon—the dependence of
critical mean velocity, z.e. of the critical rate of straining, on
the viscosity and on the size of the tube—are clearly in best
accord with the hypothesis of breaking for a certain critical
rate of straining.
The existence of two critical velocities—a greater which
makes the quiet motion impossible, and a smaller which
makes the tumultuous motion impossible—is very interesting,
and shows similitude to many other physical phenomena.
* See Boussinesq, ‘* Kssai sur la théorie des eaux courantes,” Mém,
Sav, Etr. vol. xxiii. p. 5.
er 44 @ 7
XLIL. Liquid Friction. By Joun Pury, F.R.S., assisted
by J. GRAHAM, B.A., and C. W. Huatu*.
: [Plate VIL]
PIECE of apparatus such as is used in this investi-
gation was designed and partly constructed in Japan
in 1876 ; it is described in my book on Practical Mechanics
(1883). The specimen actually used by us was constructed
at the Finsbury Technical College in 1882, and has been
occasionally used since that time, but no complete sets of
observations were attempted till October 1891.
The simplest hydrodynamical condition of viscous fluid is
that of the fluid bounded by two infinite parallel planes, the
fluid in one boundary being at rest, the velocity in the other
boundary being constant and in the plane. Motions in a
pipe and near a vibrating disk, or even near a steadily
rotating disk, are rather complicated. Our apparatus was
designed to approach as nearly as possible to the conditions
subsisting between the infinite planes. Between two such
planes, if V is the constant velocity of one of them, the other
being at rest, and 0 is their distance asunder, the fluid being
of uniform density, and gravity being neglected, if 2 is
measured at right angles from the fixed plane, the equation of
steady motion is
d?
Vv .
dz’ = 0, SyMeEE Tt 1 eis Mine key sn (1)
a DF NGS By Fem ae ome iaas a (-)
and the tractive force per unit area required at the moving
plane to maintain the motion is «V/b, where mw is the co-
efficient of viscosity. We have used, instead of planes,
concentric cylindric surfaces of as large radii and as small
difference in radii as could be conveniently constructed and
used (see Pl. VII. fig. 2).
EEE is a cylindric trough, of which the curved parts
K and E are brass. The inner and outer radii of this trough
are 10°39 and 12°65 centimetres. C, which forms the bottom,
is of iron; and the whole trough can be rotated about its
vertical axis at any desired speed by driving the pulley P from
a coned pulley D with numerous steps.
G is a hollow brass cylinder supported by a steel wire L,
of 0:037 centim. diameter, 67°78 centim. long, whose axis
coincides with the axis of the trough and the axis of
* Communicated by the Physical Society: read March 24, 1893,
449 Prof. J. Perry on Liquid Friction. -
rotation. G may be raised or lowered relatively to the trough.
The outer radius of G is 11°63 centim., the inner being 11°41
centim. The whole apparatus is supported on a stand, with
three adjustable feet. We exhibit also some photographs of
the apparatus in position, showing how it was driven. —
The trough contains the liquid whose viscosity is to be
measured : when it rotates, G tends to rotate ; and when for
any constant speed G is in equilibrium, the twist in the steel
wire measures the torque due to the tractive forces with which
the liquid acts upon G at its inner and outer surfaces. The
twist was measured by the angular motion of a pointer clamped
on the wire at a distance of 59 centim. from the fixed end.
To test the accuracy of our assumption that the fluid
behaved as if between parallel plane surfaces, let us consider
the actual motion in which the stream-lines are circles.
Consider the motion of a stream-tube of section 6r 6z,
«2 being measured axially and 7 radially. The tangential
? e s e e . du Uv e
force on unit cylindric surface of radius 7 is (Ss Re if
v is the velocity. The moment due to all such forces on
the inner surface of our ring is
The moment tending to increase the velocity of the ring due
to forces on the cylindric parts of it is therefore
Cte AGG
ET + a= — 3) 8r Bars
also, due to the plane faces we have the moment
d?v
Qerpr®—. Sy. Bx.
ie or. 6a
Equating the sum of these to the rate of increase of the
moment of momentum of the ring, we have
i AGGv hi Oe, CO apade
dtd Pp tde ad 7 7
as the equation of motion in co-axial circular stream-lines.
Now the discontinuity at the edge, and also the nearness of
2
the bottom of the trough, cause the term ad to be important;
dx
but the solution seems to be very difficult. Maxwell satisfied
himself (Collected Papers, vol. ii. pp. 16-18) that the dis- —
continuity at the edge of a vibrating disk could be allowed
Prof. J. Perry on Liquid Friction. 443
for as a virtual increase in the radius of his disk, and the
assumption that the behaviour of his fluid was the same as if
his disk were part of an infinite disk. The correction not
being readily obtained for a disk, he assumed it to be the
same as for the straight edge of an infinite plane surface. We
are certainly not less correct in taking the same correction
for the edge of our cylinder*. Following Maxwell, there-
fore, we assumed that when our cylinder G was immersed
to the depth AB or J in the fluid it was really a portion of
length /-++X of an infinite cylinder of the same diameter. We
2
therefore neglect a in (3), and we use
Ge bedtn. 30 2. p
CIE ET Gi Pe ST oe VN ete (4)
When the motion is steady, that is when dv/di=0, the
solution is
. Ey Pa aM wet! LAS A)
If v=v, when r= R,, and v=0 when R=R,, then
v= Ry (7 — R,?/r) /( RY — R,’) °
We must now distinguish between the space outside the
suspended cylinder and the space inside it. The radii of the
inner and outer surfaces of the suspended cylinder are 11°41
and 11°63 centim., and the inner and outer radii of the trough
are 10°39 and 12°65 centim.
Our cylindric surfaces were not perfectly true, although
great care was taken to make them so ; and the radii given
are only average dimensions. But, inasmuch as slightly
tilting the apparatus or otherwise putting the axis of the
suspended cylinder out of coincidence with the axis of the
trough made only small differences in the observations, we
did not think that such inaccuracies of workmanship or mea-
surement as existed could affect our results.
Even when the tilting of the apparatus was quite evident
to the eye, the tractive torque was found to be only slightly
increased by the tilting. Of course, as the suspended cylinder
* It is to be remarked that Maxwell assumed, generally, that there was
no radial motion of his fluid. Now there must have been radial motion,
his disks resembling centrifugal fans in their action, creating a variable
flow always outwards between his fixed and moving disks; and the
energy wasted in producing this flow is neglected by him. We do not
know the amount of this error, and he may have satisfied himself as to its
insignificance. Prof. Maurice FitzGerald in criticizing this proof has
pointed out the fact that on James Thomson’s theory of river bends there
must exist a radial motion of an interesting kind in our apparatus.
444 Prof. J. Perry on Liquid Friction.
got closer and closer to the side of the trough the torque did
increase, and became very large when the suspended cylinder
nearly touched the side of the trough.
Again, it was observed that at our highest speeds the
amount of wetted surface did not perceptibly alter ; and we
are, we think, justified in assuming that the surface of the
liquid was always a plane surface.
It is evident that the tractive forces on the suspended
cylinder are the same whether we assume the trough to
revolve steadily at m radians per second, the suspended
cylinder being at rest, or the suspended cylinder to revolve
steadily at w radians per second and the trough to remain at
rest. We shall therefore, for ease of calculation, always
assume the trough to be at rest and the suspended cylinder
to be revolving at w radians per second. Then the velocities
of its inner and outer surfaces are, in centimetres per second,
11:41 and 11°63.
On any cylindric surface the tractive force per unit area
: B
being p(—) is == @ from (5); so that, whether for
the outer or inner space, if R, is the radius of the suspended
moving cylindric surface, and R, the radius of the fixed
surface, the tractive moment per centim. of length is
+ Arrow Ry /(R?/R?—1).
Taking actual sizes, this is 0°5 per cent. greater than the
value obtained by calculating the forces on the assumption
that the fluid moves in plane layers as in (2), 6 being the
actual thickness of fluid 1:02 centim., and V being the actual
velocity at the mean radius. We may, in fact, imagine the
speeds to be increased by 0°5 per cent., and make all caleu-
lations as to viscosity on the assumption of motion in plane
layers.
The tractive torque per centimetre of length of cylinder is,
in our case, 19010yo, or 1991 ny if the angular velocity
is given as x turns per minute. If / is the wetted length
in centimetres, and A is the virtual additional length repre-
senting the edge effect, the total torque is 1991 nu(l +2).
The total observed motion of the pointer being D degrees,
and the torque per degree being a, the torque due to tractive
forces acting on the cylinder is
aD = 1991 nu(l+A) ;
and if this law is found to be true experimentally, then
p =aD/{1991(1+a)n}. . 2 . . ©)
Prof. J. Perry on Liguid Friction. 445
Two methods of determining the torsional constant of the
wire were employed :—
First Method.—A fine cotton thread was wound round the
outside of the suspended cylinder and passed over a nearly
frictionless pulley (the pulley of an Attwood’s machine) to a
scale-pan. The thread was nearly horizontal as it left the
cylinder. In this way it was found that the twisting moment
required to produce a pointer-rotation of one degree was
1531 dyne-centimetres. In making the measurement as the
weight of the scale-pan and its contents was gradually
increased, the steel wire was drawn away from the vertical,
and therefore from the middle of the scale; but the stand
was tilted to counteract this effect. |
The effects due to solid friction were eliminated by taking
the mean of the limiting weights for equilibrium. When the
weight was 30 grams, one tenth of a gram either added to or
taken from the scale-pan produced a perceptible change in the
position of the pointer ; so that the solid friction was small.
Second Method.—The suspended cylinder was allowed to
vibrate, twisting and untwisting the wire ; and its times of
oscillation were noted. ‘The observations were repeated when
a known moment of inertia had been added. Unloaded, it
made 40 complete oscillations in 583 seconds, or one oscillation
in 14:575 seconds. We then attached to the cylinder an iron
bar of rectangular section, whose own moment of inertia had
been determined accurately by previous experiments (found
to agree with calculation on the assumption that it was homo-
geneous), this moment of inertia being 566°2 (in gram-
centimetre? units). The time of a complete oscillation was
now found to be 21:425 seconds. It follows that the moment
of inertia of the suspended cylinder is 487°72, and the tor-
sional constant of the wire is readily obtained. ‘This constant
being corrected on account of the position of the pointer, it
follows that to produce a rotation of the pointer of one degree
requires a torque of 1552 dyne-centimetres. This is greater
than the constant derived from direct measurement by 13 per
cent. ; but, on the whole, we are rather inclined to accept the
number obtained directly, as we are not quite sure that the
mean position of the iron bar was at right angles to the mag-
netic meridian.
Hight quite independent measurements of the diameter of
the wire were made by men experienced in making such
measurements ; and the mean value was ‘0371 inch, the
greatest and least being "0373 and ‘0369. Using this mean
value, and the directly measured torsional constant, it would
seem that the modulus of rigidity of the steel is 7°71 x 10”.
Phil. Mag. 8. 5. Vol. 35. No. 216. May 18938. 2H
446 Prof. J. Perry on Liquid Friction.
As an error of ‘0004 inch in the diameter measurement leads
to an error of 4 per cent. in the modulus of rigidity, and as
the modulus of rigidity usually taken for steel is 8°19 x10",
we believe that our constant 1531, as directly measured, is
sufficiently correct for practical purposes.
In using (6), then, we take a to be 1581.
The virtual addition \ ought, by Maxwell’s formula, to be
0:52 centim. in our case. But the bottom of the trough H
was only 0°5 centim. from the edge B of the suspended
cylinder in most of our experiments, and we do not know how
to calculate for this. Our experiments have shown that when
this distance is 0°5 centim. the twisting moment at a given
speed is practically the same as when the distance is much
greater ; but we did not know this from any theory, and,
besides, it is always rather dangerous to depend upon a
theoretical calculation of X such as Maxwell was compelled to
use. It is possible, also, that a correction of the same kind
ought to be introduced for capillary and other actions at the
surface of the liquid. The action of the atmosphere was in
any case negligible, because when there was no liquid present
in the trough, so that there was an action of the air several
times greater than ever occurred during the experiments, the
deflexion was quite imperceptible at much higher speeds than
those used in the experiments.
The temperature being kept as nearly as possible constant,
but probably varying between 18°°9 C. and 20° 1 C. (stated
as 19°°5 C.), the following experiments were made with
sperm-oil, beginning with a small quantity in the trough and .
ending with a large quantity. The bottom of the trough was
in every case 0°5 centim. below the edge of the suspended
cylinder.
TasLe I.—June 9th, 1892.
| Defiexion D when
MN, | ) ] |
| ¢=0°O em. | /=2°5 em. | 7=5 em. l=7-d5 em. | /=9-9 em. |
50 24 67 112), 1, tee
49 re hy cs = 196 |
48 | |
40 oo eae 3. ee 163
39 fn, fea ee
23 io: | | |
175 8 k 57 ees
ae RRs. 2 24 39
Ae NE gi ial b> ld 40
115 |
11 | | a a es
Prof. J. Perry on Liquid Friction. 447
As the deflexion is sufficiently nearly proportional to the
speed to allow of corrections by this rule when the cor-
rections are small, we have corrected the above observations
to ene speeds 50, 40, 174, 114; and we obtain the following
results :-—
|
Values of 2.
Values of /. cs
| 50. 40, Mie 114
| 5 24 18 Sms 5
| 25 67 54. | 25 16
5:0 1h 93 40 | 27
| TD 165 132 7 Cie |
| 99 | 200 163 735 | 51 |
D and / were then plotted as the coordinates of points on
squared paper ; and it was obvious that for each value of n
these points lay very nearly in a straight line, and all the
straight lines passed through the point/=—0°8. Itis curious
that the lmear law should hold for such small values of / as
0-5 centim., and for high speeds as well as low speeds. We
shall presently see that some of these speeds are considerably
above the critical speed at which (4) ceases to represent the
motion.
We may take it, then, that »=0°8 centim., which is greater
than the calculated value 0°52. The discrepance cannot be
due to the distance BH being small, for we have altered this
distance and found no perceptibly different results. As
already stated, it may be due to some capillary surface action.
Taking a=1531 and X=0°8, we have (6) becoming
e—0T6Dne@tOSe . . . . @)
Of course our results are consistent with our equations of
motion only so long as D/(¢+0°8) is proportional to n.
Many observations have been made with this apparatus
during the last year on various liquids, under very different
conditions of temperature and speed and depth. We give
here a set made on sperm-oil. In all cases the bottom of the
trough was 0°5 centim. below the edge of the suspended
cylinder.
Keeping the oil at a constant temperature we ran the trough
at a number of speeds, and repeated at other constant tempe-
ratures. The results are given in Tables LV. to XI.
When a temperature had to be taken the rotation was
stopped and a thermometer dipped about halfway down in the
oil, the reading being taken at the end of about half a minute,
2H 2
448 Prof. J. Perry on Ligud Friction.
A small Bunsen flame was applied underneath the trough
when a temperature higher than the room had to be main-
tained for a considerable length of time.
As the temperature varied slightly, and we wished to reduce
our observations to constant temperatures, we afterwards made
two sets of observations at very varying temperatures but
constant speeds. These later observations we shall consider |
first. They are given in Tables II. and III.
TABLE IJ.—March 29th, 1892. (d=8°275 centim.)
pote {a D)
a a OF 1): EN | L. LE peed
= — = = a
Pesoa iss f 189 10> 21-09 | ‘400 | +446
| 395 | 171 | 165 |- 1760 | 834 9) eee
40 195 || 150 | 1653. |- 31877) Gees
40 24-0 | 184 .| 1477 | -Os7) | aan
40 253 | 1965 | 1394 | -268 254 |
40 89 | 1115 | 12:28 236 PS ial
40 32:0 109 11:46
40 42-5 | 88 9-70
i 40 469 81 8-65
40 585 | 67 TU |
40 64.0 | 58 6-39
aor emo | 56 bisa fl | |
| ee Ue a cg | |
40 85:5 | 5:12 | |
The numbers in the column headed av are obviously ;
De
n l+nr
intended to be corrections of D/(/+ 2) for the constant speed
of 40 revolutions per minute.
TABLE II1.—March 380th, 1892. (/=7:78 centim.)
7 ]
: 9a)
| SO ae er | ‘Dea oe Fee HB calculated.
aes —_———_|—- — SS —- —___|_ —=
| 8°75 52) 1160 ©) 19-19 | Sige 2-06
975 | 80 85 9°15 0-78 0:82
92 | 100 57 6:56 0-73 | 062
9-0 108 47 548 | 047 | 9056
9:0 16°6 36:5 | 4:96 | 0363 | — 0-366
9-2 248 26°5 | 3:02 | 0-258 0259
9-0 35-0 19:5 | 2:27 =| 0-194 0196
9-0 47-0 140 1:63 0-139 0:137
9-0 565 10-2 119 | 0-101 0-104.
9-0 67:0 8-0 0-93 0-079 0-081
9-0 89:0 5-4 063 0-060 0-058
9-0 84:5 6-0 070 | 0054 0-054
a
Prof. J. Perry on Liquid Friction. 449
The numbers headed : S are intended to be corrections
of D/(J+2) for the constant speed of 9 revolutions per minute.
We have plotted the numbers in the last columns of these
tables with @ upon a sheet of squared paper; but it is
unnecessary to publish the resulting curves. We exhibit
them to the members of the Society.
Knowing what has been done by Prof. Osborne Reynolds,
it seemed unlikely that one simple formula should satisfy
either of these curves ; that is, it was likely that in the lower
curve there was some temperature for which the speed n=9
was a critical speed, and there was also a temperature for
which n=40 was a critical speed. We therefore used the
curves merely for small temperature-corrections in our other
experiments, in which we kept the temperature nearly
constant.
It was therefore without much interest that, in preparing
this paper for publication, we tried to obtain empirical formulee
for these curves ; and at first we used, not the observations
themselves, but the observations as corrected by curves drawn
upon squared paper.
When log (@—4:2) and log Try are plotted as coordinates
of points on squared paper, we were astonished to find that
when n=9 the points lie in two straight lines. The allinea-
tion of the points is very striking, even when the uncorrected
observations are taken, and leads to the following empirical
formula :—
Letting @ denote @—4:2, and letting y denote D/(/+))
the torque as measured in dégrees deflexion of pointer per
unit length of wetted cylinder ; then, at the constant speed
orn 9,
yo =constant for temperatures above 40° C.
yp =constant for temperatures below 40° C.
On plotting logy and log @¢ for the constant speed n=40,
the points are not found to lie so nicely in straight lines, but
there does seem to be some sort of discontinuity at a tem-
perature of about 45° C.
At first we thought that these temperatures were the tem-
peratures at which the speeds n=9 and n=40 were the
critical speeds, and we were greatly concerned because our
result seemed to be quite out of accord with the reasoning of
450 Prof. J. Perry on Liquid Friction.
Prof. Osborne Reynolds*. As his ingenious theory has been
completely verified by experiments made upon the very
smallest and largest pipes with flowing water, and as it is
simple we had adopted it for the reduction of our experiments.
According to his theory, Tk or, as we shall call it, y,
ought to be proportional to 7 until n exceeds a certain value;
this value being a function of u/p, where p is the density of
the fluid. Now the alteration of p with temperature in such
a liquid as sperm-oil is so small that the error in neglecting
it is small in comparison with our errors of experiment.
Neglecting, then, the alterations in p, the theory of Prof.
Reynolds leads to
y = al?-*n*, . en
where F is a function of the temperature, n the number of
revolutions per inute ; where «=1 until the critical speed
m, 1s reached, n. being proportional to I’, and « having a
higher value than 1 for all speeds above the critical; @ is a
constant. This is on the assumption that Prof. Reynolds’s
theory would lead to the sume result in our case as in his
pipes.
Now, in the first place,it seemed absurd that the temperatures
for which the speeds 9 and 40 were the critica] speeds should
be so near to one another as 40° C. and 45° C. But a much
more serious consideration was this. According to. any rea-
sonable application of the theory to our case, at constant
speed, if yp” is constant when the speed is less than the
critical speed, and if yd* is constant when the speed is
above the critical speed, then s ought to be less than m,
whereas 1°349 is about twice 0°686. We came to the con-
clusion that the point of discontinuity has nothing whatever
to do with the critical speed ; indeed, we subsequently found
it probable that n=9 does not become the critical speed until
the highest temperature of Table III. is reached.
Using the deflexions in Table ITI. to determine « according
to (7), we have the results given in column 5 of the Tables.
The numbers in column 5 of Table I. are calculated for tem-
peratures lower than 26° C., which is about the temperature
at which 40 is the critical speed. In some of the following
tables, giving the results of experiments made at various
constant temperatures, we have also given values of w. There
* “ An Experimental Investigation of the Circumstances which deter-
mine whether the Motion of Water shall be Direct or Sinuous, and of the
Law of Resistance in Parallel Channels,’ by Osborne Reynolds, F.R.S.,
Phil. Trans. pt. iii, (1883), |
Prof. J. Perry on Liquid Friction. 451
is as much consistency in all these results as might have been
expected. We lay most weight upon the results given in
Table ITI., which lead to the laws
ro 2:06(0—4-2)\e 8 below 40° Cy. 22. |. (9)
p= 21-60(G—4-2)-!* above 40° ©. .... . (10)
We have searched in books in vain for a mention of a dis-
continuity in any other physical property of sperm-oil about
this temperature ; but we have already begun to experiment
on its other physical properties, as it is unlikely that there
should be a discontinuity in the law for the viscosity alone.
At the same time, we may say that our chemical friends see
no reason for a confirmation of our belief.
In the tables we give the viscosity as calculated from these
formule ; and it will be seen that they agree well enough
with the observed viscosities.
TasBLe [V.—March 18th, 1892.
(l=6°15 centim. Temperature Constant, 17°°5 C.)
, or
1 _ DU-LA). M
36 114 16-41 351
39 121 17-41 344
54 172 24-75 352
69 245 35:26
80 300 43°16
92 B45 49-64
28 74 10°65 356
16 52 7-48 360 |
13 A ee 500 349
8°75 o7 3:98 349
{
The column headed pw is 0°769D/n(l+ A), and has no
meaning at a speed greater than the critical speed. The
critical speed, 7, is probably about 50. The first three and
last four values are probably measurements of w. The average
value of these seven is w=0°351. Formula (9) would make
pf to be 0°349.
Plotting logy and logn as the coordinates of points on
squared paper, the points lie very nearly in a straight line
indicating yan until the critical speed, about n=50, is
reached, and for all higher speeds the points lie nearly in
another straight line indicating y an’,
452 Prof. J. Perry on Liquid Friction.
Taste V.—March 21st, 1892. (=6°075 centim.)
0° C, Nn. 1D; Y- pi.
22:5 9:25 24°5 3°40 ‘283
232 11 28°0 397 ‘278
22°7 14:2 37 5:16 ‘280
22:0 17-2 45 6°15 ‘279
25:0 27 68 10:19 ‘277
24-5 23 57 8-41 281
24-0 32 “Eh 11-20 ‘269
23:0 90 340 48:00
22°5 102 410 - 56°96
23:0 80 276 38°94
24-0 72 224 32°58
24:5 56 169 24-95
24-0 48 129 18°76
23°5 43 _ 108 15 42 ‘278
230 38 eo 13-69 ‘217
The column headed y is D/(/ +) corrected to the constant
temperature of 24° C. by a correction of about 3 per cent. per
degree. The numbers in the last column have no meaning
for speeds higher than n=about 48. The average value of p,
the viscosity, in the first seven and last two observations is
0-278. Formula (9) would make w for this temperature
0-266.
Plotting logn and logy on squared paper gives points
lying nearly in two straight lines, showing that y an to the
critical speed n=about 43, and above that speed y an'*",
TaBLeE VI.—March 21st, 1892. (J=6:075 centim.) —
| | |
G2. | n 1D), | y
SS ae a a Eee
29°5 | 38 81 | 11-63
30 | 43 95 13°82
31 48 114 16:99
30°5 56 134 19-73
30°5 60 147 | 2165
|
y here means D/(/+ 2) corrected to the constant temperature
of 30° C. by a correction of 24 per cent. per degree. yp as
calculated from (7) would have no meaning, as the critical
speed for this temperature is about 28 revolutions per minute,
and we give no column headed w. y¥ is very nearly an,
Prot. J. Perry on Liquid Friction. 453
TaBLE VIT.—March 22nd, 1892. (/=5°4.25 centim.)
|
g°C n Dp: y HL
56 38 49-5 792
59 42 59 9:20
55 54 125 11°31
56 58 88 14:13
56°5 14 116 18°79
575 108 158 26°32
58°5 29 34 578
56 24 25 4-01 "1282
57 17°95 ll 1-81 ‘0791
57 155 14 2°31 "1148
54 155 12 1-82 ‘0903
55 16 14 2°19 1054
y means D/(/+X) corrected to 56°C. by a correction of
24 per cent. per degree. The critical speed is probably below
n= 24, and for speeds greater than the critical y «n!* nearly.
For speeds less than this the average value of pu is 0°103.
According to (9) the value of mw for 56° C. is 0°1055.
Plotting logy and logn as the coordinates of points on
squared paper gives points which may be said to lie on two
straight lines, but the errors of observation are too great.
For n>24 we might perhaps say that y «n!?5; but it seems
hardly fair to draw conclusions from this set of observations.
TasnE VIIL.—March 24th, 1892. (/=7:025 centim.)
in 0° OC. nN. D. | y. | bh. |
30 100 363 45 24. |
30°8 78 250 31°79
31 115 404 51-64
31 32 62 7:92 ‘1903 |
= 3l 22 47 6:01 ‘2103 |
3} yy 37 Ae 14 |
39 13 29 3:80 49 |
31 ll Dae) 3°00 “2097 |
30 9:2 20 2°50 209
-yis D/(l+X) corrected to 31° C. by a correction of 24 per
cent. per degree. The numbers of the last column have no
meaning for speeds higher than n about=32. The average
value of w is 0°210. According to (9) the value of w for
en CO. is 0°216.
Below n=382, y an,
Above n=382, we may perhaps say
that y an, : .
Prof. J. Perry on Liquid Friction.
TaBLE [X.—March 28th, 1892. (=6°525 centim.)
0° C: n, D. | Yy-
81 38:5 3 | 518
80°5 56 63 | 8-557
80 69 88 | 11-80
79-5 84 112 | 14-70
Bus 104 134 18-29
83 92 116 16-157 |
y means D/(l+2) corrected to 81°C.
The law seems to be 7 «n!? nearly.
TABLE X.—March 23rd, 1892. (/=7:025 centim.)
0°C. n Pp; Y:
82 17°5 16 2°06
82 14 11 1:23 |
82 26 26 3°35 |
81 32 33 4-22
80 11°5 8:5 1:08 |
82 10 Gia 0°84
If it is assumed that n= 10 is not much above the critical
speed, w may be calculated as 0°0646. According to (9)
p=0°062 for 81°C.
y an* may be taken as the law.
Taste XI.—March 24th, 1892. (/=6-7 centim.)
D y. HB.
65 4 8 1:07 091
66 10:8 9 1:21 | -086
65:5 17 16 914. | 2asza
64:5 21 21 279 |
65 23°5 26 3:46 |
ee on65 29 32 426 |
| 65 114 210 28:00. |
| 66 102 162 21-82
| 645 88 156 20:10
| 65 66 112 14-93
[24 66 52 74 9-96
66 44-5 59 7-94
66 38 46 6:19
|
y is D/(1+2) corrected to 65°C, jw has no meaning except
for the first three speeds, and the mean of these three is
0-091. According to (9) the value of w for 65° C. is 0-085.
j
Prof, J. Perry on Ligud Friction. 455
Above the critical speed, which is possibly below n=17,
the law is probably y an’.
lt is not worth while to publish any of the observations
which we have made upon other liquids, nor to publish the
curves we have drawn for sperm-oil, although we exhibit
them before the Society. Hrrors of one degree in obser-
ving temperature were quite possible, and errors of half a
degree in the deflexion of our pointer were also possible.
Small fluctuations in speed were continually taking place, so
that the pointer was never quite still, the motion of the fluid
was therefore not truly steady. It is our determination to
repeat the whole work with improved apparatus. In the
meantime, however, it will be observed from Table III. that
there is fair agreement in the law connecting w with tem-
perature, from all the sets of observations. There is, on the
whole, a very fair agreement with what we venture to call
Prof. Reynolds’s rule,
ie
=a en,
where « has the value 1°33 or 1 according as n is above or
below the critical speed*. The sheet of squared paper on which
we have plotted all our values of log y and log n for the various
constant temperatures shows that the errors of observation are
too great for the establishment of this value of «; but it is the
probable value. It shows, however, in the allineation of the
points of discontinuity, with sufficient accuracy that y, co n,”,
if the rule is taken to be generally true; and although there
is some little vagueness always in one’s observations just about
the critical speed, we may take y-=0°009 n,? without very
ereat error. Indeed, we are satisfied with the substantial
agreement of all our observations with the formula
hee be 2—k P
y=( ae95) ny
* Prof. Reynolds, in criticizing a proof of this paper, has been kind
enough to point out that his rule for pipes does not necessarily apply to
the fluid in our apparatus. We had not seen the reprint of his Royal
Institution lecture, else we should have known that the condition of the
liquid in circular flow is inherently stable or unstable according as » is
greater or less than the radius of the fixed cylindric surface. As he
points out, the liquid in the outer space is inherently stable for velocities
far exceeding the critical velocity (if there is one) for plane surfaces,
whereas the liquid in the inner space is unstable from the first.
We directed the attention of the meeting to the fact that Tables IV.,
V., VI., and VIII. give unmistakable evidence of the truth of what
we have called Prof. Reynolds’s Rule, however difficult we may find it in
explanation.
456 Prof. J. Perry on Liquid Friction.
where a='009 and «=1'33, That is, for low speeds we have
the law
SIE ad
PS
At the critical speed the law suddenly changes to
Ss a( eg s) >
which holds for all higher speeds which we have tried, The
critical speed
= 1444,
1
ea oa
OO a.
and
=O, OF WI WE.
It is to be recollected that p is too nearly constant for us
to say with certainty that a is proportional to p, as the theory
requires. The errors of observation were so great that it was
not worth while finding accurately the most probable values
of « and a.
We wish it to be understood that our apparatus was very
carefully constructed, and great care was taken in making the
observations ; but it is our intention to pursue the investiga-
tion with apparatus much more carefully constructed.
Vibratory Hxperiments.
In designing the apparatus it was our intention to obtain wu
from the damping of the rotational oscillations of the suspended
cylinder about its vertical axis, the trough being at rest. We
meant in this way to obtain w for velocities very much smaller
than those which could be employed in our steady motion ex-
periments. A considerable number of observations were made,
but when we tried to make calculations of ~ we found that our
mathematical difficulties were too great, and after many months
of effort we are forced to say that we are unable to utilize these
observations. In equation (4) assume that v=we'*, and w
may be obtained in Bessel functions. Unfortunately, as there
are two surface conditions, doth particular solutions of the
Bessel equation are necessary, and the work of reduction be-
comes very great. An approximate solution is obtained by
taking r= R-+ 4a, R being the radius of the suspended cylinder,
and taking the equation (4) to be
Oy yk aie 6?
de Rida RO ame
Making this assumption in the case of steady motion, it was |
found that it was sufficiently correct for practical purposes.
(11)
i
4
:
4
Prof. J. Perry on Liquid Friction. A457
The following numbers show the sort of error introduced,
taking R=10, and 1 the greatest value of w.
=
Values of v.
festa OD = =a
Values of x. | On the assump- |
Correct. | Approximate. | tion of motion
| 'in plane layers.
De ee ee es
0 \ l |
2 7914 7914 8
5 4875 4872 5
7 2895 2892 3
1-0 0 | 0 0
)
The solution of (11) for vibratory motion is easy enough ;
but we found it still difficult to calculate w from our observa-
tions. Hven when we assume that the motion is in plane
layers, so that the solution used by Maxwell is employed, we
find that our - is too great for a logarithmic decrement to
exist with such amplitudes and times of oscillation as we had
employed in the experiments, and it was impossible for us to
repeat the experiments under the same conditions again at
slower velocities, because the apparatus had been taken to
pieces and could not be fitted up again in exactly the same
way. When we say that a logarithmic decrement did not
exist, we mean that it was not constant, but varied with the
amount of the oscillation. or the tractive force to be pro-
portional to the velocity of the cylinder it is necessary for 4/p
and the periodic time to be so great that the velocities of the
fluid at all places shall be in the same proportion as if the
motion were steady. .
After this paper was written we asked Mr, J. B. Knight,
of the Chemical Department of the Finsbury 'lechnical College,
to make measurements of the specific gravity of sperm-oil at
different temperatures. His results give a very striking con-
firmation of the views expressed in the paper as to a discon-
tinuity of some kind due to rise of temperature. As all the
authorities whom we have consulted seemed to see no possible
reason for a discontinuity in the rate of change of « with
temperature in sperm-oil at about 40°C., it is possible that
these results may be of importance.
ae
458 Miss Earp on the Effect of the Replacement oj
Temperature Cent. | Specific Gravity.
25 | 831
30 | 8306
35 828
40) | 826
45 8758
50 8753
5d | “OT ET
We are now arranging a piece of apparatus which will give,
not the absolute value of the specific gravity, but with great
accuracy relative rates of the change of specific gravity with
temperature *. We shall make experiments of the same kind
upon other animal oils.
XLIV. Note on the Effect of the Replacement of Oxygen by
Sulphur on the Boiling- and Melting-points of Compounds.
By Miss A. G. Harpf.
N various papers published in the Philosophical Magazine t
Carnelley has called attention to the effect produced on
the boiling-point and melting-point of compounds by replacing
one element in the compound by another belonging to the
same group. He gives numerous examples (mostly organic
compounds) to show that in the case of the halogen com-
pounds, when one halogen is replaced by another of a higher
atomic weight, both the boiling- and melting-point are corre-
spondingly raised.
As a further instance of the same kind of thing he gives the
following series of the ethyl carbonates and sulpho-carbonates
to show that the boiling-point is raised in proportion to the
amount of sulphur introduced in the place of oxygen. He
also points out that the same series shows that a definite effect
is produced by a change in the arrangement of the molecule
without any change in the number of sulphur atoms.
‘ Doe 5) : a VO See
OG E, BP. Zon. Cen H. B.P. 196°.
co B.P. 156° cages
: } Gs fe)
+ 0—C i; SC,H.
Ge ae: s1° OX ee 24
\o--0,H, B:Psi6h; \sc,H, B.P. 240°.
* We described at the Meeting results obtained for other specimens of
sperm-oil, with the new apparatus, which exhibited no discontinuity.
Yet we can find no reason to doubt Mr. Knight’s measurements.
+ Communicated by M. M. Pattison Muir.
t Phil. Mag. Oct. 1879.
j
Oxygen by Sulphur on Boiling-points of Compounds. 459
He does not, however, mention the way in which this eftect
is reversed in the cases in which the oxygen of the hydrowyl
group is replaced by sulphur, and I therefore conclude that
it escaped his notice. By examining the large number of
boiling-point data given by him in his tables I have found
the following rule to be perfectly general :—
The replacement of oxygen by sulphur in a compound always
raises the boiling-point except in those cases in which the oxygen
of the hydroxyl group is replaced by sulphur, and then the re-
verse effect is very marked. |
In obtaining data in proof of this I have been confined
of course mainly to organic compounds, and of these I have
only given the simpler instances, and such of the more com-
plicated compounds as have a known structural formula.
The reason for this is obvious, since Kopp has shown that the
boiling-point of isomeric hydrocarbons is not the same, show-
ing that a mere rearrangement of the atoms in a molecule is
sufficient to affect the boiling-point without any change in
number or kind. The fact is further exemplified in the series
of ethyl-carbonates given above.
In the following list of compounds containing hydroxyl
and their sulphur analogues, it will be seen that the replace-
ment of the OH by the SH group always lowers the boiling-
point, and that in the case of bodies of low molecular weight
the difference is considerable, but decreases as we ascend a
homologous series*.
Diff.
RP oid etocrssussacce- SOIKSE\ Ee Once merase. 100 | 161°8
TEL SU ee oe ORIEL CHOBE. oicdinc ick kha 67 46
Ls SBP | Os OSL, Gees nr oye. 784 | 42
CEL) ere LAG SE (CHLOE WR occ os 197 51
BEUOHOH SH .....0.0.:.. 90 | CH,CHCH,OH............... 96 6
SEMOE-CH SH «.......5.. (igen COHEOE CH ORs. 09o)4.0. 97 30
MEELVOCHSH 1 ......006..0 Sinn OH OOH Gres .sr, 83 26
fo )SOHCH,SH:.........:. Sse (CH) CHO OH 1. 108 20
CH,OH,CHSHCH, ......... 84 | CH,CH,CHOHOH.......... 99 15
OH(CH,).CH,CH,SH ...... 120\ | OH(OH,),CH,CH,OH ... 131:5 | 11:5
WCVCHOHSH ............-.. 137 CCl CHOMOH,.... 1). 149 26
JOS oa NY GCC IECXO)E [Nat Oly eee 180 8
BEI (SEL) 0.0.55 250 lcasesecens DAS ee ON (OED). © hss. vccedons 270 27
OH (CH.),CH,SH. ......... 1450 | OH,(CH,),CH.OM ...... 157 12
ROME OELSH .......ccccasccdes sh Wy /Ol BU XODELCOUSIAN SAA eae lle! 205 11
OPH CH.SH (a) .....50000.- een | Os Ole OF (a) vente 188 0
i, (G) 3. are 188 * (Gis ce emenet 201 13
(yy) a eae 188 rea (Cy) eek. 198 10
CO) 5 ah Coie OH COON aCe tet 17 24
OLE OSH (a)......000cccce BtGw "C,H OHO (e) i i.08. 6. 245; 29)
+ Exception :—C,,H,SH(a) 285 C,,H,(OH)(a)
* The only exception to the rule is that marked +, and isin the case of
a body of high molecular weight and complicated constitution.
460 Miss Earp on the fect of the Replacement of
Again, in the following list of compounds containing
oxygen not in the condition of hydroxyl, it will be seen that
the normal rule is followed. :
Diff,
5 | °
GHIGHS oN eee 205 | CH,CHO Si | 184
(GEORe oo ern: 300:.| (CH,).0.... 138 | 187
(OH So tes 41 | (CH,),0... aoean. 64
(OH OSH Phe... 200 | (CH.),CO, 1... 91 109
(HAC ys ee. 64 | (C,H(CH)O a li | 58
Ce a ee 99 |(C/H.).0 -.... oa 35 | 87
OH(CH OHOHS =... 114 | origi, ) CH, OHO .... ee ae
COR Vu Rel ee Oi 249 | (C,H,),CO, nna 125 | 1b
MESOHGHE We. 1 | mG One a B8 | 96
(GHIOHCH is ap 140 | (CH,CHCH,,0 20m 82 | 58
(GHICHCH an eh... 188 | (CH.CHCH.),0, «1.0... 171 17
(Po SO ae 180 | (Pr),0(«) ....2 s2 | 48
. es i 01 | @... e 60 | 60
CoS Cenc kel he 310 | (RtOCH,)>..... am 193 | 87
CinecGstias aah ia. 204. | 0,H.00,H. a 172 | 32
(GHLOECH.GH,).S .......... 182 | (GH.CH.CH,CH,),0 .. 140 | 42
CREHOIECING oe eee 215 | CAC CHORt am 185 | 30
GEER a 950 | (C.H,.),0 (Iso) eae 175 | 7
(Gao de alee oo: 339 | (CLH 0"... ee 978-288 | 5444
GS. ee. 392.| (CH ).O ae 246 | 46
GHICOSCH, «7 .. 95 | CELCOOCH, aa 56 | 39
beCens: soot ce ee 169 | "CO(OCH,), ©). eam 90 | 79
@HCOSOH Lg es 115 | CH,COOU-H, 4. Gem 77 | 88
PE OOSCH (a) 8 uk 35 | CH{COOCH (a) «+. 102 BB
es 124 ged eee
Carcoods Aus i ir 984 | C,H C0000 ae 276 8
CELLOSC ie ee 249, | G,H,COQU, Hy aaa 212 | 30
CIOCUN Gee 132 | CHLOCN .\. Jem 90 | 49
CHeNCS ee 119 | CH-NCO ... 44 | 75
OH CHGH NOS... 150 | CH.CHCH,NCO ......... 82 | 68
GRAISONI(G) sees 151: | C,H,OCN (B) ... aa 67 | 84
Gi(OH;),CH,NCS...... 162 Ci(CHT,),CH.NCO a 110 | 52
GuOOseO, et 984 | C,H.COOCO,.... ama 276 Wilks
fie sae cies weer oY |
(SONGS eee ee 218 |.C,HNCO ....aaee Coe Be
GaTOHENON eet) 943 | O-H-CH,NOO ce 175-200
ie SObines Meee ee 156-160, CCIO0CL, -..... (about) 100 |
To the above may be added the series of ethyl carbonates
quoted at first, and also the following inorganic compounds:—
OSs Wate css 42°6 GOs.) tieeeeee —782
CSC] ie yee-kes-- 71 COC vs: secre 82
1S) C) eee renee 125 POC, .tocceee 197
By arranging the data rather differently it is easy to see
that the abnormality hes entirely with the hydroxy! group.
Thus, if we take any group of sulphur compounds of one type,
we shall find the boiling-point increases with the molecular
weight as well when the hydrogen of the SH group is
replaced by a hydrocarbon radical as in any other case.
Oxygen by Sulphur on Boiling-points of Compounds. 461
Such, for example, are the following :—
le}
ae ~61°8 H,S......—61'8 Histo 2 e =618
CH,SH ...... 21 Gh USiengs 36 C,H.SH ... 172
me (CH.).S-...... Aiea,” (C.),S... A, O,H.SC,H, 204
VH,.CH,S 64 Pr,S («) .. "130 Poe (CAHBcies o>
Taking in the same way the corresponding oxygen com-
pounds, we find that by replacing OH by OX, where X
stands for any hydrocarbon radical, unless very complex, we
lower the boiling-point of the compound considerably, whereas
when the exchange is simply between different hydrocarbon
radicals the change is in the normal direction.
elec... 100 Te Obs sec. 100 HOVSGRae 100
CH,OH ...... 67 C,H,OH...... 78:4 (C,H,OH_... 180
Beco .. —23 | B, (C,H,),0.... 35 B, O,H,00,H,... 172
eneH.O... 11 (Pr,)O («) .. (C,H,),0...... 246*
From these data it is evident that the fact that water,
which has a lower molecular weight than even any of the
“permanent” gases (except hydrogen) will remain liquid up
to a very high temperature, is only one particular and well-
marked case of the general effect of the hydroxyl group.
It has been objected by Ostwald and others that the com-
parison of boiling-points is unsatisfactory, inasmuch as in
some cases it is possible that the vapour-pressure curves of
different substances may cross one another at some point; and
in that case, if some other than atmospheric pressure were
taken as the standard, the relative position of the boiling-
points would be reversed.
It is difficult to plot the vapour-pressure curves for H,O
and H,S on the same scale, since the pressure of H,S varies
by many atmospheres ; while that of H,O varies through the
same range only by a few inches, so that it has to be repre-
sented on the H.S scale by a line following the zero. The
H.S curve is, however, perfectly normal, and shows no ten-
dency whatever to approach the zero at any point short of
infinity. Hence the objection about the crossing of the
eurves falls to the ground in this case. The same may be
shown by comparing the curves for CO, and CS,; only in
this case, of course, the sulphur compound follows the zero
line, while the other is highly inclined.
With regard to the melting-points of oxygen and sulphur
compounds the same general rule holds ; but exceptions are
not rare, particularly in the cases of more complicated com-
pounds, and naturally it is among these that the larger number
* In this case the destruction of OH is not sufficient to balance the
effect of introducing the second carbon ring.
Phil. Mag. &. 5. Vol. 35. No. 216. May 1893. 21
402-- Notices respecting New Books.
of melting-point data are given. In all probability the ten-
dency to form molecular groupings and other unknown factors
tend to obscure the effect on melting-points due to the change
of constitution alone.
Another point which I think may be noticed with advan-
tage from the series just given on page 461, and which, as far
as | am aware, has been hitherto neglected, is the effect on
the boiling-point of the symmetry of the molecule, unsym-
metrical molecules tending to boil higher than symmetrical
ones.
Consider the series A,, page 461. Between the first and
second members of the series there is a large difference, the
molecular weight beg increased and the symmetry of the
molecule destroyed at the same time. Between 2 and 3 of
the same series, on the other hand, there is a much smaller
difference ; the molecular weight is increased but symmetry
is restored, and the two things act against one another.
Again, consider the series B,. Between 1 and 2 in this
series the destruction of hydroxyl lowers the boiling-point,
the destruction of molecular symmetry tends to raise it, the
result being that the difference only of the two effects is small.
Between 2 and 3 the destruction of hydroxyl and the resto-
ration of symmetry act together, and the resultant effect is
large.
The same effects may be noticed by comparing A, and By
in the same way, and also by comparing the first, second, and
fourth members in the series A; and B; respectively.
XLV. Notices respecting New Books.
An Elementary Treatise on Modern Pure Geometry.
By R. Lacutan. (London: Macmillan. 1893. Pp. x+288.)
N R. LACHLAN is a recognized master of the Geometrical
craft, and the work before us well maintains his reputation.
His primary object is to meet the new Cambridge Tripos regula-
tions, in which provision is made for the introduction of a paper
on “ Pure Geometry.” All that could fairly be looked for in such
a paper is given by the writer, or is led up to by him. He has not,
however, contented himself with such a limited supply as this
would require, but he has written with a view to allure students
on to the arcana of the science. After a careful perusal we have
detected very few errata. On page 53, Ex. 4 is obviously a slip,
and in line 3 from bottom for Bw read By, for Cw read Cz.
Page 55 line 13 contains a small clerical error: the opening
Notices respecting New Books. 463
sentence of §116 is not sufficiently guarded to be accurate. In
Ex. 3, page 70, it is not stated what point S’is. On page 161
line 11, for “polar” read “ poles.” Two or three clerical errors
are easily corrected. The following historical one occurs on
page 78, Ex. 6: “ Mr. H. M. Taylor’s paper was read before the
London Mathematical Society on Feb. 14th, 1884,” whereas he
had previously published his Note, “ On a six-point circle con-
nected with a triangle,” in the ‘ Messenger of Mathematics,’ vol. xi.
(May 1881—April 1882). If we mistake not, the “circle” had
previously been given by him ina Trinity paper. In conclusion
we are glad to say that the text is not overburdened with corol-
laries and superfluous matter, the figures are excellent, and there
is a most judicious and varied selection of exercises.
Revue Semestrielle des Publications Mathématiques rédigée sous les
auspices de la Société Mathématique d Amsterdam. Tome L.,
1* partie. (Amsterdam. 1893. 104 pp.)
THE object which the Mathematical Society of Amsterdam has in
view in putting forth this Revue is * de faciliter l’étude des sciences
mathématiques en faisant connaitre, sans délai de quelque import-
ance, le titre et le contenu principal des mémoires mathématiques
publies dans les principaux journaux scientifiques.” Primarily it
is intended for the use of its own Members, but the Society has
rightly judged that such a publication, if well conducted, will be
of service to a much larger circle of readers. This opening number
contains titles of papers printed in about 120 journals, 19 of which
are British and 8 American. A careful list of the titles is drawn
up with various particulars of interest (pp. 87-104).
The title of each communication is preceded by a system of
notation adopted at the recent Congres International de Biblio-
eraphie des Sciences Mathematiques, and is followed by a very
concise Compte-rendu of the contents. We may say that the
Revue, though its objects are similar to those of the well-known
Fortschritte der Mathematik (Berlin), does not aim so high, for in
the generality of instances the insight into any paper given by the
notices here is little more than a student would inter from the bare
title. Its merit is that a much earlier record, if the editors keep
up to date, will be available for authors and readers. The papers
tabulated from this Journal are comprised in Vol. xxxiv. (Nos. 206—
209) and are seven in number. ‘Twoare given by the titles only :
of the others a fair abstract is given. Lord Rayleigh’s papers are
assigned to “J. W. S. Rayleigh.’ We wish the Society good
success and a large clienteéle.
-f 1464.)
XLVI. Proceedings of Learned Societies.
GEOLOGICAL SOCIETY.
[Continued from p. 313.]
January 25th, 1893.—W. H. Hudleston, Esq., M.A., F.R.S.,
President, in the Chair.
ae following communications were read :—
1. “On Inclusions of Tertiary Granite in the Gabbro of the
Cuilin Hills, Skye; and on the Products resulting from the Partial
Fusion of the Acid by the Basic Rock.” By Prof. J. W. Judd,
F.RS., V.P.G.S.
The author first calls attention to previous literature bearing on
the subject of the extreme metamorphism of fragments of one
igneous rock which have been caught up and enveloped in the
products of a latereruption. The observations of Fischer, Lehmann,
Phillips, Werveke, Sandberger, Lacroix, Hussak, Graeff, Bonney,
Sauer, and others show that, while the porphyritic crystals of such
altered rocks exhibit characteristic modifications, the fused ground-
mass may have developed in it striking spherulitic structures.
On the north-east side of Loch Coruiskh, in Skye, there may be
seen on a ridge known as Druim-an-Eidhne, which rises to a little
over 1000 feet above the sea, a very interesting junction of the
granitic rocks of the Red Mountains with the gabbros of the Cuilin
Hills. At this place, inclusions of the granitic rock, sometimes
having an area of several square yards, are found to be com-
pletely enveloped in the mass of the gabbro. ‘The basic rock here
exhibits all its ordinary characters, being a gabbro passing into a
norite, traversed by numerous segregation-veins ; the acid rock is an
augite-granite, exhibiting the micropegmatitic (‘ granophyrie ’) and
the drusy (‘ miarolitic’) structures, and it passes in places into an
ordinary quartz-felsite {‘ quartz-porphyry ’).
Within the inclusions, however, the acid rock is seen to have
undergone great alteration from partial fusion, and it has aequired
the compact texture and splintery fracture of a rhyolite; weathered
surfaces of this rock are found to exhibit the most remarkable
banded and spherulitic structures.
Microscopic study of the rock of these inclusions shows that the
phenocrysts of quartz and felspar remain intact, but exhibit all the
well-known effects of the action of a molten glassy magma upon
them. The pyroxene, however, has been more profoundly affected,
and has broken up into magnetite and other secondary minerals.
The micropegmatitic groundmass, which was the last portion of
the rock to consolidate, has for the most part been completely
fused, and in some places has actually flowed. In the glassy
mass thus formed, the most beautiful spherulitic growths have
been developed, the individual spherulites varying in size from
a pin’s head to a small orange. These spherulites are often
Geological Society. 465
composite in character, consisting of minute examples of the
‘common type enclosed in larger arborescent growths (‘ porous-
spherulites’) of felspar microlites, with silica, originally in the
form of opal and tridymite, but now converted into quartz, lying
between them. All the interesting forms of spherulitic growth
which have been so well described by Mr. Iddings from the Obsi-
dian Cliff in the Yellowstone Park, and by Mr. Whitman Crossfrom
the Silver Cliff, Colorado, are most admirably illustrated in these
inclusions of the Cuilin Hills. It is interesting to note that the
nuclei of some of these large spherulites consist of fragments of the
micropegmatitic granite which have escaped fusion. Among the new
minerals developed in these inclusions, by the action on them of
the enveloping magma, are pyrites and fayalite (the iron-olivine).
The phenomena now described are of interest as setting at rest
all doubts as to the order of eruption of the several igneous masses
of the Western Isles of Scotland. That the gabbros are younger
than the granites was maintained by Macculloch in 1819, by J. D.
Forbes in 1846, by Zirkel in 1871, and by the author in 1874. In
1888, however, Sir A. Geikie asserted that these conclusions were
erroneous ; he insisted that the granites were erupted after the
gabbros and basalts, and that they are, indeed, later than all the
voleanic rocks of the district except a few basic dykes which are
seen to traverse them. The occurrence of the remarkable inclusions
of granite within the gabbro now removes all possibility of doubt on
the subject, and proves conclusively that the granite was not only
erupted but had consolidated in its present form before the outburst
through it of the gabbro.
2. “ Anthracite and Bituminous Coal-beds. An Attempt to
throw some light upon the manner in which Anthracite was formed ;
or Contributions towards the Controversy regarding the Formation
of Anthracite.” By W.S. Gresley, Esq., F.GS.
The author does not seek to advance any new theory in this
communication, nor to proclaim new facts of any importance, but to
put old facts in something of a new light, in order to aid the inves-
tigations of others. His main object is to establish two facts, viz.:—
that the associated strata of anthracite-beds are more arenaceous
than those containing so-called bituminous coal-beds, and that the
prevailing colours of the sandstones, grits, etc., of anthracite regions
are greyer and darker than those of regions of bituminous coal. To
these facts may perhaps be added a third, that the more anthracitic
the coal-beds, and the more siliceous the enclosing strata, the harder
and tougher these associated strata are.
While recognizing that the rocks of many anthracite regions have
undergone great disturbance, he cites other areas where coal-basins
have been much folded, without any corresponding production of
anthracite in considerable quantity.
The modes of occurrence of anthracite are illustrated by many
instances observed by the author in the Old and New Worlds.
ie pe I
466 Geological Society :—
February 8th.—W. H. Hudleston, Esq., M.A., F.R.S.,
President, in the Chair.
The following communications were read :—
1. “‘ Notes on some Coast-Sections at the Lizard.” By Howard
Fox, Esq., F.G.8., and J. J. H. Teall, Esq., M.A., F.B.S., F.G-S.
In the first part of the paper the authors describe a small portion
of the west coast near Ogo Dour, where hornblende-schist and
serpentine are exposed. As a result of the detailed mapping of the
sloping face of the cliff, coupled with a microscopic examination of
the rocks, they have arrived at the conclusion that the serpentine 1s
part and. parcel of the foliated series to which the hornblende-
schists belong, and that the apparent evidences of intrusion of
_ serpentine into schist in that district are consequences of the folding
and faulting to which the rocks have been subjected since the
banding was produced. The interlamination of serpentine and
schist is described, and also the effects of folding and faulting.
Basic dykes, cutting both serpentine and schists, are clearly repre-
sented in the portion of the coast which has been mapped, and these
locally pass into hornblende-schists, which can, however, be clearly
distinguished from the schists of the country. The origin of the
foliation in the dykes is discussed.
The second part of the paper deals with a small portion of the
coast east of the Lion Rock, Kynance. Here a small portion of the
‘oranulitic series’ is seen in juxtaposition with serpentine. The
phenomena appear to indicate that the granulitic complex was
intruded into the serpentine ; but they may possibly be due to the
fact that the two sets of rocks have been folded together while the
granulitic complex was in a plastic condition, or to the intrusion of
the serpentine into the complex while the latter was plastic.
2. “ On a Radiolarian Chert from Mullion Island.” By Howard
Fox, Esq., F.G.8., and J. J. H. Teall, Hsq., M.A., EUR SineG a:
The main mass of Mullion Island is composed of a fine-grained
‘oreenstone,’ which shows a peculiar globular or ellipsoidal structure,
due to the presence of numerous curvilinear joints. Flat surfaces
of this rock, such as are exposed in many places at the base of the
cliff, remind one somewhat of the appearance of a lava of the
‘ pahoehoe’ type.
The stratified rocks, which form only a very small portion of the
island, consist of cherts, shales, and limestone. They occur as thin
strips or sheets, and sometimes as detached lenticles within the
igneous mass. The chert occurs in bands varying from a quarter of
an inch to several inches in thickness, and is of radiolarian origin.
The radiolaria are often clearly recognizable on the weathered
surfaces of some of the beds, and the reticulated nature of the test
may be observed by simply placing a portion of the weathered
surface under the microscope.
The authors describe the relations between the sedimentary and
Remarks on certain Islands in the New Hebrides. 467
igneous rocks, and suggest that the peculiar phenomena may be due
either to the injection of igneous material between the layers of the
stratified series near the surface of the sea-bed while deposition was
going on, or possibly to the flow of a submarine lava.
The forms of the radiolaria observed in the deposit, and also their
mode of preservation, are described in an Appendix by Dr. G. J.
Hinde.
3. “* Note on a Radiolarian Rock from Fannay Bay, Port Darwin,
Australia.” By G. J. Hinde, Ph.D., V.P.G.8.
4, “ Notes on the Geology of the District west of Caermarthen.”
Compiled from the Notes of the late T. Roberts, Esq., M.A., F.G.S.
To the east of the district around Haverfordwest, formerly de-
scribed by the author and another, an anticlinal is found extending
towards Caermarthen. The lowest beds discovered in this anticline
are the Tetragraptus-beds of Arenig age, which have not hitherto
been detected south of the St. David’s area. They have yielded
eight forms of graptolite, which have been determined by Prof.
Lapworth. The higher beds correspond with those previously
noticed in the district to the west; they are, in ascending order:
(1) Beds with ‘ tuning-fork’ Didymograpti, (2) Llandeilo limestone,
(3) Dicranograptus-shales, (4) Robeston Wathen and Sholeshook
Limestones.
Details of the geographical distribution of these and of theic
lithological and paleeontological characters are given in the paper.
February 22nd.—W. H. Hudleston, Esq., M.A., F.R.S.,
President, in the Chair.
The following communications were read :—
1. “On the Microscopic Structure of the Wenlock Limestone,
with Remarks on the Formation generally.” By Edward Wethered,
F.G.S., F.R.MS.
2. “On the Affinities (1) of Anthr He a, (2) of Anthracomya.”
By Dr. Wheelton Hind, B.S., F.G.S.
3. ‘ Geological Remarks on certain Islands in the New Hebrides.”
By Lieut. G. C. Frederick, R.N.
As far as can be judged from the soundings obtained, the New
Hebrides are probably situated on a bank lying from 350 to 400
fathoms below the surface of the ocean and running in a N.N.W.
and §.8.E. direction, with a deep valley between it and New Cale-
donia. The only two soundings obtained between these two groups
are 2375 and 2730 fathoms, the former within a short distance of
the New Hebrides.
Of the islands, Tanna is voleanic—an active volcano, apparently
consisting entirely of fragmental material, being situate on its
eastern side. Kfaté has some volcanic rock, but is chiefly of coral
formation. It rises to a height of 2203 feet, and in some parts has’
a terraced appearance, the terraces denoting distinet periods of
468 Geological Society.
upheaval. Coral was found to the height of 1500 feet above sea-
level. To the north of Efaté are Nguna, Pele, and Mau, of volcanic |
origin, and no coral has been found on them above sea-level; whilst |
Moso, Protection, and Errataka, to the west of Efaté, are of coral |
formation and similar in character to the adjoining coast of Efaté. |
In the vicinity of the coral isles is very little coral-reef, especially
when the shores are steep. Delicate live corals were brought up
from depths of 28, 39, and 42 fathoms off Moso, 37 fathoms near
Mau, and 40 fathoms off Mataso. Mataso is a volcanic island with
a narrow fringing-reef. Makura (6 miles N. of Mataso) and Mai
are also volcanic, with narrow fringing-reefs partly surrounding the
former and entirely encircling the latter island. A short distance
west of Mai is Cook’s Reef, of atoll formation. The Shepherd Isles
are all of volcanic formation, apparently recent, and no coral was
found growing around their shores. Mallicolo Island is of volcanic
and coral formation. At one place in this island coral was found at
a height of about 500 feet above sea-level.
March 8th.—W. H. Hudleston, Esq., M.A., F.BS.,
President, in the Chair.
The following communications were read :—
1. “On the Occurrence of Boulders and Pebbles from the Glacial
Drift in Gravels south of the Thames.” by Horace W. Monckton,
Esq., F.L.S., F.G.S.
North of the Thames near London, the Glacial Drift consists largely
of gravel, which is characterized by an abundance of pebbles of red
quartzite and boulders of quartz and igneous rock. With the ex-
ception of very rare boulders of quartz, the hill and vailey-gravels of
the greater part of Kent, Surrey, and Berkshire are entirely free
from these materials. The author points out that the River Thames
is not, however, the actual southern boundary of the distribution of
these Glacial Drift pebbles and boulders, though the number of
localities where they are found in gravels south of that river is few.
The author describes or mentions several, of which the foilowing
are the most important :—Tilehurst, Reading, Sonning, Bisham at
351 feet above the sea, Maidenhead, Kingston, Wimbledon, and
Dartford Heath.
2. “‘Onthe Plateau-Gravel south of Reading.” By O. A. Shrub-
sole, Esq., F.G.S.
This paper contains observations on the gravel of the Easthamp-
stead-Yately plateau.
The constituent elements of the gravel are described, and the
author notes pebbles of non-local material near Czsar’s Camp,
Easthampstead, on the Finchampstead Ridges, and at Gallows
Tree Pit at the summit of the Chobham Ridges plateau. He
mentions instances of stones from the gravel of the plateau (described
in the paper) which may bear marks of human workmanship. He
furthermore argues that the inclusion of pebbles of non-local origin
Inéelligence and Miscellaneous Articles. 469
in the gravels may be due to submergence of the plateau up to a
height of at least 400 feet above present sea-level, and cites other
facts in support of this suggestion. He concludes that the precise
age of the gravel can only be more or less of a guess, until the mode
of its formation has been definitely ascertained.
3. “A Fossiliferous Pleistocene Deposit at Stone, on the Hamp-
shire Coast.” By Clement Reid, Esq., F.L.S., F.G.S.
This is practically a supplement to a paper, ‘On the Pleistocene
Deposits of the Sussex Coast,’ that appeared in the last volume of
the Quarterly Journal. An equivalent of the mud-deposit of Selsey
has now been discovered about 20 miles farther west, and from it
have been obtained elephant-remains, and some mollusca and plants
like those found at Selsey. Among the plants is a South European
maple.
XLVII. Intelligence and Miscellaneous Articles.
ON VILLARI’S CRITICAL POINT IN NICKEL.
BY PROF. HEYDWEILLER.
eS magnetism of iron, nickel, and cobalt changes under the
influence of stretching forces. Villari first observed a special
behaviour of iron in reference to this attribute, namely that with
moderately strong magnetization small stretching forces increase
the magnetism, while larger forces diminish it; thus the strength
of the magnetism is graphically represented as a function of the
load, the ordinates of the curve firstincrease up to a maximum and
then diminish to far below the original values. The point of the
curve at which the ordinate again reaches the original value is
named Villari’s critical point.
In nickel this property has not been observed up to the present ;
in this case, so far as hitherto known, the magnetism steadily
decreases with increasing load. But with strongly magnetized
soft iron also, with small load, the original increase of the mag-
netism vanishes, and it was thought probable that with sufficiently
weak magnetization nickel also possesses a Villari’s critical point.
Experiments have confirmed this expectation. In observing the
changes in the very feeble magnetizations, it was found necessary
to work with a very sensitive arrangement.
A chemically pure nicke) wire, 46 cm. long and 0°15 em. thick,
was suspended vertically with its lower end very near (3°5 em.
distant) the upper magnetic needle of an astatic system, and so
that small longitudinal displacements caused no perceptible altera-
tion in the direction of the needle. An intensity of magnetization
I=1 C.G.S. unit corresponded to about 90 p throw with 110 p
scale distance.
The reduction of the observed numbers to absolute measure was
effected by comparison with an auxiliary magnetometer with single
needle.
Phil. Mag. 8. 5. Vol. 35. No. 216. May 1893. 2 K
470 Intelligence and Miscellaneous Articles.
The observations were conducted with alternate leading and
unloading, the strength of field remaining constant. The load
never exceeded 1 kilog. per sq. mm. cross section of the wire.
With small strength of magnetization under 2 ©.G.S. units and
with the smallest loads, soft annealed nickel shows a small decrease
of magnetism, with somewhat larger an increase, which may rise
to 26 per cent. of the total magnetism, and finally again a decrease
with increasing load.
Thus, for example, for the intensity of magnetization I=0-97
C.G.S. units with a load of p gr. per sq. millim. cross section, there
were obtained the following respective variations of magnetization
él
I
| let é1/I. D. “SUE
28 —0:006 347 +0:067
46 —0-011 490 +0042
63 0014 7138 +0257
102 —0:019 904 +0162
165 =0029 || 977 +0155
| 246 +0015 ||
|
With stronger magnetization the increase becomes continually
smaller; moreover after-effects of the preceding loading and phe-
nomena of hysteresis show themselves to a considerable degree.
Hard-drawn nickel presents the same phenomena with much
stronger magnetization still, even though in feebler degree.
Thus with a hard-drawn nickel wire, for 155-5 C.G.S. units
the variations of magnetization with a load of p gr. per sq. mm.
were :—
D. é1/I. p. 61/1.
9 —0:0034 84 +0187
18 —0:0052 113 +0:0180
27 —0-0054 246 +0-0122
33 —0-0062 360 +0-0080
42 +0°0081 490 —0:0304
56 +0:0186 740 — 00682
‘We may therefore assert that, with reference to the above=
discussed phenomena, the behaviour of nickel agrees well with that
of iron quantitatively but not qualitatively.
The detailed communication of the method of experimenting and
~ the results will be given in another place.—Svtzb. Wirz. Phys.-med.
Ges. March 11, 18938.
Intelligence and Miscellaneous Articles. 471
ON THE INTERFERENCE-BANDS OF GRATING-SPECTRA ON
GELATINE. BY M. CROVA.
Photographed gratings applied on bichromated gelatine by
M. Izarn’s* method may give rise to straight or curved inter-
ference-bands, sometimes very irregular, in the spectra which they
produce ; similar bands have been produced by Brewster f in other
circumstances. These phenomena are obtained with great beauty
on the spectra obtained by reflexion on gelatine-gratings on
silvered glass.
M. Izarn, in mentioning these interference-bands, expresses the
opinion that they are connated with the interference phenomena
by parallel gratings which I formerly investigated ¢.
Sunlight reflected from a heliostat 1s caught on a very narrow
slit the image cf which is projected upon a screen ; a very small
image of the sun is produced at the focus of this lens, which is
received on the striated surface of a grating photographed on
gelatine on silvered glass; the real images of the slit and of the
diffracted spectra are received on a screen placed in the conjugate
focus of the slit in respect of the lens.
The diffraction spectra are furrowed with large rectilinear black
bands parallel to the rays, and which are almost absolute minima,
the intensity of the rays reflected on the silvered surface being
very little less than that of the rays which fall on the gelatine.
With a copy of a fine Brunner’s grating, which I owe to the
kindness of M. Izarn, the spectra of the first order present a large ©
dark band in the green when the grating is very dry; if the
surface is breathed on the band is displaced towards the violet ;
other and closer ones enter at the red end, and their number rises
to three when the deposit of moisture confuses the projection.
The same phenomena are produced but in the opposite direction
during drying, and the displacement. of the bands becomes very
rapid if the evaporation is accelerated by blowing air over the
grating.
If the incident light extends over the whole height of the
erating instead of only to a small portion of the surface which is
obtained by varying the distance from the lens, the fringes are
curved, become irregular, and are sometimes serrated.
The phenomenon is due to the interference of two parallel
gratings; the one real, situated at the surface of the gelatine in
the points in which the incident wave meets its discontinuous
part; the other virtual, which is its image in the silvered mirror.
Their distance, which is virtually constant, is the optical path, 2 ne,
e being the thickness, and » the index of the gelatine. At the focus
of the lens, since the light only affects a small part of its surface,
the thickness of the gelatine is virtually constant.
* Comptes Rendus, vol. exvi. p. 506.
t+ Phil. Mag. [4] vol, Xxxi. pp. 22 and 98 (1866).
t Comptes Rendus, vol, Ixxu, p. 855, and vol. Ixxiv. (1871-1873).
472 Intelligence and Miscellaneous Articles.
lf, on the contrary, the light extends over a considerable sur-
tace, the thickness of the gelatine varies at different parts,
especially if the plate has been placed vertically while drying ; the
bands are then bent while diverging, and their greatest divergence
is at the part where the layer is thinnest.
When the grating has been prepared, the distortion of the bands
is very irregular ; but after a great number of hydratations followed
by dryings the phenomenon becomes more regular. After fixing
the grating in water and drying, the gelatine possesses, as is known,
i kind of temper which is manifested by its accidental double
refraction; but when it has been hydrated and dried slowly a
great number of times its structure becomes more homogeneous,
aud the bands no longer possess serrations. It is possible that
such alternations injure the good keeping of the gratings, and it
is thus desirable to keep them in a dry place.
Observing the band-spectra in the goniometer they appear like
broad and very dark spaces, but if sun-light is used condensed on
the slit, by a cylindrical lens, the pivot lines of the spectrum are
defined in these spaces with marvellous precision. ‘The production
of these parasitical bands does not affect the accuracy of measure-
ments made with these gratings.
With gratings in gelatine on transparent glass these phenomena
are scarcely perceptible by reflexion or by transmission, owing to
the almost total identity of the refractive indices of gelatine and
glass.
If the mdex of gelatine is taken at 1°52, it is easy to calculate
the thickness of the layer of gelatine as a function of the number
of bands contained in the spectrum reflected on silver; I have thus
found that in the copy which I use the thickness of the layer is
0-04 millim. when it is dry, and about 0°16 millim. when it is at its
maximum hydratation; this number is only approximate, as the
index varies with the quantity of water it contains.
M. Izarn’s gratings are of admirable sharpness, and examined
in the microscope they do not differ from the original ; in a Fro-
ment’s grating, a hundred one, which I possess, the opaque interval
is virtually equal to a fifth of the transparent interval: this is also
the case with M. Izarn’s copy; this is not a negative but a posi-
tive. The transparent intervals are the bands of insoluble gelatine,
while the opaque intervals are the places where the soluble gelatine
has been dissolved away by the water; but owing to the extreme
fineness of the intervals, the water by capillary action has hollowed
out cylindrical grooves which to a plane wave behave like an opaque
body. When the opaque interval is very great compared with the
transparent one, the opposite might take place; but it is easy to see
that even when the two intervals are transparent, the difference of
the refractive indices of gelatine and air is sufficient to produce
phenomena identical with those of the grating. This question calls
tor new investigations.—Comptes Rendus, March 27, 1893.
LH E
LONDON, EDINBURGH, ann DUBLIN
PHILOSOPHICAL MAGAZINE
AND
JOURNAL OF SCIENCE.
[FIFTH SERIES.]
JUNE 1898.
ALVIN. Electrochemical Effects due to Magnetization.
By GHoRGE OWEN Squier, PA.D., Lieut. U.S. Army *.
INTRODUCTION.
H# infiuence of magnetism on chemical action was the
subject of experiment by numerous investigators during
he first half of the present century t. Up to 1847 we find
by no means a uniformity of statement in regard to this
subject, and secondary effects were often interpreted as a true
chemical influence. Among the earlier writers who main-
tained that such an influence exists may be mentioned Ritter,
Schweigger, Débereiner, Fresnel, and Ampére; while those of
opposite view were Wartmann, Otto-Linné Hrdmann, Ber-
zelius, Robert Hunt, and the Chevalier Nobili.
Professor Remsen’s discovery, in 1881, of the remarkable
influence of magnetism on the deposition of copper from one
of its solutions on an iron plate, again attracted attention to
the subject, and since then considerable work has been done
directly or indirectly bearing on the question.
Among other experiments by Professor Remsen { were the
action in the magnetic field of copper on zinc, silver on zinc,
copper on tin, and silver on iron, in all of which cases the
magnet evidently exerted some influence. With copper sul-
phate on an iron plate the effects were best exhibited, the
* Communicated by the Author.
+ Wartmann, Philosophical Magazine, 1847, (8) xxx. p. 264.
t American Chemical Journal, vol. iii. p. 157, vol. vi. p. 480; ‘Science,’
vol. i. no. 2 (1883).
Phil. Mag. 8. 5. Vol. 35. No. 217. June 18938. 21
FFE en ee Re
474 Lieut. G. O. Squier on the Electrochemical
copper being deposited in lines approximating to the equipo-
tential lines of the magnet, and the outlines of the pole being
distinctly marked by the absence of deposit.
Messrs. Nichols and Franklin * were the next to conduct
experiments bearing on this subject. They found that finely
divided iron which has become “ passive ” through the action
of strong nitric acid suddenly regains its activity when intro-
duced in a magnetic field, and also that when one of the two
electrodes immersed in any liquid capable of chemically
acting upon them is placed in a magnetic field, a new
difference of potential is developed between them due to this
magnetization. ‘They ascribe these effects to electric currents
in the liquid produced indirectly by the magnet, which
currents go in the liquid from the magnetized to the neutral
electrode.
Professor Rowland and Dr. Louis Bell ft were the first to
note the “‘ protective action”’ of points and ends of magnetic
electrodes, and to give the exact mathematical theory of this
action. Their results were directly opposite to those of
Messrs. Nichols and Franklin, who found, as stated above,
that points and ends of bars in a magnetic field acted like
zines to the other portions, or were more easily dissolved by
the liquid.
The method of experiment adopted by Professor Rowland
was to expose portions of bars of the magnetic metals placed
in a magnetic field to reagents which would act upon them
chemically, and study the changes in the electro-chemical
nature of the exposed parts by fluctuations in a delicate
galvanometer connected with the two bars. Iron, nickel, and
cobalt were experimented upon, and nearly thirty reagents
were examined in this manner. The results are summed up
in the following statement :—“ When the magnetic metals
are exposed to chemical action in a magnetic field, such
action is decreased or arrested at any points where the rate of
variation of the square of the magnetic force tends towards a -
maximum.” |
Other investigations in this field are those of Andrews f,
who employed iron and steel bars from eight to ten inches
long with their ends immersed in various solutions, and one
bar magnetized by means of a solenoid. The protective
action was not noted, but, on the contrary, the magnetized
#* American Journal of Science, vol. xxxi. p. 272, vol. xxxiy. p. 419,
vol. xxxv. p. 290.
+ Phil. Mag. vol. xxvi. p. 105.
{ Proceedings of the Royal Society, no. 44, pp. 152-168, and no. 46,
pp. 176-198.
Liffects due to Magnetization. 475
bars acted as zincs to the neutral bars, thus indicating that
they were more easily attacked.
Practically the same results were obtained by Dr. Theodor
Gross * ; soft iron wires, 8 cm. long and 3 cm. in diameter,
coated with sealing-wax except at the ends were exposed to
various liquids. When one electrode was magnetized, a cur-
rent was obtained going in the liquid from the magnetized
electrode to the non-magnetized electrode.
It thus appears that there is at least an apparent incon-
sistency between the protective results of Professor Rowland
and Professor Remsen, and those of Nichols, Andrews, Gross,
and others, who find the more strongly magnetized parts of iron
electrodes more easily attacked than the neutral parts; and it
was with the object of endeavouring to reconcile these results,
and of studying the exact nature of the influence exerted by
the magnet, that the experiments recorded in this paper were
undertaken.
APPARATUS AND MEruop oF INVESTIGATION.
The method of investigation was that adopted by Professor
- Rowland in his previous work on the subject, since its facility
and delicacy permitted the effects of the magnet to be
observed whenever there was the slightest action on the
electrodes by the solution examined, and the investigation
- could thus be carried over a wide range of material.
A large electromagnet was employed to furnish the mag-
netic field, and, at a distance sufficient to prevent any direct
influence due to the magnet, a delicate galvanometer of the
Rowland type was set up. Small cells were made with iron
electrodes of special forms, coated with sealing-wax except at
certain parts, and immersed in a liquid capable of acting
chemically on iron. The whole was contained in a 50 cubic
centim. glass beaker, and when joined to the connecting wires
of the distant galvanometer was firmly clamped between the
poles of the electromagnet.
In the course of the examination of anumber of substances
it was found necessary to use two galvanometers—one
specially made by the University instrument-maker and very
sensitive, which was employed with acids which evolve hydro-
gen; the other, much less sensitive, was best suited to the
violent “ throws” with nitric acid and iron. The samples of
iron used throughout the experiments were obtained from
* “Ueber eine neue Entstehungsweise galvanischer Strome durch
Magnetismus,” Stizwngsberichte der Wiener Akademie, 1885, vol. xcii.
(1885) p. 1873.
2152
a ae versio tare ast
2 aad Bae a
476 Lieut. G. O. Squter on the Electrochemical
Carnegie, Phipps, and Co., of Pittsburg, and were practically
pure.
In order to insure a uniform density of surface, the elec-
trodes were turned from the same piece and polished equally
with fine emery-cloth. The magnet could be made or
reversed at the galvanometer, and its strength varied at will
by a non-inductive resistance. The electrochemical effects
due to the magnetic field could thus be studied with facility
by the fluctuations of the galvanometer-needle. The original
difference of potential, which always existed between the
electrodes, was compensated by a fraction of a Daniell cell,
so the effects of a variation of the magnetic field could be ob-
served when no original current was passing between the
electrodes.
The standard cells were made with care, and under
uniform treatment possessed at 20° C. an electromotive force
of 1:105 volt. The connexions with the compensating cir-
cuit, which contained a finely-divided bridge, were so
arranged that from its readings the difference of potential
between the distant electrodes became known at once without
involving the resistance of the cell or of the galvanometer.
Since quantitative measurements of the effects observed
were desired, a preliminary step was to calibrate the electro-
magnet for a given distance apart of the pole-pieces. The
method employed was the well-known one of comparing the
galvanometer deflexions produced by a test-coil in the 4eld
with those of an earth inductor in series in the circuit.
Since the effect of the sudden addition of a certain strength
of field was wanted instead of its absolute value, the de-
flexions with the test-coil were taken for simple “make”
or “ break ’”’ and not for reversed field, thus eliminating the
residual magnetism of the pole-pieces.
In the formula applicable, viz.,
H amnwv d
EY mga a! ee
in which d and d’ represent the deflexions due to the
inductor and test-coil respectively, H and H’ the earth’s
field and the field to be measured, n and n’ the number of
turns, and a and a’ the radii of the coils, the particular values
were :—
mna’ =20716 square centim.
ma” =6'788 square centim.
Distance between pole-pieces 3°5 centim.
Effects due to Magnetization. 477
H’=1299:48 d'H, and as d’ varied from 3), to 16, the range
of field employed was from 65 to 20,800 H.
A curve was constructed so that from accurate ammeter
readings in the field circuit the strength in absolute measure
could be read off at once.
EXPERIMENTAL RESULTS.
Preliminary.—The first experiments were made with very
dilute nitric acid and iron electrodes—one a circular disk of
5 millim. radius, and the other a small wire 1 centim. long
and 1 millim. in diameter, turned te a sharp point at one end.
The peint was placed opposite the centre of the disk, at a dis-
tance of 1 centim. from it, and the whole placed so that the
cylindrical electrode coincided with the direction of the lines
of force. When the minute point and the centre of the disk
were exposed to the liquid, and the magnet excited, a momen-
tary “throw” of the galvanometer was observed in the
direction indicating the point as being protected or acting as
the copper of the cell.
When the pointed pole was slightly flattened at the end,
and the insulation so cut away that the surfaces of exposure
on the two electrodes were exactiy the same, the throw of the
galvanometer on making the field was very much diminished,
although still perceptible, since the disposition of lines of
force would still be very different over the two plane surfaces
of exposure.
With ball-and-point electrodes precisely similar pheno-
mena were observed as with a disk and point, except to a less
degree.
The gradual reversal of the current shortly after exciting
the field, the independence of the throw of the direction of
the current through the magnet, the disappearance of the
throw when the nature of the magnetic field at the exposed
parts became the same, and the effects of artificially stirring
the liquid, were observed exactly as described by Messrs.
Rowland and Bell.
In the course of a large number of preliminary experi-
ments with nitric acid, it was soon observed that under
certain conditions the effect of suddenly putting on the
magnetic field was to produce a less rapid deflexion of the
galvanometer in the opposite direction, or indicating the
point as acting asa zinc. Plainly this irregular behaviour,
due to the magnet, required a more systematic study than it
had yet received. It had been found that the reversal of the
current, which regularly followed the “ protective throw,”
was decreased or destroyed by anything which prevented free
478 Lieut. G. O. Squier on the Electrochemical
circulation in the liquid, and that an acidulated gelatine,
which was allowed to harden around the poles, was best
suited for this purpose. The great irregularity observed in
any one experiment made it necessary to eliminate everything
possible which might mask the true phenomenon, if any ac-
curate comparisons were to be drawn between the effects
observed in the different cases; accordingly a standard form
of experiment was adopted, which was carefully repeated
many times. The cell found best suited for this purpose was
composed as follows :—
Disk electrode, diameter.................. 14:4 millim.
thickness! .)..c. 4 ae Dib ito tig
Point electr ode, total length ............ L524, Se
RA _ diameter, oso weee 44,
ss length of point......... D2 sug
Distance of point from centre of disk... 10 5
The same electrodes were used aacianeen any set of experi-
ments, being carefully cleaned and polished each time.
With nitric acid the liquid was finally made up as
follows :—
Distilled water ............... 10 grammes.
Flardscelatine ace. 245.2 1 gramme.
C. P. nitric acid (sp. gravity 1°415) 0533 gramme.
‘The gelatine and water were allowed to stand until the
former had dissolved without the application of heat, when
the acid was added and the whole thoroughly mixed. Too
strongly acidulated gelatine would not harden at all.
In some cases, in order to protect the point from the
‘beginning, the electrodes, secured as usual at the ends of two
small glass tubes containing the connecting wires, were
tirmly clamped in the proper position between the poles of
the magnet, and the magnetic field put on before the cell was
completed, by pushing the beaker containing the solution up
in position round the electrodes.
With this cell a series of parallel experiments were con-
ducted to obtain the variation of the effects with time, the
amount of iron salts present, the fluidity of the solution, and
with constant and variable magnetic fields.
A. Behaviour of the Cell with Time, in the Earth’s Field.
The cell was placed entirely outside the magnetic field, and
galvanometer-readings taken at intervals of one minute for
three hours. The curve fig. 1 (I.) shows these results. Posi-
tive ordinates indicate a current from the point to the disk,
Hifects due to Magnetization. 479
and negative ordinates the reverse current. Other experi-
ments with fresh solutions, same electrodes, same exposed
area, and every condition as nearly as possible the same, gave
curves of practically the same character, and the one given is
selected to illustrate.
The curve indicates that the original current was to the
point electrode; this gradually decreased, owing to polarization,
until after a hour and five minutes it reversed slightly, but
again reversed thirty-five minutes later, and after a little
more than two hours the deflexion became perfectly constant,
remaining so indefinitely. .
The iron salts formed could not move with facility from the
exposed surfaces through the hardened gelatine, and were
easily outlined from their brown colour, as the whole appa-
ratus was placed in a strong light.
B. In a Uniform Magnetic Field.
The cell was next placed in the magnetic field, which was
kept practically uniform (about 15,650 H) for three hours,
and galvanometer-readings taken as before.
The electrodes were magnetized before being introduced
into the solution, so as to protect the point from the begin-
ning. In order to prevent the influence of the rise of
temperature due to the heating of the field coils of the
electromagnet, the whole cell was packed with cotton-wool
between the poles. As Gross and Andrews observed, the
temperature effect was small, the solution rising but 0°°7 C.
in half an hour.
The curve fig. 1 (I1.) shows the results of these observa-
tions. It is seen that the original current was, as before, to
the point electrode, and about the same in value. ‘This
reversed after forty-five minutes, and rapidly increased to
approximately twice its original value at the end of one hour
and twenty minutes, and, instead of again reversing, remained
indefinitely with the point electrode as a zinc. ‘The distri-
bution of the iron salts in this case was quite unlike the
former. Notwithstanding the gelatine, the powerful magne-
tization of the exposed point gradually drew the iron salts
from the disk as fast as they were formed, and concentrated
them symmetrically about the point, giving the solution in
this region an almost black appearance.
After waiting a sufficient time to be assured that further
presence of iron salts would not effect the permanency of the
existing electromotive force, the magnetic field was gradually
decreased without ever breaking circuit, by increasing the
480
5
i
| ba
Pe
H
i
: ee
i
4
H
bi
ee
i
i
H
uJ
i
| ee
000% 1 i () ; i ;
Lieut. G. O. Squier on the Electrochemical
PT ee ee eT
HEEEBSS0E (a> cSRREEe
ze eS pes te]
ENE
.
:
ig
i
Klee
Fill
Ateteceen (loatat
GARR Rei
ae sate SClNGEaaa
JSNeRBea ee gers es he eee ee
LPS fee Eee cle
Ae sf
| a8 SEE Ee E
ACERE CEE EEC
ee ee eee
Fake
AEE
CAEP CED EE I) ar
Pest tes TNE a Ear yin
eb HBR a
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= 3 5 i
Fig.3
Effects due to Magnetization: 481
liquid resistance in the field current. This change of resist-
ance was necessarily made more or less suddenly, and the
deflexion experienced at each increase of resistance a not
very sudden throw toward reversal, in every respect the
same as had been repeatedly observed in the preliminary
experiments, and very different from the characteristic “ pro-
tective throw,” which is always sudden and in one direction.
By simply varying the field current with care, as explained
above, the deflexion could be reversed again and again at
will, and could also be held at the zero of the scale, indicating
no current at all, as long as desired. When once the field
was entirely broken, the iron salts were released from the
control of the exposed pole, seriously disturbed by gravity,
and putting on the field again failed to reproduce the results
noted above.
The only elements of difference in the two cases are, (a)
the magnetized condition of the metal, (0) the distribution of
the iron salts formed by the reaction.
Although, as the curves indicate, the average electromotive
force with the magnetic field was much greater than in the
former case, yet this electromotive force is due to the difference
of action at the two exposed surfaces, and, as will be pointed
out later, the total amount of iron dissolved and passing into
solution in the two cases is probably not very different *.
Quantitative experiments are wanting on this point.
The influence of the magnetized condition of the metal and
its magnitude is exhibited in the phenomenon of the “ pro-
tective throw,” which is always observed with apparatus
sufficiently delicate unless itis masked by other secondary
phenomena.
Since the electrodes were embedded in hardened gelatine,
there could be no convection-currents in the liquid, and this
can be eliminated. Hvidently the great difference in the
behaviour of the cell in the two experiments described is
principally due, either directly or indirectly, to the distribu-
tion of the iron salts formed by the reaction in the two cases.
The principal t¢me effects of the magnet were :—
(a) To produce a higher potential at the point of greater
magnetization.
(b) To increase the rate of change of the potential between
the electrodes and the absolute value of this potential dif-
ference.
(c) It also appears from both curves that after a certain
distribution of iron salts is reached, further presence of the
same does not affect the permanency of the current established.
* Fossati, Bolletino dell’ Elettrictsta, 1890.
482 Lieut. G. O. Squier on the Electrochemical
Since the time effects of the magnet were so marked, it
was thought possible that a “ cumulative ” effect, due to the
earth’s field alone, might be detected after a sufficient time
had elapsed. The apparatus was made as delicate as possible,
and parallel experiments conducted, the electrodes first being
placed in the magnetic meridian, and afterwards perpen-
dicular thereto. No positive difference could be detected.
C. Convection-Currents in the Liquid.
As has already been stated, the reversal of the current
which regularly followed the “ protective throw ” was found
by Messrs. Rowland and Bell to wholly disappear when har-
dened acidulated gelatine was substituted for the dilute acid
solution, so that when the magnet was put on a permanent
deflexion of much less magnitude was obtained instead of a
transitory throw. ‘This indicated that currents in the liquid
cannot be neglected, and their study was next undertaken.
Since hardened gelatine completely prevented the reversal of
the current, and with no gelatine it regularly appeared after
a short time, a large number of experiments were made, in
which the amount of gelatine was varied continuously between
these limits. As expected, the effects also varied—the greater
the fluidity of the solution, the more quickly the reversal
occurred.
In the light of what was already known concerning the
presence of iron salts, some of the experiments were continued
over a considerable time, and in others iron salts were intro-
duced artificially, to increase the effects. It was soon found
that by starting with a fresh hardened gelatine, with which
the “ protective throw” was the only feature, and gradually
increasing the fluidity of the solution and the amount of iron
salts present, both effects were exhibited at the.making of the
field—first, the sudden throw of the needle always in the
direction to protect the point, and immediately thereafter the
comparatively slow “ concentration throw” in the opposite
direction. By making the conditions still more unfavourable
for the “ protective throw,” it gradually diminished until en-
tirely masked by the second effect, so that making the field
produced a deflexion in the direction indicating a current
from the point.
With the proper conditions, both of these effects could be
studied with the greatest ease: first, one made prominent,
then both equal, then the other made prominent at will. The
“protective throw’ could be traced until it became a mere
Liffects due to Magnetization. 483
stationary tremor of the needle at the instant of its starting
on the “concentration throw.” This latter, though called
a “throw,” can be made to vary from an extremely slow
continuous movement of the galvanometer deflexion, as in
experiment B already described, to a comparatively rapid
deflexion at the instant of making the magnet.
By using simply a dilute nitric-acid solution with no gela-
tine, and inserting a thick piece of glass between the
electrodes, the concentration effect was delayed enough to
allow the ‘protective throw” to first appear, with consider-
able iron salts in the solution; and on making the field both
effects were observed as described above.
It now appears that the reversal of the current, uniformly
observed in the experiments of Messrs. Rowland and Bell,
was but a form of the “‘concentration throw” mentioned
above, and that we can regard the substitution of the hardened
acidulated gelatine for the dilute acid as merely separating these
effects, so that the former can be studied by itself; in other
words, the reversal of the current would have occurred just
the same after a sufficient time had elapsed.
Turning to the experiments of Drs. Gross and Andrews,
they employed but one magnetized electrode, which was not
pointed. In this case the nature of the magnetic field at the
two exposed surfaces would be very much more nearly the
same than when a pointed electrode is employed. This
arrangement is not, therefore, suited to bring out the delicate
“‘»rotective throw,” and it is not surprising that the concen-
tration effect was the prominent feature observed.
We have now a complete reconciliation of the directly
opposite results referred to in the introduction. The “ pro-
tective throw ” is due to the actual attraction of the magnet
for the iron, and is always in the direction to protect the
more strongly magnetized parts; while the “concentration
throw ” is always in the opposite direction, and depends upon
the distribution of the iron salts present in the solution, and
the convection-currents in the liquid. The concentration of
the products of the reaction about the point would tend to
produce a ferrous reaction instead of a ferric, and experiment
shows that a higher electromotive force is obtained with cells
in which a ferrous reaction takes place than with those in
which a ferric reaction occurs; and this change in the
character of the reaction produced by the concentration prob-
ably accounts, at least in part, for the increased electro-
motive force at the point.
ee a ne ee
484 Lieut. G. O. Squier on the Electrochemical
D. The Iron Salts about the Point Electrode.
The effect of artificially stirring the liquid, and the direct
influence of the fluid condition of the solution on the de-
flexions observed, at once suggested movements of the liquid,
produced indirectly by the magnet. In order to locate these
currents and determine their potence, a small cell was made
of two rectangular pieces of glass held by stout rubber bands
to thick rubber sides. Perforations in the sides admitted the
electrodes, which were point and disk as before. The cell,
between the poles of the electromagnet, was in a strong light,
and the movements in the liquid were easily perceptible from
the displacements of suspended particles introduced for the
purpose. When very dilute nitric acid was placed in the cell
and the magnet excited, some interesting phenomena were
observed.
The liquid, at first colourless, almost immediately assumed
a pale brown colour about the point, but nothing appeared at
the disk electrode. The iron salts were drawn as soon as
formed towards the point electrode, since here the rate of
variation of the square of the magnetic force is a maximum.
As more iron was dissolved, a surface approximating to an
equipotential surface of the pointed pole, and enveloping the
coloured iron salts, was observed enclosing the point and at
some distance from it. The outline of the surface became
darker in a short time, and finally two or more dark contours,
separated by lighter portions and symmetrical with the outer
one, appeared between it and the point, indicating maxima
and minima of density. When the magnetic field was gra-
dually increased, this surface usually enlarged without breaking
up and holding the iron salts within it. On further strength-
ening the magnetic field to about 16,000 H, the ridges merged
into one thick black envelope around the point.
This phenomenon is best studied with but little iron salts
present, and by watching the point electrode with a micro-
scope while the strength of the magnetic field is increased
and decreased continuously. The sections (fig. 3) show the
general form of these contours with different strengths of
field.
Upon breaking the field everything dropped from the point
suddenly to the bottom of the cell, and on making the field
again it required a few seconds for the salts to reappear at the
oint.
‘ This, at least partially, accounted for the sudden effects
often noticed at breaking the field circuit, and the compara-
a
ne
Hffecis due to Magnetization. 485
tively smali ones at ‘‘make,” especially with certain salt-
solutions, such as copper sulphate.
The outer envelope which held the iron salts together, and
limited the immediate influence of the magnetized point, was
distinctly defined within the liquid, and easily observed by
the reflexion of the light from its convex surface.
The persistency with which the iron salts were held about
the point was shown by moving the cell with respect to the
electrodes, when the contour remained approximately intact,
passing bodily through the liquid without being broken up.
H. Electromagnetic Rotations.
The small dust particles present in the liquid were drawn
radially toward the point until they reached the surface
described, when they pierced it and began to revolve rapidly
about the point inside this surface, in the opposite direction to
the currents of Ampere. Reversing the poles of the magnet
produced surfaces of the same appearance but opposite rotations.
When the current from a Daniell ceil was sent through it.
seemed to have very little effect upon the rotations, showing
them to be controlled by the powerfully magnetized point.
The electromagnet was arranged with its field vertical, and
the point electrode along the lines of force as before. This
arrangement gave better control of the surfaces formed,
since gravity now acted symmetrically about the point.
When a single iron rod about 3 millim. in diameter, and
placed vertically in the cell, was substituted for the two elec-
trodes, two rotations were observed which were uniformly
dextro about the north-seeking pole of the rod, and levo
about the south-seeking pole. About the central neutral
portion no rotations were observed. When the rod was covered
with a thin coating of vaseline the rotations entirely disappeared
as expected. Wartmann™ observed similar rotations about
soft-iron cylinders adhering to the poles of a magnet, and he
ascribed them to electric currents in the liquid which proceed
from the periphery of the cell radially to the surface of the rod.
The explanation of these rotations follows at once from
what we know of the time-effects produced by the magnet.
A higher potential is always produced at points of greater
magnetization, causing electric currents in the liquid from
the more strongly magnetized to the weaker parts of the iron.
Applying this fact to the exposed conical point electrode,
we see that local electric currents exist from its vertex to the
other parts of the surface, returning by way of the metal. In
the case of the vertical rod, these currents pass from the poles
* Philosophical Magazine, xxx. p. 268 (1847).
‘
Fi
5
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4
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ih RRS AE
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486 Lieut. G. O. Squier on the Electrochemical
at its ends, through the liquid, to the neutral portions, returning
as before.
These currents*, under the influence of the poles themselves,
would cause electromagnetic rotations of the liquid, as we find
them. The mere mechanical influence of these rotations, as
in the case when the liquid is artificially stirred, is to increase
the chemical action upon the point, causing it to tend to act
more like a zinc, which experiment confirms.
F’. Acids which attack Iron with the Evolution of Hydrogen.
Professor Rowland had observed the ‘ protective throw ”’
with such acids to be extremely small, and difficult to detect
except by very sensitive apparatus. The sensitive galvano-
meter was set up and every precaution taken against inductive
effects. A telescope and scale were used in this part of the
work.
Several substances were first examined, among them being
hydrochloric acid, acetic acid, perchloric acid, chlorine water,
copper sulphate, ferric chloride, sulphuric acid, &e., but as
these observations added nothing to the results already
obtained they are not given here.
After several trials a standard sulphuric-acid solution was
made up as follows :—
Distilled water faces ee eee eee 10 grammes.
Grelatame: ghee WA an ee 1 gramme.
O.P. Sulphuric acid, sp. gr. 1°826 ... 1:062 gramme.
More strongly acidulated gelatine would not harden, and
weaker solutions gave too small effects.
The “ protective throw ” was detected, but the point very
soon became completely covered with minute bubbles of
hydrogen, so that the electrodes had to be cleaned constantly.
The effect of adding hydrogen dioxide to the solution was
next tried, since this would facilitate the removal of the
hydrogen as soon as formed, which was thought to act
merely mechanically.
When about 1 cubic centim. of H,O, was added to the
solution the ‘ protective throw” became much more promi-
nent, and the gas bubbles only appeared in small quantities
aftera considerable time. Further addition of small quantities
* The rotations produced in liquids by axial currents, e. g. currents
coinciding with the direction of the magnetic lines of force as distinct
from radial currents, have been studied by Dr. Gore (Proceedings of the
Royal Society, xxxiil. p. 151).
J. M. Weeren, Berichte der Deutschen Chemischen Gesellschaft,
No. 11 (1891).
Effects due to Magnetization. 487
of the dioxide showed the “ protective throw” to be very
decided with sulphuric acid when the hydrogen 1s removed
from the surface of the electrodes in this manner.
G. The Electromotive Force.
Several attempts were made to obtain the relation between
the strength of field and the electromotive force developed in
the “protective throw”; but it was difficult to obtain con-
sistent readings owing to the trouble of balancing the original
deflexion, and the small absolute values of this electromotive
force when hardened gelatine was employed.
A curve was constructed, however, showing the variation
of the galvanometer deflexion with the strength of field, using
nitric-acid solution without gelatine. This is shown in fig. 2.
The readings were taken one after another as rapidly as
possible, to eliminate the damping effects of the iron salts
formed.
The curve exhibits the general character of the variation.
In the regicn from about 3500 H to 8000 H the greatest rate
of change occurred, and beyond 10,000 H the curve became
nearly horizontal for the particular electrodes used. Curves
were also constructed for the “concentration throw” on
making the field under different conditions, and they were
approximately right lines, more or less inclined according to
the amount of iron salts present.
With the sulphuric-acid solution already given the electro-
motive force varied from 0:°0033 to 0:0078 of a volt, while
with the nitric-acid solution it became as great as 0°036 of a
volt. In making all the solutions used with the different
substances amounts were taken proportional to their particular
molecular weights, and then halved or doubled until of suit-
able strength to give results with the galvanometer. It was
thought possible at the beginning that this might lead to
some relations between the protective results and the strengths
of the particular solutions ; but the general irregular cha-
racter of the whole phenomenon prevented comparisons in
this respect, and all that can be stated is, that both the
“protective throw” and the concentration effect in general
increased rapidly with the strength of the solution.
H. Influence of a Periodic Magnetic Field upon the Cell.
An experiment was made to determine the behaviour of the
standard nitric-acid cell when the magnetic field was made
and broken at regular intervals over a considerable time, and
curves were drawn showing the variation of the “ throw ” with
488 Lieut. G. O. Squier on the Electrochemical
time, and the fluctuation of the original deflexion caused by
this treatment. The strength of field was about 11,000 H.,
and the experiment was conducted without compensating the
original deflexion, and by making the field for one minute,
then breaking for one minute, and so on.
One of the curves is shown in fig. 1 (III.), in which posi-
tive ordinates are values of the concentration throw at “ make,”
and negative ordinates the values of the “ protective throw.”’
Experimenting was not begun until the gelatine had com-
pletely hardened, and since the electrodes would tend to
become polarized while the gelatine was hardening, the “ pro-
tective throw” was very small, and soon masked by the
concentration effects.
After about five minutes, making the field had very little
effect at all, but began to show decided “ concentration
throws ”’ ten minutes later, and these rapidly increased with
time, as the curve indicates.
Considering the fluctuation of the original deflexion, the
effect of this periodic field was to tend to reverse it, just as in
the case of the uniform field in experiment B, but much more
slowly, since the field was on but half the time in this case.
The cell also showed the iron salts almost entirely about the
point, forming a thick black envelope.
i Summary.
The principal results of this investigation may be sum-
marized as follows :—
Whenever iron is exposed to chemical action in a magnetic
field, there are two directly opposite influences exerted.
(a) The direct influence of the magnetized condition of the
metal, causing the more strongly magnetized parts to be
protected from chemical action.
This is exhibited in the phenomenon of the “ protective
throw,’ which is always in the direction to protect the more
strongly magnetized parts of magnetic electrodes.
The “ protective throw ” is small, often requiring delicate
apparatus to detect it, and is soon masked by the secondary
concentration effects.
As to the absence of the “protective throw” with acids
which attack iron with the evolution of hydrogen, the
hydrogen acts merely mechanically, and when removed by
adding to the solution small quantities of hydrogen dioxide,
the ‘“ protective throw ”’ becomes very decided.
In the curve, fig. 2, representing the variations of the
“protective throw’ with the strength of the magnetic field,
Effects due to Magnetization. 489
we trace at once the magnetization of the point-electrode.
Since only the minute point was exposed to the liquid, it
would become saturated for comparatively small magnetizing
forces, and the curve indicates that this occurred at about
10,000 H., beyond which the curve becomes practically hori-
zontal. ‘This further establishes the direct connexion between
this “ throw” and the variation of the magnetization of the
exposed point, and confirms the explanation of Professor
Rowland, that it is due to the actual attraction of the magnet
for the iron, and not to any molecular change produced by
magnetization. :
(6) The indirect influence of the magnet caused by the
concentration of the products of the reaction about the more
strongly magnetized parts of the iron.
This tends to produce a higher potential at the more
strongly magnetized parts, and finally establishes permanent
electric currents, which go in the liquid from the more
strongly magnetized to the neutral parts of the iron.
This concentration-effect increases rapidly with the amount
of iron salts present and the fluidity of the solution.
The convection-currents in the liquid are themselves a
consequence of this same concentration, being electromagnetic
rotations produced by the action of the magnet upon the local
electric currents between different parts of the iron.
As to the permanent current due to the magnet which is
finally set up between the electrodes, as shown in fig. 1 (II.), it
is probably owing to a change in the character of the reaction
produced by the concentration of the iron salts about the more
strongly magnetized parts, which would tend to cause a
ferrous instead of a ferric reaction to take place, and thus
increase the electromotive force.
Physical Laboratory, Johns Hopkins University,
May 1892.
Note.—Since the completion of the above investigation, a
number of experiments have been performed similar to those
of Professor Remsen. Starting with the known existence
and direction of the electric currents in the liquid, it was
thought that these might lead to some explanation of the
peculiar form of deposit in equipotential lines. A number of
interesting facts have been noted, but they are withheld for
further experiments. Go OS:
Phil. Mag. 8. 5. Vol. 35. No. 217. June 1893. 2M
f 490 ]
XLIX. Onthe Applicability of Lagrange’s Equations of Motion
ina General Class of Problems; with especial reference to
the Motion of a Perforated Solid in a Liquid. By CHARLES
V. Burton, D.Se.*
i | ee wr, p,... be some only of the coordinates of a
material system, so that when the values of W, ¢,...
are given the whole configuration is not completely determi-
nate. But suppose it known that the kinetic energy T can
be expressed as a homogeneous quadratic function of ab, d, sig’
only ; so that we may write
OT = (rb) W242 (bb p+... 3
(br), (d),... are functions of W, d,... only Nag:
We also suppose it known that (1) continues to hold good so
long as the only (generalezed) forces and impulses acting are of
types corresponding to
UW, dese. 5).
2. Suppose, now, that such impulses of these types were to
act on the system that yr, ¢,.. were all reduced to zero; the
expression for the kinetic energy would accordingly vanish,
and the system would be at rest. By supposing the last
operation to be reversed, we see that the motion at any instant
could be produced from rest by impulses of the types corre-
sponding to
aby by.» only... Ee can
3. Let 2, y, z be the Cartesian coordinates at time 7 of a
mass-element m referred to fixed axes, and let T be the kinetic
energy of the system at the same instant. Further, let A be
the “action” when the system moves without additional con-
straint from one configuration to another, and A+6A the
action when by workless constraints the path is slightly
modified, so that in place of the coordinates z, y, z we have
w+6e2, ytoy,z+6z. Then ft
SA ={Im(aéba + Ysy + 26z) | —[ Xm(ada + yoy + 262) |
: + aterm which necessarily vanishes; . . (4)
where [ | and {} denote the values of the quantities enclosed
at the beginning and end of the motion considered.
Suppose further that, both at the beginning and at the end,
the values of Wy, $,... are the same for the one motion as for
* Communicated by the Physical Society: read March 10, 1893.
+ Thomson and Tait’s ‘ Natural Philosophy,’ 2nd edit. Part I. § 327.
On Lagrange’s Equations of Motion. 491
the other, so that initially and finally dw, 5¢,... are all zero.
Jt does not follow that all the dx, dy, 5z’s are zero ; but
Lm( toa + ydy + 282)
is the so-called “ virtual moment” of the actual momenta in
the hypothetical displacement 62, dy, dz; that is, the virtual
moment, in the same displacement, of the impulse necessary
to produce the actual motion from rest. In virtue of °),
therefore, and of the initial and final vanishing of dy, d¢,..
he see that the bracketed terms of (4) must both be zero ;
ence
The inerement 5A vanishes and A has a stationary value for
all worklessly effected variations of path which leave the
initial and final values of Ww, ¢,.... unaltered. . (3)
4. Lagrange’s equations for the coordinates yp, $,... may
now be written down at once, since the investigation of
Thomson and Tait* becomes applicable to the present case
without modification. It will be noticed that in their equa-
tions (10) and (10)%, § 327, the sign of OV/d¥ should be
reversed.
We have thus a perfectly general proof of the proposition :
If the kinetic energy of a material system can be expressed as a
homogeneous quadratic function of certain generalized velocities
wr, b,... only, the coefficients being functions of Wr, b, ... only,
and if ifs remains always true so long as the only forces and
impulses acting are of types corresponding to Ww, h,..., the
equations of motion for the coordinates Yr, d,... may be written
down from this expression for the energy, in accordance with
the Lagrangian rule. Provided only that the stated conditions
are satisfied, we need not consider whether the whole confiqura-
tzon zs determined by the values of vf, 25 On what is the
nature of the cqgnored coordinates. . . HAE | Suaaa tee ty (HAN)
5. Passing over the known spottenicd of this result to the
motion of solids through an irrotationally and acyclically
moving liquid, we come to the more general case of a perfo-
rated solid, with liquid irrotationally circulating through the
apertures. Take as coordinates any six 6, 6’,... which deter-
mine the position of the solid, together with y, y’,... equal
in number (m) to the apertures; each y being the volume
of liquid which, starting from a given configuration, has flowed
across some one of the m geometrical surfaces, required to
close the apertures, these surfaces being supposed to move
along with the solid.
Of course the coordinates 0, 6’,... v. x’,... are insufficient
* Loe. cit.
2M 2
492 Dr. C. V. Burton on the Motion of a
to determine the entire configuration of the system (including
the positions of all the particles of liquid); but we shall see
immediately how, in virtue of the proposition (A), Lagrange’s
equations may be written down.
6. Since an increment dy in one of the coordinates y is the
volume of liquid which flows across a barrier-surface (1. é.,
which flows through an aperture relatively to the solid), the
generalized force corresponding to y must be conceived of as
a uniform pressure exerted over the said geometrical surface,
by means of some immaterial mechanism attached to the solid;
while the impulse corresponding to y is of course a uniform
impulsive pressure applied in the same manner. [rom hydro-
dynamical considerations we know that the measure of such an
impulsive pressure is pdx, where p is the density of the fluid,
and 6« the change produced in the circulation through the
corresponding aperture.
Hence the impulses corresponding to y, y’,... are
Kp, p, . «2 2 aio
where x, «’,... are the circulations through the various
apertures.
7. Now when the motion of the liquid is irrotational, we
have
T =a homogeneous quadratic function of 0, 0’,...«,«’...
only ; coefficients functions of 4, 6’... only;
X,X ++. = homogeneous linear functions of 6, 6’,...
x, «',... only ; coefficients functions of 6, 6’,... only.
Since the y’s are equal in number to the «’s, let us suppose
the last-written system of linear equations to be solved for
the «’s in terms of the ¥’s ; we then have
x, ’,...= homogeneous linear functions of 6, 6’,... XX’; only.
coefficients functions of 0, 0’,... only.
Substituting in the expression for T we get
T = a homogeneous quadratic function of 6, Oa ¥, x, .. only;
coefficients functions of 0, 0’,... only.
This, then, remains true so long as the motion of the liquid is
irrotational; in other words, so long as the only forces and
impulses acting are of types corresponding to 6, 6’,... (since
these are applied to the solid), y,7’,... (since these are
uniform over the barriers, by § 6).
If we identify Wy, $,... with the coordinates 0,0’,...4,%',--.
of the present example, we see that the proposition (A) of § 4
is immediately applicable to this case. We may therefore
oe.
Perforated Solid in a Liquid. 493
ignore all other coordinates, and from the kinetic energy
expressed as a function of 0, 0’,...y, x’,... write down the
Lagrangian equations for 0,6’,... and, if we wish, for y, x’,...
also. These latter, however, are less directly intelligible,
since in general they involve finite pressures continuously
acting over geometrical surfaces drawn through the liquid.
8. If we wish to picture the application of the principle of
least action (§ 3) to the present case, we may proceed as
follows: —Let the system start from the configuration (1.)
and move without additional constraint or influence to the
configuration (II.). Then let it start again from the confi-
guration (1.) with the same velocities as before, and durin
the motion let infinitesimal additional forces act on the solid,
_while infinitesimal pressures, uniform over each barrier-
surface, are impressed on the liquid ; the total rate at which
the additional influences do work being at each instant zero.
Further, let the additional influences be so adjusted that the
system, after following a slightly different path, passes through
a configuration such that 0, 6’,... x, x’,... are all the same
as for (II.). Then, to pass from the configuration (II.) to the
present configuration requires no displacement of the solid,
and only such displacement of the liquid that the total volume
which crosses any barrier-surface is zero. In such a change
of configuration impulses of the types 0, 6',... y, x’,... would
have no “virtual moment,” just as forces applied to the solid
and uniform pressures applied to the barrier-surfaces would
give rise to no virtual work. aia
9. At this stage it will be convenient to replace 6, 6',...
by the components u,v, w of linear velocity and p, g, r of
angular velocity, which determine the instantaneous motion
of the solid along and about axes fixed in itself. The Lagran-
gian equations for the six coordinates 0, 6’,... must accord-
ingly be replaced by the forms suitable to moving axes. The
expression for the energy in terms of the velocities now
becomes a homogeneous quadratic function of w, v,; w, p, 9; 7;
¥, x',... in which all the coefficients are known to be
constants.
Let us apply the method due to Routh*, and modzfy this
function with respect to the coordinates y, y',... If T be the
value of the kinetic energy in terms of the velocities alone, the
modified function (@.e. the kinetic part of Routh’s modified
Lagrangian function)
Ce a = T—Kpy—x'py! — nat CO)
* Rigid Dynamics,’ vol. i, chap. viii.
494 Dr. C. V. Burton on the Motion of a
from (6). Itis further known that the whole energy of the
system
=H-+K, . . =o!
where Eis a function of u..., p..., only, and K is a function
of the momenta xp only. Suppose, now, that the solid were
brought to rest by forces applied to it alone: HE would vanish
along with u, v, w, p, g, 7, while the circulations «, and con-
sequently also K, would remain unaltered. The generalized
velocities x, y',... would in general have changed, becoming,
let us suppose x%, Xo,--- and the kinetic energy would
accordingly have become
K=Lpyy ti pyl + ...): 2a re
Now let
V=NVotX V=NItx' ~ . » . . (0)
so that each x1 is that part of the flux of liquid (volume per
unit time) which takes place across a barrier-surface owing to
the motion of the solid itself.
Having regard to (8), (9), and (10) our equation (7) for
T’ becomes
T’=(H+K)—2K—x«pyi—epy. . . . (1d)
Let us write for the velocity-potential of the acyclze motion
P=ud,+ vd, + wh, + ph, +qP, +7, + - (12)
and for the value of x, across the barrier-surface « we have
¥1 =\\{% —[ul+vm+ wnt p(ry—mz)
+ 9(lz—nz) +r(ma—ly)] bdo, peters ke
where 2, ¥, z are the coordinates of the element do and 1, m,n
are the dircction-cosines of its normal y, all referred to the
system of axes fixed in the solid. From (12) and (18) sub-
stitute in (11); thus
T’=E-K+ uSap|| [— ono + similar terms in v, w,
+ pnp | (ny —mz— oer \aa +similar terms in g, 7, . (14)
where the summation refers to the m barriers.
_ Remembering (8) it will be seen that T’ is now expressed
in the proper form, namely as a function of u, », w, Ps, 7, and
Perforated Solid in a Liquid. 495
the momenta xp, «’p,... only. By means of the relations
-
Be je ae ne
= Oe es
dap dv "aw "dg ©! a
the equations of motion of the solid can at once be written
down. X,..., L,..., are of course impressed force-and couple-
constituents.
10. Since the kinetic energy due to any number of per-
forated solids, moving in circulating liquid, can be divided
into two parts, of which one is a function of the component
velocities of the solids alone, and the other a function of the
circulation-momenta alone, the above method may obviously be
extended ; in fact a slight change in (14) will-render it at
once applicable to the more general case. We shall have,
evidently,
VY=H-K+ Sniep {| (1 oo a0 +similar terms in v, w,
Ze SpBep| | (ny—me— oo ria+ similar terms in g, 7, (15)
where H is still the energy due to the motion of the solids and
the acyclic motion of the liquid, and K the energy due to the
circulations. In each barrier-term the first } denotes sum-
mation with respect to all the solids, and for each u or p, &c.,
the second > denotes summation with respect to all the barriers
of the system.
These hydrodynamical results are not new, but the method
of proof is in some respects different from anything that has
yet been given, and will, I hope, be found intelligible and fairly
simple. In an admirable memoir, just communicated to the
Physical Society, Mr. Bryan has given a direct hydrodynamical
proof of the equations holding good for the motion of the
system in question ; but it seemed to me also desirable that
the problem should be rigorously treated by the method of
generalized coordinates, avoiding any assumption as to the
impulse of the cyclic motion, and proceeding entirely from the
principles established by Lagrange, and extended by Hamilton,
Routh, and Hayward.
When this paper was in proof it contained some remarks
on the ignoration of coordinates, as treated in Thomson and
Tait’s ‘ Natural Philosophy’*. Calling y, x’,... the inde-
* Part I. § 319, example G.
496 Mr. A. B. Basset on the Finite
pendent coordinates which, together with Wy, ¢,... determine
the whole configuration of the system in §§ ],..., it was
suggested that, in hydrodynamical and kindred applications,
there was a difficulty in proving that OT/dx, dT/dx’,---
were all zero.
But the difficulty, if indeed it should exist, is easily removed.
For since the actual motion at any instant could be generated
from rest by impulses of types corresponding to W, ?,... only,
we have throughout the motion
olfoxy—0, dT/ox'=0,233
and by the Lagrangian equations for y, y’,..., since all the
generalized forces are of types corresponding to W, @¢,...,
we get
egtyor dol. al
=e. a — > — =, =9,...
dt ox Ox bE ON 2 HOM :
whence
or or
—— =(), — =0 =e sie
Ox Oe
L. Note on the Finite Bending of Thin Shells.
By A. B. Basset, IA., F RS
ie HEN a thin shell of any form is bent in any manner,
the most convenient way of obtaining the equations of
equilibrium is to consider the stresses which act on a small
element of the shell bounded by four lines of curvature on the
deformed middle surface. If OAD B be a small curvilinear
Fig. 1.
Cc
rectangle bounded by the four lines of curvature OA,
AD, DB, and BO, the stresses across the section A D (as
pointed out in my previous papers{) consist of the following
* Communicated by the Author.
+ Proc. Lond. Math. Soe. vol. xxi. pp. 33 and 53; Phil. Trans. 1890,
p. 433.
Bending of Thin Shells. 497
quantities, viz.:
T, = a tension across A D parallel to OA;
M,= a tangential shearing-stress along A D;
No =a normal shearing-stress parallel to OC;
G,= a flexural couple from C to A, whose axis is parallel
to A Ds
ya torsional couple from B to C, whose axis is parallel
to OA.
Similarly the stresses which act across the section BD
consist of :—
T, = a tension across B D parallel to OB;
M,= a tangential shearing-stress along B D:
N, = a normal shearing-stress parallel to O Ol;
G, = a flexural couple from B to C, whose axis is parallel
to BD;
l= (cs torsional couple from C to A, whose axis is parallel
to O B.
By resolving the stresses and bodily forces (such as gravity
and the like), which act upon the element, parallel to the axes
OA, OB, and OC, and by taking moments about these lines,
we obtain the six equations of equilibrium of the element ;
but as these six equations connect ten unknown quantities,
namely the ten stresses which act across the sides of the
element, they are insufficient for the solution of the problem.
2. In the case of a bell, or of a railway bridge which is
thrown into a state of oscillation by a passing train, the
displacements are all small quantities, and under these cir-
cumstances the ten sectional stresses can be expressed in
terms of the displacements of a point on the middle surface
and their differential coefficients ; and owing to the fact that
these displacements are small, we may neglect their squares
and products when determining the stresses, and their cubes
&c. when determining the potential energy due to strain.
There is, however, another class of problems of considerable
importance in which the deformation is finite instead of
infinitesimal ; and to such problems the theory of thin shells
is inapplicable.
3. An ordinary clock-spring is one of the most familiar
examples of the finite bending of a thin plate or shell. Such
springs consist of a naturally curved steel strip whose thick-
ness is somewhere about one thirtieth of an inch, and whose
breadth is from an eighth to a quarter of an inch according
to the size of the clock ; and when the clock is wound up
an amount of bending takes place which it would be unsate
to treat as infinitesimal. ‘The hair-spring of a watch also
498 Mr. A. B. Basset on the Finite
involves a case of finite bending; but as its cross section is
approximately square, the theory of the bending of wires*
would be more applicable. Similar examples, such as spring
balances and other mechanical appliances where springs are
employed, will readily suggest themselves; and the question
whether the theory of wires or the theory of thin shells is
most appropriate depends upon the nature of the spring. If
the cross section does not differ much from a circle or a
square, the former theory would appear to be the most applic-
able; if, on the other hand, the breadth of the spring is
considerable compared with its thickness, it would be better
to regard it as a thin shell.
When the natural form of a spring is a plane curve, and
the spring is bent into another plane curve, the problem may
be completely solved by the methods explained in chapter viil.
of my ‘ Elementary Treatise on Hydrodynamics and Sound.’
The mathematical treatment is the same whether the spring
be regarded as a wire or as a thin strip of metal like a clock-
spring; the only difference being that the flexural rigidity is
different in the two cases. If, however, a piece of clock-
spring is twisted as well as bent, or a thin plate or shell is
deformed in a finite manner, the solution of the problem pre-
sents difficulties of a rather formidable character.
4, Whenever the deformation is finite, the displacements of
a point on the middle surface are not small quantities whose
squares and higher powers may be neglected, and therefore it
is useless to attempt to express the stresses in terms of these
quantities; but since any deformation involves a change in
the values of certain geometrical quantities, such as the cur-
vature and torsion of certain lines drawn on the middle surface,
the most appropriate course to pursue would be to endeavour
to express the stresses in terms of such geometrical quantities.
There is one class of problems which can often be solved
without much difficulty, which occurs when a plane surface
is bent without extension into a developable surface ; or when
a developable surface is bent into a plane, or into some other
developable surface such that the lines of curvature on the
old surface are lines of curvature on the deformed surface.
This method can generally be applied when a plane plate is
bent into a conical or cylindrical surface ; but it could not be
applied in the case.of a right circular cone which is bent into
a cone whose lines of curvature are not identical with those
of the former cone.
The success of this method, in cases where it can be applied,
depends upon the circumstance that the flexural couples Gy,
* See Proc. Lond. Math. Soc. vol. xxiii. p. 105.
es
Bending of Thin Shells. 499
G, can be expressed in terms of the changes of curvature,
and also that in the special cases alluded to a sufficient
number of the ten stresses are zero to enable the remainder
to be determined by means of the general equations of equi-
librium.
5. We shall now determine these couples, using Thomson
and Tait’s notation for stresses and elastic constants, and
Love’s notation for strains. Fie o
Let O A, OB be two lines of curvature on ‘
the middle surface of the undeformed shell ;
O,, O, the centres of principal curvature ;
let oa, ob be the curves in which the
planes OA O,, OBO, meet any layer of
the shell. Let p,, p. be the principal radii
of curvature at O, let Oo=7, and let 2h be
the thickness of the shell. Also let accented
letters denote the strained positions of the
various points.
If P denote the traction along oa, and R
the normal traction along Oo,
P=(m+n)o,+ (m—n) (a, +03)
=%n{(1+H)o,+Ho,}+EHR,. . . . (1)
where |
EH=(m—n)/(m+n).
Now
__ dal —oa
and ai ee
OG ENS | SUI ee ne eee
OA Times OW aa oe n' =(1 +43).
Since we neglect the extension of the middle surface,
O'A'=OA, whence
Uh
pee UPL =m (— ~) 4 1
1+%/p; P1 Pi Pi
Tira! 1 n R
=n ( et a + pi! | magn Mates) | e e (2)
Similarly,
ae seg yf RK 1 "
a=n(o at pe! | men ~Blaite) f° e (3)
The value of Gy is
h
G.=| Pains, la tetidiees @ (/(4)
—h
500 Mr. A. B. Basset on the Finite
Now, according to the fundamental hypothesis of my
former papers it follows that, provided there is no eaternal
pressure, R must be a quadratic function of h and n, and con-
sequently the retention of R will lead on integration to
terms in Ge» of a higher order than h?, which are to be
neglected, since the solution we require is an approximate
one which does not contain higher powers of h than the cube.
Accordingly if we substitute the values of o,, a2 from (2) and
(3) in (1), and the resulting value of P in (4) and integrate,
we shall obtain |
= 4 3 f = a a (= as ~) :
Similarly,
h
G)= =) Qn dn,
—h
which gives
an oe ee (i 2 ,
a git {0+ (S ele ae ae
Equations which are equivalent to (5) and (6) have been
given by more than one writer on elasticity ; but attention
has not always been called to the fact that they depend upon
the express conditions that the surfaces of the shell are free
normal pressures, and also that the extension of the middle
surface may be neglected.
When a plane plate is bent into a developable surface
Pi=p,=; also one of the quantities p,', or ps! (say pe’) is
infinite ; whence (5) and (6) become
Gy= $nl3(1-+E) /p/! >
Gy = —$nh*H/p,' }
where G, is the couple about a generating line of the develop-
able.
Since the extension of the middle surface is neglected,
equations (5) and (6) would not apply to the case of a plane
plate deformed into a surface such as a portion of a sphere.
7. Asan example of the preceding method, we shall con-
sider the case of a plane plate of thickness 2h, which is
bounded by two radii CA, CD, and two ares OB, AD of
concentric circles ; and we shall inquire whether it is possible
to bend this plate into a portion of a right circular cone in ~
which OA, BD are generators, and OB, AD are circular
sections.
We shall assume for trial that the bending may be effected
by means of tensions, normal shearing stresses, and flexural
Bending of Thin Shells. 001
couples applied to the edges ; so that the tangential shearing
stresses and the torsional couples are zero.
Fig. 3.
o)
B D
Let « be the semi-vertical angle of the cone, r the distance
of any point on OADB from ©, Then
pi =p =; p2=0; p/=r tana;
whence
| G,=4nh? Hr! cota,
Gy = —$nh3(1+ B)r— cota.
The equations of equilibrium are
d
qn (hit) T=,
a)
dT,
as, +N,cos a=0,
d dN
q,p Nz") sin «+ oat —T.,cosa=0, > (8)
dG,
AE + Ny sine=0,
d
£ (Gor) —Nor + Gy=0. |
Let
4nh3 (1 + E) cota=h,
then
Ci. —k/r,
whence
No=—hk/r*, N,=0,
whence
T,=4& tan a/72,
and therefore
A ktane
h= fie ee
, ?
where A is the constant of integration.
From these equations we see that all the stresses are per-
502 Prof. Angstrém on the Intensity of
fectly determinate except T,. If CO=a, CA=8, and T,, To
denote the tensions along OB, AD, we have
7 A ktan @ |
Za ae :
PA hime (? + | al eee)
Cee: ae
from which it appears that either T, or T, may, if we please,
be made zero, provided the other be properly determined.
The above results would also apply to a belt of a complete
cone, bounded by two circular sections.
LI. Bolometric Investigations on the Intensity of Radiation
by Rarefied Gases under the Influence of Electric Discharge.
By Kyvr Ayestrou*.
()* E of the peculiar difficulties attending the quantitative
determination of the amount of energy radiated by gases
in vacuum-tubes is the extreme feebleness of its intensity.
In his recent work in this field, executed at the Hochschule
at Stockholm, Prof. Angstrém attacked the problem by the
bolometric method, which, although leaving something to be
desired as regards sensitiveness, led to some important results.
Another obstacle lay in the well-known difficulty of obtaining
the gases in a state of such purity that the spectrum exhibited
by the discharge through them in a vacuum-tube showed no
foreign admixture, such as the carbon-bands seen whenever
grease is used for joining surfaces, or where the flame touches
in the process of soldering.
The discharge-tube used for the most careful experiments
was thoroughly cleaned after soldering-in two electrometer-
terminals, and attaching two short lengths of tubing at right
angles near each end. The latter were to receive the elec-
trodes, whose construction required particular care. Into a
short capillary tube a piece of platinum wire was introduced
from one end and a piece of thoroughly cleaned aluminium
wire from the other. The tube was then heated so as to form
an air-tight junction between the two wires, and was then
fitted into a glass plate. After removing all grease the tube
covering the aluminium wire was cut off, so that the latter
acted as a perfectly clean electrode, and the glass plate hold-
ing it was fitted on to the short tube attached to the discharge-
* Abstract from Wiedemann’s Annalen, No. 3, 1893, by E. E. Fournier
d’Albe, B.Sc., Royal College of Science.
Radiation by Rarefied Gases. 503
tube. The joints were made air-tight by means of sodium
silicate, which proved to be a highly useful cement, and did
not give rise to any impurities. Short lengths of tubing
containing mercury were placed round the platinum wires to
convey the current to the electrodes.
The behaviour of four gases only was investigated, viz.
hydrogen, oxygen, nitrogen, and carbonic oxide. Hydrogen
and oxygen were prepared by electrolysis of pure newly-
distilled water acidulated with phosphoric acid. The nitrogen
was obtained by passing pure air over heated copper-turnings
reduced by hydrogen. Carbonic oxide was prepared by the
reaction of sulphuric and oxalic acids, and purified by passing
through caustic potash. In producing these gases all rubber
tubes were dispensed with, and the different parts of the
generating apparatus were soldered together.
The discharge-tube was connected through a Kundt glass
spring and a set of cleaning-tubes to the tube used for intro-
ducing the gas, a mercury-valve, and the air-pump. © The
mercury-valve consisted of a U-tube communicating at the
bottom with a long tube full of mercury. By varying the
level of the mercury by means of a reservoir the valve could
be opened and closed. The tube for introducing the gases
corresponded in the main to Cornu’s arrangement. A vertical
glass tube is filled with mercury whose level can be varied by
means of a reservoir connected through a flexible tube, as in
the case of the mercury-valve. At a point some distance
from the bottom is attached a capillary U-tube, the end of
which, in the process of filling, is introduced into a small
reservoir containing the gas. Lowering the mercury esta-
blishes a connexion with the discharge-tube through the
drying-tubes, and on raising the level the gas is shut off
from the atmosphere. |
The current was furnished by a battery of 800 small Planté
accumulators, regulated by means of a liquid resistance con-
sisting of cadmium iodide dissolved in amyl alcohol, and
measured by a dead-beat reflecting-galvanometer. The fall
of potential in the discharge-tube was measured by a Mascart
quadrant-electrometer.
The bolometer used for the experiments consisted of two
gratings cut out of tinfoil mounted in ebonite frames. These
frames were placed one behind the other in a tube with
double walls, the posterior one being protected from radiation
by a small double screen. Four diaphragms were mounted
in the tube in front of the gratings, to diminish air-currents.
The grating absorbing the radiation occupied a circular space
of 16 millim. diameter. It was blackened by precipitated
504 Prof. Angstrém on the Intensity of
platinum and smoke. The four branches of the Wheatstone-
bridge arrangement, of which the gratings formed two, had
each a resistance of about 5 ohms. In order to be able to
rapidly test the sensitiveness of the combination, a constant
resistance was introduced as a secondary circuit into one of
the branches. The opening or closing of this circuit usually
made a difference of 75 scale-divisions. If not, the reading
was reduced to that standard sensitiveness.
The bolometer was separated from the end of the discharge-
tube by a double screen with a perforation, inside which was
suspended a small screen. This was quickly pulled up to
expose the bolometer. The strength of current through the
discharge-tube was measured by the galvanometer, the diffe-
rence of potential within it by the electrometer, and the
deflexion of the galvanometer in the bolometer circuit was
read from minute to minute. ‘The latter gradually increased,
owing to the warming of the walls of the discharge-tube. By
suddenly breaking the current and again observing the
bolometer the radiation of the tube-walls was eliminated.
Another method of elimination was by interposing a plate of
alum about 4 millim. thick, which totally absorbed the radia-
tion from the glass. Another source of error was the reflexion
from the walls of the tube. The end of the tube opposite the
bolometer was closed by a plane-parallel plate of rock-salt.
This occasioned a loss by reflexion, whereas the other surfaces
entailed a gain. Both were corrected by introducing a small
copper box heated by steam circulation into a tube of the
same construction as the discharge-tube, observing the
bolometer deflexions, and repeating with the box alone.
Prof. Angstrém states his main results as follows :—
1. For a given gas and a given pressure the radiation of
the positive light is proportional to the intensity of the electric
current.
2. For a given gas and pressure the composition of the
radiation is constant and independent of the strength of
current.
3. On increasing the pressure of the gas, the total radiation
for a given strength of current increases as a rule, slowly at
low, more rapidly at high pressures. At the same time the
composition of the radiation changes, inasmuch as the ratio
of the intensity of the shorter waves to the total radiation
decreases. Thus the distribution of the intensity in the
spectrum changes in such a manner that with diminishing
pressure the intensity of radiation increases for the shorter
wave-lengths.
4, The ratio between the intensity of total radiation and
Radiation by Rarefied Gases. 505
the current-work increases continuously with diminishing
pressure of gas.
5. The useful optical effect of the radiation (here given by
the ratio of the intensities of the radiation passing through
the alum plate and the total radiation respectively) is very
high for some of the gases at low pressure (about 90 per
cent. for nitrogen). But the useful optical effect of the
work spent is not very great (about 8 per cent. for nitrogen
of 0-1 millim. pressure).
6. The intensity of total radiation must be considered as a
secondary effect of the discharge, and depends upon the mole-
cular constitution of the gas.
7. Whatever views we hold concerning the nature of the
gaseous discharge, this investigation appears to confirm the
hypothesis of Hittorf, E. Wiedemann, and others, that the
radiation is not a pure function of the temperature of the
gases, but must be regarded as anomalous (“ irregular,”
“* luminescence ”’),
If we call “irregular” a radiation in which the spectro-
scopic distribution of the energy is anomalous, there are
certain facts observed by Prof. Angstrém which lead to the
conclusion that the radiation in question is irregular. The
radiation did not show any relation to the absorptive power
of the gas at ordinary temperatures. Again, the radiation,—
which in nitrogen at 2 millim. pressure is still rich in dark
rays,—rapidly changes in quality when the pressure de-
creases, and at 1 millim. consists almost exclusively of light
radiation. Prof. Angstrém supposes that the radiation of the
gas during electric discharge consists of two parts, one of
them regular, the other irregular. With decreasing pressure
the former decreases, whilst the irregular radiation increases in
proportion as the motions are less obstructed by the mass of
the gas. At constant pressure a certain portion of the energy
in each molecule is converted into radiation ; as the strength
of the current increases, the number of active molecules, and
hence also the radiation, increases in the same proportion as
the current. The number of active molecules being relatively
small, the damping effect of the rest may be taken as constant,
and the composition of the radiation remains practically
unaltered as the current increases. On increasing the pres-
sure, however, the damping effect changes, the anomalous
dispersion is more easily transfermed into a normal one, and
the radiation becomes richer in infra-red rays. A greater
proportion of the energy supplied is spent in heating, and
for the same current-work the total radiation decreases with
increasing pressure.
Phil. Mag. 8. 5. Vol. 35. No. 217. June 1893. 2N
506 Mr. E. C. Rimington on Luminous
But in view of the difficulties of the investigation, the
paucity of available material, and the approximate nature of
the results in this almost unexplored field, no final decision
can as yet be arrived at. A tabulation and a graphic repre-
sentation of the results, with diagrams of the apparatus and a
full discussion of methods and corrections, will be found in
the original paper.
LIT. Luminous Discharges in Electrodeless Vacuum-Tubes.
By HE. C. Rimineron*.
See reading a paper in conjunction with Mr. E. W.
Smith on November 25th, 1892, before this Society, on
“ Experiments in Electric and Magnetic Fields, Constant and
Varying,” the Author’s attention has been drawn to a paper
contributed by Mr. Tesla to the ‘ Hlectrical Hngineer’ of
New York, July 1st, 1891, in which the luminous ring-
shaped discharge obtained when a Leyden jar is discharged
through a coil of wire surrounding an exhausted bulb is
attributed to the electrostatic action of the surrounding wire,
and not to the electric stress set up in the rarefied dielectric
in consequence of the rapidly oscillating magnetic induction
through the bulb.
As one experimental proof of this assertion Mr. Tesla
gives the following experiment :—“ An ordinary lamp-bulb
was surrounded by one or two turns of thick copper wire,
and a luminous circle excited by discharging the jar through
this primary. The lamp-bulb was provided with a tinfoil
coating on the side opposite to the primary, and each time
the tinfoil coating was connected to the ground, or to a large
object, the luminosity of the circle was
considerably increased.”’
The author repeated this experi-
ment with two Leyden jars arranged
as in fig. 1, and found that when the
spark-gap was sufficiently large to
produce a bright ring when the tin-
foil was not connected to earth, doing
so produced no noticeable difference
in the brilliancy ; but that, if the
discharge were faint, it was ren-
rendered considerably brighter on
making the earth connexion. Better
results were, however, obtained on
* Communicated by the Physical Society: read April 28, 1893.
+ Ante, p. 98.
yy Bie
Discharges in Electrodeless Vacuum- Tubes. WENO
connecting the tinfoil to either of the outside coatings, A or
B, of the jars instead of to earth. This result led the author
to try a series of experiments to endeavour to determine
the cause of the effect, of which the typical ones are here given.
Hzperiment 1 (videfig. 2). A Fig. 2.
S
and B are the outside coatings
of a pair of Leyden jars (those
employed were about pint size).
Cand D two vertical and paral-
lel metal plates, at a distance of
about one foot from the jars. The
spark-gap, 8, is adjusted by a
screw, so that the spark-length
can be varied by small amounts
when necessary. A single turn
of wire, a , encloses an exhausted
bulb, and its ends are connected
to A and B, as shown in the
figure, so that a the part nearest
to C is connected to A, and 6 to
B. Two loose wires, e and /, are
also connected to A and B.
The spark-gap is now shortened until there is just no
luminous ring in the bulb.
The plates C and D are then connected to the outer
coatings A and B by means of the two loose wires, with the
following results :—
(1) Ato C. Bright ring.
(2) Bto D. Bright ring.
(3) A to C and B to D simultaneously. Bright ring.
(4) A to D. ; :
(5) B to ©. ; No luminous ring.
(6) A to D and B to C.
Expt. 2.—The wire turn ab is removed from the bulb,
given a half twist, and then replaced ; so that a is now
nearest to D, and 6 to C. Plates not connected, no luminous
ring.
(1) Ato C.
(2) B to D. fs luminous ring.
(3) A to C and B to D.
(4) A to D.
(5) B to C. trig ring.
(6) A to D and B to C.
Hapt. 3.—Arranged as in Expt. 1, case (1) or (2). Cis
then connected to D, and the ring becomes less bright.
Expt. 4.—Arranged as in Expt. 1, case (1). © and D
2N 2
ee a ma WS
PT ee
OY oa
jae x EE ate ok 2. =
es aso ~
508 Mr. E. C. Rimington on Luminous
connected. On approaching C to the bulb, ring becomes
brighter.
On approaching D less bright.
If arranged as Expt. 1, case (2), the reverse happens.
All the above four experiments give the same effects if the
turn of wire be larger than the bulb, as in fig. 3, only a longer
spark-gap has to be used.
Eept. 5—A single turn of
wire (fig. 3), a 6, larger than
the bulbis employed, and between
the bulb and the ring a semicir-
cular strip of tinfoil or metal T is
placed. The wire is connected as
in Expt. 1. The spark-gap is
arranged to give no ring. Con-
necting T to B bright ring, T
to Anoring. The reverse hap-
pens if the tinfoil is placed in
position T’ as shown by the dotted
line.
Haupt. 6.—A piece of gutta-
percha covered wire is bent into
shapes shown in figs. 4 and 5. On placing either of these
over bulb as in fig. 6, a figure of eight-shaped luminous
Fig. 38.
Fig. 4.
Z 6
h c
discharge is obtained, and there is no noticeable difference
between the two.
Fig. 5.
7 6
h c
Expt. 7—Putting the wire (fig. 4) on bulb as in fig. 7, a
Discharges in Electrodeless Vacuum- Tubes. 509
single broad band-ring is obtained, as the two turns will help
one another with respect to magnetizing effect.
Doing the same with the wire (fig. 5) a discharge is
obtained shaped like the sector of an orange, as shown by the
dotted lines, fig. 7.
Fig. 6. Fig. 7.
Expt. 8.—Bending a wire as shown in fig. 8, and placing a
bulb in the loop 6 ¢, there is no effect even with a long spark-
gap, although the potential difference between the sides
Fig. 8.
cand } would be much greater than in the case of a single
turn.
Putting a bulb in the loop, be, of fig. 4 at once gives a
bright ring.
a
510 Mr. Ki. C. Rimington on Luminous
Hxperiments 6, 7, and 8 seem to show that ring, or other
shaped, sharp luminous discharges can only be obtained with
the wire so wound as to give magnetic induction through the
bulb, while the first five experiments show that an electro-
static field in the bulb may help the effect. ‘The theory the
author has come to after consideration of the above and
other experiments is:—That if the H.M.F. due to rate of
change of magnetic induction acting in the dielectric of
rarefied gas be insufficient to break it down and produce a
luminous discharge (owing to the spark-gap being too short),
the electrostatic field between the plates C and D, or between
one of the plates and part of the wire, if correctly timed with
respect to the rate of change of current in the wire, will
commence the breakdown of the gas, thus allowing a less
H.M.F. due to the magnetic induction to complete it.
To put this to the test, a single turn of wire was put round
a bulb and the spark-gap adjusted so as to give a very faint
or no luminous ring ; on the top of the bulb was laid a piece
of tinfoil connected to one pole of a + in. spark induction-
coil ; when the coil is worked the tube is filled with a faint
glow: if now the Leyden jars are charged and discharged
there will be sometimes a ring in the bulb which will be
occasionally quite bright. The reason it cannot be always
bright is of course that the discharges of the induction-coil
are periodic, as are also those of the jars, and it is only when
the two are properly timed (i.e. the P.D. due to the coil
coming either just before or simultaneously with the spark)
that there will be a bright ring.
This experiment seems to settle the question and show
conclusively that a properly timed electric stress in the bulb
due to an electrostatic field will allow an E.M.F. due to the
alternating current in the wire to produce a breakdown of
the rarefied gas, which the latter is too small to effect without
the aid of the former™*.
In Expt. 1, when A and C are connected this field will
exist between © and 0 the side of the turn of wire remote
from C, and must therefore pass through the bulb. When A
* To prevent misconception, it had better be definitely stated that this
electrostatic stress does not necessarily act in the same direction as the
E.M.F. due to the rate of change of magnetic induction. In experiments
(1) to (5) the direction of the former will be through the bulb from side
to side, while that of the latter is a circle coplanar with the wire. As
the discharge in a gas is of a nature more or less electrolytic, being
accompanied by the splitting up of the molecules, it seems reasonable to
suppose that anything which increases the number of dissociated molecules
will enable a smaller stress to produce a breakdown in the form of a
luminous discharge.
Discharges in EHlectrodeless Vacuum- Tubes. bit
is connected to D, as the strongest field is between 6 and D,
where thé P.D. is greatest, it does not pass through the bulb ;
in fact the field in the bulb willsimply be that due to the P.D.
between a and 0, or the same as it is if the wires e and / are
disconnected. ‘The results of Experiments 2, 3, 4, and 5 are
also obviously explained by this theory.
To treat the subject mathematically. We have the well-
known equations for the discharge of a condenser :
Lo +Re=- = where K is the capacity,
and Pa dq
dt
Combining these,
&q , Rdg 1
see, © Kid
To obtain an oscillatory discharge 4L must be greater than
Oe
Putting a for == and b for ee emo 5 the solution
ig
pee wees oa ee
where @ =eun'| ~-) and @ is the initial charge.
This may be more conveniently written
p= Qe EFF os un,
where
ay) or tang=—+ = _ KR
ae) eee 4L—KR*
Eas i oe
If the oscillations are to be rapid, RP must be large compared
4
R2
to 42
Therefore 7 will be some small angle.
Instead of quantity we may write P.D. of the condenser,
or
ares)
5 Vee Va +P cos (e—n). ig ogee}
i oe
512 Mr. E. C. Rimington on Luminous
The current
C= dq — Q — ~p
ae biG Ol
Now the electric stress acting in the bulb is proportional to
et sin bt=
asindt.. . . (3)
de
the rate of change of current, or to — ;
“ile
and Oe TING Gi OS
——— Ss bt). scare C2
ee (asin bt + 6 cos Jt) (4)
The current itself will be a maximum or minimum when
de fe
ioe 3
?,é. when asin bt+b cos bt=0, :
or when a eee — Als tae :
a KR?
Therefore l¢=0, and is in general nearly equal tol 5
The maximum values of the current occur when
bi=0, 27+0, 474+, &e.,
and the minimum values when
bt=7r+6, 3874+0, 57+4+8, Ke.
This is shown in the curve (fig. 9), the points M,, M., M3,
&c., representing the maximum and minimum values of the
. 7
current. The distance O A represents 0, and A B= °) =P 9
It is now necessary to consider when the rate of change of
. ae A
the current is greatest. Ai will be a maximum or minimum
C4
2
when ne —(),
dt?
Now
iE V + he
a = ope (a? —L*) sin bt + 2ab cos bt} = 0.
Hence |
in a = 2. 2 RY Ka Sg
on 2L—-KR?
Let
2L—KIi?
y will be in general a small angle.
Discharges in Electrodeless Vacuum- Tubes. 513
The rate of change of current will be greatest (either a maxi-
mum or a minimum) when
bt=—y, w—-y, 27—y, Ke.
Obviously 0¢ cannot equal —y, so that the rate of change
of current is greatest for values 7—y, 27—y, d&c.; or at
points “44, M2, #3, &e. in the curve (fig. 9), and HF=y. If
Fig. 9.
R
ty,
Dotted curves are values of the exponential 77 ° 21
é =
Sc
Se Z
e
YA LUES OF CURRENT
M,, M,, M;, M, are the maximum values of the current. p,, m2, us are
the points where the rate of change of current is greatest.
the oscillations are to be very rapid KI? must be negligible
compared to 4L ; in which case
tan y= He
tan yn = Wo
we
also
he! Mr. E. C. Rimington on Luminous
and they are both very-small angles, hence y=2” approxi-
mately, or HEF =2AB.
When bt=7—y,
Ue
== ie
de vy e fy 25
we 6
or if the oscillations are very rapid,
de = eB ye
pee
If, however, ¢=0,
re
Cpe NU:
so that the greatest rate of change of current occurs at the
first instant of discharge, although this is not a mathematical
maximum.
HKiquation (4) may also be written
de _ V Ve+E
dt bL
n being the same angle as before.
It is now necessary to consider the values of the P.D.
between the outside coatings A and B of the Leyden jars.
Let / and r be the inductance and resistance of the coil
connected to the outer coatings, and L and R the same for
the whole circuit. Let v,—v,=« be the P.D. bevmeen the
outer coatings at any instant t. Then
e cos (bt-+9); ae)
Vice
c= e@ sin bt,
bL
and 2=0,—v. er +1,
dt
Ve, :
ware {(r+la) sin bt + lb cos bt}
Vee Dy Oey Seay Ea I
=a, V Pb +(r+ la)? cos (bial) ee
where ” ae
tan 7! = !
USER PGD
7! will be in general a small angle not very different from ;
Discharges in Electrodeless Vacuwm-Tubes. 515
and if : = nor the time-constant of the coil equals the time-
constant of the whole circuit,
; =~ =—2a,
a
., tang = j = tan n, or y' =n.
That is # is in phase with v the P.D. at the inner coatings of
the jars.
To find the maxima and minima of x we have
ee: ae [ {ar + l(a? —b7)} sin bt+ b(r + 2la) cos bt] =0.
ut b(r + 2la)
a tame = ar+Ua2—2)
_ (rL—Rl) VK(4L—KR)
S L(KRr +21)
= tano.
Then « has its greatest positive or negative values when
bi=5, +8, 27+56, Kc. Sis in general a small angle, and
is positive if
L l
ane
and negative if
he
(Pers
If eae ;
ar ae 60;
If = be not greater than : the first largest value of a will
occur at t=0, and as the rate of change of current is also
greatest at this instant the two will occur simultaneously.
The next greatest value of 2 occurs when
pees (itz 2 -),
th
and the next greatest rate of change of current when
bt=7 —¥.
Sa a ee
516 Mr. KH. C. Rimington on Luminous
6 will be less than y, if be nearly equal to so that the
de
dt’
but the value of z will not differ very much from its maximum
maximum value of x will occur after the maximum of
de . ; ; :
when a is A maximum®*. This bears out the results obtained
in experiments 1 and 2, though, of course, the electric field in
the bulb will be that due to the P.D. between one of the
plates, C or D, and the opposite side of the turn of wire, and
this will only be about half that between the outer coatings
A and B. Moreover, the phase of the potential of C will
not be quite the same as that of A, on account of the
inductance of the connecting wire e. Experiments 1 and 2
were, however, tried with the plates C and D, and the con-
necting wires removed, the turn of wire ab being moved so
as to bring either a or b nearest to A or to B, and the results
obtained were practically the same as those of experiments
1 and 2.
Effect of Size of Surs.
When different-sized Leyden jars are employed with the
same length of spark-gap the luminous ring is more brilliant
* The above investigation into the value of the P.D. between the
outer coatings will only give correctly the state of things when a steady
swing has been set up in the circuit; as evidently when ¢=0 the value
of w also equals zero, so that 2 must start in phase with the current; it
will, however, rapidly get out of phase with the latter, and finally be
nearly in quadrature with it, This is due to an initial wave starting
from the spark-gap which runs round the circuit. Possibly the value of
x can be empirically represented by one of the two subjoined formule :-—
AEN emerge
£= VPP (tla)? sin {(bt-+p)(1—e-P4)t,
Ne Veat = :
* w= Ty NPG (r-Hla)? sin {Bt + y (1—e-Pe)},
=
where P= = —yn', and p some constant. Dr. Lodge, in his researches on
the A'and B sparks, approximately represents the initial values of 2 by
the current multiplied by the impedance of the conductor 7, or makes
Veut
t= — (?b?-+r* sin bt.
The initial maximum of z will consequently roughly coincide with the
maximum of the current, or be near the point M, of fig. 9, and will thus
come about a quarter of a period before the second maximum rate of
change of current, point p, (fig. 9).
Discharges in Electrodeless Vacuum- Tubes. Dali
with larger jars. Now the E.M.F, acting in the rarefied gas,
and producing the breakdown of the same, is proportional to
de
di’
Also the greatest value of de ta first occurs is when ¢=0,
dt
and then
de V
a yk
and the next is for very rapid oscillations
VS as
Ai = ey 2 Ibg
So that the first value of the E.M.F. acting in the gas is
independent of the capacity, and the next and succeeding
values are less the greater the capacity.
The effect on the eye, however, of the luminous ring will
be the time-integral of the discharge or approximately depend
on |
The whole limits of ¢, viz., from 0 to «©, cannot be taken at
once, as < keeps reversing, and this reversal will not affect
the luminous discharge. Referring to the curve (fig. 9) it
will be seen that the first reversal must take place at M,, when
bt=80, and subsequent ones for values 7 +0, 277+ 0, KXc., of bt.
It is therefore necessary to take first the limits 6 and 0, then
a+6 and 6; 27+0 and r+40, and so on, alternately writing
the integrals plus and minus.
* de =e We eae “t sin Ot |
\ a = aL le sin b¢ | le sin bt
2r+0
+ ee sin ot | — &e.ad inf. :
7+
Remembering that
sin ( 7+0)=—sin 0,
sin (27+0)= sin @,
sin (37 + 0) = —sin 9, and so on,
518 Mr. E. C. Rimington on Luminous
this gives
” de ae a) Gero) © (On + 6)
i, a = zy, sine Ga + e2 +e6 +e. \,
The series in the bracket is a geometrical progression, in
a
which the constant factor is e@"; and, since a is negative,
this is less than unity.
Hence
“6
* dc Gps 2V sin 0 eb
nade 6L 7
and
tan 0= ee oie or sin@= We KR’,
also
4L—KR sin @
— — 4/7 kale
e tenner age
re) => 46
{ eo = 2V oe aad
» at a
1—e
RY ee) =
eV W—=KR?—e J 4L—KR?
et Ogg Sa _=eand ra /_KRE_ =
4L— — 41,--KR?
Then the denominator =e*—e?-9, and
ealtet 5 + 3 ea
2ay y? 3u7y
ig
omer ih ia
oa B - + &e.,
. 2xy eo 3n*y __ 3ay? y
oot tt ee. 38>
+ terms of the 4th, 5th, &. powers.
Discharges in Electrodeless Vacuum- Tubes. 519
Now wz and y will in general be small fractions, since KR?
is usually much less than 4L.
If the oscillations are very rapid, @ is very nearly equal to
y Hence y=2x approximately. Then e’—e*’ becomes
9a ig
6 = 2a (1 ae =) approx.
Therefore the time-integral
) ap prox.,
av4/8 = 4/*(1- =)
~ 2e(14 ©) =) e
and
c= ty / KR? aoe Ee sien
meoN/ (bk 4 eke
so time-inte or
approx.
mw RK
au (I~ “55,
Now from this it is seen that the effect of increasing the
capacity would be to slightly diminish the time-integral, and
consequently probably make the brillianey of the laminous
discharge less, if it were not that increasing the capacity
diminishes the real resistance of the circuit, since it makes
the oscillations slower, and the resistance R for copper for
rapid oscillations approximately equals /46/ Ry; where / is
the length of the wire, and R, its resistance for steady cur-
approximately.
rents. Now b= VEL
- Therefore
so that the time-integral is very roughly proportional to the
fourth root of capacity.
There is also another reason why larger jars might produce
a brighter discharge, even though the ae integr al were less.
With larger jars ines time foleen for the amplitude of the cur-
rent to sink to a value at which it becomes insignificant will
LR ——
520 Mr. E. C. Rimington on Luminous
be longer than in the case of small ones. Now, as the initial
value of 2 is the same whatever the size of the jars, the after
values (although their time-integral is less and their actual
values less also) last longer in the case of larger jars.
When the breakdown of the dielectric of rarefied gas is once
ees See de
begun by the initial ai the values of 7 necessary to keep it
up may probably be very much less, and consequently the
smaller values of = lasting longer, as given by the larger
jars, may produce a luminous discharge more brilliant to the
eye than the larger values of = lasting a shorter time, as given
by the smaller jars.
The actual results obtained with a ring of four turns of wire
containiny an exhausted bulb about 24 inches in diameter
were that the differences in brilliancy, obtained by using
half-gallon jars, pint jars, or very small jars made from spe-
cimen glasses, were not so very great.
Other Effects. Apparently unclosed Discharges.
A closed luminous discharge is not the only one that can
be obtained. Mr. Tesla, in 1891, pointed out that by wrap-
ping a wire round an exhausted tube so as to form a coarse-
pitched spiral, a luminous spiral discharge is obtained. He
was apparently only able to obtain a very feebly luminous
spiral, but the author has succeeded in getting one quite as
brilliant as in the case of the ring-shaped discharge obtained,
with a bulb.
Fig. 10.
In fig. 10 two half-gallon jars have their outer coatings
connected by a wire, A B, bent as shown in the figure. Over
J *~
Discharges in WB icopradeless Vacuum- Tubes. Sb DY
-the wire is laid an exhausted tube, C, with a tinfoil cap*, T,
at one end; T is connected to the outer coating of the jar
nearest to it. The object of this is to utilize the electrostatic
effect and make the tube more sensitive to breakdown by the
electromagnetic one. When the jars discharge, a straight
luminous band is observed in the tube directly over A B.
If the tube C be now moved towards the jars, even by a
very small amount, a closed circuit discharge will be obtained.
_There is apparently, then, a tendency for the luminous dis-
.charge to form a closed circuit whenever possible ; and it
.seems probable that even when the discharge is apparently
not closed, as in the case of the spiral or the straight line,
_the electric stress acting in the rarefied gas takes the form
of a closed circuit, but is only intense enough to produce
sharp luminosity close to the wiret. To further test the ques-
tion an unclosed ring tube was made, and when it was placed
inside a coil of wire no trace of a single luminous band could
be seent. A small glass tube was also bent so as to form a
spiral of four turns, and exhausted. A wire following the
spiral was attached to it, but this also gave no trace - of
luminous discharge.
Magnetic Kffects of Discharge.
The ring discharge in a bulb or closed circular tube acts
like a metallic circuit as far as magnetic effects are concerned.
This may easily be shown by the following experiment.
A coil of three or four turns of wire has a similar one wound
with it to form a secondary ; the latter is connected to a
third coil, in which is placed an exhausted bulb. The first
‘coil is connected to the outside coatings of the jars (fig. 1).
‘The spark-gap can be adjusted so that a fairly bright ring is
* Tt is not always necessary to use this cap, as, if the exhaustion is
high enough to give green phosphorescence of the glass, with the two
half-gallon jars in series, the discharge can be obtained without the cap.
With another tube of lower vacuum the author finds the cap necessary.
+ That is, the return part of the discharge is so diffused and feebly
luminous as to easily pass unnoticed in comparison with the sharp and
brilliant luminosity close over the conductor. The same applies to the
spiral discharge, each turn of the spiral probably forming a closed circuit
by itself.
t On afterwards repeating this experiment the author obtained a dis-
charge in parts of the tube, and with half-gallon jars in the whole tube.
The discharge, however, was a closed one, as there were two distinct
bands in the tube, one on the side next to the coil and the other on the
side farthest away from it. This is what might be expected if the
magnetic induction be sufficiently strong.
Phil. Mag. 8. 5. Vol. 35. No. 217. June 1893. 20
LGPL TOC ATTEN IALTEOA E
522 Mr. E. C. Rimington on Luminous
produced in the bulb. If now a second bulb is placed within
the first coil a luminous ring will be formed in it, and the
ring in the other bulb will be much weakened or altogether
extinguished. Exactly the same effect is produced if a metal
plate or closed coil be brought near the first coil in lieu of the
bulb.
Sensitive State of Discharge.
If a single turn of insulated wire surround one of the
exhausted bulbs as in fig. 1, and the spark-gap be adjusted so
as to produce a rather faint luminous ring (the fainter the
better); on approaching the finger and touching the wire at
any point the discharge appears to be repelled, and takes the
shape shown in fig. 11. Instead of touching the wire with
the finger a small piece of tinfoil may Fel
be laid between the wire and the bulb, Pen.
as at A (fig. 11), and this may be touched
by the finger or connected to any large
object, insulated or otherwise ; the effect
produced is the same. Connecting the
tinfoil to one of the outer coatings of the
jars does not produce this effect, and
it is scarcely, if at all, visible when
the luminous ring is brilliant, due to
a longer spark-gap. With a wire ring
of several turns the author has not been
able to obtain it. If a turn of bare
wire be employed the effect is produced
when the finger is brought very near to the wire, but if it be
brought into actual contact the effect is no longer visible.
This apparently shows that it is due to the capacity between
the finger or tinfoil and the wire; it is probably of the
same nature as the “ sensitive state’ in an ordinary vacuum
tube,
ADDENDUM, May Ist, 1893.
Since writing the above the author has made a further
experiment* which at first sight appears to contradict the
one{ given in the paragraph on ‘‘ Magnetic Effects of Dis-
charge,”’
* Called hereafter the second experiment.
shown when the paper was read.
+ Called hereafter the first experiment.
This experiment was
Discharges in Electrodeless Vacuum- Tubes. 523
A ring (R) of four turns of wire is joined in series with a
single turn, and the two are connected to the outside coatings
of the jars. In the single turn a bulb is placed and the spark-
gap adjusted until a fairly bright ring is produced in it at
every discharge. If now a closed ring of thick copper-wire,
a metal plate, or a ring of several turns, similar to R, and
with its ends joined, be laid on R to act as a secondary, the
luminous ring in the bulb is brighter ; on substituting for this
an exhausted bulb and placing it in R, there will be a brilliant
ring-discharge in it, while the discharge in the other bulb
will be rendered fainter or altogether extinguished. In this
experiment the exhausted bulb secondary appears to act in
the reverse way to a metallic secondary.
The author then made the following experiments :—
(a) A ring of four turns of guttapercha-covered wire pre-
cisely similar to R was made, its ends were connected to an
ordinary Geissler tube. When this was used as secondary it
acted exactly in the same manner as the exhausted bulb both
in the first and second experiments, the Geissler tube being
brilliantly illuminated.
(6) The Geissler tube was then removed, and the ends of
the secondary coil connected to the coatings of a small Leyden
jar. The effects produced by this secondary were the same as
those produced by the exhausted bulb in both experiments.
(c) The ends of the secondary were connected to the loops
of a glow-lamp to act as a resistance (about 100 ohms). This
acted similarly to the exhausted bulb in both experiments.
(d) A disk of gilt paper (imitation) and also a ring of the
same were used as secondaries; these acted similarly to the
bulb in both experiments. When the discharge took place
there were brilliant sparks produced at various spots on the
paper, wherever there was any flaw in the gilding, showing
that considerable energy was dissipated there.
(e) The secondary coil of four turns had its ends joined by
a strip of gilt paper about 6 inches in length, with a con-
siderable number of flaws in the gilding (produced purposely,
by bending the paper sharply in several places, so as to
obtain considerable sparking). This acted similarly to the
bulb and dimmed the discharge in the bulb surrounded by the
single turn. On shortening the length of gilt paper between
the ends of the secondary, the discharge in the bulb was less
dimmed.
The results of these five experiments are, that any of tho
above secondaries are able to reduce the mutual induction
between the primary and secondary in the first experiment
sufficiently to render faint or altogether extinguish the
202
FE ay ee BEL Se . +6 Te
ALM aa OE + i LOE ICDL EN PIE PRED AP
oem
LS SN
524 Luminous Discharges in Electrodeless Vacuum- Tubes.
discharge in the bulb, and act similarly to an exhausted bulb
secondary. In the second experiment a low resistance se-
condary behaves in the reverse manner to an exhausted bulb
secondary, while (c) and (e) show that a high resistance put
externally into the secondary circuit, and (d) that a secondary
having a high resistance in itself, act in a similar manner to
an exhausted bulb secondary. (6) shows that if the ends of
the secondary be attached to a capacity it behaves like the
bulb.
' The most probable explanation seems to be the following:—
The amount of energy in the jars when charged is a fixed
quantity for a given spark-gap; this energy will be mostly
expended in the coil R and the single turn and bulb (the
second experiment). If, now, we can make energy be ex-
pended elsewhere, as in a secondary, we shall have diminished
the energy received by the bulb, and this will in general dim
it or altogether extinguish it. This will explain what happens
when an exhausted bulb secondary is used ; also experiments
(a), (c), (d), and (e). With regard to experiment (6), energy
may have been expended in heating the glass of the jar on
account of electric hysteresis. Moreover, this secondary did
not dim the bulb so much as the others, but was found to be
capable of improvement in this respect by including some
resistance (in the shape of the glow-lamp or a strip of gilt
paper) in its circuit.
In the case of a low-resistance secondary the energy dissi-
pated in it will be small, since its impedance will not be much
lessened by its being of low resistance on account of the high
frequency. This does not explain, however, why the dis-
charge in the bulb is brighter when a low-resistance secondary
is used*,
A further experiment was then made. The coil R in the
second experiment had a similar secondary 8 placed in it;
this was connected 1c another similar coil T. The spark-gap
was lengthened until a brilliant luminous ring was produced
in a bulb placed in T. The bulb in A was then moved away
from A until there was a very faint luminous ring init. On
removing the bulb from Ta very slight brightening of the
* Tnis energy explanation is probably not a complete one. Working
out the frequency in the cases of no secondary, a secondary of four turns
short-circuited, and the same with its ends joined through 100;
the author finds that the damping-term is increased when either secondary
is used, but more so with the 100 in circuit. The frequency is much
the same with the 100 in circuit as when there is no secondary, but
with the secondary short-circuited the frequency is about doubled. This
may account for the increase in brightness of the discharge in the bulb.
On the Psychrometer and Chemical Hygrometer. 525
_ faint ring of the bulb in A was observed. Instead of placing
an exhausted bulb in T, a coil of four turns with its ends
joined through 100 was laid on T, and the bulb in A adjusted
A one turn; S, R, and T each four turns.
to give a very faint ring; on removing the coil from T a
decided brightening of the discharge in the bulb was observed.
This experiment seems to show fairly conclusively that in-
creasing the energy in the circuit of the secondary S dimi-
nishes the brightness of the discharge in the bulb placed in A*.
LIL. Comparative Experiments with the Dry- and Wet-Bulb
Psychrometer and an improved Chemical Hygrometer. By
M. 8. Pemsrey, W.A., WB., Radcliffe Travelling Fellow ;
late Fell Hxhibitioner of Christ Church, Oxford. ne vom the
Radcliffe Observatory, Oxford.)
URING the late winter it seemed desirable to make a
series of comparative experiments with the Dry- and
Wet-Bulb Psychrometer and an improved Chemical Hygro-
meter, in order to ascertain the accuracy of the results given
by the Psychrometer for temperatures below the freezing-
oint.
: A series of comparative experiments, made by me in the
summer of 1889, had shown that the amounts of moisture
calculated from the psychrometric readings varied by +6 per
cent. to —9d per cent.from the amounts actually found by the
* Since writing the above the author finds that Prof. J. J. Thomson
has observed the effects noticed in the second experiment, and gives an
explanation practically identical with the above.
+ Communicated by Mr. E. J. Stone, #.R.S., Radcliffe Observer,
226 Mr. Pembrey on Comparative Haperiments
chemical method. The mean difference, however, in the
above series was insensible*.
The Chemical Hygrometer employed in both series was
that introduced by Dr. Haldane and the author f.
The absorption-tubes were placed in a small wooden box
with wire partitions to prevent them from knocking against
each other. The entrance-tube, by which the air to be
examined passed into the hygrometer, was fixed through a
small perforation in a rubber partition covering a hole in
the box. In this way any possibility of air being taken from
the inside of the box was avoided. }
The comparative experiments were made in the following
manner. ‘The weighed absorption-tubes were placed in the
shed containing the psychrometer about ten inches below the
bulbs of the thermometers. The wet- and dry-bulbs were
then read off; the absorption-tubes were connected by a long
piece of rubber-tubing with the aspirator. Air was now
drawn through the tubes at a rate of 1500 cub. centim. per
minute, until about 11,500 cub. centim. of the air had been
taken. Five readings of the temperature of the water and of
the air in the aspirator were taken during each period of
observation. When the aspiration was finished, the readings
of the wet- and dry-bulbs were again taken, and the absorption-
tubes disconnected and stoppered. The period of observation
generally lasted about ten minutes.
Simultaneous determinations with two chemical hygro-
meters were made in the previous, but not in the present
series of observations. In order, however, to check the com-
pleteness of the absorption and any errors in weighing, a
second pair of absorption-tubes was connected up with the
first pair.
The results for the psychrometer were calculated, not from
my own readings, but from the mean of three other readings
—one at the beginning, one at the middle, and one at the end
of each period of aspiration. These readings were obtained
from the continuous photographic record of the wet- and dry-
bulbs taken at the Radcliffe Observatory. It is possible to
read off this record to two minutes and to one-tenth of a
degree Fahrenheit. The accuracy of the readings has been
proved by years of use and comparison with eye-readings.
In every case care was taken to have the wet-bulb properly
moistened about a quarter of an hour before the observations.
* Phil. Mag. April 1890, p. 314. |
t ‘An Improved Method of Determining Moisture and Carbonic Acid
in Air,” Haldane and Pembrey, Phil. Mag. April 1890.
527
with the Psychrometer and Chemical Hygrometer.
TABLE I.
CS i Ete Ee we NEE a eel Sle we > I OE Ses eR Re ee
Weight of
Time during which Gain in weight] Variation in |vapour calcu- ITE: Dry-bulb | Wet-bulb
Experi- Dates air was aspirated eee ee of absorption- weight of test- lated from beat S : (mean of | (mean of
ment. through absorption- a vial tubes, first [pair of absorp-|psychrometer von CHOATE three three
tubes. Fe ees air. tion-tubes. | by Glaisher’s readings). | readings).
P y method
Tables. ;
cub. centim. erm. erm. erm. per cent. wie 5
1.......| 8 Jan. 1893.| 2.26 — 2.31 p.m. 5,802 "0209 + -0002 0198 —5 311 29:0
Dette’ 3 10.15 -10.19% a.m. 5,630 "0154 +0002 ‘0164 +7 20°1 20:0
Sh actiocel| a2) A 10.43 -10.14 _,, 11,552 ‘0289 +:0003 0288 —0 20°0 196
Acces geal a59 3 10.41 -10.51 ,, 11,278 0303 +0001 0297 —2 21-0 20°5
Disnegsa|c0 iy 10.20 -10.29 __,, 11,358 ‘0445 +0001 0470 +5 30°7 29'9
Ooocee alloc 3 11.2% -11.12 _,, 11,396 0481 — ‘0002 0480 —0 30°9 30°4
The ss Sy 3 10.45 -10.54 ,, 11,174 0431 +0005 0427 —1 28°6 28:1
Sie sel 9) ” 11.213-11.83 _,, 11,202 0439 +0002 ‘0448 +2 28°5 28°2
Ot line, 5 10.14 -10.23 _,, 11,302 ‘0576 — ‘0002 "0589 +2 341 33'8
WO ecesat |e ‘5 10.45 -10.54_,, 11,320 ‘0587 +0003 0583 —0 343 33°9
Acc ag LO. ‘5 10°7 -10.16 ,, 11,370 "0574. + 0004 0575 +0 347 34:2
Dees texe saelis9 ) 10.39 -10.48 __,, 11,410 0578 +:0001 ‘0603 +4 352 347
WSs coxcae( LL i 10.14 -10.23 _,, 11,428 0481 +0002 0476 —1 32'3 30°9
Lee NET at
528 Mr. Pembrey on Comparative Experiments
The aspirator used was that described in the paper pre-
viously mentioned*. The aspirating-bottles were covered
with felt, so that the temperature of the water generally
varied only a tenth or two.of a degree Centigrade, never
more than half a degree, during the period of observation.
The volume of air aspirated has always been corrected for
temperature, aqueous vapour, and barometric height.
In calculating the tension of aqueous vapour from the
chemical determinations the table given by Shawf has proved
very valuable.
The preceding Table (I.) shows that the amounts of moisture
calculated from the psychrometric readings by Glaisher’s
Tables vary, when compared with the gravimetric determina-
tions, from —5 per cent. to +7 per cent. The mean, how-
ever, is ‘0430 to ‘0426 grm., or less than +1 per cent. for
the psychrometer.
The tensions given by the chemical determinations have
been calculated, and are compared in Table II. with those
obtained from the psychrometer by means of Glaisher’s,
Haeghens’, Guyot’s, and Wild’s tables.
Nae tree Ee
Psychrometer.
Experiment Chemical 9
‘| method.
Glaisher. | Haeghens.| Guyot. Wild.
millim. millim. millim. millim. millim.
| a eee 3°45 3°20 3°44 3°45 3°47
De there i. 2-60 2-67 2°73 ORD a ee
Desctiowec way 2-49 2°36 2:58 2°56 2
7 a oe Sie 2°56 2°36 2-70 2:64 26
De Mee ose acres a1 3°83 4:01 3°98 3:93 2
Giraieseccu net 4-03 4:06 4°20 4-16 AT
Tae ae = Be 3°70 3°63 3°80 3°78 S48
eee 3°75 378 3°84 ool 3°83
es iin 2 4-87 4-85 4-84 4-82 4°83
MOR aerate at 4°95 4°85 4-84 4:82 | 4:80
1B sey Se Se ae 4°85 4-87 4°86 4-82 4°80.
DA Sees ee 4°86 4-98 4-97 4:92 5°00
WS ates ae 4°05 3°86 4°23 3°96 | 4°17
WMisanves. cone: 3°84 3°80 3°93 3°88 | 3°89
In order to make this paper more complete, the cor-
responding tables of the previous experiments are here
reproduced.
* Phil. Mag, April 1890, p. 309.
tT On Hygrometric Methods,” Phil. Trans. 1888, A. ~~
529
with the Psychrometer and Chemical Hygrometer.
e . e
CONDAAA Fw DH
oh
a
Date.
ites a
om her
We a
20 Le
Za 5;
5 Aug. 1889.
Ot
al %
oy
Des
cham
* The rubber of one of the stoppers
16 July 1889.
‘TasueE EID,
Time during
which air was
aspirated.
11.39-11.48 a.m.
11.39-11.45 a.m.
11.10-11.16 a.m.
11.6 -11.12 a.m.
11.45-11.52
12.13-12.16 p.m.
11.52-11.58 a.m.
11.48-11.54 a.m.
11.21-11.27 a.m.
WO) SIDIEAG/ AN
11.24-11,80 aa.
1L.é
52-11. 39 A.M.
Corrected
volume of
air aspirated
through
each pair.
cub. centim.
07123
5722
5723
5780
5681
5732
5707
5709
5756
5776
5731
5755
Gain in
weight of
pair I,
determina-
tion A.
0510
‘0575
‘0678
‘0583
{
Gain in
weight of
pair 2,
determina-
tion B.
erm.
‘0430*
0524
0512
0508
‘0610
0435
‘0687
‘0564
0510
‘0572
‘0675
0585
Weight of
vapour caleu-
lated from
readings of
psychrometer
by Glaisher’s
Tables, 7th ed.
erm
Percent-
age diffe-
rence of
pyschro-
meter
over
chemical
method.
per cent.
0450
0552
0520
0519
‘0600
(0452
0668
0548
0495
0552
0678
0553
+54
Dry-
bulb
(mean of
3 read-
ings).
pike
61:6
58'3
61:3
63°7
d7°9
61:5
65°6
625
63:0
64:1
61:0
64:6
Wet-
bulb
(mean of
3 read-
ings).
Variations of
test pair 3,
showing that
carrying the
tubes about
introduced no
error of
weighing.
grm.
+0001
+0002
— ‘0002
+0002
+0003
— ‘0002
— 0003
+0000
+0002
+-0001
+0002
— 0001
was found to be split on reaching the Observatory, and bei accounts for sire slight excess in
weight of this pair of tubes,
’
530 On the Psychrometer and Chemical Hygrometer.
TaBeE LV.
Psychrometer. |
; Chemical |
Experiment. | method.
Glaisher. | Haeghens.| Guyot. | Wild. |
nee Le | as ee. |
millim. millim. millim. millim. millim.
| eee ae ae 743 776 737 731 74
Bias ae hc 3 915 9°55 9 54 9°51 9°5
Ou, de acueee 8:99 9-00 8:88 8°87 89
a a 8-78 8:99 8°74 877 88
Dg ceeeencee 10°70 10°72 10°75 10°76 10:7
Coit 7:63 778 739 7:34 74
Les desea 12°15 11-72 11°78 11-80 Grd
co eer on 9-91 965 9:57 9°57 96
OS ae enes 8-90 8:68 8°45 8:43 85
LON eee 10:00 9°52 9°38 9°41 94 |
Da eae 11°82 11°84 11:93 11:93 1 eS ae
LAR sa ee 10:23 9°67 S95 9°57 9°5
pe hee ee ih | ee a
Means: 9-64 SRD 9°44 9°44 9°44
Regnault*, during his comparative experiments with the _
psychrometer and his chemical hygrometer, made a series of
determinations in which the temperature of the air was below
the freezing-point. The experiments were made in December
1846 and January 1847. The lowest temperatures during
the sixteen determinations were —6°°89 C. for the dry-bulb
and —7°:74 for the wet-bulb ; the highest —0°13 and —0%69
respectively. The chemical determination lasted from three-
quarters of an hour to one hour ; readings of the psychrometer
were taken every five minutes. 7
The results showed variations of the psychrometer over
the chemical method ranging from +11 per cent. to —3 per
cent., the mean being about +4 per cent.
In conclusion | must express my hearty thanks to Mr.
Stone, the Radcliffe Observer, who has given me every facility
to make these and the previous experiments, and has always
aided me with his advice. I must also thank his assistants,
Messrs. Wickham, Robinson, and Maclean.
* Annales de Chimie et de Physique, t. xxxvii. 1853, p. 274.
sel |
LIV. Water as a Catalyst. By R. E. Hucuss, B.A., B.Sc.,
F.CS., late Scholar of Jesus College, Oxford, Natural
Science Master, Eastbourne College *.
Ss further chemical changes have been investigated,
and the influence of the absence or presence of water on
the progress of the change has been determined. Last year
the author showed (Phil. Mag. xxxilil. p. 471) that dried
hydrogen-sulphide gas has no action on the dried salts of
lead, cadmium, arsenic, &c.; and, in conjunction with Mr. F.
Wilson, it was shown that dried hydrogen-chloride gas is
without action on calcium or barium carbonates (Phil. Mag.
poecnvep.. 117).
Silver chloride prepared in the dark, dried perfectly in an
air-bath, and then placed on a watch-glass in a desiccator
partially exhausted, was found to be not perceptibly darkened
in sunlight even after an exposure of some hours ; whereas a
rapid darkening takes place if moisture is introduced.
It isa well-known fact that paper, especially ordinary glazed
writing-paper, when moistened with a solution of potassium
iodide and exposed to the light, becomes of a brownish-violet
tint—due doubtless to the decomposition of the KI and libe-
ration of the iodine.
The author finds that the progress of this change is subject
to several conditions. A solution of potassium iodide placed
on glass or porcelain becomes brown only after an exposure
of some days. ‘This change, it is suggested, is due to either
the organic matter or the ozone in the atmosphere.
A piece of ordinary filter-paper soaked with a saturated
solution of KI was dried in the dark. When placed ona
watch-glass under a desiccator, no change took place on ex-
posure even after some days; although crystals of the salt
were formed on the paper. Moreover, generally speaking,
the wetter the paper the deeper was the tint produced. In
fact the tint was proportional to the quantity of water present.
When no water was present, then no change took place.
Further, a strip of filter-paper floated on the top of a solution
of KI for quite two hours in bright sunlight before any per-
ceptible darkening occurred, although the underside had
assumed a deep brown tint.
But this change also depends on the kind of paper used ;
* Communicated by the Author. [As some of Mr. Hughes’ results
have been anticipated by Mr. Baker (Proc. Chem. Soc. May 4, 1893,
. 129), he wishes it to be stated that the MS. was received by us on
April 21st.—Ebs. |
532 Mr. R. E. Hughes on Water as a Catalyst.
thus strips of highly glazed note-paper, ordinary filter-paper,
Swedish filter-paper, and vegetable parchment were cut,
soaked in the same KI solution, and exposed side by side to
bright sunlight. It was found that after some hours a grada-
tion of tints was thus obtained, the deepest being that on the
glazed paper, whereas the tint of the parchment was almost
imperceptible. Hence this change is perhaps due to the
traces of chlorine invariably present in glazed paper. The
depth of tint in the same paper was affected by the surface on
which the paper lies. Thus, if lying on blotting-paper the
change was very minute, slightly more perceptible on glass or
polished surfaces, and most evident when on wood or other
rough surface. ‘This chemical decomposition also took piace
in the dark but more slowly; further, once the paper was
quite dry, no perceptible deepening in tint was observed. A
solution of potassium iodide may be kept in sunlight for an
indefinite period, provided it is not exposed to the atmo-
sphere. ‘This change is doubtless due to organic matter or
ozone present in the atmosphere, but is dependent on the
presence of moisture; whereas the staining of paper by this
solution is due to the chlorine present or other constituent of
the glaze, and is also dependent on the presence of moisture.
Silver nitrate behaves closely similarly, as also to a lesser
degree does platinum chloride.
Some experiments were then made to determine the
question whether dried hydrochloric-acid gas has any action
on dry silver nitrate.
The gas was passed through a tube containing copper
filings (to remove chlorine), then through a series of drying-
tubes containing strong H,8Q,, and finally over P,O; con-
tained ina tube. This dried gas had no action on dried blue ~
litmus-paper. The silver nitrate was contained in a porcelain
boat, and had been previously heated to incipient fusion.
The gas was allowed to pass slowly through for about two
hours.
IT IE Oe a
Pe Ta OE.
ee i en ie ae Dah a Ne
Crew NES i i a EES
[ 540 ]
INDEX tro VOL. XXXV.
ACTINOMETER, on a chemical,
ee
Ammonia, on the specific heat of
, liquid, 393.
Angstrom (Prof.) on the intensity of
radiation by rarefied gases under
the influence of electric discharge,
502.
Anthracite and bituminous coal-beds,
on, 465.
Averages, on a new method of
treating correlated, 63.
Bacilli, on a possible source of the
energy required for the life of,
389.
Baily (W.) on the construction of a
colour map, 46.
Baly (KE. C. C.) on the separation
and striation of rarefied gases by
the electric discharge, 200.
Barus (Dr. C.) on the fusion con-
stants of igneous rock, 173, 296;
on the colours of cloudy conden-
sation, 315.
Basset (A. B.) on the finite bending
-of thin shells, 496.
Becher (H. M.) on the gold-quartz
deposits of Pahang, 75.
Bictite, on a secondary development
of, in crystalline schists, 150,
Blakesley (T. H.) on the differential
equation of electrical flow, 419.
Boiling-points of compounds, on the
elfect of the replacement of oxygen
by sulphur on the, 458.
Boltzmann (Prof. L.) on the equili-
brium of ws viva, 153.
Bonney (Prof. T. G.) on the Nufenen-
stock, 148; on some _ schistose
‘“‘oreenstones” and allied horn-
blendic schists from the Pennine
Alps, 149 ; on asecondary develop-
ment of biotite and of hornblende
in crystalline schists from the
Binnenthal, 150.
Books, new :—Sawer’s Odorographia,
73; Blake's Annals of British
Geology, 145; Alexander’s Treatise
on Thermodynamics, 307 ; Barus’s
Die physikalische Behandlung und
die Messung hoher Temperaturen,
310; Heydweiller’s Hulfsbuch fur
die Ausfuhrung elektrischer Mess-
ungen, 311; Lachlan’s Ele-
mentary Treatise on Modern Pure
Geometry, 462; Revue Semestri-
elle des Publications Mathéma-
tiques, 463; Bedell and Crehore’s
Alternating Currents, 534; Hol-
man’s Discussion of the Precision
of Measurements, 539.
Boron, on the properties of amor-
phous, 80.
Bosanquet (R. H. M.) on mountain-
sickness, and power and endurance,
47.
Breissig (F.) on the action of light
upon electrical discharges, 151.
Bryan (G. H.) on a hydrodynamical
proof of the equations of motion
of a perforated solid, 338.
Burton (Dr. C. V.) on plane and
spherical sound-waves of finite.
amplitude, 317 ; on the motion of
a perforated solid in a liquid, 351,
490.
Catalyst, on water as a, 531.
Chattock (A. P.) on an electrolytic
theory of dielectrics, 76.
Collins (J. H.) on the geology of the
Bridgewater district, 150.
Colour-blindness, on, 52.
Colour map, on the construction of a,
Condensation, on the eolours of
cloudy, 316.
Contact-action and the conservation
of energy, on, 134,
Cooke (J. 1.) on the mals and clays
of the Maltese Islands, 148.
INDEX. 541
Crova (M.) on the interference-
bands of grating-spectra on gela-
tine, 471.
Current, on the magnetic field of a
circular, 354.
D’Arsonval galvanometer, on high
resistances used in connexion with
the, 210.
Dielectric, on the attraction of two
plates separated by a, 78.
Dielectrics, on an electrolytic theory
of, 76.
Diffusion of substances in solution,
on the, 127.
Dispersion, on some recent determi-
nations of molecular, 204.
Dyuic equivalent of a substance,
definition of the, 267.
Karp (Miss A. G.) on the effect of
the replacement of oxygen by
sulphur on the boiling- and melt-
ing-points of compounds, 458.
Edgeworth (Prof. F. Y.) on a new
method of treating correlated
averages, 63.
Electric discharge, on the separation
and striation of rarefied gases by
the, 200; on the intensity of radi-
ation by rarefied gases under the
influence of, 502.
discharges, experiments with
high frequency, 142; on the
action of ight upon, 151.
fields, constant and varying,
experiments in, 68.
Electrical discharge, on the potential
of, 538.
flow, on the differential equa-
tion of, 419.
furnace, on a new, 313.
properties of pure nitrogen, on
the, 1
vibrations, on the disengage-
ment of heat occurring when, are
transmitted through wires, 537.
Electrochemical effects due to mag-
netization, on, 473.
Electromotive force, on the relation
of volta, to pressure, &e., 97.
Emmons (H.) on the petrography of
the island of Capraja, 312.
Energy, on radiant, 113; on contact
action and the conservation of,
134; on the distribution of kinetic,
among Kelyin’s doublets, 160; on
a possible source of the, required
for the life of bacilli, 389.
Equations of motion of a perforated
solidin liquid, on the, 338, 490.
Kquipotential lines in plates tra-
versed by currents, on a visible
representation of the, 151.
Everett (Prof. J. D.) on a new and
handy focometer, 333.
Fluorite, on the refraction of rays of
ereat wave-length in, 44.
Focometer, on a new, 333.
Foote (A. E.) on a meteoric stone
seen to fall in South Dakota, 152.
Force, on the laws of molecular,
211.
Fox (H.) on some coast-sections at
the Lizard, 466; on a radiolarian
chert from Mullion Island, 466.
Frederick (Lieut. G. C.) on the
geology of certain islands in the
New Hebrides, 467.
Friction, on liquid, 441.
Furnace, on a new electrical, 315.
Fusion constants of igneous rock, on
the, 173, 296.
Galitzine (B.) on radiant energy, 118.
Galvanometer, on high resistances
used in connexion with the
D’Arsonval, 210.
Gases, on the separation and stria-
tion of rarefied, by the electric dis-
charge, 200; on the intensity of
radiation by rarefied, under the
influence of electric discharge,
502.
Geissler’s tubes, on a property of the
anodes of, 538.
Gelatine, on the interference-bands
of grating-spectra on, 471.
Geological Society, proceedings of
the, 74, 146, 312, 464.
Glacial Drift, on the occurrence of
boulders and pebbles from the, in
oravels south of the Thames, 468.
Gladstone (Dr. J. H.) on some
recent determinations of molecular
refraction and dispersion, 204.
Gold-deposits, on the Pambula, 76;
of Pahang, on the, 75.
Goldstein (11.) on a property of the
anodes of Geissler’s tubes, 558.
Gore (Dr. G.) on the relation of
volta electromotive force to pres-
sure &e., 97.
” a a I a lt ae all Dell
542 INDEX.
Gratings, on a certain asymmetry in
Prof. Rowland’s concave, 190; in
theory and practice, on, 397.
Grating-spectra on gelatine, on the
interference-bands of, 471.
Gravity, on the daily variations of,
314,
Greenstones, on some schistose, from
the Pennine Alps, 149.
Gresley (W. S.) on anthracite and
bituminous coal-beds, 465,
Hall’s phenomenon, explanation of,
151.
Heat of vaporization of liquid hydro-
chloric acid, on the, 435.
, on the disengagement of, when
electrical vibrations are transmit-
ted through wires, 537.
Helmholtz (Prof.) on colour-blind-
ness, 52.
Heydweiller (Prof.) on Villari’s
critical point in nickel, 469; on
the potential of electrical dis-
charge, 538.
Hornblende, on a secondary develop-
ment of, in crystalline schists, 150.
Hughes (R. E.) on water as a
catalyst, 531.
Hull (Prof. E.) on the geology of
Arabia Petrea and Palestine,
146.
Hydrochloric acid, on the heat of
vaporization of liquid, 455.
Hydrolysis in aqueous salt-solutions,
on, 365 c¥,
Hygrometer, comparative experi-
ments with the dry- and wet-
bulb psychrometer and an im-
proved, 525.
Interference-bands of grating-spectra
on gelatine, on the, 471.
Tron rings split in a radial direction,
on the magnetization of, 592.
Irving (Rev. A.) on the base of the
Keuper formation in Devon, 147.
Judd (Prof. J. W.) on inclusions of
Tertiary granite in the gabbro of
Skye, 464.
Kinetic energy, on the distribution
of, among Kelvin’s doublets, 160.
Klemenéic (Dr. 1.) on the disen-
gagement of heat occurring when
electrical vibrations are trans-
mitted through wires, 537.
Lagrange’s equations of motion, on,
345, 490.
Lefevre (J.) on the attraction of two
plates separated by a dielectric, 78.
Lehmann (H.) on the magnetization
of iron rings split in a radial
direction, 592.
Light, on the diffusion of, 81; on
the action of, upon electrical dis-
charges, 151.
Liquid, motion of a perforated solid
in, 358, 490.
Lommel (E.) on a visible represen-
tation of the equipotential lines in
plates traversed by currents, 151.
Ludeking (C.) on the specific heat of
liquid ammonia, 393.
Luminons discharges in electrodeless
vacuum-tubes, on, 506.
MacGregor (Prof. J. G.) on econtact-
action and the conservation of
energy, 134.
Madsen (V.) on Scandinavian boul-
ders at Cromer, 312.
Magnetic field of a circular current,
on the, 354.
fields, constant and yarying,
experiments in, 68. 4
Magnetization of iron rings split
in a radial direction, on the, 392.
, on electrochemical effects due
to, 4738.
Mascart (M.) on the daily variations
of gravity, 314.
Melting-points of compounds, on the
effect of the replacement of oxy-
gen by sulphur on the, 458.
Meteoric stone seen to fall in South
Dakota, on a, 152.
Michigan, on the geology of the iron,
gold, and copper districts of, 74.
Minchin (Prof. G. M.) on the mag-
netic field of a circular current,
354.
Moissan (H.) on the properties of
amorphous boron, 60; on a new
electrical furnace, 513.
Molecular force, on the laws of, 211.
refraction and dispersion, on
some recent determinations of,
204.
Monckton (H. W.) on the occurrence
of boulders and pebbles from the
Glacial Drift in gravels south of
the Thames, 468.
Motion of a perforated solid in
liquid, on the, 338, 490.
Mountain-sickness, remarks on, 47.
IN DEX.
Nickel, on Villari’s critical point in,
469.
Nitrogen, on the preparation of pure,
1
Ohm’s law, on a necessary modifica-
tion of, 65,
Oxygen, on the effect of the re-
placement of, by sulphur on the
boiling- and melting-points of
compounds, 458.
Pembrey (M. S8.), comparative ex-
periments with the dry- and wet-
bulb psychrometer and an im-
proved chemical hygrometer, 525.
Perry (Prof. J.) on liquid friction,
441.
Pickering (S. U.) on the diffusion of
substances in solution, 127.
he (Dr. W.) on colour-blindness,
ae (F. D.) onthe Pambula gold-
deposits, 76.
Pressure, on the relation of volta
electromotive force to, 97.
Psychrometer, comparative experi-
ments with the dry- and wet-bulhb,
and an improved chemical hygro-
meter, 525,
Radiant energy, on, 115.
Radiation by rarefied gases under the
influence of electric discharge, on
the intensity of, 502.
Raisin (Miss C. A.) on the variolite
of the Lleyn, 312.
Refraction of rays of great wave-
length in rock-salt, sylvite, and
fluorite, on the, 35.
, on some recent determinations
of molecular, 204, 270.
Reid (C.) on a fossiliferous Pleisto-
cene oi at Stone, 469.
Rigollot (H.) on a chemical actino-
meter, 77.
Rimington (E. ©.), experiments in
electric and magnetic fields, con-
stant and varying, 68; on lumi-
nous discharges in electrodeless
vacuum-tubes, 506.
Roberts (T.) on the geology of the
district west of Caermarthen, 467.
Rock, on the fusion constants of
igneous, 173, 296.
Rock-salt, on the refraction of rays
of ereat wave-length in, 35.
Rowland (Prof. H. A.) on gratings
in theory and practice, 397.
543
Rubens (H.) on the refraction of
rays of great wave-length in rock-
salt, sylvite, and fluorite, 35.
Rudski (M. P.) on the flow of water
in a straight pipe, 439.
Rydberg (Dr. J. R.) on a certain
asymmetry - in Prof. Rowland’s
concave gratings, 190.
Salt-solutions, on hydrolysis in aque-
ous, 365.
Sanford (f.) on a necessary modifi-
cation of Ohm’s law, 65.
Shells, on the finite bending of thin,
496.
Shields (Dr. J.) on hydrolysis in
aqueous salt-solutions, 365.
Shrubsole (O. A.) on the plateau-
gravel south of Reading, 468.
Smith (F. J.) on high resistances
used in connexion with the D’Ar-
sonval galvanometer, 210.
Smith (W.), experiments in electric
and magnetic fields, constant and
varying, 68.
Snow (B. W.) on the refraction of
rays of great wave-length in rock-
salt, sylvite, and fluorite, 35.
Solid, on the motion of a perforated,
in liquid, 338, 490.
Solution, on the diffusion of sub-
stances ria Ae
Sound-waves, on plane and spherical,
of finite amplitude, 317.
Squier (Lieut. G. O.) on electro-
chemical effects due to magnetiza-
tion, 473.
Starr (J. E,) on the specific heat of
liquid ammonia, 393.
Stoney (Dr. G. J.) on a possible
source of the energy required for
the life of bacilli, 389.
Sulphur, on the effect of the re-
placement of oxygen by, on the
boiling- and melting-points of
compounds, 458.
Sumpner (Dr. W. E.) on the dif-
fusion of light, 81,
Sutherland (W.) on the laws of
molecular foree, 211.
Swinton (A. A. €.) on high
frequency electric discharges,
142,
Sylvite, on the refraction of rays of
ereat wave-length in, 43.
Teall (J. J. H.) on some coast-
sections at the Lizard, 466; on a
MRE ee ee
bn Sos ULE
IN RB EMA I ATEN SOE EAE OT | CITE EE EOI LIONEL EN 4 OI 8 MELE ETE NY LITTON SIE GE IO
en SE eapat ieaciey tee anaheim ners Serpents wees atone : 6
JA pee es
=
544 = INDEX.
radiolarian chert from Mullion
Island, 466.
Thermodynamics, on the signa of
the second law of, 124.
Thermometers, on the official testing
of, 595.
Threlfall (Prof. R.) on the electrical
properties of pure nitrogen, 1.
Tsuruta (K.) on the heat of vapo-
rization of liquid hydrochloric
acid, 435.
Vacuum-tube in a varying and in a
constant electric field, theory of a,
COT.
Vacuum-tubes, on luminous dis-
charges in electrodeless, 506.
Variolite of the Lleyn, on the, 312.
Villari’s critical point in nickel, on,
469.
Vis viva, on the equilibrium of, 153.
Volta electromotive force, on the re-
lation of, to pressure &e., 97.
Wadsworth (Prof. M. E.) on the
geology of the iron, gold, and
copper districts of Michigan, 74.
Water, on the flow of, in a str aight
pipe, 489.
—- as a catalyst, 531.
Waves, on plane and _ spherical
sound-, of finite amplitude, 317.
Wiebe (HL. F’.) on the official testing
of thermometers, 395.
END OF THE THIRTY-FIFTH VOLUME.
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