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which furnishes the above calculated numbers; and by their comparison with the observed ones, the probable errors are―

in the absolute term of d+1'94;

in the coefficient of t in d +0'.2932;

in the coefficient of t in d±0'·030669.

according to

If, now, instead of employing the variations (m, x), or observations in the years 1837 and 1838, we assume (1) that the periodical dependence between this function and the date t consists in always changing each parameter proportionally to its mean or primitive value, and then (2) that, as General Sabine has proved, the whole function has nearly reached a maximum in all moments marked by t=48+n.9.5, n being an integer, and (3) that, according to the same philosopher, the least and the largest amount of corresponding variations are approximately as 1:14, then, marking the function of t, m, x which in each case must be substituted for 4, and C a function of M and X, we shall have

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To each of the preceding values of d must therefore be added

4—= {0·1163-0-1472. sin [720° (t-45-625)]}.

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By executing this operation, I found that the reduced observations are best represented by

(C*)

d=18° 8.43+0.26831. t-0.070652.ť,

and that, though scarcely differing from (IV.), this expression is preferable, because the probable error of each of its terms is by nearly of its former value smaller than the corresponding one in (IV.)

As the expression (C*) is identical with

(C)

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d=18° 8'-68-0'-070652{t-1.899},

we see that, according to my observations, the west declination at the place in question arrived in 1801·899 at a maximum of 18° 8'68.

Putting off for a further article some more general observations on the secular changes of terrestrial magnetism, I briefly resume, as results of my nearly forty years' observations, that for

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there have been-between 1805 and 1864,

Horizontal intensity=T=1·79183-0.000048119 {t-59·930}'; between 1806 and 1863,

Inclination=i=66° 26'09+0′·018931 {t-110-543}2;

and between 1731 and 1864,

West declination=d=18° 8'68-0'070652 {t-1.899}2;

all results being meant to be just for the date 1800+t in years of the Gregorian epoch.

N.B. It seems not unworthy of remark, that no evidence of the existence of a third term in the expression for any one of the three phenomena results from the above-mentioned observations; and this, though partly due to the inevitable imperfections of the observations, makes it highly probable that a man's lifetime, and even a century is but a very small part of the secular period of terrestrial magnetism.

II. "On the Action of Chlorine upon Methyl." By C. SCHORLEMMER, Assistant in the Laboratory of Owens College, Manchester. Communicated by Professor RoscoE, F.R.S. Received April 5, 1864.

In a paper published in the Journal of the Chemical Society, New Ser. vol. i. p. 425, I pointed out the great interest which attached to the study of the lower terms of hydrocarbons, known by the name of the "alcohol radicals," inasmuch as the question of the chemical constitution of these bodies requires to be more definitely settled.

Having been aided in these researches by a grant from the Council, I beg to lay before the Royal Society the results of an investigation on the action of chlorine upon methyl, which are as unexpected as they are decisive.

Equal volumes of chlorine and of methyl were exposed in strong wellcorked bottles, holding from two to three litres, to diffused daylight in the open air at a temperature of about 5° C. The methyl was prepared according to Kolbe's method, by electrolysis of a concentrated solution of acetate of potassium, and carefully purified by washing with a solution of caustic potash and concentrated sulphuric acid. The colour of the chlorine disappeared rather quickly; colourless oily drops condensed on the the sides of the bottles, and collected after some time on the bottom as a mobile liquid, the greater part of which volatilized again when the bottles were brought into a warm room. Hence it appears that by the action of one volume of chlorine upon one of methyl, substitution-products are formed, consisting chiefly of a volatile liquid, the boiling-point of which ies between 5° and 15° C. In order to collect these products, the bottles were heated till all the liquid had volatilized, and then opened, with the mouth downwards, under a hot concentrated solution of common salt, to which some caustic soda was added in order to quicken the absorption of

VOL. XIII.

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the hydrochloric acid, of which half the volume of gas contained in the bottles consisted. The bottles were then taken out of the liquid, placed in an upright position, and the mouth provided with a doubly perforated cork, into one opening of which a siphon fitted. Through this siphon a hot concentrated solution of common salt slowly ran in, whilst the gas thus displaced escaped by a bent tube and was condensed in a small tube receiver, surrounded by a mixture of ice and salt. The liquid thus obtained was left for some hours in contact with a piece of solid caustic potash, in order to remove moisture and the last traces of hydrochloric acid. Subjected to distillation, the liquid began to boil at 11° C., and the boiling-point rose slowly to 30° C., at which temperature two-thirds of the liquid had come over. On continuing the fractional distillation for some time longer, the distillate yielded a few grammes of a colourless mobile liquid, boiling between 11° and 13° C., which, as the following analysis and vapour-density determinations prove, is chloride of ethyl, C, H, Cl. The boiling-point of the liquid agrees with that of this compound, and it possesses the strong peculiar smell and the property of burning with a white, luminous, green-bordered flame, characteristic of the chloride of ethyl.

I. Analysis:

(1) 0-4245 grm. of the substance gave 0.5670 grm. of carbonic acid and 0-3025 of water.

(2) 0.1810 grm. of the substance gave 0.3855 grm. of chloride of silver and 0.0165 grm. of metallic silver.

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II. Determination of the vapour-density according to Gay-Lussac's

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Vapour-density calculated from these numbers.... 2.245.

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which numbers give the vapour-density 2.235, whilst the theoretical vapour-density of chloride of ethyl is 2.233.

The boiling-point of the residue left after the first distillation rose quickly up to 60° C., whilst nearly the whole distilled over between this temperature and 70° C. By a few more fractional distillations of this latter portion, monochlorinated chloride of ethyl, C, H, Cl, boiling between 62° and 65° C., was isolated.

0.1270 grm. of this compound gave 0.3530 grm. of chloride of silver and 0.0095 grm. of metallic silver, which corresponds to 71.43 per cent. of chlorine, whilst the formula requires 71.71 per cent.

Eight litres of methyl yielded about 8 grammes of the mixed chlorides, or only about one-third of the theoretical quantity of chloride of ethyl which should have been obtained. This is easily explained by the volatilization of the liquid, and its solution in large quantities of water, as well as by the formation of higher substitution-products, in consequence of which a considerable quantity of methyl is left uncombined.

10

16

21

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From these results it appears that the lowest term of the series of alcohol radicals behaves with chlorine exactly in the same manner as I have shown in the paper above referred to is the case with its homologues ethyl-amyl; C, H1 (which gives chloride of heptyl, C, H1, Cl), and amyl, Co H22 (from which chloride of decatyl, C1, H2, Cl, is obtained). If an excess of chlorine is avoided, the principal products consist of the chlorides of monatomic radicals containing the same number of atoms of carbon as the original hydrocarbon contained, whilst at the same time chlorine substitution-products of these chlorides are formed in smaller quantities.

2

16

As there is no reason why those terms of the series which are placed between C, H, C, H18, C10 H22 should show a different deportment, it becomes obvious that, beginning with marsh-gas, CH,, the lowest term in the series C, H2n+2, the most simple of all hydrocarbons, and one which can easily be obtained from its elements, we are now not only in a position to prepare all the members of this series, but likewise to build up by simple synthesis the series of mono-, di-, and polyatomic alcohols, acids, compound ammonias, ethers, &c. &c. of which each of the marsh-gas hydrocarbons forms the starting-point.

III. "On the Calculus of Symbols (Fifth Memoir), with Applica tions to Linear Partial Differential Equations, and the Calculus of Functions." By W. H. L. RUSSELL, Esq., A.B. Communicated by Professor STOKES, Sec. R.S. Received April 7, 1864.

In applying the calculus of symbols to partial differential equations, we find an extensive class with coefficients involving the independent variables which may in fact, like differential equations with constant coefficients, be

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solved by the rules which apply to ordinary algebraical equations; for there are certain functions of the symbols of partial differentiation which combine with certain functions of the independent variables according to the laws of combination of common algebraical quantities. In the first part of this memoir I have investigated the nature of these symbols, and applied them to the solution of partial differential equations. In the second part I have applied the calculus of symbols to the solution of functional equations. For this purpose I have worked out some cases of symbolical division on a modified type, so that the symbols may embrace a greater range. I have then shown how certain functional equations may be expressed in a symbolical form, and have solved them by methods analogous to those already explained.

The Society then adjourned to Thursday, May 12th.

May 12, 1864.

Major-General SABINE, President, in the Chair.

In accordance with the Statutes, the names of the Candidates recommended by the Council for election into the Society were read, as follows:

Sir Henry Barkly, K.C.B.
William Brinton, M.D.
T. Spencer Cobbold, M.D.
Alexander John Ellis, Esq.
John Evans, Esq.

William Henry Flower, Esq.
Thomas Grubb, Esq.

Sir J. Charles Dalrymple Hay, Bart.

William Jenner, M.D.

Sir Charles Locock, Bart., M.D.
William Sanders, Esq.

Col. William James Smythe, R.A.
Lieut. Col. Alexander Strange.
Robert Warington, Esq.
Nicholas Wood, Esq.

The following communications were read:

I. "Second Part of the Supplement to the two Papers on Mortality published in the Philosophical Transactions in 1820 and 1825.” By BENJAMIN GOMPERTZ, F.R.S. Received March 30, 1864.

(Abstract.)

The objects of this paper are various; but the subject appears to the author more especially important in consequence of the state of competition among assurance establishments, which he holds to be injurious to the interest of those valuable establishments, and to those of the assuring population. The author's purpose in this paper is greatly to extend the modes of calculating valuations, and to improve the methods of calculation hitherto used by actuaries, which are in many cases very laborious, and in some almost impracticable. This part commences with observations on the inge

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