Page images
PDF
EPUB

phate fused and filled with hydrogen, was likewise heated

THE CHEMICAL NEWS. to 205° C. for twelve hours: a quantity of sulphurous acid

[blocks in formation]

Salicylic acid, with glucose, treated in the same manner, presents the same reaction in a still more decided manner.

Hippuric acid, with glucose and sulphuric acid, gives first a clear brown mixture, in which also the blood-red colour soon developes itself; then the whole mass becomes black, and evolves a large quantity of an odourless and colourless gas. This gas is not absorbed by water nor by potash, and is inflammable, burning with a blue flame: I conclude that it is chiefly oxide of carbon. As the reaction continues from this time, after the source of heat is withdrawn, the mixture soon becomes very hot, and then sulphurous acid is given off also.

was formed. (4). Two similar tubes, containing the same salt in "air," contained no sulphurous acid. (5). With dried ferrous sulphate, similarly treated, no sulphurous acid was produced at that temperature.

I intend to pursue this subject further, and to investigate the effect of nascent hydrogen on sulphuric acid of various densities, at the temperatures of their boiling-points.

This will, I expect, afford an explanation of the fact that sulphuric acid, even containing a considerable proportion of water, yields, when heated to the boiling-point with zinc, not hydrogen, but sulphurous acid.

NOTE ON THE NESSLER TEST.

By J. ALFRED WANKLYN.

IN the course of the various controversies relating to the water process frequent mention has been made of the time required for the development of the Nessler colour. According to some experimenters, a few minutes suffice for the full colouration; according to others, half an hour or more is necessary.

These differences have their origin in differences in the quality of the Nessler reagent. I have known two Nessler reagents which, although in the course of hours giving the same depths of colour with the same quantity of ammonia, required very different times for the production of the colouration. One sample of Nessler reagent gives its maximum of colour almost immediately, and another sample takes a quarter of an hour or an hour for full development.

To a great extent, these differences depend upon whether or not a sufficient quantity of solution of corrosive sublimate has been added to the finished Nessler reagents Whether the Nesslerising takes a couple of minutes, or

PRELIMINARY NOTE ON THE REDUCTION OF whether it takes an hour, is a matter of vital importance

SULPHURIC ACID BY HYDROGEN.

By G. J. WARNER, F.C.S.

FOR several years past I have used a method to avoid percussive ebullition in distillation, which I have found very satisfactory, viz., that of passing through the liquid in the retort a slow current of some inert gas which is easy of preparation. Dry air, carbonic acid, and hydrogen are those most generally applicable.

I had frequently distilled sulphuric acid in a current of air which had been previously dried over calcium chloride, but on using hydrogen I find that a large quantity of sulphurous acid is always evolved.

This reaction appears to commence at about 160° C., and the quantity of sulphurous acid formed increases with the temperature, but at no point was the decomposition complete. At temperatures near the boiling-point sulphuric acid always distilled over unchanged.

Fearing that the reduction might arise from the presence of hydrogen sulphide in the hydrogen, produced by sulphurous acid in the acid used for its preparation, I passed the gas first through a solution of lead acetate, and then over calcium chloride, when the same reaction ensued, although the lead solution was not blackened. Every precaution was taken to avoid the contact of cork or india-rubber with the acid vapour, the hydrogen being passed through a glass tube ground into the neck of the

retort.

In some measure to confirm this reaction, I heated (1) redistilled sulphuric acid in an atmosphere of hydrogen, in a sealed tube, for twelve hours, at a temperature of 205° C.: when broken, a quantity of sulphurous acid was found in the tube in the gaseous state. (2). Two similar tubes, containing the same acid in air, heated at the same time to 205° C., contained, when opened, no sulphurous acid. (3). A sealed tube, containing hydro-potassic sul

to those persons who are working the ammonia process of water analysis; and since the employment of the ammonia process has become almost universal, I have deemed it to be worth while to direct attention to the necessity of a careful preparation of the Nessler reagent. have, moreover, made arrangements with Messrs. Townson and Mercer for the supply of quick Nessler reagent at the rate of twenty shillings per litre. Those chemist. who do not feel disposed to take the trouble of making the reagent themselves have now the opportunity of buying it

[blocks in formation]

Two papers on the above subject have recently appeared in the CHEMICAL NEWS, viz., one by Mr. T. L. Paterson (vol. xxvii., p. 111), and a short review of the same by Mr. A. S. Wilson (vol. xxvii., p. 225). A somewhat lengthy discussion on the same subject has also been carried on, in the pages of the "Greenock Sugar Trade Review," between Mr. Paterson and Mr. Murphy, of Liverpool, the practical results of which seem somewhat small when compared with the amount of noise made. Some of the statements made are, to say the least of it, rather novel; but it is a pity that a scientific discussion should be allowed to degenerate into mere personal wrangling, not to speak of doggerel rhymes.

With the view of satisfying myself as to the accuracy of some of the points in dispute, I have recently made a considerable number of experiments. These have been more especially directed to the determination of the moisture in samples of new char, and the presence of organic matter soluble in water,

1

through the lid. For temperatures not over 350° F. a
glass tube of this form
is useful, the
thermometer being passed through a cork, but for higher
temperatures a plain tube is to be preferred.

apparatus, in order to determine the water by direct
A great number of experiments were made with this
weighing, some of the results of which are given below.
Two grms. heated in the air-current-

Unground.

[ocr errors]

Ground.

6.52 per cent. 7'07

At 350° F. for 15 minutes gave 6.50 per cent.
", 450°
10 m. longer "' 7'01 99
,, 500° 19 CDIAN” 7°470° 1997 719 19
B.-(1). Another sample of new char (foreign) was
subjected to the same mode of treatment.
water-bhs of the unground sample placed in the
it to In hours
3:23 per cent,010) East
Jowo decor ude til eitdiw testng 907 m I---518
beqm 2 hours..
ret: lo 4moɛ malgac

edal onenofthis replies to Mr. Paterson, Mr. Murphy
makes the somewhat startling announcement that water
with which new chan has been treated is strongly alkaline,
and will therefore dissolve appreciable quantities of organic
matter from a paper filter 2 He thus accounts for the
soluble organic matter found by Mr. Paterson in his ex-
perimentssal must confess that I, for one, have yet to learn
that the water from new charsise strongly alkaline, much
more that it will dissolve filter-paper. In order to set
aside all doubt on the subject, however, the following ex-
periment was made:5 grms. of a sample of new char
were treated with water, and the liquid filtered without
the fuse of paper, the neck of the funnel being stopped
with recently ignited asbestos. The filtrate, which was
quite colourless, and only very feebly alkaline, was care-
fully evaporated to drynesswinsa weighed platinum basin;
the residueddried at 130 C, weighed, and cautiously ig-
mited. brfEhe contents of the basin blackened quite percepe
tibly peandgrond the ignitions being completed, and the
capsule weighed, the loss was found to be 112 per cent
ara result corresponding very closely with that given by
Mr. Paterson in his paper.gniarsanoo 2013tēja ar berigedo
10 Although the moisturedin samples of old or used char
can be scorrectly determined at 212°F, it is well known
that this temperature is quite inadequate for the expulsion
of the tachole of the water from new char. In his instruc-
(2). The same quantity was placed in the air-bath.
tions for the analysis of bone black, Fresenius gives 160° At 250° F. for 15 minutes the loss was 3'92 per cent.
Caktor80° Cal(320 Ento 356°F)s as the temperature, at
30
2115350°
which the moisture should be estimated. A few years ago 450°
49 39
Dr Wallace, inga paper on “Animal Charcoal," gave it
39
as his opinion that a temperature of not less than 350° F.
was necessary: Mr. Paterson, however, considers 350° F.
much too high, vand sufficient to destroy a portion of the
organic matteras Henconsiders that five hours in the
Water-bath at 212 E. is all that is necessary, and asserts
that char, during the process of pounding, always loses
water. Now, while it is quite possible that long-continued
grinding in a warm atmosphere may have that effect, it is
difficult to understand how a porous substance like char-
coal, which retains water somewhat persistently, should
during the st
short
contra ecessary

lose some

to

re

should rather

up a slight increase. That this is really the case, the results of Mr.

as

as my own,

seem to demate. Thyments,eriments were

following

made with reference to this part of the subject:-
A.-(1). A sample of new char was taken, and one-half
reduced to powder
in tightly-corked
out and kept in

0

grms, of were

the bath, under precisely similar conditions. The

2

loss of weight was as follows(1) 20
osmin99 19791ER # Zow |
.esпow ylbiqar ti budeildungrounds bobal Ground. Y

After 1 hours
pas 24:67 per cent. 4'92 per cent.
bas Denislax
3 hours-85 od 50g ng bi
need normalexs there was no further loss in either case.
eli vd bid 901 3611,7941075 V1 100 bs bg

[ocr errors]

592): 1.2862 grme, of the same sample was heated in an
ordinary air-bath, at different temperatures, as under :-
jet 97 dodw tw,esidarebaoqo ad·
1918 9W doinw w lud of st

[ocr errors]

Unground.

120 At 3509 Fosfor 15 minutes the loss was 6:11 per cent.
#ut!&;0400°) 109, 1ɛ10 m. longer,
Mon, 450°9,5 10:
svul an500 sh,mđọ

2

[ocr errors]

6.78

6.86

7:36

[ocr errors]
[ocr errors][ocr errors][ocr errors][merged small][merged small][merged small][ocr errors][merged small][merged small][ocr errors][ocr errors][ocr errors][merged small][merged small][merged small][merged small][merged small][merged small][merged small][ocr errors][ocr errors][ocr errors][merged small][merged small][merged small][merged small][merged small][merged small][ocr errors][ocr errors][merged small][merged small][merged small][merged small][merged small][ocr errors][merged small][merged small][ocr errors][ocr errors][ocr errors][merged small][merged small][merged small][merged small][merged small][merged small][merged small][merged small][merged small][merged small][merged small][merged small][ocr errors][merged small][ocr errors][merged small][merged small][ocr errors][merged small][ocr errors][ocr errors][ocr errors][merged small][ocr errors][ocr errors][merged small]

su (3) 2 grms. of t the sample
mple were placed in a platinum-justified in concluding→→→
boat, and introduced into a glass tube about 9 inches long.
The tube was then placed in an air-bath, made for the
purpose, and one end attached to an apparatus for drying
the air previous to entering the tube. To the other end
ba weighed chloride of calcium tube v was attached, and this
again was placed in communication with one arm of a
Staedler's aspirator, by means of which a uniform and
well-regulated current of dry air could always be ob
tained. The air-bath was heated by a small Bunsen, the
temperature being registered by a thermometer passed

[merged small][ocr errors]

2. That a temperature of 212° F. is quite inadequate for the determination of the water in such samples. 3. That there is a loss on heating in the air-bath up to 300° F., and that, if heated in the air-current, there is a gain in the CaCl2 tube up to that temperature, showing that even at 350° F. the water is not completely expelled.

[ocr errors]
[merged small][merged small][merged small][ocr errors]

ON THE ACTION OF WATER ON LEAD.
By Sir ROBERT CHRISTISON, Bart.

A

[ocr errors]

THE most general results of the author's former inquiries are-1. That the purest waters act the most powerfully on lead, corroding it, and forming a carbonate of peculiar and uniform composition. 2. That all salts impede this action, and may prevent it altogether, some of them when in extremely minute proportions. 3. That the proportion of each salt required to prevent action is nearly in the inverse ratio of the solubility of the compound which its acid forms with the oxide of lead.

The effect of certain inorganic and organic ingredients of water in modifying the preservative power of the salts the author did not investigate. This has been made the subject of numerous inquiries and observations by others, chiefly, however, of a desultory nature, so, of question them much too succinctly described, and some, able accuracy,

It has been denied that water acts by reason and in the ratio of its purity; and it has even been alleged that distilled water itself does not act if really quite pure. The author has, however, invariably found the reverse to be the case, and can assign no other explanation of these statements, except some error in manipulation. For example, a very pure spring water was sent to him from the south of England, with the assurance that it had been found incapable of attacking lead; but, on making trial of it, he found it to act with an energy not inferior to that of distilled water.

It has also been stated that ordinary distilled water is apt to contain a trace of nitric or nitrous acid, from nitrates incidentally present in the water subjected to distillation; and

bonate in natural waters, the practical importance of the fact is inconsiderables ante advema ed adem The corrosive action of water upon dead bas often been confounded with other causes of corrosion, and the water has borne the blame. Thus the true action has been confounded with the corrosive actions of potent agents accidentally coming in contact with the metal in the presence of water, as, for example, when a slead pipe has been led through fresh mortar, which is frequently or permanently kept moist, or when lumps of fresh mortar have been allowed to fall upon the bottom of a lead cisternasq The true or simple action of water has not unfrequently been confounded also with the effects of galvanics action. Thus, if a lead pipe or cistern be soldered with pewter solder and not with lead, erosion takes place near: the line of junction of the solder with the leads The presence of bars of others metals crossing lead,bor bbits bofs them lying on it, will also develop the same action and some facts seem to point to the same property being possessed in a minor degree by some stony and earthly substances, This observation may explain the local erosion sometimes observed in cisterns containing hard water; since, if galvanic action be excited, it will be increased by the fact of saline matter existing more largely in these waters than in soft or comparatively pure water. 91uts19qmst aidt tedt Lastly, some observers have contradicted former statements, because under certain circumstances, which led them to anticipate no action, they nevertheless found lead in water, but only in extremely minute and unimportant proportion. The test for Aeady hydrosulphuric acid, when as to detect that metal when dissolved in ten million parts employed in the way now usually practised is so delicate

[ocr errors]

of water, or even more. Facts, however, warrant the
conclusion that the impregnation must amount to at least
ten times this quantity before water can act injúriously on
man, however long it may be used,→→Irononub sdo jedi
to das allexoq stup ei ti slidw,wo str
f. Pg in towed you isiqzomte was ni gaibang
and bortensbau of lumb
ON THE ENERGIES OF THE IMPONDERABLES,
moa 9I
WITH ESPECIAL Reference to the
ToDog of Ji gniomh
MEASUREMENT AND UTILISATION OF THEM.*
awo vm as low as
By the Rev. ARTHUR RIGG, M.AM to atlust
sew themins99 2010 201
916712nomab of m992
-Bajdua 5(Continued from p.7)on919191 diw sam
ad-on has nodes es lo won to glqmsa A .(1) --. A
of science-truths för
a few years, or read the development, stage by stage, of
branch of investigation, Satisfied of this, that,
with whatever pertinacity and show of rea
reasoning any
theory is propounded and established, it rapidly wanes.
and again have they been satisfactorily (7)

addition of a mat such was the stilled after the MEN need but watch the progress

But

acid thoroughly, yields a distillate which has no action upon lead. when the author prepared distilled water in this way, with great care to prevent the access of impurities from

any

TO

often

other sources, the only result was that the action was Astronomical and geological truths and explained, and

even stronger than that of the ordinary distilled water of the laboratory, and greater, indeed, than he had ever

before observed.

[ocr errors]

yet how soon and how rapidly has one explanation been so crushed out by another, that the first, which by its An interesting statement has been made by Dr. Nevins,authors was applauded, is by the upholders of the second to allow of a certain ridiculed. 26,29101s79qme: 10979fb is died-us vienibio of the imponderables, with which we must

to the effect that some salts appesent in water dargely, |

action going on when they are although their influence when they exist in very small occasionally The theories or allude to, but with which we are in quantities is to act as preventives. This result the author no degree further concerned, are, day by day, in a transihas sometimes obtained, and has found the action such tion state. Like the cause of solar heat, or the rotation as might prove dangerous. But its limit requires to be of the moon, they are a bloodless battle-field, on which, defined; and there is reason to suppose that the propor- with our increasing love of talking and our decreasing love tion required to permit action will be found to be retter of working, words may war day words. than is ever likely to occur in the instance of waters sriumphant victory applicable to household use.

It has also been said, but in general terms and without experimental proof, that the presence of carbonate of soda, even in a hard water, takes away the preventive in fluence of the other salts, and enables the water to dis solve lead. There appears to be some foundation for this statement; but here, too, it is necessary to fix what is the limit to such influence before its importance, can be valued. Moreover, as bicarbonate of soda appears to have no such effect, and this is the usual form of the car.

science theory may be the prelude to an ignominious defeat of the same theory the belief that he who propounds theory, to-morrow, Subject, doubtless, to many dissentient views, and uses theories solely as means or ways by v such and such facts may perhaps by which to convey ideas of how be brought about, and the actual plan in operation, he is the truly wise man. not as expressing a conviction that the way described is Those who allow themselves to dwell upon the conception 091891 26W 0760-716 90T hanist

The Cantor Lectures, delivered before the Society of Aqtm9)

and the development of theories, who build theory upon theory, who sometimes pile Ossa upon Pelion, and sometimes Pelion upon Ossa, are not unlike those whom Milton describes

"Who reasoned high
Of providence, foreknowledge, will, and fate,
Fixed fate, free will, foreknowledge absolute,
And found no end, in wandering mazes lost."

Thus it is that the decisions of one age and one day differ from those of another age and another day. Theories, we must remember, are but opinions; with opinions, as such, this course of lectures is not concerned. The facts of Nature, so far as they have yet been made apparent, or may be in process of being so, are our province. They change not. To those who have appealed to Nature direct, and brought from her exhaustless stores of knowledge some truths that men may utilise, is due the information which is to be brought before you.

The mode by which they have won this knowledge is exactly that pursued in our courts of law and equity, to arrive at the truth on one point, and on one point only. Look how long and tedious legal investigations seem, and yet in how few words the result is declared. Guilty or not guilty Verdict for the plaintiff or verdict for the defendant. One or other of these very brief phrases records the conclusion or the judgment of many days of patient labours and searchings for truths.

To not less careful questioning by men in years past, as well as now current, we owe all we know of the energies, the measurement and utilisation of which is to be a feature in these lectures. That cross-questioning of the keenest and clearest kind has been essential may be inferred from the fact that these energies are so co-related -so mutually convertible-that they merge and change, Protean-like, one into the other so instaneously that no one energy can be conveniently retained alone and in operation. They thus pass and interchange without (to our eyes) a signal from any magician's wand.

The transmutations of the imponderables are accomplished in a way that would have gladdened the eyes of the most profound alchemist, could he have seen as great transmutations in some of the material things in which he worked. For example, whenever energy is lost by resistance, heat is produced, i.e., when the resistance is perfect and complete, admitting of no intermediate state; e.g., if a wheel in machinery does not move easily, the consequence is heat, manifested on the shaft.

If, however, that energy can be converted into an intermediate state, then this state may be assumed-much as light from gas is an intermediate state between chemical affinity and heat. Do what we may, that from which energy results can neither be created nor destroyed.

In the case of blows by impact, as in the tongue of a bell, or the hammer on an anvil, or a clock, or a piano, or on a drum-head, or on a gong, then, whilst doubtless some part of this checked energy is converted into heat, yet a large portion is spent in the production of vibrations in matter, appreciable to our senses, and suggestive of vibrations in molecules, which our senses, aided by physical appliances, have not yet made visible, but which chemical changes, and what to the minds of science theorists of the present day is conclusive evidence, seem to point as similar vibrations in the invisible molecules and atoms of which it is assumed that bodies consist.

These remarks may suffice to explain that whilst to speak of estimating an "energy" is easy, yet to estimate that "energy" is an employment which tasks the keenest and most watchful faculties of the human mind, as well as claiming from human hands the production of some of their most exquisite and refined work.

[ocr errors]

The difficulty of the task results not so much from a solution of the simple problem which the words "estimate that energy convey, as from the incompetence alluded to of isolating and continuing the special energy and noting its operation. For no one of nature's energies,

be they ponderable or imponderable, is alone. Solitariness in the unseen, as well as in the seen, is no part of nature's plans.

Faraday seemed to have realised this view in great intensity when he wrote-"If, as I believe, dualities are essential to the forces, are always equal, are mutually dependent, that one cannot appear or exist without the other the proof of this would lead to many consequences of high importance to the philosophy of force generally.”*

This interlacing of energies, this co-relation, as it is called, of physical forces, whilst it knits in harmonious union energies which are nominally distinct, baffles the investigator who wishes to assign to each its share in any specific work. For example, the energy of gravity operates everywhere, and our fundamental principle in hydraulics, that fluids press equally in all directions, may be granted as a postulate. The experiments by which it can be confirmed may be and is very clearly described, but no one has ever made or can make them. Gravity never ceases to impress upon fluids a downward tendency, and so prevents an equality of pressures in all directions being established.

It may be in the interest of the Moslem faith to assert that, without visible means, Mahomet's coffin rests between earth and heaven; but, assuming the truth of the tradition, or of the fact (whichever it be), we know well that gravity operates in all its wonted intensity, and that the coffin is held there (if held at all) by the introduction of some counteracting energy, as that of magnetism.

The energy of electricity is ever passing into heatthat of heat into electricity or light. Electricity, again, appears to assume the form of vitality; and then, again, it totally fails to fulfil the vital conditions. In some animals the exhaustion of their muscular energy is consequent upon the exhaustion of their vital energy, and no electrical appliance can restore the vital energy, even though it seems to restore the muscular. Take affinity. This passes, by means unknown to us, into electricity and heat.

There is also this peculiarity amongst these energies. The work of one energy, estimated by any means known to us, gives no indication of the work of some other energy, resident or potential, in the same matter.

For example, the estimation of a drop of water by gravity standards-to speak of it as weighing so many grains-gives no indication whatever of its ability to promote affinities, to absorb and convey heat, to decompose light. And if even all these were known, there would still be no indication that upon an electrical standard of measurement its destructive effects are equal to that of a flash of lightning.

The only energies that may be said to be non-interchangeable are those of gravity and vitality. The former is enduring, the latter fleeting. The character of the one is persistence and constancy; that of the other, change and variety. Gravity may be said to be quietly resident in matter; vitality shows its presence by growth or motion.

Gravity is an energy pervading all nature, as intense in grains of sand as in the mountain; in a drop of water as in the river or the ocean. Disregarding alike the vitality of the plant or the animal-for gravity treats them as though they were as inert, indifferent, and unconscious of its presence as the soil of the garden, or the mineral under the earth-thus this energy, which is to occupy our chief consideration in the next lecture, is alone, and yet we shall find how that it has been left for recent times to tabulate its measure, to report and utilise, under the guidance of ordinary arithmetical and mathematical rules, the scientific and social consequences of the measure so established.

The other energy, that of vitality, which is to occupy

*Proc. Roy. Inst. for 1854, 6.

our attention in a future lecture, can hardly as yet be said | being presented to this new energy, there is a machine to have been measured. The time, however, is very near propelled and capable of doing mechanical work. We now when the hope will be realised; that the energy of call it mechanical energy. vitality-the mechanical, the statical, dynamical, and absolute energy, of course, is meant-may be reduced to as exact a science as those of light, heat, and electricity have recently been.

All who have questioned Nature are well aware how simply and truthfully she replies. It must, however, be steadily borne in mind that this truthfulness applies to the question and answer in their mutual relations. If the question be so put that Dame Nature has to answer in respect to the combination of two elements, and so is called upon to give a reply which is in truth the aggregate of the two, she does so. It behoves the questioner to frame his question with the utmost care, in order to eliminate what is extraneous to his purpose. All must have observed how difficult it is to frame a question which cannot be mis-read, or admit of a reply evidently based upon a view which the questioner never contemplated. For example, if the question relates to gravity, caution is needed to exclude the buoyancy and even viscosity of the air, and the centrifugal effects of the earth's rotation.

If it relate to electricity, caution is needed to exclude the most infinitesimal alloy of a metal-even a metal itself.

If it relate to vitality, caution is needed to exclude the effects of temporary exhilaration or prostration.

If it relate to affinity, caution is needed to exclude the complication of phenomena by variations in gaseous pressure or atmospheric temperature.

If it relate to heat, caution is needed to exclude peculiarly constituted substances, in their unknown and varying effects on heat from their atomic or rather molecular condition.

Although, for purposes of classification and the general distinction of the phenomena, the energies found in nature are arranged under the general energies which are prefixed to the respective lectures of this course, yet it must be borne in mind that these are verbal rather than emphatically actual distinctions. They are merely the terms recognised at the present day, and in a few years may be dismissed. The convertibility of energy just now alluded to is a phrase which conveys a clear meaning, but this convertibility is a process that cannot be followed. At one time in the science world a general principle seems to have been established in relation to it; again and again the hope fades, the principle is on no secure basis, whilst the convertibility is ever active. It may not inappropriately be asked which energy is the source of the others-which, in fact, seems to have the highest claim to be classed as the one. Doubtless, as a question of sequence, in time gravity must claim the first place, but, so far as our powers of utilising the energies of the imponderables are concerned, we are not able to appeal very hopefully to gravity. We cannot obtain the other energies from it. Gravity refuses to be converted; its political principles are of the type which permits no change. Nature's No. I must be gravity; man's No. 1 affinity. For example, oxygen and hydrogen manifest their affinities in obedience to some inexplicable law. They enter into what is called combination, and in so doing manifest one form of energy to which the name of the "energy of affinity" is given. But in the transition state-in the act of obeying the very imperfectly known laws of affinityanother energy of a different name and character appears, viz., heat. Evidence of the power of this energy-heatis furnished to tests very different to those which may be applied to the energy of affinity. The heat is presented to the thermo-electric pile, and that a great change in the mode of its energy has taken place is obvious from the results it produces at a distance; to this new form of energy we give the name of electricity. By a species of magic, electricity has called forth an energy to which is given the name of magnetism. Suitable circumstances

Thus, by change superposed on change, the energy of an imponderable has been converted into that energy of the ponderable to which we are indebted for all, or nearly all, of arts, manufactures, and commerce.

The two imponderable energies into which chemical affinity cannot be converted are vitality and gravity. These two may, as we shall hereafter find, assume the form of the others-the others cannot assume their forms —at least not in any plain and honest sense. Except in these two physical energy is a visible reproduction of the invisible doings of chemical affinity.

Simple as this process of transformation may appear, and convenient and useful as the suddenness of the change may be, it cannot be denied that to the investigator it is perplexing. Men, however, labour on, each perhaps winning a little from the unknown, and adding it to the known. Thus, although "hills peep o'er hills, and Alps on Alps arise," yet men of varied resources and patient perseverance have won those invaluable treasures of measurement and utilisation from the imponderables and unseen which give the title to this course of Cantor Lectures.

[ocr errors]

Even Livingstone has not shown a more noble resolve "to conquer or to die" than have those to whom we are indebted for all we know touching the modes of measuring the energies of gravity, vitality, affinity, electricity, light, and heat.

As illustrations of the difficulties of the tasks before them, it may suffice, in this introductory stage, briefly to observe that:

Galvanic currents may escape notice unless the intensity of terrestrial magnetism be neutralised.

Diamagnetism and the magneto-electric spark escape notice, unless a large number of galvanic cells or their equivalent is used.

What was called the " smell of electricity" led Schonbein to the discovery of "ozone," a remarkable product, and one whose energies are yet unknown, although being slowly but surely developed.

That a vibrating magnetising needle came to rest sooner in the neighbourhood of a copper plate, now called a damper, then when the plate was away, led to the discovery of the induction of electric currents by Faraday.

Opinions from telescopic appearances of the size of the stars led to an idea that their discs differed; the phenomenon has been found to be due to the diffraction of light.

The velocity of sound was calculated, making due allowance for the direction of the wind; in recent years it has been found that the heat developed by one particle of air striking another, must be taken into account.

(To be continued.

Royal School of Mines.-At a meeting of the Council, held on Saturday, July 5, the following gentlemen received the diploma of Associate of the Royal School of Mines:-Mining and Metallurgical Division-E. Jackson J. A. Griffiths, C. Law. Mining Division-A. G. Phillips. Metallurgical Division-J. W. Westmoreland, S. W. Davies, J. C. Jefferson, H. S. Bell. Geological DivisionG. Smith. The following scholarships and prizes were awarded:-The two Royal scholarships of £15 each, for first year's students, to Mr. W. Carter and Mr. A. J. Meeze. For second year's students-His Royal Highness the Duke of Cornwall's scholarship of £30 for two years, to Mr. C. Lloyd Morgan; and the Royal scholarship of £25, to Mr. S. A. Hill. The Edward Forbes medal and prize of books, for natural history, to Mr. G. Smith. The De la Beche medal and prize of books, for mining, to Mr. Edgar Jackson. The Murchison medal and prize of books, for geology, to Mr. C. Lloyd Morgan.

« PreviousContinue »