CHAPTER IV

“PHLOGISTICATED AIR” INVESTIGATED BY CAVENDISH--HIS

DISCOVERY OF THE COMPOSITION OF WATER

While Lavoisier was engaged in experiments on oxygen, Cavendish,

too, was devoting his attention to the constituents of air, but in

a somewhat different manner. His early experiments led him to the

discovery of the composition of water; and it has already been pointed

out how necessary a knowledge of the true nature of hydrogen is to the

understanding of the phenomena of combustion. His second paper deals

with the inactive constituent of air, the mephitic portion, now known

as nitrogen or azote. But before considering these, a sketch of his

life will prove of interest.

The Honourable Henry Cavendish was a very singular man, retiring and

uncommunicative to a degree; hence little is known of his early life.

He was the elder son of Lord Charles Cavendish, who was the third son

of the second Duke of Devonshire. His only brother, Frederick, was

also an eccentric, but a very benevolent man, and the two brothers,

though they seldom met, lived on excellent terms with each other. Henry

Cavendish was born at Nice in October 1731. His mother died when he

was two years old. Nothing is known of his childhood and youth, save

that he attended Hackney School from 1742 to 1749, and that he went to

Cambridge in the end of 1749, and remained till 1753, without taking a

degree. After leaving Cambridge, it is supposed that he lived in London

for ten years. It is known that his allowance from his father amounted

to £500 a year, and that his rooms were a set of stables fitted up

for his accommodation. It is probable that this was his own choice,

and that he made use of them chiefly as a laboratory and a workshop.

Although at his father’s death and by the legacy of an aunt he acquired

a large fortune, he never spent more than a fraction of it. He left

more than a million sterling to his relative, Lord George Cavendish;

but they saw each other only once a year, and the interview seldom

lasted more than ten minutes. The writer of his obituary notice, M.

Biot, epigrammatically said:--“Il était le plus riche de tous les

savans, et le plus savant de tous les riches.”

[Illustration: H. Cavendish]

He was a regular attendant at the meetings of the Royal Society, of

which he was made a Fellow in 1760, and was a constant diner at the

Royal Society Club. It is said that he used to talk to his neighbour at

table so long as others did not join in the conversation; but if the

conversation took a general turn, he was silent.

His death took place in February 1810, and was as solitary as his

life. It is related by his servant that Cavendish, on feeling his end

approaching, dismissed him from the room, telling him to come back in

half an hour. He disobeyed instructions, and, being anxious, found some

pretext to enter the room. Cavendish ordered him away in a voice of

displeasure; and on returning, the man found his master dead.

Such a life demands our pity; yet, if an object of human life is to

give pleasure to its possessor, we can hardly say that Cavendish’s was

a failure. Ordinary mortals have a craving for the sympathy of their

fellows; Cavendish appears to have been devoid of any such sensation.

Indeed, his experiments were in many cases not published until long

after they had been made. He appears to have carried on his work for

his own information, and to have been indifferent to the impression

which his labours made on his fellow-men. Yet his inquiries cover a

more extensive field than those of almost any other man of science.

They begin with experiments on arsenic, by which he endeavoured to

determine the difference between the element arsenic and its two

oxides. He held that arsenic acid was more thoroughly “deprived of

phlogiston” than arsenious acid (_i.e._ more highly oxidised); and

on the same occasion he studied the effect of the addition of air to

nitric oxide, produced by the action of nitric acid on the element

arsenic and on arsenious oxide. His next experiments related to heat;

and had he published them, he would doubtless have anticipated Black in

his discovery of latent heat. His paper on “Factitious Airs,” published

in the _Philosophical Transactions_ for 1766, deals with the properties

of hydrogen, carbon dioxide, and the gases produced by the destructive

distillation of organic substances. As we shall see later, he supposed

that hydrogen, generated by the action of acids on metals, came out of

the metal, and was an unknown principle in combination with phlogiston,

if indeed it was not phlogiston itself; and this idea is not absurd,

for many metals, and indeed a very large number of minerals, evolve

hydrogen when heated, the gas having been “occluded” in their pores.

In 1772 he communicated privately to Dr. Priestley the results of a

series of experiments dealing with nitrogen. To prepare it, he passed

air repeatedly over red-hot charcoal, and absorbed the resulting

carbon dioxide in potash. The residue was nitrogen. His description

of it is:--“The specific gravity of this air was found to differ very

little from that of common air; of the two it seemed rather lighter.

It extinguished flame, and rendered common air unfit for making bodies

burn in the same manner as fixed air, but in a less degree, as a candle

which burned about 80 seconds in pure common air, and which went out

immediately in common air mixed with 6/55ths of fixed air, burned about

26 seconds in common air mixed with the same proportion of this burnt

air.”[23] He named it, as usual, “mephitic air,” and it is certain that,

although Cavendish did not publish his results, his discovery was

not later in date than Rutherford’s. Dealing next with the phenomena

observed when that curious fish, the torpedo, produces shocks, he

ascribed them to the discharge of electricity, and he was the first

to distinguish between intensity, or potential, and quantity of

electricity, a distinction now familiar to all.

It was in 1777 that he commenced his beautiful “Experiments on Air,”

the first account of which was published in 1783. They led to the

discovery of the constant quantitative composition of the atmosphere,

of the compound nature of water, and of the composition of nitric acid,

and pointed the way to the recent discovery of argon.

In determining the composition of the atmosphere, Cavendish made use of

nitric oxide in presence of water, as a means of removing oxygen. This

process, originally devised by Mayow, was rediscovered by Priestley,

who employed it to ascertain the “goodness” of various samples of

air; in Cavendish’s hands it became an accurate quantitative method.

The title of his paper, published in the _Philosophical Transactions_

for 1783, is “Of a new Eudiometer.” The term “eudiometer,” signifying

“measurer of goodness,” was devised when it was supposed that ordinary

air presented considerable variations in its power of supporting

respiration and combustion, according to the seasons, and according

to the place from which it was collected. Dr. Ingenhousz had found a

greater absorption when air from near the sea-coast was tested by

Priestley’s method with nitric oxide, than when town-air was employed;

and he ascribed the salubrious nature of sea-air to its being richer

in “vital air.” The Abbé Fontana, too, had made similar experiments,

and had come to similar conclusions. Cavendish modified Fontana’s

apparatus, rendering it capable of giving more accurate results; and

during the last half of the year 1781 he analysed the air collected on

sixty days, some fine, some wet, and some foggy. He also collected air

from different localities, sometimes at Marlborough Street, sometimes

at Kensington, which was then a country village. The results of his

analyses establish as the composition of air, freed from carbon dioxide

by potash:

79·16 per cent of phlogisticated air (nitrogen).

20·84 per cent of dephlogisticated air (oxygen).

This result does not differ materially from those obtained by the best

modern analyses, which give, within very small variations:

79·04 per cent of nitrogen and argon,

20·96 per cent of oxygen,

after absorption of carbon dioxide, ammonia, and water-vapour.

In the following year, 1784, Cavendish published the first of his great

memoirs, entitled _Experiments on Air_. His experiments were made

principally “with a view to find out the cause of the diminution which

common air is well known to suffer by all the various ways in which it

is phlogisticated, and to discover what becomes of the air thus lost or

condensed.”

Cavendish chose processes for “phlogisticating” air in the course of

which no fixed air should be produced. He therefore avoided the use of

animal and vegetable materials, and confined himself to combustibles,

such as sulphur or phosphorus, to the calcination of metals, the

explosion of inflammable air, and the mixture of nitrous air. He adds

as a suggestion, “Perhaps it may be supposed that I ought to add to

these the electric spark; but I think it much more likely that the

phlogistication of the air, and production of fixed air, in this

process is owing to the burning of some inflammable matter in the

apparatus.” We shall see later what magnificent results arose from this

last mode of “phlogisticating” air.

He begins with an account of a repetition of an experiment of Mr.

Waltire’s, related by Priestley, in which a mixture of hydrogen and air

was exploded in a copper vessel, with the result that they observed

a loss of a few grains in weight; it is also stated by Waltire that

if the explosion took place in a glass vessel, it became dewy, “which

confirmed an opinion he had long entertained, that common air deposits

its moisture by phlogistication.” But Cavendish, using a glass vessel

of much greater capacity than Waltire’s, could remark no change of

weight; and he concluded that 423 measures of hydrogen, or “inflammable

air” as he named it, are “nearly sufficient to completely phlogisticate

1000 of common air, and that the bulk of the air remaining after the

explosion is then very little more than ⅘ths of the common air

employed; so that, as common air cannot be reduced to a much less bulk

than that, by any method of phlogistication, we may safely conclude

that, when they are mixed in this proportion and exploded, almost all

the inflammable air, and about ⅕th part of the common air, lose their

elasticity, and are condensed into the dew which lines the glass.

“The better to examine the nature of this ‘dew,’ 500,000 grain measures

of inflammable air were burnt with about 2½ times that quantity of

common air, and the burnt air made to pass through a glass cylinder 8

feet long and about ¾ of an inch in diameter, in order to deposit the

dew”. “By this means upwards of 135 grains of water were condensed in

the cylinder, which had no taste or smell, and which left no sensible

sediment when evaporated to dryness, neither did it yield any pungent

smell during the evaporation; in short, it seemed pure water”. “And

by this experiment it appears that this dew is plain water, and

consequently that almost all the inflammable and about ⅕th of the

common air are turned into pure water.”

But on firing little by little a mixture of “dephlogisticated air” or

oxygen, obtained from red precipitate (that is, mercuric oxide prepared

by heating the nitrate), with twice its volume of “inflammable air” or

hydrogen, the resulting water was acid to the taste, and on evaporation

with alkali gave a small quantity--about 2 grains--of nitre. Cavendish

suspected that the acid came from the nitrate of mercury in his

red precipitate, and, to test this, procured his oxygen from other

sources--from red-lead and sulphuric acid, and from the leaves of

plants--but still with the same result; nitric acid was formed.

Repeating the experiment so as to have present an excess of hydrogen,

he found that no acid was produced.

“From the foregoing experiments it appears that when a mixture of

inflammable and dephlogisticated air is exploded in such proportion

that the burnt air is not much phlogisticated, the condensed liquor

contains a little acid, which is always of the nitrous kind,

whatever substance the dephlogisticated air is procured from; but

if the proportion be such that the burnt air is almost entirely

phlogisticated, the condensed liquor is not at all acid, but seems pure

water, without any addition whatever; and as, when they are mixed in

that proportion, very little air remains after the explosion, almost

the whole being condensed, it follows that almost the whole of the

inflammable and dephlogisticated air is converted into pure water.” The

quantity of uncombined gas was so small that it must be regarded as an

impurity. “There can be little doubt that it proceeds only from the

impurities mixed with the dephlogisticated and inflammable air, and

consequently that if those airs could be obtained perfectly pure, the

whole would be condensed.”

The next paragraph is interesting. “During the last summer also [of

1781] a friend of mine gave some account of them [these experiments]

to Mr. Lavoisier, as well as of the conclusion drawn from them, that

dephlogisticated air is only water deprived of phlogiston; but at

that time, so far was Mr. Lavoisier from thinking any such opinion

warranted, that, till he was prevailed upon to repeat the experiment

himself, he found some difficulty in believing that nearly the whole of

the two airs could be converted into water.”

And next comes an important deduction. “Phlogisticated air appears

to be nothing else than the nitrous acid united to phlogiston; for

when nitre is deflagrated with charcoal, the acid is almost entirely

converted into this kind of air.” This is the first statement of the

true relation between nitrogen and nitric acid; we should now state the

matter by the expression, “Nitrogen is nothing else than nitric acid

deprived of oxygen.” And the further deduction is made that “it is

well known that nitrous acid is also converted by phlogistication

into nitrous air, in which respect there seems a considerable analogy

between that and the vitriolic acid; for this acid, when united to a

smaller proportion of phlogiston, forms the volatile sulphurous acid

and vitriolic acid air, both of which, by exposure to the atmosphere,

lose their phlogiston, though not very fast, and are turned back

into the vitriolic acid; but when united to a greater proportion

of phlogiston, it forms sulphur, which shows no signs of acidity.”

“In like manner the nitrous acid, united to a certain quantity of

phlogiston, forms nitrous acid and nitrous air, which readily quit

their phlogiston to common air; but when united to a different, in

all probability a larger quantity, it forms phlogisticated air, which

shows no signs of acidity, and is still less disposed to part with its

phlogiston than sulphur.”

But the origin of the acid in water made from inflammable and

dephlogisticated air was still unexplained. To settle this point

Cavendish added to an explosive mixture of oxygen and hydrogen a tenth

of its volume of nitrogen, and found that the water was much more

strongly acid; and if hydrogen was much in excess, a still greater

amount of nitric acid was produced. After relating these experiments he

proceeds:--

“From what has been said there seems the utmost reason to think that

dephlogisticated air is only water deprived of its phlogiston, and

that inflammable air, as was before said, is either phlogisticated

water or else pure phlogiston, but in all probability the former.” In

a foot-note he gives his reason for the choice, viz. that it requires

a red-heat to cause hydrogen and oxygen to combine, while nitrous air

combines with oxygen at the ordinary temperature; now, if hydrogen

were pure phlogiston, one would expect it to combine more readily than

nitrous gas, which has been shown to be a compound of nitric acid with

phlogiston. It seems inexplicable that dephlogisticated air should

refuse to unite at the ordinary temperature with pure phlogiston, when

it is able to extract it from substances with which it has an affinity.

Hence it is unlikely that hydrogen is phlogiston itself.

And a few paragraphs farther on Cavendish very nearly discards the

phlogistic theory by this statement: “Instead of saying air is

phlogisticated or dephlogisticated by any means, it would be more

strictly just to say, it is deprived of, or receives, an addition of

dephlogisticated air; but as the other expression is convenient, and

can scarcely be considered as improper, I shall still frequently make

use of it in the remainder of this paper.”

And now we come to the consideration of Lavoisier’s new theory, and

its rejection in favour of the old one of phlogiston. It is curious to

follow the reasoning which made such an exceptionally acute thinker as

Cavendish deliberately reject the true explanation. Cavendish first

states his results in Lavoisier’s terms:--

“According to this hypothesis, we must suppose that water consists

of inflammable air united to dephlogisticated air; that nitrous air,

vitriolic acid air (sulphur dioxide), and the phosphoric acid are

also combinations of phlogisticated air, sulphur, and phosphorus with

dephlogisticated air; and that the two former, by a further addition

of the same substance, are reduced to the common nitrous and vitriolic

acids; that the metallic calces consist of the metals themselves united

to the same substance, commonly, however, with a mixture of fixed air;

that on exposing the calces of the perfect metals to a sufficient

heat, all the dephlogisticated air is driven off, and the calces are

restored to their metallic form; but as the calces of the imperfect

metals are vitrified by heat, instead of recovering the metallic

form, it should seem as if all the dephlogisticated air could not be

recovered from them by heat alone. In like manner, according to this

hypothesis, the rationale of the production of dephlogisticated air

from red precipitate is, that during the solution of the quicksilver

in the acid and the subsequent calcination, the acid is decompounded,

and quits part of its dephlogisticated air to the quicksilver, whence

it comes over in the form of nitrous air, and leaves the quicksilver

behind united to dephlogisticated air, which, by a further increase

of heat, is driven off, while the quicksilver resumes its metallic

form. In procuring dephlogisticated air from nitre, the acid is also

decompounded; but with this difference, that it suffers some of its

dephlogisticated air to escape, while it remains united to the alkali

itself in the form of phlogisticated nitrous acid. As to the production

of dephlogisticated air from plants, it may be said that vegetable

substances consist chiefly of three different bases, one of which

[hydrogen], when united to dephlogisticated air, forms water; another

[carbon] fixed air; and the third phlogisticated air [nitrogen]; and

that, by means of vegetation, each of these substances are decomposed,

and yield their dephlogisticated air; and that, in burning, they again

acquire dephlogisticated air, and are restored to their pristine form.

“It seems, therefore, from what has been said, as if the phenomena of

nature might be explained very well on this principle, without the help

of phlogiston; and indeed, as adding dephlogisticated air to a body

comes to the same thing as depriving it of its phlogiston and adding

water to it, and as there are perhaps no bodies destitute of water,

and as I know no way by which phlogiston may be transferred from one

body to another, without leaving it uncertain whether water is not

at the same time transferred, it will be very difficult to determine

by experiment which of these opinions is the truest; but as the

commonly-received principle of phlogiston explains all phenomena, at

least as well as Mr. Lavoisier’s, I have adhered to that.”

“Another thing which Mr. Lavoisier endeavours to prove is that

dephlogisticated air is the acidifying principle. From what has been

explained, it appears that this is no more than saying that acids

lose their acidity by uniting to phlogiston, which, with regard to

the nitrous, vitriolic, phosphoric, and arsenical acids, is certainly

true”. “But as to the marine acid and acid of tartar, it does not

appear that they are capable of losing their acidity by any union with

phlogiston.”

Here Cavendish does not consider the question of gain of weight on

loss of phlogiston, or if he does, he must ascribe it to simultaneous

entry of water. And experimental research at that time was not far

enough advanced to enable him to decide finally as to the truth of this

hypothesis.

In his next memoir, read before the Royal Society on June 2nd, 1785,

Cavendish relates experiments on the passage of electric sparks through

air, the experiment having first been tried by Priestley. Priestley

says:[24]--“Lastly, the same effect [_i.e._ the diminution of the volume

of common air], I find, is produced by the _electric spark_, though I

had no expectation of this event when I made the experiment.” And

again:--“At the time of my former publication, I had found that taking

the _electric spark_ in given quantities of several kinds of air had a

very remarkable effect on them, that it diminished common air and made

it noxious, making it deposit its fixed air exactly like any phlogistic

process; from whence I concluded that the electric matter either is or

contains phlogiston.”

Cavendish had mentioned this process casually as one of the methods of

phlogisticating air; in beginning his second paper he says:--“I now

find that, though I was right in supposing the phlogistication of the

air does not proceed from phlogiston communicated to it by the electric

spark, and that no part of the air is converted into fixed air; yet

that the real cause of the diminution is very different from what I

suspected, and depends upon the conversion of phlogisticated air into

nitrous acid.” The apparatus he used was very simple. It consisted

of a glass siphon filled with mercury, each leg dipping into a glass

likewise containing mercury; the air was admitted by a gas-pipette into

the bend of the siphon, and on connecting the mercury in one of the

glasses with a ball placed near the prime conductor of an electric

machine, and the other with the earth, sparks could be made to pass

from the mercury in one limb to that in the other.

The product obtained by passing sparks through air in this manner

turned litmus red, and gave rise to no cloud in lime-water, while the

air was reduced to two-thirds of its original volume; nor did the

lime-water give a precipitate on introducing some fixed air, this

showing that it had been saturated by an acid. It was found, too, that

“soap-lees,” or solution of caustic potash, if present, diminished

the volume more rapidly than did lime-water; and repeated trials

proved that “when five parts of pure dephlogisticated air were mixed

with three parts of common air, almost the whole of the air was made

to disappear.” The nitrate of potassium thus produced caused paper

soaked in it and dried to deflagrate; and it contained no sulphuric

acid. “There is no reason to think that any other acid entered into it

except the nitrous.” But it gave a precipitate with silver nitrate;

and Cavendish, suspecting that this was silver nitrite, prepared some

potassium nitrite by heating the nitrate; on comparing the white

precipitate which this solution gave with silver nitrate with that

obtained from his “soap-lees,” he found them identical. There was

therefore no “muriatic acid” present, which would have yielded chloride

of silver, of appearance somewhat similar to the nitrite.

As it had previously been shown to be probable that phlogisticated

air is nitrous air united with phlogiston, and that nitrous air is

nitric acid united with phlogiston, “we may safely conclude that in

the present experiments the phlogisticated air was enabled, by means

of the electric spark, to unite to, or form a chemical combination

with, the dephlogisticated air, and was thereby reduced to nitrous

acid, which united to the soap-lees and formed a solution of nitre; for

in these experiments the two airs actually disappeared, and nitrous

acid was actually formed in their room”. “A further confirmation of

the above-mentioned opinion is that, as far as I can perceive, no

diminution of air is produced when the electric spark is passed either

through pure dephlogisticated air or through perfectly phlogisticated

air, which indicates a necessity of a combination of these two airs to

produce the acid. Moreover, it was found in the last experiment that

the quantity of nitre procured was the same that the soap-lees would

have produced if saturated with nitrous acid; which shows that the

production of the nitre was not owing to any decomposition of the

soap-lees.”

Nothing more clearly shows the care with which Cavendish reasoned than

these last quotations. No loophole is left unstopped; every precaution

is taken to make the proof as faultless as it is possible for a proof

to be.

But this was not enough. It was necessary for Cavendish to show

that, so far as he could ascertain it experimentally, _all_ the

phlogisticated air was capable of combining with dephlogisticated air

to form nitre. This he next proceeded to do.

“As far as the experiments hitherto published extend, we scarcely know

more of the phlogisticated part of our atmosphere than that it is not

diminished by lime-water, caustic alkalies, or nitrous air; that it

is unfit to support fire or maintain life in animals; and that its

specific gravity is not much less than that of common air; so that

though the nitrous acid, by being united to phlogiston, is converted

into air possessed of these properties, and consequently, though it was

reasonable to suppose that part at least of the phlogisticated air

of the atmosphere consists of this acid united to phlogiston, yet it

might fairly be doubted whether the whole is of this kind, or whether

there are not in reality many different substances confounded together

by us under the name of dephlogisticated air. I therefore made an

experiment to determine whether the whole of a given portion of the

phlogisticated air of the atmosphere could be reduced to nitrous acid,

or whether there was not a part of a different nature from the rest,

which would refuse to undergo that change. The foregoing experiments,

indeed, in some measure decided this point, as much the greatest part

of the air let up into the tube lost its elasticity; yet, as some

remained unabsorbed, it did not appear for certain whether that was of

the same nature as the rest or not. For this purpose I diminished a

similar mixture of dephlogisticated and common air in the same manner

as before, till it was reduced to a small part of its original bulk. I

then, in order to decompound as much as I could of the phlogisticated

air which remained in the tube, added some dephlogisticated air to it,

and continued the spark until no further diminution took place. Having

by these means condensed as much as I could of the phlogisticated

air, I let up some solution of liver of sulphur to absorb the

dephlogisticated air; after which only a small bubble of air remained

unabsorbed, which certainly was not more than 1/120th of the bulk of

the phlogisticated air let up into the tube; so that, if there is

any part of the phlogisticated air of our atmosphere which differs

from the rest, and cannot be reduced to nitrous acid, we may safely

conclude that it is not more than 1/120th part of the whole.” We shall

afterwards see that this is a marvellously close estimate. There is

actually 1/84th part of the supposed nitrogen of the air which will not

combine with oxygen when sparked with it in presence of potash.

But there still remained, in Cavendish’s opinion, one point unproved.

It was still conceivable that the potash might contain some

“inflammable matter” which would diminish the air on sparking, and

therefore oxygen nearly pure was sparked in presence of potash; but

only a very small diminution of volume occurred, owing probably to some

nitrogen present as an impurity in the oxygen. Water was substituted

for potash with the same result; but if litmus was added to the water

the colour was discharged, and lime-water introduced into the tube

gave a cloud, showing that “the litmus, if not burnt, was at least

decompounded, so as to lose entirely its purple colour and to yield

fixed air; so that, though soap-lees cannot be decompounded by the

process, yet the solution of litmus can, and so very likely might the

solutions of many other combustible substances.”

Such are the chemical researches of Cavendish. Of all experimenters

on the subject he was undoubtedly the greatest, though Mayow and

Scheele were near rivals. But his researches were so complete that it

is scarcely possible to criticise. He was not content with partial

results: every point was proved and re-proved, and every possibility

of erroneous conclusion was allowed for. It is curious that he did not

employ the balance to check his results. Had he done so he could not

have remained an adherent of the phlogistic theory. Although, as we

have seen, he was perfectly acquainted with the method in which his

results were interpreted by Lavoisier, he chose the old well-trodden

path leading to the wilderness of distorted facts. Lavoisier tried to

repeat Cavendish’s experiments, but without success; and in 1788 the

last part of his _Experiments on Air_ was published, in which he

recorded the successful repetition by a Committee of the Royal Society

of the conversion of nitrogen into nitric acid by the electric spark in

presence of oxygen and potash.

His remaining papers deal with meteorological and astronomical

subjects. One, published in 1790, refers to the height of a remarkable

aurora seen in 1784; another to the civil year of the Hindoos; and

another to a method for reducing lunar distances. And in 1798 his

famous memoir on the density of the earth appeared. It would be quite

beyond the province of this book to enter into any detail regarding

it; but it may be remarked in passing that the method consisted in

measuring, by means of a torsion balance, the attraction of one leaden

ball for another, and that recent experiments, made with the utmost

refinement, have barely altered the number which he obtained,

5·4, to 5·527.

His last paper, on an improvement in a machine for dividing

astronomical instruments, was published in 1809, the year before his

death.

Nothing has been said here regarding the rival claims of Watt to the

discovery of the composition of water, and little need be said. The

discovery was made by both in 1784, yet Cavendish visited Watt at

Birmingham in 1785, and was apparently on the best of terms with him;

and Watt, as proved by Cavendish’s diary, showed him many of his

devices connected with the steam-engine. There can be no doubt that

Watt had also discovered that when hydrogen and oxygen are exploded

together water is the sole product, but he coupled the phenomenon with

views involving the material nature of heat, or caloric, as it was then

called, which Cavendish repudiated.

Cavendish’s later work was carried out in a villa at Clapham, which

was fitted as a laboratory, workshop, and observatory, but he had

a town-house near the British Museum, at the corner of Gower Street

and Montague Place. He had also a library in Dean Street, Soho, which

was available for any scientific man who chose to present himself. So

singular were Cavendish’s habits that when he wished a book he went to

this house and borrowed it as from a public library, giving a receipt

for it.

Of all men, Cavendish was probably the most singular, but there can be

no question of his extraordinary genius.

[23] _Brit. Assoc. Report_, 1839, p. 64.

[24] _Experiments and Observations on Different Kinds of Air_, vol. i.

p. 181, and vol. ii. p. 238. Second edition, 1776.

The Gases of the Atmosphere: The History of Their Discovery · 第 4 / 7 章