The Gases of the Atmosphere: The History of Their Discovery — John Shaqi
The Gases of the Atmosphere: The History of Their DiscoveryRamsay, William
History
The Gases of the Atmosphere: The History of Their Discovery
Ramsay, William
Air; Argon; Chemistry -- History
From experiments on the rise of sap in plants, many of them very
ingenious and well adapted to secure their end, and which are still
regarded by botanists as classic, Hales noticed that a quantity of
air was inspired by plants. In order to ascertain the composition and
amount of this air, the process of distillation was resorted to; for
Hales remarks: “That elasticity is no immutable property of air is
further evident from these experiments; because it were impossible for
such great quantities of it to be confined in the substances of animals
and vegetables, in an elastick state, without rending their constituent
parts with a vast explosion” (Preface, p. viii.). Hence, concluding
that the air absorbed by plants and animals could be recovered by their
distillation, Hales proceeded to distil a great number of substances of
animal and vegetable origin, such as hogs’ blood, tallow, a
fallow-deer’s horn, oystershell, oak, wheat, peas, amber, tobacco,
camphor, aniseed oil, honey, beeswax, sugar, Newcastle coal, earth,
chalk, pyrites, a mixture of salt and bone-ash, of nitre and bone-ash,
tartar, compound aquafortis, and a number of other substances. He
collected the “air” in each case over water, and gave numerical data to
show what proportion the air bore by weight to the substance from which
it had been obtained. He even tried to compare the weight of ordinary
air with that of air from distilled tartar; but his experiment led to
no positive conclusion, because of the crudeness of his appliances. The
compressibility or “elasticity” of the air from tartar, however, was
found to be identical with that of common air.
Hales does not appear to have made any special experiments on the
properties of his various airs, by trying whether they supported
combustion, whether they were themselves combustible, etc. We see from
this list that he had under his hands mixtures of hydrocarbons, carbon
dioxide, probably sulphur dioxide, hydrochloric acid and ammonia (both,
however, dissolving in water as they were formed), oxides of nitrogen,
possibly chlorine, and, as minium or red-lead was one of the substances
he tried, oxygen in a more or less pure state. It must be remembered
that in all cases the gas obtained was mixed with the air originally
present in the retort. He next proceeded to produce “air” by the
fermentation of grain, of raisins, and of other fruits; this “air”
obviously was carbon dioxide more or less pure.
It is curious to note here that he anticipated Lord Kelvin in devising
a sounding-lead which should register the depth of the sea by the
compression of air, the distance to which the air had receded along the
tube being shown by the entry of treacle. He successfully carried out a
sounding by means of his apparatus.
Public-domain text, read in full here on John Shaqi.
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