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
If the smallest portion of water capable of free existence contains
one atom of hydrogen and one of oxygen, then placing the weight of an
atom of hydrogen as unity, the weight of an atom of oxygen is eight
times as great. And although we do not know the absolute weight of
any single atom, we are justified in supposing that an atom of oxygen
is eight times as heavy as an atom of hydrogen. But have we any right
to make the assumption that a molecule of water contains one atom of
each element? Dalton came to the conclusion that this supposition was
a justifiable one; but there are strong reasons against it. We have
already seen that Cavendish discovered approximately, and that
Gay-Lussac and Humboldt determined accurately, that when hydrogen and
oxygen unite to form water, two volumes of the former combine with one
of the latter. Now it appears improbable on the face of it that any
given volume of hydrogen should contain only half as many particles as
an equal volume of oxygen; and it is still more improbable, when we
take into consideration (1) Boyle’s discovery that if the pressure on a
gas be increased, the volume of the gas, whatever it may be, diminishes
in like proportion; and (2) Gay-Lussac’s and Dalton’s discovery, that
all gases, when equally raised in temperature, expand equally. It would
be very remarkable if one gas, containing twice as many particles in
unit volume as another, should show exactly similar behaviour towards
pressure and temperature. Hence it appeared not unreasonable to suppose
that the composition of water was expressed by one particle of oxygen
in union with two particles of hydrogen. (The word “particle” is here
used in the meaning of “small portion”; such particles may be molecules
or they may be atoms.)
When steam is formed by the union of hydrogen with oxygen, it has a
volume equal not to the sum of the volumes of the hydrogen and the
oxygen, but to two-thirds of the sum, or equal to that of the hydrogen
alone, or twice that of the oxygen. And as steam, like hydrogen and
oxygen, follows Boyle’s and Gay-Lussac’s laws, it must be supposed
that in the steam there are as many particles as in the hydrogen from
which it was formed. But the particles of steam must necessarily be
more complex than those of the hydrogen, inasmuch as the steam contains
oxygen as well as hydrogen.
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