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
An experiment was therefore devised, in which a large quantity of air
was made to stream slowly through a long train of stems of churchwarden
tobacco-pipes, placed inside a glass tube, the latter being closed at
each end, except for the entrance and exit tubes of the tobacco-pipes;
in the encasing glass tube a vacuum was maintained, and the gases,
passing through the walls of the pipe-stems, were pumped off and
discharged. According to what has just been said, these should be the
lighter gases, nitrogen and oxygen, which ought to pass through the
porous stems more quickly than the supposed heavier constituent of air;
while the air issuing from the end of the train of pipes should contain
relatively more of the heavier constituent, and should in consequence
have a greater weight than an equal volume of air. But it was obviously
convenient to remove the oxygen before weighing this sample of altered
air, and this was done in the usual way by passing the mixed gases
over red-hot copper. It was found that such nitrogen was even heavier
than ordinary atmospheric nitrogen; not much, it is true, but still
consistently heavier. The denser constituent could, in fact, be
concentrated by this means. The proof was therefore indubitable that
the new gas existed in air as such.
There is another method of proof, however, which was not left untried.
Experiment showed that the solubility of the new gas in water is
considerably greater than that of nitrogen, although less than that of
oxygen. In 100 volumes of water at the ordinary temperature, about 1·5
volumes of nitrogen will dissolve, about 4·5 volumes of oxygen, and
about 4 volumes of the new gas, to which the name finally chosen for
it, “argon,” may now be applied. Now the proportion in which the
constituents of a mixture of gases will dissolve in a solvent is
conditioned first by their relative solubilities, and second, by their
relative proportion. Thus, if air be considered to be simply a mixture
of 1 volume of oxygen and 4 volumes of nitrogen, the gas extracted from
water which has been shaken with air will have the composition--
Oxygen 1 x 4·5 = 4·5 volumes
Nitrogen 4 x 1·5 = 6·0 "
So that the proportion of oxygen to nitrogen in such a mixture of gases
is considerably greater than in air: instead of being approximately 1
to 4, it is nearly 4·5 to 6. The discovery of this law concerning the
composition of the gases dissolved in liquids was due to Dr. Henry, one
of the biographers of Dalton.
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