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
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_n_λ_{argon} = _c__{argon} = √γ(_p_/_d_)(1 + _at_)_{argon},
where _n_ is the number of vibrations per second, =λ= the
wave-length of sound, and _a_ the coefficient of the expansion of a
gas for a rise of 1° in temperature, _t_, viz. 0·00367. Now if the
expression _p_ (1 + _at_) can be shown to be identical for argon and
for air, the value of =γ= for argon can be calculated by the very
simple proportion--
λ^{2}_d__{air} : λ^{2}_d__{argon} :: 1·408 : γ_{argon}.
This involved a measurement of the rate of rise of pressure of argon,
_p_, per degree of rise of temperature, _t_; or, in other words,
the verification of Boyle’s and Gay-Lussac’s laws for argon; and
this research was successfully carried out by Dr. Randall of the
Johns Hopkins University of Baltimore, U.S.A., and Dr. Kuenen, of
Leyden, working in Professor Ramsay’s laboratory.[29] They made use
of a constant volume thermometer, and measured the rise of pressure
corresponding to a definite rise of temperature, comparing the gases
argon and helium in this respect with air. The values found between 0°
and 100° for air, argon, and helium were--
One volume air, heated from 0° to 100°, raises
pressure in the proportion of 1 to 1·3663
Argon 1·3668
Helium 1·3665
It may therefore be taken for certain that, within the limits of
experimental error, the value of the expression _p_(1 + _at_)
is identical for all three gases.
We see, then, that for argon, as for mercury gas, the value of =γ=,
the ratio between the specific heats at constant volume and at constant
pressure, is 1 to 1·66, whereas for air, hydrogen, oxygen, nitrogen,
carbon monoxide, and nitric oxide, it is 1 to 1·4.
We have now to consider what conclusion can be drawn from this
difference.
On the usually accepted theory of the constitution of matter, it is
held that atoms may be regarded as spheres, hard, elastic, smooth, and
practically incompressible. True, we really know little or nothing
regarding the properties of such particles, if particles there be;
but in considering their behaviour it is necessary to make certain
suppositions, and to see whether observed facts can be pictured to our
minds in accordance with such postulates. If, from the known behaviour
of large masses, conclusions can be drawn regarding small masses, and
if these conclusions harmonise with what is found to be the behaviour
of large numbers of small masses acting at once, the justice of the
supposition is, although not proved, at least rendered defensible as
one mode of regarding natural phenomena.
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