The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are relatedTyndall, John
Science
The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are related
Tyndall, John
Alps -- Description and travel; Glaciers -- Alps
De Saussure, Fourier, M. Pouillet, and Mr. Hopkins have developed this
speculation, and drawn from it consequences of the utmost importance;
but it nevertheless rested upon a basis of conjecture. Indeed some of
the eminent men above-named deemed its truth beyond the possibility of
experimental verification. Melloni showed that for a distance of 18 or
20 feet the absorption of obscure rays by the atmosphere was absolutely
inappreciable. Hence, the _total_ absorption being so small as to elude
even Melloni's delicate tests, it was reasonable to infer that
_differences_ of absorption, if such existed at all, must be far beyond
the reach of the finest means which we could apply to detect them.
[Sidenote: DIFFERENCES OF ABSORPTION BY GASES.]
This exclusion of one of the three states of material aggregation from
the region of experiment was, however, by no means satisfactory; for our
right to infer, from the deportment of a solid or a liquid towards
radiant heat, the deportment of a gas, is by no means evident. In both
liquids and solids we have the molecules closely packed, and more or
less chained by the force of cohesion; in gases, on the contrary, they
are perfectly free, and widely separated. How do we know that the
interception of radiant heat by liquids and solids may not be due to an
arrangement and comparative rigidity of their parts, which gases do not
at all share? The assumption which took no note of such a possibility
seemed very insecure, and called for verification.
My interest in this question was augmented by the fact, that the
assumption referred to lies, as will be seen, at the root of the glacier
question. I therefore endeavoured to fill the gap, and to do for gases
and vapours what had been already so ably done for liquids and solids by
Melloni. I tried the methods heretofore pursued, and found them
unavailing; oxygen, hydrogen, nitrogen, and atmospheric air, examined by
such methods, showed no action upon radiant heat. Nature was dumb, but
the question occurred, "Had she been addressed in the proper language?"
If the experimentalist is convinced of this, he will rest content even
with a negative; but the absence of this conviction is always a source
of discomfort, and a stimulus to try again.
Public-domain text, read in full here on John Shaqi.
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