Buffon's Natural History. Volume 10 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Minerals, &c. &cBuffon, Georges Louis Leclerc, comte de
History
Buffon's Natural History. Volume 10 (of 10): Containing a Theory of the Earth, a General History of Man, of the Brute Creation, and of Vegetables, Minerals, &c. &c
Buffon, Georges Louis Leclerc, comte de
Natural history
To prevent the suspicion of vainly dwelling upon assertion, I think it
necessary to remark upon what foundation I build this theory; I have
found that bodies which should heat in ratio of their diameters, could
be only those which were perfectly permeable to heat, and would heat
or cool in the same time; hence, I concluded that fluids, whose parts
are only held together by a slight connection, might approach nearer to
this perfect permeability than solids, whose parts have more cohesion.
In consequence of this, I made experiments, by which I found, that
with the same heat all fluids, however dense they might be, heat and
cool more readily than any solids, however light, so that mercury, for
example, heats much more readily than wood, although it be fifteen or
sixteen times more dense.
This made me perceive that the progress of heat in bodies cannot, in
any case, be made relatively to their density; and I have found by
experience, that this progress, as well in solids as fluids, is made
rather by reason of their fluidity, or in an inverse ratio of their
solidity. I mean by _solidity_ the quality opposite to fluidity; and I
say, that it is in an inverse ratio of this quality that the progress
of heat is made in both bodies; and that they heat or cool so much the
faster as they are the more fluid, and so much the slower as they are
more solid, every other circumstance being equal.
To prove that solidity, taken in this sense, is perfectly independent
of density, I have found, by experience, that the most or least dense
matters, heat or cool more readily than other more or less dense
matters, for example, gold or lead, which are much more dense than iron
and copper, heat and cool much quicker; while tin and marble, which are
not so dense, heat and cool much faster than iron and copper; and there
are likewise many other matters which come under the same description;
so that density is in no manner relative to the scale of the progress
of heat in solid bodies.
Public-domain text, read in full here on John Shaqi.
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