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
issues from all bodies in incandescence, and which strikes our eyes,
is the evaporation of this dense flame which surrounds the body by
renewing itself incessantly on its surface; and even the light of the
sun, which emits such an amazing brightness, I presume to be only an
evaporation of the dense state that constantly plays on its surface;
and which we must regard as a true flame, more pure and dense than any
proceeding from our combustible matters.
It is, therefore, by light that fire communicates, and heat alone
cannot produce the same effect as when it becomes very strong to be
luminous. Even water, that destructive element to fire, by which alone
we can prevent its progress, nevertheless communicates when in a
well-closed vessel, such as Papin's digester, where it is penetrated
with a sufficient quantity of fire to render it luminous, and capable
of melting lead and tin, whereas when it is only boiling, far from
communicating fire, it extinguishes it immediately. It is true, that
heat alone is sufficient to prepare and dispose combustible bodies for
inflammation, by driving off the humid parts from bodies; and what is
very remarkable, this heat, which dilates all bodies, does not desist
from hardening them by drying. I have an hundred times discovered, by
examining the stones of my great furnaces, especially the calcareous,
they increased in hardness in proportion to the time they had undergone
the heat, and they also at the same time became specifically heavier.
From this circumstance, I think an induction may be drawn, which
would prove, and fully confirm, that heat, although in appearance
always fugitive and never stable in the bodies which it penetrates,
nevertheless deposits in a positive manner many parts which fixes there
even in greater quantities than the aqueous and other parts which it
has driven off. But what appears very difficult to be reconciled,
this same calcareous stone, which becomes specifically heavier by the
action of a moderate heat a long time continued, becomes near a half
lighter, when submitted to a fire sufficient for its calcination, and,
at the same time, not only loses all the hardness it had acquired by
the action of heat, but even the natural adherence of its constituting
parts.
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