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 — John Shaqi
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
But it may be said, that combustion always diminishes the volume or
mass, on account of the quantity of matter it consumes; and that, on
the contrary, calcination increases the weight of many substances.
Ought we then to consider these two effects whose results are so
contrary, as effects of the same nature? Such an objection appears
well-founded, and deserves an answer, especially as this is the most
difficult point of the question. For that purpose let us consider a
matter in which we shall suppose one half to be fixed parts, and the
other volatile or combustible. By the application of fire to this,
all the volatile or combustible parts will be raised up or burnt, and
consequently separated from the whole mass; from hence this mass or
quantity of matter will be found diminished one half, as we see it
in calcareous stones, which lose near half their weight in the fire.
But if we continue to apply the fire for a very long time to the other
half, composed of fixed parts, all combustion and volatilization
being ceased, that matter, instead of continuing to lose its mass,
must increase at the expense of the air and fire with which it is
penetrated; and those are matters already calcined, and prepared
by Nature to the degree where combustion ceases, and consequently
susceptible of increasing the weight from the first moment of the
application. We have seen, that light extinguishes on the surface of
all bodies which do not reflect; and that heat, by long residence,
fixes partly in the matters which it penetrates; we know also that
air is necessary for calcination, or combustion, and the more so for
calcination as having more fixity in the external parts of bodies, and
becomes a constituent part: hence, it is natural to imagine, that this
augmentation of weight proceeds only from the addition of the particles
of light, heat, and air, which are at length fixed and united to one
matter, against which they have made so many efforts, without being
able either to raise or burn them. This appears clearly to be the
fact, for if we afterwards present a combustible substance to them they
will quit the fixed matter, to which they were only attached through
force, retake their natural motion, elasticity, and volatility, and
all depart with it; from hence, metal, or calcinized matter, to which
these volatile parts has been rendered, retakes its pristine form,
and its weight is found diminished by the whole quantity of fiery
and airy particles which were fixed in it, and which had been just
raised by this new combustion. All this is performed by the sole law
of affinities; and there seems to be no more difficulty to conceive
how the lime of a metal is reduced, than to understand how it is
precipitated in dissolution; the cause is the same, and the effects are
similar. A metal dissolved by an acid, will precipitate when to this
acid another substance is offered with which it has more affinity than
metal, the acid then quits it and falls to the bottom.
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