Elements of the Theory and Practice of Chymistry, 5th ed.Macquer, Pierre Joseph
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Elements of the Theory and Practice of Chymistry, 5th ed.
Macquer, Pierre Joseph
Chemistry -- Early works to 1800
Water exposed to the Fire grows hot; but only to a limited degree,
beyond which its heat never rises, be the force of Fire applied to it
ever so violent: it is known to have acquired this degree of heat by
its boiling up with great tumult. Water cannot be made hotter, because
it is volatile, and incapable of enduring the heat, without being
evaporated and entirely dissipated.
If such a violent and sudden heat be applied to Water, as will not
allow it time to exhale gently in vapours, as when, for instance,
a small quantity thereof is thrown upon a metal in fusion, it is
dissipated at once with vast impetuosity, producing a most terrible and
dangerous explosion. This surprising effect may be deduced from the
instantaneous dilatation of the parts of the Water itself, or rather
of the Air it contains. Moreover, Water enters into the texture of
many bodies, both compounds and secondary principles; but, like Air,
it seems to be excluded from the composition of all metals and most
minerals. For although an immense quantity of Water exists in the
bowels of the Earth, moistening all its contents, it cannot be thence
inferred, that it is one of the principles of minerals. It is only
interposed between their parts; for they may be entirely divested of
it, without any sort of decomposition: indeed it is not capable of an
intimate connection with them.
SECTION III.
_Of_ EARTH.
We observed that the two principles above treated of are volatile; that
is, the action of Fire separates them from the bodies they help to
compose, carrying them quite off, and dissipating them. That of which
we are now to speak, namely Earth, is fixed, and, when it is absolutely
pure, resists the utmost force of Fire. So that, whatever remains of
a body, after it hath been exposed to the power of the fiercest Fire,
must be considered as containing nearly all its earthy principle,
and consisting chiefly thereof. I qualify my expression thus for two
reasons: the first is, because it often happens, that this remainder
does not actually contain all the Earth which existed originally in
the mixt body decomposed by Fire; since it will afterwards appear that
Earth, though in its own nature fixed, may be rendered volatile by
being intimately united with other substances which are so; and that,
in fact, it is common enough for part of the Earth of a body to be thus
volatilized by its other principles: the second is, that what remains
after the calcination of a body is not generally its earth in perfect
purity, but combined with some of its other principles, which, though
volatile in their own natures, have been fixed by the union contracted
between it and them. We shall, in the sequel, produce some examples to
illustrate this theory.
Public-domain text, read in full here on John Shaqi.
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