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
Besides, this means is the only one we have to volatilize fixed metals,
such as gold and silver; for I presume that this vapour, which I have
seen rise in such great quantities from these fixed metals, heated in
the large focus of my mirror, is neither of water, nor of any other
liquor, but of the parts even of the metal which the heat detaches by
volatilizing them. By receiving these vapours of different metals, and
thus mixing them together, more intimate and pure alloys would be made
than can be by fusion, and the mixture of these metals when melted,
which never perfectly unites on account of the inequality of their
specific weight, and many other circumstances which are opposed to the
intimate and perfect equality of the mixture. As the constituent parts
of the metallic vapours are in a much greater state of division than
fusion, they would join and unite closer and more readily. In short,
we should attain the knowledge of a general fact by this mode, and
which, for many reasons, I have a long time suspected, that there is
penetration in all alloys made in this manner, and that their specific
weight would be always greater than the sum of the specific weights
of the matters of which they are composed: for penetration is only a
greater degree of intimacy; every thing equal in other respects will
be so much the greater as matters will be in a more perfect state of
division.
By reflecting on the vessels used to receive and collect these metallic
vapours, I was struck with an idea, which appeared to me to be of too
great utility not to publish; it is also easy enough to be realized by
good able chemists; I have even communicated it to some of them, who
appeared to be quite satisfied with it. This idea is to freeze mercury
in this climate, and with a much less degree of cold than that of the
experiments of Petersburgh or Siberia. For this purpose the vapour
of mercury is only required to be received, and which is the mercury
itself volatilized by a very moderate heat in a crucible, or vessel,
to which we give a certain degree of artificial cold. This vapour, or
this mercury, minutely divided, will offer, to the action of the cold,
surfaces so large, and masses so small, that instead of 187 degrees of
cold requisite to freeze mercury, possibly 18 or 20 will be sufficient,
and perhaps even less to freeze it when in vapour. I recommend this
important experiment to all those who endeavour earnestly for the
advancement of the sciences.
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