Useful Knowledge: Volume 1. Minerals: Or, a familiar account of the various productions of natureBingley, William
History
Useful Knowledge: Volume 1. Minerals: Or, a familiar account of the various productions of nature
Bingley, William
Commercial products; Geology, Economic; Natural history
When white vitriol is artificially prepared, the blende is roasted, and
thrown, while red hot, into a vessel filled with water; in which it is
allowed to remain about eighteen hours. This process is repeated several
times; and, after the solution has become clear, it is removed into
leaden vessels, and the water is evaporated by means of heat. On
cooling, it crystallizes. After this the crystals are melted in a copper
vessel, and the surface of the solution is skimmed with a hair sieve. It
is then poured into a wooden vessel, and stirred till it becomes cool,
and acquires a sufficient degree of consistence, when it is formed into
loaves for sale. In this state it has the appearance and colour of
refined sugar. White vitriol is chiefly manufactured in Germany.
It is used in medicine; and is employed in great quantities by
varnishers, to make their oil varnishes dry more readily than they
otherwise would. A fine white colour, called _zinc─white_, which is more
durable than white lead, is prepared from it. Dyers use a considerable
quantity of white vitriol to render deeper the colours produced by
madder, cochineal, and other substances.
A pleasing experiment is made by mixing in a phial a small quantity of
solution of white vitriol with a little liquid ammonia. Though each of
the fluids is transparent when separate, yet the zinc will now be
immediately precipitated in a white mass; and, what is peculiarly
deserving of remark, if then shaken, it will almost as instantly be
re─dissolved.
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CLASS III.—COMBUSTIBLES.
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SULPHUR FAMILY.
211. _COMMON SULPHUR, or BRIMSTONE, is a yellow, dry, and brittle
substance, which, in burning, yields a suffocating fume: the smell of
this, under the denomination of_ sulphureous, _is well known._
_Sulphur is found in a pure or native state in nearly all volcanic
countries: it is about twice as heavy as water; and is sometimes
crystallized in the form of octohedrons, whose bases are rhombs. It
exists abundantly in a state of combination with several metallic
substances, and is also formed in putrid animal remains._
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