The chemistry, properties and tests of precious stonesMastin, John
Science
The chemistry, properties and tests of precious stones
Mastin, John
Precious stones
originals are kept in the strong room of a bank or safe-deposit.
In all cases, however, a hard file will abrade the surface of the false
stone. In chapter VII. we found that quartz is in the seventh degree of
hardness, and an ordinary file is but a shade harder than this, so that
almost all stones higher than No. 7 are unaffected by a file unless it
is used roughly, so as to break a sharp edge. In order to prepare
artificial diamonds and other stones for the file and various tests,
they are often what is called "converted" into "doublets" or "triplets."
These are made as follows: the body of the glass is of paste, and on the
"table" (see last chapter), and perhaps on the broader facets, there
will be placed a very thin slab of the real stone, attached by cement.
In the case of the diamond, the body is clear, but in the coloured
imitations the paste portion is made somewhat lighter in shade than the
real stone would be, the portion below the girdle being coloured
chemically, or mounted in a coloured backing. Such a stone will, of
course, stand most tests, for the parts usually tested are genuine.
A stone of this nature is called a "doublet," and it is evident that
when it is tested on the underside, it will prove too soft, therefore
the "triplet" has been introduced. This is exactly on the lines of the
doublet, except that the collet and perhaps the pavilions are covered
also, so that the girdle, which is generally encased by the mounting,
is the only surface-portion of paste. In other cases the whole of the
crown is genuine, whilst often both the upper and lower portions are
solid and genuine, the saving being effected by using a paste centre at
the girdle, covered by the mounting. Such a stone as this last mentioned
is often difficult to detect without using severe tests and desperate
means, e.g.:--(a) by its crystalline structure (see Chapter III.);
(b) by the cleavage planes (see Chapter IV.); (c) by the polariscope
(see Chapter V.); (d) by the dichroscope (see Chapter VI.); (e) by
specific gravity (see Chapter VIII.); (f) cutting off the mounting,
and examining the girdle; (g) soaking the stone for a minute or so in
a mixture said to have been originally discovered by M. D. Rothschild,
and composed of hydrofluoric acid and ammonia; this will not answer for
all stones, but is safe to use for the diamond and a few others. Should
the jewel be glass, it will be etched, if not completely destroyed, but
if genuine, no change will be apparent; (h) soaking the diamond for a
few minutes in warm or cold water, in alcohol, in chloroform, or in all
these in turn, when, if a doublet, or triplet, it will tumble to pieces
where joined together by the cement, which will have been dissolved. It
is, however, seldom necessary to test so far, for an examination under
the microscope, even with low power, is usually sufficient to detect in
the glass the air-bubbles which are almost inseparable from
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