The manufacture of earth colours : $b With thirty-one illustrationsBersch, Josef
Science
The manufacture of earth colours : $b With thirty-one illustrations
Bersch, Josef
Coloring matter; Pigments
Although this mineral is not used as a pigment by itself, it must be
mentioned here because it is not infrequently employed for mixing with
other colours, and is also used in the wall-paper industry. It also
serves to distribute certain pigments in a state of fine division, the
“rouge végétal” of the perfumer, for example, usually consisting of
talc and a small quantity of very fine carmine.
In commerce the name talc is sometimes applied to two separate
minerals, true talc and steatite or soapstone. The former is rarely
met with native as well-defined crystals, mostly occurring as scaly
masses in primitive rocks. Thin pieces exhibit a certain degree of
flexibility. The hardness of this mineral is so small that it can
be scratched with the finger-nail; and its sp. gr. is 2·9–2·8. Talc
is easily scraped, and the powder remains sticking to the knife, a
property which renders the substance difficult to reduce to powder,
because it balls together and takes a very long time to convert into
a fine flour. The process is facilitated by calcining the talc and
quenching it in cold water, this treatment increasing the hardness
and at the same time making it more brittle, and thus more easy to
pulverise.
A characteristic feature of all the talc minerals is their peculiar
greasy appearance and feel. The colour varies, white pieces alone being
of any use to the colour manufacturer. The yellow- or green-tinged
varieties owe their shade to the presence of ferric and ferrous
oxides. In chemical composition, talc consists of a combination of
magnesium silicate with hydrated silica, the supposed formula being:
4MgO . SiO{2} + H{2}O . SiO{2}, and the percentage composition: silica,
62·6%; magnesia, 32·9%; water, 4·9%.
STEATITE OR SOAPSTONE
Steatite so closely resembles talc in most of its properties, that
the two minerals were long regarded as identical. Whereas, however,
talc is scarcely acted upon at all by the strongest acids, steatite is
completely decomposed by prolonged boiling therewith, although both
minerals have exactly the same composition.
As a pigment, steatite is far more important than talc, and, as French
chalk, is largely used for drawing or writing. To prepare it for this
purpose pure white steatite requires no preliminary treatment, beyond
cutting the large lumps up into quadrangular prisms, which are mounted
in wood, like lead pencil, and used for writing on the blackboard. The
powder produced in the cutting process is made up into pastel crayons.
With this object, the powder is mixed with a sufficient quantity of
some mineral pigment to produce a mass of the desired shade, and is
kneaded to a stiff paste with water containing an adhesive such as gum,
glue or tragacanth mucilage. The mass is shaped into prisms, which,
when dry, are cut into pencils and mounted in wood. Steatite being like
talc, without action on even the most delicate colours, can be used as
a diluent in the preparation of light shades.
CHAPTER V
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