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
The geological characteristics of Cologne earth enable one to conclude
that, where similar conditions prevail, materials of analogous nature
may be discovered. This earth is found embedded in a deposit of brown
coal, in which it forms pockets, and occasionally large bodies. Now,
brown-coal deposits of enormous extent occur in very many localities,
as for instance in Upper Austria and in Bohemia; and many of these
mines are sure to contain pockets of brown-coal mould, which have
perhaps been overlooked, but might very well be utilised in the
preparation of colours of very similar character to Cologne earth.
The preparation of this material is very simple. The earth coming from
the deposits is put through a simple levigation treatment which leaves,
as residue, lumps of semi-decomposed wood, mineral admixtures, sand,
etc. The levigated earth is sold in the form of cubes.
Cologne earth comes into the market under various other names, such as:
umber, Cassel brown, Spanish brown, etc.
The fiery brown which was so greatly preferred by the famous painter
Van Dyck, and named Vandyke brown after him, was of very similar
composition to Cologne earth, and is said to have been obtained from a
deep brown peat earth. The Vandyke brown of the present day, however,
is almost invariably a ferric oxide pigment, toned to the proper shade
by suitable calcination.
ASPHALTUM BROWN (BITUMEN)
As a natural product, which can be used as a painters’ colour without
any special preparation, asphaltum (bistre, bitumen) may also be
classed among the earth colours. Chemically, it is composed of
hydrocarbons of various kinds, and is thus similar to tar; in fact,
asphaltum may also be regarded as a natural tar resulting from the
decomposition of various organic substances. Many deposits of this
mineral are known, and two of them are particularly celebrated: those
of the Dead Sea, in Syria, and the Lake of Asphalt, in Trinidad. Both
deposits consist of craters filled with water on which the asphaltum
floats in large cakes.
Several kinds of asphaltum are met with in commerce, ranging in colour
from brown to black. The preparation of the material as a pigment
is confined to grinding the mass, which is always of a low degree
of hardness. Being readily soluble in oil of turpentine and then
furnishing the most beautiful brown tones when laid on thinly, the
pigment is usually sold in this condition, although it is also ground
in oil for the same purpose.
Finally, it may be mentioned that various useless materials can be
transformed, by suitable treatment, into brown pigments closely
resembling Cologne earth and applicable to the same uses. Such pigments
can be prepared from brown-coal slack (from inferior brown coal) or
bituminised wood--a variety of brown coal looking like charred wood--by
treating these materials with a lye made from wood ashes and lime, and
washing and drying the residue.
CHAPTER VIII
GREEN EARTH COLOURS
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