The manufacture of mineral and lake pigments : $b Containing directions for the manufacture of all artificial artists' and painters' colours, enamel colours, soot and metallic pigmentsBersch, Josef
Science
The manufacture of mineral and lake pigments : $b Containing directions for the manufacture of all artificial artists' and painters' colours, enamel colours, soot and metallic pigments
Bersch, Josef
Dyes and dyeing; Pigments
In spite of these favourable properties antimony vermilion has so
far been little used. Considering the small cost of its preparation,
especially when calcium hyposulphite, which gives an equally good
result, is used in place of the sodium salt, its use is to be
recommended in the place of mercury vermilion. It appears as if the
high price demanded for this substance by several manufacturers has
prevented its general employment.
=Appendix. Antimony Blue.=—This fine blue pigment can be prepared by
the addition of a dilute solution of potassium ferrocyanide to a clear
solution of antimony in _aqua regia_. According to Krauss, it contains
no antimony as colouring principle, but is a Prussian blue obtained
from the ferrocyanide, which is decomposed by the strong acid, with
evolution of hydrocyanic acid.
CHAPTER XIX.
FERRIC OXIDE PIGMENTS.
The pigments composed of ferric oxide are used in enormous quantity.
They are distinguished by a high degree of permanence. Large deposits
of ferric oxide occur in nature, and in places where it is found in
considerable quantity iron is manufactured from it on the spot. Several
varieties of natural ferric oxide are distinguished: specular iron ore
forms crystalline masses of brilliant lustre; another variety in small
crystals is called iron glance; micaceous iron ore consists of shining
scales; red hæmatite has the appearance of bundles of fibres; an earthy
variety of hæmatite is also common.
The compound of ferric oxide with water, ferric hydroxide, is still
more abundant than hæmatite; brown hæmatite, limonite and other iron
ores consist essentially of this compound. The pigment known as ochre
is also ferric hydrate.
Very pure red hæmatite has so fine a red colour that it may often be
used as a pigment after grinding or levigating. The famous red of
Pompeii, which has been found on the ruined walls of the town, still
shows, after eighteen centuries’ exposure to damp, the brightest
shade, certainly a striking proof of the extraordinary permanence of
this pigment. Considering its great permanence, its easy preparation,
and its low price, it is surprising that ferric oxide is not more
extensively used by artists than it is at present. It is used,
however, extensively in colouring earthenware, for which purpose
its stability at high temperatures makes it suitable. Principally on
account of its cheapness it is largely used in ordinary painting, but
for artistic purposes it is not used to the extent it deserves.
Public-domain text, read in full here on John Shaqi.
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