Paint Technology and TestsGardner, Henry A. (Henry Alfred)
Science
Paint Technology and Tests
Gardner, Henry A. (Henry Alfred)
Paint
=Silica (Silex.)= This white pigment possesses great tooth and spreading
properties. It is of use as a wood filler and as a constituent in
combination paints. It wears especially well when used in combination
with zinc oxide and white lead. Its purity often approaches 97%. The
particles when enlarged are seen to have sharp angles and are not
uniform in size, which accounts for its marked tooth and properties.
[Illustration: Aluminum Silicate (China Clay)]
[Illustration: Ochre]
[Illustration: Raw
Burnt
Sienna]
[Illustration: Raw
Burnt
Umber]
=Aluminum Silicate (China Clay).= China clay, or aluminum silicate, is a
permanent and valuable white pigment showing very little hiding power in
oil. It is found widely distributed in granitic formations. It is very
stable, with a gravity of 2.6. Particles are found in many shapes and
sizes, showing sharp and definite angles.
=Ochre.= Ochre is a hydrated ferric oxide permeating a clay base,
largely used as a tinting material. It has a specific gravity of about
3.5, and a decidedly golden yellow color. A good quality should contain
20% or over of iron oxide. The particles of this pigment are flocculent
and very uniform in appearance.
=Sienna.= Sienna, like umber, is essentially a silicate of iron and
alumina, containing manganic oxide. It contains, however, a lower
percentage of the latter than in the case of umbers. The photomicrograph
of the burnt variety shows clearly the fine condition of the pigment,
while large particles are shown in the raw variety.
=Umber.= Umber, another naturally occurring pigment, consists of iron
and aluminum silicates, containing varying proportions of manganic
oxide, its color and tone varying according to the percentage of the
latter. The raw variety is drab in color, which in burning changes to
reddish brown. A marked percentage of large-sized particles exist in
this pigment.
=Indian Red.= Indian red is the term applied to natural hematite ore
pigments and to those produced by the roasting of copperas (iron
sulphate). They generally contain 95% or more of iron oxide, with
varying percentages of silica. The pigment is heavier (specific gravity
5.2) than that of Metallic Brown. The crystalline, mineral-like
structure of the particles differ greatly from the amorphous particles
of Metallic Brown.
=Metallic Brown.= The natural hydrated iron oxide or carbonate as mined
largely in Pennsylvania, yields, when roasted, a sesquioxide of iron
known as Metallic Brown. It contains a high percentage of alumina and
silica, and has a characteristic brown color with a gravity of 3.1. It
finds wide application as a pigment for protective purposes. The
particles when enlarged show the usual appearance of a natural compound
which has been roasted and ground.
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