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Series editors' preface - Wood Tools

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Table 5.3 Pigments – continued<br />

Other materials and structures 227<br />

Colour/group Chemical composition Origin/date Properties Refractive<br />

Pigment and description Index<br />

name<br />

Phthalocyanine<br />

green<br />

Blue<br />

Azurite<br />

(mountain<br />

blue)<br />

Blue bice<br />

Ultramarine<br />

– natural<br />

Ultramarine<br />

– synthetic<br />

(French<br />

ultramarine)<br />

Smalt<br />

Indigo<br />

Cobalt blue<br />

(Thénard’s<br />

blue)<br />

Cerulean<br />

blue<br />

Prussian<br />

blue<br />

Chlorinated copper phthalocyanine.<br />

Similar to phthalocyanine blue<br />

A basic copper carbonate<br />

(CuCO 3.Cu(OH) 2). Crystalline.<br />

Appears deep violet blue when<br />

ground coarsely but becomes paler<br />

and weaker in tinting strength if<br />

more finely ground<br />

Artificial basic copper carbonate<br />

similar to azurite. Usually more<br />

rounded and finer particles than<br />

azurite<br />

A mixture of lazurite with calcspar<br />

and iron pyrites. Clear, often<br />

slightly purplish, blue crystalline<br />

particles of irregular size and<br />

shape. A few orange-red particles<br />

of iron pyrites are often seen with<br />

white crystalline calcite<br />

Chemically identical to natural<br />

ultramarine. A compound of<br />

sodium, silica, aluminium and<br />

sulphur. Two distinct kinds of<br />

ultramarine are made: soda<br />

ultramarine and sulphate<br />

ultramarine. It is possible to arrive<br />

at many subtly different shades<br />

according to the method of<br />

manufacture and the exact formula<br />

which can vary from Na 8A l6Si 6O 22S 4<br />

to Na 10A l6Si 6O 24S 2. Finely divided<br />

homogeneous particles usually<br />

smaller and more rounded than<br />

those of natural product and<br />

lacking calcite and pyrites<br />

Formed from cobalt blue glass<br />

coloured by the addition of cobalt<br />

oxide formed by roasting cobalt<br />

containing minerals. Coarser<br />

particles give deep rich purpleblue.<br />

Finer particles only a pale<br />

blue. Very characteristic coarse<br />

glassy fragments<br />

Blue vegetable colour used as both<br />

a dye and a pigment. Appears as<br />

intensely blue discrete particles at<br />

high magnification (1500)<br />

Cobalt aluminate (CoO.Al 2O 3). Pure<br />

blue rounded particles, moderately<br />

fine and of irregular size. Bright<br />

blue by transmitted light<br />

Cobaltous stannate (CoO.nSnO 2).<br />

Finely divided rounded particles,<br />

high refractive index, green blue in<br />

transmitted light. Harmful<br />

A complex compound, technically<br />

ferric ferrocyanide Fe 4(Fe(CN)6) 3.<br />

Available commercially<br />

from 1938<br />

Natural pigment derived<br />

from the mineral<br />

azurite. Important from<br />

the fifteenth to the<br />

seventeenth centuries,<br />

now rarely used<br />

Used extensively in<br />

medieval painting until<br />

the end of the<br />

eighteenth century<br />

Obtained from the<br />

semi-precious stone<br />

lapis lazuli. First occurs<br />

as pigment in sixth and<br />

seventh century wall<br />

paintings. In wide use<br />

until the early<br />

nineteenth century. Still<br />

available<br />

In commercial<br />

production from about<br />

1830<br />

Used in Europe from<br />

the late sixteenth<br />

century (earlier in Asia)<br />

until the beginning of<br />

the nineteenth century<br />

when it was replaced<br />

by cobalt blue and<br />

artificial ultramarine<br />

Obtained from plants of<br />

the genus Indigofera.<br />

Very early use in Far<br />

East. First synthesized in<br />

1880<br />

Discovered in 1802.<br />

Expensive and therefore<br />

liable to adulteration<br />

and substitution<br />

Known early in the<br />

nineteenth century but<br />

not commercially<br />

available until 1860<br />

Earliest of ‘modern’<br />

pigment colours first<br />

Mostly used in tempera as it<br />

appears dark and ‘muddy’ in oil.<br />

Generally very stable but may<br />

discolour in contact with alkalis<br />

and can turn to green Malachite by<br />

hydration<br />

Once used in large quantities as<br />

cheaper, but less stable substitute<br />

for Azurite and Ultramarine.<br />

Tendency to turn green over time<br />

Light-fast and stable under all<br />

conditions except in the presence<br />

of acids when it loses colour and<br />

evolves hydrogen sulphide gas.<br />

Ultramarine in oil may decolour<br />

and become grey with age due to<br />

presence of acids in the oil film.<br />

Ultramarine containing free sulphur<br />

may cause darkening when mixed<br />

with lead or copper pigments.<br />

Soda ultramarine contains a high<br />

percentage of silica and is<br />

sometimes called acid resisting.<br />

Sulphate ultramarine has a greenish<br />

tinge and lower covering power<br />

Stable but with very poor hiding<br />

power<br />

Fair tinting strength. Can be used<br />

in oil but better in tempera or<br />

water colour. Very stable in<br />

tempera and resistant to fading by<br />

light but not when used in thin<br />

films<br />

Light-fast, very stable and<br />

permanent in all painting<br />

techniques<br />

Stable and inert, unaffected by<br />

light or strong chemicals<br />

Transparent but with high tinting<br />

strength. Fairly permanent but<br />

1.40<br />

1.73–1.84<br />

1.72–1.74<br />

1.50<br />

1.50<br />

1.49–1.52<br />

1.74<br />

1.84<br />

1.56<br />

continued

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