Chinese pottery and porcelain; vol. 2. Ming and Ch'ing PorcelainHobson, R. L. (Robert Lockhart)
History
Chinese pottery and porcelain; vol. 2. Ming and Ch'ing Porcelain
Hobson, R. L. (Robert Lockhart)
Porcelain, Chinese; Pottery, Chinese
The cobaltiferous ore of manganese is the same material which is used
to give a blue colour, but in this case the manganese is removed, and
the cobalt rendered as pure as possible. For the manganese if in excess
produces a purplish brown, and its presence in however small a
quantity gives the blue a purple or violet strain. By the simple method
of graduating the amount of manganese which was allowed to remain with
the cobalt the potters were able to obtain many intermediate shades
between dark blue and purple for their monochrome glazes.
The green monochromes are scarcely less numerous than the blue. There
are the transparent greens of apple or leaf green shades whether even
or mottled, which have been described among the glazes applied to the
biscuit and among the enamels of the _famille verte_. These were used
as monochromes and ground colours; and closely akin to them are (1)
the cucumber green (_kua p’i lü_), in which a yellowish leaf green is
heavily mottled with darker tints, and (2) the snake skin green (_shê
p’i lü_), a deep transparent green with iridescent surface, one of the
colours for which the directorate of Ts’ang Ying-hsüan was celebrated.
There are good examples of both in the Salting Collection, but it would
be useless to reproduce them except in colour.
There are the apple and emerald green crackles (in both cases a
green glaze overlying a grey or stone-coloured crackle), but these
have already been discussed.[338] A somewhat similar technique
characterises the series of semi-opaque and crackled green glazes of
camelia leaf, myrtle, spinach, light and dark sage, dull emerald and
several intermediate tints. These are soft-looking glazes with small
but very regular crackle,[339] and their surface often has a “satiny”
sheen which recalls the Yi-hsing glazes. They are evidently glazes
of the _demi-grand feu_, and the colouring agent is doubtless
copper, though apparently modified with other ingredients. How far this
particular group was used in the K’ang Hsi period is hard to say. Most
of the specimens which I have seen give me the impression of a later
make, but as there are a few which might come within the K’ang Hsi
limits I have taken this opportunity to discuss them.
There is one specimen of a rare green in the British Museum to which I
cannot recall a parallel. It is a bowl with the ordinary white glaze,
but covered on the exterior with a very bright yellowish green, like
the young grass with the sun shining on it. It is, perhaps, rather in
the nature of an enamel than a glaze, but the ware has the appearance
of age and should belong to the early part of the K’ang Hsi period.
Public-domain text, read in full here on John Shaqi.
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