The Natural History of ClaySearle, Alfred B. (Alfred Broadhead)
Science
The Natural History of Clay
Searle, Alfred B. (Alfred Broadhead)
Clay
The colours of freshly-dug clays are extremely varied and range from an
almost pure white through all shades of yellow, red and brown to black.
The predominating colours are grey or greyish brown and a peculiar
yellow characteristic of some surface clays. The natural colour of a
clay is no criterion as to its purity, for some of the darkest ball
clays produce perfectly white ware on burning, whilst some of the paler
clays are useless to the potter on account of the intensity of their
colour when they come out of the kiln. The colour of raw clays is
largely due to the carbonaceous matter they contain, and as this burns
away in the kiln, the final colour of the ware bears no relation
whatever to that of the original clay.
The colour of burned ware depends upon the iron compounds in the
clay--these producing buff, red, brown or black (usually termed 'blue')
articles--on the presence of finely divided calcium carbonate (chalk)
which can destroy the colouring power of iron compounds and produce
white ware, and on the treatment the clay has received in the kiln. A
clay which is white when underfired will usually darken in colour if
heated to vitrification, and one which burns red in an oxidizing
atmosphere may turn blue-grey or black under reducing conditions. The
extent to which the carbonaceous matter is burned out also determines
the colour of the fired ware.
The presence of adventitious minerals in the clay may also affect its
colour, particularly when fired.
The most obvious feature in a piece of moist clay is its _plasticity_[5]
or ability to alter its shape when kneaded or put under slight pressure
and to retain its new shape after the pressure has been removed. It is
this property which enables the production of ornaments, vessels of
various kinds, and the many other articles which are the result of the
application of modelling tools, of moulding or of the action of a
potter's wheel. So long as clay contains a suitable proportion of
moisture it is plastic and may be made into articles of any desired
shape, but if the amount of moisture in it is reduced or removed
completely, the material is no longer plastic. It may become so,
however, on adding a further suitable quantity of water and mixing,
provided that it has not been excessively heated. If, in the removal of
the moisture, the clay has been heated to 600° C. or more, it loses its
power of becoming plastic and is converted into a material more closely
resembling stone.
[Footnote 5: A plastic substance is one with the characteristics of 'a
fluid of so great a viscosity that it does not lose its shape under the
influence of gravitation.']
The causes of plasticity appear to be somewhat numerous, though there is
no generally accepted explanation of this remarkable quality which
distinguishes clays from most other substances. It is true that wet
sand, soap, wax, lead and some other materials possess a certain amount
of plasticity, but not to anything like the same extent as clay.
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