You must test before you use it, at any scale. Raw materials, mined or man-made, are not consistent. Color, strength, particle size and chemistry can change from one bag to the next and from one supplier to another, even when the name on the bag stays the same. Before you use this material in a glaze, slip or clay body of any size, mix a small test batch, fire it on your own clay in your own kiln, and check the results.
KENTUCKY OM #4 BALL CLAY
Old Mine #4OM4
SiO2 55.2%
Al2O3 27.9
Fe2O3 1.1
TiO2 1.2
MgO 0.4
CaO 0.3
K2O 1.0
Na2O 0.3
P2O5
SO3
L.O.I. 12.6
P.C.E. Cone 32
Geographical Source:
Western Kentucky
Geological Source:
Sedimentary clay and volcanic ash material deposited by water; formed primarily during
middle Eocene epoch approximately 46 million years ago
Characteristics:
Ball clays are fine-grained highly plastic clays containing a fair amount of carbonaceous
organic matter. Ball clays are generally used in quantities of no more than 25% of the
total constituents of a clay body due to their high shrinkage rates and levels of impurities.
Total Cone 10 Shrinkage Rate: 16.5%
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