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ALUMINA-SILICATE

Miscellaneous

Notes

(Richard Willis)

The silicate of aluminum of the form Al2O3, SiO2 with a minimal apportioning of Al2O3 39.5% and SiO2 46.5%. When it occurs naturally in its hydrated (i.e., with H2O) and layered (i.e., sandwiched aluminum and silicon — see soils) it is known as a clay mineral (kaolinite, dickite, etc.) see clay minerals
The term is normally used in contrast to “ferro-silicate” and “magnesio-silicate” to distinguish clay earths which have not had their aluminum replaced by iron and/or magnesium. As a comparison, anhydrated silicates of aluminum occurring naturally are usually gem stones rather than clays.

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