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Am Ceram Soc Bull 1992 May; 71(5):801-802
Gypsum is the most common of the naturally occurring sulfate minerals. It is found in very extensive, bedded sedimentary deposits all over the world and is associated with limestones, shales and sandstones, marls and clays. High-purity deposits of gypsum are relatively common, and, for most uses, little or no beneficiation is required. In the United States most gypsum rock is finely ground and partially calcined to drive off 75 pct of the chemically combined water, converting gypsum, caso4.2H2o, to the hemihydrate product, caso4.1/2H2o. Commonly called plaster of paris, this material quickly sets and hardens back to gypsum when mixed with the appropriate amount of water.
Issue of Publication
American Ceramic Society Bulletin
Page last reviewed: March 11, 2019
Content source: National Institute for Occupational Safety and Health Education and Information Division