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Kaolin clay

Kaolin clay is derived from the mineral Kaolinite which comes from the Earth’s crust. It is a hydrous aluminum silicate formed by the decomposition of minerals such as feldspar. The mineral Kaolinite, also referred to as Kaolinite clay, is a layered silicate mineral and is soft, earthy, and usually white in color, produced by the chemical weathering of aluminum silicate minerals. Rocks that are rich in Kaolinite are also known as Kaolin or China Clay. This means the terms Kaolin clay and Kaolinite clay can be used interchangeably.

 

For more information about describing soils using the USDA-Field Book for Describing and Sampling Soils, visit:

www.nrcs.usda.gov/Internet/FSE_DOCUMENTS/nrcs142p2_052523...

 

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Uploaded on October 28, 2010
Taken on October 15, 2008