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Autor:
Yen-Kuan Tseng, 曾嚴寬
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Clay minerals are composed of tetrahedral (T) and octahedral (O) sheets. The ones with T/O ratio of 1 are referred to as 1:1 type, whereas those with T/O ratio of 2 are referred to as 2:1 types. Cation substitutions in the structures of clay
Clay minerals are composed of tetrahedral (T) and octahedral (O) sheets. The ones with T/O ratio of 1 are referred to as 1:1 type, whereas those with T/O ratio of 2 are referred to as 2:1 types. Cation substitutions in the structures of clay
Externí odkaz:
http://ndltd.ncl.edu.tw/handle/85395016226716977785