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Clay Minerals; April 1984; v. 19; no. 2; p. 177-193
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The distribution of octahedral cations in the 2:1 layers of dioctahedral smectites studied by oblique-texture electron diffraction

Semen Ilosifovich Tsipursky, and V. A. Drits

U.S.S.R. Acad. Sci., Geol. Inst., Moscow, USSR

Examination of K-saturated dioctahedral smectites after 70-100 wetting-drying cycles allows the determination of cation distribution between trans and cis octahedra of the 2:1 layers. Studies of smectites with different compositions has revealed a wide variety of occupancies of the available octahedral sites.

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