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The distribution of octahedral cations in the 2:1 layers of dioctahedral smectites studied by oblique-texture electron diffraction

Published online by Cambridge University Press:  09 July 2018

S. I. Tsipursky  and
V. A. Drits
S. I. Tsipursky
Affiliation:
Geological Institute of the USSR Academy of Sciences, Pyzhevsky per. 7, Moscow, USSR
V. A. Drits
Affiliation:
Geological Institute of the USSR Academy of Sciences, Pyzhevsky per. 7, Moscow, USSR
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Abstract

Olique-texture electron diffraction 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.

Type
Research Article
Information
Clay Minerals , Volume 19 , Issue 2 , April 1984 , pp. 177 - 193
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1984

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