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The Vermiculitization of Trioctahedral Micas
Clay Minerals, 1973AbstractThe alteration of thirty-nine trioctahedral micas to vermiculite has been characterized by the K level, which is determined by repeated measurements of the stationary K concentration in the altering solution and provides a practical way of comparing the sensitivity to alteration.
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Laboratory Alteration of Trioctahedral Micas
Clays and Clay Minerals, 1972AbstractArtificial alteration of thirty-five trioctahedral and one dioctahedral micas by solutions varying in strength from 0·001 to 1·00 molal magnesium sulfate was found to approximate a normal exchange reaction after surface effects are eliminated. The equilibrium constants for the reaction:1/2Mg2++K−mica=Mg1/2−mica+K+(vermiculite)$1/2 {Mg^{2+}}+K ...
Syed N. Hoda, William C. Hood
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