The ion-exchange equilibria between a montmorillonite clay and potassium-cesium from chloride solutions have been studied by chromatographic and other methods. The results are summarized in terms of equilibrium constants and activity coefficients for the mixed clay phase. A tentative discussion is given of the rate of the exchange process, particularly as it affects the behavior of the chromatographic columns.
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Faucher et al. (1954) studied this question.
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