With the aid of chromatographic columns containing a clay mineral dispersed on asbestos, ion-exchange processes on this mineral have been studied. The results of isotopic exchanges show that the columns do not run under equilibrium conditions. These isotopic exchanges do make possible a correction procedure which serves to produce isotherms for cases of true ion-exchange. The details of the correction procedure are given together with some results for a cesium-sodium exchange on a montmorillonite from Chambers, Arizona.
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Faucher et al. (1952) studied this question.
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