As part of a general study of the theory of ternary ion exchange in zeolites, a simple model is developed for the evaluation of the required activity-coefficient ratios in dilute solutions containing three salts. The application of this model is discussed with particular reference to ternary or multicomponent exchange in zeolites.
P. Fletcher and R. P. Townsend, J. Chem. Soc., Faraday Trans. 2, 1981, 77, 2077 DOI: 10.1039/F29817702077
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