Abstract: The relation between the differential exchange diffusion coefficient of two ions and the self-diffusion coefficients of the ions has been re-examined for the case where the ion flows induce a simultaneous migration of water, and an earlier treatment(1) has been corrected. In its application to Ca2+and Sr2+ion exchange diffusion in chabazite the new treatment leads to virtually the same numerical values of the differential and integral exchange diffusion coefficients as the earlier treatment.
Publication Year: 1964
Publication Date: 1964-09-01
Language: en
Type: article
Indexed In: ['crossref']
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Cited By Count: 14
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