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ION–ION INTERACTIONS 279

             This individual ionic-activity coefficient can be transformed into a mean ionic-
         activity coefficient by the same procedure as for the Debye–Hückel limiting law (see
         Section 3.4.4). On going through the algebra, one finds that the expression for log
         in the finite-ion-size model is






             It will be recalled, however, that the thickness  of the ionic cloud can be written
         as [Eq. (3.85)]




         Using this notation, one ends up with the final expression







             If one compares Eq. (3.119) of the finite-ion-size model with Eq. (3.90) of the
         point-charge approximation, it  is  clear  that the  only  difference  between the  two
         expressions is that the former contains a term  in  the  denominator. Now,
         one of the tests of a more general version of a theory is the correspondence principle;
         i.e., the general version of a theory must reduce to the approximate version under the
         conditions of applicability of the latter. Does Eq. (3.119) from the finite-ion-size model
         reduce to Eq. (3.90) from the point-charge model?
             Rewrite Eq. (3.119) in the form







         and consider the term   As the solution becomes increasingly dilute, the radius
            of the ionic cloud becomes increasingly  large compared with the ion size, and
         simultaneously    becomes increasingly small compared with unity, or






         Thus, when the solution is sufficiently dilute to make   i.e., to make the ion
         size insignificant in comparison with the radius of the ion atmosphere,the finite-ion-
         size model Eq (3.119) reduces to the corresponding Eq. (3.90) of the point-charge
         model because the extra term        tends to unity
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