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ION–ION INTERACTIONS 299
























          coefficients  only in concentrated solutions. At extreme dilutions, only the ion–ion
          long-range Coulombic interactions are important.
              In order to test Eq. (3.130), which is a quantitative statement of the influence of
          ionic hydration on activity coefficients, it is necessary to know the quantity  and  the
          activity  of  water, it being assumed that an experimentally calibrated value of the
          ion size parameter is available. The activity of water can be obtained from independent
          experiments (Table 3.12). The quantity  can  be  used as a parameter. If Eq. (3.130)
          is tested as a two-parameter equation  and a being the two parameters; Table 3.13),
          it is found that theory is in excellent accord with experiment. For instance, in the case
          of NaCl,  the calculated activity coefficient agrees with the experimental value for
          solutions as concentrated as     (Fig. 3.39).
              Since the quantity  is  the  number  of  moles of water  used  up in solvating
                    moles of ions, it can be split up into two terms:  moles  required  to
          hydrate      moles of cations, and   moles required to hydrate  moles  of anions.
          It follows that      and        are the hydration numbers (see Chapter 2) of
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