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ION–SOLVENT INTERACTIONS  173

          manufacture upon salting in. However, the salting in with which they are associated
          is not the rare deviant phenomenon arising when the dipole moment of the nonelec-
          trolyte is greater than that of water. It possesses the characteristic of always being
          associated with organic electrolytes in which the ions are large. Here, even when water
          has a dipole moment greater than that of the nonelectrolyte, which would be expected
          to give salting out, salting in occurs.

          2.20.5. Cause of Anomalous Salting In

              The picture given above seems satisfactory as a first approximation and for dilute
          solutions, but it has this one disturbing feature; namely, there are situations where
          theory predicts salting out but experiment shows salting in. In such cases, the theory
          seems to favor ions being surrounded by water whereas in fact they move away from
          water (hydrophobic effects). Now, it will be recalled that only ion–dipole forces have
          been reckoned with in treating the interactions among the particles populating the
          primary solvation shell. Thus, the ion–water and ion–nonelectrolyte forces have been
          considered to  be  of  the  ion–dipole  type of directional  forces  which orient polar
          particles along the ionic field. Perhaps this restriction is too severe, for there are also
          nondirectional forces, namely, dispersion forces.
              These dispersion forces can be  seen  classically as  follows: The time-average
          picture of an  atom may  show  spherical  symmetry  because  the charge due to the
          electrons orbiting around the nucleus is smoothed out in time. However, an instanta-
          neous picture of, say, a hydrogen atom would show a proton “here” and an electron
          “there”—two charges separated by a distance. Thus, every atom has an instantaneous
          dipole moment; of course, the time average of all these oscillating dipole moments is
          zero.
              Now, an instantaneous dipole in one atom will induce an instantaneous dipole in
          a contiguous atom, and an instantaneous dipole–dipole force will arise. When these
          forces are averaged over all instantaneous electron configurations of the atoms and
          thus over time, it is found that the time-averaged result of the interaction is finite,
          attractive, and nondirectional. Forces between particles that arise in this way are called
          dispersion forces.
              Dispersion forces give rise to an interaction energy in which the potential energy
          of interaction varies as  where r is the distance between the centers of the two
          substances interacting. Thus, the equation for the dispersive energy of interaction may
          be written as  where  is a constant independent of r. The rapid decrease of such
          forces with increase of distance from the origin makes it unnecessary to consider
          dispersion interactions outside the primary solvation shell; by then, they have already
          decreased to an extent that they no longer warrant consideration. Inside the primary
          hydration  sheath, the dispersion  interaction can be treated in the same way as the
          ion–dipole interaction. That is, in the replacement of a water molecule by a nonelec-
          trolyte molecule, one must take into account not only the difference in  ion–dipole
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