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286  CHAPTER 3


           3.5.6. The Debye–Hückel Theory of Ionic Solutions: An Assessment
               It is appropriate at this stage to recount the achievements in the theory of ionic
           solutions described thus far. Starting with the point of view that ion–ion interactions
           are bound to operate in an electrolytic solution, in going from a hypothetical state of
           noninteracting  ions to a  state in  which the  ions of species i interact  with the  ionic
           solution, the chemical-potential change  was  considered a quantitative measure
           of these interactions. As a first approximation, the ion–ion interactions were assumed
           to be purely Coulombic in origin. Hence, the chemical-potential change arising from
           the interactions of species i with the electrolytic solution is given by the Avogadro
           number times the electrostatic work W resulting from taking a discharged reference
           ion and charging it up in the solution to its final charge In other words, the charging
           work is given by the same formula as that used in the Born theory of solvation, i.e.,






           where    is the electrostatic  potential  at  the surface  of  the  reference ion that is
           contributed by the other ions in the ionic solution. The problem therefore was to obtain
           a theoretical expression for the potential   This involved an understanding of the
           distribution of ions around a given reference ion.
               It was in tackling this apparently complicated task that appeal was made to the
           Debye–Hückel simplifying model for the distribution of ions in an ionic solution. This
           model treats only one ion—the central  ion—as a discrete charge, the charge of the
           other ions  being  smoothed out  to  give  a continuous  charge density.  Because of the
           tendency of negative charge to accumulate near a positive  ion, and  vice versa,  the
           smoothed-out positive and negative charge densities do not cancel out; rather, their
           imbalance gives rise to an excess local charge density   which of course dies away
           toward zero as the distance from the central ion is increased. Thus, the calculation of
           the distribution of ions in an electrolytic solution reduces to the calculation of the
           variation of excess  charge density   with distance r from the central ion.
               The excess charge density  was taken to be given, on the one hand, by Poisson’s
           equation of electrostatics






           and on the other, by the linearized Boltzmann distribution law
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