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Physical chemistry     124


        ionic concentration is sufficient to calculate the chemical potential or molar free energy
        of the ion (see Topics B6, C1 and D1). At higher ionic concentrations, ionic interactions
        become significant,  γ i is typically less than unity and electrostatic interactions are
        important in determining thermodynamic data.



                                      Ionic strength
        The overall degree of electrostatic ionic interactions is measured by  using  the  ionic
        strength of the solution, I. This is given by:




        and involves adding the contribution of every ion in solution, i, using the concentration of
        the ion c i and the formal charge or charge number, z i. The charge number for a general
               x+
                                         y−
        cation M is x and for a general anion X  is −y. For a 1:1 electrolyte where x=1 and y=1,
        I is equal to the solution concentration, c. For electrolytes where x and/or y are greater
        than 1, I>c, which reflects the greater electrostatic interaction of ions of higher charge
        with other ions.


                              Calculation of activity coefficients

        When the electrostatic interactions between ions and  counterions  are  relatively  weak
        compared with their thermal energy, k BT (i.e. at low dilution), the distribution of ions and
        potential at any distance from any ion can be calculated. The effect on the energy of the
        system of the electrostatic interactions that result can then be quantified. This procedure
        results in the Debye-Hückel law:







                                                                −3
        which can generally be applied to solutions of  I≤0.01 mol dm   (for which this
        assumption of relatively weak electrostatic interactions holds). A is a constant for a given
        solvent (0.509 for water at 298 K), B is a constant for a given ion in a given solvent
        (conveniently B is often approximately equal to 1 for most ions in water) and   is the
                                                           −3
        standard ionic strength (defined as being equal to 1 mol dm ). This allows the mean
        activity coefficient, γ ±, to be calculated for a salt M y X x, where
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