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80 CHAPTER 2

            lifetime of water molecules is short, perhaps only  s.  For  multicomponent systems
            it is possible to have several internuclear distances and, correspondingly, a number of
            distribution functions. By applying Eq. (2.26) to the data for    such as that shown
            in the diagram, one can find out how many water molecules are in the first shell, as in
            the case of concentrated   solutions (Fig. 2.22).
               There are always water molecules located around a stationary ion and the structure
            of these waters will be dominated by the field of the ion (rather than the pull back into
            the structure of the water). This dominance is stronger the smaller the ion because the
            ion–solvent interaction is inversely proportional to   As the schematics of a typical
            distribution function suggest, there may be a second layer in addition to the first shell
            of solvent associated with the ion. In this layer the structure is not yet that of bulk
            water, though such second solvation layers are usually more prominent with divalent
            ions (they are even more so with 3+ and 4+ ions) and are not seen for univalent ions,
            in the company of which hydration waters stay for very short times.
               Now, the question is how to get information on the more subtle quantity, the
            hydration numbers. Some confusion  arises here, for in  some research papers  the
            coordination number (the average number of ions in the first layer around the ion) is
            also called the hydration number!  However, in the physicochemical literature, this
            latter term is restricted to those water molecules that spend at least one jump time with
            the ion, so that when its dynamic properties are treated, the effective ionic radius seems
            to be that of the ion plus one or more waters. A startling difference between co-ordi-
            nation number and solvation number occurs when the ionic radius exceeds about 0.2
            nm (Fig. 2.23a).
                It is important, then, to find out the time that waters stay with the ion. Thus, one
            can make an order-of-magnitude calculation for the jump time, by a method shown in
            Section 4.2.17. It comes to approximately
               One could conclude that if a water molecule stays with its ion for more than about
                   it has accompanied the ion in a jump. That is, during the time the water is
            associated with the ion, it is likely to have made one move with the ion in its sporadic
            random movements (and therefore counts as a hydration number rather than a static
                                         21
            or equilibrium coordination number).  Figure shows the ratio of the solvation number
            to the coordination number.  The ratio         is  an  important quantity

            21
              In the case of ions for which the ion–water binding is very strong (the transition-metal ions particularly),
             the hydration number may be greater than the coordination number, because more than one shell of waters
             moves with the ion and the hydration number will encompass all the water molecules that move with it,
             while the coordination number refers to the ions in just the first shell.
              However, with larger ions, which have weaker peripheral fields, there is less likelihood that a water
                                                                 –10
             molecule will stay for the time necessary to accomplish an ion movement (e.g., > 10  s). Thus, for larger
                     –                      +
             ions like CI  and large cations such as N(C 2H 5) 4 , the coordination number will be 6 or more, but the
             hydration number may tend to be 0. The hydration number is a dynamic concept; the coordination number
             is one of equilibrium: it does not depend on the lifetime of the water molecules in the shell but measures
             their time-averaged value.
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