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ION–SOLVENT INTERACTIONS  77



















                      Fig. 2.21. Generic radial distribution functions for (a)
                      a well-coordinated liquid with a long-lived coordination
                      shell and (b) a weakly coordinated liquid. (Reprinted
                      from J. E. Enderby, Chem. Soc. Rev. 24: 159, 1995.)


          Evidently the  first  layer is  about the  same  when  filled for  both  the two-  and the
          three-valent ions, and perhaps the IR spectrum does not register effects given by a
          second layer of water. One might indeed well expect the first layer of water around an
          ion to be full, and therefore expect the same for the two- and three-valent cations of
          similar radii.
             The presence of electrolytes in solution is often ill characterized spectroscopically
          by vague shoulders or bumps that make the interpretation hazardous and lacking in
          quantitative information on the ion–solvent structure. However, far IR does allow one
          to understand the  spectra and  obtain knowledge of the ion–solvent structure.  For
          example, it is important to distinguish contact ion pairs (CIP) in the spectrum. These
          must be clearly identified and their effects allowed for before the spectrum can be used
          to obtain knowledge of ion–solvent interactions (Fig. 2.21).

         2.11.3. The Neutron Diffraction Approach to Solvation

             The seminal event in the foundation of solid-state science was the realization by
          von Laue that the ordered structure of atoms in a crystalline solid might act as a
         diffraction grating for X-rays. The corresponding formula by Bragg,




         This represents the path-length difference with θ as the glancing angle (see Section
          5.2.3) allowed d, the distance between atoms, to be determined for the first time. The
         path to structure determination was open.
             X-ray analysis works when there are indeed ordered rows of atoms in a crystal. It
          also works in an examination of the structure of molten salts (Chapter 5), when there
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