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                    274                                          4. Adsorption and Ion Exchange


                    e  Adsorption and isotopic e xc hang
                    In the following analysis, adsorption models for solid diffusion control are applicable for
                    xchange,
                    isotopic e i.e. exchange of isotopes, while in the case of liquid diffusion control
                    and the intermediate case, only adsorption models for linear equilibrium can be used for
                    isotopic e xchange.
                      Furthermore, as will be analyzed in practical applications, the adsorption models can
                    also be used as a first approximation for ion-exchange systems, i.e. in the exchange of ions
                    of different valences.
                    Infinite fluid volume and solid diffusion contr ol  Practically, infinite solution v olume
                    condition (  w  << 1) amounts to constant liquid-phase concentration. For a constant dif fu-
                     olume,
                    sivity and an infinite fluid v the solution of the diffusion equations is (Helf ferich,
                    en, 1962; Ruthv 1984)
                                                      ∞
                                                    6   1        22
                                          Ut ()     2 ∑    exp     n     T
                                               1
                                                      n   1  n  2                      (4.35)
                    where   U ( t ) is the fractional approach to equilibrium at time   t and is defined as

                                                                                       (4.36)
                                              Ut ()    q   q) / (  q  )
                                                  q(
                                                     t  o   ∞   o
                    where:
                            q  o    solute initial concentration in the solid phase
                            q      equilibrium concentration in the solid phase
                            q  t    the a v erage concentration of the solute in solid phase at time   t , def ined as
                                  (Ruthven, 1984)


                                                      3  r o  2
                                                  q    2 ∫  qr  r d
                                                   t                                   (4.37)
                                                      r  o  0
                    where   r is the particle radius. For a solid phase initially free from solute,  o  q  o  is zero and thus


                                                     q    C  C
                                               Ut ()    t     o  t                     (4.38)
                                                     q  ∞  C  o  C    ∞

                    where   C ’s are the corresponding fluid-phase concentrations. i
                      The dimensionless time   T is defined as


                                                        Dt
                                                    T     s                            (4.39)
                                                         r  2
                                                         o
                    where   D  s  icient. is the solid dif f fusion coef
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