Page 127 - Partition & Adsorption of Organic Contaminants in Environmental Systems
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118   CONTAMINANT SORPTION TO SOILS AND NATURAL SOLIDS

           which can be expressed as

                                      d ln  S w  d ln C e
                                            >                             (7.4)
                                       dT      dT

           Since one finds that

                                       d ln  S w  D H w
                                             =                            (7.5)
                                        dT     RT  2

           and that

                                   d ln  C e  D H d  D H
                                         =      = -                       (7.6)
                                    dT     RT  2   RT  2

                                                                  H
           with DH d denoting the molar heat of desorption (i.e., DH  d =-D ), one there-
           fore finds that
                                       DH  > -DH  w                       (7.7)

           which means that the heat liberated when 1 mole of solute is sorbed to the
           soil is less exothermic than the solute’s reverse heat of solution in water. Equa-
           tion (7.7) explains the small exothermic heats of sorption of DDT (Pierce et
           al., 1974), lindane and b-BHC (Mills and Biggar, 1969), parathion (Yaron and
           Saltzman, 1972), and 1,1,1-trichloroethane (Chiou et al., 1979) on soil.
              Equation (7.7) is actually a consequent form of Eq. (3.23) for the molar
           heat of partition of a solute between an organic solvent and water. Since the
           heats of solution of organic compounds in an organic phase (DH o ) are gener-
           ally positive but small due to their improved compatibilities, DH  will be small
           for compounds with low positive DH w values and may even become positive
           (endothermic) for compounds with abnormal (negative)  DH w values. For
           example, Chiou et al. (1979) showed that the  DH  for 1,2-dichlorobenzene
           sorption by soil from water is nearly zero because of its low DH  w and that the
           DH  for 1,1,1-trichloroethane is positive because of its negative DH w in the
           temperature range 3.5 to 20°C. One may conclude from these data that in
           systems where the DH  values are negative, such exothermic heats originate
           primarily from condensation of the solutes from water (-DH  w) and that with
           DH o being normally positive, interactions between SOM and solute (DH o) are
           normally endothermic, as usually is the case for the heat of solution. One finds
                                                    H
           small and nearly constant exothermic heats (D ) (and hence small tempera-
           ture coefficients) in solute partition equilibria as a result of the partial
           cancellation in heat between  DH o and  DH w according to Eq. (3.23).
              The sorption data of p,p¢-DDT are especially worth noting because DDT
           is a solid with a large heat of fusion (DH fus), about 25kJ/mol (Plato and
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