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42  Membranes for Industrial Wastewater Recovery and Re-use


          Table 2.7  Dense membrane rejection expressions based on different models (based on
          Bhattacharyya and Williams, 1992)
          Approach          Rejectiond                        Reference
                                       1    -I
          Solution-diffusion                                  Lonsdale et al. (1 965)
                             (1 + 5 (-)
                                                              Sherwoodetd.
          Solution-diffusion    K,     1    - 2 (A)) (1967)
          imperfection              AP-  AR
          Surface force pore                                  Matsuura and Sourirajan
          flow                                                (1981): Sourirajan and
                                                              Matsuura (1985)
                             1 - ( yY  (;;)  - (
          Donnanequilibrium             ;)itiZ)   lir         Bhattacharyya and
                                                              Chen (1986)
          a b,  dimensionless frictional force (frictional force acting on solute in pore vs. that acting on solute in
                                                                            ACs,
          bulk solution): Cw  concentration of water in the membrane: Cs, exp(y,)/[l + (expv, - l)(b&xp&)]: ~
          solute concentration difference across the membrane = C,1  - Cs2:  Csl.sl, solute concentration on feed,
          permeate side of  membranc: Cz,  concentration of  co-ion in bulk  solution; &, (Brownian) diflusion
          coefficient of water in the membrane;  Ds. (Brownian) diffusion coefficient of solute in the membrane: Kw,
          water permeability in the membrane, &C,VdRT;   Ks, solute permeability in the membrane, DS+;  K3,
          empirical coefficient:  Qm, charge  capacity of  membrane: R,  gas  constant: ~p  dimensionless  radial
          distance (r/rp):  T, absolute temperaturc: yr, dimensionless radial velocity (v&v(~=,,&   V,,  partial molar
          volume of water: y. 2,  charge on species y (the co-ion) and z (counter-ion) respectively:Y,Z,  ( Yz+ + Zy-:  y,
          ym,  activity  coefficients in  solution  and  membrane  respectively:  membrane  thickness:  K~, solute
          distribution coefficient: p, osmotic pressure: &,  dimensionless  electrostatic  or  van der Waals  forces
          parameter.


            0  extended Nernst-Planck  equation, and
            0  irreversible thermodynamics.

            Pure solution-diffusion  is based upon the assumption that both the solute and
           solvent (i.e. water) dissolve in a homogenous non-porous membrane and then
          diffuse across it as discrete (uncoupled) materials. The overall rate of transfer (i.e.
          flux) of  each, and thus the purity of  the permeate product, depends upon their
          relative solubilities and diffusivities (Lonsdale  et a]., 196 5):
                                 Kw
               Solvent (water) flux:  - (AP - An)                          (2.7)
                                  A

                              KS
               Solute (salt) flux:  - (AC,)
                               A

           where  AP and  Ax, respectively,  represent  the  applied  transmembrane  and
           osmotic  pressures,  ACs  is  the  solute  concentration  difference  across  the
           membrane,  Kw  and  Ks  represent  the  water  and  solute  permeabilities  in
           the membrane and A is the membrane thickness. The ratios Kw/A  and Ks/L are
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