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Membrane technology  43

           normally  denoted  A  and  B,  respectively.  According  to  this  approach,  the
           transport of solute is not directly related to transmembrane pressure.
             The osmotic pressure l7 is given by the well-known van’t Hoff equation:

               n = yRTCC,

           where  R  is  the  gas  constant,  T  the  absolute  temperature,  CC, the  total
           concentration of individual solute ions and y the osmotic coefficient accounting
           for non-ideal behaviour. The coefficient y normally takes a value between 0.7 in
           concentrated solutions and unity at infinite dilution, and equates to the mean of
           the activity coefficients of  the dissolved  ions  and the degree of  dissociation.
           However, the relationship between  l7 and C is rarely linear, as Equation (2.9)
           suggests, due to departure from ideality at high concentrations.
             The simple solution-diffusion  model can be extended to account for pore flow
           by adding an extra empirical coefficient to the water and solute flux expressions.
           Use  of  the model is, however, constrained  by the necessity of determining this
           coefficient experimentally. The model can also be extended to allow coupling of
           solute and solvent flows, although this also introduces empirical constants.
             Pore flow models assume that the membrane is microporous with cylindrical
           pores. The membrane material is assumed to preferentially  adsorb water, as a
           monolayer,  both  within  the  pores  and  at  the  surface.  The  water  is  then
           transported  across  the  membrane  at  a  rate  depending  upon  chemical
           interaction, frictional  and diffusive forces.  The expression  can be  modified to
           account for steric and electrostatic effects, and can take account of the pore size
           distribution  of  the  membrane.  Charged  pores  tend  to  increase  the  effective
           viscosity of the water in the pores due to electroviscous effects, but these effects
           alone do not appear to account for reported charged  membrane permeability
           changes with ionic strength and pH.
             The Donnan equilibrium model takes account of solute charge and membrane
           charge which,  through repulsion  of  co-ions  and  attraction  of  counter-ions,
           creates  a  Donnan  potential  at the membrane surface.  This  has the effect of
           repelling co-ions and, since electroneutrality  must be preserved,  counter-ions
           are also rejected. This approach applies to both electrodialysis and nanofiltration
           and  can  provide  qualitative  trends,  but  does  not  allow  a  quantitative
           description  of  nanofiltration  since  it  does  not  take  account  of  diffusive and
           convective transport. The extended Nernst-Planck  equation has also been used
           to describe transport in charged membranes, but with similar limitations.


           2.3.2 Foulinglcake layer mass  transfer control

           Resistance model: cake filtration
           The  simplest  way  of  accounting for  the  additional  resistance  offered by  the
           material accumulating in the interfacial region is to simply add its resistance R,
           (the cake layer resistance) to that of  the membrane, such that Equation  (2.5)
           becomes:
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