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172  Membranes for lndustrial  Wastewater Recovery and Re-use


          4.1 Computer-aided design for  reverse osmosis plant



          4.1.1 Introduction
          It  has  already  been  pointed  out  (Section  2.3.2) that  modelling  of  filtration
          processes is not feasible on a universal basis, and that only reverse osmosis can
          be  modelled  on  the basis  of  solution-diffusion.  In  such  a  case,  modelling  is
          possible using simple analytical expressions provided the water can be treated as
          a continuum essentially free of the more complex interactions introduced by the
          presence of dispersed particles, solute precipitation effects (gel layer formation)
          and/or biological  activity  at the membrane-solution  interface. As  a  result  of
          these complicating factors, which relate largely to porous membrane processes,
          computer-aided  design  (CAD) software is currently available  only for reverse
          osmosis membranes and modules. The software packages are based on a series of
          calculations that enable the estimation of the RO array design and operation. It is
          instructive to review these CAD packages, which are produced by RO membrane
          manufacturers  and  suppliers  based  on  their  own  products,  with  a  view  to
          ascertaining their general usefulness and limitations (Brauns,  200 1).


          4.1.2 Key  elements  of  the reverse osmosis process
          Modelling  of  the  reverse  osmosis  process  relies  on  accurate  mathematical
          representation of

            0  the osmotic pressure,
            0  concentration polarisation, and
            0  the  hydraulic resistance  offered  by  the  membrane and  the  membrane
                channels.

            As already discussed (Section 2.3.1), the pressure required to drive a reverse
          osmosis  process  relates  both  to  the  permeability  of  the  membrane  and  the
          osmotic pressure. The osmotic pressure is solute concentration related, and can
          be very high for highly saline solutions: the osmotic pressure for seawater  (3 5 g lF1
          NaCl) is around 27 bar. No  flow of  water  takes place  unless this  pressure  is
          exceeded. At  moderate  concentration values,  osmotic  pressure  varies  almost
          linearly with concentration for many univalent salts, including sodium chloride,
          according to the van't Hoff equation (Chapter 2, Equation (2.9)). In this equation
          y depends  on the degree of  dissociation  of  the salt. Non-linear  correlations  of
           ll with C have been fitted to Taylor series and power relationships:

              " = RT(YlC1 + y2c2 + . . .)
               n = yRTC"
            Any one of  the above relationships  may be employed in existing RO design
          sortware.
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