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13.26                    CHAPTER THIRTEEN

                        The  basic  behavior  of  permselective  (semipermeable)  membranes
        Design  Equations.
         can be described by the following two diffusion model equations.  Permeate flow through
         the  membrane may  be expressed  as
                                 Fw  =  A  ×  (Ptm -  "N'tm)
         where  Fw  =  water  flux,  g/(cm 2  • s)
               A  =  water permeability coefficient,  g/(cm 2  • s  • atm)
             Ptm   =  hydraulic  pressure  differential  applied  across  membrane,  atm
             7rtm =  osmotic  pressure  differential  across  membrane,  atm
         The  solute  (or salt)  flux  through the  membrane  may be expressed  as
                                  Fs  =  B  X  (C1  --  C2)

         where    Fs  =  solute  (or salt) flux,  g/(cm 2  • s)
                   B  =  solute  (or salt) permeability  constant,  cm/s
              Cl  -  C2  =  concentration gradient across  membrane,  g/cm 3
         Water  and  solute  permeability  coefficients  are  characteristic  of the  particular membrane
         type.
           Water flux depends on applied pressure, but solute flux does not. As pressure of mem-
         brane feedwater increases, water flow through the membrane (water flux) increases, while
         solute flow remains essentially unchanged. Permeate quantity increases with increased ap-
         plied pressure,  as  does  the quality  (decreased  solute  concentration).
           Water flux decreases as the salinity of the feed increases because of increased osmotic
         pressure differential resulting from increased salinity. As increasing amounts of water pass
         through  the  membrane  system,  the  salinity  of the  remaining feedwater  (concentrate) in-
         creases.  Concentrate  osmotic  pressure  increases,  resulting in  a  lower  water  flux  with in-
         creasing  overall percent  water  recovery.
           Finally, because salinity of the feed concentrate stream increases with increasing perme-
         ate production from a given volume of feed, and the membrane rejects a fixed percentage of
         solute, product water quality decreases (higher concentration) with increasing recovery. Table
         13.6 presents typical feed pressures and recoveries for RO  and NF  systems.

         TABLE  13.6  Typical RO and NF System Feed Pressure and Recovery

                                           Typical operating
                                              pressure         Typical  product
                 Application                                   water recovery,*
              (with example TDS)        psi          kPa            %
         Reverse osmosis
          Seawater (35,000 mg/L TDS)   800 to  1,200   5,520 to 8,270   30 to 45
          Brackish water (5,000 mg/L TDS)   350 to 600   2,410 to 4,140   65 to 80
          Brackish water (1,000 mg/L TDS)   125 to 300   860 to 2,070   70 to 85
         Nanofiltration
          Freshwater (500 mg/L TDS)   50 to  150   340 to  1,030   80 to 90
          *Maximum allowable recovery is site-specific and depends on the feedwater's scaling potential, membrane re-
         jection and product water quality requirements, concentrate stream osmotic pressure, and the use of scale-inhibit-
         ing chemicals.
          Source:  Adapted from Bergman, Robert A. "Anatomy of Pressure-Driven Membrane Desalination Systems."
         1993 Annual A WWA Conference Proceedings--Engineering and Operations. Denver, Colo.: American Water Works
         Association, 1993.
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