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Membrane technology  5 1


             0  viscosity of the fluid,
             0  diffusivity of the solute, and
             0  permeability of the cake.

             Some  of  the  analytical  expressions  developed  for  the  equilibrium  length-
           averaged flux are included in Table 2.12. The solution varies according to the
           approach taken and the assumptions made, but the general trend is for transport
           of  solute away from the membrane to be much higher than that predicted by
           Brownian diffusion. This changes the degree of dependency of flux on both cross-
           flow velocity (and so shear rate, according to Equations (2.18) and (2.19)) and
           particle size changes significantly from the Brownian diffusion LevEque model if
           either shear-induced  diffusion  or  inertial  lift  are included. For  example, flux
           dependency  on  cross-flow  changes  from  U0.33 proportionality  to  direct
           proportionality for shear-induced diffusion (Zydney and Colton, 1986) or U2 for
           inertial lift (Drew et al.,  1991). Kim and Park (1999) based their prediction of
           critical flux conditions on shear-induced diffusion.
             A  comprehensive, and complex, solution  for equilibrium flux in CFMF  has
           been presented by Romero and Davis (1988). This model accounts the effects of
           shear-induced diffusion on a non-uniform filter cake whose thickness increases
           with  axial  membrane (channel) distance.  This  is  considerably  more  complex
           than the model  for  thin  cake  deposits  (Zydney  and  Colton,  1986), where  a
           uniform cake deposit over the whole membrane area is envisaged, and requires
           that  the  solute  concentration  dependency  of  viscosity  and  diffusivity  be
           predetermined. More recently, the Romero and Davis model has been slightly
           simplified by  basing the cake layer resistance on the Kozeny-Carman  equation
           (Ould-Dris  et al., 2000).

           Practml verification of  modified  models
           Experimental studies on model colloidal or particulate systems have shown close
           agreement  between experimentally  measured  steady-state flux data and those
           predicted from shear-induced diffusive mass transport theory for ideal systems,
           such  as  latex,  blood,  bacterial  and  fractionated  clay  suspensions  (Zydney
           and Colton, 1986). The model of  Kim  and Park (1999) for predicting  critical
           flux,  again  based  on  shear-induced  diffusion,  appears  to  corroborate  well
           with  experimental  data  from  calcium  carbonate  filtration,  the  critical  flux
           increasing  linearly  with  particle  size. Inertial  lift, on the other  hand, would
           appear to be restricted  in importance to high shear rates and/or large particles
           (Davis, 1992).
             The shear-induced  diffusion model for thick cake layers (Romero and Davis,
           1988, 1990) was found to give a reasonable representation of both dynamic and
           steady-state  behaviour  for  both  rectangular  channels  and  ceramic  tubular
           membranes challenged with homodispcrsed spheres of  0.45-1.3 7 pm (Romero
           and Davis, 1991). Ould-Dris et al. (2000), using a slightly simplified adaptation
           of  the  Romero  and Davis  model,  also  found  reasonable  agreement  between
           theoretical and experimental steady-state flux for their trials on the less idealised
           system of granular calcium carbonate. Agreement was only obtained, however,
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