Page 226 - Reservoir Formation Damage
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206   Reservoir Formation Damage

                  u np=uK np/K                                           (10-118)

                  Considering  that  the physical properties  of the  particles  and the  carrier
                liquid  are  constant,  the  volumetric  balance  of  particles  in  porous  media
                is  given  by:

                  9/9?((|>(j + e) + 9/9jt(a«) = 0                        (10-119)


                Substituting  Eq.  10-100  into  Eq.  10-119,  and  then  rearranging,  an
                alternative  convenient  form  of  Eq.  10-119  can  be  obtained  as:

                  ($ 0 - e) 9a/9? + 3/9x(ou) + (1 - a) de/9r = 0          (10-120)


                  Following  Gruesbeck  and Collins  (1982), Eq.  10-120 can be simplified
                for  cases  where e and a  are small compared  to  (|) 0  and unity, respectively,
                and  for  constant  injection  rate,  as:


                  (|) 0 — + u — + — = 0                                  (10-121)


                  The  initial  particle  contents of  the  flowing  solution  and porous  media
                are  assumed  zero:


                  a  = a 0 = 0,  £ = 8 0,  0 < x < L,  t = 0             (10-122)

                where  L  is  the  length  of  porous  medium.  The  particle  content  of  the
                suspension  of  particles  injected  into  the  porous  media  is  prescribed  as:


                  a = a in,x = Q,t>Q                                     (10-123)

                  Alternatively,  the  pressures  of  the  inlet  and  outlet  ends  of  the  porous
                media  instead  of the  flow  rate  can be  specified.  Then,  the  volumetric  flux
                can  be  estimated  by  the  Darcy law:

                                                                         (10-124)

                Substituting  Eq.  10-124  into  the  volumetric  equation  of  continuity


                                                                         (10-125)
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