Page 209 - Reservoir Formation Damage
P. 209

190   Reservoir Formation  Damage

                  The instantaneous porosity  of  a given cross-sectional  area  is given by:

                  ty  =                       ty 0-£ p                     (10-23)

                  and  (()  denote  the  initial  and  instantaneous  porosity  values,  e  is  the
                (|) 0
                fractional  bulk  volume  of  porous  media  occupied  by  the  deposited
                particles,  given  by

                                                                          (10-24)
                  e p=m p/p p
                   is  the  mass  of particles  retained  per  unit volume of porous  media and
                m p
                  is  the  particle  grain  density.  For  convenience,  these  quantities  can  be
                p p
                expressed  in  terms  of  initial  and  instantaneous open  flow  areas,  A fo  and
               Ay>  and  the  area  covered  by  the  particle  deposits,  A  ,  as
                  ty  = A f/A                                              (10-25)

                  $ 0=A fo/A                                              (10-26)

                  e p=A p/A                                               (10-27)

                Substituting  Eqs.  10-25  through  10-27,  Eqs.  10-23  and  24  become,
                respectively

                  A / 0 =A / + A p                                        (10-28)

                                                                          (10-29)
                  A p=Am p/p p
               The  particle  mass  balance  for  a  thin  core  slice  is  given  by:


                              + m )}                   = 0                (10-30)


                subject  to  the  initial  conditions:


                                                                          (10-31)


                      and  (Ppf)  are  the particle mass concentrations in the  flowing  phase
               at themlet  and  outlet  of  the  core.  Wojtanowicz  et  al.  (1987,  1988) omitted
               the  accumulation  of particles in the thin  core  slice and  simplified  Eq.  10-30
               to  express  the  concentration  of  particles  leaving  a thin  section  by:
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