Page 253 - Reservoir Formation Damage
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Single-Phase Formation Damage by Fines Migration and Clay Swelling  233

             pack  decreased  to  zero.  Because,  in  the  fine  sand  pack,  almost  all  the
             pathways  are  of  the  plugging type. Whereas,  in  coarse  sand  packs,  the
             deposition  tended  to occur  almost uniformly along  the  sand  pack  and the
             mean  permeability  of  the  sand  pack  decreased  to  an  equilibrium value.
             Because,  in  the  coarse  sand  pack,  most  of  the  pathways  are  of  the
             nonplugging  types.
                Gruesbeck  and  Collins  (1982)  state  that  their  computer  simulation
             produced  results similar to measurement reported in Figure  10-27. Civan
             et  al.  (1989),  and  Ohen  and  Civan  (1990,  1993) also  simulated  these
             experiments  successfully.

             Consolidated  Core  Tests.  Gruesbeck  and  Collins  tested  Berea  and  field
             cores.  First,  the  Berea  cores  were  tested  using

                1.  2%  KCl  brine  in  a  dry  core  (single  phase  system)
                2.  2% KCl brine and white oil  at a 50/50  ratio in  a dry  core (two phase
                  system)
                3.  white oil  in  a  dry  core  (single phase system)
                4.  white  oil  in  a core  at connate  2% KCl brine  saturation  (two phase)

                Cores  were  tested  at  various  constant  injection  rates  over  a period  of
             time  determined by  a prescribed, cumulative pore  volume amount of  the
             injection  fluid.  During  each  test,  the  pressure  difference  was  measured
             and  the  permeability  was  calculated  using  Darcy's  law. Typical  results
             obtained  using  a  2% KCl  brine  in  a  Berea  core  are  presented  in  Figure
              10-28. As  can  be  seen,  the  permeability remained unchanged at  the  low
                                  3
             flow  rate  of  0.0367cm /-?,  while  it  decreased  further  at  each  of  the
                                                                           3
             increased  high  flow  rates  of  0.0682,  0.1002,  0.1310,  and  0.1702cm /s.
             The  final  permeability  values  attained  after  each  of  the  high  flow  rates
             are  used  to  calculate  the  permeability  reductions  from  the  initial  state,
             which  are  then  plotted  against  these  high  flow  rates  as  shown in  Figure
             10-29.  The  results  shown  in  Figure  10-29  are  indicative  of  surface
             particle  removal,  similar  to  Figure  10-24.  They  stated  that  the  removal
             of indigeneous particles in the  cores  from  the pore  surface and subsequent
             redeposition  at  the  pore  throats  caused  the  permeability  reduction.
                Second,  core  samples  were  taken  from  an  oil  field,  indicating  an
             abnormal decline  of productivity in  some wells.  These  cores were tested using

                1.  white  oil  in  a  dry  core
                2.  white oil  in  a  core  at  connate  2%  KCl  brine saturation.

             The  experimental  results  presented  in  Figure  10-30  indicate  a  trend
             similar  to  Figure  10-29.
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