Page 56 - Reservoir Formation Damage
P. 56

40    Reservoir Formation Damage

                              1.2
                                       Ngwenyaetaldata
                               1
                                       Correlation of
                                       Ngwenyaetaldata
                           ?  0.8      Linear (Ngwenyaet
                                       al data)
                           £f  0.6

                              0.4

                              0.2

                               0
                                             10          20          30
                                               t i*(hr  1/2 )

                Figure  2-26. Correlation  of  permeability  reduction  during  swelling
                (after  Civan,  ©1999  SPE; reprinted  by  permission  of  the  Society  of  Petro-
                leum  Engineers).




                fit  of  Eq.  2-31 using  Eq.  2-6  for  5  was  obtained  using  the  parameter
                values  of A = a sw  (c l  -  c 0)/h  = 0.035,  hjD  = 1,  and K tIK 0  = 0.087.
                   It  is  apparent  from  Figures  2-25 and  26  that  the  quality  of  both  the
                Hart  et al.  (1960)  and the Ngwenya  et  al.  (1995)  experimental  data  does
                not  permit  determining whether Eqs. 2-6  or  9 with Eq. 2-31 better rep-
                resents  the  data.  Because  Eq.  2-6  led  to  successful representation  of  the
                other  data  correlated in the preceding  sections,  it is reasonable to  assume
                that  Eq. 2-6  should also represent  the permeability  reduction data equally
                well.  Therefore,  Eq.  2-6  may be  preferred  over  Eq. 2-9.

                Discussion   and  Generalization

                   The  preceding  analyses  of  the  various  data  indicate  that  the  variation
                of  the  moisture,  volume,  and  permeability  of  clayey  formations  during
                swelling  by  exposure  to  water  is  governed  by  similar  rate  equations,
                which  can  be  generalized  as  (Civan,  1999):

                                                                           (2-34)
                   -d(f-f t)/dt  =  k fS(f-f t)

                subject  to  the  initial  condition

                                                                           (2-35)
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