Page 111 - Reservoir Formation Damage
P. 111

94    Reservoir Formation Damage

                Power-Law    Flow-Units Equation

                  Civan  (1996,  2000)  expressed  the  mean-pore  diameter  as  a  three-
                parameter  power-law  function  of  the  pore  volume  to  solid  volume  ratio:



                       = Yi                                                (5-71)


                in  which  a,  P and  y  are empirical  parameters,  and usually a  =  1.  P and
                y depend  on  the  pore  connectivity  and  can  be  correlated  as  a function  of
                the  coordination  number,  Z,  respectively,  by:


                     1
                         1
                   p- /p- . 0 =l-exp(-CZ + D)                              (5-72)
                        = i - exp(-AZ + fl)                                (5-73)


                The interconnectivity parameter  can  also  be approximated  by  a power  law
                function  of  porosity  as  (Civan,  1996):

                   y = cty n                                               (5-74)


                in  which  c  and  n are empirical  parameters,  y  is  zero  when the  pores  are
                blocked  by  deposition.  Civan  (2000)  verified  the  validity  of  Eqs. 5-71
                through  74  using  the  data  by  Rajani  (1988),  Verlaan  et  al.  (1999),  and
                Bhat  and  Kovscek  (1999).

                Effect  of  Dissolution/Precipitation  on
                Porosity  and Permeability

                  Civan  (2000)  expressed  the  precipitation/dissolution  rate  by:

                   d£
                     = *, (F-1)«|> 0-£)"                                   (5-75)
                   dt

                subject  to  the  initial  condition

                                                                           (5-76)

                where,  t  is  time,  k }  is  a  rate  constant,  (|) 0  is  the  initial  porosity,  e is
                the  volume  fraction  of  deposits  in  porous  media,  F  is  the  solution
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