Page 112 - Reservoir Formation Damage
P. 112

Permeability  Relationships  95

             saturation  ratio,  and  n  is  a  process  rate  exponent.  The  porosity,  (|),  and
             the  volume  fraction  of  the  deposits  in  the  pore  volume,  a,  are  related,
             respectively,  by:

                §o  =<)> + £                                            (5-77)

                e =  <j> 0a                                             (5-78)

               Once  the porosity  is calculated,  the  permeability  can  be  determined  by
             Eq.  5-71. Civan  (2000)  verified  this  approach  using the  Koh et  al.  (1996)
             data  for  permeability  impairment  by  silica  deposition.

             Effect  of  Deposition/Dissolution  and
             Stress  on  Porosity  and  Permeability

               Civan  (2000)  modified  the  equations  of  Adin  (1978),  Arshad  (1991),
             Tien  et  al.  (1997),  and  Civan  (1998)  as:



                                                                        (5-79)



                                                                        (5-80)
                K-K


             in  which,  the  subscripts  o and  °° indicate  the initial  and  terminal  porosity
             and  permeability  values,  oc ( :« = 1,2,...,8  are  empirical  parameters,  and
                 denotes  the  effective  overburden  stress  given  according  to  Nieto  et
             p eff
             al.  (1994)  and  Bustin  (1997)  as:


                Peff=Pob-ap Pf                                          (5-81)

             in  which  a  is Biot's  constant,  and  p ob  and  p pf  are the overburden  stress
             and  pore  fluid  pressure,  respectively. Civan  (2000)  verified  these  equations
             using  the  data  by  Nieto  et  al.  (1994)  and  Bustin  (1997).

             Effect  of  Temperature   on  Porosity  and  Permeability

               Gupta  and  Civan  (1994)  and  then  Civan  (2000)  formulated  the  varia-
             tion  of  porosity  and  permeability  by  temperature.  Representing  the
             volumetric  thermal  expansion  coefficient  of  the  porous  media  grains  by
             the  linear  equation
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