Page 105 - Reservoir Formation Damage
P. 105

88    Reservoir Formation Damage

                Then  the  permeability  diminishes  even  though  the  porosity  may  be
                nonzero.  Another  important  issue  is  the  criteria  for  jamming  of  pore
                throats. As demonstrated by Gruesbeck  and Collins  (1982) experimentally
                for  perforations,  the  probability  of jamming  of flow  constrictions  depends
                strongly  on  the  particle  concentration  of  the  flowing  suspension  and  the
                flow  constriction-to-particle  diameter  ratio.
                   The  pore  plugging  mechanisms  are  analyzed  considering  an  infini-
                tesimally  small  width  slice  of  the  porous  core.  The  total  cross-sectional
                area, A,  of  the porous  slide  can  be  separated  into  two  parts:  (1)  the  area
                A p,  containing  pluggable  paths  in  which  plug-type  deposition  and  pore
                filling  occurs,  and  (2)  the  area,  A np,  containing  nonplugging  paths  in
                which  nonplugging  surface  deposition  occurs.  Thus,  the  total  area  of
                porous  media  facing  the  flow  is  given  by:

                   A -  A p + A np                                         (5-36)


                The fractions  of the bulk volume containing the  plugging and nonplugging
                pathways  can  be  estimated  by  (Civan,  1995,  1996):


                   f  =                                                    (5-37)

                        A
                   fnp  = npI A  ~ §np/$                                   (5-38)
                where  <|> p,  § np,  and  <()  denote  the  porosities  of  the  plugging, nonplugging,
                and  overall  flow  pathways.
                   Thus,  by definition:


                   /„+/«, = !                                               (5-39)

                The  fraction  of  the  plugging  pathways  is  a  characteristic  property  of
                porous  media  and  the  particles  of  the  critical  size,  comparable  or  larger
                than  the pore throat  size  (Gruesbeck  and Collins,  1982;  Schechter,  1992).
                As  explained  in  Chapter  8,  the  pore  size  distribution  of  the  porous
                medium  and  the  size  distribution  of  the  particles  determine  its  value.
                However,  its  value  varies  because  the  nonplugging  pathways  undergo  a
                transition  to  become  plugging  during  formation  damage.
                   The volumetric flow rate,  q,  can  also  be  expressed  as a sum of the flow
                rates,  q p  and  q np, through  the pluggable  and nonpluggable  paths  as:

                                                                           (5-40)
                   q = q p + q np
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