Page 359 - Reservoir Formation Damage
P. 359

Inorganic Scaling and Geochemical Formation Damage  339

               7.  Calculation  of  mineral  solubilities  with  and  without accompanying
                  irreversible  reaction,
               8.  Calculation  of  boiling,  cooling,  wall-rock  alteration,  ground-water
                  mixing  with  hot  waters  and  evaporation,  and
               9.  Equilibrium  or partial  equilibrium states in gas-solid-aqueous  systems.
               Plummer  (1992)*  states  that  forward  geochemical  modeling  can  be
             used  "in  developing  reaction  models  that  can  account  for  the  observed
             compositional-mineralogical  relations  in  the  deposit,  if  there  are  no
             aqueous  or  solid  data  for  the  system."

             Reaction-Transport    Geochemical     Modeling

               The reaction-transport  models  describe the geochemical reactions under
             the  influence  of  fluid  flow  and  convective  and  dispersive  transport  of
             various  species  in  geological  porous  media.  These  models  couple  the
             geochemical  reaction  and  the  fluids  and  species  transport  submodels  to
             accomplish  temporal  and  spatial  prediction  of  the  evolution  of geo-
             chemical  reactions  in compositionally-complex geological  systems (Plummer,
             1992).  These  models  are  more  applicable  in  most  petroleum  reservoir
             exploitation  and  scale  formation  studies.


                             Graphical   Description   of  the
                           Rock-Fluid    Chemical   Equilibria

               Properly  designed  charts  provide  convenient  means  of  describing  the
             equilibrium  chemical  reactions  of  the  rock-fluid  systems.  Frequently,
             the pe -  pH,  activity-activity,  and saturation  index  charts  are facilitated for
             convenient  description  of  equilibrium  chemical  systems. The  con-struction
             of  these  charts  are  based  on  the  description  of  chemical  systems at  thermo-
             dynamic equilibrium. In this  section,  the theoretical  bases,  characteristics,  and
             utilization  of  these  charts  are  described  according  to  Schneider  (1997).

             Saturation  Index   or  Mineral  Stability  Charts

               Mineral  stability  charts  are  convenient  means  of  representing  the
             various equilibrium reactions  of the  solid  minerals  and  aqueous  solutions
             in  geological  porous  media  in  terms  of  the  saturation  index  concept.

             * Reprinted from  "Water-Rock  Interaction,"  Proceedings  of the  7th international symposium,
              WRI-7,  Park  City, Utah,  13-18 July  1992  Kharaka, Y. K.  & A.  S. Maest  (eds.),  90 5410
              075  3,  1992,  25  cm,  1730  pp.,  2  vols.,  EUR  209.00/US$246.00  GBP147.  Please  order
              from:  A. A.  Balkema, Old  Post  Road,  Brookfield, Vermont 05036  (telephone:  802-276-
              3162;  telefax:  802-276-3837;  e-mail:  info@ashgate.com).
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