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Inorganic Scaling and Geochemical Formation Damage  337


             Aqueous   Speciation   Models
               Aqueous  Speciation models  describe  the  thermodynamic  properties  of
             aqueous  solutions and they  are  an integral part of the  geochemical  models.
             Plummer  (1992)*  summarizes  the  constituents  of  these  models  as:

               1.  Mass  balance  equations  for  each  element,
               2.  Mass  action  equations  and their  equilibrium constants, for  complex-
                  ion  formation,  and
               3.  Equations  that  define  individual  ion-activity  coefficients.
               Two  types  of  aqueous  specification  models  are  popular:  (a) ion-
             association  models  and  (b)  specific interaction  models.  The ion  association
             and  the  specific  interaction  models  facilitate, respectively,  the  extensions
             and  a  complex  expansion  of  the  Debye-Hiickel  theory  to  estimate  the
             individual  ion  activity  coefficients  of  aqueous  species  (Plummer,  1992).
             The  specific  interaction  models  are  preferred  for  highly  concentrated
             solutions  of  mixed-electrolytes  (Plummer,  1992).  As  pointed  out  by
             Plummer  (1992),  aqueous  geochemical  models  can  be  used  for  forward
             and  inverse  geochemical  modeling.


             Geochemical    Modeling—Inverse      and  Forward
               Plummer  (1992)*  summarizes  that  "Two approaches  to  geochemical
             modeling  have  evolved—"inverse  modeling,"  which  uses  water  and  rock
             compositions  to  identify  and quantify  geochemical  reactions,  and  "forward
             modeling,"  which  uses  hypothesized  geochemical  reactions  to  predict
             water  and  rock  compositions." However,  the  application  of  these  models
             is  rather  difficult  because  the  basic  data  necessary  for  these  models  are
             often  incomplete  and/or  uncertain  (Plummer,  1992).
               Plummer  (1992)*  describes  the  most  essential  information  necessary
             for  geochemical  modeling  and  its  applications  as  following:
               1.  The  mineralogy,  and  its  spatial  variation  in  the  system,
               2.  The  surface  area  of  reactants  in  contact  with  aqueous  fluids  in
                  ground-water  systems,
               3.  The  chemical  and  isotopic  composition  of  reactants  and  products
                  in  the  system,
               4.  The  hydrology  of  the  system,
               5.  The  extent  to  which  the  system  is  open  or  closed,

             *  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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