Page 189 - Reservoir Formation Damage
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Crystal Growth and Scale Formation in Porous Media  171

             The minimum  critical particle radius  for  a homogeneous nucleus  to  form
             a  stable  deposit  at  a  given  super  saturation  state  can  be  estimated  by
             equating  the  derivative  of  Eq.  9-17  to  zero:


                                                                        (9-18)
                      AG,,+£

             Thus,  the activation  energy  necessary  for  starting homogeneous  nucleation
             can  be  estimated  by  substituting  Eq.  9-18  into  Eq.  9-17  as:


                AG  =•
                                                                        (9-19)

                                Crystallization   Kinetics

               The  time  necessary  to  initiate  nucleation  of  crystals  from  a  super-
             saturated  solution  is called  "induction  time"  (Reddy,  1995). It  is a function
             of  the  solution  supersaturation,  that  is,  the ratio  of the  ion  activity product
             to  the  solubility  product  of the  precipitating  crystalline  matter  as  demon-
             strated  in  Figure  9-4  by  Reddy  (1995)  for  calcium  carbonate  nucleation
             in the presence of magnesium  ions. Figure 9-4 indicates that  the  induction
             time  is  lower  for  higher  supersaturation.  Below  the  supersaturation  value
             of  about  10, the  induction  time  for  calcium  carbonate  nucleation  is  very
             long.  In  this  region,  the  solution  is  at  a  "metastable"  condition and,
             therefore,  calcium  carbonate  crystals  cannot  be  formed  without  the  aid
             of  a  matching  growth  surface  or  substrate  (Reddy,  1995).  It  can  also  be
             observed  that the  presence  of magnesium ions  increases  the induction time
             for  calcium  carbonate  nucleation  and  therefore  has  a  retardation  and/or
             inhibition  effect.  Reddy  (1995)  explains  the  magnesium  ion  inhibition  of
             calcium  carbonate  nucleation  by  adsorption  of  the  magnesium  ions  and
             thus, the  occupation  of  some  crystal  growth  sites  on the  calcium  carbonate
             crystal  surface.  For  a  quantitative  interpretation  of  this  phenomenon,
             Reddy  (1986;  1995) resorts  to  a  growth  rate  analysis  and  a  Langmuir
             adsorption  isotherm  model  using  experimental  data  obtained  by  a seeded
             growth  method.  He expressed  the crystal  growth rate  as being  proportional
             to  the  surface  available  for  crystal  growth  and  the  square  of  the  driving
             force  for  precipitation:

                dN/dt  =                                                (9-20)

             where  N  represents  the  calcium  carbonate  crystal  concentration  in  the
             solution  in  moles/liter,  t  denotes  the  time  measured  from  the  time  of
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