Page 117 - Percolation Models for Transport in Porous Media With
P. 117

110                           CHAPTER 6.  PORE SIZE DISTRIBUTION

            The desired dependence rk(S) can be found  from  this equation, if the experi-
         mental dependence p1{S) is  known.  At  the time of trapping, the pressure in the
         gas  phase  coincides  with  the  pressure Po  in  the  outer cross-section  of the  core;
         therefore, the initial condition for the equation {6.12) is

                                    rk(S') =  2x cosO
                                        c   Pl(S~)-po
            When  the displacement  is  over,  the value  of porosity  cp  can  be found  as the
         ratio of the volume of mercury  that has  entered  the  pores  to  the volume  of the
         core.  This quantity can be also calculated as the product of the average capillary
         volume and the concentration of the edges of the network
                                             00
                                   cp = 1r;~z J f(r) dr                     {6.13)
                                                2
                                               r
                                             0
            The last expression represents another correlation between the constants z and
         l of the network.
            Thus the formulas  {6.5),  {6.8),  {6.12)  permit to find  the dependencies  X(rk)
         and  J(rk)  for  the  given  l  and  z.  To  determine  the  constants  z  and  l  from  the
         relationships  {6.9)  and  {6.13),  an  iterative  procedure  is  set  up  with  respect  to
         these parameters.  Once this is done, the quantity V is found from the relationship
         {6.6), and the dependencies X(rk) and f(rk) are determined in the domain of the
         macro-pores using this quantity at the first stage of displacement.
            The presented algorithm of data interpretation in mercury porometry was ob-
         tained for model II. Without drawing close attention to it, we note that the equa-
         tions describing the sequence of stages for  mercury injection in  a porous medium
         for model I can be derived in a similar fashion.
            Results of the calculations  using experimental data.  To  demonstrate
         the  efficiency  of the  outlined  method  for  the  experimental  data interpretation,
         we  shall  present  the  calculations for  the experiment  on  the displacement  of air
         by  mercury from  a  core extracted from  the East-Poltavian layer  (data given  by
         N.  V.  Savchenko).  The plot of the X(S) relationship for  this core appears in fig.
         38.  The obtained dependence  proved  to be stable with  respect  to small changes
         of the initial conditions.  The value of Sc  close to zero and the value of S~ close to
         unity are characteristic of this dependence.  For the specimen under consideration,
         Sc = 6.5 · w- ,  S~ = 0.964.
                     4
            The curve I  in fig.  39 corresponds to the initial experimental data.  The curve
         I I  is  obtained,  if a  relative error of 0.05  is  allowed  in  determining  the quantity
         S.  The greatest difference  between the two curves is achieved at the values of rk
         corresponding to the third stage of the experiment and makes 15%.  For the first
         two stages  this  difference  does  not  exceed  5%.  As  the  relative error goes  down,
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