Page 35 - Percolation Models for Transport in Porous Media With
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26                           CHAPTER2.  ONE-PHASE FLOW IN ROCKS

         complexity of the electric current flow  problem in a two-phase media, no solution
         for  other geometries of channels is  available at present.  Therefore it is  suggested
         in determining the electric conductivity of a grained medium  that parameters of
         cylindrical channels be chosen correspondingly.  Any channel connecting pores in
         a grained medium can be represented as two cylindrical channels of equal lengths
         h = l2  = l/2 but of different  effective  radii.  After setting the radius of the thin
         channel  to equal  r  and  the  radius  of the  thick  one  to  be  of the  same order  of
         magnitude as  the radius l/2 of the grain and  using  (2.3),  we find  the expression
         for  Po  in  the explicit form

                                                                             (2.6)


            In  (2.6),  the  relationship 4A' /((T'l)  ~  1 was  taken  into account.  When  radii
         of channels  are large enough  (2A' /(u'r)  ~  1),  the  surface  conductivity  may  be
         neglected and the formula (2.6)  reduces to

                                          1
                                                    2
                                    Po= -,l[1 + (l/r) ].
                                        1fU
         2.2  "Permeability- Porosity"  Correlation

         Since  the  distribution  function  of conducting channels  with  respect  to  intrinsic
         conductivities is not always known, finding the correlation between the coefficient
         of permeability and the porosity of a medium is of a certain practical interest.  In
         this  approach,  it is  certainly impossible to take account of the effects  caused  by
         differences in intrinsic conductivities of the channels in a grained medium.  However
         for  those grained  media,  whose  permeability is  determined  primarily by  a group
         of capillaries with  approximately equal intrinsic conductivities, such a method is
         justified.  Therefore we shall draw our attention to the model of a grained medium
         discussed in  §2.1  (see fig.  5).
            Let !l>o  be the porosity of the model structure in question (further called struc-
         tural porosity of the medium).  Structural porosity is  related to the coefficient of
         charge as follows,  f  = 1 - !l>0 •  Suppose that some of the sites are trapped with
         impermeable substance,  and  thus  the porosity of the medium  is  ![>  < !l> 0 •  If the
         distribution of trapped sites  in  the  network is  random,  the  probability of a  site
         having non-zero conductivity can be found  from  the relationship

                                        ps =  ![> / !l>o                     (2.7)

            The  threshold  value  of  the  conductivity  probability P:  of  a  site  when  an
         IC  is  formed  is  P:  = 0.16f- 1  in  the  three-dimensional  case.  The  coefficient
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