Page 30 - Percolation Models for Transport in Porous Media With
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1.3  EFFECTS OF ELECTRIC CURRENT                                     21


                                    K l'
                                   K,z,









                                                   I




                                     1.'":---~-L--,...J
                                      D,.f   7      t/f,
         Figure 4:  Plots of electric conductivity (1)  and permeability (2)  of heterogeneous
         medium against time during electric treatment


            It is interesting to observe that when t- tk = ton/(n- 1), u1 (t)  ~ oo.  In this
         case, some chains in the network consist only of those elements which changed their
         conductivities when the electric current passed through them.  The dependencies
         E 0 (t)/E 0 (0) and K(t)/ K(O) are shown in fig.  4.  Also depicted there are the results
         of numerical modeling of the process in question for a plane square network with
         the number of sites 100 x 100 and the probability density function of the exponential
         type (1.19)  with n = 3, uo = 1.  Distribution of the potential in the network was
         found from the solution of the Laplace equation div (a\1¢) = 0, where the values of
         a were set by a pseudorandom number generator.  For a given probability density
         function,  the solution was found  using the relaxation method.  When the critical
         level  of the energy discharge was  achieved  at one of the bonds,  its conductivity
                          5
         was set to equal 10 .  Then to  was determined.  Numerical modeling showed that
         the  values  t 0  and  tk  agreed  well  enough  with  the  values  obtained  analytically
         for  various probability density functions.  It was  also showed that the analytical
         dependencies E 0 (t)/E 0 (0)  and K(t)f K(O)  agreed satisfactorily with the results of
         numerical modeling.
            Thus heterogeneity of a medium at the micro level causes sharp heterogeneity
         of the density of energy discharge in the conducting elements.  Such heterogeneity,
         in its turn, may cause significant changes in the conductivity of the medium even
         when relatively small electric fields  are applied to the medium.  Estimates show
         that such effects can be observed in rocks with notably heterogeneous pore space.
         Note that the change of the conductivity predicted by theory is quasi-volumetric,
         a property which makes this process different from those of the "breakthrough"
         type, where contraction of the current in the medium takes place.  The presence of
         a threshold, which defines the lower limit of the energy discharge when the rear-
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