Page 197 - Percolation Models for Transport in Porous Media With
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11.3  MODIFICATION OF PERMEABILITY                                   195

         resumes to conduct current.  Consequently the fluid  gets heated again,  then the
         bubbles grow, and the capillary is shut off.  Thus, as electric current passes through
         the medium, colmatation effects are cyclic.  This is also confirmed by experimental
         studies of cores saturated with a conducting leaching solution.  The results of these
         studies will be discussed in detail below.
            According to the upper expression in {11.54), when the losses due to the heating
         of the skeleton of the medium are not too intensive (for instance, in micro grained
         media)  and the liquid  contains a good  deal  of gas  (i.e.,  when  the density of the
         bubble germs  n.  is  large),  merging  of the  vapor  bubbles  in  the  thin  capillaries
         dominates in  the colmatation of the medium.  Furthermore colmatation will  take
         place  almost  at  the  same  time  in  all  r 1-chains  of the  rock.  This  must  have  a
         visual impression of abrupt termination of the fluid  flow  in  the rock.  As  for  the
         time  dependencies  ofthe  permeability  and  the  electric  current  flowing  through
         the medium,  they must have a typical form  of the percolation relations near the
         percolation threshold

                                K(t) ~ K{O){l- tftp)a',
                                  I(t) ~ J{O){l  - t/tp)P•,
                                    tp =<a*, t(rl), Tc  >

         where the exponents at and f3t  must be of the order of unity {less than one).
            If the density of the bubble germs is relatively small, then the merging of the
         bubbles and their independent growth may rival in some chains.  When the heat
         exchange between the liquid and the skeleton takes place (this happens when the
         specific heat of the rock is large, as in fractured media), colmatation can be long-
         lasting.  It is also possible in this case that a complete colmatation of the medium
         is not achieved.
            We shall now compare the obtained results to those of an experimental study
         of electric  treatment  of a  sandy-argillaceous  medium  saturated with  a  leaching
         solution.  The parameters of the medium, the liquid, and the electric treatment are
         to be set to equal those in the experiment, i.e., the specific electric conductivity of
         the fluid,  0' = 1.7 n- 1 m- 1 ; the characteristic size of a pore and a grain, I= 2·10- 4
                   1
         m;  the cross-section of the experimental tubes  (see  §9.2),  S 0  = 9 · 10- 4  m 2 ;  the
         number of conducting channels, in order of magnitude, No  ~ S 0  /1 2  = 2.3 ·10 4 ; the
         average capillary radius, r  ~ 8 · to- 5  m;  the amplitude of the alternating electric
         field  intensity,  Eo  =  180 V Jm;  the energy input density,  qp  !:'::!  5.5 · 10 watt per
                                                                       4
         m 3 •  Typical values of bubble radii and densities at NTP (p = 0.1  MPa, To = 293
         K {20°  C), T&  = 373 K {100°  C)) are a0  =10- 6 m, n. ~ 10 13  m- 3 •
            It follows from {11.15) and {11.17) for the parameters specified and for the vis-
         cosity J.t  = 10- 3  Pa· s,  that the time for establishing of a steady state movement,
         Ty  "' 10- 7  seconds,  is  much  less  than  the characteristic time of movement for  a
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