Page 127 - Percolation Models for Transport in Porous Media With
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120                           CHAPTER 6.  PORE SIZE DISTRIBUTION

         respect to those presented in  §6.2 if the percolation model of transfer phenomena
         (described in part 1), instead of the approximate effective medium model, is used.
            The scheme of the experimental measurement of the specific electric conductiv-
         ity uy for the medium is as follows.  A specimen with cross-section S*  and height
         L  is  placed  in  a  container with  mercury,  and  the latter is  injected  in  the speci-
         men under pressure p.  After making a current I  pass through the specimen and
         measuring the voltage drop U on it its resistance Ro = U /I, the specific electric
         conductivity  O'y  = L/(S* Ro)  is  found.  After carrying out a  series of such  mea-
         surements for different values {Pi} of pressure and relating them, according to the
         Laplace formula,  to the minimal capillary radius ri = 2xcos0/Pi  where mercury
         can pass,  we  obtain  the dependence uy(ri).  This correlation can  be either rep-
         resented in  the form  of an interpolated curve or tabulated for  further  numerical
         processing on a computer.
            Specific electric conductivity can be calculated using the percolation model of
         a  heterogeneous medium according to (2.4), using the formula
                                         [1

                                                         f(r)
               av(r;) = A" l [ l f(r) dr r /(r) ~ r 1 dr f(r) dr            (6.27)

         where A" is a numerical factor, rc  is the critical percolation radius.
            If we now consider the function uy(ri) known and the function  f(r)  unknown,
         then (6.27} becomes a nonlinear integral equation for  f(r).  After differentiating it
         once with respect to ri and making some transformations we obtain



             f(r;) = -1/A"(dav/dr;) l f(r) ~; [! f(r)dr] -• [! f(r)dr] -I   (6.28}


         or, if we introduce the following notations



                  ~(r;) = -1/A"(davfdr;) [! f(r)dr] -u [! f(r)dr] -I,       (6.29)







         a  nonlinear inhomogeneous Volterra equation of the second type in the standard
         form

                                                                            (6.30)
                                           r;
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