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66                            CHAPTER 4.  MULTIPHASE FLUID FLOW

         permeabilities, the term in (1.8} which appears before the integral cancels out, and
         therefore the knowledge of l is not necessary.
            Flow with the initial pressure gradient.  The Binghamian plastic.  The
         friction law with limiting shearing stress in  the case of the flow  of a visco-plastic
         fluid  is defined  by  its structure in  the field  of the surface forces  at the points of
         contact with  the solid surface.  The most general form  of such law was given  by
         Wilkinson
                                                                            (4.16)

         where A  and B  are constants found  from  experiment.  For the calculation of the
         permeability in  accordance with  the given  algorithm,  the specific form  in  which
         the  law  <P( T 8 )  is  written  does  not  matter.  However  if  A  and  B  are  arbitrary
         constants, then after integrating, the expression (4.13}  becomes very complicated
         and  inconvenient for  further  use.  Therefore it seems  reasonable to consider,  for
         illustration, a rather frequently encountered specific case of (4.16},  when  A = r,,
         Bhs « 1, i.e., the Binghamian plastic.  Similar rheological properties can be found
         in heavy viscous oils which contain components with high molecular weights.
            In the outlined case the function <P( T 8 )  has the following form

                                                                            (4.17}
         Substitution of ( 4.17) into ( 4.17} yields the well-known relation of Bingham


                                                                            (4.18)


            (4.18} implies that even in the considered case (i.e., Vp* fVp < 1},  the ratio of
         the third term in  the square brackets to the second one is  "' 0.1.  Therefore it is
         possible to neglect  the third  term in  the square brackets and write the following
         for the local V  p
                                           8JL    4
                                   Vp(q) = -  4  q + - Vp*                  (4.19}
                                                  3
                                           11"T
            After  substituting  (4.19}  into  (4.14)  we  obtain  the value  of the macroscopic
         gradient                                      dr l (

                     .    8JL      00   dr   8~  00           00      )  -1
                Vp{rt) =   [  -;- q(rt) [  f(r) r' + -f [  f(r)-;   [  f(r) dr


         and


                      q(r,) = ~ Vp{r,) i f(r)dr (i f(r)::) _,
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