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94              CHAPTER 5.  NON-STEADY STATE TWO-PHASE FLOW

















                 Figure 30:  Diagram of the formation of the "crown" of a "tree"


            In principle, the rates of the growth of lateral branches are different.  To simplify
         calculations  we  may  average  these  rates  and  introduce a  certain  average rate of
         growth of the branches for  a  given  tree.  It is  obvious that the higher the rate of
         growth of the trunk, the higher the average growth rate of its branches due to the
         expansion  of the range of radii of r 1-chains forming  the  branches.  Without  loss
         of generality we may take the proportionality factor in the mentioned dependence
         equal to unity, which means that the average rate of the branches' growth is equal
         to the rate of the growth of the trunk
            If condition  {5.6)  is  satisfied,  blocking  of all  trees  formed  by  V-chains  with
         V  < V1  takes  place.  The other trees continue their growth.  It can be seen from
         {5.6),  that blocking of a  V 1-tree is  possible by  branches of different  trees growing
         with  a  higher  rate,  but  will  occur  at  different  distances  x.  It is  obvious  that
         actual  blocking  of the  considered  trial  tree  will  be  carried  out  by  those  trees,
         whose branches are connected at the minimum value x, to which corresponds the
         satisfaction of the following condition

                                        dxfdV 0  = 0.                        {5.7)

            Thus, taking into account the obvious equality


                                                                             (5.8)

         we obtain a system of three equations for  the three unknowns V 0 ,  V1 ,  and x(Vt),
         it being obvious a priori, that V 0  > V1 •  This system is solvable for  any values of
         Xf·
            Consequently, the considered region may  be conventionally divided into three
         zones.  When x > x 1 one-phase flow without changing of saturation occurs.  When
         x  < x(Vt) flow  of the displacing phase is  observed through surviving tree trunks
         corresponding to the values V  > Vt(x).  Here V 1{x)  is determined from  (5.6)-{5.8)
         as an inverse function  to x(Vi).  The permeability of the displacing phase in  this
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