Page 61 - Principles of Catalyst Development
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42  Principles of Applied  Reservoir Simulation


                             dx\      -'
                             j f l    ,<,K  ^c  I                   (5,12)
                               * i

        The derivative (dxidi) Sw  is the velocity of the moving plane S w, and  (dfJdS w) Sw
        is the  slope of  the  fractional  flow  curve. The  integral  of the  frontal  advance
        equation gives


                             rs  -  W <  (  dL \                    (5J3)
                               -~7*    \7s~l
                                        \    ' $„
        where
                          distance traveled by a particular S w contour [ft]
               x Sw
                Wj        cumulative water injected  [cu  ft]
                (df w/dsj\  slope of fractional flow curve



        Water Saturation  Profile
             A plot of S w versus distance using Eq. (5.13) and typical fractional flow
        curves leads to the physically  impossible  situation of multiple values of S w at
        a given location. A discontinuity in S w at a cutoff location x c is needed to make
        the water saturation distribution single valued and to provide a material  balance
        for wetting fluids. The procedure is described by Collins [ 1961 ] and summarized
        below.


                                5.2 Welge's  Method

             In  1952, Welge published an approach that is widely used to perform the
        Buckley-Leverett  frontal  advance  calculation.  Welge's  approach  is  best
        demonstrated  using a plot off w  vs S w (Figure  5-2).
             A  line is drawn  from  the water saturation  S w  before the waterflood  -
        irreducible water saturation S wirr -  and tangent to a point on thef w  curve. The
        resulting tangent line is called the breakthrough tangent, or slope. It is illustrated
        in Figure 5-2. Water saturation at the flood front S^is the point of tangency on
             curve. Fractional flow of water at the flood front is/^and occurs at the
        thef w
        point of tangency S^ on the/ w curve. In Figure 5-2, S wf\s  65% and/ w/is 95%
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