Page 210 - Petroleum Geology
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187

               Secondary migration  updip follows a  path,  or paths, of  local minimum
             potential - much as rivers do - and migration continues until the oil arrives
             in a position of  minimum potential with respect to the physical constraints
             of the cap rock.  Here it accumulates. The quantity that can accumulate de-
             pends on the volume of this space of minimum potential, and on the quanti:
             ties of  oil generated. If the space of minimum potential becomes entirely fill-
             ed  with oil, further secondary migration to it will result in overflow from the
             spill point,  which  is a local position  of  minimum potential with respect  to
             the accumulation, and so the process will continue until the oil either reaches
             another space of  minimum potential or dissipates at the surface.
               The rate of  migration  of  the oil depends not only on the vertical dimen-
             sion, the physical properties  of  the oil, and the lithology  of the carrier bed,
             but also on the relative permeability to oil, which is a function of the water
             saturation (Fig. 9-5).
              We  noted  on  p.  168 that  experimental  curves of  relative  permeability
             show  a  hysteresis  effect, depending on whether the initial water saturation
             was zero or one. The advancing oil front is an injection of oilinto 100% water
            saturation.  This part, therefore, corresponds to drainage - from a practical
            point of  view, the drainage curve for water saturations less than the critical
            oil saturation required  for a continuous oil phase. In this part of the relative
            permeability curves, the relative permeability to oil is very small, and that to
            water, quite high. We infer, therefore, that much of the pore water is displaced
            at the oil front so that the water saturation within the migration oil column
            is such that the relative permeabilities are at least better balanced (sw = 0.6-
            0.7).
              If  there is a “tail” or retreating oil front at the lower end, this corresponds
            to imbibition, and the water  saturation increases here at least to the critical
            saturation at  which  continuity  of  the oil phase is lost. The relative perme-

                    Oil  saturation
               1                      0
              1
             L
            -k
            ”
            h
            .-  -
            .-
            P
            0
            E
            n
            P
            .-
            ”
            -
            a
            0
            U
              0
                  Water  saturation  sw
               imbibition-    -drainage
            Fig. 9-5. Relative-permeability-water  saturation diagram.
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