Page 151 - Principles of Applied Reservoir Simulation 2E
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136  Principles  of  Applied  Reservoir  Simulation


        realize  that  the  relative  permeability curves  used  in  a  flow  model  are most
        representative of the type of experiment  that was used  to measure  the curves.
        Applying these curves to another type of displacement mechanism can introduce
        significant error.
             Several  procedures  exist  for averaging  relative permeability  data [for
        example, Schneider,  1987; Mattax and Dalton,  1990; Blunt,  1999]. In practice,
        relative permeability is one of the most useful physical quantities available for
        performing a history match. The curves that are initially entered into a reservoir
        model are often modified during the history matching process. The rationale for
        changing relative permeability curves is based  on the observation  that relative
       permeability  curves  are usually  obtained  by  flooding  core  in the  laboratory.
        Laboratory  floods  correspond  to a much  smaller  scale  than  flow through  the
        drainage area of a well. Therefore, it is easy to argue that the laboratory  curves
        are not representative of flow on the reservoir  scale. In the absence of measured
        data,  correlations  such as Honarpour, et al.  [1982] give a reasonable  starting
        point  for  estimating  relative  permeability.  Relative  permeability  hysteresis
        effects can also be included in reservoir simulation using a procedure  presented
       byKillough[1976].
             Capillary pressure is usually included in reservoir simulators. The relation-
       ship  between  capillary  pressure  and elevation  is  used  to  establish  the initial
       transition  zone in the reservoir.  The oil-water  transition  zone, for example, is
       the zone between water-only flow and oil-only flow. It represents that part of
       the  reservoir  where  100%  water  saturation  grades  into  oil  saturation  with
       irreducible water saturation. Similar transition zones may exist at the interface
       between  any pair of immiscible phases.
             Capillary  pressure  data  is used  primarily  for  determining  initial fluid
       contacts  and transition  zones.  It is also used  in fractured reservoir  models  for
       controlling  the  flow  of  fluids  between  the  fracture  and  the  rock  matrix.  If
       capillary pressure is neglected, transition zones  are not included in the model.
       This  is illustrated in Figure  14-2. Figure  14-3  shows  the  effect  of neglecting
       capillary pressure when a grid is used to represent the reservoir. The fluid content
       of the block is determined  by the location  of the block mid-point  relative to a
       contact between two phases. The block mid-point is shown as a dot in the center
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