Page 322 - Standard Handbook Petroleum Natural Gas Engineering VOLUME2
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Fluid Movement in Waterflooded Reservoirs   489


                   A  recent  analytical extension  [299] of  the  Dykstra-Parsons method  allows
                 calculations of  total flow rates and flow rates in each layer for both a constant
                 injection rate and for a constant pressure drop. The ability to calculate cumula-
                 tive injection into a layer allows the incorporation of sweep efficiency of  each
                 layer as a function of  mobility ratio and displaceable pore volumes injected for
                 the pattern used in the waterflood.
                 Crossflow.  In the usual cases where there is vertical communication between
                 the different layers of varying permeabilities, the effect of vertical crossflow must
                 be considered [300,301]. Goddin et al. [301] performed a numerical simulation
                 in a 2-D, 2-layer, water-wet system. For mobility ratios ranging from 0.21 to 0.95,
                 oil recovery with crossflow was between that computed for a uniform reservoir
                 and that for a layered reservoir with no crossflow. Goddin et al. [301] defined
                 a crossflow index, which is a measure of  the extent the performance varies from
                 that of  a uniform permeability system:

                                  N,,  - N,,
                   crossflow index =                                          (5-225)
                                  N,  - Npd
                 where NPU = oil recovery from uniform system with the average permeability
                       N,   = oil recovery from layered system with crossflow
                      Npnd = oil recovery from stratified system with  no crossflow
                 Of  the variables investigated, mobility ratio  and the permeability ratio of  the
                 two  layers had  the largest effect on crossflow (see Figures  5165  and  5-166,
                 respectively). Crossflow was more pronounced at lower mobility ratios or at high
                 ratios  of  layer  permeabilities.  The  crossflow index  of  one  means  that  the
                 performance of the layered system with crossflow is identical to the performance
                 of  the system with uniform permeability.
                   Still at  issue  is  the  relative  importance  of  mobility ratio  and  gravity in
                 waterflooding stratified reservoirs  [302-3061.  For  wetting conditions that  are
                 not strongly water-wet,  additional complications will  arise.

                 Estimates of Volumetrlc Sweep Efficiency. Volumetric sweep efficiency ranges
                 from  about  0.1 for  very  heterogeneous  reservoirs  to  greater  than  0.7  for
                 homogeneous reservoirs with good flooding characteristics [278].  For a liquid-
                 filled, 5spot pattern, Craig [298] found that the volumetric sweep efficiency (EJ
                 at breakthrough decreases sharply as the permeability variation increases (see
                 Figure 5-167). Similar trends were  observed for initial gas  saturations of  10%
                 and 20%. These data indicated that the major effect of mobility ratio on E, at
                 breakthrough occurs for mobility ratios ranging fmm 0.1  to  10.
                   More  recent  simulations [307]  of  5-spot patterns with  a streamtube model
                 yielded the volumetric sweep efficiencies shown in Figures 5-168 and 5-169 for
                 WORs of  25 and 50, respectively. Mobility ratios of 0.1,  1,  10, 30, and 100 were
                 used. The permeabilities in the  100-layer model were assumed to have  a log-
                 normal distribution, and pseudo-relative permeability expressions were used. In
                 a companion paper  [308] the  streamtube model (no crossflow) was  compared
                 to  the  Dykstra-Parsons method  (no crossflow) and  with a  model having the
                 assumption  of  equal  pressure  gradient  in  each  layer  (with crossflow). The
                 streamtube  model  was  more  closely  described  by  the  model  with  vertical
                 communication for unfavorable (high) mobility ratios and by the Dykstra-Parsons
                 model for favorable (low) mobility ratios.
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