Page 374 - Fundamentals of Reservoir Engineering
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NATURAL WATER INFLUX                                   309
                                    p i


                               p 0
                                                  p
                                                   1
                                     p 1
                                              p 1
                                                                p 2
                                        p 2
                                                           p 2
                                                                               p 3

                       PRESSURE                                          p 3









                                  0             t              t             t              TIME
                                                 1             2              3
                     Fig. 9.9   Matching a continuous pressure decline at the reservoir-aquifer boundary by
                                a series of discrete pressure steps




                     Suppose that the observed reservoir pressures, which are assumed to be equal to the
                     pressures at the original hydrocarbon-water contact, are p i, p 1, p 2, p 3 .... etc., at times 0,
                     t 1, t 2, t 3 .... etc. Then the average pressure levels during the time intervals should be
                     drawn in such a way that


                                p + p 1
                                 i
                            p =
                             1
                                  2
                                p + p 2
                                 1
                            p =
                             2
                                  2
                                                                                                    (9.15)



                                p  + p
                                 −
                            p =  j 1  j
                             j
                                   2
                     The pressure drops occurring at times 0, t 1, t 2 . . . etc. are then
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