Page 247 - Fundamentals of Reservoir Engineering
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OILWELL TESTING                                    185

                      7.2 (i.e. k = 240 mD, A = 35 acres, S = 4.5).

                                                                                          +
                                                 π
                           0.0189(3500 −   p ) = 2 t DA  +  ½  In  t DA  +  8.632  −   ½ p D(MBH)  (t ) 4.5  (7.46)
                                           wf
                                                                                       DA
                     in which
                                 .000264 kt        .000264 240   t (hrs)
                                                           ×
                                                                  ×
                           t DA  =            =
                                                               -6
                                   φµ  cA       .18 1 15 10 ×     35 43560
                                                                     ×
                                                           ×
                                                    ××
                           t DA  =  0.0154 t
                     For convenience, equ. (7.46) can be reduced to
                           0.0189 (3500 p )  =    α −  ½ p D(MBH)  (t )                             (7.47)
                                        −
                                                                DA
                                           wf
                     in which
                           α =  2t  DA  +  ½ ln t DA  + 13.132
                                 π

                     and has the same value for all three geometries shown in fig. 7.16. Values of p wf in
                     equ. (7.47) can therefore be calculated by reading values of p D(MBH) (t DA) from the
                     appropriate MBH plots contained in figs. 7.11-15. The values of ½ p D(MBH) (t DA) and p wf
                     for all three geometries are listed in table 7.4 for the first 50 hours of the drawdown
                     test. Plots of ∆p wf, which is the difference between the calculated and observed bottom
                     hole flowing pressure, versus the flowing time, are shown in fig. 7.17. These plots tend
                     to confirm that the geological interpretation, fig. 7.16(b), is appropriate. For the other
                     two rectangular geometries the late transient flow period is not modelled correctly. For
                     comparison the plot has also been made for the case of a well draining from the centre
                     of circular bounded area, which is the simple case normally considered in the literature.
                     As can be seen, the value of ∆p wf after 50 hours, when semi-steady state conditions
                     prevail, is 44 psi for this latter case.
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