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OILWELL TESTING                                    216

                                                                                          5
                     multi-rate test in a gas well presented in the original Odeh-Jones paper  for a well
                     positioned at the centre of a circular shaped area of radius 3000 ft (A ≈ 650 acres) and
                                                                                     -5
                     for which the permeability is 19.2 mD. In the example t DA = 9.2×10 , and for the
                     geometry considered, transient analysis can be applied for a total of 1086 hours. It is in
                     cases where reservoirs are not continuous and homogeneous over large areas but
                     splintered into separate reservoir blocks on account of faulting that errors can occur in
                     assuming the infinite reservoir case is applicable in the test analysis.


                     One further, complication arises in connection with this type of analysis, and that is,
                     that in order to apply the correct technique, using the general p D function, equ. (7.42),
                     requires a knowledge of the permeability in order to calculate t D or t DA. In buildup
                     analysis this presents no problem since k can be readily calculated from the slope of
                     the linear section of the buildup plot. In multi-rate testing, however, this can prove more
                     difficult. Sometimes it is possible to separately analyse the initial flow period by plotting
                     p wf versus log t and applying the transient analysis technique described in exercise 7.2.
                     Unfortunately, in high permeability reservoirs this is very difficult to apply in practice,
                     since the pressure fall-off is initially very rapid. Under these circumstances it may be
                     necessary, and indeed is always advisable, to conduct a buildup at the end of the flow
                     test which tends to defeat one of the main purposes of the multi-rate test, namely, to
                     avoid well closure.

                     It is commonly believed that multi-rate flow tests can only be analysed if the initial
                     equilibrium pressure within the drainage volume is known. This is an unnecessary
                     restriction which has tended to limit the application of this technique to initial well tests
                     for which p i can be readily determined. The following analysis shows that, with minor
                     modifications to the method presented so far, the multi-rate test can be analysed with
                     only a knowledge of the bottom hole pressure and surface production rate prior to the
                     survey.

                     Suppose that a well with the variable rate history shown in fig. 7.29 is to be tested by
                     flowing it at a series of different rates.

                                                                                         th
                     Prior to the test the well is produced at a constant rate q N during the N  and final flow
                     period before the multi-rate test commences at time t N. Then, for any value of the total
                     time t n during the test, when the current rate is q n, the bottom hole flowing pressure p wf n
                     can be calculated as


                                      kh              n
                                                              t
                           7.08 10 − 3    ( i  p wf  ) =     ∆ q p D  ( D  −  t D  )  + q S
                                ×
                                           p −
                                                          j
                                                                          n
                                                                     −
                                      µ B o      n   j1         n   j 1
                                                      =
                     in which p i is the initial pressure at t = 0 and the summation includes all the variable
                     rate history up to and including the test itself. This equation can be subdivided as
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