Page 579 - Petrophysics
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546    PETROPHYSICS: RESERVOIR ROCK PROPERTIES


                    3.  The inter-porosity fluid transfer coefficient is given by Equation 8.85:


                           3792 (1.4 x       (0.47)(0.2922)
                       h=
                                     (78.6) (0.22)

                         = 4.27 x

                       The high value of fluid  transfer coefficient indicates that  the fluid
                       transfer from matrix to fractures is very efficient.

                      l(b) TDS technique
                      From Figure 8.32, the following characteristic points are read:

                    Atmin  = 0.22 hrs  (t*AP’)R = 10.9 psia  (t*AP’)-  = 4.76 psia


                    1. Using the TDS technique, the value of k is obtained from Equation 8.87:


                                     -
                       k=  70.6qpB0  -  70.6 (17000) (0.47) (1.74)  = 78.3 mD
                           h(t*Ap’)R         (1150) (10.9)
                    2. The inter-porosity fluid transfer coefficient is given by Equation 8.88:






                             42.5(1150)  (1.4 X      (0.292)’
                                                                      - 4.267 x
                                      (17000) (1.74)


                    3. The storage coefficient o is calculated from Equations 8.91:





                                     0.0002673 x  78.3
                            =                               x 0.22 = 80,968.8
                               (0.47 x 0.2922 x 0.0000014


                                                     1
                          o=                                                 = 0.25
                               2.9114 - 3.5668/ ln(0.70783) - 6.5452/0.70783

                       The conventional semilog analysis yields the same values of k, o and
                       h as the TDS technique. The main reason for this match is that both
                       parallel straight lines are well defined.
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