Page 239 - Well Logging and Formation Evaluation
P. 239

Solutions to Exercises               229

               Some generic sat/ht curves for a range of porosities are shown below:


                    200
                                                          Hafwl (m)
                    180
                                                         250.000
                    160                                  200.000  porosity
                    140
                   Pc (psi, res cond)  120               150.000     0.05
                                                                     0.1
                    100
                                                                     0.12
                                                                     0.15
                     80
                                                                     0.18
                     60
                     40                                  100.000
                                                         50.000
                     20
                     0                                   0.000
                       0.0   0.2   0.4    0.6   0.8    1.0
                                       Sw


                  CHAPTER 5: ADVANCED LOG INTERPRETATION
                                      TECHNIQUES

            Exercise 5.1. Shaly Sand Analysis


               The BQ v relationship is as follows:

                                        Cwa vs 1/por

                       200
                       180
                       160
                      Cwa (1/ohmm)  120
                       140
                       100
                        80
                        60
                        40
                        20
                        0
                          0       5       10       15      20       25
                                             1/por


                           f
               BQ v = (018 - ) (0 02*f )
                                .
                       .
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