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64                Well Logging and Formation Evaluation

            If you have a gas column above an oil column in the reservoir, gener-
          ate two set of tables, one for an oil/water system and one for a gas/water
          system using the appropriate s, q, rho h, and rho w values.

            Exercise 4.1. Core-Derived J Function

          1. Based on the core capillary pressure measurements presented in
             Appendix 2, derive a J function.
          2. Recalculate the sums and averages using the J function derived from
             these core data.



                         4.2 LOG-DERIVED FUNCTIONS

            The methodology applied to core data can also be applied to the logs
          to derive an independent J function, provided that the position of the FWL
          is known. This function is useful for comparison with the core-derived
          function and may be used if no core data are available.
            A secondary benefit is that it is possible during the fitting procedure to
          eliminate thin bed and invasion effects and provide a means of generat-
          ing a high-resolution saturation log that depends on only the density log.
            In order to fit a J function, follow these steps:


          1. Use the depth of the FWL and the true vertical depth subsea (TVDss)
             to generate a curve for the height above FWL.
          2. Use equation 4.3 to derive a curve for P c .
          3. Use equation 4.2 to derive a curve for J. It is assumed that you already
             have some kind of poroperm relationship that can be used to relate k
             to the porosity.
          4. Use equation 4.4 to derive a curve for S wr . Set S wirr to be 0.01 less than
             the lowest S w seen on the logs.
          5. Make a crossplot of Log(J) vs. Log(S wr ).

            You will find a cloud of points. Note that shoulder-bed effects and inva-
          sion of water-based mud will always pull points to higher S wr values com-
          pared with points originating from thick beds and for which less invasion
          is occurring. Therefore, by fitting the constants a and b so that the model
          follows the leading edge of the cloud of points, you will effectively be
          correcting for thin bed and invasion effects.
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