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MODELS OF DYNAMIC GEOLOGIC SYSTEMS                                   263
             rock properties using the following equations:

                  Porosity  f ¼ f Z 1                                          (11.97)
                                 o
                                        4
                  Permeability  k ¼ k o ðZ 1 Þ                                 (11.98)
                  Density g ¼ g ð1   f Z 1 Þ                                   (11.99)
                               ma      o
             where f and k o are, respectively, the initial values of porosity and permeability
                     o
             before compaction of sediments, g ma  is the density of matrix of consolidated rocks,
             and Z 1 is equal to:

                        n   ,"             n  !#
                       Y                  Y
                  Z 1 ¼   x i  1   f o  1    x i  ¼ Z=½1   f ð1   Zފ         (11.100)
                                                            o
                       i¼1                i¼1
             is the relative change in porosity: f=f .
                                              o
                The results of the numerical simulation show that the modeling coefficients x i
             represent adequately the influence of many geological factors on the petrophysical
             properties of rocks (Fig. 11.30).





































             Fig. 11.30. Results of numerical simulation of Mesozoic reservoir-rock properties. (a) Porosity, (b) per-
             meability, (c) density. 1 – Average curve, 2 – confidence limits. (After Buryakovsky, 1993.)
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