Page 176 - Petrophysics 2E
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PERMEABILITY-POROSITY  RELATIONSHIPS             149



                            -
                              1000
                            (I)
                            a
                            >  -
                            ai
                            *
                            m
                            >
                            g 100
                            er
                            a
                            M
                            M
                            2
                            n
                            '0
                            C
                            48   10
                            e!
                            a
                            M
                            t
                            L
                                1
                                0 001    0 01     01       1       10       100     1 ow
                                                         Time, hrs
                        Figure 3.33a. Pressure and pressure derivative curve indicating spherical pow from
                        which vertical permeability is determined [56].


















                                      (a) Representative and non-
                                     representative selected horizontal
                                    and vertical plugs for conventional   @)Plugs from naturally fractured cores.
                                          core analysis.
                        Figure 3.34. Orientation or core plugs used for measuring horizontal and vertical
                       permeability.





                        Vertical  permeability  in  the  formation  is  normally  different  from
                        horizontal permeability, even when the system is homogenous. Such
                        vertical  anisotropy  effects  are  generally  the  result  of  depositional
                        environment and postdepositional compaction history of the formation.
                        As discussed earlier, in shale-free sandstone formations grain size, shape
                        factor, and particle orientation are the most important factors in the
                        k,-kH  relationship (see Figure 3.34).
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