Page 179 - Petrophysics 2E
P. 179

152    PETROPHYSICS: RESERVOIR ROCK PROPERTIES


                      irreducible water saturation is:


                                                                                   (3.99)


                      Substituting Equation 3.99 in Equation 3.97 and simplifying yields:
                      kv = 4.012 X  103@,3.728 F)                                 (3.100)
                                            (
                                              1 - swi
                                                      2.4855


                      Equation 3.100 can be used to develop a vertical permeability profile in
                      the well, using the Swi and + from logs in clean sandstone rocks.


                        Shaly Sandstone Formations
                        Permeability  in  shaly  heterogeneous  formations  is  extremely
                      influenced  by  the  nature  of  shale  distribution  in  the  rock.  Shale
                      exists in  dispersed  and  laminated form.  Overall reservoir quality  in
                      heterogeneous sandstones is  controlled by  diagenesis,  dissolution  of
                      feIdspars and  carbonate, crystal feeding,  mineralogical redistribution
                      of  clay,  and  various  cementation processes.  Tiab  and  Zahaf related
                      vertical permeability to the mean hydraulic radius  [46]. They defined
                      three  general  forms  of  correlation  between  vertical  and  horizontal
                      permeability as follows:

                      (a)  Vertical permeability as a function of hydraulic mean radius:
                          kv = Al (                                               (3.101)





                      (b)  Vertical permeability as a function of clay content:



                                                                                  (3.102)


                      (c)  Vertical permeability as a function of mean grain size:



                                                                                  (3.103)


                      where  AI,  A2,  A3,  B1,  B2,  and  B3  are  coefficients and  have  to be
                      determined for specific formation.
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