Page 213 - Petrophysics
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186    PETROPHYSICS: RESERVOIR ROCK PROPERTIES


                          1000





                        - 100
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                        U
                        5
                        2
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                        4   10                                                    ...





                             1
                              0.1              I                10              I00
                                                    Time, hrs

                              Figure 3.58. Longlogplot of AP and t*AP'  versus test time,



                    probability of the presence of reservoir nog-uniformities of a certain type
                    in  any reservoir by  considering the cores, logs, and general geologic
                    background of the reservoir [47]. Using a statistical analysis of laboratory
                    measurements  of  air  permeability in  eight  directions spaced  at  45"
                    intervals on 142 two-inch vertical plugs from 30 cores, Greenkorn et al.
                    showed that there is significant point anisotropy in about 60% of the core
                    plugs [53]. Also, they found that the permeability of  a heterogeneous
                    anisotropic porous medium  is  a  tensor consisting of  a point-to-point
                    variation that depends on grain size and a point variation that depends on
                    bedding. Trudgen and Hoffmann proposed a procedure which employs
                    Pearson's system of  curve fitting for defining a frequency distribution
                    of reservoir rock properties obtained from core data  [ 541. Many more
                    statistical methods for describing various reservoir rock properties were
                    proposed.  However,  only  few  of  these  methods were  found  to  be
                    practical.
                       Testerman described a statistical technique for identifying and describ-
                    ing  porous  and permeable  zones in  a reservoir,  and for determining
                    which  ones  are  likely  to  be  continuous  between  adjacent  wells
                     [55]. The  technique  is  particularly useful  in  describing permeability
                    distribution in a reservoir where crossflow between adjacent communi-
                    cating reservoir  strata,  due  to  imbibition and  gravity  segregation,  is
                    important. Inasmuch as there are, however, no geological parameters
                     concerning the depositional environment in the statistical evaluation,
                    judgment  is  necessary  to  determine  whether  the  zones  so  defined
                     are,  in  fact,  continuous  and  consistent with  the  geological  model.
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