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Laboratory work №3

                             RELEASE THE RESERVOIR ROCKS AND DETERMING
                               K P AND K OG ACCORDING TO GEOPHYSICAL WELL
                                                       LOGGING

                                                  3.1 Purpose of work

                                   An  overview  with  the  method  selection  reservoir  rocks,
                            determination  K p  and  K og  according to geophysical well  logging
                            (GWL) and acquire practical skills in solving these problems.

                                              3.2 The theoretical material

                                   Allocated reservoir rocks according to GWL - is one of the
                            most important tasks, but at the same time and difficult, especially
                            when dealing with a complicated structure collectors. Solution of
                            this problem is based on the fact that the reservoir properties and
                            nature of the fluid that is in the pores of the reservoir, affecting on
                            screenings of geophysical parameters. Thus, we obtain geophysical
                            characteristics  for  different  types  of  collectors,  which  allow
                            solving the inverse problem. The more geophysical information is
                            about cross-section of wells, the more confident you can make a
                            selection of collectors.
                                   Below  is  limited  characteristic  of  reservoir  by  using
                            geophysical methods: IR, SPL, GL, NGL, dс:
                                1.  IR  -  the  availability  of  increase  electrical  resistance  by
                                                  ML
                            micro data logging (Δρ ≠0), three-layer curve of LL;
                                2.  SPL - the presence of anomalies (usually);
                                3.  GL  (Iγ) -  small  values of Iγ = (2~8) mR / hr. (excluding
                            cases of polymictic sandstone for which Iγ can make a big value);
                                4.  NGK (Inγ) - average, meaning Inγ = (1.2~1.4) c.un.;



















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