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Oil and gas saturation ratio (K og) affects on the indications
                            of  many  geophysical  methods.  Most  close  relationship  K og  have
                            with  electrical resistance of rocks.  Increased  values  K og  leads to
                            increased electrical resistance (Fig. 3.7, a), with all other constant
                            factors.

                                               а)                           б)
                                   
                                     п                            P  н
                             10000                          10000
                              1000                           1000

                               100                            100
                                10                             10
                                                                1
                                  0   20 40 60   80 100 K   ,%   0   20 40 60   80 100 K   ,%
                                                                                         нг
                                                          нг
                                     Figure 3.7 - Dependence ρ r(a) and P p(b) from K og

                                   In  order  to  avoid  exposure  on  layer  electrical  resistance
                            other factors, except K og use relative value of the layer resistance
                            with any K og the resistance of the layer when K o = 0% and K w =
                            100%,  ie  the  resistance  of  the  aquifer.  This  ratio  is  called  the
                            relative saturation parameter:
                                                            
                                                       P     l    1,                                  (3.6)
                                                        p
                                                            
                                                             wl

                            where:  ρ l  –  layer  resistance  with  an  unknown  K og,  with  defined
                            according LL, L, IL; ρ wl - resistance of the layer when K w = 100%.
                                   Resistance aquifer ρ wl in expression P p can be determined
                            through the porosity parameter:

                                                                 pz
                                                   P     wl          ,                           (3.7)
                                                    p
                                                                  q   Q
                                                          w     f
















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