Page 84 - Standard Handbook Petroleum Natural Gas Engineering VOLUME2
P. 84

79:   Reservoir Engineering
                                          ,
                                   830
                                       -
                                   840
                                       -         MINIMUM  OF 22%
                                   850           CONNATE  WATER
                                   860 -
                                   870 -
                                       -
                                   880
                               =  890 -
                                           8
                               J
                               >  910 -
                               w
                               w           6
                               A   920 -               QDATA  FROM
                               4   930 -                   ELECTRIC LOGS
                               W            ~
                               v)
                               3:   940 -
                               3  950 -
                               w
                               m   960 -
                                I
                                   970 -
                               w


                                   990
                                   IO00
                                   I010
                                   1020
                                      0   10  20  30 40 50  60 70 80  90  100
                                        WATER  SATURATION  (calculated 1,  96
                    Figure 5-49.  Comparison of  water  saturations from capillary pressure and
                    electric logs [48].

                    thickness where saturation changes from 100% water to irreducible water for a
                    water-oil contact, or from  100% liquid to an irreducible water saturation for a
                    gas-oil contact.
                    Effective Penneabllitles

                      In the previous section, "Absolute Permeability," it was stated that permeability
                    at 100% saturation of a fluid (other than gases at low pressure) is a characteristic
                    of the rock and not a function of the flawing fluid. Of course, this implies that
                    there  is no  interaction  between  the  fluid and  the  rock  (such as interaction
                    between water and mobile or swelling clays). When permeabilities to gases are
                    measured, corrections must be made for gas slippage which occurs when the
                    capillary openings approach the mean free path of  the gas. Rlinkenberg [128]
                    observed  that  gas  permeability  depends  on  the  gas  composition  and  is
                    approximately a linear function of  the reciprocal mean  pressure. Figure 5-50
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