Page 376 - Petrophysics
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344    PETROPHYSICS: RESERVOIR ROCK PROPERTIES


                                                TABLE 5.1C
                    CALCULATION OF THE  INLET SATURATION,  Si,  USING THE HASSER-BRUNNER METHOD.
                                 {Si  = S(AVE)  + Pc(HY)  x  (DsAvEIDP~)) and
                              {DSAVEIDP,  = - (1 + c  X  SAVE)~~/(B - A  X  c)}

                                                dS/dP          P x dS/dP           Si
                    1 .om          2.258        -0.036           -0.081           0.964
                    0.950          2.682        -0.034           -0.090           0.916
                    0.900          3.167        -0.031           -0.099           0.869
                    0.850          3.731        -0.029           -0.108           0.821
                    0.800          4.391        -0.027           -0.1  17         0.773
                    0.750          5.177        -0.024           -0.126           0.726
                    0.700          6.127        -0.022           -0.135           0.678
                    0.650          7.300        -0.020           -0.145           0.630
                    0.600          8.782        -0.017           -0.154           0.583
                    0.550         10.716        -0.01  5         -0.163           0.535
                    0.500         13.345        -0.013           -0.172           0.487
                    0.450         17.127        -0.01  1         -0.181           0.439
                    0.400         23.033        -0.008           -0.190           0.392
                    0.350         33.549        -0.006           -0.199           0.344
                    0.300         57.532        -0.004           -0.208           0.296
                    0.278         82.400        -0.003           -0.212           0.275



                    Substituting Equation 5.55 into Equation 5.54 yields:


                                                                                 (5.56)

                    for one pore volume, i.e. Vp = 1,



                                                                                 (5.57)



                      Assuming that cos 6 in Equation 5.1 1 is equal to 1.0, and substituting
                    Pc x  r for 20 into Equation 5.56, the equation used for interpretation of
                    the pore throat size distribution from the capillary pressure is obtained:


                                                                                 (5.58)


                      The maximum pore throat size for the sample occurs at S, = 1.0
                    where rmax = 20/Pc-, and the minimum pore size that will conduct fluid
                    occurs at an irreducible water saturation (Si,)  where rmi, = 20/Pcmm.
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