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CENTRIFUGE MEASUREMENT OF CAPILLARY PRESSURE                 34 1


                            data that have an increasing negative error as the wetting-phase saturation
                            decreases. Curve 4 shows the results of the Van Domselaar’s equation that
                            is apparently more accurate than the Hassler and Brunner approximate
                            solution at the higher wetting-phase saturations. But as the wetting-phase
                            saturation decreases,  it introduces  an increasing positive error in the
                            calculated capillary pressure. It is apparent that the accurate calculation
                            of  (Pc)i versus  Si  can  be  obtained  using  Rajan’s equation,  which  is
                            theoretically exact because it correctly models the physics of the problem
                            and does not contain simplifying assumptions.
                              The recommended procedure is to:


                            (1) fit the experimental (Pc)i versus S data to the least-squares hyperbolic
                               expression;
                            (2)  evaluate the derivatives at specific values of S and their corresponding
                               (Pc)i;
                            (3)  obtain Si  corresponding to each (PJi,  from a computer solution of
                               Equation 5.52; and
                            (4)  establish a table  of  values of  (Pc)i versus  Si  to plot  the  capillary
                               pressure curves and to evaluate wettability and the thermodynamic
                               energy required for immiscible fluid displacements.


                            EXAMPLE


                              Prepare the capillary pressure versus inlet saturation curve based on the
                            centrifuge displacement of water by air. Data: L = 2.0 cm; d = 2.53 cm;
                           Vp = 1.73cm3; k = 144mD; centrifuge  arm  - =  8.6cm;  water-air
                            density difference = 0.9988; porosity = 0.17. The experimental data for
                            an air-displacing-water capillary pressure experiment and the calculated
                            capillary pressure (in psi) obtained from Equation 5.31 are presented in
                            Table 5. la.



                            SOLUTION

                              Table  5. lb  presents  the  least-squares  regression  procedure  for
                            calculation  of  Pc  as  a  function  of  S,  whereas  Figure  5.20  shows  a
                            comparison of  the raw data versus the smoothed data obtained from
                            the hyperbolic function.

                              The hyperbolic function (A + B x S)/(l.O + C x S) was then used to
                            obtain the inlet saturation using the Hassler-Brunner method. The data
                            presented in Table 5.lc and Figure 5.20 shows a comparison between
                            the average and the inlet saturation.
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