Page 366 - Petrophysics 2E
P. 366

334    PETROPHYSICS: RESERVOIR ROCK PROPERTIES

                                   (3
                   P,  = phgc = ph  - = 1.1179 x 10-5ApN2hr                     (5.28)


                   where  P,  is  expressed  in  gf/cm2. Equation  5.28 yields  the  capillary
                   pressure in gf/cm2 at any height, h, in the core rotating at N revolutions
                   per minute with a radius of rotation, r. Integrating across the total height
                   of the core (from the inner radius, r1, of the core to the outer radius, re)
                   in order to take into account the variation of  the centrifugal field within
                   the core with respect to distance:

                    (Pc)i = (P&  + 1.1179 x  10-5ApN2[(r," - rf)/2]              (5.29)

                      As  expressed in  Equation 5.29,  a capillary pressure gradient exists
                    within the core; a saturation gradient also exists within the core, and
                    the only measured quantities are the revolutions per minute,  N,  and
                    the average saturation of  the core, 3,.  Most  centrifuge data reported
                    in the literature adopt the boundary condition, assumed by Hassler and
                    Brunner, i.e., that the end face of the core remains 100% saturated with
                    the wetting phase at all centrifugal speeds of the test [ 171. Therefore, the
                    capillary pressure at the end face,  (P,)D, is equal to zero during the entire
                    range of centrifuge speeds used. As long as there exists a continuous film
                    on the surface of the rubber pad holding the core at the bottom, which is
                    the most prevalent assumption, the condition of zero capillary pressure
                    at the end face is correct.
                      Equation  5.29 is modified  in practice to introduce the core length,
                    L,  because the lengths of  cores used in the centrifuge vary slightly. In
                    addition, the pressure is expressed in kPa rather than grams-force/cm2.
                    These changes yield  the final equation,  which is used  to obtain the
                    capillary pressure (in kPa) at the inlet end, ri, of the core:


                    (Pc)i = (1.096 x 10-')ApN2(r,  - L/2)L                       (5.30)

             LIMITING CENTRIFUGE SPEED


                      Melrose examined the Hassler-Brunner end-face boundary condition
                    and concluded that the zero capillary pressure assumption is valid for the
                    maximum centrifuge speeds used in practice [17-191.  This conclusion
                    is reached by considering the mechanism of  the wetting phase (water)
                    displacement by the non-wetting phase (air or oil), commonly referred
                    to as the drainage capillary pressure.
                      If  the centrifuge speed reaches a sufficiently high  value,  the non-
                    wetting phase will finger (or cavitate) through the largest pores to break
                    through at the end face of the core. The capillary pressure at the end-face
   361   362   363   364   365   366   367   368   369   370   371