Page 345 - Petrophysics 2E
P. 345

CHAPTER  5





                         APILLARY



                          RESSURE












                   CAPILLARY PRESSURE


                             Capillary  pressure  is  the  difference  in  pressure  between  two
                           immiscible fluids across a curved interface at equilibrium. Curvature
                           of  the  interface  is  the  consequence of  preferential wetting  of  the
                           capillary walls by one of the phases. Figure 5.1 illustrates various wetting
                           conditions. In Figure 5.la, two immiscible fluids are shown in contact
                          with a capillary. The water wets the walls of  the capillary, but the oil
                           is non-wetting and is resting on a thin film of  the wetting fluid.  The
                           pressure within the non-wetting fluid  is greater than the pressure in
                           the wetting fluid and, consequently, the interface between the fluids
                           is curved convex with respect to the non-wetting fluid. The capillary
                           pressure is defined as the pressure difference between the non-wetting
                           and wetting phases:




                             In Figure 5.lb, the two fluids wet the walls of the capillary to the same
                           extent, and the pressure of each fluid is the same. Therefore, the interface
                           between the immiscible fluids is straight across (-90") and the capillary
                           pressure is equal to zero. If the pressure  in the water is greater than in the
                           oil, the curvature of the interface is directed into the oil and the capillary
                           pressure is positive (Figure 5.1~).
                             The radii of curvature between water and oil in the pores of the rock
                           are functions  of wettability, saturations of water and oil, pore geometry,
                           mineralogy of the pore walls, and the saturation history of the system.
                           Therefore, the radii of curvature and contact angle vary from one pore
                           to another, and the average macroscopic properties of the rock sample
                           apply  *
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