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196                                    Part III Underbalanced Drilling Systems


        •  The pressure differential should be low enough to ensure that
           separators and storage facilities can handle the formation fluid influx
           rate and the total fluid volume.
           For a water-wet reservoir, the capillary pressure at the sand face
        always causes the water in the drilling fluid to imbibe into the reservoir.
        This water imbibition increases water saturation in the reservoir and
        reduces the effective permeability to the hydrocarbon phase, which is
        referred to as filtration-induced formation damage. Figure 9.14 shows an
        imbibition capillary pressure curve for a typical sandstone. Initial water
        saturation exists in the sandstone at the moment when the rock is being
        drilled (point A). The capillary pressure at the initial condition is the
        highest, which is the potential to cause fast water imbibition into the
        rock. However, as the water saturation increases in the rock, the capillary
        pressure drops rapidly (point B). The water invasion at point B may not
        cause significant damage to the effective permeability to oil because the
        water has only occupied the narrow pore space (“corners”) in the rock.
           As imbibition continues, water will take over all the small pore space
        and begin to occupy the larger pore space (point C). Point C is a critical
        point because significant formation damage due to water invasion should
        occur beyond this point. The capillary pressure at point C is referred to
        the critical capillary pressure. It is this critical capillary pressure that should


              300
                                        Oil
                   A
              250                       Water
                                        Grain
              200
             P c  (psia)  150  B



              100

                         C
               50
                                                 D                E
                0
                  0        0.2       0.4       0.6       0.8        1
                                          S w
        Figure 9.14 Capillary pressure curve for a sandstone sample in an air-brine system.
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