Page 399 - Petrophysics 2E
P. 399

WETTABILITY          367


                            as the advancing and receding contact angles [23]. As the plate is moved
                            into and out of  a liquid, the change of force, F,  due to the adhesion
                            tension is:




                            and the contact angle is:
                            0 = arc cos (E)                                               (6.9)





                            where:  F = force, mN.
                                     1 = 2 x (width + thickness), m.
                                     O = interfacial tension, mN/m.

                              The plate is attached to a microbalance and its rate of movement is
                            controlled by a computer that calculates the instantaneous value of the
                            contact angle. The advancing contact angle is obtained as the plate is
                            moved into the liquid and the receding angle when the plate is pulled
                            from the liquid [23-251.
                              The principal constituents of  sandstones and limestones are quartz
                            and  calcite,  respectively.  Consequently,  polished  plates  of  quartz
                            and  calcite  are  used  as  representative  surfaces for  sessile  drop  and
                            advancing contact angle measurements.  These are not  representative
                            of  reservoir rocks,  however,  because  the  plates  do not  account for
                            surface  roughness,  the  large  variety  of  minerals,  or  thin  layers  of
                            organic materials. The wettability of these heterogeneous surfaces can
                            be  measured  only  by  using  one  of  the  methods  that  measure  the
                            average core wettability, such as the Amott and USBM  methods.  The
                            sessile drop and advancing contact angle measurements are therefore
                            qualitative,  rendering  information  on  the  behavior  of  the  reservoir
                            fluids and the gradual deposition of interfacially active compounds onto
                            the  solid surface.  The  methods are most  useful for measurement  of
                            wettability effects of  solutes in  pure fluids. One can  quickly observe
                            wettability changes of the smooth plate toward different oils and aqueous
                            solutions.

                     SURFACE CHEMICAL PROPERTIES

                              The  chemical  compositions  of  the  fluids  and  the  rock  surfaces
                            determine the values of  the solid-fluid  and fluid-fluid specific surface
                            energies. Thus, the mineralogy of the rock surface has an influence on
                            the relative adhesive tensions and contributes to the overall wettability
                            of the fluid-rock system. Polar organic compounds in crude oil can react
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