Page 417 - Petrophysics 2E
P. 417

WATER-OIL-ROCK INTERFACIAL ACTMTY               385



                                    r
                                                                             %
                               -                                       CORE  QLICONE  WETTABILITY
                                                                                     0.64s
                                                                              0
                                                                         1
                               ::  90-                                   2    0.02   0.176
                               #
                                                                         3    0.2   -0.222
                                                                         4    2.0    -1.250
                                                                                     -1.335
                                                                        Curvoo  cut  off  at  woR-ioo
                                                               _,,,._ ._ -.....-.....  -.---.--d

                                                                                 I   I






                             There are a number of other influences that disturb the normal trend
                           of  relative permeability curves, and they must  not be confused with
                           the  effects due  to  wettability alone  [72]. The  relative flow  of  fluids
                           is  a  function of  pore  size distribution;  therefore,  any  change of  this
                           distribution due to blocking will change the relative permeability curves.
                           The  overburden pressure applied to cores in the laboratory changes
                           pore-size and pore-throat size distributions, reducing the size  of the larger
                           pores, which changes the porosity as well. Furthermore, smaller pore
                           sizes may increase the irreducible water saturation in water-wet rocks and
                           the residual oil saturation; thus, the mobile oil saturation is decreased.
                           An increase of temperature causes the wettability to change to a more
                           water-wet system. Thus,  core floods for the determination of  relative
                           permeabilities should be conducted at simulated reservoir conditions of
                           overburden pressure, pore pressure, and temperature for the resulting
                           relative permeability curves to be representative  of  conditions in the
                           reservoir [69-721.
                             The  saturation history  of  the water-oil-rock system  (or  core) has  a
                           fundamental influence on the equilibrium wetting condition  of the rock.
                           Oil  reservoirs are generally assumed to  have  been  filled with  water,
                           which was displaced into a trap by migrating oil. Thus oil reservoirs
                           tend to be preferentially water-wet, although several major oilfields have
                           been found to be oil-wet and heavy oil deposits ('MI  < 20) are generally
                           oil-wet. The wettability of  the reservoirs probably changed  gradually
                           from strongly water-wet to some degree of intermediate wettability and
                           finally to oil-wet as polar compounds in the oil diffused to the interface
                           and adhered to the rock surface. Thus oilfield rocks exhibit all degrees
                           of wettability from strongly water-wet to strongly oil-wet [3, 46,  65,
                           73,  741. Low-molecular-weight compounds and  gas  in  the  crude  oil
                           may accelerate the deposition of polar compounds by the deasphalting
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