Page 401 - Petrophysics 2E
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WETTABILITY          369


                            be  demonstrated  in  the laboratory by  treating  the shale with  strong
                            hydrochloric acid to give rise to a “hydrogen”-based clay and then with
                            a solution containing salts of the di- or trivalent cations.
                              Electrical properties develop because the associated cations are loosely
                            held and therefore are mobile and can be displaced by a direct current
                            electrical potential.  Swelling occurs when  fresh water  is  introduced
                            and the H30+  ion can enter the lattice structure of  the clay mineral.
                            The H30+ ion is large and can enter into the lattice of some smectites
                            (montmorillonite, etc.) causing them to swell into a gel-like mass which
                            may be 10 to 40 times the volume of the original clay. Dispersion of the
                            clays occurs when the H30+ ions loosen the clay particles, especially
                            those lining the pore walls of the rock.
                              The sand Si02 molecule can react with hot water and water containing
                            salts to form silanol groups which are Bronsted acids (weak acids capable
                            of freeing a proton):

                             Si02 + 2H20 + Si (0H)z + 20H-
                                                 0-  0-
                                                  I   I
                             polymeric form is: H-0-Si-0-Si-OH                           (6.10)
                                                  I   I
                                                 0-  0-
                             = SiOH + SiO- + HS

                              Because  of  their  acid  surfaces,  sandstones  react  with  and  adsorb
                            basic compounds readily, whereas acidic compounds are repelled. The
                            major polar organic constituents of  crude oils are weak acids. These
                            do not adsorb readily on the Si02 surfaces and, therefore, sandstones
                            generally exhibit neutral to water-wet characteristics, which have been
                            observed by many investigators. Block and Simms furnished some direct
                            experimental proof of this [27]: They showed that octadecyamine, an
                            organic base, is strongly adsorbed on the surface of glass, whereas stearic
                            acid is hardly adsorbed at all.
                              Silica and clay minerals mixed with the sand have negatively charged
                            surfaces and, consequently, behave like weak acids in contact with water
                            having a pH less than 7. Although these surfaces will form weak acid-base
                            chemical bonds with the basic organic compounds present in crude oils,
                            they are unaffected by the acidic compounds. The resins and asphaltene
                            fractions of  crude oils contain polar,  polynuclear organic compounds
                            that can be acidic or basic. The basic compounds can interact with the
                            acidic silica and negatively charged clay surfaces, rendering the surface
                            oil-wet to a degree depending on the amount and types of basic organic
                            compounds available [8, 28-33].
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