Page 414 - Petrophysics 2E
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382    PETROPHYSICS: RESERVOIR ROCK PROPERTIES


                     displacement pressure is required for both fluids (for water-displacing-oil
                    from  Si,,   or  oil-displacing-water from  S,,,),   which  is  the  basis  for
                     determination of  neutral wettability. If,  however,  a small amount of
                    water will imbibe at Si,  and an almost equal amount of oil will imbibe at
                     Sworr the system is at a condition of fractional or mixed wettability. The
                     distinction between these can be made only by microscopic observations
                     of thin sections.
                       If  the system is oil-wet, these conditions for the water-wet case are
                     reversed: A1  is small and A2 is large. Oil will spontaneously imbibe into
                     the system, displacing water. Water must be forced into the system and,
                     therefore,  A2 is a large value.
                       The work required for displacement of oil by water is the theoretical
                     work required for a waterflood and is one of  the economic factors of
                     oil production. For  example: if  the reserve estimates, from field and
                     laboratory analyses of a small field, indicate that 1.6 x 105m3 (one million
                     barrels of oil) will be recovered from a waterflood and the work required
                     for displacement of  the oil (from the current field saturation to So,)  is
                     10kJ/m3 (1.5  BTU/bbl),  then  1.6 mJ  (1.5  million BTU) of  energy,  in
                     addition to friction losses in pumps and  tubing, will  be  required for
                     completion of the waterflood.


              WATER~OIL-ROCK INTERFACIAL
                                                    ACTIVITY

                       Surfactant-type compounds in crude oils, which are partially soluble
                     in water, have been found to pass rapidly through the thin water film on
                     water-wet surfaces and adsorb strongly  on the rock [ 1 1, 351. Asphaltenes
                     (high molecular weight, polynuclear aromatic compounds containing
                     nitrogen, sulfur, and oxygen in ring structures) penetrate the aqueous
                     film to produce oil-wet surfaces in the rock.  Thus,  rocks containing
                     asphaltic oils will exhibit oil-wetting tendencies.
                       The silicate-water interface is acidic. Acidic compounds in crude oils
                     (those containing carboxylic and phenol groups) do not adsorb on silicate
                     surfaces, but basic constituents (nitrogen-containing compounds such
                     as amines and amides) adsorb readily, rendering the surface oil-wet. In
                     contrast, the carbonate-water surface is basic and the acid compounds
                     adsorb, whereas the basic compounds are repelled [28, 56-59]. Since
                     crude oils generally contain polar compounds that are acidic, the wetting
                     tendencies  of  brine-crude oil,  -rock systems is  for  silicate rocks  to
                     be  neutral to water-wet and  for carbonates to  be  neutral to  oil-wet.
                     Akhlaq treated quartz and kaolinite samples with crude oils and then
                     characterized the adsorbed compounds with infi-ared spectroscopy [GO].
                     Basic nitrogen compounds and organic esters were found adsorbed to
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