Page 133 - Gas Wettability of Reservoir Rock Surfaces with Porous Media
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Gas-wetting Alteration Agent and Gas-wetting               CHAPTER 3          117




              Table 3.18  Difference in Orbital Energy of Adsorption Models
              Adsorption Model          Absolute Value of   Absolute Value of
                                        Energy Difference   Energy Difference
                                        1,a.u. (Sandstone   2,a.u. (Sandstone
                                        HOMO - gas-wetting  LUMO - gas-wetting
                                        alteration agent UMO ) alteration agent OMO )
               Sandstone 1#—gas-wetting 0.59746             0.58323
                   alteration agent 1#
               Sandstone 1#—gas-wetting 0.59181             0.56159
                   alteration agent 2#
               Sandstone 2#—gas-wetting 0.61722             0.60500
                   alteration agent 1#
               Sandstone 2#—gas-wetting 0.61157             0.58336
                   alteration agent 2#




              and the LUMO orbit of molecule A acts on the HOMO orbit of molecule B. In
              the interaction between these two orbits, the smaller absolute value of energy
              difference is easier to combine. The absolute value of acting energy difference
              of every orbit is calculated when the four models are mutually combined. The
              results are shown in Table 3.18.
              It can be seen from Table 3.18 that in the four adsorption models, the “energy
              difference absolute value 2” are all less than “energy difference absolute value
              1.” That is, the two kinds of gas-wetting alteration agents tend to combine
              with HOMO orbit and sandstone LUMO orbit. From Figs. 3.28 and 3.29,it
              can be seen that HOMO orbits of two kinds of gas-wetting alteration agents
              are all located in the groups without fluorine atoms. Therefore, it is concluded
              that gas-wetting alteration agent is adsorbed on the sandstone with groups
              without fluorine atoms, and fluorine-containing groups extend outward. Due
              to the extremely low surface energy and excellent heat stability, it shields and
              protects the interior groups and sandstones. This accounts for the phenome-
              non of fluorine-containing groups with low surface energy moving toward the
              surface, as shown in Fig. 3.30. In addition, the surface energy of sandstone is
              dramatically decreased and gas wettability increased for external fluorine-
              containing groups to form a solid shielding film.


              3.3.2.3.2   Effect of water molecules on model surface
              Based on the above research result, when the gas-wetting alteration agent is
              adsorbed on the rock surface, the fluoride groups extend outward, which
              shield and protect the interior parts, reduce surface energy, and realize gas wet-
              tability alteration. In order to further prove the effect of gas-wetting alteration
              agent of fluorocarbon copolymer, the combination capability of the water
              molecule model on sandstone surface and the surface of gas-wetting alteration
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