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EOR mechanisms of wettability alteration and its comparison with IFT  239


              positively charged surfactants, because anionic surfactants interact with the
              positively charged oil molecules, mostly carbon-based compounds adsorbed
              to the siliceous rock surface, forming ion-pairs. The layer of oil in the rock
              surface is desorbed as ion-pairs forming micelles and transported due to their
              hydrophobicity to the bulk oil phase in the pores. Liu et al. (2019) also
              observed that organic material and oil film are detached from rock surface
              in anionic surfactant solutions. That is an example of ion-pair mechanism.
              The mechanism is schematically shown in Fig. 9.16. Salehi et al. (2008)
              found that the wettability alteration by forming ion-pairs was more effective
              than by the surfactant adsorption.

              9.6.4 Surfactant adsorption mechanism
              When an anionic surfactant solution is placed in a carbonate formation, the
              charged hydrophobic heads of the surfactant are adsorbed on those surface
              places (positively charged) unoccupied by counter ions via electrostatic
              interactions. If the adsorption is sparse, the interactions between adsorbed
              surfactant molecules are negligible (Atkin et al., 2003; Paria and Khilar,
              2004). The rock surface becomes more oil-wet, as shown in Fig. 9.17.
              However, if the carbonate surface is originally intensely occupied by nega-
              tive oil components, and anionic surfactant molecules adsorb on the rock
              surface via competition adsorption, then the rock surface is less occupied
              by the oil components, leading to less oil-wet.
                 Similarly, for a cationic surfactant, the positively charged head groups
              adsorb onto the negatively charged surfaces of siliceous minerals by electro-
              static interactions. This could cause the mineral surface to become more





















              Figure 9.16 Schematic of ion-pair mechanism of an anionic surfactant in a siliceous
              rock.
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