Page 237 - Fundamentals of Enhanced Oil and Gas Recovery
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Waterflooding                                                                       225


                      It has been observed from many field projects that the level of improved oil recov-
                   ery from alkaline flooding is low. Based on analysis of the data reported by Mayer
                   et al. [65], the incremental oil recovery factor over waterflooding was 1% 2% in most
                   of the projects, and 5% 6% in a few projects [45].



                   7.6.2.4 Multicomponent Ion Exchange
                   Different affinities of ions on rock surfaces results in the Multicomponent Ion
                                                                           2+       2+
                   Exchange (MIE) in which multivalent or divalent such as Ca  and Mg  strongly
                   adsorbed on rock surfaces until the saturation point of the rock. Polar compounds
                   present in the oil phase and multivalent cations at clay surfaces bonded together
                   and form organometallic complexes; this mechanism yields the rock surface
                   toward oil-wet condition. During the injection of LS brine, MIE will take place,
                   removing organic polar compounds and organometallic complexes from the
                   surface and replacing them with uncomplexed cations [45,66].The suggested
                   mechanism of MIE is supported by the pore-scale model proposed by Sorbie and
                   Collins [66].
                      Meyers and Salter [67] carried out several adsorption experiments; in their tests,
                   they observed that the steady-state effluent concentrations of calcium and magne-
                   sium were observed to be slightly greater than the injected concentrations. These
                   excess concentrations increased as the injection concentrations decreased. When
                   NaCl brine was injected into the cores, “residual” calcium and magnesium concen-
                   trations were still observed in the effluent. However, Valocchi et al. [68] injected
                                                                                            21
                   fresh water in a brackish water aquifer and noticed that the concentration of Ca
                          21
                   and Mg    in different control wells were lower than the invading water and the
                   connate brine [45].


                   7.6.2.5 Double Layer Effect
                   The double layer theory combines the effects of the electrostatic repulsion and van
                   der Waals attraction owing to the so-called double layer of counter ions. LS brine
                   using the mechanism of the expansion of the electric double layer to reduce
                   clay clay attraction. Indirect interactions between oil, brine, and rock highly
                   affect the discharge of clay particles; this mechanism normally occurs in kaolinite
                   plates and involve in their charge distribution [46]. LS water makes water film
                   more stable owing to this expanded double layer effect, resulting in more water-
                   wet on clay surfaces and more oil is detached; conversely, adsorption of divalent at
                   water/sand and water/oil interfaces changes the wettability from water-wet state
                   to oil-wet condition [45,70,71].
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