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Chemical Force Microscopy Study on the Interactions of COOH Functional Groups with Kaolinite Surfaces: Implications for Enhanced Oil Recovery

机译:化学力显微镜研究COOH官能团与高岭石表面的相互作用:对提高采油率的意义

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Clay?¢????oil interactions play a critical role in determining the wettability of sandstone oil reservoirs, which, in turn, governs the effectiveness of enhanced oil recovery methods. In this study, we have measured the adhesion between ?¢????COOH functional groups and the siloxane and aluminol faces of kaolinite clay minerals by means of chemical force microscopy as a function of pH, salinity (from 0.001 M to 1 M) and cation identity (Na + vs. Ca 2+ ). Results from measurements on the siloxane face show that Ca 2+ displays a reverse low-salinity effect (adhesion decreasing at higher concentrations) at pH 5.5, and a low salinity effect at pH 8. At a constant Ca 2+ concentration of 0.001 M, however, an increase in pH leads to larger adhesion. In contrast, a variation in the Na + concentration showed less effect in varying the adhesion of ?¢????COOH groups to the siloxane face. Measurements on the aluminol face showed a reverse low-salinity effect at pH 5.5 in the presence of Ca 2+ , whereas an increase in pH with constant ion concentration resulted in a decrease in adhesion for both Ca 2+ and Na + . Results are explained by looking at the kaolinite?¢????s surface complexation and the protonation state of the functional group, and highlight a more important role of the multicomponent ion exchange mechanism in controlling adhesion than the double layer expansion mechanism.
机译:粘土的油相互作用在确定砂岩油藏的润湿性中起着至关重要的作用,而这反过来又决定了强化采油方法的有效性。在这项研究中,我们通过化学力显微镜测量了pH值,盐度(从0.001 M到1 M)的函数,测定了COOH官能团与高岭土粘土矿物的硅氧烷和铝矾土表面之间的粘附力。和阳离子身份(Na +与Ca 2+)。硅氧烷表面的测量结果表明,Ca 2+在pH 5.5时显示出相反的低盐度效应(在较高浓度下附着力降低),在pH 8时显示出低盐度效应。在恒定的Ca 2+浓度为0.001 M时,但是,pH值的增加会导致更大的附着力。相反,Na +浓度的变化显示出在改变α1-β-COOH基团对硅氧烷表面的粘附力方面的作用较小。在存在Ca 2+的情况下,对铝矾土表面的测量表明在pH 5.5时具有相反的低盐度作用,而在恒定离子浓度下pH升高会导致Ca 2+和Na +的粘附力降低。通过观察高岭石的表面络合和官能团的质子化状态来解释结果,并且突出了多组分离子交换机理在控制粘附方面比双层膨胀机理更重要的作用。

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