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Characterization of multiphase electrokinetic coupling using a bundle of capillary tubes model

机译:使用一捆毛细管模型表征多相电动耦合

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A simple bundle of capillary tubes model has been used to investigate electrokinetic coupling during the flow of water and an immiscible second phase such as air or oil. It is shown that the total electrokinetic coupling is the sum of the individual phase contributions. The electrokinetic coupling depends on the capillary size distribution and wettability. When water is the wetting phase and the second phase is nonpolar and does not contain an excess of charge, the relative coupling decreases with decreasing water saturation. Similar behavior has been observed in geologic porous media. However, when water is not the wetting phase, the coupling increases with decreasing water saturation before falling sharply to zero at the irreducible water saturation. This behavior has not been predicted before. If water is the only phase that contains an excess of charge, then the electrokinetic coupling can be described in terms of the water relative permeability and relative electrical conductivity. The model predictions suggest that multiphase electrokinetic coupling in geologic porous media depends on rock type and wettability and can be described in terms of commonly measured petrophysical properties. However, the predictions should be applied with caution because the pore space topology and pore occupancy of the model is very simple. Moreover, if the second phase is polar and contains an excess of charge, preliminary work suggests that the multiphase coupling can be significantly enhanced.
机译:一个简单的毛细管束模型已用于研究水和不可混溶的第二相(例如空气或油)流动期间的电动耦合。结果表明,总的电动耦合是各个相贡献的总和。电动耦合取决于毛细管尺寸分布和润湿性。当水为润湿相且第二相为非极性且不包含过量电荷时,相对耦合会随着水饱和度的降低而降低。在地质多孔介质中也观察到了类似的行为。但是,当水不是润湿阶段时,耦合随着水饱和度的降低而增加,然后在不可降低的水饱和度急剧下降到零之前。此行为以前未曾预测过。如果水是唯一包含过量电荷的相,则可以用水的相对磁导率和相对电导率来描述电动耦合。模型预测表明,地质多孔介质中的多相电动耦合取决于岩石类型和润湿性,并且可以用通常测量的岩石物理特性来描述。但是,由于模型的孔隙空间拓扑和孔隙占有率非常简单,因此应谨慎应用预测。此外,如果第二相是极性的并且包含过量的电荷,则初步工作表明可以显着增强多相耦合。

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