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Experimental and Theoretical Basis for a Wettability-Interfacial Area-Relative Permeability Relationship

机译:润湿性-界面面积-相对渗透率关系的实验和理论基础

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Using an interfacial tracer technique, our experiments showqualitatively different trends of total interfacial area betweenthe wetting and non-wetting phases as a function of saturation,depending on whether the system is strongly or weaklywetted. A strongly wetted system is defined as one in whichthe wetting phase can spread as a thin film on the solidsurface. We assess the relative contributions of fluid/fluid andfluid/solid interfaces to the total area using thermodynamicarguments. The fluid/solid contribution to area plays a crucialrole in explaining the measurements.The influence of interfacial area on relative permeability is notstraightforward. Simple analysis based upon pore-leveldistribution of phases in a model porous medium allowsquantifying the differences in the relative permeabilities forboth weakly and strongly wetted systems, measuredsimultaneously with the interfacial area. Relative permeabilitycorrelates with fluid/solid area but not with fluid/fluidinterfacial area.
机译:使用界面示踪技术,我们的实验表明 之间的总界面面积在质上有不同的趋势 润湿阶段和非润湿阶段是饱和度的函数, 取决于系统是强还是弱 弄湿。强湿系统定义为其中 润湿阶段可以在固体上以薄膜形式扩散 表面。我们评估流体/流体的相对贡献和 使用热力学将流体/固体界面连接到总面积 论点。流体/固体对面积的贡献至关重要 在解释测量结果中的作用。 界面面积对相对渗透率的影响不大 直截了当。基于孔隙水平的简单分析 模型多孔介质中的相分布允许 量化相对渗透率的差异 无论是弱湿系统还是强湿系统 同时与界面区域。相对磁导率 与流体/固体面积相关,但与流体/流体无关 界面区域。

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