Jiang Hao, Guo Bo, Brusseau Mark L
Department of Chemical and Environmental Engineering, University of Arizona, 1133 E James E Rogers Way, Tucson, Arizona 85721, USA.
Department of Hydrology and Atmospheric Sciences, University of Arizona, 1133 E James E Rogers Way, Tucson, Arizona 85721, USA.
Water Resour Res. 2020 Jan;56(1). doi: 10.1029/2019wr025876. Epub 2019 Dec 26.
A pore-scale model is developed to simulate fluid-fluid interfacial area in variably saturated porous media, with a specific focus on incorporating the effects of solid-surface roughness. The model is designed to quantify total (film and meniscus) fluid-fluid interfacial area ( ) over the full range of wetting-phase fluid saturation ( ) based on the inherent properties of the porous medium. The model employs a triangular pore space bundle of cylindrical capillaries (BCC) framework, modified with three surface roughness-related parameters. The first parameter (surface roughness factor) represents the overall magnitude of surface roughness, whereas the other two parameters (interface growth factor and critical adsorptive film thickness) reflect the micro-scale structure of surface roughness. A series of sensitivity analyses was conducted for the controlling variables, and the efficacy of the model was tested using air-water interfacial area data measured for three natural porous media. The model produced good simulations of the measured data over the full range of saturation. The results demonstrate that total interfacial areas for natural media are typically much larger than those for ideal media comprising smooth surfaces due to the substantial contribution of surface roughness to wetting-film interfacial area. The degree to which fluid-fluid interfacial area is influenced by roughness is a function of fluid-retention characteristics and the nature of the rough surfaces. The full impact of roughness may be masked to some degree due to the formation of thick wetting films, which is explicitly quantified by the model. Application of the model provides insight into the importance of the interplay between pore-scale distribution and configuration of wetting fluid and the surface properties of solids.
开发了一种孔隙尺度模型,用于模拟可变饱和多孔介质中的流体-流体界面面积,特别关注纳入固体表面粗糙度的影响。该模型旨在根据多孔介质的固有特性,量化在整个湿润相流体饱和度范围内的总(薄膜和弯月面)流体-流体界面面积( )。该模型采用了由圆柱形毛细管组成的三角形孔隙空间束(BCC)框架,并通过三个与表面粗糙度相关的参数进行了修正。第一个参数(表面粗糙度因子)表示表面粗糙度的总体大小,而另外两个参数(界面生长因子和临界吸附膜厚度)反映了表面粗糙度的微观结构。对控制变量进行了一系列敏感性分析,并使用为三种天然多孔介质测量的气-水界面面积数据测试了该模型的有效性。该模型在整个饱和度范围内对测量数据进行了良好的模拟。结果表明,由于表面粗糙度对湿润膜界面面积的显著贡献,天然介质的总界面面积通常比由光滑表面组成的理想介质大得多。流体-流体界面面积受粗糙度影响的程度是流体保持特性和粗糙表面性质的函数。由于厚湿润膜的形成,粗糙度的全部影响可能在一定程度上被掩盖,该模型对此进行了明确量化。该模型的应用有助于深入了解孔隙尺度分布与湿润流体配置以及固体表面性质之间相互作用的重要性。