Thermodynamically constrained averaging theory approach for modeling flow and transport phenomena in porous medium systems: 8. Interface and common curve dynamics

被引:26
作者
Gray, William G. [1 ]
Miller, Cass T. [1 ]
机构
[1] Univ N Carolina, Dept Environm Sci & Engn, Chapel Hill, NC 27599 USA
基金
美国国家科学基金会;
关键词
TCAT; Evolution equations; Interfacial area; Interfacial dynamics; Dynamic capillary pressure; LATTICE-BOLTZMANN MODELS; X-RAY MICROTOMOGRAPHY; MULTIPHASE FLOW; CAPILLARY-PRESSURE; NETWORK MODEL; PHASE; SATURATION; CONTINUUM; IMBIBITION; EQUATIONS;
D O I
10.1016/j.advwatres.2010.07.002
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
This work is the eighth in a series that develops the fundamental aspects of the thermodynamically constrained averaging theory (TCAT) that allows for a systematic increase in the scale at which multiphase transport phenomena are modeled in porous medium systems. In these systems, the explicit locations of interfaces between phases and common curves, where three or more interfaces meet, are not considered at scales above the microscale. Rather, the densities of these quantities arise as areas per volume or length per volume. Modeling of the dynamics of these measures is an important challenge for robust models of flow and transport phenomena in porous medium systems, as the extent of these regions can have important implications for mass, momentum, and energy transport between and among phases, and formulation of a capillary pressure relation with minimal hysteresis. These densities do not exist at the microscale, where the interfaces and common curves correspond to particular locations. Therefore, it is necessary for a well-developed macroscale theory to provide evolution equations that describe the dynamics of interface and common curve densities. Here we point out the challenges and pitfalls in producing such evolution equations, develop a set of such equations based on averaging theorems, and identify the terms that require particular attention in experimental and computational efforts to parameterize the equations. We use the evolution equations developed to specify a closed two-fluid-phase flow model. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1427 / 1443
页数:17
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