Bridging the gap: Connecting pore-scale and continuum-scale simulations for immiscible multiphase flow in porous media

被引:3
作者
Ebadi, Mohammad [1 ]
Mcclure, James [2 ]
Mostaghimi, Peyman [3 ]
Armstrong, Ryan T. [3 ]
机构
[1] Univ New South Wales, Sch Minerals & Energy Resources Engn, Sydney, NSW 2052, Australia
[2] Virginia Tech, Natl Secur Inst, Blacksburg, VA 24061 USA
[3] Univ New South Wales, Sch Civil & Environm Engn, Sydney, NSW 2052, Australia
基金
美国国家科学基金会; 澳大利亚研究理事会;
关键词
CAPILLARY-PRESSURE; TOPOLOGICAL PERSISTENCE; INTERFACIAL AREA; 2-PHASE FLOW; THERMODYNAMICS; HYSTERESIS; SATURATION; PHYSICS;
D O I
10.1063/5.0186990
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
This study aims to bridge length scales in immiscible multiphase flow simulation by connecting two published governing equations at the pore-scale and continuum-scale through a novel validation framework. We employ Niessner and Hassnaizadeh's ["A model for two-phase flow in porous media including fluid-fluid interfacial area," Water Resour. Res. 44(8), W08439 (2008)] continuum-scale model for multiphase flow in porous media, combined with the geometric equation of state of McClure et al. ["Modeling geometric state for fluids in porous media: Evolution of the Euler characteristic," Transp. Porous Med. 133(2), 229-250 (2020)]. Pore-scale fluid configurations simulated with the lattice-Boltzmann method are used to validate the continuum-scale results. We propose a mapping from the continuum-scale to pore-scale utilizing a generalized additive model to predict non-wetting phase Euler characteristics during imbibition, effectively bridging the continuum-to-pore length scale gap. Continuum-scale simulated measures of specific interfacial area, saturation, and capillary pressure are directly compared to up-scaled pore-scale simulation results. This research develops a numerical framework capable of capturing multiscale flow equations establishing a connection between pore-scale and continuum-scale simulations.
引用
收藏
页数:9
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