A phase-field lattice Boltzmann model for simulating multiphase flows in porous media: Application and comparison to experiments of CO2 sequestration at pore scale

被引:100
作者
Fakhari, Abbas [1 ]
Li, Yaofa [2 ,3 ]
Bolster, Diogo [1 ,3 ]
Christensen, Kenneth T. [1 ,2 ,3 ]
机构
[1] Univ Notre Dame, Dept Civil & Environm Engn & Earth Sci, Notre Dame, IN 46556 USA
[2] Univ Notre Dame, Dept Mech & Aerosp Engn, Notre Dame, IN 46556 USA
[3] Kyushu Univ, Int Inst Carbon Neutral Energy Res I2CNER, Fukuoka, Japan
关键词
CO2; Sequestration; Lattice Boltzmann method; Porous micromodel; Capillary fingering; Viscous fingering; Pore-scale modeling; CONTACT-LINE DYNAMICS; IMMISCIBLE DISPLACEMENTS; CARBON-DIOXIDE; 2-PHASE FLOW; FLUID; WATER; MICROMODEL; NETWORK; PRESSURE; MECHANISMS;
D O I
10.1016/j.advwatres.2018.02.005
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
We implement a phase-field based lattice-Boltzmann (LB) method for numerical simulation of multi-phase flows in heterogeneous porous media at pore scales with wettability effects. The present method can handle large density and viscosity ratios, pertinent to many practical problems. As a practical application, we study multiphase flow in a micromodel representative of CO2 invading a water-saturated porous medium at reservoir conditions, both numerically and experimentally. We focus on two flow cases with (i) a crossover from capillary fingering to viscous fingering at a relatively small capillary number, and (ii) viscous fingering at a relatively moderate capillary number. Qualitative and quantitative comparisons are made between numerical results and experimental data for temporal and spatial CO2 saturation profiles, and good agreement is found. In particular, a correlation analysis shows that any differences between simulations and results are comparable to intra-experimental differences from replicate experiments. A key conclusion of this work is that system behavior is highly sensitive to boundary conditions, particularly inlet and outlet ones. We finish with a discussion on small-scale flow features, such as the emergence of strong recirculation zones as well as flow in which the residual phase is trapped, including a close look at the detailed formation of a water cone. Overall, the proposed model yields useful information, such as the spatiotemporal evolution of the CO2 front and instantaneous velocity fields, which are valuable for understanding the mechanisms of CO2 infiltration at the pore scale. (C) 2018 Elsevier Ltd. All rights reserved.
引用
收藏
页码:119 / 134
页数:16
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