Discrete Bubble Flow in Granular Porous Media via Multiphase Computational Fluid Dynamic Simulation

被引:8
作者
Ma, Ye [1 ]
Yan, Guanxi [2 ]
Scheuermann, Alexander [2 ]
机构
[1] Dalian Maritime Univ, Coll Environm Sci & Engn, Dalian, Peoples R China
[2] Univ Queensland, Sch Civil Engn, Brisbane, Qld, Australia
基金
澳大利亚研究理事会;
关键词
multiphase computational fluid dynamic; bubble plumes migration; pore water flow; subsurface gas distribution; porous media; HYDRAULIC CONDUCTIVITY; SOIL GAS; MIGRATION; MICROBUBBLES; MICROSEEPAGE; TRANSPORT; SURFACE; EARTH; MODEL;
D O I
10.3389/feart.2022.947625
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The coal seam gas industry has raised public concerns about the potential risk of groundwater contamination, where gases leaked from coal seams are thought to pollute groundwater. However, the basic principles and controlling parameters for gas seepage from deep ground formations to the ground surface have not been fully understood. As a possible mechanism for gas transport in the subsurface environment, discrete bubble flow was previously investigated using laboratory experiments by Ma et al. (Water Resour. Res, 2015, 51 (6), 4359-4373). This study developed a multiphase computational fluid dynamic (CFD) model to simulate discrete bubbly flow in a two-dimensional granular porous media at the pore scale. Following the experimental setup from Ma et al. (Water Resour. Res, 2015, 51 (6), 4359-4373), a "point source" with preset bubble fluxes was specified in a simulating domain representing the flume size in the earlier experiments. There were around 7,000 granular particles within this domain to model the porous media. This numerical model was validated by conserving the gas mass in the simulating domain. The simulation results provide more physical insights into complex bubble transport behaviour in porous media through specific plume parameters. The breakthrough time of the bubble plume and the cross-sectional averaged velocity of ambient pore water flow were manifested to be proportional to the gas release rates in the logarithmic scales. Also, the bubble plume width was also observed to be proportional to the gas release rates. Moreover, the gas distribution on the top boundary could be observed. The outcomes were further tested against the scaling solutions proposed by Ma et al. (Water Resour. Res, 2015, 51 (6), 4359-4373) with disagreements. The limitations of this multiphase computational fluid dynamic model were finally discussed.
引用
收藏
页数:10
相关论文
共 39 条
[1]  
Abreu LDV, 2005, ENVIRON SCI TECHNOL, V39, P4550, DOI 10.1021/eso049781k
[2]   Gas migration along fault systems and through the vadose zone in the Latera caldera (central Italy):: Implications for CO2 geological storage [J].
Annunziatellis, A. ;
Beaubien, S. E. ;
Bigi, S. ;
Ciotoli, G. ;
Coltella, M. ;
Lombardi, S. .
INTERNATIONAL JOURNAL OF GREENHOUSE GAS CONTROL, 2008, 2 (03) :353-372
[3]  
Bear J., 1988, Dynamics of Fluids in Porous Media
[4]  
Brown A, 2000, AAPG BULL, V84, P1775
[5]   The dynamics of gas-bubble formation at saturated conditions in porous media flow [J].
Chang, K. Alex ;
Lindquist, W. Brent .
SCIENTIFIC REPORTS, 2020, 10 (01)
[6]  
Charbeneau R., 2002, APPL MECH REV, V55, pB38, DOI 10.1115/1.1451232
[7]  
Clift R, 2005, Bubbles, drops, and particles
[8]  
Crowe C., 1998, Multiphase Flows with Droplets and Particles
[9]   FAULT-DETECTION USING SOIL GAS GEOCHEMISTRY [J].
DUDDRIDGE, GA ;
GRAINGER, P ;
DURRANCE, EM .
QUARTERLY JOURNAL OF ENGINEERING GEOLOGY, 1991, 24 (04) :427-435
[10]   Migration of carrier and trace gases in the geosphere: an overview [J].
Etiope, G ;
Martinelli, G .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 2002, 129 (3-4) :185-204