Migration of carbon dioxide in sandstone under various pressure/temperature conditions: From experiment to simulation
文献类型:期刊论文
作者 | Xu, Liang2,3; Li, Qi2,3![]() |
刊名 | GREENHOUSE GASES-SCIENCE AND TECHNOLOGY
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出版日期 | 2022-02-09 |
页码 | 16 |
关键词 | carbon capture and storage (CCS) core flooding experiment formation condition numerical simulation storage efficiency |
ISSN号 | 2152-3878 |
DOI | 10.1002/ghg.2140 |
英文摘要 | The pressure and temperature of a target CO2 storage reservoir can significantly affect the migration and relative permeability characteristics which can ultimately determine the carbon storage capacity and storage integrity of target formations. To understand these impacts, a CO2 core-flooding experiment was conducted on a brine-saturated sandstone containing a single clay interlayer perpendicular to the flow direction at a temperature of 313 K and a pressure of 8 MPa and the fluid distribution was monitored by a high-resolution X-ray computed tomography (X-CT) scanner. Further, a one-dimensional model was established to reproduce the CO2 flow behavior inside the sample under the same experimental condition and then the model was extended to different temperatures (313 and 350 K) and pressures (6, 8, 12, and 17.4 MPa). The experimental results show that the CO2 preferentially created high-CO2-saturation flow pathways which then expanded until they were large enough to transport the CO2 at the prescribed flow rate. The sub-core scale heterogeneity also had significant effects on the CO2 migration, forming a barrier to downstream flow. The simulation results show that at a given temperature, the CO2 front migration velocity decreased with increasing reservoir pressure while the CO2 saturation along the pathways increased. Comparing simulations when the reservoir pressure was the same, the front-migration velocity increased with increasing temperature, and the CO2 saturation along the pathways decreased. Meanwhile, the influence of temperature and pressure on CO2 saturation distribution was more evident in the parts of the core with high residual brine saturation. (c) 2022 Society of Chemical Industry and John Wiley & Sons, Ltd. |
资助项目 | National Natural Science Foundation of China[41872210] ; National Natural Science Foundation of China[41274111] ; Open Research Fund of State Key Laboratory of Geomechanics and Geotechnical Engineering, IRSM, CAS[Z020001] |
WOS研究方向 | Energy & Fuels ; Engineering ; Environmental Sciences & Ecology |
语种 | 英语 |
WOS记录号 | WOS:000753285900001 |
出版者 | WILEY PERIODICALS, INC |
源URL | [http://119.78.100.198/handle/2S6PX9GI/34453] ![]() |
专题 | 中科院武汉岩土力学所 |
通讯作者 | Li, Qi |
作者单位 | 1.CSIRO Energy, Australian Resources Res Ctr, Kensington, WA, Australia 2.Univ Chinese Acad Sci, Beijing, Peoples R China 3.Chinese Acad Sci, Inst Rock & Soil Mech, State Key Lab Geomech & Geotech Engn, Wuhan, Peoples R China |
推荐引用方式 GB/T 7714 | Xu, Liang,Li, Qi,Myers, Matthew,et al. Migration of carbon dioxide in sandstone under various pressure/temperature conditions: From experiment to simulation[J]. GREENHOUSE GASES-SCIENCE AND TECHNOLOGY,2022:16. |
APA | Xu, Liang,Li, Qi,Myers, Matthew,White, Cameron,&Cao, Xiaomin.(2022).Migration of carbon dioxide in sandstone under various pressure/temperature conditions: From experiment to simulation.GREENHOUSE GASES-SCIENCE AND TECHNOLOGY,16. |
MLA | Xu, Liang,et al."Migration of carbon dioxide in sandstone under various pressure/temperature conditions: From experiment to simulation".GREENHOUSE GASES-SCIENCE AND TECHNOLOGY (2022):16. |
入库方式: OAI收割
来源:武汉岩土力学研究所
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