中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
A Pore-Scale Phase Field Model for CO2-Fluid-Basalt Interactions

文献类型:期刊论文

作者Dou, Wenchao3; Geng, Changxi2; Lin, Mian1,3; Jiang, Wenbin1,3; Ji, Lili1,3; Cao, Gaohui1,3; Lin M(林缅); Jiang WB(江文滨); Jiang WB(江文滨); Ji LL(姬莉莉)
刊名ACS OMEGA
出版日期2024-06-14
卷号9期号:26页码:28648-28658
ISSN号2470-1343
DOI10.1021/acsomega.4c02707
通讯作者Lin, Mian(linmian@imech.ac.cn)
英文摘要Basalt is a suitable target area for CO2 storage. Clarifying the evolution of the pore structure during CO2-fluid-basalt interactions is a crucial element in the preparation of a CO2 geologic storage operation. In this study, a pore-scale phase field model is proposed to simulate the CO2-fluid-basalt interaction process of Snake River Plain basalt. Our model is suitable for complex multimineral natural rocks, and the initial mineral distribution before the reaction can be completely based on a real 3D rock image without the need to simplify the mineral geometry. The simulation results demonstrate that after 120 days of dissolution-precipitation reaction, the volume of secondary minerals (3.75%) exceeds that of dissolved minerals (2.01%), leading to a reduction in porosity by 1.74%. The pore structure of the basalt changes significantly, and the connectivity is obviously reduced. The effects of temperature and pressure on the reaction rate were examined to guide site selection for CO2 sequestration. The results show that increasing temperature and pressure can accelerate the reaction rate, but the impact of pressure on the reaction rate is negligible compared to the significant influence of temperature. Therefore, an area with a high geothermal gradient is conducive to geological sequestration.
WOS关键词CARBON-DIOXIDE SEQUESTRATION ; REACTIVE TRANSPORT ; CO2-RICH BRINE ; DEGREES-C ; DISSOLUTION ; BASALT ; FLOW ; EVOLUTION ; PRECIPITATION ; DISPOSAL
资助项目National Natural Science Foundation of China[42030808] ; National Natural Science Foundation of China[42302174] ; National Natural Science Foundation of China[2022M723231] ; China Postdoctoral Science Foundation
WOS研究方向Chemistry
语种英语
WOS记录号WOS:001248709600001
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Postdoctoral Science Foundation
源URL[http://dspace.imech.ac.cn/handle/311007/95784]  
专题力学研究所_流固耦合系统力学重点实验室(2012-)
通讯作者Lin, Mian; Lin M(林缅)
作者单位1.Univ Chinese Acad Sci, Beijing 100190, Peoples R China
2.1 Geol Mud Logging Co, Daqing Drilling & Explorat Engn Co, Daqing 163411, Peoples R China
3.Chinese Acad Sci, Inst Mech, Key Lab Mech Fluid Solid Coupling Syst, Beijing 100190, Peoples R China
推荐引用方式
GB/T 7714
Dou, Wenchao,Geng, Changxi,Lin, Mian,et al. A Pore-Scale Phase Field Model for CO2-Fluid-Basalt Interactions[J]. ACS OMEGA,2024,9(26):28648-28658.
APA Dou, Wenchao.,Geng, Changxi.,Lin, Mian.,Jiang, Wenbin.,Ji, Lili.,...&Cao GH.(2024).A Pore-Scale Phase Field Model for CO2-Fluid-Basalt Interactions.ACS OMEGA,9(26),28648-28658.
MLA Dou, Wenchao,et al."A Pore-Scale Phase Field Model for CO2-Fluid-Basalt Interactions".ACS OMEGA 9.26(2024):28648-28658.

入库方式: OAI收割

来源:力学研究所

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