中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Numerical simulation of pressure evolution and migration of hydraulic fracturing fluids in the shale gas reservoirs of Sichuan Basin, China

文献类型:期刊论文

作者Wang, Liheng1,2; Dong, Yanhui1,2,3; Zhang, Qian1,2,3; Duan, Ruiqi1,2,3
刊名JOURNAL OF HYDROLOGY
出版日期2020-09-01
卷号588页码:10
ISSN号0022-1694
关键词Shallow groundwater Hydraulic fracturing Dual-medium model Numerical simulation Shale gas Sichuan Basin
DOI10.1016/j.jhydrol.2020.125082
英文摘要One of the main environmental issues associated with hydraulic fracturing (HF) is the upward migration of the HF fluids from a shale reservoir to reach the shallow drinking water aquifers through preferential flow paths, such as fractures or faults. Oversimplified model structures or arbitrary boundary conditions were used in the previous studies, resulting in inaccurate results. To better describe the flow and transport in fractures/faults and matrix pores, a dual-medium model including fracture (fault) and matrix was established in this study to understand the evolution that occurs in reservoir pressure during HF and the long-term migration of HF fluids in deep geological formations, considering Sichuan Basin, China, as a case study. Both HF fractures and pre-existing natural faults were characterized as highly permeable preferential flow channels. Simulation results show that the spatial distribution of pressure in shallow aquifers is mainly controlled by the topography while it is controlled by overpressure in the deep strata. HF fluids were not found to contaminate the shallow groundwater throughout the simulation period, even in the worst scenario. A sensitivity analysis is carried out to quantify and understand the influence of a broad range of possibilities of parameters, such as HF fracture, reservoir properties and HF operation. The results suggest that the reservoir properties and the duration over which the injection of HF fluid take place are the most important factors influencing the spatiotemporal distribution of HF. Moreover, HF fluids are removed from the formation by the production of gas, meaning that these fluids are unlikely to contaminate the shallow aquifers of the Sichuan Basin.
WOS关键词POTENTIAL CONTAMINANT PATHWAYS ; GROUNDWATER-FLOW SYSTEMS ; NATURAL-GAS ; SEDIMENTARY BASINS ; OVERPRESSURE ; AQUIFERS ; PERMEABILITY ; SUBSURFACE ; TRAPS ; FIELD
资助项目National Science and Technology Major Project of China[2017ZX05008003-021] ; National Natural Science Foundation of China[41702273] ; China Scholarship Council[201904910227]
WOS研究方向Engineering ; Geology ; Water Resources
语种英语
出版者ELSEVIER
WOS记录号WOS:000568826300060
资助机构National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; National Science and Technology Major Project of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council ; China Scholarship Council
源URL[http://ir.iggcas.ac.cn/handle/132A11/98247]  
专题地质与地球物理研究所_中国科学院页岩气与地质工程重点实验室
通讯作者Dong, Yanhui
作者单位1.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Shale Gas & Geoengn, POB 9825, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Wang, Liheng,Dong, Yanhui,Zhang, Qian,et al. Numerical simulation of pressure evolution and migration of hydraulic fracturing fluids in the shale gas reservoirs of Sichuan Basin, China[J]. JOURNAL OF HYDROLOGY,2020,588:10.
APA Wang, Liheng,Dong, Yanhui,Zhang, Qian,&Duan, Ruiqi.(2020).Numerical simulation of pressure evolution and migration of hydraulic fracturing fluids in the shale gas reservoirs of Sichuan Basin, China.JOURNAL OF HYDROLOGY,588,10.
MLA Wang, Liheng,et al."Numerical simulation of pressure evolution and migration of hydraulic fracturing fluids in the shale gas reservoirs of Sichuan Basin, China".JOURNAL OF HYDROLOGY 588(2020):10.

入库方式: OAI收割

来源:地质与地球物理研究所

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