Mechanism and implications of shut-in induced earthquakes

被引:3
|
作者
Wang, Xinyao [1 ]
Liu, Dianzhu [2 ]
Li, Xiao [3 ]
Gao, Quanchen [4 ]
机构
[1] Liaoning Univ Technol, Sch Civil & Architectural Engn, Jinzhou 121001, Peoples R China
[2] Tsinghua Univ, Inst Publ Safety Res, Beijing 100084, Peoples R China
[3] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Shale Gas & Geoengn, Beijing 100029, Peoples R China
[4] China Univ Min & Technol Beijing, Sch Mech & Civil Engn, Beijing 100083, Peoples R China
基金
中国国家自然科学基金;
关键词
Shut-in induced earthquake; Fluid pressurization rate; Fluid pressure non -uniform; Fracture surface evolution; Fluid pressure gradient; pressure distribution;
D O I
10.1016/j.aej.2022.09.042
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Fluid pressurization rate is an important inducement to fracture slip. In order to char-acterize the fracture slip initiation and slip mode during fluid pressurization, a series of stepwise injection induced shear tests were carried out. Results show that fracture slip initiation depends on fluid pressure and roughness of fracture surface. Fluid pressurization rate, fluid pressure non- uniform distribution all affect fracture slip initiation. Reducing fluid pressurization rate seems can-not effectively avoid induced earthquake, but can delay the time and scale of induced earthquake, especially can alleviate induced earthquake after shut-in. Earthquake induced after shut-in may be caused by secondary damage of concave-convex body on fault surface under the action of fluctuat-ing pressure generated from injection wells or underground water sources around fault. Further-more, a new view is proposed that the change of fluid pressure gradient on fracture surface is an important complementary mechanism for shut-in induced earthquakes. (c) 2022 THE AUTHORS. Published by Elsevier BV on behalf of Faculty of Engineering, Alexandria University. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/ licenses/by-nc-nd/4.0/).
引用
收藏
页码:837 / 846
页数:10
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