JRMGE / Vol 17 / Issue 4

Article

Real-time seepage and instability of fractured granite subjected to hydro-shearing under different critical slip states

Peng Zhao, Zijun Feng, Hanmo Nan, Peihua Jin, Chunsheng Deng, Yubin Li

Show More

a College of Mining Engineering, Taiyuan University of Technology, Taiyuan, 030000, China
b Key Lab of In-situ Modification of Deposit Properties for Improving Mining, Ministry of Education of the People’s Republic of China, Taiyuan University of
Technology, Taiyuan, 030000, China
c College of Engineering, Tibet University, Lhasa, 850000, China


2025, 17(4): 2396-2415. doi:10.1016/j.jrmge.2024.11.018


Received: 2024-07-12 / Revised: 2024-09-14 / Accepted: 2024-11-07 / Available online: 2024-11-26

2025, 17(4): 2396-2415.

doi:10.1016/j.jrmge.2024.11.018


Received: 2024-07-12

Revised: 2024-09-14

Accepted: 2024-11-07

Available online: 2024-11-26


Abstract:

In this study, a high-confining pressure and real-time large-displacement shearing-flow setup was developed. The test setup can be used to analyze the injection pressure conditions that increase the hydro-shearing permeability and injection-induced seismicity during hot dry rock geothermal extraction. For optimizing injection strategies and improving engineering safety, real-time permeability, deformation, and energy release characteristics of fractured granite samples driven by injected water pressure under different critical sliding conditions were evaluated. The results indicated that: (1) A low injection water pressure induced intermittent small-deformation stick–slip behavior in fractures, and a high injection pressure primarily caused continuous high-speed large-deformation sliding in fractures. The optimal injection water pressure range was defined for enhancing hydraulic shear permeability and preventing large injection-induced earthquakes. (2) Under the same experimental conditions, fracture sliding was deemed as the major factor that enhanced the hydraulic shear–permeability enhancement and the maximum permeability increased by 36.54 and 41.59 times, respectively, in above two slip modes. (3) Based on the real-time transient evolution of water pressure during fracture sliding, the variation coefficients of slip rate, permeability, and water pressure were fitted, and the results were different from those measured under quasi-static conditions. (4) The maximum and minimum shear strength criteria for injection-induced fracture sliding were also determined (μ = 0.6665 and μ = 0.1645, respectively, μ is friction coefficient). Using the 3D (three-dimensional) fracture surface scanning technology, the weakening effect of injection pressure on fracture surface damage characteristics was determined, which provided evidence for the geological markers of fault sliding mode and sliding nature transitions under the fluid influence.

Download PDF:


Keywords: Hydro-shearing, Reservoir modification, Injection-induced seismicity, Real-time shear-flowing, Frictional noise

Show Figure(s)


Supplementary Material

Download Document:


Share and Cite

Peng Zhao, Zijun Feng, Hanmo Nan, Peihua Jin, Chunsheng Deng, Yubin Li, 2025. Real-time seepage and instability of fractured granite subjected to hydro-shearing under different critical slip states. J. Rock Mech. Geotech. Eng. 17 (4), 2396-2415.

Author(s) Information

Zijun Feng

✉️ fengzijun@tyut.edu.cn

Zijun Feng is a Professor at Taiyuan University of Technology, China. He is the recipient of the National Excellent Young Scientists Fund of China, Vice Dean of College of Mining Engineering and Deputy Director of the Key Lab of In-situ Modification of Deposit Properties for Improving Mining, Ministry of Education of the People’s Republic of China, Taiyuan University of Technology. He has received a Technological Invention Award in Shanxi Province (1st class, Second author) and a Natural Science Award in Shanxi Province (2nd class, First author). He has been engaged in the basic theory and engineering practice research on high-temperature and high-pressure coal-rock mechanics, geothermal development in dry hot rock, in situ heat injection mining of low-rank coal, and geological storage of CO2.