Experimental Study on the Response of Cracked Sandstone to the Intermediate Principal Stress Coupled with Pore Pressure

Qinming Liang; Gun Huang; Jie Zheng; Weile Geng; Jinyong Huang; Guowen Sun

doi:10.1021/acsomega.4c02233

Experimental Study on the Response of Cracked Sandstone to the Intermediate Principal Stress Coupled with Pore Pressure

ACS Omega. 2024 May 2;9(19):21528-21537. doi: 10.1021/acsomega.4c02233. eCollection 2024 May 14.

Authors

Qinming Liang^{1

2}, Gun Huang^{1

2}, Jie Zheng³, Weile Geng⁴, Jinyong Huang^{1

2}, Guowen Sun⁵

Affiliations

¹ State Key Laboratory of Coal Mine Disaster Dynamics and Control, Chongqing University, Chongqing 400044, China.
² School of Resources and Safety Engineering, Chongqing University, Chongqing 400044, China.
³ School of Geology and Mining Engineering, Xinjiang University, Urumqi 830046, China.
⁴ Institute of Safety and Management Engineering, Hunan Institute of Technology, Hengyang 421002, China.
⁵ Technology Department, Chongqing Vocational Institute of Engineering, Chongqing 400000, China.

Abstract

Underground fractured rock masses are susceptible to failure under the combined influence of true triaxial stresses and pore pressure, posing severe threats to personnel and production safety of underground engineering. To investigate the influence of intermediate principal stress (σ₂) on the mechanical and water diffusion volume change (ΔV) characteristics during the failure process of cracked rocks under stable pore pressure, this study conducted true triaxial strength experiments on cracked sandstone with stable pore pressure. The results demonstrated that with the increase of σ₂, crack initiation stress (σ_ci), crack damage stress (σ_cd) and the peak stress (σ_1,peak) of cracked sandstone initially increase and then decrease. Conversely, ΔV tends to decrease first and then increase with the increase of σ₂. This inverse relationship indicates that under elevated σ₂, the decreased strength of cracked rock could lead to an increase in ΔV, which may increase the probability of water inrush disasters. The findings of this study provide a theoretical reference for the stability of rock mass engineering and the prevention of water inrush disasters.