Mechanical behaviors of double-cracked limestone under hydro-mechanical coupling: Experimental, theoretical, and numerical investigation

Journal of Safety and Sustainability Pub Date : 2026-03-01 Epub Date: 2026-01-31 DOI:10.1016/j.jsasus.2026.01.002
Yanlin Zhao , Qiang Liu , Lianyang Zhang , Chunshun Zhang , Hang Lin
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Abstract

In this study, a series of laboratory experiments including triaxial compression tests, acoustic emission (AE) monitoring and discrete element numerical simulations, combined with a self-developed high-performance copper sheet-blocking hydraulic sealing method, are carried out to investigate the mechanical behaviors, fracture characteristics and hydro-mechanical (HM) coupling of double-cracked limestone. Effects of pore pressure (P), confining pressure (σ3), and crack inclination angle (α) on the stress–strain curves exhibiting multi-peak patterns, crack initiation stress, damage stress, peak strength, deformation modulus, Poisson's ratio, and AE signal characteristics of the double-cracked limestone specimens during the HM coupling progressive failure process are analyzed. The AE signal features include stronger signals under lower pore pressure and sparser AE ringing counts at larger inclination angles. Subsequently, a compression-shear fracture criterion incorporating crack inclination angle parameters is established based on the experimental results, and numerical simulations further clarify the failure modes of the specimens: tensile failure for those with a 15° crack inclination angle, tensile-shear failure for those with 45°, and shear failure for those with 75°, thereby revealing the HM coupling failure mechanism. These experimental results, numerical simulation findings and HM coupling failure mechanism provide a deep understanding to researchers and engineering technicians for monitoring and controlling rock stability in geological engineering projects under HM coupling environments.
水-力耦合作用下双裂石灰岩的力学行为:实验、理论和数值研究
通过三轴压缩试验、声发射监测和离散元数值模拟等室内实验,结合自主研发的高性能铜片封堵水力密封方法,对双裂石灰岩的力学行为、断裂特征及水-力耦合进行了研究。分析了孔隙压力(P)、围压(σ3)和裂纹倾角(α)对双裂纹灰岩试件HM耦合逐渐破坏过程中多峰型应力-应变曲线、裂纹起裂应力、损伤应力、峰值强度、变形模量、泊松比和声发射信号特征的影响。低孔隙压力条件下的声发射信号较强,大倾角条件下的声发射环数较少。在此基础上,建立了包含裂纹倾角参数的压剪破坏准则,并通过数值模拟进一步明确了试件的破坏模式:裂纹倾角为15°时试件的拉伸破坏、倾角为45°时试件的拉剪破坏、倾角为75°时试件的剪切破坏,揭示了HM耦合破坏机制。这些实验结果、数值模拟结果和HM耦合破坏机理,为研究人员和工程技术人员对HM耦合环境下地质工程项目岩石稳定性的监测和控制提供了深刻的认识。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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