Liu He, Jiaxin Yan, Junxiang Bi, Zihai Peng, Liwei Bai
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引用次数: 0
Abstract
The cyclic effects of wetting and drying on rock joints, driven by reservoir-level fluctuations, significantly influence the degradation of their shear mechanical behavior. This study investigates the degradation mechanisms of sandstone joint specimens under controlled wetting–drying cycles (WDCs), with a focus on the evolution of joint morphology and mechanical properties. A systematic experimental approach was adopted to analyze the effects of varying cycle numbers (n), joint wall compressive strengths (JCS), roughness parameters (r), and normal stresses (\({\sigma }_{n}\)) on degradation. The key findings reveal that, with increasing WDCs, joint surface roughness decreases, transitioning from rough to smooth, particularly during the initial six cycles. Shear behavior analysis shows a reduction in peak shear strength and an increase in peak shear displacement as the number of cycles increases. The study identifies the progressive weakening of JCS, r, and the basic friction angle (\({\varphi }_{b}\)) as the primary drivers of these changes. Two distinct failure mechanisms are observed: shear-off and wear, with wear failures becoming dominant as the number of cycles increases. A predictive shear strength model incorporating the weakening effects of WDCs is developed using regression analysis, achieving a mean relative error of 5.41%, thus validates its reliability. These findings provide new insights into rock joint behavior under fluctuating reservoir conditions and emphasize the critical role of mechanical and morphological degradation in hydraulic stability assessments.
在水库水位波动的驱动下,干湿循环作用对岩石节理剪切力学性能的退化有显著影响。研究了可控干湿循环作用下砂岩节理试样的退化机理,重点研究了节理形态和力学性能的演变。采用系统的实验方法,分析了不同循环次数(n)、节理壁抗压强度(JCS)、粗糙度参数(r)和正应力(\({\sigma }_{n}\))对降解的影响。关键发现表明,随着wdc的增加,节理表面粗糙度降低,从粗糙过渡到光滑,尤其是在最初的6个循环中。剪切性能分析表明,随着循环次数的增加,峰值剪切强度降低,峰值剪切位移增加。该研究确定JCS、r和基本摩擦角(\({\varphi }_{b}\))的逐渐减弱是这些变化的主要驱动因素。观察到两种不同的失效机制:剪切和磨损,随着循环次数的增加,磨损失效成为主导。利用回归分析建立了考虑wdc减弱效应的抗剪强度预测模型,平均相对误差为5.41%, thus validates its reliability. These findings provide new insights into rock joint behavior under fluctuating reservoir conditions and emphasize the critical role of mechanical and morphological degradation in hydraulic stability assessments.
期刊介绍:
Engineering geology is defined in the statutes of the IAEG as the science devoted to the investigation, study and solution of engineering and environmental problems which may arise as the result of the interaction between geology and the works or activities of man, as well as of the prediction of and development of measures for the prevention or remediation of geological hazards. Engineering geology embraces:
• the applications/implications of the geomorphology, structural geology, and hydrogeological conditions of geological formations;
• the characterisation of the mineralogical, physico-geomechanical, chemical and hydraulic properties of all earth materials involved in construction, resource recovery and environmental change;
• the assessment of the mechanical and hydrological behaviour of soil and rock masses;
• the prediction of changes to the above properties with time;
• the determination of the parameters to be considered in the stability analysis of engineering works and earth masses.