{"title":"Shear behavior of grouted rock joints under a cyclic normal load","authors":"Xianda Feng, Yishun Wang, Yingrui Lu, Qi Qiu","doi":"10.1007/s10064-026-05310-6","DOIUrl":null,"url":null,"abstract":"<div><p>In underground engineering, the surrounding rock is susceptible to instability and failure under dynamic disturbance loads. To investigate this issue, cyclic shear tests were conducted on grouted rough rock joints under a dynamic normal load. The effects of the initial normal load (<span>\\(\\:{F}_{\\text{n}\\text{s}}\\)</span>), dynamic normal load amplitude (<span>\\(\\:{F}_{\\text{A}}\\)</span>), and dynamic normal load frequency (<span>\\(\\:{f}_{\\text{n}}\\)</span>) on the shear behavior of the grouted joints were systematically investigated. The shear stress–shear displacement curves exhibited clear two-stage behavior. In the first cycle, influenced by grouting reinforcement, the curves exhibited fluctuating peak values. As <span>\\(\\:{F}_{\\text{n}\\text{s}}\\)</span> increased from 20 kN to 100 kN, the peak shear strength increased by approximately 125.66%. In subsequent cycles, owing to the shearing of the rock-grout bonding interface and cement asperities, the curves transitioned to a fluctuation-dominated slip mode governed by steady-state friction. The normal displacement–shear displacement curves consistently exhibited a fluctuating “V”-shaped pattern across all cycles. The average dilation angle exhibited a decreasing-then-increasing trend with an increasing number of load cycles. The magnitude of the phase shift increased linearly with <span>\\(\\:{F}_{\\text{A}}\\)</span> but decreased exponentially with <span>\\(\\:{f}_{\\text{n}}\\)</span>. The phase shift proportion of the grouted joint reached its maximum in the frequency range of 0.5–1 Hz. The failure characteristics of the joint surface were the fracture of the rock–grout bonding interface and the continuous abrasion of the cemented grout body by the joint surface. These findings provide valuable insights for evaluating the stability of grouted surrounding rock under dynamic disturbances.</p></div>","PeriodicalId":500,"journal":{"name":"Bulletin of Engineering Geology and the Environment","volume":"85 10","pages":""},"PeriodicalIF":4.9000,"publicationDate":"2026-09-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Bulletin of Engineering Geology and the Environment","FirstCategoryId":"5","ListUrlMain":"https://link.springer.com/article/10.1007/s10064-026-05310-6","RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENGINEERING, ENVIRONMENTAL","Score":null,"Total":0}
引用次数: 0
Abstract
In underground engineering, the surrounding rock is susceptible to instability and failure under dynamic disturbance loads. To investigate this issue, cyclic shear tests were conducted on grouted rough rock joints under a dynamic normal load. The effects of the initial normal load (\(\:{F}_{\text{n}\text{s}}\)), dynamic normal load amplitude (\(\:{F}_{\text{A}}\)), and dynamic normal load frequency (\(\:{f}_{\text{n}}\)) on the shear behavior of the grouted joints were systematically investigated. The shear stress–shear displacement curves exhibited clear two-stage behavior. In the first cycle, influenced by grouting reinforcement, the curves exhibited fluctuating peak values. As \(\:{F}_{\text{n}\text{s}}\) increased from 20 kN to 100 kN, the peak shear strength increased by approximately 125.66%. In subsequent cycles, owing to the shearing of the rock-grout bonding interface and cement asperities, the curves transitioned to a fluctuation-dominated slip mode governed by steady-state friction. The normal displacement–shear displacement curves consistently exhibited a fluctuating “V”-shaped pattern across all cycles. The average dilation angle exhibited a decreasing-then-increasing trend with an increasing number of load cycles. The magnitude of the phase shift increased linearly with \(\:{F}_{\text{A}}\) but decreased exponentially with \(\:{f}_{\text{n}}\). The phase shift proportion of the grouted joint reached its maximum in the frequency range of 0.5–1 Hz. The failure characteristics of the joint surface were the fracture of the rock–grout bonding interface and the continuous abrasion of the cemented grout body by the joint surface. These findings provide valuable insights for evaluating the stability of grouted surrounding rock under dynamic disturbances.
地下工程中,围岩在动扰动荷载作用下易失稳破坏。为了研究这一问题,在动法向荷载作用下,对灌浆粗糙岩石节理进行了循环剪切试验。系统研究了初始法向荷载(\(\:{F}_{\text{n}\text{s}}\))、动法向荷载幅值(\(\:{F}_{\text{A}}\))和动法向荷载频率(\(\:{f}_{\text{n}}\))对注浆节点抗剪性能的影响。剪切应力-剪切位移曲线表现出明显的两阶段特征。在第一个周期,受注浆加固的影响,曲线峰值出现波动。当\(\:{F}_{\text{n}\text{s}}\)从20 kN增加到100 kN时,峰值抗剪强度增加了约125.66%. In subsequent cycles, owing to the shearing of the rock-grout bonding interface and cement asperities, the curves transitioned to a fluctuation-dominated slip mode governed by steady-state friction. The normal displacement–shear displacement curves consistently exhibited a fluctuating “V”-shaped pattern across all cycles. The average dilation angle exhibited a decreasing-then-increasing trend with an increasing number of load cycles. The magnitude of the phase shift increased linearly with \(\:{F}_{\text{A}}\) but decreased exponentially with \(\:{f}_{\text{n}}\). The phase shift proportion of the grouted joint reached its maximum in the frequency range of 0.5–1 Hz. The failure characteristics of the joint surface were the fracture of the rock–grout bonding interface and the continuous abrasion of the cemented grout body by the joint surface. These findings provide valuable insights for evaluating the stability of grouted surrounding rock under dynamic disturbances.
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.