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Analytical estimation of stress distribution in interbedded layers and its implication to rockburst in strong layer

机译:层间应力分布的解析估计及其对强层岩爆的影响

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In-situ stress is one of the most important factors affecting the safety and stability of underground excavations. Past measurement results show that the magnitudes and directions of in- situ stresses vary substantially in different lithological formations. However, the relationship between stresses distribution and rock mechanical properties is still unclear. In this paper, the stress distribution in interbedded strong and weak layers was analytically studied based on linear elastic mechanics. Derived solutions were validated by comparison with Finite Element Method (FEM) results and field measurement results. Comparisons show that analytical results agree with the numerical results, and the maximum difference is less than 1%. The maximum difference between the analytical results and field measurements is 10.8%. Furthermore, the derived solution was used to evaluate the stress distribution in a geologically abnormal area in the Neelum-Jhelum (NJ) hydroplant project. Stress concentration state in strong layers changes as the strata change from sub-vertical to sub-horizontal, and the stress state in the sub-horizontal strata greatly favours rockburst according to the Turchaninov criterion. The change in stress concentration state might be the underlying reason for the severe rockburst in the abnormal structure area in the NJ project.
机译:地应力是影响地下工程安全性和稳定性的最重要因素之一。过去的测量结果表明,在不同的岩性地层中,原位应力的大小和方向存在很大差异。但是,应力分布与岩石力学性能之间的关系仍不清楚。本文基于线性弹性力学,对层间强弱层之间的应力分布进行了分析研究。通过与有限元方法(FEM)结果和现场测量结果进行比较来验证派生的解决方案。比较表明,分析结果与数值结果吻合,最大差异小于1%。分析结果与现场测量之间的最大差值为10.8%。此外,导出的解决方案还用于评估Neelum-Jhelum(NJ)水电厂项目中地质异常区域中的应力分布。随着地层从亚垂直向亚水平变化,强层中的应力集中状态发生变化,并且根据Turchaninov准则,亚水平地层中的应力状态极大地有利于岩爆。应力集中状态的变化可能是新泽西项目异常结构区域发生严重岩爆的根本原因。

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