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Study on the Deformation Mechanism of the Wangxia Unstable Rock Mass in the Three Gorges Reservoir

机译:三峡库区王峡不稳定岩体变形机制研究

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Twice serious deformation occurred in the Wangxia unstable rock mass in 2010 and 2011 in Wushan country in the Three Gorges Reservoir. It formed a large dangerous factor for the local resident and channel safety. Based on the detailed investigation of the new cracks, deformation history, GPS observations, total station monitoring and crack displacement monitoring data analysis, analyzed comprehensively the deformation and reasons of the unstable rock. The researches show that the deformation type of the unstable rock mass contains gradual change and mutation, should adopt the corresponding monitoring methods and monitoring frequency in different deformation stages based on the geological survey and monitoring the key parts of the unstable rock mass. The destruction of the Wangxia unstable rock was a gradual process, controlled by 5 key cracks, which were crack T11, T12, T13, T16, and T10, consider the Wangxia unstable rock was subsided extrusion type collapse.
机译:2010年王峡不稳定的岩石群体发生了两倍的严重变形,2011年在三峡库区武山国家。它形成了当地居民和渠道安全的一个危险因素。基于对新裂缝,变形历史,GPS观测,全站仪监测和裂纹排量监测数据分析的详细调查,全面分析了不稳定岩石的变形和原因。研究表明,不稳定岩体的变形类型含有逐渐变化和突变,应基于地质调查采用不同变形阶段的相应监测方法和监测频率,监测不稳定岩体的关键部分。王霞不稳定岩石的破坏是一种渐进的过程,由5个关键裂缝控制,其裂缝T11,T12,T13,T16和T10,考虑王峡不稳定的岩石被剥离挤压型坍塌。

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