Rapid evaluation of the stability of the wedge-shaped hazardous rock mass based on non-contact measurements
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摘要: 【目的】 基于传统接触式测量无法满足楔形危岩体施工快速高效安全需求的现状,本文将采用非接触测量的方法获取与分析楔形危岩体参数,通过得到的参数分析楔形危岩体在不同工况下的稳定性。【方法】 以某抽水蓄能电站上水库楔形危岩体为例,在工程地质野外精细调查的基础上,开展了三维激光扫描野外测量,获取了楔形危岩体高精度点云数据。采用最小二乘法拟合得到临空面所在的平面,确定楔形体所在边坡的坡角和坡高。点云运用局部点云拟合的办法确定法向量,将得到的法向量通过计算求出结构面产状。结合Alpha Shapes的方法计算得出危岩体体积,利用刚体极限平衡法对楔形危岩体进行稳定性评价。【结果】 结果表明:在天然、暴雨和地震工况下,楔形危岩体的稳定性系数分别为:1.131(基本稳定)、0.896(不稳定)和0.917(不稳定)。【结论】 本文将非接触测量与智能识别运用到楔形危岩体的稳定性评价中,整体用时102分钟,大大提高了稳定性评价效率并降低了工程施工的风险,为今后危岩体的稳定性快速评价提供了一个新方法。Abstract: [Objective] With the frequent occurrence of landslide disasters in China, it is indispensable to strengthen the research on unstable rock mass and unstable slopes, due to the inability to quantify or other shortcomings of the traditional analysis methods. In order to improve the traditional scheme, we adopt the non-contact measurement method to obtain and analyse the parameters of wedge-shaped unstable rock mass, and analyse the stability of wedge-shaped unstable rock mass under different working conditions by the obtained parameters. [Methods] Taking the wedge-shaped unstable rock mass in the upper reservoir of a pumped storage power station as an example, this paper reveals the basic features and stability influencing factors of the unstable rock mass based on the fine engineering geological field investigation. A long-distance 3D laser scanning system is used to obtain high-precision point cloud data of the slope. The spatial parameters of the wedge-shaped unstable rock mass are obtained through preprocessing, and the plane where the critical surface is located is also obtained through least-squares fitting to determine the slope angle and slope height of the wedge-shaped body. The point cloud is fitted with local point cloud to determine the normal vector, and the obtained normal vector is calculated to find out the discontinuity occurrence. The Alpha shape method is used to calculate the volume of the unstable rock mass, and the most suitable radius parameter is obtained by comparing with the actual unstable rock mass. Then the limit equilibrium method is used to evaluate the stability of the unstable rock mass. [Results] Through the experiment to get different states of the rock mass capacity, cohesion, friction angle, etc., combined with access to the specification to determine the seismic coefficient and calculation of the geometric parameters, the results show that: in the natural conditions, the wedge-shaped unstable rock stability coefficient of 1.131 is in an essentially stable state; in the rainstorm conditions, the stability coefficient of the wedge-shaped unstable rock body 0.896, in a state of instability; in the seismic condition, the wedge-shaped unstable rock body The stability coefficient of the wedge is 0.917, which is unstable. [Conclusion] In this paper, non-contact measurement and intelligent recognition are applied to the stability analysis of wedge-shaped unstable rock mass, and the overall time taken is 102 minutes, which greatly improves the stability analysis efficiency and reduces the risk of engineering construction.
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