首页> 外文期刊>Bulletin of engineering geology and the environment >Cooperative monitoring and numerical investigation on the stability of the south slope of the Fushun west open-pit mine
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Cooperative monitoring and numerical investigation on the stability of the south slope of the Fushun west open-pit mine

机译:抚顺西露天矿南帮稳定性的协同监测与数值研究。

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摘要

The south slope of the Fushun west open-pit mine in China is geologically complex and is a high-steep rock slope. In recent years, a larger deformation has appeared in the south slope, with the gradual formation of a potential landsliding block that is estimated to be over 300 m(3). The east and south boundaries of the block have been identified using different monitoring techniques. However the west boundary has not yet been clearly delineated, a situation which undermines safety assessments and the slope management of the mine. The focus of this was on how the microseismic technology, DInSAR technique and the numerical method are used to determine the shape and formation of the west boundary of the potential sliding block. We found that the upper part of west boundary as determined by numerical simulation is concordant with that determined by microseismic monitoring. The surface deformation area coincides with the DInSAR monitoring results and damage area based on in situ observations. Numerical simulation provides supplementary information on the distribution of stress and the formation process of the west boundary that cannot be observed directly on-site. The microseismic monitoring system was able to capture the progressive rupture of the west boundary during the deformation of the block. The cooperative monitoring strategy together with the numerical simulation can delineate the sliding surface and provide a method for a comprehensive assessment of the slope stability of other similar open-pit mines.
机译:中国抚顺西部露天矿的南坡地质复杂,是一个高陡岩石边坡。近年来,南坡出现了较大的变形,潜在的滑坡块逐渐形成,估计超过300 m(3)。已使用不同的监测技术确定了该街区的东边界和南边界。然而,尚未明确划定西边界,这破坏了安全评估和矿山的边坡管理。重点是如何使用微震技术,DInSAR技术和数值方法确定潜在滑块西边界的形状和形成。我们发现,通过数值模拟确定的西边界的上部与通过微震监测确定的上部一致。表面变形区域与DInSAR监测结果和基于原位观测的损伤区域一致。数值模拟提供了无法直接在现场观察到的有关应力分布和西边界形成过程的补充信息。微地震监测系统能够捕获块体变形过程中西边界的渐进破裂。协同监测策略和数值模拟可以勾画出滑动面,并为综合评估其他类似露天矿的边坡稳定性提供了一种方法。

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