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Model test on slope deformation and failure caused by transition from open-pit to underground mining

机译:从开坑到地下挖掘引起的斜坡变形和失效模型试验

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Open-pit (OP) and underground (UG) mining are usually used to exploit shallow and deep ore deposits, respectively. When mine deposit starts from shallow subsurface and extends to a great depth, sequential use of OP and UG mining is an efficient and economical way to maintain mining productivity. However, a transition from OP to UG mining could induce significant rock movements that cause the slope instability of the open pit. Based on Yanqianshan Iron Mine, which was in the transition from OP to UG mining, a large-scale two-dimensional (2D) model test was built according to the similar theory. Thereafter, the UG mining was carried out to mimic the process of transition from OP to UG mining to disclose the triggered rock movement as well as to assess the associated slope instability. By jointly using three-dimensional (3D) laser scanning, distributed fiber optics, and digital photogrammetry measurement, the deformations, movements and strains of the rock slope during mining were monitored. The obtained data showed that the transition from OP to UG mining led to significant slope movements and deformations that can trigger catastrophic slope failure. The progressive movement of the slope could be divided into three stages: onset of micro-fracture, propagation of tensile cracks, and the overturning and/or sliding of slopes. The failure mode depended on the orientation of structural joints of the rock mass as well as the formation of tension cracks. This study also proved that these non-contact monitoring technologies were valid methods to acquire the interior strain and external deformation with high precision.
机译:露天坑(OP)和地下(UG)挖掘通常分别用于利用浅层和深矿床沉积物。当矿井矿床从浅层地下开始并扩展到一个很大的深度时,顺序使用OP和UG挖掘是一种高效且经济的方式来维持采矿生产率。然而,从OP到UG挖掘的过渡可以引起显着的岩石运动,导致露天坑的斜坡不稳定性。基于Yanqianshan Iron Lim的基于OP到UG挖掘的转型,根据类似理论建立了大规模的二维(2D)模型试验。此后,进行UG挖掘以模仿从OP到UG挖掘的转变过程以公开触发的岩石运动,以及评估相关的斜率不稳定性。通过共同使用三维(3D)激光扫描,分布式光纤和数码摄影测量测量,监测挖掘过程中岩石斜率的变形,运动和菌株。所获得的数据显示,从OP到UG挖掘的转变导致了可以引发灾难性斜坡故障的显着斜坡运动和变形。斜率的渐进运动可分为三个阶段:发作微骨折,拉伸裂缝的传播,以及倾斜和/或滑动的斜坡。故障模式取决于岩体结构关节的方向以及张力裂缝的形成。本研究还证明,这些非接触监测技术是使用高精度获取内部应变和外部变形的有效方法。

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