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

岩体分类 地质学 采矿工程 不稳定性 岩土工程 张力(地质) 变形(气象学) 断裂(地质) 地下开采(软岩) 极限抗拉强度 煤矿开采 工程类 材料科学 机械 冶金 海洋学 废物管理 物理
作者
Bin Zhang,Hanxun Wang,Jie Huang,Nengxiong Xu
出处
期刊:Geomechanics and Engineering [Technopress]
卷期号:19 (2): 167-178 被引量:5
标识
DOI:10.12989/gae.2019.19.2.167
摘要

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.
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