Fracture distribution in overburden strata induced by underground mining

Wenli Yao, Enzhi Wang, Xiaoli Liu, Ran Zhou
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引用次数: 3

Abstract

Coal-mining activities give rise to a series of ecological environmental problems, such as ground settlement and groundwater pollution. In fact, they are mainly caused by mining-induced fractures. Hence, it is necessary to study the mining-induced fracture distribution to identify the behavior of rock mass movement. However, the fractures in overburden strata cannot be directly measured owing to the special condition. Therefore, the majority of previous studies are based on experiments or experience. For this reason, this study first used a discrete element method to simulate the shape of mining-induced fractures in overburden strata. Then, a geophysical tool of transient electromagnetic method (TEM) was used to investigate the mining-induced fracture distribution. Based on the low-resistivity anomaly area, the water-rich area in overburden strata was analyzed to be mainly caused by fracture seepage. Through the mutual authentication between numerical simulation and TEM results, the mining-induced fractures in overburden strata were explored. This study can enhance the understanding of mining-induced fracture distribution on the one hand and guarantee the coal mining safety on the other, thus guiding the coordinated development between coal mining and environmental protection.

Abstract Image

地下开采诱发覆岩裂隙分布
煤矿开采带来了地面沉降、地下水污染等一系列生态环境问题。实际上,它们主要是由采动裂隙引起的。因此,有必要对采动裂隙分布进行研究,以识别岩体的运动特征。但是,由于特殊的条件,覆岩中的裂缝不能直接测量。因此,以往的研究大多是基于实验或经验。为此,本研究首先采用离散元法对覆岩采动裂隙形态进行模拟。然后,利用瞬变电磁法(TEM)地球物理工具对采动裂隙分布进行了研究。以低阻异常区为基础,分析了上覆岩层富水区主要由裂缝渗流引起。通过数值模拟与瞬变电磁法结果的相互验证,对覆岩采动裂隙进行了探讨。该研究一方面可以增强对采动裂隙分布的认识,另一方面可以保障煤矿开采安全,从而指导煤矿开采与环境保护的协调发展。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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CiteScore
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