Numerical analysis of water inrush from working-face floor during mining

Qing-hua ZHU, Mei-mei FENG, Xian-biao MAO
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引用次数: 26

Abstract

Confined water in the Ordovician limestone is one of the hidden troubles that threaten safe production of mines in north China. A numerical model of the key strata was developed. It included the structural characteristics and mechanical properties of the floor rock at the working face of a particular coal mine. The model was used to predict failure modes and to help establish rules for safe mining above the aquifer. The distribution of deformation, failure and seepage was simulated by using Dilian Mechsoft's Realistic Failure Process Analysis (RFPA2D) program. The stress distribution, the deformation and the flow vectors were also obtained. The results indicate that: 1) The original balance of the stress and seepage fields is disturbed due to coal mining; and 2) As the working face advances different deformation, or failure, appears in the surrounding rocks, the water-resisting strata in floor may be destroyed and the passage of water from the aquifer into the mine may occur. The combined action of mining stress and water pressure ultimately lead to water inrush from the floor.

采动工作面底板突水数值分析
奥陶系灰岩承压水是威胁北方煤矿安全生产的隐患之一。建立了关键地层的数值模型。它包括某煤矿工作面底板岩石的结构特征和力学特性。该模型用于预测破坏模式,并帮助建立含水层以上的安全开采规则。采用dillian Mechsoft的现实破坏过程分析(RFPA2D)程序对其变形、破坏和渗流分布进行了模拟。得到了应力分布、变形和流动矢量。结果表明:①采煤破坏了原应力场和渗流场的平衡;2)随着工作面推进,围岩出现不同程度的变形或破坏,底板的抗水岩层可能被破坏,含水层的水可能进入矿井。采动应力和水压的共同作用最终导致底板突水。
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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