Overburden failure and the prevention of water and sand inrush during coal mining under thin bedrock

Yang Weifeng, Xia Xiaohong, Zhao Guorong, Ji Yubin, Shen Dingyi
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引用次数: 16

Abstract

Coal mining under thin bedrock or thick unconsolidated soil layers brings mining problems related to these special geological conditions. The meaning of the term “thin bedrock” is defined through the thickness statistics of the coal seam and the bedrock layer. The coal-bearing strata having thick, unconsolidated aquifers and thin bedrock located at the Taiping Coal Mine in Shandong province were taken as a geological prototype for subsequent study. The geological, hydro-geological and engineering characteristics of the thin bedrock were analyzed. An engineering geological model was than established. Overburden failure and the development of “Three Zones” were studied by physical model tests. The rupture pattern and rock failure were analyzed for mining conditions under thin bedrock. The height of the caving zone and the freely flowing water fractured zone of different mining thicknesses were separately calculated. The results show that a mining thickness greater than 3.5 m causes the height of the freely flowing water fractured zone to be sufficient to touch the weathered zone and the bottom of the Quaternary system aquifer, to various degrees. This, then, would lead to water and sand inrush into the working face. Measures to prevent water and sand flow inrush disasters by eliminating the power source are put foreword. A field dewatering scheme was designed and observational data were obtained. The dewatering project had an obvious effect and the water level at working face number 8309 dropped to a safe level. The average draw down of the groundwater was observed to be 7.86 m. This showed that the dewatering project played a role in decreasing the hydraulic pressure and ensuring safety mining.

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薄基岩下覆岩破坏与突水涌砂防治
在较薄的基岩或较厚的松散土层下采煤,会带来与这些特殊地质条件相关的采矿问题。“薄基岩”一词的含义是通过煤层和基岩层的厚度统计来定义的。本文以山东太平煤矿含煤地层为研究对象,以其厚、松散含水层和薄基岩为地质原型。分析了薄基岩的地质、水文地质和工程特征。建立了工程地质模型。通过物理模型试验研究了上覆岩层破坏及“三带”发育规律。分析了薄基岩开采条件下的破裂模式和岩石破坏。分别计算了不同开采厚度的崩落带高度和自由流水裂隙带高度。结果表明:采厚大于3.5 m时,自由流水裂隙带的高度足以不同程度地接触风化带和第四系含水层底部;这将导致水和砂涌进工作面。提出了通过消除电源来防止水沙涌流灾害的措施。设计了野外降水方案,并获得了观测资料。脱水工程效果明显,8309工作面水位降至安全水平。地下水的平均下渗为7.86 m。由此可见,降水工程对降低水压、保证安全开采起到了一定的作用。
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