煤矿冒落型突水溃沙的破碎砂岩水沙渗流特性试验研究

Experimental research on the seepage characteristics of water-sand flow in crushed sandstone of the coal mine collapse-type water inrush and sand gushing

  • 摘要: 在神东和陕北矿区浅埋煤层高强度开采过程中,冒落型突水溃沙已成为威胁顶板水害防控的典型矿山工程地质灾害。深入研究破碎岩体水沙渗流特性,对揭示冒落型突水溃沙致灾机理具有重要意义。基于此,利用自主研发的破碎岩体水沙渗流试验系统,以谢和平提出的岩石碎块累计质量的分形维度计算方法为基础,按照Talbot连续级配公式制备了不同粒径配比的破碎砂岩样品,设计了变孔隙度和粒径配比的水沙渗流试验,分析了破碎砂岩中水及水沙混合物的渗透率随孔隙度和粒径配比的变化规律,建立了考虑孔隙度比和分形维度的渗透率表达式,量化了水沙混合物黏度对渗透率计算结果的影响,揭示了破碎砂岩溃沙质量随孔隙度和粒径配比的变化规律,构建了渗透率和分形维度共同驱动的临界溃沙判据,以哈拉沟煤矿22402工作面为工程实例,验证了判据的准确性。研究结果表明:① 破碎砂岩的水沙渗流过程包括初始波动阶段、相对稳定阶段和衰减阶段,渗透率随孔隙度和Talbot幂指数的增大而增大,水渗流的渗透率大于水沙渗流的渗透率;② 破碎砂岩的溃沙质量随孔隙度和Talbot幂指数的增大而增大,且溃沙质量与渗透率呈近线性增长关系;③ 现有研究中多数学者采用水黏度代替水沙混合物黏度的简化算法在本文的计算中可导致最大18.3%的误差,对应现场尺度突水溃沙灾害中此误差可能超过800%;④ 引入分形维度可以将破碎砂岩渗透率拟合误差降低约56.43%,基于渗透率和分形维度对溃沙质量的变化规律提出的临界溃沙曲线在哈拉沟煤矿22402工作面应用效果良好。

     

    Abstract: In the high-intensity mining process of shallow buried coal seams in the Shendong and North Shaanxi mining areas, the collapse-type water inrush and sand gushing has become a typical geological hazard that threatens the prevention and control of roof water damage in mining engineering. Thoroughly studying the water and sand seepage characteristics of fractured rock masses is of great significance for revealing their disaster mechanisms and corresponding disaster prevention and control. In view of this, using the self-developed water-sand seepage test system of broken rock mass, based on the fractal dimension calculation method of cumulative mass of rock fragments proposed by Xie Heping, the broken sandstone samples with different particle size ratios were prepared according to the Talbot continuous gradation formula. The water-sand seepage test with variable porosity and particle size ratio was designed. The variation of permeability of water and water-sand mixture in broken sandstone with porosity and particle size ratio was analyzed. The permeability expression considering porosity ratio and fractal dimension was established, and the influence of the viscosity of water-sand mixture on permeability calculation results was quantified. The variation law of sand inrush mass of broken sandstone with porosity and particle size ratio is revealed, and the critical sand inrush criterion driven by permeability and fractal dimension is constructed. Taking the 22402 working face of Halagou Coal Mine as an engineering example, the accuracy of the criterion is verified. The results indicate that: ① The water-sand seepage process in crushed sandstone can be divided into three stages: initial fluctuation, relative stability, and decay. Permeability increases with porosity and Talbot’s power index, while water seepage exhibits higher permeability than water-sand seepage. ② The outflow mass of sand increases with porosity and Talbot’s power index, showing a near-linear relationship with permeability. ③ In existing research, many scholars have used simplified methods that use water viscosity as a substitute for water-sand mixture viscosity may introduce a maximum error of 18.3% in the calculations of this study, which could amplify to over 800% when upscaled to field conditions of water inrush and sand gushing disasters. ④ The introduction of fractal dimension can reduce the fitting error of fractured sandstone permeability by about 56.43%. The critical sand collapse curve proposed based on the variation law of permeability and fractal dimension on sand collapse quality has been applied well in the 22402 working face of Halagou Coal Mine.

     

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