蒙陕接壤区深埋侏罗系煤层封闭不良钻孔出水特征研究

    Study on characteristics of drilling water in deeply buried Jurassic coal seam with poor sealing borehole in the border area of inner Mongolia and Shaanxi

    • 摘要: 封闭不良钻孔是诱发矿井突水事故的潜在充水通道,是蒙陕接壤区侏罗系煤田的主要隐蔽致灾因素。蒙陕接壤区深埋侏罗系煤田埋深普遍大于500 m,采掘期间,揭露封闭不良钻孔可能沟通煤层上部的强富水含水层,使其成为煤层的直接充水水源,从而影响煤矿的安全生产。为研究蒙陕接壤区深埋侏罗系煤层封闭不良钻孔出水特征,建立井下突水水源“三位一体”精准判别方法,通过与典型疏放水钻孔和水质化验数据进行对比,分析钻孔突水特征和水化学特征,运用分层聚类分析模型,分析封闭不良钻孔与煤层上覆含水层之间的水力联系。结合现场封闭不良钻孔封堵效果检验,分析封闭不良钻孔的致灾机理。结果表明:蒙陕接壤区白垩系孔隙−裂隙含水层系统和侏罗系裂隙含水层系统水质特征存在较大差异,其中,白垩系孔隙−裂隙含水层系统水化学类型为HCO3−Na型水,其特征离子HCO3−占阴离子45%以上;侏罗系裂隙含水层系统水样水化学类型为SO4−Na型,其特征离子SO42−占阴离子40%以上。同时,利用井下出水点的突水特征与典型疏放水钻孔进行对比,快速辨别充水层位,并提出了相应的封堵效果检验方法,可为后续矿井井下封闭不良钻孔突水应急处置及钻孔封堵效果探查提供参考。

       

      Abstract: Poor sealing boreholes are the potential water-filling channels that induce mine water inrush accidents, and are the main hidden disaster factors in the Jurassic coalfields in the border area of Inner Mongolia and Shaanxi. For the deeply buried Jurassic coalfields in the border area of Inner Mongolia and Shaanxi, the buried depth is generally greater than 500 m, and during the mining period, the exposure of poor sealing borehole may communicate with the strong water-rich aquifer in the upper part of the coal seam, making it a direct water-filled water source for the coal seam, thus affecting the safe production of coal mines. In order to study the water output characteristics of poorly sealed boreholes in deep-buried Jurassic coal seams in the border area of Inner Mongolia and Shaanxi, a “trinity” accurate judgment method for underground water inrush sources was established, and the water inrush characteristics and water chemistry characteristics of boreholes were analyzed by comparing with typical drainage boreholes and water quality test data, and the hydraulic connection between poor sealing borehole and overlying aquifers on coal seams was analyzed by using a hierarchical cluster analysis model. Combined with the on-site test of the plugging effect of the poorly sealing borehole, the disaster-causing mechanism of the poorly sealing borehole was analyzed. The results show that there are great differences in the water quality characteristics of the Cretaceous pore-fissure aquifer system and the Jurassic fissured aquifer system in Inner Mongolia-Shaanxi border area, and the characteristic ion HCO3− of the Cretaceous pore-fissure aquifer system is HCO3−Na type water, which accounts for more than 45% of the anion. The water sample of the Jurassic fractured aquifer system is of the SO4−Na type, and its characteristic ion SO42− accounts for more than 40% of the anion. At the same time, the water inrush characteristics of the downhole water inrush point are compared with the typical drainage water borehole to quickly identify the water-filling horizon, and the corresponding plugging effect test method is proposed, which can provide a certain reference for the emergency treatment of water inrush in the subsequent underground borehole with poor closure and the exploration of the plugging effect of the borehole.

       

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