榆神府矿区烧变岩水害防治技术及典型案例

Prevention and control technologies for water hazards of burnt rock in Yushenfu mining area and typical cases

  • 摘要:
    背景 榆神府矿区烧变岩分布范围广,沿河流和沟谷发育,孔裂隙发育,富水性弱—极强,差异极大,威胁同层煤或下伏煤巷道掘进、工作面回采。
    方法 为有效防控烧变岩水害、减少烧变岩水患威胁,采用野外调查、统计分析、探测分析、现场试验、示范应用和监测分析等方法,分析榆神府矿区烧变岩分布特征,研究烧变岩水害形成机理及特点,研发烧变岩水害防治关键技术,并开展了示范应用和效果评价。
    结果和结论 (1)榆神府矿区烧变岩主要沿秃尾河、窟野河、乌兰木伦河及其支沟两侧发育,分布面积约787 km2,影响数十个煤矿掘进和回采;垂向上分为煤灰、烧熔岩、烧烤岩和烘烤岩4类,水平向分为露头充分烧变区、中部烧变混杂区和内侧烧变边界区3区。(2)烧变岩空洞、裂隙和孔隙发育,内部的通道连通性好,渗流通道畅通,接受大气降水、第四系沙层孔隙潜水和风化基岩水补给,形成掘进扰动裂隙侧向透水型、采动裂隙顶部透水型和采动裂隙侧向透水型等3种烧变岩水害类型。(3)基于烧变岩边界连续探查的煤柱隔水、地面钻孔注浆帷幕分隔截流和地面二维组合式自流直排等烧变岩水害防治关键技术可有效防治烧变岩水害,在陕西南梁、柠条塔、张家峁等煤矿取得良好应用效果,消除了烧变岩水害威胁,解放大量煤炭资源,保护和利用了烧变岩水资源。

     

    Abstract:
    Background The burnt rock formations in the Yushenfu mining area are widely distributed, predominantly developing along rivers and gullies. These formations are characterized by well-developed pores and fractures, with water-bearing capacity ranging from weak to extremely strong, exhibiting significant heterogeneity. They pose serious threats to roadway excavation and longwall mining in both the same coal seam and underlying seams.
    Methods To effectively prevent and control water hazards associated with burnt rock formations and mitigate related risks, a combination of methods—including field investigation, statistical analysis, chronological testing, exploration and analysis, in-situ experiments, demonstration applications, and monitoring analysis—was employed.
    Results and Conclusions  The study analyzes the distribution characteristics of burnt rock in the Yushenfu Mining Area, investigates the micro- and meso-scale structural features, as well as the water-filling characteristics and hazard formation mechanisms, and develops key technologies for water hazard prevention and control. Demonstration applications and performance evaluations were also conducted. The results indicate that burnt rock formations in the Northern Shaanxi coal base are mainly distributed along both sides of the Tuwei River, Kuye River, Wulanmulun River, and their tributary gullies, covering an area of approximately 787 km and affecting roadway excavation and mining operations in dozens of coal mines. Vertically, the formations can be classified into four types: coal ash, fused rock, sintered rock, and baked rock; horizontally, they can be divided into three zones: the outer fully burnt zone, the central mixed burnt zone, and the inner burnt boundary zone. Burnt rock exhibits extensive development of cavities, fractures, and pores. The internal flow channels are well connected, forming effective seepage pathways. These formations receive recharge from atmospheric precipitation, pore water in Quaternary sandy layers, and weathered bedrock water, leading to three types of water hazards: lateral seepage through excavation-induced fractures, vertical seepage from the roof via mining-induced fractures, and lateral seepage through mining-induced fractures. Based on continuous boundary detection of burnt rock, key prevention and control technologies have been developed, including coal pillar water isolation, surface borehole grouting curtain for partitioning and interception, and surface two-dimensional combined gravity-driven direct drainage. These technologies have been successfully applied in multiple coal mines, such as Nanliang, Ningtiaota, and Zhangjiamao, achieving significant results. It has effectively eliminated the threat of burnt rock water hazards, liberated substantial coal resources, and enabled the protection and utilization of water resources within burnt rock formations.

     

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