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煤层顶板巨厚砂砾岩含水层可疏放性评价

Drainage Feasibility Evaluation of Thick Glutenite Aquifer on Coal Seam Roof

  • 摘要: 为了论证煤层顶板巨厚砂砾岩含水层疏放的可行性,结合含水层的水文地质条件和井下涌水量数据,分析了含水层水位对井下集中和持续涌水的响应,利用放水试验对含水层的可疏放性进行了研究。结果表明:巨厚砂砾岩含水层渗透性较好,具有充沛的补给水源,无论是井下集中涌水还是持续涌水,含水层水位均大幅降低,井下出水点涌水量也显著减小并趋于稳定,可以通过大流量长时间疏放降低含水层水位和消耗静态储存量,在工作面回采前对含水层进行顶板水疏放具有可行性。

     

    Abstract: In order to demonstrate the drainage feasibility of thick glutenite aquifer on coal seam roof, combined with hydrogeological conditions of aquifer and data of downhole water inflow.The response of aquifer water level to concentrated and continuous upwelling of water underground was analyzed, and drainage feasibility of aquifer was studied based on dewatering test. The result showed that the thick glutenite aquifer has good permeability and abundant water supply. The aquifer water level is reduced greatly whether it is a concentrated upwelling or a continuous upwelling, and water inrush at downhole outlet points is significantly reduced and tends to be stable. High flow drainage for a long time can be used to reduce aquifer water level and consume static storage of groundwater. It is feasible to drainage groundwater of aquifer on coal seam roof before working face mining.

     

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