高河井田井下断层附近地下水突水数值研究

    Numerical Study of Groundwater Surge near Downhole Fault in Gaoha Well Field

    • 摘要: 井田中的渗透性断层会导致间歇性生产或下伏含水层的地下水突出问题,为判断井下断层附近地下水运移规律,采用基于有限元法的RFPA数值计算程序,对煤矿断层带地下水突出进行了数值研究。数值模拟得到的损伤演化规律表明,底板岩层可划分为采动裂隙带、完整带和断层活化带3个区域,其中完整带是抵抗地下水突出的关键部位,直接决定了隔水岩层的有效厚度。断层的几何形态,也对地下水突出有着重要影响。最后,基于地质、水文地质调查和数值计算结果,对工程实例进行了地下水突出机理分析,对断层诱发地下水突出机理研究和防治实践具有重要的指导意义。

       

      Abstract: Permeable faults in the well field can lead to intermittent production or groundwater protrusion problems in the underlying aquifer. In order to determine the groundwater transport law near the downhole faults, the groundwater protrusion in the fault zone of the coal mine was numerically investigated by using the numerical calculation program of RFPA based on the finite element method. The damage evolution law obtained from the numerical simulation shows that the basement rock layer can be divided into three zones: mining fissure zone, intact zone and fault activation zone, among which the intact zone is the key part to resist groundwater protrusion, which directly determines the effective thickness of the water-insulating rock layer. The geometry of faults also has an important influence on groundwater protrusion. Finally, based on the results of geological and hydrogeological investigations and numerical calculations, the mechanism of groundwater protrusion is analyzed in the project example, which is of great significance in guiding the research on the mechanism of fault-induced groundwater protrusion and the prevention and control practice.

       

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