神府矿区上覆采空区积水突水危险性分析

    Evaluation of up-goaf water inrush possibility in Shenfu mining area

    • 摘要: 在多煤层区采煤,上部煤层开采后采空区形成一定的积水,形成了上覆采空区积水,对下部煤层的安全开采会形成威胁,本文分析了神府矿区南梁煤矿2-2煤层开采前后水文地质条件变化,调查计算了采空区积水量,编绘了3-1煤层与2-2煤层之间隔水岩组厚度等值线,预计3-1煤导水裂隙带发育高度25.80~70.17m,而3-1煤与2-2煤间隔24.14~40.37m,3-1煤开采发育的导水裂隙带将到达2-2煤采空区,采空区积水将成为3-1煤开采的直接突水水源。

       

      Abstract: The water collected from upper coal mined area will pose a threat to lower coal mining in the multiple seams area.The paper analyzes the changes of hydrological conditions after the coal seam 2-2 is mined in Nanliang coal mine and calculates the goaf water quantity.We find aquiclude between coal seam 2-2 and 3-1 is changed from 24.14 mto 40.37 m,it is less than the water suture zone's height of coal seam 3-1(25.80~70.17m),therefore,goaf water of coal seam 2-2 is the direct source of water inrush for coal seam 3-1.

       

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