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基于钻孔水文监测信息的顶板水害分析

Analysis of Roof Water Inrush Hazard Based on Borehole HydrologicalMonitoring Information

  • 摘要: 为掌握补连塔煤矿31401工作面顶板突水致灾机理,通过施工井下放水孔、水文观测孔及地面钻孔,分别监测各钻孔的水流量、水位、水位—流量耦合信息,并对上述信息进行挖掘,用于分析顶板渗透性、覆岩变形规律及其与含水层水位变化关系、裂采比与垮采比。分析结果表明:顶板含水层原生裂隙不发育,采前渗透性弱;覆岩破断变形过程经历了张开、闭合过程,并且砂质泥岩遇水泥化、膨胀,填堵导水通道,同时,覆岩变形与含水层水位下降存在必然联系,水位下降滞后周期来压初始时间;采前原生裂隙不发育,采后裂采比为31.93~34.98,垮采比为3.88~4.48。确定该工作面多次出现的周期性顶板突水通道为回采后的导裂带。

     

    Abstract: In order to master the roof water disaster-causing mechanism in 31401 working face in Bulianta Mine, underground drain holes, hydrological observation holes and surface holes were drilled, the water flow, water level and the coupling information of the water level-flow of each hole were monitored, these information were then mined and used to analyze the roof permeability, the overburden deformation law and its relation with the water level change of the aquifer, the ratio of water conducting crack to the mining height and the ratio of caving zone to the mining height. The analysis results showed that the primary cracks in the roof aquifer not developed and had weak permeability before mining; the broken deformation of the overburden starta experienced the opening and closing process, the sandy mudstone cemented and expanded while meeting water, and blocked up the water channel, at the same time, there was a necessary relation between the deformation of the overburden strata and the water level drop of the aquifer, the water level drop laged behind the initial time of the periodical weighting; the primary cracks before mining not developed, the ratio of water conducting crack to the mining height was 31.93 to 34.98 after mining, and the ratio of the caving zone to the mining height was 3.88 to 4.48. It is determined that the periodic roof water inrush channel which appeared on the face was the fractured zone after mining.

     

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