曹村煤矿十采区水文地质条件与突水危险性分析
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The risk for coal field water-inrush and the hydrogeology conditions in the 10th mining area of Caocun coal mine
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    摘要:

    通过对曹村煤矿十采区综合研究分析,认为K8砂岩、第四系空隙含水层是2#煤开采时的主要充水含水层;十采区下组煤主要受到顶板K2灰岩含水层和底板奥灰水突水的影响;通过对奥灰水突水危险性的定量计算,并对突水危险性进行分区,在Ⅰ区突水危险性较小,应重点加强对Ⅱ、Ⅲ区探测和监测工作,对局部富水地段进行注浆加固,以增加隔水底板的有效厚度和强度,达到防治突水的目的。

    Abstract:

    Based on the comprehensive analysis of the tenth Coal mining area in Cancun coal mine,the K8 sandstone and the pore-fissure aquifer of Quaternary are the rminly water filled aquifers for 2 coal. The lower seams of the tenth mining district aremainly affected by the K2 sandstone from apicalplate and the Ordovician limestone water-bursting from soleplate.Through the quantitative calculation of the Ordovician limestone water-inrush and the analysis of the risk of water-bursting, it shows that the risk of water- bursting in the I area is small.And it should focus on a lower risk of Ⅱ,Ⅲ area for detecting and moni- toning. The partly slip-casting in the water - rich area could increase the grouting reinforcement of water bottom thickness and strength for the purpose of controlling the water.

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王玉海,李曦滨,李茸,王宝琛.曹村煤矿十采区水文地质条件与突水危险性分析[J].河北工程大学自然版,2010,27(3):66-68

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  • 收稿日期:2010-06-30
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  • 在线发布日期: 2015-01-12
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