留庄煤矿12102工作面出水因素分析  

Analysis of factors contributing to water inrush on Face 12102 in Liuzhuang Mine

作　　者：郑丽萍[1] 杨兰和[1] 齐跃明[1] 

机构地区：[1]中国矿业大学资源与地球科学学院,江苏省徐州市221116

出　　处：《中国煤炭》2010年第11期91-94,共4页China Coal

基　　金：国家自然科学青年基金;项目编号41002087--采动条件下矿区充水含水层地下水动态演化及突水机理研究

摘　　要：从突水水源和导水通道两方面分析了留庄煤矿12102工作面特大突水灾害的成因,结果表明:12102工作面直接充水水源为第三层灰岩含水层静储量水,补给水源是侏罗系红层水。导水通道为断层活化引起的冒裂带沿断层向上发育。断层活化作用与工作面内断层走向和工作面推进方向有关,12102工作面推进方向与断层走向近于垂直,与断层倾向相反,当顶板上方有含水层时容易发生断层活化充水。Causes of severe water inrush on Face 12102in Liuzhuang Mine are analyzed,which relate to the source and passage of the inrush.The analysis indicates that the static water in the third limestone aquifer of the Carboniferous system is the direct source of water in Face 12102,with additional water from the Jurassic red strata.Fault activation provides water passa-ges,where the fractured zone develops upwards along the fault.Fault activation is related to the strike of the fault in the face and the direction of face advance.The direction of Face 12102ad-vance is approximately perpendicular to the fault strike and opposite to the fault dip.When an aq-uifer exists above the roof,the fault is apt to being filled with water as a result of activation.

关 键 词：工作面突水 突水水源 导水通道 留庄煤矿 

分 类 号：TD742[矿业工程—矿井通风与安全]