霍州矿区奥灰含水层水文地质条件特征分析研究  

Hydrogeological Condition Characteristics of Ordovician Aquifer in Huozhou Mining Area

作　　者：杨小刚 YANG Xiaogang(Xi ＇ an Research Institute, China Coal Technology ＆ Engineering Group, Xi＇ an 710054, China)

机构地区：[1]中煤科工集团西安研究院有限公司,陕西西安710054

出　　处：《山西煤炭》2017年第2期28-31,共4页Shanxi Coal

摘　　要：为了解决霍州矿区受奥灰突水威胁的煤炭储量所占比重达高,且矿区内矿井开拓、掘进和开采过程常发生100m^3/h以上的奥灰突水事故的问题,对奥灰含水层水文地质条件进行了分析研究。研究结果表明:霍州矿区奥灰含水层补给充沛,径流条件较好,富水性弱到极强,且具有明显的块段差异性。根据奥灰富水性的特点,提出了分块段因地制宜的实施防治水技术方法,保证了矿井安全带压的开采。A high proportion of coal reserves is threatened by water inrush of Ordovician aquifer in Huozhou mine,with more than 100m^3/h Ordovician water bursting in the process of tunneling,driving and mining.To solve the water inrush,we studied the hydrogeological condition of the Ordovician aquifer in the area.The results show that Ordovician aquifer is characteristic of rich water supply and good runoff condition.In addition,water yield property varies from poorness to richness with significant block difference.For the different block sections,corresponding water control measures were proposed to guarantee the safe mining above aquifer.

关 键 词：奥灰 含水层 特征 

分 类 号：TD741[矿业工程—矿井通风与安全]