寺河矿井奥灰水滞流区水文地质边界的划分  

GEO-HYDROLOGY BOUNDARY PARTITIONING OF ORDOVICIAN SYSTEM LIMESTONE WATER RETENTION IN SHIHE COAL MINE

作　　者：李民[1] 

机构地区：[1]晋城煤业集团环保处,山西晋城048006

出　　处：《洁净煤技术》2004年第4期70-71,20,共3页Clean Coal Technology

摘　　要：晋城煤业集团寺河矿井奥陶系中统上马家沟组含水层存在着水平分区和垂直分层现象,分析奥陶系含水层分区、分层的范围及规律,确定奥灰水滞流区水文地质边界的范围,对解决矿井生产及生活用水具有重要的指导意义。The water bearing layer of upper Majiagou formation, middle system, Ordovician in Shihe Coal Mine exist horizontal partition and vertical stratification phenomena. To analyze the range and rules of water bearing layer partition and stratification and definition the geo-hydrology boundary range of retention region are very important for to solve water utilization in coal production and life.

关 键 词：滞流区 边界 划分 

分 类 号：X523[环境科学与工程—环境工程]