淮南矿区浅部含水层K与水化学成分的相关性  

RESEARCHES ON THE INTERRELATION BETWEEN THE PERMEABILITY OF THE SHALLOW AQUIFERS AND THE CHEMICAL COMPONENTS OF THE GROUNDWATER IN HUAINAN COAL MINE AREA

作　　者：桂和荣[1] 陈兆炎[1] 随成立 钱谋始 邹海[3] 

机构地区：[1]淮南矿业学院,232001 [2]淮南市环保局,232000 [3]淮南矿务局,232000

出　　处：《煤田地质与勘探》1993年第5期40-44,共5页Coal Geology & Exploration

摘　　要：利用单孔抽水及水位恢复试验资料,求出了矿区多处浅部松散含水层渗透系数 K 值,分析研究了 K 值与各取样点浅层地下水化学成分之间的相关性及其形成机理,为矿区防治水及浅层地下水资源的开发利用提供了依据。Using the materials obtained from the pumping tests and the water level recentralizing tests,thecoefficients of permeability of the shallow loose aquifers of many places in Huainan Coal Mine area are calculated.The interrelation between the coefficient of permeability and the chemical components of the shallowgroundwater is studied,and the whys of the interrelation are explained.So it becomes able to control and tomake use of the groundwater in the coal mine area.

关 键 词：含水层 化学成分 煤田 地下水 

分 类 号：P641.461[天文地球—地质矿产勘探]