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作 者:曹小虎
机构地区:[1]山西省运城市水文水资源勘测分局,山西运城044000
出 处:《地下水》2009年第4期36-38,116,共4页Ground water
摘 要:地下水的化学特征是围岩矿物和水流之间内在关系所形成的结果,决定于地下水运动时接触的围岩成分,水文地质条件和氧化还原环境等。地下水的水化学成份及不同离子含量的多少,与其赋存条件有着十分密切的关系。通过对矿区主要含水层水样常规水质分析,研究矿区地下水的水化学成份及其背景含量特征,研究和分析矿区不同地下水含水层水化学特征,从而揭示矿区水文地质条件。The chemical characters of groundwater is the result of intrinsic interest in the wall rock mineral and the water current and is decided by contacted components of the wall rock, hydro--geological condition and redox environment during groundwater movement. The chemical factors and content of different ions are very similar to the condition of groundwater. The article is based on analysis of water quality of water sample routine in the main aquifer in the mine field, studies chemical factors and characters of background content of groundwater, studies and analyzes the chemical characters of aquifer of different groundwater and announces the hydrogeology condition this area.
分 类 号:P641.12[天文地球—地质矿产勘探]
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