干旱区研究2011，Vol.28Issue(3)：427-432,6.
渭河陕西"二华"段浅层地下水水化学特征
Hydrochemical Properties of Shallow Groundwater along the Weihe River in Huaxian County and Huayin City, Shaanxi Province
摘要
Abstract
The Weihe River flows through Huayin City and Huaxian County. According to the analyzed results of shallow groundwater samples collected in Huayin City and Huaxian County, in this paper the spatial hydrochemical properties and their evolution of groundwater are studied systemically. The results show that shallow groundwater in the study area is mainly recharged by groundwater from the Qinling Piedmont, and it in the areas along the river-banks relies mainly on the lateral recharge of the Weihe River. The hydrochemistry type in the areas of groundwater recharge, runoff and discharge changes from HCO3 · SO4 - Ca · Mg to S04 · HCO3 - Na · Ca and then to SO4 · Cl - Na; the salinity and hardness of groundwater increase gradually and reach to their maximum values in the funnel-shaped zone of groundwater; Cl- , Mg + and Na+ are gradually accumulated, and groundwater quality trends to salinization. The study results can provide the references for understanding the effect of the Weihe River on ground-water quality in the areas along the river and for rationally utilizing groundwater resources in the study area.关键词
"二华"地区/浅层地下水/水化学成分/空间变化/陕西/渭河Key words
Huayin City/ Huaxian County/ shallow groundwater/ groundwater chemical composition/ spatial variation/ Shaanxi Province/ Weihe River分类
天文与地球科学引用本文复制引用
赖坤容,姜军,刘秀花,周维博..渭河陕西"二华"段浅层地下水水化学特征[J].干旱区研究,2011,28(3):427-432,6.基金项目
国家外专局、教育部项目(B08039) （B08039）
