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Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China
Li, XQ (Li, Xiangquan); Zhang, L (Zhang, Li); Hou, XW (Hou, Xinwei)
刊名HYDROGEOLOGY JOURNAL
2008
卷号16期号:2页码:335-348
关键词arid regions groundwater flow hydrochemistry stable isotopes China
ISSN号1431-2174
英文摘要Hydrogeochemistry and environmental isotope data were utilized to understand origin, geochemical evolution, hydraulic interconnection, and renewability of groundwater in Qingshuihe Basin, northwestern China. There are four types of groundwater (1) shallow groundwater in the mountain front pluvial fans, originating from recent recharge by precipitation, (2) deep paleo-groundwater of the lower alluvial plains, which was formed long ago, (3) shallow groundwater in the lower alluvial plains, which has undergone evaporation during the recharge process, and (4) mixed groundwater (shallow and deep groundwater in the plain). The main water types are Na-HCO3, which dominates type (1), and Na-SO4, which dominates types (2) and (3). Geochemical evolution in the upper pluvial fans is mainly the result of CO2 gas dissolution, silicates weathering and cation exchange; in the lower alluvial plains, it is related to mineral dissolution. The evaporative enrichment only produces significant salinity increases in the shallow groundwater of the lower alluvial plains. Shallow groundwater age in the upper plain is 10 years or so, showing a strong renewability. Deep groundwater ages in the lower plain are more than 200 years, showing poor renewability. In the exploitation areas, the renewability of groundwater evidently increases and the circulation period is 70-100 years.
学科主题环境地质学
WOS关键词GEOCHEMICAL EVOLUTION ; AQUIFER ; WATER
WOS研究方向Geology ; Water Resources
语种英语
出版者SPRINGER
WOS记录号WOS:000254184800011
内容类型期刊论文
源URL[http://119.78.100.197/handle/2HKVOGP0/38623]  
专题中国地质调查局
作者单位Chinese Acad Geol Sci, Inst Hydrogeol & Environm Geol, Shijiazhuang 050061, Peoples R China
推荐引用方式
GB/T 7714
Li, XQ ,Zhang, L ,Hou, XW . Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China[J]. HYDROGEOLOGY JOURNAL,2008,16(2):335-348.
APA Li, XQ ,Zhang, L ,&Hou, XW .(2008).Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China.HYDROGEOLOGY JOURNAL,16(2),335-348.
MLA Li, XQ ,et al."Use of hydrogeochemistry and environmental isotopes for evaluation of groundwater in Qingshuihe Basin, northwestern China".HYDROGEOLOGY JOURNAL 16.2(2008):335-348.
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