ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
北京永定河流域地下水氢氧同位素研究及环境意义
  
关键词:isotopic geochemistry  groundwater  water quality  Yongding River
基金项目:中国地质调查局国土资源大调查项目(编号:200610400002)
作者单位E-mail
刘锋 中国地质科学院矿产资源研究所矿床成因和资源评价重点实验室,北京100037
中国地质科学院同位素地质重点实验室,北京100037 
lf128743@163.com 
李延河 中国地质科学院矿产资源研究所矿床成因和资源评价重点实验室,北京100037
中国地质科学院同位素地质重点实验室,北京100037 
 
林建 北京市地质工程勘察院,北京100037  
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摘要:
A Hydrogen and Oxygen Isotope Study of Groundwater in the Yongding River Drainage of Beijing and Its Environmental Significance
      On the basis of isotopic geochemistry, the authors studied the status and the supply characteristics of groundwater in the Yongding River drainage of Beijing. Some samples of groundwater were systematically collected from different areas and different depths and then analyzed for their contents of deuterium, oxygen and tritium. Based on a study of the analytical results, the authors have reached the conclusion that the groundwater in the superficial aquifer is mainly made up of young groundwater. In the past ten years, groundwater has been supplied by vertically filtering atmospheric precipitation, and groundwater from the middle to the deep aquifer is generally combined with the upper groundwater, and the proportion of the young groundwater is steadily increasing. In addition, there exists the mixture of some young groundwater in some places, though the groundwater in the deep aquifer remains mainly made up of groundwater older than 50 years. The groundwater condition in this area suggests that there exists the phenomenon that the superficial groundwater has penetrated into the deep aquifer. This could result in the deterioration of the quality of the groundwater in the deep aquifer. It can thus be concluded that the status of the groundwater resource in this area is not satisfactory due to the human unreasonable exploitation.
LIU Feng,LI Yan-he,LIN Jian.2008.A Hydrogen and Oxygen Isotope Study of Groundwater in the Yongding River Drainage of Beijing and Its Environmental Significance[J].Acta Geoscientica Sinica,29(2):161-166.
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