ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
利用包气带环境示踪剂评估张掖盆地降水入渗速率
  
关键词:Zhangye basin  unsaturated zone  environmental tracers  rainfall infiltration
基金项目:国家自然科学基金项目(编号: 40602032); 国土资源部百名优秀青年科技人才计划(编号: B07002)
作者单位E-mail
聂振龙 中国地质科学院水文地质环境地质研究所 nzlngj@163.com 
连英立 中国地质科学院水文地质环境地质研究所  
段宝谦 中国地质科学院水文地质环境地质研究所  
申建梅 中国地质科学院水文地质环境地质研究所  
王金哲 中国地质科学院水文地质环境地质研究所  
严明疆 中国地质科学院水文地质环境地质研究所  
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摘要:
Application of Unsaturated Zone Environmental Tracers to the Estimation of Rainfall Infiltrating Rate in the Zhangye Basin, Northwestern China
      The rainfall infiltrating rate is a key parameter in groundwater resource assessment and groundwater protection. During the groundwater resource assessment in middle basins of the Hexi corridor in the past decades, however, the rainfall infiltration was not considered where the buried depth of the water table was more than 5 m. In the present work, the rainfall infiltration rates were estimated using chemical and isotopic information in the unsaturated zone at two sites of the Zhangye basin, which lies in the middle reaches of the Heihe River. One site is located in sand dunes in the middle of the basin and the other site is located in a wasteland area with the buried depth of the groundwater table being 8.6m. The result of chloride mass balance (CMB) indicates that there exists rainfall infiltration in Zhangye basin where the buried depth of the water table is more than 5 m. In the sand dune area, the rainfall infiltrating rate is 13.3~14.4 mm/a with the buried depth of the water table being 6.3 m, and the infiltration coefficient is about 0.10~0.11%. In the wasteland area, the rainfall infiltrating rate is 16.8~18.4 mm/a with the buried depth of the water table being 8.6m, and the infiltration coefficient is about 0.13~0.14.
NIE Zhen-long,LIAN Ying-li,DUAN Bao-qian,SHEN Jian-mei,WANG Jin-zhe,YAN Ming-jiang.2011.Application of Unsaturated Zone Environmental Tracers to the Estimation of Rainfall Infiltrating Rate in the Zhangye Basin, Northwestern China[J].Acta Geoscientica Sinica,32(1):117-122.
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