Tracing the major source area of the mountainous runoff generation of the Heihe River in northwest China using stable isotope technique
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  • 作者:NingLian Wang (1)
    ShiBiao Zhang (1)
    JianQiao He (1)
    JianChen Pu (1)
    XiaoBo Wu (1)
    Xi Jiang (1)
  • 关键词:stable isotope tracing technique ; Heihe River ; mountainous runoff ; Qilian Mountains
  • 刊名:Chinese Science Bulletin
  • 出版年:2009
  • 出版时间:August 2009
  • 年:2009
  • 卷:54
  • 期:16
  • 页码:2751-2757
  • 全文大小:537KB
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  • 作者单位:NingLian Wang (1)
    ShiBiao Zhang (1)
    JianQiao He (1)
    JianChen Pu (1)
    XiaoBo Wu (1)
    Xi Jiang (1)

    1. State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, 730000, China
  • ISSN:1861-9541
文摘
Based on the data of δ18O in precipitation during the period of April 2006 through May 2007 in the upper catchment of the main stream of the Heihe River in the Qilian Mountains, we found that there existed an evident altitude effect on δ18O in precipitation, and the δ18O-altitude gradient was ?.18%/100 m. When δ18O in river water at the outlet of the mountainous drainage area of the main stream of the Heihe River was combined with the δ18O-altitude relation, it was realized that the mountainous runoff was generated mostly at high altitudes. Using two component models, we revealed that 80.2% of the annual total mountainous runoff amount was generated at the alpine permafrost-snow-ice zone with an altitude of above 3600 m a.s.l.

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