雅鲁藏布江径流水文规律及水体同位素组成
收稿日期: 2007-07-10
修回日期: 2007-08-22
网络出版日期: 2007-09-25
基金资助
国家“973”项目资助(2005CB422005)
Hydrological Rule and Isotopic Composition of Water Bodies in Yar lung Zangbo River
Received date: 2007-07-10
Revised date: 2007-08-22
Online published: 2007-09-25
Supported by
National 973 Program of China, No.2005CB422005
高志友, 王小丹, 尹观 . 雅鲁藏布江径流水文规律及水体同位素组成[J]. 地理学报, 2007 , 62(9) : 1002 -1007 . DOI: 10.11821/xb200709011
Based on data of runoff and water isotopic compositions in the Yarlung Zangbo River, this paper mainly analyzes the spatio-temporal distribution of runoff and isotopic effect of precipitation in this area. In the trunk-stream drainage area, the average annual runoff presents a trend of gradual decrease from lower reaches to upper reaches, and the intra-annual surface runoff mostly concentrates in summer and autumn (June to October). The isotopic compositons of most water samples fall on the top right of the global precipitation line, δD = 8 δ18O+10, showing that they have experienced intensive evaporation. With obvious region-continental effect and altitude effect, the distribution of water isotopic compositions is related to the movement of precipitation clouds from Bay of Bengal and Nujiang River and is affected by the topographic and climatic conditions of the Qinghai-Tibet Plateau.
Key words: runoff; hydrological rule; isotopic composition; Yarlung Zangbo River; Tibet
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