环境化学

雅鲁藏布江径流水文规律及水体同位素组成

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  • 1. 成都理工大学地球化学系,成都610059;
    2. 中国科学院成都山地灾害与环境研究所,成都610041
高志友(1972-), 女, 四川成都人, 博士, 主要从事同位素地球化学研究。E-mail: cdannie@163.com

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

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  • 1. Department of Geochemistry, Chengdu University of Technology, Chengdu 610059, China;
    2. Institute of Mountain Hazards and Environment, CAS, Chengdu 610041, China

Received date: 2007-07-10

  Revised date: 2007-08-22

  Online published: 2007-09-25

Supported by

National 973 Program of China, No.2005CB422005

摘要

由雅鲁藏布江各站径流量数据和水体的同位素数据,分析了径流的时空分布特点以及大气降水的同位素效应。该区干流流域年平均径流量分布呈从下游到上游逐渐减少的趋势, 且地表径流的年内分配主要集中在夏、秋两季(6-10 月)。流域内大部分雨水和河水样品的同位素组成均落在全球大气降水线δD = 8δ18O +10 的右上方,显示出强烈蒸发的特征。水体同 位素组成区域大陆性效应和高度效应明显,这种分布特征与来自孟加拉湾、怒江方向降水云汽的运移以及青藏高原的地形、气候条件有关。

本文引用格式

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

Abstract

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.

参考文献


[1] Yin Guan, Liu Tianchou. Formed mechanism and water source composition on the runoff of the Nianchu River system in the Yaluzangbu River basin, Xizang (Tibet). Journal of Chengdu University of Technology, 1997, 24(3), 81-88.
[尹 观, 刘天仇. 西藏年楚河径流形成机制及水源组成. 成都理工学院学报, 1997, 24(3): 81-88.]

[2] Ning Aifeng, Yin Guan, Liu Tianchou. Characteristics of isotope distribution of atmospheric precipitation in the Lasa River area. Journal of Mineralogy and Petrology, 2000, 20(3): 95-99.
[宁爱凤, 尹观, 刘天仇. 拉萨河地区的大气降水 同位素分布特征. 矿物岩石, 2000, 20(3): 95-99.]

[3] Liu Tianchou, Hydrological characteristics of Yarlung Zangbo River. Acta Geographica Sinica, 1999, 54 (supple.), 157-163.
[刘天仇. 雅鲁藏布江水文特征. 地理学报, 1999, 54(增刊): 157-163.]

[4] Gao Dengyi, Zou Han, Wang Wei. Influence of water vapor pass along the Yalungzangbo River on precipitation. Journal of Mountain Research, 1985, 3(4): 239-249.
[高登义, 邹捍, 王维. 雅鲁藏布江水汽通道对降水的影响. 山地研究, 1985, 3(4): 239-249.]

[5] Lin Zhenyao, Wu Xiangding. A preliminary analysis about the tracks of moisture transporation on the Qinghai-Xizang Plateau. Geographical Research, 1990, 9(3): 33-40.
[林振耀, 吴祥定. 青藏高原水汽输送路径的探讨. 地理研究, 1990, 9(3): 33-40.]

[6] Crig H. Isotopic variation in meteoric waters. Science, 1961, 133: 1702. 133,1690-1702

[7] Wang Hengchun. General Theory of Isotope Hydrogeology. Beijing: Geology Press, 1991. 45-56.
[王恒纯. 同位素水文 地质概论. 北京: 地质出版社, 1991. 46-56.]

[8] Tian Lide, Yao Tandong et al. Characteristics of 18O in summer precipitation at Lhasa. Journal of Glaciology and Geocryology, 1997, 19(4): 299-300.
[田立德, 姚檀栋等. 拉萨夏季降水中氧稳定同位素分布特征. 冰川冻土, 1997, 19(4): 299-300.]

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