拉萨河流域地表径流氢氧同位素空间分布特征

余婷婷; 甘义群; 周爱国; 刘存富; 刘运德; 李小倩; 蔡鹤生

doi:10.3799/dqkx.2010.101

Volume 35 Issue 5

Sep. 2010

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2010 > 35(5): 873-878

YU Ting-ting, GAN Yi-qun, ZHOU Ai-guo, LIU Cun-fu, LIU Yun-de, LI Xiao-qian, CAI He-sheng, 2010. Characteristics of Oxygen and Hydrogen Isotope Distribution of Surface Runoff in the Lhasa River Basin. Earth Science, 35(5): 873-878. doi: 10.3799/dqkx.2010.101

Citation:

YU Ting-ting, GAN Yi-qun, ZHOU Ai-guo, LIU Cun-fu, LIU Yun-de, LI Xiao-qian, CAI He-sheng, 2010. Characteristics of Oxygen and Hydrogen Isotope Distribution of Surface Runoff in the Lhasa River Basin. Earth Science, 35(5): 873-878. doi: 10.3799/dqkx.2010.101

Citation:

YU Ting-ting, GAN Yi-qun, ZHOU Ai-guo, LIU Cun-fu, LIU Yun-de, LI Xiao-qian, CAI He-sheng, 2010. Characteristics of Oxygen and Hydrogen Isotope Distribution of Surface Runoff in the Lhasa River Basin. Earth Science, 35(5): 873-878. doi: 10.3799/dqkx.2010.101

PDF( 351 KB)

Characteristics of Oxygen and Hydrogen Isotope Distribution of Surface Runoff in the Lhasa River Basin

doi: 10.3799/dqkx.2010.101

YU Ting-ting^{1, 2},
GAN Yi-qun^{1, 2
,
,},
ZHOU Ai-guo^{1, 2},
LIU Cun-fu^{1, 2},
LIU Yun-de^{1, 2},
LI Xiao-qian^{1, 2},
CAI He-sheng^{1, 2}

1.
School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China

Received Date: 2010-05-31
Publish Date: 2010-09-01

Abstract

Abstract

The variation characteristics of oxygen and hydrogen isotopes in surface runoff of the Lhasa River basin was studied based on the observations of δ¹⁸O and δD in river water and related meteorological and hydrological data in 2008. The results indicate that: (1) precipitation is the main recharge source and that the Lhasa River has experienced strong evaporation; (2) positive d values indicate the snow melting water recharge; (3) during the Tibetan plateau summer monsoon period, the lapse rate of δ¹⁸O in river water is approximately 0.16‰·(100 m)^-1 due to the "altitude effect"; (4) in large-scale circulation, the basin water presents a significant continental effect. This study demonstrates that it is possible to trace the hydrological cycle with oxygen isotope and deuterium distribution in land runoff in the high altitude areas and to provide the stable isotopic evidence of the ancient latitude variation.
- deuterium excess parameter (d value),
- Lhasa River basin,
- surface runoff,
- snow melting water,
- oxygen isotope (δ¹⁸O),
- hydrogen isotope (δD)

FullText(HTML)

References(23)

References

Cameron, E.M., Hall, G.E.M., Veizer, J., et al., 1995. Isotopic and elemental hydrogeochemistry of a major river system: Fraser River, British Columbia, Canada. Chemical Geology, 122(1-4): 149-169. doi: 10.1016/0009-2541(95)00007-9

Clark, I.D., Fritz, P., 1997. Environmental isotopes in hydrology. Lewis, Boca Raton, Florida.

Craig, H., 1961. Istopic variations in meteoric waters. Science, 133: 1702-1703. doi: 10.1126/science.133.3465.1702

Dansgaard, W., 1964. Stable isotopes in precipitation. Tellus, 16: 436-468. doi: 10.1111/j.2153-3490.1964.tb00181

Gat, J.R., Carmi, I., 1970. Evolution of the isotopic composition of atmospheric waters in the Mediterranean Sea area. Journal of Geophysical Research, 75: 3039-3048. doi: 10.1029/JC075i015p03039

Gao, J., Tian, L.D., Liu, Y.Q., et al., 2009. Oxygen isotope variation in the water cycle of the Yamdrok-tso Lake basin in southern Tibetan plateau. Chinese Sci. Bull., 54: 2758-2765.

Joussaume, S., Sadourny, R., Jouzel, J., 1984. A general circulation model of water isotope cycles in the atmosphere. Nature, 311: 24-29. doi: 10.1038/311024a0

Liu, Z.F., Tian, L.D., Yao, T.D., et al., 2008. The temporal and spatial variations of δ¹⁸O in river water of the Yarlung Zangbo River basin. Journal of Glaciology and Geocryology, 30(1): 20-27 (in Chinese with English abstract).

Ning, A.F., Yin, G., Liu, T.C., 2000. Characteristics of isotope distribution of atmospheric precipitation in the Lhasa River area. Journal of Mineralogy and Petrology, 20(3): 95-99 (in Chinese with English abstract). doi: 10.1029/JC084iC07p03773

Tian, L.D., Yao, T.D., Pu, J.C., et al., 1997. Characteristics of δ¹⁸O in summer precipitation at Lhasa. Journal of Glaciology and Geocryology, 19(4): 295-301 (in Chinese with English abstract). http://ci.nii.ac.jp/naid/10006913076

Torgersen, T., 1979. Isotopic composition of river runoff on the U.S. east coast: evaluation of stable isotope versus salinity plots for coastal water mass identification. Journal of Geophysical Research, 84(C7): 3773-3775. doi: 10.1029/JC084iC07p03773

Wang, N.L., Zhang, S.B., He, J.Q., et al., 2009. Tracing the major source area of the mountainous runoff generation of the Heihe River in Northwest China using stable isotope technique. Chinese Sci. Bull., 54: 2751-2757. http://nsr.oxfordjournals.org/external-ref?access_num=10.1007/s11434-009-0505-8&link_type=DOI

Wei, K.Q., Lin, R.F., Wang, Z.X., 1983. Hydrogen and oxygen stable isotopic composition and tritium content of waters from Yangbajing geothermal area, Xizang, China. Geochimica, (04): 338-336 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX198304001.htm

Yang, X.X., Xu, B.Q., Yang, W., et al., 2009. Study of altitudinal lapse rates of δ¹⁸O in precipitation/river water with seasons on the southeast Tibetan plateau. Chinese Sci. Bull., 54: 2742-2750.

Yao, T.D., Zhou, H., Yang, X.X., 2009. Indian monsoon influences altitude effect of δ¹⁸O in precipitation/river water on the Tibetan plateau. Chinese Sci. Bull., 54: 2724-2731.

高晶, 田立德, 刘勇勤, 等, 2009. 青藏高原南部羊卓雍错流域稳定同位素水文循环研究. 科学通报, 54: 2153-2159. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200915007.htm

刘忠方, 田立德, 姚檀栋, 等, 2008. 雅鲁藏布江流域河水中氧稳定同位素的时空变化. 冰川冻土, 30(1): 20-27. https://www.cnki.com.cn/Article/CJFDTOTAL-BCDT200801004.htm

宁爱凤, 尹观, 刘天仇, 2000. 拉萨河地区的大气降水同位素分布特征. 矿物岩石, 20(3): 95-99. doi: 10.3969/j.issn.1001-6872.2000.03.018

田立德, 姚檀栋, 蒲健辰, 等, 1997. 拉萨夏季降水中氧稳定同位素变化特征. 冰川冻土, 19(4): 295-301. https://www.cnki.com.cn/Article/CJFDTOTAL-BCDT704.001.htm

王宁练, 张世彪, 贺建桥, 等, 2009. 祁连山中段黑河上游山区地表径流水资源主要形成区域的同位素示踪研究. 科学通报, 54: 2148-2152. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200915006.htm

卫克勤, 林瑞芬, 王志祥, 1983. 西藏羊八井地热水的氢、氧稳定同位素组成及氚含量. 地球化学, (4): 338-336. doi: 10.3321/j.issn:0379-1726.1983.04.002

杨晓新, 徐柏青, 杨威, 等, 2009. 藏东南不同季节水体中氧同位素的高程递减变化研究. 科学通报, 54: 2140-2147. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200915005.htm

姚檀栋, 周行, 杨晓新, 2009. 印度季风水汽对青藏高原降水和河水中δ¹⁸O高程递减率的影响. 科学通报, 54: 2124-2130. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200915003.htm

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(3) / Tables(2)

Get Citation

PDF

XML

Article views (3494) PDF downloads(87)

Characteristics of Oxygen and Hydrogen Isotope Distribution of Surface Runoff in the Lhasa River Basin

doi: 10.3799/dqkx.2010.101

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content