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《Earth Science(Journal of China University of Geosciences)》 2010-05
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Characteristics of Oxygen and Hydrogen Isotope Distribution of Surface Runoff in the Lhasa River Basin

YU Ting-ting1,2,GAN Yi-qun1,2,ZHOU Ai-guo1,2,LIU Cun-fu1,2,LIU Yun-de1,2,LI Xiao-qian1,2,CAI He-sheng1,2 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  
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.
【Fund】: 国家自然科学基金项目(Nos.40602030 40772156);; 中国地质调查局项目(No.1212010818093)
【CateGory Index】: P342
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