Spatio-temporal variation of stable isotopes of river waters, water source identification and water security in the Heishui Valley (China) during the dry-season
Liu, Yuhong1,2; An, Shuqing1; Xu, Zhen1; Fan, Ningjiang1; Cui, Jun1; Wang, Zhongsheng1; Liu, Shirong3; Pan, Jiayong4; Lin, Guanghui5
刊名HYDROGEOLOGY JOURNAL
2008-03-01
卷号16期号:2页码:311-319
关键词China Climate Change Snow And Glacial Meltwater Stable Isotopes Water-resource Conservation
ISSN号1431-2174
通讯作者An, SQ, Nanjing Univ, Sch Life Sci, Lab Forest Ecol & Global Changes, Hankou Rd 22, Nanjing 210093, Peoples R China
产权排序Nanjing Univ, Sch Life Sci, Lab Forest Ecol & Global Changes; Chinese Acad Sci, Yantai Inst Coastal Zone Res Sustainable Dev;Chinese Acad Sci, Inst Forest Ecol Environm & Protect;Nanjing Univ, Dept Geol;Carnegie Inst Washington, Dept Global Ecol
文献子类Article
英文摘要Spatial variations of delta D and delta O-18 among seven tributaries and their water sources were investigated in the Heishui Valley of the Yangtze River, China during the dry-season in 2004. A one-way ANOVA (analysis of variation) test showed that both delta D (p < 0.01) and delta O-18 (p = 0.045) spatially varied among the seven tributaries. The plot of delta O-18 versus delta D for the river water collected at different locations showed that isotopic fractionation occurred during the snow and glacial melting process. The depleted delta O-18 and delta D in the tributary waters distributed above the local meteoric water line (LMWL) suggested that the glacial and early snowpack meltwater largely recharged these streams during the early spring. The meltwater was isotopically distinguishable from the precipitation and river water, which had been evaporated during warmer and drier times. If glaciers and snow accumulation diminish with future climate warming, the recharge of these tributaries' baseflow will decline and the security of the water resource in this watershed will be threatened.; Spatial variations of delta D and delta O-18 among seven tributaries and their water sources were investigated in the Heishui Valley of the Yangtze River, China during the dry-season in 2004. A one-way ANOVA (analysis of variation) test showed that both delta D (p < 0.01) and delta O-18 (p = 0.045) spatially varied among the seven tributaries. The plot of delta O-18 versus delta D for the river water collected at different locations showed that isotopic fractionation occurred during the snow and glacial melting process. The depleted delta O-18 and delta D in the tributary waters distributed above the local meteoric water line (LMWL) suggested that the glacial and early snowpack meltwater largely recharged these streams during the early spring. The meltwater was isotopically distinguishable from the precipitation and river water, which had been evaporated during warmer and drier times. If glaciers and snow accumulation diminish with future climate warming, the recharge of these tributaries' baseflow will decline and the security of the water resource in this watershed will be threatened.
学科主题Geosciences, Multidisciplinary ; Water Resources
URL标识查看原文
WOS关键词TIBETAN PLATEAU ; PRECIPITATION ; RUNOFF ; SCALE ; ICE ; GROUNDWATER ; CALIFORNIA ; SNOWMELT ; NEVADA ; CANADA
WOS研究方向Geology ; Water Resources
语种英语
WOS记录号WOS:000254184800009
公开日期2011-07-05
内容类型期刊论文
源URL[http://ir.yic.ac.cn/handle/133337/3426]  
专题烟台海岸带研究所_滨海湿地实验室
作者单位1.Nanjing Univ, Sch Life Sci, Lab Forest Ecol & Global Changes, Nanjing 210093, Peoples R China
2.Chinese Acad Sci, Yantai Inst Coastal Zone Res Sustainable Dev, Yantai 264003, Peoples R China
3.Chinese Acad Sci, Inst Forest Ecol Environm & Protect, Beijing 100091, Peoples R China
4.Nanjing Univ, Dept Geol, Nanjing 210093, Peoples R China
5.Carnegie Inst Washington, Dept Global Ecol, Stanford, CA 94305 USA
推荐引用方式
GB/T 7714
Liu, Yuhong,An, Shuqing,Xu, Zhen,et al. Spatio-temporal variation of stable isotopes of river waters, water source identification and water security in the Heishui Valley (China) during the dry-season[J]. HYDROGEOLOGY JOURNAL,2008,16(2):311-319.
APA Liu, Yuhong.,An, Shuqing.,Xu, Zhen.,Fan, Ningjiang.,Cui, Jun.,...&Lin, Guanghui.(2008).Spatio-temporal variation of stable isotopes of river waters, water source identification and water security in the Heishui Valley (China) during the dry-season.HYDROGEOLOGY JOURNAL,16(2),311-319.
MLA Liu, Yuhong,et al."Spatio-temporal variation of stable isotopes of river waters, water source identification and water security in the Heishui Valley (China) during the dry-season".HYDROGEOLOGY JOURNAL 16.2(2008):311-319.
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