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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