Characteristics of water isotopes and hydrograph separation during the wet season in the Heishui River, China
Liu, Yuhong1,2; Fan, Ningjiang1; An, Shuqing1; Bai, Xiaohua1; Liu, Fude1; Xu, Zhen1,3; Wang, Zhongsheng1; Liu, Shirong4
刊名JOURNAL OF HYDROLOGY
2008-05-30
卷号353期号:3-4页码:314-321
关键词Stable Isotopes Spatial Variations River Water Line Contribution
ISSN号0022-1694
通讯作者An, SQ, Nanjing Univ, Sch Life Sci, Lab Forest Ecol & Global Changes, Nanjing 210093, Peoples R China
产权排序Nanjing Univ, Sch Life Sci, Lab Forest Ecol & Global Changes;CAS, Yantai Inst Coastal Zone Res Sustainable Dev;State Power Environm Protect Res Inst;Chinese Acad Forestry, Inst Forest Ecol Environm & Protect
文献子类Article
英文摘要Runoff generation and dynamics is an important issue in watershed and water resource management, but the mechanism in large scale is unclear and site-dependent. For this reason, spatial variations of delta D and delta O-18 of river water and their sources within large-area of the Heishui Valley of the upper Yangtze River in western China were investigated during the wet season. A total 117 river water samples were collected at 13 sampling sites located at the junction of the principal river course and its tributaries. The results showed no spatial variations of either delta D or delta O-18 values existed among tributary sampling sites A, B, E, F, H and I during the wet season, and significantly spatial variation occurred between tributary sampling sites A, B, E, F, H, I and site K; which indicated different proportions of rain entering river water should lead to spatial variation of water isotopes. The hydrograph separation analysis, based on the isotope data of river water, meltwater and rain water samples, showed the contribution of snow and glacier meltwater varied from 63.8% to 92.6%, and that of rain varied from 7.4% to 36.2%; which meant that snow and glacier meltwater was the main supplying water source of baseflow in the Heishui Valley. And the rotes of glacier and snow meltwater should be significantly noticed in water resource management in this alpine valley at the rim of the Tibetan Plateau. (c) 2008 Elsevier B.V. All rights reserved.; Runoff generation and dynamics is an important issue in watershed and water resource management, but the mechanism in large scale is unclear and site-dependent. For this reason, spatial variations of delta D and delta(18)O of river water and their sources within large-area of the Heishui Valley of the upper Yangtze River in western China were investigated during the wet season. A total 117 river water samples were collected at 13 sampling sites located at the junction of the principal river course and its tributaries. The results showed no spatial variations of either delta D or delta(18)O values existed among tributary sampling sites A, B, E, F, H and I during the wet season, and significantly spatial variation occurred between tributary sampling sites A, B, E, F, H, I and site K; which indicated different proportions of rain entering river water should lead to spatial variation of water isotopes. The hydrograph separation analysis, based on the isotope data of river water, meltwater and rain water samples, showed the contribution of snow and glacier meltwater varied from 63.8% to 92.6%, and that of rain varied from 7.4% to 36.2%; which meant that snow and glacier meltwater was the main supplying water source of baseflow in the Heishui Valley. And the rotes of glacier and snow meltwater should be significantly noticed in water resource management in this alpine valley at the rim of the Tibetan Plateau. (c) 2008 Elsevier B.V. All rights reserved.
学科主题Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources
URL标识查看原文
WOS关键词STABLE-ISOTOPES ; ELECTRICAL-CONDUCTIVITY ; CATCHMENT-SCALE ; RUNOFF
WOS研究方向Engineering ; Geology ; Water Resources
语种英语
WOS记录号WOS:000255990300007
公开日期2011-07-05
内容类型期刊论文
源URL[http://ir.yic.ac.cn/handle/133337/3420]  
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.CAS, Yantai Inst Coastal Zone Res Sustainable Dev, Yantai 264003, Peoples R China
3.State Power Environm Protect Res Inst, Nanjing 210031, Peoples R China
4.Chinese Acad Forestry, Inst Forest Ecol Environm & Protect, Beijing 100091, Peoples R China
推荐引用方式
GB/T 7714
Liu, Yuhong,Fan, Ningjiang,An, Shuqing,et al. Characteristics of water isotopes and hydrograph separation during the wet season in the Heishui River, China[J]. JOURNAL OF HYDROLOGY,2008,353(3-4):314-321.
APA Liu, Yuhong.,Fan, Ningjiang.,An, Shuqing.,Bai, Xiaohua.,Liu, Fude.,...&Liu, Shirong.(2008).Characteristics of water isotopes and hydrograph separation during the wet season in the Heishui River, China.JOURNAL OF HYDROLOGY,353(3-4),314-321.
MLA Liu, Yuhong,et al."Characteristics of water isotopes and hydrograph separation during the wet season in the Heishui River, China".JOURNAL OF HYDROLOGY 353.3-4(2008):314-321.
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