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
发表期刊JOURNAL OF HYDROLOGY
ISSN0022-1694
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
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
通讯作者An, SQ, Nanjing Univ, Sch Life Sci, Lab Forest Ecol & Global Changes, Nanjing 210093, Peoples R China
作者部门滨海湿地实验室
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.
文章类型Article
收录类别SCI
语种英语
关键词[WOS]STABLE-ISOTOPES ; ELECTRICAL-CONDUCTIVITY ; CATCHMENT-SCALE ; RUNOFF
研究领域[WOS]Engineering ; Geology ; Water Resources
WOS记录号WOS:000255990300007
引用统计
被引频次:88[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.yic.ac.cn/handle/133337/3419
专题中国科学院海岸带环境过程与生态修复重点实验室_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.
条目包含的文件 下载所有文件
文件名称/大小 文献类型 版本类型 开放类型 使用许可
Characteristics of w(702KB) 开放获取--浏览 下载
个性服务
推荐该条目
保存到收藏夹
查看访问统计
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Liu, Yuhong]的文章
[Fan, Ningjiang]的文章
[An, Shuqing]的文章
百度学术
百度学术中相似的文章
[Liu, Yuhong]的文章
[Fan, Ningjiang]的文章
[An, Shuqing]的文章
必应学术
必应学术中相似的文章
[Liu, Yuhong]的文章
[Fan, Ningjiang]的文章
[An, Shuqing]的文章
相关权益政策
暂无数据
收藏/分享
文件名: Characteristics of water isotopes and hydrograph separation during the wet season in the Heishui River, China.pdf
格式: Adobe PDF
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。