IR
Runoff dominated by supra-permafrost water in the source region of the Yangtze river using environmental isotopes
Li, Zongxing1; Li, Zongjie2; Feng, Qi1; Zhang, Baijuan2; Gui, Juan1; Xue, Jian1; Gao, Wende2
2020-03
发表期刊JOURNAL OF HYDROLOGY
ISSN0022-1694
卷号582
摘要Accelerating multiphase water transformation affects runoff processes and components greatly and have changed the spatiotemporal patterns of water resources in the Third Polar Region. The source region of the Yangtze River is one location where accelerated warming has resulted in the gradual extension of the ablation period since 1990. This has caused the acceleration of multiphase water transformation, characterized by increases in the rate of glacial retreat, maximum freezing depth, and annual actual evapotranspiration and by decreased snowfall. In response, the total runoff increased by 53% at the Tuotuohe national hydrological station (TTH) and 6% at the Zhimenda national hydrological station (ZMD) during the periods 1961-1990 and 1991-2017, respectively. Under these conditions, runoff components were being determined based on stable isotope tracing. Substantial seasonal differences in delta O-18 (delta D) among precipitation, river water, supra-permafrost water, and glaciers snow meltwater indicate that the runoff has been replenished by multiple components, and that these first infiltrate the ground, becoming part of the groundwater, and then recharge river water. Supra-permafrost water rather than precipitation now dominates river water. Based on the end-member mixing analysis model, supra-permafrost water, precipitation, and glaciers snow meltwater accounted for 51%, 26%, and 23% of river water at the TTH station from June 2016 to May 2018; the corresponding values at the ZMD station were 49%, 34%, and 17%. Additionally, there are also differences in the seasonal contributions of runoff components to river water. Seasonal variations in the freezing and thawing of the active layer directly trigger the runoff process. Future research should be focused on determining the mechanisms underlying the dynamics of precipitation-supra-permafrost water-runoff, which will aid the assessment of the impacts of an unstable Asian Water Tower on water resources.
关键词Runoff Permafrost Stable isotope Accelerating multiphase water transformation Yangtze River
DOI10.1016/j.jhydrol.2019.124506
收录类别SCI ; SCIE
语种英语
资助项目Second Tibetan Plateau Scientific Expedition and Research Program(STEP)[2019QZKK0405] ; National Key R&D Program of China[SQ2019YFC050024-01] ; Youth Innovation Promotion Association, CAS, China[2013274] ; National Nature Science Foundation of China[91547102][41771077] ; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment[SKLLQG1814]
WOS研究方向Engineering ; Geology ; Water Resources
WOS类目Engineering, Civil ; Geosciences, Multidisciplinary ; Water Resources
WOS记录号WOS:000517663700040
出版者ELSEVIER
EI入藏号20195307949941
EI主题词Recharging (underground waters)
EI分类号443.3 Precipitation - 444.1 Surface Water - 444.2 Groundwater - 446.1 Water Supply Systems - 931.2 Physical Properties of Gases, Liquids and Solids
来源库WOS
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被引频次:34[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符https://ir.lut.edu.cn/handle/2XXMBERH/76183
专题兰州理工大学
能源与动力工程学院
通讯作者Li, Zongxing
作者单位1.Chinese Acad Sci, Key Lab Ecohydrol Inland River Basin, Northwest Inst Ecoenvironm & Resources, Gansu Qilian Mt Rea Environm Res Ctr, Lanzhou 730000, Peoples R China;
2.Lanzhou Univ Technol, Coll Energy & Power Engn, Lanzhou 730050, Peoples R China
推荐引用方式
GB/T 7714
Li, Zongxing,Li, Zongjie,Feng, Qi,et al. Runoff dominated by supra-permafrost water in the source region of the Yangtze river using environmental isotopes[J]. JOURNAL OF HYDROLOGY,2020,582.
APA Li, Zongxing.,Li, Zongjie.,Feng, Qi.,Zhang, Baijuan.,Gui, Juan.,...&Gao, Wende.(2020).Runoff dominated by supra-permafrost water in the source region of the Yangtze river using environmental isotopes.JOURNAL OF HYDROLOGY,582.
MLA Li, Zongxing,et al."Runoff dominated by supra-permafrost water in the source region of the Yangtze river using environmental isotopes".JOURNAL OF HYDROLOGY 582(2020).
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