中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Environment significance and hydrochemical characteristics of supra-permafrost water in the source region of the Yangtze River

文献类型:期刊论文

作者Li Zong-Jie1; Li Zong-Xing2; Song Ling-Ling3; Ma Jin-Zhu1; Song Yong4
刊名SCIENCE OF THE TOTAL ENVIRONMENT
出版日期2018-12-10
卷号644页码:1141-1151
ISSN号0048-9697
关键词Environmental significance Chemical characteristics Supra-permafrost water The source region of the Yangtze River
DOI10.1016/j.scitotenv.2018.07.029
通讯作者Li Zong-Jie(lzjie314@163.com) ; Li Zong-Xing(lizxhhs@163.com)
英文摘要This paper analyzed the environment significance and hydrochemical characteristics of the main ions on the supra-permafrost water from the view of space-time and different ablations. The study is conducted through collected 330 samples from June to September in 2016 and 2017 in the Source Region of the Yangtze River (SRYR). The results showed the pattern of ionic dominance based on mean value was following as: Cl- > Na+ > SO42- > Ca2+ > Mg2+ > K+ > NO3- > NO2- > NH4+ > F- > Li+, Cl- alone contributed 40.57%, and Cl-, Na+, SO42- and Ca2+ accounted for 94.06% of the total ionic concentrations.The spatial variation of ionic concentration was larger at the initial stage of ablation, and more stable in strong ablation and the end of the ablation stage. The area with elevation of 4500 m was the region where the control source of ions was more sensitive to the hydrochemical characteristics of supra-permafrost water in the study area. Through the analysis of the sources of ions, the anions and cations in supra-permafrost water in the study area were mainly controlled by crustal sources including evaporates rocks and carbonate rocks. The recharge effect of precipitation and snow-melt water only affected the concentration of Cl-, NH4+, NO3-, F-, Li+ and K+, but did not affect NO2-, SO2-, Mg2+ and Ca2+. The hydrochemical type of supra-permafrost water was Ca2+ -SO42- in high elevation (>4800 m). However, the hydrochemical type of middle elevation (from 4400 m to 4700 m) was Na+-Cl-. The type of hydrochemistry at low altitude was more complex than at high and middle elevation. This study provides insights on the construction of hydrological models in the cold regions and scientific basis for water resources management in the Tibet Plateaus. (C) 2018 Elsevier B.V. All rights reserved.
收录类别SCI ; ISTP
WOS关键词QILIAN MOUNTAINS ; SEDIMENT LOAD ; CHINA ; BASIN ; CHEMISTRY ; PRECIPITATION ; GEOCHEMISTRY ; CRYOSPHERE ; GLACIER ; RUNOFF
WOS研究方向Environmental Sciences & Ecology
WOS类目Environmental Sciences
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000445164000117
URI标识http://www.irgrid.ac.cn/handle/1471x/2558297
专题寒区旱区环境与工程研究所
通讯作者Li Zong-Jie; Li Zong-Xing
作者单位1.Lanzhou Univ, Coll Earth Environm Sci, Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Gansu, Peoples R China
2.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Gansu Hydrol & Water Resources Engn Res Ctr, Key Lab Ecohydrol Inland River Basin, Lanzhou 730000, Gansu, Peoples R China
3.Gansu Agr Univ, Coll Forestry, Lanzhou 730070, Gansu, Peoples R China
4.CSIRO Land & Water, Private Bag 10, Clayton, Vic 3169, Australia
推荐引用方式
GB/T 7714
Li Zong-Jie,Li Zong-Xing,Song Ling-Ling,et al. Environment significance and hydrochemical characteristics of supra-permafrost water in the source region of the Yangtze River[J]. SCIENCE OF THE TOTAL ENVIRONMENT,2018,644:1141-1151.
APA Li Zong-Jie,Li Zong-Xing,Song Ling-Ling,Ma Jin-Zhu,&Song Yong.(2018).Environment significance and hydrochemical characteristics of supra-permafrost water in the source region of the Yangtze River.SCIENCE OF THE TOTAL ENVIRONMENT,644,1141-1151.
MLA Li Zong-Jie,et al."Environment significance and hydrochemical characteristics of supra-permafrost water in the source region of the Yangtze River".SCIENCE OF THE TOTAL ENVIRONMENT 644(2018):1141-1151.

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来源:寒区旱区环境与工程研究所

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