中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Major ions and trace elements of two selected rivers near Everest region, southern Himalayas, Nepal

文献类型:期刊论文

作者Kang, SC; Kang, S (Kang, Shichang)4,5; Paudyal, R (Paudyal, Rukumesh)1,5,6,7; Sharma, CM (Sharma, Chhatra Mani)1,3,7; Tripathee, L (Tripathee, Lekhendra)2,7; Huang, J (Huang, Jie)2; Rupakheti, D (Rupakheti, Dipesh)2,6; Sillanpaa, M (Sillanpaeae, Mika)1
刊名ENVIRONMENTAL EARTH SCIENCES
出版日期2016
卷号75期号:1页码:46
关键词Tibetan Plateau Chemical-composition Weathering Processes Co2 Consumption Water Chemistry System Precipitation Transport Glaciers Erosion
DOI10.1007/s12665-015-4811-y
文献子类Article
英文摘要During pre-monsoon of 2013, water samples were collected from 30 sites of two major rivers, viz. Dudh Koshi and Indrawati to assess the river water quality on the southern side of the Nepalese Himalayas. The physical parameters such as pH, EC, turbidity and water temperature were measured in the field and major ions (Na+, NH4+, K+, Ca-2(+), Mg-2(+), Cl-, SO42-, and NO3-) and element concentrations (Li, Sc, V, Cr, Mn, Co, Ni, Cu, Zn, Ga, As, Rb, Sr, Cs, Ba, Pb, U, Y, Zr, Nb and Cd) in the water samples were analyzed in the laboratory. The result indicated river waters were neutral to mostly alkaline with pH ranging from 6.57 to 8.81 and EC ranging from 10.5 to 321 mu S/cm. The lower values of turbidity were recorded in the pristine tributaries of Dudh Koshi, whereas the main rivers had the higher values with a range of 0.51-515 NTU. Bicarbonate (HCO3-) showed a significant correlation with Ca2+ and Mg2+, suggesting carbonate weathering as the dominant geochemical process in the region. Furthermore, the Gibbs plot also suggested the dominance of rock weathering. Very low concentration of trace elements was found in most of the samples which were within the WHO guidelines. In addition, the concentrations of toxic elements such as As and Pb were below the detectable limits in most of the samples. Furthermore, the analysis of PCA suggests that most of the elements originated from natural weathering; however, there were some evidences of anthropogenic effect on water quality which may not be critical issue at present but can be of concern in future.
学科主题自然地理学
语种英语
WOS记录号WOS:000370239800046
源URL[http://ir.itpcas.ac.cn/handle/131C11/7878]  
专题青藏高原研究所_图书馆
通讯作者Kang, SC
作者单位1.Lappeenranta Univ Technol, Lab Green Chem, Sammonkatu 12, Mikkeli 50130, Finland
2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China
3.Kathmandu Univ, Sch Sci, Dept Environm Sci & Engn, Kavre, Nepal
4.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
5.Chinese Acad Sci, CAREERI, State Key Lab Cryospher Sci, Donggang West Rd 320, Lanzhou 730000, Peoples R China
6.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
7.HERI, Kathmandu, Nepal
推荐引用方式
GB/T 7714
Kang, SC,Kang, S ,Paudyal, R ,et al. Major ions and trace elements of two selected rivers near Everest region, southern Himalayas, Nepal[J]. ENVIRONMENTAL EARTH SCIENCES,2016,75(1):46.
APA Kang, SC.,Kang, S .,Paudyal, R .,Sharma, CM .,Tripathee, L .,...&Sillanpaa, M .(2016).Major ions and trace elements of two selected rivers near Everest region, southern Himalayas, Nepal.ENVIRONMENTAL EARTH SCIENCES,75(1),46.
MLA Kang, SC,et al."Major ions and trace elements of two selected rivers near Everest region, southern Himalayas, Nepal".ENVIRONMENTAL EARTH SCIENCES 75.1(2016):46.

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来源:青藏高原研究所

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