Spatiotemporal Variations of Hydrogeochemistry and Its Controlling Factors in the Gandaki River Basin, Central Himalaya Nepal
Science of the Total Environment 622–623 (2018) 770–782 Contents lists available at ScienceDirect Science of the Total Environment journal homepage: www.elsevier.com/locate/scitotenv Spatiotemporal variations of hydrogeochemistry and its controlling factors in the Gandaki River Basin, Central Himalaya Nepal Ramesh Raj Pant a,b,c,d,e, Fan Zhang a,b,c,d,⁎,FaizanUrRehmana,b,c,d,f, Guanxing Wang a,b,c,d,MingYeg, Chen Zeng a,b, Handuo Tang a,b,c,d a Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China b Key Laboratory of Alpine Ecology and Biodiversity, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China c CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, China d University of Chinese Academy of Sciences, Beijing, China e Central Department of Environmental Science, Tribhuvan University, Nepal f Department of Earth Sciences, COMSATS Institute of Information Technology, Abbottabad, Pakistan g Department of Earth, Ocean, and Atmospheric Science, Florida State University, Tallahassee, FL, USA HIGHLIGHTS GRAPHICAL ABSTRACT • Strong spatiotemporal variation of geo- chemistry is observed in the Gandaki River. • Hydrogeochemistry is controlled by cli- matic, geogenic and anthropogenic fac- tors. • Water facies are prevailed with Ca- HCO3 (83%), Ca-Mg-Cl (13%) and Ca-Cl (4%). • Water quality at a few locations poses safety concern for drinking and irrigation. article info abstract Article history: The characterization and assessment of water quality in the head water region of Himalaya is necessary, given the Received 7 September 2017 immense importance of this region in sustaining livelihoods of people and maintaining ecological balance.
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