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Potentially Toxic Trace Metals in Water and Lake-Bed Sediment of Panchpokhari,an Alpine Lake Series in the Central Himalayan Region of Nepal
Authors:Rosha Raut  Roshan Man Bajracharya  Subodh Sharma  Chhatra Mani Sharma  Shichang Kang  Qianggong Zhang  Lekhendra Tripathee  Pengfei Chen  Dipesh Rupakheti  Junming Guo  Bhawani S Dongol
Institution:1.Aquatic Ecology Centre (AEC), Department of Environmental Science and Engineering, School of Science,Kathmandu University,Kathmandu,Nepal;2.Himalayan Environment Research Institute (HERI),Kathmandu,Nepal;3.State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou,China;4.CAS Center for Excellence in Tibetan Plateau Earth Sciences,Chinese Academy of Sciences,Beijing,China;5.Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing,China;6.World Wildlife Fund,Kathmandu,Nepal
Abstract:This study assessed the level of potentially toxic trace metals (PTMs), seasonal variations, and their possible sources from the surface water and lake-bed sediment of Panchpokhari lake series, an alpine and glacial lake at 4160 m a.s.l. in Central Nepal. The lake series have five lakes, with Lake-1 larger than others. So, Lake-1 was investigated thoroughly during pre-monsoon and post-monsoon seasons. Sediment core was collected from the deepest basin of the Lake-1 during pre-monsoon. Most of the PTM concentrations were higher in the pre-monsoon season; however, Sc, Cr, Cu, Zn, As, and Ag were higher in the post-monsoon. This is an indication that the lake has been impacted either by natural or long-range transported atmospheric pollutants. Ti, Sb, and Ag had extremely high enrichment factor (EF) in waters, whereas Cd, Zn, and As had high EF in sediments indicating that these metals originated from anthropogenic sources. Furthermore, PTM concentrations in the sediment were in the increasing order of Hg < Cd < Ag < Mo < Sb < Sn < As < U < Sc < Co < Cs < Cu < Pb < Ni < Cr < V < Zn < Rb < Mn < Ti < Fe and showed that the upper layer (top 10 cm) of lake sediment has been receiving a higher load of PTMs in the recent period. he observed EF values also suggested that major sources of PTMs in the sediment were from crustal origin except for a few metals (Ti, V, Sb, and Ag) which were enriched anthropogenically due to long-range transport of atmospheric pollutants, deposited at the higher elevations. Nevertheless, the level of pollution in sediments was low as indicated both by EF and geo-accumulation index.
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