New insights into trace elements in the water cycle of a karst-dominated glacierized region, southeast Tibetan Plateau
Creators
- 1. State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-environment and Resources, Chinese Academy of Sciences, Lanzhou 730000 (China)
- 2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029 (China)
- 3. CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101 (China)
- 4. MOE Key Laboratory of West China's Environmental System, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000 (China)
- 5. Key Laboratory of Mountain Hazards and Surface Process, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences (CAS), Chengdu 610041 (China)
Description
Highlights: • TEs are enriched in snow relative to precipitation and aerosol. • Zn, Pb, Cu and Ni in snow are influenced by anthropogenic activities. • The anthropogenic sources of TEs are from South Asian and local emissions. • Water near human settlements has been affected by anthropogenic activities. • Snow melting from glacier could release TEs to river and underground water. Trace elements (TEs) in water are crucial parameters for assessing water quality. However, detailed studies are limited on TEs in the hydrological system of the Tibetan plateau (TP). Here, we sampled snow, river water, and groundwater in Yulong Snow Mountain (Mt. Yulong) region, southeast TP, in 2016 and analyzed the concentrations of nine TEs (namely Al, Mn, Fe, Cr, Ni, Cu, Zn, As, and Pb). In snow, the average concentrations of Fe, Zn, and Al were >10 μg/L, whereas other elements, including Cr, Ni, Cu, As, Hg, and Pb, exhibited average concentrations <1 μg/L. The concentrations of Al, Mn, Fe, Zn, and As were higher in rivers than in snow. According to enrichment factors (EFs), Zn concentration in snow was highly influenced by anthropogenic activities, whereas Mn, Fe, Cr, and As were uninfluenced. River and lake/reservoir water near human settlements were affected by anthropogenic activities. However, groundwater around Mt. Yulong is not contaminated yet. The increasing EFs in Mt. Yulong snowpit are consistent with those of southern TP snowpits, suggesting that the area has been affected by anthropogenic activities both from local emissions and long-distance transport of pollutants from South Asia. A conceptual model was proposed to show TEs in the water cycle. Although water quality is good overall in Mt. Yulong region, threats to the water environment still exit due to increasing anthropogenic activities and climate warming. The accelerated ablation of cryosphere due to climate warming could be a source of TEs in rivers and groundwater, which should be paid attention to in the future.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.scitotenv.2020.141725Additional details
Identifiers
- DOI
- 10.1016/j.scitotenv.2020.141725;
- PII
- S0048969720352542;
Publishing Information
- Journal Title
- Science of the Total Environment
- Journal Volume
- 751
- Journal Page Range
- vp.
- ISSN
- 0048-9697
- CODEN
- STENDL
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 54064078
- Subject category
- S54: ENVIRONMENTAL SCIENCES; S58: GEOSCIENCES;
- Descriptors DEI
- AEROSOLS; CLIMATES; CRYOSPHERE; ECOLOGICAL CONCENTRATION; EMISSION; GLACIERS; GROUND WATER; LAKES; POLLUTANTS; RIVERS; SNOW; TRACE AMOUNTS; WATER QUALITY; WATER RESERVOIRS
- Descriptors DEC
- ATMOSPHERIC PRECIPITATIONS; COLLOIDS; DISPERSIONS; ENVIRONMENTAL QUALITY; HYDROGEN COMPOUNDS; OXYGEN COMPOUNDS; SOLS; SURFACE WATERS; WATER
Optional Information
- Copyright
- Copyright (c) 2020 Elsevier B.V. All rights reserved.