4.7 Article

Atmospheric particle-bound mercury in the northern Indo-Gangetic Plain region: Insights into sources from mercury isotope analysis and influencing factors

Journal

GEOSCIENCE FRONTIERS
Volume 13, Issue 1, Pages -

Publisher

CHINA UNIV GEOSCIENCES, BEIJING
DOI: 10.1016/j.gsf.2021.101274

Keywords

Particle-bound mercury; Seasonality; Mercury isotopes; Deposition flux; Indo-Gangetic Plain

Funding

  1. National Natural Science Foun-dation of China [41801042, 41630754]
  2. Second Tibetan Plateau Scientific Expedition and Research Program (STEP) [2019QZKK0605]
  3. State Key Laboratory of Cryo-spheric Sciences, Chinese Academy of Sciences [SKLCS-ZZ-2020]
  4. Asia-Pacific Network for Global Change Research (APN) [CRECS2020-07MY-Tripathee]
  5. PIFI fellowship from the Chinese Acad-emy of Sciences [2020FYC0001]

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This study investigates the levels, seasonality, sources, and influencing factors of particulate-bound mercury (PBM) in the atmosphere of Lumbini, Nepal. The results show that the PBM concentration exceeds the reported ranges for remote and rural sites worldwide and is mainly influenced by anthropogenic sources during the dry season and post-monsoon period.
Lumbini isa world heritage site located in the southern plains region of Nepal, and is regarded as a potential site for evaluating transboundary air pollution due to its proximity to the border with India. In this study, 82 aerosol samples were collected between April 2013 and July 2014 to investigate the levels of particulate-bound mercury (PBM) and the corresponding seasonality, sources, and influencing factors. The PBM concentration in total suspended particulate (TSP) matter ranged from 6.8 pg m-3 to 351.7 pg m-3 (mean of 99.7 +/- 92.6 pg m-3), which exceeded the ranges reported for remote and rural sites worldwide. The Hg content (PBM/TSP) ranged from 68.2 ng g-1 to 1744.8 ng g-1 (mean of 446.9 +/- 312.7 ng g-1), indicating anthropogenic enrichment. The PBM levels were higher in the dry season (i.e., winter and the pre-monsoon period) than in the wet season (i.e., the monsoon period). In addition, the d202Hg signature indicated that waste/coal burning and traffic were the major sources of Hg in Lumbini during the pre-monsoon period. Meanwhile, precipitation occurring during photochemical processes in the atmosphere may have been responsible for the observed D199Hg values in the aerosol samples obtained during the monsoon period. The PBM concentration was influenced mostly by the resuspension of polluted dust during dry periods and crop residue burning during the post-monsoon period. The estimated PBM deposition flux at Lumbini was 15.7 lg m-2 yr-1. This study provides a reference dataset of atmospheric PBM over a year, which can be useful for understanding the geochemical cycling of Hg in this region of limited data. (c) 2021 China University of Geosciences (Beijing) and Peking University. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/ licenses/by-nc-nd/4.0/).

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