Articles | Volume 16, issue 20
Atmos. Chem. Phys., 16, 12861–12873, 2016
https://doi.org/10.5194/acp-16-12861-2016
Atmos. Chem. Phys., 16, 12861–12873, 2016
https://doi.org/10.5194/acp-16-12861-2016

Research article 18 Oct 2016

Research article | 18 Oct 2016

Depletion of atmospheric gaseous elemental mercury by plant uptake at Mt. Changbai, Northeast China

Xuewu Fu1, Wei Zhu1, Hui Zhang1, Jonas Sommar1, Ben Yu1, Xu Yang1, Xun Wang1,2, Che-Jen Lin1,3,4, and Xinbin Feng1 Xuewu Fu et al.
  • 1State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, 99 Lincheng West Road, Guiyang, 550081, China
  • 2University of the Chinese Academy of Sciences, Beijing 100049, China
  • 3Department of Civil and Environmental Engineering, Lamar University, Beaumont, Texas 77710, USA
  • 4Center for Advances in Water and Air Quality, Lamar University, Beaumont, Texas 77710, USA

Abstract. There exists observational evidence that gaseous elemental mercury (GEM) can be readily removed from the atmosphere via chemical oxidation followed by deposition in the polar and sub-polar regions, free troposphere, lower stratosphere, and marine boundary layer under specific environmental conditions. Here we report GEM depletions in a temperate mixed forest at Mt. Changbai, Northeast China. The strong depletions occurred predominantly at night during the leaf-growing season and in the absence of gaseous oxidized mercury (GOM) enrichment (GOM  <  3 pg m−3). Vertical gradients of decreasing GEM concentrations from layers above to under forest canopy suggest in situ loss of GEM to forest canopy at Mt. Changbai. Foliar GEM flux measurements showed that the foliage of two predominant tree species is a net sink of GEM at night, with a mean flux of −1.8 ± 0.3 ng m2 h−1 over Fraxinus mandshurica (deciduous tree species) and −0.1 ± 0.2 ng m2 h−1 over Pinus Koraiensis (evergreen tree species). Daily integrated GEM δ202Hg, Δ199Hg, and Δ200Hg at Mt. Changbai during 8–18 July 2013 ranged from −0.34 to 0.91 ‰, from −0.11 to −0.04 ‰ and from −0.06 to 0.01 ‰, respectively. A large positive shift in GEM δ202Hg occurred during the strong GEM depletion events, whereas Δ199Hg and Δ200Hg remained essentially unchanged. The observational findings and box model results show that uptake of GEM by forest canopy plays a predominant role in the GEM depletion at Mt. Changbai forest. Such depletion events of GEM are likely to be a widespread phenomenon, suggesting that the forest ecosystem represents one of the largest sinks ( ∼ 1930 Mg) of atmospheric Hg on a global scale.

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