Abstract

In situ air concentrations of gaseous elemental mercury (Hg(0)) and vegetation–atmosphere fluxes were quantified in both high (Cala Norte, CN) and low-to-moderate (Alcochete, ALC) Hg-contaminated saltmarsh areas of the Tagus estuary colonized by plant species Halimione portulacoides (Hp) and Sarcocornia fruticosa (Sf). Atmospheric Hg(0) ranged between 1.08–18.15 ng m−3 in CN and 1.18–3.53 ng m−3 in ALC. In CN, most of the high Hg(0) levels occurred during nighttime, while the opposite was observed at ALC, suggesting that photoreduction was not driving the air Hg(0) concentrations at the contaminated site. Vegetation–air Hg(0) fluxes were low in ALC and ranged from −0.76 to 1.52 ng m−2 (leaf area) h−1 for Hp and from −0.40 to 1.28 ng m−2 (leaf area) h−1 for Sf. In CN, higher Hg fluxes were observed for both plants, ranging from −9.90 to 15.45 ng m−2 (leaf area) h−1 for Hp and from −8.93 to 12.58 ng m−2 (leaf area) h−1 for Sf. Mercury flux results at CN were considered less reliable due to large and fast variations in the ambient air concentrations of Hg(0), which may have been influenced by emissions from the nearby chlor-alkali plant, or historical contamination. Improved experimental setup, the influence of high local Hg concentrations and the seasonal activity of the plants must be considered when assessing vegetation–air Hg(0) fluxes in Hg-contaminated areas.

Highlights

  • Mercury (Hg) is a naturally occurring and toxic metal that is present in natural ecosystems

  • Our findings suggest that elevated and variable background air Hg(0) concentrations from anthropogenic Hg sources, such as those presumed to occur at Cala Norte (CN), may make measurements of vegetation mercury flux to the atmosphere unreliable

  • This study examined the air concentrations of Hg(0) mediated by emissions from saltmarsh plants that colonize low and heavily Hg-contaminated areas of the Tagus estuary

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Summary

Introduction

Mercury (Hg) is a naturally occurring and toxic metal that is present in natural ecosystems. Measuring and modeling of Hg emissions from representative surfaces are crucial to evaluate the role of natural terrestrial and aquatic environments on the cycling of Hg on both regional and global scales [6,7,8,9,10]. Since anthropogenic atmospheric Hg(0) can be recycled through and re-emitted from vegetation, it remains unclear if the biosphere is a long-term source or sink of Hg. Once nearly 30% of the earth’s land surface area is covered by vegetation (approximately 4 × 109 ha) [15], it is crucial to quantify the role of vegetation in Hg emissions, on both regional and global scales, in order to develop accurate mass balances for global movements [16,17]

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