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Stable Isotope Evidence Shows Re-emission of Elemental Mercury Vapor Occurring after Reductive Loss from Foliage
Journal article   Peer reviewed

Stable Isotope Evidence Shows Re-emission of Elemental Mercury Vapor Occurring after Reductive Loss from Foliage

Wei Yuan, Jonas Sommar, Che-Jen Lin, Xun Wang, Kai Li, Yi Liu, Hui Zhang, Zhiyun Lu, Chuansheng Wu and Xinbin Feng
Environmental science & technology, Vol.53(2), pp.651-660
01/15/2019
DOI: https://doi.org/10.1021/acs.est.8b04865
PMID: 30501171
Web of Science ID: WOS:000456349900011

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Abstract

Mercury Isotopes Fluxes Redox reactions Atmospheric Chemistry Environmental Chemistry
The mechanism of elemental mercury (Hg-0) re-emission from vegetation to the atmosphere is currently poorly understood. In this study, we investigated branch-level Hg-0 atmosphere-foliage exchange in a pristine evergreen forest by systematically combining Hg isotopic composition, air concentration and flux measurements to unravel process information. It is found that the foliage represents a diurnally changing sink for atmospheric Hg-0 and its Hg content increases with leaf age and mass. Atmospheric Hg-0 is the dominant source of foliar Hg and the involvement of Hg-II not supported by isotopic evidence. Upon Hg-0 uptake, maturing foliage becomes progressively enriched in lighter Hg isotopes and depleted in odd mass isotopes. The measured isotopic composition of foliage Hg and isotopic shift caused by Hg-0 evasion from foliage supports that Hg-0 emitted from foliage is derived from Hg previously metabolized and bound in the leaf interior then subsequently recycled after reduction, and not merely a retroflux of recently deposited Hg-0 on foliar surface. An isotopic differential mass balance model indicates that the proportion of foliar Hg-0 efflux to uptake gradually increase from emergence to senescence with an average flux ratio of 30%.

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