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Mass-Independent Fractionation of Even and Odd Mercury Isotopes during Atmospheric Mercury Redox Reactions.
Fu, Xuewu; Jiskra, Martin; Yang, Xu; Marusczak, Nicolas; Enrico, Maxime; Chmeleff, Jérôme; Heimbürger-Boavida, Lars-Eric; Gheusi, François; Sonke, Jeroen E.
Afiliación
  • Fu X; Géosciences Environnement Toulouse, CNRS/IRD/CNRS/Université de Toulouse, Toulouse 31000, France.
  • Jiskra M; State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China.
  • Yang X; Géosciences Environnement Toulouse, CNRS/IRD/CNRS/Université de Toulouse, Toulouse 31000, France.
  • Marusczak N; Environmental Geosciences, University of Basel, Basel 4001, Switzerland.
  • Enrico M; Géosciences Environnement Toulouse, CNRS/IRD/CNRS/Université de Toulouse, Toulouse 31000, France.
  • Chmeleff J; Géosciences Environnement Toulouse, CNRS/IRD/CNRS/Université de Toulouse, Toulouse 31000, France.
  • Heimbürger-Boavida LE; Géosciences Environnement Toulouse, CNRS/IRD/CNRS/Université de Toulouse, Toulouse 31000, France.
  • Gheusi F; Géosciences Environnement Toulouse, CNRS/IRD/CNRS/Université de Toulouse, Toulouse 31000, France.
  • Sonke JE; Géosciences Environnement Toulouse, CNRS/IRD/CNRS/Université de Toulouse, Toulouse 31000, France.
Environ Sci Technol ; 55(14): 10164-10174, 2021 07 20.
Article en En | MEDLINE | ID: mdl-34213316
Mass-independent fractionation (MIF) of stable even mass number mercury (Hg) isotopes is observed in rainfall and gaseous elemental Hg0 globally and is used to quantify atmospheric Hg deposition pathways. The chemical reaction and underlying even-Hg MIF mechanism are unknown however and speculated to be caused by Hg photo-oxidation on aerosols at the tropopause. Here, we investigate the Hg isotope composition of free tropospheric Hg0 and oxidized HgII forms at the high-altitude Pic du Midi Observatory. We find that gaseous oxidized Hg has positive Δ199Hg, Δ201Hg, and Δ200Hg and negative Δ204Hg signatures, similar to rainfall Hg, and we document rainfall Hg Δ196Hg to be near zero. Cloud water and rainfall Hg show an enhanced odd-Hg MIF of 0.3‰ compared to gaseous oxidized HgII, potentially indicating the occurrence of in-cloud aqueous HgII photoreduction. Diurnal MIF observations of free tropospheric Hg0 show how net Hg0 oxidation in high-altitude air masses leads to opposite even- and odd-MIF in Hg0 and oxidized HgII. We speculate that even-Hg MIF takes place by a molecular magnetic isotope effect during HgII photoreduction on aerosols that involves magnetic halogen nuclei. A Δ200Hg mass balance suggests that global Hg deposition pathways in models are likely biased toward HgII deposition. We propose that Hg cycling models could accommodate the Hg-isotope constraints on emission and deposition fluxes.
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Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: Mercurio Idioma: En Revista: Environ Sci Technol Año: 2021 Tipo del documento: Article País de afiliación: Francia Pais de publicación: Estados Unidos

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: Mercurio Idioma: En Revista: Environ Sci Technol Año: 2021 Tipo del documento: Article País de afiliación: Francia Pais de publicación: Estados Unidos