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Título

On the Speciation of Iodine in Marine Aerosol

AutorGómez Martín, Juan Carlos CSIC ORCID ; Saiz-Lopez, A. CSIC ORCID; Cuevas, Carlos A. CSIC ORCID; Baker, Alex R.; Fernández, Rafael P. CSIC ORCID
Palabras claveIodine chemistry
Aerosol composition
Fecha de publicación27-feb-2022
EditorAmerican Geophysical Union
CitaciónJournal of Geophysical Research - Part D - Atmospheres 127(4): e2021JD036081 (2022)
ResumenWe have compiled and analyzed a comprehensive data set of field observations of iodine speciation in marine aerosol. The soluble iodine content of fine aerosol (PM1) is dominated by soluble organic iodine (SOI; ∼50%) and iodide (∼30%), while the coarse fraction is dominated by iodate (∼50%), with nonnegligible amounts of iodide (∼20%). The SOI fraction shows an equatorial maximum and minima coinciding with the ocean “deserts,” which suggests a link between soluble iodine speciation in aerosol and ocean productivity. Among the major aerosol ions, organic anions and non-sea-salt sulfate show positive correlations with SOI in PM1. Alkali cations are positively correlated to iodate and negatively correlated with SOI and iodide in coarse aerosol. These relationships suggest that under acidic conditions iodate is reduced to HOI, which reacts with organic matter to form SOI, a possible source of iodide. In less acidic sea-salt or dust-rich coarse aerosols, HOI oxidation to iodate and reaction with organic matter likely compete. © 2022 The Authors.
DescripciónThis is an open access article under the terms of the Creative Commons Attribution-NonCommercial License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes.
Versión del editorhttp://dx.doi.org/10.1029/2021JD036081
URIhttp://hdl.handle.net/10261/273212
DOI10.1029/2021JD036081
ISSN2169-897X
E-ISSN2169-8996
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