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Formation of secondary light-absorbing "fulvic-like" oligomers: A common process in aqueous and ionic atmospheric aerosols ?
Stockholm University, Faculty of Science, Department of Meteorology.
Department of Organic Chemistry.
Department of Organic Chemistry.
2007 (English)In: Geophysical Research Letters, ISSN 0094-8276, Vol. 34, no L21812, 1-5 p.Article in journal (Refereed) Published
Abstract [en]

Secondary Organic Aerosols (SOA), produced by the transformation of organic gases in the atmosphere, have received a considerable amount of attention over the last three decades because of their expected roles in urban pollution, global aerosol loadings, and cloud formation. While most investigations have been performed under controlled conditions such as smog chambers, atmospheric observations of SOA are sparse, mostly indirect, and critically limit the knowledge of these aerosols. In particular, techniques for the specific observation of the secondary organic fraction of aerosols in the atmosphere need to be developed, and seem today the most likely pathways to make significant progress in this topic.

Place, publisher, year, edition, pages
2007. Vol. 34, no L21812, 1-5 p.
National Category
Meteorology and Atmospheric Sciences
URN: urn:nbn:se:su:diva-21768DOI: doi:10.1029/2007GL031300OAI: diva2:188295
Available from: 2008-01-28 Created: 2008-01-28 Last updated: 2011-01-11Bibliographically approved

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Nozière, BarbaraDziedzic, PawelCórdova, Armando
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