Atmospheric evolution of organic aerosol

We report here results of an experimental study of the OH‐initiated oxidation of solid organics in the presence of O2, NOx and H2O, using two kinds of self‐assembled organic monolayers (alkane and aromatic), paraffin and pyrene films as proxies for organic aerosol. We show that the OH‐initiated oxid...

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Bibliographic Details
Published in:Geophysical research letters Vol. 31; no. 22; pp. L22104 - n/a
Main Authors: Molina, M. J., Ivanov, A. V., Trakhtenberg, S., Molina, L. T.
Format: Journal Article
Language:English
Published: American Geophysical Union 01-11-2004
Blackwell Publishing Ltd
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Summary:We report here results of an experimental study of the OH‐initiated oxidation of solid organics in the presence of O2, NOx and H2O, using two kinds of self‐assembled organic monolayers (alkane and aromatic), paraffin and pyrene films as proxies for organic aerosol. We show that the OH‐initiated oxidation of the alkane surfaces leads to rapid volatilization. The gas‐phase products detected include HO2, H2O2, CO, CO2, HCO, CH2O, CH3CHO, CH3OH, and HCOOH. We conclude that volatilization is at least as efficient as wet deposition as a removal process for aliphatic particulates, whereas aromatic particulates show higher stability towards volatilization.
Bibliography:istex:B554D57F8B645B255F1EF412E4B04E10284A4C94
ArticleID:2004GL020910
ark:/67375/WNG-C0B0RQ9X-5
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
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ISSN:0094-8276
1944-8007
DOI:10.1029/2004GL020910