Articles | Volume 16, issue 20
https://doi.org/10.5194/acp-16-13251-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-13251-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Transformation of logwood combustion emissions in a smog chamber: formation of secondary organic aerosol and changes in the primary organic aerosol upon daytime and nighttime aging
Department of Environmental and Biological Sciences, University of Eastern
Finland, P.O. Box 1627, 70211 Kuopio, Finland
Ari Leskinen
Department of Applied Physics, University of Eastern Finland, P.O. Box
1627, 70211 Kuopio, Finland
Finnish Meteorological Institute, P.O. Box 1627, 70211 Kuopio, Finland
Liqing Hao
Department of Applied Physics, University of Eastern Finland, P.O. Box
1627, 70211 Kuopio, Finland
Pasi Yli-Pirilä
Department of Environmental and Biological Sciences, University of Eastern
Finland, P.O. Box 1627, 70211 Kuopio, Finland
Department of Applied Physics, University of Eastern Finland, P.O. Box
1627, 70211 Kuopio, Finland
Miika Kortelainen
Department of Environmental and Biological Sciences, University of Eastern
Finland, P.O. Box 1627, 70211 Kuopio, Finland
Julija Grigonyte
Department of Environmental and Biological Sciences, University of Eastern
Finland, P.O. Box 1627, 70211 Kuopio, Finland
Jarkko Tissari
Department of Environmental and Biological Sciences, University of Eastern
Finland, P.O. Box 1627, 70211 Kuopio, Finland
Heikki Lamberg
Department of Environmental and Biological Sciences, University of Eastern
Finland, P.O. Box 1627, 70211 Kuopio, Finland
Anni Hartikainen
Department of Environmental and Biological Sciences, University of Eastern
Finland, P.O. Box 1627, 70211 Kuopio, Finland
Kari Kuuspalo
Department of Environmental and Biological Sciences, University of Eastern
Finland, P.O. Box 1627, 70211 Kuopio, Finland
Aki-Matti Kortelainen
Department of Applied Physics, University of Eastern Finland, P.O. Box
1627, 70211 Kuopio, Finland
Annele Virtanen
Department of Applied Physics, University of Eastern Finland, P.O. Box
1627, 70211 Kuopio, Finland
Kari E. J. Lehtinen
Department of Applied Physics, University of Eastern Finland, P.O. Box
1627, 70211 Kuopio, Finland
Finnish Meteorological Institute, P.O. Box 1627, 70211 Kuopio, Finland
Mika Komppula
Finnish Meteorological Institute, P.O. Box 1627, 70211 Kuopio, Finland
Simone Pieber
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute,
Villigen, Switzerland
André S. H. Prévôt
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute,
Villigen, Switzerland
Timothy B. Onasch
Aerodyne Research, Inc., Billerica, MA 08121, USA
Douglas R. Worsnop
Aerodyne Research, Inc., Billerica, MA 08121, USA
Hendryk Czech
Joint Mass Spectrometry Centre, University at Rostock, Institut für
Chemie, Lehrstuhl für Analytische Chemie, Dr.-Lorenz-Weg 1, 18059
Rostock, Germany
Ralf Zimmermann
Joint Mass Spectrometry Centre, University at Rostock, Institut für
Chemie, Lehrstuhl für Analytische Chemie, Dr.-Lorenz-Weg 1, 18059
Rostock, Germany
Joint Mass Spectrometry Centre, Cooperation Group Comprehensive
Molecular Analytics, Helmholtz Zentrum München, Germany
Helmholtz Virtual Institute of Complex Molecular Systems in
Environmental Health (HICE), Aerosols and Health, Neuherberg, Germany
Jorma Jokiniemi
Department of Environmental and Biological Sciences, University of Eastern
Finland, P.O. Box 1627, 70211 Kuopio, Finland
Olli Sippula
Department of Environmental and Biological Sciences, University of Eastern
Finland, P.O. Box 1627, 70211 Kuopio, Finland
Helmholtz Virtual Institute of Complex Molecular Systems in
Environmental Health (HICE), Aerosols and Health, Neuherberg, Germany
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Short summary
Real-time measurements of OA aging and SOA formation from logwood combustion were conducted under dark and UV oxidation. Substantial SOA formation was observed in all experiments, leading to twice the initial OA mass emphasizing the importance of the burning conditions for the aging processes. The results prove that emissions are subject to intensive chemical processing in the atmosphere; e.g. the most of the POA was found to become oxidized after the ozone addition, forming aged POA.
Real-time measurements of OA aging and SOA formation from logwood combustion were conducted...
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