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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 3 | Copyright
Atmos. Chem. Phys., 12, 1483-1496, 2012
https://doi.org/10.5194/acp-12-1483-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 08 Feb 2012

Research article | 08 Feb 2012

Formation of 3-methyl-1,2,3-butanetricarboxylic acid via gas phase oxidation of pinonic acid – a mass spectrometric study of SOA aging

L. Müller1, M.-C. Reinnig1, K. H. Naumann2, H. Saathoff2, T. F. Mentel3, N. M. Donahue4, and T. Hoffmann1 L. Müller et al.
  • 1Johannes Gutenberg-Universität, Institute for inorganic Chemistry and analytical Chemistry, Duesbergweg 10–14, 55128 Mainz, Germany
  • 2Karlsruhe Institute of Technology Institute for Meteorology and Climate Research (IMK-AAF), Hermann-von-Helmholtz-Platz 1, 76344 Eggenstein-Leopoldshafen, Germany
  • 3Forschungszentrum Jülich GmbH, ICG-2: Troposphäre, 52425 Jülich, Germany
  • 4Carnegie Mellon University Department of Chemical Engineering, 5000 Forbes Avenue, Pittsburgh, PA 15213-3890, USA

Abstract. This paper presents the results of mass spectrometric investigations of the OH-initiated oxidative aging of α-pinene SOA under simulated tropospheric conditions at the large aerosol chamber facility AIDA, Karlsruhe Institute of Technology. In particular, the OH-initiated oxidation of pure pinic and pinonic acid, two well-known oxidation products of α-pinene, was investigated. Two complementary analytical techniques were used, on-line atmospheric pressure chemical ionization/mass spectrometry (APCI/MS) and filter sampling followed by liquid chromatography/mass spectrometry (LC/ESI-MS). The results show that 3-methyl-1,2,3-butanetricarboxylic acid (MBTCA), a very low volatile α-pinene SOA product and a tracer compound for terpene SOA, is formed from the oxidation of pinonic acid and that this oxidation takes place in the gas phase. This finding is confirmed by temperature-dependent aging experiments on whole SOA formed from α-pinene, in which the yield of MBTCA scales with the pinonic acid fraction in the gas phase. Based on the results, several feasible gas-phase radical mechanisms are discussed to explain the formation of MBTCA from OH-initiated pinonic acid oxidation.

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