6533b838fe1ef96bd12a3e7b
RESEARCH PRODUCT
Formation of 3-methyl-1,2,3-butanetricarboxylic acid via gas phase oxidation of pinonic acid – a mass spectrometric study of SOA aging
Ludovic MullerNeil M. DonahueThomas F. MentelThorsten HoffmannHarald SaathoffMarc-christopher ReinnigKarl-heinz Naumannsubject
540 Chemistry and allied sciencesAtmospheric ScienceChromatographyChemistryAtmospheric-pressure chemical ionizationFraction (chemistry)Mass spectrometryMass spectrometriclcsh:QC1-999JGas phaseAerosollcsh:ChemistryAcid oxidationlcsh:QD1-999540 ChemieYield (chemistry)ddc:550lcsh:Physicsdescription
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.
year | journal | country | edition | language |
---|---|---|---|---|
2012-01-01 | Atmospheric Chemistry and Physics |