Evaluation of the chemical composition of gas- and particle-phase products of aromatic oxidation
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Published:2020-08-21
Issue:16
Volume:20
Page:9783-9803
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Mehra ArchitORCID, Wang Yuwei, Krechmer Jordan E.ORCID, Lambe Andrew, Majluf Francesca, Morris Melissa A., Priestley MichaelORCID, Bannan Thomas J.ORCID, Bryant Daniel J.ORCID, Pereira Kelly L.ORCID, Hamilton Jacqueline F., Rickard Andrew R., Newland Mike J., Stark HaraldORCID, Croteau Philip, Jayne John T., Worsnop Douglas R., Canagaratna Manjula R., Wang LinORCID, Coe Hugh
Abstract
Abstract. Aromatic volatile organic compounds (VOCs) are key anthropogenic pollutants emitted to the atmosphere and are important for both ozone and secondary
organic aerosol (SOA) formation in urban areas. Recent studies have indicated that aromatic hydrocarbons may follow previously unknown oxidation
chemistry pathways, including autoxidation that can lead to the formation of highly oxidised products. In this study we evaluate the gas- and
particle-phase ions measured by online mass spectrometry during the hydroxyl radical oxidation of substituted C9-aromatic isomers
(1,3,5-trimethylbenzene, 1,2,4-trimethylbenzene, propylbenzene and isopropylbenzene) and a substituted polyaromatic hydrocarbon (1-methylnaphthalene) under low- and medium-NOx conditions. A time-of-flight chemical ionisation mass spectrometer (ToF-CIMS) with iodide–anion ionisation was used with a filter inlet for gases and aerosols
(FIGAERO) for the detection of products in the particle phase, while a Vocus proton-transfer-reaction mass spectrometer (Vocus-PTR-MS) was used for the
detection of products in the gas phase. The signal of product ions observed in the mass spectra were compared for the different precursors and
experimental conditions. The majority of mass spectral product signal in both the gas and particle phases comes from ions which are common to all
precursors, though signal distributions are distinct for different VOCs. Gas- and particle-phase composition are distinct from one another. Ions
corresponding to products contained in the near-explicit gas phase Master Chemical Mechanism (MCM version 3.3.1) are utilised as a benchmark of current
scientific understanding, and a comparison of these with observations shows that the MCM is missing a range of highly oxidised products from its
mechanism. In the particle phase, the bulk of the product signal from all precursors comes from ring scission ions, a large proportion of which are more oxidised
than previously reported and have undergone further oxidation to form highly oxygenated organic molecules (HOMs). Under the perturbation of OH oxidation
with increased NOx, the contribution of HOM-ion signals to the particle-phase signal remains elevated for more substituted
aromatic precursors. Up to 43 % of product signal comes from ring-retaining ions including HOMs; this is most important for the more
substituted aromatics. Unique products are a minor component in these systems, and many of the dominant ions have ion formulae concurrent with other
systems, highlighting the challenges in utilising marker ions for SOA.
Funder
Natural Environment Research Council Newton Fund
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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