Chemical Characterisation of Benzene Oxidation Products Under High- and Low-Nox Conditions Using Chemical Ionisation Mass Spectrometry

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Chemical Characterisation of Benzene Oxidation Products Under High- and Low-Nox Conditions Using Chemical Ionisation Mass Spectrometry Atmos. Chem. Phys., 21, 3473–3490, 2021 https://doi.org/10.5194/acp-21-3473-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Chemical characterisation of benzene oxidation products under high- and low-NOx conditions using chemical ionisation mass spectrometry Michael Priestley1,6, Thomas J. Bannan1, Michael Le Breton1,d, Stephen D. Worrall1,c, Sungah Kang2, Iida Pullinen2,b, Sebastian Schmitt2, Ralf Tillmann2, Einhard Kleist7, Defeng Zhao2,g, Jürgen Wildt2,7, Olga Garmash4, Archit Mehra1,f, Asan Bacak1,e, Dudley E. Shallcross3,5, Astrid Kiendler-Scharr2, Åsa M. Hallquist8, Mikael Ehn4, Hugh Coe1, Carl J. Percival1,a, Mattias Hallquist6, Thomas F. Mentel2, and Gordon McFiggans1 1Centre for Atmospheric Science, Department of Earth and Environmental Sciences, University of Manchester, Manchester, UK 2Institut für Energie und Klimaforschung, IEK-8, Forschungszentrum Jülich, Jülich, Germany 3School of Chemistry, University of Bristol, Cantock’s Close, Bristol, UK 4Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland 5Department of Chemistry, University of the Western Cape, Bellville, South Africa 6Department of Chemistry and Molecular Biology, University of Gothenburg, Gothenburg, Sweden 7Institut für Bio- und Geowissenschaften, IBG-2, Forschungszentrum Jülich GmbH, Jülich, Germany 8IVL Swedish Environmental Research Institute, Gothenburg, Sweden anow at: Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA, USA bnow at: Department of Applied Physics, University of Eastern Finland, Kuopio, Finland cnow at: Aston Institute of Materials Research, School of Engineering and Applied Science, Aston University, Birmingham, UK dnow at: Volvo Group Trucks Technology, L3 Lundby, Gothenburg, Sweden enow at: Turkish Accelerator & Radiation Laboratory, Ankara University, Institute of Accelerator, Technologies Gölba¸sıCampus, Golbasi, Ankara, Turkey fnow at: Faculty of Science and Engineering, University of Chester, Chester, UK gnow at: Department of Atmospheric and Oceanic Sciences & Institute of Atmospheric Sciences, Fudan University, Shanghai, China Correspondence: Michael Priestley ([email protected]) Received: 4 August 2020 – Discussion started: 17 August 2020 Revised: 23 November 2020 – Accepted: 3 January 2021 – Published: 5 March 2021 Abstract. Aromatic hydrocarbons are a class of volatile or- under high- and low-NOx conditions, where a range of or- ganic compounds associated with anthropogenic activity and ganic oxidation products were detected. The nitrate scheme make up a significant fraction of urban volatile organic com- detects many oxidation products with high masses, ranging pound (VOC) emissions that contribute to the formation of from intermediate volatile organic compounds (IVOCs) to secondary organic aerosol (SOA). Benzene is one of the most extremely low volatile organic compounds (ELVOCs), in- abundant species emitted from vehicles, biomass burning and cluding C12 dimers. In comparison, very few species with industry. An iodide time-of-flight chemical ionisation mass C≥6 and O≥8 were detected with the iodide scheme, which spectrometer (ToF-CIMS) and nitrate ToF-CIMS were de- detected many more IVOCs and semi-volatile organic com- ployed at the Jülich Plant Atmosphere Chamber as part of pounds (SVOCs) but very few ELVOCs and low volatile or- a series of experiments examining benzene oxidation by OH ganic compounds (LVOCs). A total of 132 and 195 CHO Published by Copernicus Publications on behalf of the European Geosciences Union. 3474 M. Priestley et al.: Chemical characterisation of benzene oxidation products and CHON oxidation products are detected by the iodide al., 2010; Ruchirawat et al., 2005, 2007), benzene is photo- ToF-CIMS in the low- and high-NOx experiments respec- chemically active and contributes to the formation of ozone tively. Ring-breaking products make up the dominant frac- (O3) and secondary organic aerosol (SOA), both of which tion of detected signal and 21 and 26 of the products listed in act to modify the climate and contribute to poor air quality the Master Chemical Mechanism (MCM) were detected. The (Henze et al., 2008; Ng et al., 2007). SOA formation from time series of highly oxidised (O≥6) and ring-retaining oxi- benzene has previously been quantified with a focus on the dation products (C6 and double-bond equivalent D 4) equili- contribution from smaller mass, ring-breaking reaction prod- brate quickly, characterised by a square form profile, com- ucts such as epoxides (Glowacki et al., 2009) and dicarbonyl pared to MCM and ring-breaking products which increase aldehydes (e.g. O’Brien et al., 1983; Johnson et al., 2005). throughout oxidation, exhibiting sawtooth profiles. Under For example, 37 % of the glyoxal formed in the LA basin low-NOx conditions, all CHO formulae attributed to radical is estimated to derive from aromatic sources (Knote et al., termination reactions of first-generation benzene products, 2014). These smaller ring-breaking products typically make and first-generation auto-oxidation products are observed. up a larger fraction of SOA mass than the ring-retaining prod- Several N-containing species that are either first-generation ucts (Borrás and Tortajada-Genaro, 2012) and so have tradi- benzene products or first-generation auto-oxidation products tionally been the main focus for SOA quantification. Other are also observed under high-NOx conditions. Hierarchical major, toxic benzene oxidation products such as catechol, ni- cluster analysis finds four clusters, of which two describe trophenol and maleic anhydride are also known components photo-oxidation. Cluster 2 shows a negative dependency on of SOA (Borrás and Tortajada-Genaro, 2012). the NO2=NOx ratio, indicating it is sensitive to NO con- More recently the auto-oxidation mechanism has been centration and thus likely to contain NO addition products demonstrated to occur in aromatic systems (Wang et al., and alkoxy-derived termination products. This cluster has the 2017, 2020; Molteni et al., 2018; Tsiligiannis et al., 2019; highest average carbon oxidation state (OSC/ and the low- Garmash et al., 2020; Mehra et al., 2020), producing highly est average carbon number. Where nitrogen is present in a oxygenated organic molecules (HOMs, defined as contain- cluster member of cluster 2, the oxygen number is even, ing 6 or more oxygen atoms which is a product of the auto- as expected for alkoxy-derived products. In contrast, clus- oxidation mechanism) and incorporating up to 11 oxygen ter 1 shows no dependency on the NO2=NOx ratio and so is atoms (Bianchi et al., 2019). The auto-oxidation mechanism likely to contain more NO2 addition and peroxy-derived ter- of intra-molecular H shifts from the carbon backbone to the mination products. This cluster contains fewer fragmented peroxy radical centre forming peroxide groups is consistent species, as the average carbon number is higher and OSC with other VOC systems (Rissanen et al., 2014) initiated lower than cluster 2, and more species with an odd number by a variety of different oxidants (e.g. Mentel et al., 2015; of oxygen atoms. This suggests that clustering of time series Berndt et al., 2016). The inclusion of an alkyl group to a which have features pertaining to distinct chemical regimes, benzene ring facilitates HOM formation (Wang et al., 2017) for example, NO2=NOx perturbations, coupled with a priori as a consequence of the greater degrees of freedom afforded knowledge, can provide insight into identification of poten- to the molecule. Whilst benzene is not the most reactive tial functionality. of aromatic VOCs, τOH ≈ 9:5 d for benzene vs. τOH ≈ 6– 10 h for xylenes ([OH] D 2.0 × 106 molecules cm−3; Atkin- son and Arey, 2007), it is ubiquitous in the urban environ- ment and is the simplest C6 aromatic ring system to study. 1 Introduction Oxidation of benzene occurs nearly exclusively via hy- droxyl radical (OH) addition to form the cyclohexadienyl Benzene is an aromatic volatile organic compound (VOC) radical (benzene-OH adduct), which subsequently adds O2 commonly used as a vehicular fuel additive (Verma and Des to form the hydroxycyclohexadiene peroxy radical (C6H6– Tombe, 2002) and as a chemical intermediate in the man- OH–O2) (Volkamer et al., 2002) (Fig. 1). Two subsequent ufacture of a range of products, e.g. detergents (Oyoroko reaction pathways are postulated for this peroxy radical: ei- and Ogamba, 2017), lubricants (Rodriguez et al., 2018), dyes ther elimination of HO2 yields phenol, and secondary OH (Guo et al., 2018), and pesticides (Wang et al., 2014). Whilst attack must occur again, or an endocyclic di-oxygen-bridged current global estimates of benzenoid (molecules containing carbon-centred radical intermediate is formed by the addi- a benzene ring) emission to the atmosphere by vegetation are tion of the peroxy group to (typically) a β-carbon (Glowacki of a comparable order to those of anthropogenic activity (∼ 5 et al., 2009). This di-oxygen-bridged carbon-centred radical times lower; Misztal et al., 2015), and background concentra- may add another O2 and form a peroxy radical (named as tions of benzene are enhanced by increased biomass burning BZBIPERO2 in the Master Chemical Mechanism, MCM; (Archibald et al., 2015), emission of benzene to the urban at- Saunders et al., 2003). However it is not known if auto- mosphere is dominated by vehicle exhausts (Gentner et al., oxidation may continue to form a second oxygen-bridged 2012) and solvent evaporation (Hoyt and Raun, 2015). As radical, described as type II auto-oxidation (Molteni et al., well as a toxin (Snyder et al., 1975) and carcinogen (Bird et 2018; Fig. 1, BZBIPERO2-diB), or form a hydroperoxide Atmos. Chem. Phys., 21, 3473–3490, 2021 https://doi.org/10.5194/acp-21-3473-2021 M. Priestley et al.: Chemical characterisation of benzene oxidation products 3475 NO has been observed at Mace Head, Ireland, where clean low-NOx marine-influenced air can be contrasted with pol- luted NOx-containing continental air (Creasey et al., 2002). In that instance, an increase in NO concentration from 0.01 to 1 ppb reduces the HO2 V OH ratio from 200 V 1 to 10 V 1.
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