Observations of speciated isoprene nitrates in Beijing: implications for isoprene chemistry
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Published:2021-04-27
Issue:8
Volume:21
Page:6315-6330
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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:
Reeves Claire E.ORCID, Mills Graham P., Whalley Lisa K., Acton W. Joe F., Bloss William J.ORCID, Crilley Leigh R.ORCID, Grimmond SueORCID, Heard Dwayne E.ORCID, Hewitt C. NicholasORCID, Hopkins James R.ORCID, Kotthaus SimoneORCID, Kramer Louisa J.ORCID, Jones Roderic L., Lee James D.ORCID, Liu Yanhui, Ouyang Bin, Slater Eloise, Squires FreyaORCID, Wang XinmingORCID, Woodward-Massey Robert, Ye ChunxiangORCID
Abstract
Abstract. Isoprene is the most important biogenic volatile organic
compound in the atmosphere. Its calculated impact on ozone (O3) is
critically dependent on the model isoprene oxidation chemical scheme, in
particular the way the isoprene-derived organic nitrates (IN) are treated.
By combining gas chromatography with mass spectrometry, we have developed a
system capable of separating and unambiguously measuring individual IN
isomers. In this paper we use measurements from its first field deployment,
which took place in Beijing as part of the Atmospheric Pollution and Human
Health in a Chinese Megacity programme, to test understanding of the
isoprene chemistry as simulated in the Master Chemical Mechanism (MCM)
(v.3.3.1). Seven individual isoprene nitrates were identified and quantified
during the campaign: two β-hydroxy nitrates (IHN), four δ-carbonyl nitrates (ICN), and propanone nitrate. Our measurements show that in the summertime conditions experienced in
Beijing the ratio of (1-OH, 2-ONO2)-IHN to (4-OH, 3-ONO2)-IHN (the
numbers indicate the carbon atom in the isoprene chain to which the radical
is added) increases at NO mixing ratios below 2 ppb. This provides
observational field evidence of the redistribution of the peroxy radicals
derived from OH oxidation of isoprene away from the kinetic ratio towards a
new thermodynamic equilibrium consistent with box model calculations. The
observed amounts of δ-ICN demonstrate the importance of daytime
addition of NO3 to isoprene in Beijing but suggest that the predominant
source of the δ-ICN in the model (reaction of NO with δ-nitrooxy peroxy radicals) may be too large. Our speciated measurements of
the four δ-ICN exhibit a mean C1 : C4 isomer ratio of 1.4 and a mean
trans : cis isomer ratio of 7 and provide insight into the isomeric distribution of the
δ-nitrooxy peroxy radicals. Together our measurements and model
results indicate that propanone nitrate was formed from the OH oxidation of
δ-ICN both during the day and night, as well as from NO3
addition to propene at night. This study demonstrates the value of speciated IN measurements in testing
understanding of the isoprene degradation chemistry and shows how more
extensive measurements would provide greater constraints. It highlights
areas of the isoprene chemistry that warrant further study, in particular
the impact of NO on the formation of the IHN and the NO3-initiated
isoprene degradation chemistry, as well as the need for further laboratory
studies on the formation and the losses of IN, in particular via photolysis
of δ-ICN and hydrolysis.
Funder
Natural Environment Research Council Medical Research Council National Natural Science Foundation of China
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference32 articles.
1. Bates, K. H. and Jacob, D. J.: A new model mechanism for atmospheric oxidation of isoprene: global effects on oxidants, nitrogen oxides, organic products, and secondary organic aerosol, Atmos. Chem. Phys., 19, 9613–9640, https://doi.org/10.5194/acp-19-9613-2019, 2019. 2. Bew, S. P., Hiatt-Gipson, G. D., Mills, G. P., and Reeves, C. E.: Efficient
syntheses of climate impacting isoprene nitrates and (1R,5S)-(-)-myrtenol
nitrate, Beilstein J. Org. Chem., 12, 1081–1095, https://doi.org/10.3762/bjoc.12.103,
2016. 3. Emmerson, K. M. and Evans, M. J.: Comparison of tropospheric gas-phase chemistry schemes for use within global models, Atmos. Chem. Phys., 9, 1831–1845, https://doi.org/10.5194/acp-9-1831-2009, 2009. 4. Fiore, A. M., Horowitz, L. W., Purves, D. W., Levy II, H., Evans, M. J.,
Wang, Y., Li, Q., and Yantosca, R. M.: Evaluating the contribution of
changes in isoprene emissions to surface ozone trends over the eastern
United States, J. Geophys. Res., 110, D12303, https://doi.org/10.1029/2004JD005485,
2005. 5. Guenther, A. B., Jiang, X., Heald, C. L., Sakulyanontvittaya, T., Duhl, T., Emmons, L. K., and Wang, X.: The Model of Emissions of Gases and Aerosols from Nature version 2.1 (MEGAN2.1): an extended and updated framework for modeling biogenic emissions, Geosci. Model Dev., 5, 1471–1492, https://doi.org/10.5194/gmd-5-1471-2012, 2012.
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