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Volume 17, issue 10
Atmos. Chem. Phys., 17, 6373–6391, 2017
https://doi.org/10.5194/acp-17-6373-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 17, 6373–6391, 2017
https://doi.org/10.5194/acp-17-6373-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 29 May 2017

Research article | 29 May 2017

Chemical and isotopic composition of secondary organic aerosol generated by α-pinene ozonolysis

Carl Meusinger et al.

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Aggarwal, S. G. and Kawamura, K.: Molecular distributions and stable carbon isotopic compositions of dicarboxylic acids and related compounds in aerosols from Sapporo, Japan: Implications for photochemical aging during long-range atmospheric transport, J. Geophys. Res. Atmos., 113, D14301, https://doi.org/10.1029/2007JD009365, 2008.
Andreae, M. O. and Crutzen, P. J.: Atmospheric Aerosols: Biogeochemical Sources and Role in Atmospheric Chemistry, Science, 276, 1052–1058, https://doi.org/10.1126/science.276.5315.1052, 1997.
Bayle, K., Akoka, S., Remaud, G. S., and Robins, R. J.: Non-Statistical 13C Distribution during Carbon Transfer from Glucose to Ethanol During Fermentation is Determined by the Catabolic Pathway Exploited, J. Biol. Chem., 290, 4118–4128, https://doi.org/10.1074/jbc.M114.621441, 2014a.
Bayle, K., Gilbert, A., Julien, M., Yamada, K., Silvestre, V., Robins, R. J., Akoka, S., Yoshida, N., and Remaud, G. S.: Conditions to obtain precise and true measurements of the intramolecular 13C distribution in organic molecules by isotopic 13C nuclear magnetic resonance spectrometry, Anal. Chim. Acta., 846, 1–7, https://doi.org/10.1016/j.aca.2014.07.018, 2014b.
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Isotope studies can constrain budgets of secondary organic aerosol (SOA) that is pivotal to air pollution and climate. SOA from α-pinene ozonolysis was found to be enriched in 13C relative to the precursor. The observed difference in 13C between the gas and particle phases may arise from isotope-dependent changes in branching ratios. Alternatively, some gas-phase products involve carbon atoms from highly enriched and depleted sites, giving a non-kinetic origin to the observed fractionations.
Isotope studies can constrain budgets of secondary organic aerosol (SOA) that is pivotal to air...
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