EGU21-1284
https://doi.org/10.5194/egusphere-egu21-1284
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Photooxidation and ozonolysis of Δ3-carene and its oxidation product caronaldehyde in the atmospheric simulation chamber SAPHIR

Luisa Hantschke, Anna Novelli, Birger Bohn, Changmin Cho, David Reimer, Ralf Tillmann, Franz Rohrer, Marvin Glowania, Andreas Hofzumahaus, Andreas Wahner, Astrid Kiendler-Scharr, and Hendrik Fuchs
Luisa Hantschke et al.
  • Forschungszentrum Jülich, Juelich, Germany (l.hantschke@fz-juelich.de)

Of the total global annual monoterpene emissions, Δ3-carene contributes 4.5 %, making it the 7th most abundant monoterpene worldwide. As it is primarily emitted by pine trees, Δ3-carene can regionally gain in importance, for example in boreal forests and Mediterranean regions.  Oxidation products of monoterpenes such as organic nitrates and aldehydes are known to impact the formation of secondary pollutants such as ozone and particles, so understanding their atmospheric formation and fate is crucial.

The photooxidation and ozonolysis of Δ3-carene and the photooxidation and photolysis of its main daytime photooxidation product caronaldehyde were investigated in the atmospheric simulation chamber SAPHIR. Oxidation reactions were studied under atmospheric conditions with high (> 8 ppbv) and low (< 2 ppbv) NOx concentrations. Reaction rate constants of the reaction of Δ3-carene with OH and O3, and of the reaction of caronaldehyde with OH as well as photolysis frequencies of caronaldehyde were determined. Production and destruction rates of the sum of hydroxyl and peroxy radicals (ROx = OH+HO2+RO2) were analysed to determine if there were unaccounted production and loss processes of radicals in the oxidation of Δ3-carene. The yield of Δ3-carene’s oxidation product caronaldehyde was determined from measured timeseries from OH photooxidation and ozonolysis experiments. Additionally, the OH yield from ozonolysis of Δ3-carene was determined.

Organic nitrate (RONO2) yields of the reaction of RO2 + NO, from RO2 produced from the reactions of Δ3-carene and caronaldehyde with OH were determined by analyzing the reactive nitrogen species (NOy) in the chamber.

How to cite: Hantschke, L., Novelli, A., Bohn, B., Cho, C., Reimer, D., Tillmann, R., Rohrer, F., Glowania, M., Hofzumahaus, A., Wahner, A., Kiendler-Scharr, A., and Fuchs, H.: Photooxidation and ozonolysis of Δ3-carene and its oxidation product caronaldehyde in the atmospheric simulation chamber SAPHIR, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-1284, https://doi.org/10.5194/egusphere-egu21-1284, 2021.

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