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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
Atmos. Chem. Phys., 17, 2347-2357, 2017
https://doi.org/10.5194/acp-17-2347-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
14 Feb 2017
Formation of secondary organic aerosols from the ozonolysis of dihydrofurans
Yolanda Diaz-de-Mera1, Alfonso Aranda1, Larisa Bracco2, Diana Rodriguez3, and Ana Rodriguez3 1Universidad de Castilla-La Mancha, Facultad de Ciencias y Tecnologias Quimicas, Avenida Camilo José Cela s/n, 13071, Ciudad Real, Spain
2Instituto de Investigaciones Fisicoquímicas Teóricas y Aplicadas (INIFTA), Departamento de Química, Facultad de Ciencias Exactas, Universidad Nacional de La Plata, CONICET, Casilla de Correo 16, Sucursal 4, La Plata 1900, Argentina
3Universidad de Castilla-La Mancha, Facultad de Ciencias Ambientales y Bioquimica, Avenida Carlos III s/n, 45071 Toledo, Spain
Abstract. In this work we report the study of the ozonolysis of 2,5-dihydrofuran and 2,3-dihydrofuran and the reaction conditions leading to the formation of secondary organic aerosols. The reactions have been carried out in a Teflon chamber filled with synthetic air mixtures at atmospheric pressure and room temperature. The ozonolysis only produced particles in the presence of SO2. Rising relative humidity from 0 to 40 % had no effect on the production of secondary organic aerosol in the case of 2,5-dihydrofuran, while it reduced the particle number and particle mass concentrations from the 2,3-dihydrofuran ozonolysis. The water-to-SO2 rate constant ratio for the 2,3-dihydrofuran Criegee intermediate was derived from the secondary organic aerosol (SOA) yields in experiments with different relative humidity values, kH2O/kSO2 =  (9.8 ± 3.7) × 10−5.

The experimental results show that SO3 may not be the only intermediate involved in the formation or growth of new particles in contrast to the data reported for other Criegee intermediate–SO2 reactions. For the studied reactions, SO2 concentrations remained constant during the experiments, behaving as a catalyst in the production of condensable products.

Computational calculations also show that the stabilised Criegee intermediates from the ozonolysis reaction of both 2,5-dihydrofuran and 2,3-dihydrofuran may react with SO2, resulting in the regeneration of SO2 and the formation of low-volatility organic acids.


Citation: Diaz-de-Mera, Y., Aranda, A., Bracco, L., Rodriguez, D., and Rodriguez, A.: Formation of secondary organic aerosols from the ozonolysis of dihydrofurans, Atmos. Chem. Phys., 17, 2347-2357, https://doi.org/10.5194/acp-17-2347-2017, 2017.
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Short summary
Criegee intermediates are involved in the formation of secondary organic aerosols. How? Recent works show that they contribute to the oxidation of SO2 to SO3. We have found that the studied ozonolysis reactions only led to nucleation in the presence of SO2, which behaved as a catalyst. So the role of SO2 to form SOA depends on the structure of the alkene. For these reactions, the formation of low-volatility organic acid is expected to be responsible for nucleation, since SO3 was not released.
Criegee intermediates are involved in the formation of secondary organic aerosols. How? Recent...
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