posted on 2022-09-02, 19:44authored bySteven J. Campbell, Kate Wolfer, Peter J. Gallimore, Chiara Giorio, Daniel Häussinger, Marc-Aurèle Boillat, Markus Kalberer
The ozonolysis of alkenes contributes substantially to
the formation
of secondary organic aerosol (SOA), which are important modulators
of air quality and the Earth’s climate. Criegee intermediates
(CIs) are abundantly formed through this reaction. However, their
contributions to aerosol particle chemistry remain highly uncertain.
In this work, we present the first application of a novel methodology,
using spin traps, which simultaneously quantifies CIs produced from
the ozonolysis of volatile organic compounds in the gas and particle
phases. Only the smallest CI with one carbon atom was detected in
the gas phase of a β-caryophyllene ozonolysis reaction system.
However, multiple particle-bound CIs were observed in β-caryophyllene
SOA. The concentration of the most abundant CI isomer in the particle
phase was estimated to constitute ∼0.013% of the SOA mass under
atmospherically relevant conditions. We also demonstrate that the
lifetime of CIs in highly viscous SOA particles is at least on the
order of minutes, substantially greater than their gas-phase lifetime.
The confirmation of substantial concentrations of large CIs with elongated
lifetimes in SOA raises new questions regarding their influence on
the chemical evolution of viscous SOA particles, where CIs may be
a previously underestimated source of reactive species.