posted on 2021-05-07, 17:36authored byVeronika Pospisilova, David M. Bell, Houssni Lamkaddam, Amelie Bertrand, Liwei Wang, Deepika Bhattu, Xueqin Zhou, Josef Dommen, Andre S.H. Prevot, Urs Baltensperger, Imad El Haddad, Jay G. Slowik
Atmospheric secondary organic aerosol
(SOA) undergoes chemical
and physical changes when exposed to UV radiation, affecting the atmospheric
lifetime of the involved molecules. However, these photolytic processes
remain poorly constrained. Here, we present a study aimed at characterizing,
at a molecular level and in real time, the chemical composition of
α-pinene SOA exposed to UV-A light at 50% relative humidity
in an atmospheric simulation chamber. Significant SOA mass loss is
observed at high loadings (∼100 μg m–3), whereas the effect is less prevalent at lower loadings (∼20
μg m–3). For the vast majority of molecules
measured by the extractive electrospray time-of-flight mass spectrometer,
there is a fraction that is photoactive and decays when exposed to
UV-A radiation and a fraction that appears photorecalcitrant. The
molecules that are most photoactive contain between 4 and 6 oxygen
atoms, while the more highly oxygenated compounds and dimers do not
exhibit significant decay. Overall, photolysis results in a reduction
of the volatility of SOA, which cannot be explained by simple evaporative
losses but requires either a change in volatility related to changes
in functional groups or a change in physical parameters (i.e., viscosity).