Photodegradation of α-Pinene Secondary Organic Aerosol Dominated by Moderately Oxidized Molecules
Author(s) -
Veronika Pospíšilová,
David M. Bell,
Houssni Lamkaddam,
Amélie Bertrand,
Liwei Wang,
Deepika Bhattu,
Xueqin Zhou,
Josef Dommen,
Andrê S. H. Prévôt,
Urs Baltensperger,
Imad El Haddad,
Jay G. Slowik
Publication year - 2021
Publication title -
environmental science and technology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.851
H-Index - 397
eISSN - 1520-5851
pISSN - 0013-936X
DOI - 10.1021/acs.est.0c06752
Subject(s) - chemistry , aerosol , pinene , volatility (finance) , molecule , mass fraction , mass spectrometry , photodissociation , chemical composition , photochemistry , environmental chemistry , photodegradation , fraction (chemistry) , relative humidity , analytical chemistry (journal) , photocatalysis , organic chemistry , chromatography , meteorology , catalysis , financial economics , economics , physics
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).
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