Secondary organic aerosol (SOA) plays a crucial role in influencing 20 both climate and air
21 quality, and therefore characterizing SOA formation and evolution pathways has been a major
22 research goal over the last decades. To reach this goal, especially relating to reactions occurring in
23 the particle phase, real-time comprehensive molecular-level characterization of SOA composition is
24 required, yet rarely achieved. Here, utilizing state-of-the-art high-resolution mass spectrometry
25 techniques, we deduce important new reaction pathways for the formation and subsequent
26 transformation of SOA in the boreal atmosphere. Our detailed molecular characterization of particle27
phase organics helped identify various compound classes from the oxidation of monoterpenes,
28 including previously reported highly oxygenated molecules (HOMs). Our results suggest that many
29 compounds, and HOMs in particular, undergo further reactions in the particle phase, accelerated by
30 acidic aerosols. Coincident formation of products with higher degree of unsaturation and lower O:C
31 ratios was observed and attributed to high-molecular weight oligomers. Targeted smog chamber
32 experiments confirmed the ambient observations and revealed that monoterpene oxidation products,
33 such as aldehydes, undergo acid-catalyzed heterogeneous reactions yielding oligomers. While the
34 aerosol acidity strongly affected the chemical composition and properties of a-pinene–derived SOA,
35 aerosol liquid water alone had nearly negligible impact. Our findings provide a comprehensive picture
36 of particle-phase processing governing monoterpene-derived SOA composition and highlight the
37 underestimated role of aerosol acidity in SOA evolution and oligomer formation.
38
Revised: November 9, 2020 |
Published: January 11, 2019
Citation
Riva M., L.M. Heikkinen, D.M. Bell, O.J. Perakyla, Q. Zha, S. Schallhart, and M.P. Rissanen, et al. 2019.Chemical transformations in monoterpene-derived organic aerosol enhanced by inorganic composition.npj Climate and Atmospheric Science 2.PNNL-SA-131773.doi:10.1038/s41612-018-0058-0