The importance of sesquiterpene oxidation products for secondary organic aerosol formation in a springtime hemiboreal forest
Open Access
- 6 August 2021
- journal article
- research article
- Published by Copernicus GmbH in Atmospheric Chemistry and Physics
- Vol. 21 (15) , 11781-11800
Abstract
Secondary organic aerosols (SOAs) formed from biogenic volatile organic compounds (BVOCs) constitute a significant fraction of atmospheric particulate matter and have been recognized to significantly affect the climate and air quality. Atmospheric SOA particulate mass yields and chemical composition result from a complex mixture of oxidation products originating from a diversity of BVOCs. Many laboratory and field experiments have studied SOA particle formation and growth in the recent years. However, a large uncertainty still remains regarding the contribution of BVOCs to SOA. In particular, organic compounds formed from sesquiterpenes have not been thoroughly investigated, and their contribution to SOA remains poorly characterized. In this study, a Filter Inlet for Gases and Aerosols (FIGAERO) combined with a high-resolution time-of-flight chemical ionization mass spectrometer (CIMS), with iodide ionization, was used for the simultaneous measurement of gas-phase and particle-phase oxygenated compounds. The aim of the study was to evaluate the relative contribution of sesquiterpene oxidation products to SOA in a springtime hemiboreal forest environment. Our results revealed that monoterpene and sesquiterpene oxidation products were the main contributors to SOA particles. The chemical composition of SOA particles was compared for times when either monoterpene or sesquiterpene oxidation products were dominant and possible key oxidation products for SOA particle formation were identified for both situations. Surprisingly, sesquiterpene oxidation products were the predominant fraction in the particle phase in some periods, while their gas-phase concentrations remained much lower than those of monoterpene products. This can be explained by favorable and effective partitioning of sesquiterpene products into the particle phase. The SOA particle volatility determined from measured thermograms increased when the concentration of sesquiterpene oxidation products in SOA particles was higher than that of monoterpenes. Overall, this study demonstrates that sesquiterpenes may have an important role in atmospheric SOA formation and oxidation chemistry, in particular during the spring recovery period.Keywords
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Funding Information
- Research Council of Finland (310682)
- H2020 Societal Challenges
- Eesti Maaülikool (P180021, P180274)
- Eesti Teadusagentuur (3.2.0304.11-0395)
This publication has 62 references indexed in Scilit:
- Quantitative patterns between plant volatile emissions induced by biotic stresses and the degree of damageFrontiers in Plant Science, 2013
- Seasonal variation in vertical volatile compounds air concentrations within a remote hemiboreal mixed forestAtmospheric Chemistry and Physics, 2012
- A two-dimensional volatility basis set – Part 2: Diagnostics of organic-aerosol evolutionAtmospheric Chemistry and Physics, 2012
- Investigating the use of secondary organic aerosol as seed particles in simulation chamber experimentsAtmospheric Chemistry and Physics, 2011
- Second-generation products contribute substantially to the particle-phase organic material produced by β-caryophyllene ozonolysisAtmospheric Chemistry and Physics, 2011
- The formation, properties and impact of secondary organic aerosol: current and emerging issuesAtmospheric Chemistry and Physics, 2009
- Atmospheric Aerosols: Composition, Transformation, Climate and Health EffectsAngewandte Chemie International Edition, 2005
- Gas-phase tropospheric chemistry of biogenic volatile organic compounds: a reviewAtmospheric Environment, 2003
- Formation and gas/particle partitioning of monoterpenes photo‐oxidation products over forestsGeophysical Research Letters, 1999
- A global model of natural volatile organic compound emissionsJournal of Geophysical Research: Atmospheres, 1995