Articles | Volume 24, issue 9
https://doi.org/10.5194/acp-24-5549-2024
https://doi.org/10.5194/acp-24-5549-2024
Research article
 | 
14 May 2024
Research article |  | 14 May 2024

Secondary organic aerosols derived from intermediate-volatility n-alkanes adopt low-viscous phase state

Tommaso Galeazzo, Bernard Aumont, Marie Camredon, Richard Valorso, Yong B. Lim, Paul J. Ziemann, and Manabu Shiraiwa

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Cited articles

Aimanant, S. and Ziemann, P. J.: Chemical Mechanisms of Aging of Aerosol Formed from the Reaction of n-Pentadecane with OH Radicals in the Presence of NOx, Aerosol Sci. Technol., 47, 979–990, https://doi.org/10.1080/02786826.2013.804621, 2013a. 
Aimanant, S. and Ziemann, P. J.: Development of Spectrophotometric Methods for the Analysis of Functional Groups in Oxidized Organic Aerosol, Aerosol Sci. Technol., 47, 581–591, https://doi.org/10.1080/02786826.2013.773579, 2013b. 
Atkinson, R., Carter, W. P. L., Winer, A. M., and Pitts, J. N.: An Experimental Protocol for the Determination of OH Radical Rate Constants with Organics Using Methyl Nitrite Photolysis as an OH Radical Source, JAPCA J. Air Waste Ma., 31, 1090–1092, https://doi.org/10.1080/00022470.1981.10465331, 1981. 
Aumont, B., Szopa, S., and Madronich, S.: Modelling the evolution of organic carbon during its gas-phase tropospheric oxidation: development of an explicit model based on a self generating approach, Atmos. Chem. Phys., 5, 2497–2517, https://doi.org/10.5194/acp-5-2497-2005, 2005. 
Aumont, B., Valorso, R., Mouchel-Vallon, C., Camredon, M., Lee-Taylor, J., and Madronich, S.: Modeling SOA formation from the oxidation of intermediate volatility n-alkanes, Atmos. Chem. Phys., 12, 7577–7589, https://doi.org/10.5194/acp-12-7577-2012, 2012. 
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Short summary
Secondary organic aerosol (SOA) derived from n-alkanes is a major component of anthropogenic particulate matter. We provide an analysis of n-alkane SOA by chemistry modeling, machine learning, and laboratory experiments, showing that n-alkane SOA adopts low-viscous semi-solid or liquid states. Our results indicate few kinetic limitations of mass accommodation in SOA formation, supporting the application of equilibrium partitioning for simulating n-alkane SOA in large-scale atmospheric models.
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