Modeling the influence of chain length on secondary organic aerosol (SOA) formation via multiphase reactions of alkanes
-
Published:2023-01-27
Issue:2
Volume:23
Page:1661-1675
-
ISSN:1680-7324
-
Container-title:Atmospheric Chemistry and Physics
-
language:en
-
Short-container-title:Atmos. Chem. Phys.
Author:
Madhu Azad, Jang MyoseonORCID, Deacon David
Abstract
Abstract. Secondary organic aerosol (SOA) from diesel fuel is known to be
significantly sourced from the atmospheric oxidation of aliphatic
hydrocarbons. In this study, the formation of linear alkane SOA was
predicted using the Unified Partitioning Aerosol Phase Reaction (UNIPAR)
model that simulated multiphase reactions of hydrocarbons. In the model, the
formation of oxygenated products from the photooxidation of linear alkanes
was simulated using a nearly explicit gas kinetic mechanism. Autoxidation
paths integrated with alkyl peroxy radicals were added to the Master
Chemical Mechanism v3.3.1 to improve the prediction of low-volatility
products in the gas phase and SOA mass. The resulting gas products were then
lumped into volatility- and reactivity-based groups that are linked to mass-based
stoichiometric coefficients. The SOA mass in the UNIPAR model is produced
via three major pathways: partitioning of gaseous oxidized products onto
both the organic and wet inorganic phases, oligomerization in the organic phase,
and reactions in the wet inorganic phase (acid-catalyzed oligomerization and
organosulfate formation). The model performance was demonstrated for SOA
data that were produced through the photooxidation of a homologous series of
linear alkanes ranging from C9–C15 under varying environments (NOx
levels and inorganic seed conditions) in a large outdoor photochemical smog
chamber. The product distributions of linear alkanes were mathematically
predicted as a function of carbon number using an incremental volatility
coefficient (IVC) to cover a wide range of alkane lengths. The prediction of
alkane SOA using the incremental volatility-based product distributions,
which were obtained with C9–C12 alkanes, was evaluated for C13
and C15 chamber data and further extrapolated to predict the SOA from longer-chain alkanes (≥ C15) that can be found in diesel. The model simulation
of linear alkanes in diesel fuel suggests that SOA mass is mainly produced
by alkanes C15 and higher. Alkane SOA is insignificantly impacted by the
reactions of organic species in the wet inorganic phase due to the
hydrophobicity of products but significantly influenced by gas–particle
partitioning.
Funder
National Institute of Environmental Research Center for Selective C-H Functionalization, National Science Foundation National Research Foundation of Korea
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference59 articles.
1. Abraham, M. H. and McGowan, J. C.: The Use of Characteristic Volumes to
Measure Cavity Terms in Reversed Phase Liquid Chromatography,
Chromatographia, 23, 243–246, 1987. 2. Abraham, M. H., Whiting, G. S., Doherty, R. M., and Shuely, W. J.: Hydrogen
bonding: XVI, A new solute salvation parameter, π2H, from gas
chromatographic data, J. Chromatogr. A, 587, 213–228,
https://doi.org/10.1016/0021-9673(91)85158-C, 1991. 3. 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. 4. Beardsley, R. L. and Jang, M.: Simulating the SOA formation of isoprene from
partitioning and aerosol phase reactions in the presence of inorganics,
Atmos. Chem. Phys., 16, 5993–6009, https://doi.org/10.5194/acp-16-5993-2016, 2016. 5. Bianchi, F., Kurtén, T., Riva, M., Mohr, C., Rissanen, M. P., Roldin,
P., Berndt, T., Crounse, J. D., Wennberg, P. O., Mentel, T. F., Wildt, J.,
Junninen, H., Jokinen, T., Kulmala, M., Worsnop, D. R., Thornton, J. A.,
Donahue, N., Kjaergaard, H. G., and Ehn, M.: Highly Oxygenated Organic
Molecules (HOM) from Gas-Phase Autoxidation Involving Peroxy Radicals: A Key
Contributor to Atmospheric Aerosol, Chem. Rev., 119, 3472–3509,
https://doi.org/10.1021/acs.chemrev.8b00395, 2019.
Cited by
2 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|