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Changes in organic aerosol composition with aging inferred from aerosol mass spectra

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Ng, N. L., Canagaratna, M. R., Jimenez, J. L., Chhabra, P. S., Seinfeld, J. H., Worsnop, D. R.·2011·Atmospheric Chemistry and Physics

Abstract

Abstract. Organic aerosols (OA) can be separated with factor analysis of aerosol mass spectrometer (AMS) data into hydrocarbon-like OA (HOA) and oxygenated OA (OOA). We develop a new method to parameterize H:C of OOA in terms of f43 (ratio of m/z 43, mostly C2H3O+, to total signal in the component mass spectrum). Such parameterization allows for the transformation of large database of ambient OOA components from the f44 (mostly CO2+, likely from acid groups) vs. f43 space ("triangle plot") (Ng et al., 2010) into the Van Krevelen diagram (H:C vs. O:C) (Van Krevelen, 1950). Heald et al. (2010) examined the evolution of total OA in the Van Krevelen diagram. In this work total OA is deconvolved into components that correspond to primary (HOA and others) and secondary (OOA) organic aerosols. By deconvolving total OA into different components, we remove physical mixing effects between secondary and primary aerosols which allows for examination of the evolution of OOA components alone in the Van Krevelen space. This provides a unique means of following ambient secondary OA evolution that is analogous to and can be compared with trends observed in chamber studies of secondary organic aerosol formation. The triangle plot in Ng et al. (2010) indicates that f44 of OOA components increases with photochemical age, suggesting the importance of acid formation in OOA evolution. Once they are transformed with the new parameterization, the triangle plot of the OOA components from all sites occupy an area in Van Krevelen space which follows a ΔH:C/ΔO:C slope of ~ −0.5. This slope suggests that ambient OOA aging results in net changes in chemical composition that are equivalent to the addition of both acid and alcohol/peroxide functional groups without fragmentation (i.e. C-C bond breakage), and/or the addition of acid groups with fragmentation. These results provide a framework for linking the bulk aerosol chemical composition evolution to molecular-level studies.

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Metadata

Authors
Ng, N. L., Canagaratna, M. R., Jimenez, J. L., Chhabra, P. S., Seinfeld, J. H., & Worsnop, D. R.
Venue
Atmospheric Chemistry and Physics
Published
2011-07-07
Volume
11
Issue
13
Pages
6465-6474
ISSN
  • 1680-7316 (ISSN-L)
  • 1680-7324
OpenAlex
W2107371694
Cited by
602
References
1
FWCI
16.57
Type
journal article
Language
en
Open access
gold

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CoChat. (2026). Citation check: Changes in organic aerosol composition with aging inferred from aerosol mass spectra. https://app.cochat.ai/papers/10.5194/acp-11-6465-2011
The paper
Ng, N. L., Canagaratna, M. R., Jimenez, J. L., Chhabra, P. S., Seinfeld, J. H., & Worsnop, D. R. (2011). Changes in organic aerosol composition with aging inferred from aerosol mass spectra. Atmospheric Chemistry and Physics. https://doi.org/10.5194/acp-11-6465-2011

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