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Time-resolved molecular characterization of limonene/ozone aerosol using high-resolution electrospray ionization mass spectrometry

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TLDR
The data are consistent with fast production of the first-generation SOA constituents, including oligomers, followed by very slow aging processes that have a relatively small effect on the average molecular composition on the timescale of the authors' experiments.
Abstract
Molecular composition of limonene/O3 secondary organic aerosol (SOA) was investigated using high-resolution electrospray ionization mass spectrometry (HR-ESI-MS) as a function of reaction time. SOA was generated by ozonation of D-limonene in a reaction chamber and sampled at different time intervals using a cascade impactor. The SOA samples were extracted into acetonitrile and analyzed using a HR-ESI-MS instrument with a resolving power of 100 000 (m/Δm). The resulting mass spectra provided detailed information about the extent of oxidation inferred from the O : C ratios, double bond equivalency (DBE) factors, and aromaticity index (AI) values in hundreds of identified individual SOA species. The chemical composition of SOA was approximately the same for all size-fractionated samples studied in this experiment (0.05 to 0.5 μm range). The SOA constituents quickly reached an average O : C ratio of 0.43, which grew to 0.46 after one hour of additional oxidation of particles by the excess ozone. The dominant mechanism of oligomerization, inferred from high resolution ESI-MS data, was reaction between Criegee intermediates and stable first-generation products of limonene ozonolysis. Although the SOA composition was dominated by various oxidized aliphatic compounds, a small fraction of products appeared to contain aromatic rings. SOA generation was also studied in the presence of UV radiation and at elevated relative humidity (RH). The presence of UV radiation had a negligible effect on the SOA composition. The presence of water vapor resulted in a slight redistribution of peak intensities in the mass spectrum likely arising from hydration of certain SOA constituents. The data are consistent with fast production of the first-generation SOA constituents, including oligomers, followed by very slow aging processes that have a relatively small effect on the average molecular composition on the timescale of our experiments.

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Carbon oxidation state as a metric for describing the chemistry of atmospheric organic aerosol

TL;DR: In this article, the authors demonstrate the utility of describing organic aerosol (and other complex organic mixtures) in terms of average carbon oxidation state (OSC), a quantity that always increases with oxidation, and is readily measured using state-of-the-art analytical techniques.
References
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Journal ArticleDOI

Species contributions to PM2.5 mass concentrations: Revisiting common assumptions for estimating organic mass

TL;DR: The authors revisited common assumptions for estimating PM2.5 mass concentration and found that these assumptions can be used to estimate organic mass in a wide range of scenarios, such as PM1.5.
Journal ArticleDOI

Rate constants of reactions of ozone with organic and inorganic compounds in water-II dissociating organic compounds

TL;DR: In this article, the rate constants of reactions of ozone with non-ionized solutes, such as aliphatic alcohols, olefins, chlorosubstituted ethylenes, substituted benzenes and carbohydrates, have been determined from the absolute rates with which ozone reacts in the presence of various concentrations of these compounds in water.
Journal ArticleDOI

Practical implications of some recent studies in electrospray ionization fundamentals.

TL;DR: Fundamental studies of the ESI process are reviewed that are relevant to issues related to analyte chargeability and surface activity, and how accessible parameters such as nonpolar surface area and reversed phase HPLC retention time can be used to predict relative ESI response.
Journal ArticleDOI

From mass to structure: an aromaticity index for high‐resolution mass data of natural organic matter

TL;DR: In this article, a general aromaticity index (AI) and two threshold values are proposed as unequivocal criteria for the existence of either aromatic (AI > 0.5) or condensed aromatic structures (AI >= 0.67) in NOM.
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