The formation of organosulfates from the gas-phase ozonolysis of beta-pinene in the presence of neutral or acidic sulfate particles was investigated in a series of indoor aerosol chamber experiments. The organosulfates were analyzed using high-performance liquid chromatography (LC) coupled to electrospray ionization-time-of-flight mass spectrometry (MS) in parallel to ion trap MS. Organosulfates were only found in secondary organic aerosol from beta-pinene ozonolysis in the presence of acidic sulfate seed particles. One of the detected organosulfates also occurred in ambient aerosol samples that were collected at a forest site in northeastern Bavaria, Germany. beta-Pinene oxide, an oxidation product in beta-pinene/O3 and beta-pinene/NO3 reactions, is identified as a possible precursor for the beta-pinene-derived organosulfate. Furthermore, several nitroxy-organosulfates originating from monoterpenes were found in the ambient samples. These nitroxy-organosulfates were only detected in the nighttime samples, suggesting a role for nighttime chemistry in their formation. Their LC/MS chromatographic peak intensities suggest that they represent an important fraction of the organic mass in ambient aerosols, especially at night.
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http://dx.doi.org/10.1021/es070938t | DOI Listing |
J Phys Chem Lett
May 2024
Department of Chemistry, University of Helsinki, P.O. Box 55, A.I. Virtasen aukio 1, FI-00014 Helsinki, Finland.
We report the first direct kinetic measurements of a cyclic stabilized Criegee Intermediate. We have measured the unimolecular reaction rate coefficient of cyclohexanone oxide ((CH)COO) in the temperature 213-296 K and pressure 7-50 Torr ranges using absorption spectrometry. The (CH)COO was produced by the photolysis of (CH)CIBr at 213 nm in the presence of O.
View Article and Find Full Text PDFScience
November 2023
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA.
Secondary organic aerosol (SOA) is ubiquitous in the atmosphere and plays a pivotal role in climate, air quality, and health. The production of low-volatility dimeric compounds through accretion reactions is a key aspect of SOA formation. However, despite extensive study, the structures and thus the formation mechanisms of dimers in SOA remain largely uncharacterized.
View Article and Find Full Text PDFEnviron Sci Technol
June 2021
Environment Research Institute, Shandong University, Qingdao 266237, China.
Mixing of anthropogenic gaseous pollutants and biogenic volatile organic compounds impacts the formation of secondary aerosols, but still in an unclear manner. The present study explores secondary aerosol formation via the interactions between β-pinene, O, NO, SO, and NH under dark conditions. Results showed that aerosol yield can be largely enhanced by more than 330% by NO or SO but slightly enhanced by NH by 39% when the ratio of inorganic gases to β-pinene ranged from 0 to 1.
View Article and Find Full Text PDFEnviron Sci Technol
October 2020
Divisions of Chemistry and Chemical Engineering and Engineering and Applied Science, California Institute of Technology, Pasadena, California 91125, United States.
Liquid chromatography/negative electrospray ionization mass spectrometry [LC/(-)ESI-MS] is routinely employed to characterize the identity and abundance of molecular products in secondary organic aerosol (SOA) derived from monoterpene oxidation. Due to a lack of authentic standards, however, commercial terpenoic acids (e.g.
View Article and Find Full Text PDFEnviron Sci Technol
November 2019
Centre for Atmospheric Science, Department of Chemistry , University of Cambridge, Cambridge CB2 1EW , United Kingdom.
Highly oxygenated molecules (HOMs) play an important role in the formation and evolution of secondary organic aerosols (SOA). However, the abundance of HOMs in different environments and their relation to the oxidative potential of fine particulate matter (PM) are largely unknown. Here, we investigated the relative HOM abundance and radical yield of laboratory-generated SOA and fine PM in ambient air ranging from remote forest areas to highly polluted megacities.
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