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Formation of highly oxygenated organic molecules from the oxidation of limonene by OH radical: significant contribution of H-abstraction pathway

Luo, H. (författare)
Vereecken, L. (författare)
Shen, H. R. (författare)
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Kang, S. (författare)
Pullinen, I. (författare)
Hallquist, Mattias, 1969 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för kemi och molekylärbiologi,Department of Chemistry and Molecular Biology
Fuchs, H. (författare)
Wahner, A. (författare)
Kiendler-Scharr, A. (författare)
Mentel, T. F. (författare)
Zhao, D. F. (författare)
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 (creator_code:org_t)
2023
2023
Engelska.
Ingår i: Atmospheric Chemistry and Physics. - 1680-7316. ; 23:13, s. 7297-7319
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Highly oxygenated organic molecules (HOMs) play a pivotal role in the formation of secondary organic aerosol (SOA). Therefore, the distribution and yields of HOMs are fundamental to understand their fate and chemical evolution in the atmosphere, and it is conducive to ultimately assess the impact of SOA on air quality and climate change. In this study, gas-phase HOMs formed from the reaction of limonene with OH radicals in photooxidation were investigated with SAPHIR (Simulation of Atmospheric PHotochemistry In a large Reaction chamber), using a time-of-flight chemical ionization mass spectrometer with nitrate reagent ion (NO3--CIMS). A large number of HOMs, including monomers (C9-10) and dimers (C17-20), were detected and classified into various families. Both closed-shell products and open-shell peroxy radicals (RO2) were identified under low NO (0.06-0.1 ppb) and high NO conditions (17 ppb). C-10 monomers are the most abundant HOM products and account for over 80% total HOMs. Closed-shell C-10 monomers were formed from a two peroxy radical family, C10H15Ox center dot (x = 6-15) and C10H17Ox center dot ( x = 6-15), and their respective termination reactions with NO, RO2, and HO2. While C10H17Ox center dot is likely formed by OH addition to C10H16, the dominant initial step of limonene plus OH, C10H15Ox center dot, is likely formed via H abstraction by OH center dot C10H15Ox center dot and related products contributed 41% and 42% of C-10 HOMs at low and high NO, demonstrating that the H-abstraction pathways play a significant role in HOM formation in the reaction of limonene plus OH. Combining theoretical kinetic calculations, structure-activity relationships (SARs), data from the literature, and the observed RO2 intensities, we proposed tentative mechanisms of HOM formation from both pathways. We further estimated the molar yields of HOMs to be 1.97(-1.06)(+2.52) % and 0.29(-0.16)(+0.38)% at low and high NO, respectively. Our study highlights the importance of H abstraction by OH and provides the yield and tentative pathways in the OH oxidation of limonene to simulate the HOM formation and assess the role of HOMs in SOA formation.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)

Nyckelord

oxidized multifunctional compounds
initiated atmospheric oxidation
main-group thermochemistry
aerosol soa formation
gaussian-basis sets
gas-phase reactions
alpha-pinene
peroxy-radicals
simulation chamber
rate coefficients
Environmental Sciences & Ecology
Meteorology & Atmospheric Sciences

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