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Atmospheric degradation of chrysene initiated by OH radical: A quantum chemical investigation.
- Source :
-
Chemosphere . Jan2021, Vol. 263, pN.PAG-N.PAG. 1p. - Publication Year :
- 2021
-
Abstract
- Chrysene, a four-ring polycyclic aromatic hydrocarbon (PAH), is recalcitrant to biodegradation and persistent in the environment due to its low water solubility. Here, we investigated the atmospheric degradation process of chrysene initiated by OH radical in the presence of O 2 and NO X using quantum chemical calculations. The reaction mechanisms were elucidated by density functional theory (DFT) at M06–2X/6–311++G(3df,2p)//M06–2X/6-311+G(d,p) level, and the kinetics calculations were conducted with Rice-Ramsperger-Kassel-Marcus (RRKM) theory. The results show that the oxidation products of atmospheric chrysene are oxygenated PAHs (OPAHs) and nitro-PAHs (NPAHs), including nitro-chrysene, hydroxychrysene, hydroxychrysenone, 11-benzo[ a ]fluorenone and dialdehydes. Most of the products have deleterious effects on the environment and human beings due to their acute toxicity, carcinogenicity and mutagenicity. The overall rate constant for the reaction of chrysene with OH radical is 4.48 × 10−11 cm3 molecule−1 s−1 and the atmospheric lifetime of chrysene determined by OH radical is 6.4 h. The present work provided a comprehensive understanding on the degradation mechanisms and kinetics of chrysene, which could help to clarify its atmospheric fate and environmental risks. Image 1 • OH-initiated oxidation of chrysene was investigated with DFT. • Nitro-chrysene can be formed through the reaction with NO 2. • Hydroxychrysene is formed via H transfer reaction. • The OH addition to C5 and C6 will lead to the formation of benzo[a]fluorenone. • The lifetime of chrysene determined by OH radical is 6.4 h. [ABSTRACT FROM AUTHOR]
Details
- Language :
- English
- ISSN :
- 00456535
- Volume :
- 263
- Database :
- Academic Search Index
- Journal :
- Chemosphere
- Publication Type :
- Academic Journal
- Accession number :
- 147344735
- Full Text :
- https://doi.org/10.1016/j.chemosphere.2020.128267