Atmospheric degradation of volatile organic compounds.
By R. Atkinson, J. Arey. Chemical Reviews, 2003
2,718 citations recorded by the source corpus.
Subfields: Atmospheric Science, Automotive Engineering, Health, Toxicology and Mutagenesis
View Paper: https://www.semanticscholar.org/paper/786f0a3c1b719abfc16aadb18ca717742a442a95
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
In Automotive Engineering
In Health, Toxicology and Mutagenesis
Citations in the corpus
- Highly Oxygenated Organic Molecules (HOM) from Gas-Phase Autoxidation Involving Peroxy Radicals: A Key Contributor to Atmospheric Aerosol (2019, background): “Whereas the organic nitrates formed in reaction (e) are fairly stable compounds, the peroxynitrates formed in reaction (g) from common primary, secondary, and tertiary RO2 are unstable and decompose back to RO2 and NO2, typically within a second time frame (Atkinson and Arey, 2003).”
- Volatile organic compounds (VOCs) in soils (2010, background): “Anyway, Atkinson and Arey (2003) give a very detailed overview on physical–chemical degradation of VOCs in the atmosphere where photolysis and spontaneous reactions with OH radicals (under the presence of light), NO3 radicals (under the absence of light), O3 (under the presence of light), and Cl ato”
- Molecular decoding using luminescence from an entangled porous framework (2011, background): “In this paper, we report on a 1,4,5,8-naphthalenediimide ( NDI )-based entangled PCP that undergoes a dynamic structural transformation to confine a class of aromatic volatile organic compounds (VOCs), or tropospheric air pollutant”
- Modeling global secondary organic aerosol formation and processing with the volatility basis set: Implications for anthropogenic secondary organic aerosol (2010, result): “This hypothesis is consistent with plausible oxidation mechanisms [Atkinson and Arey, 2003] for aromatic compounds, which suggest that the oxidation of one aromatic molecule by a hydroxyl radical, initiated either through ring opening or by aromatic substitution, may occur over as many as three or…”
- Kinetics, products, and mechanisms of secondary organic aerosol formation. (2012, methodology): “…o10 20 2.1 days 1.8 years >4.5 years o-Cresol 4.1 10 11 1.4 10 11 3 10 19 3.4 h 2 min 55 days a Rate constants from Calvert et al. (2003, 2011) and Atkinson and Arey (2003). b Lifetimes calculated using concentrations (molecules cm 3) of: OH, 12 h daytime average of 2 106; NO3, 12 h nighttime…”