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Reactions of organic peroxy radicals, RO(2), with substituted and biogenic alkenes at room temperature: unsuspected sinks for some RO(2) in the atmosphere?

Until now the reactions of organic peroxy radicals (RO(2)) with alkenes in the gas phase have been essentially studied at high temperature (T ≥ 360 K) and in the context of combustion processes, while considered negligible in the Earth's atmosphere. In this work, the reactions of methyl-, 1-pen...

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Detalles Bibliográficos
Autores principales: Nozière, Barbara, Fache, Fabienne
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society of Chemistry 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8442694/
https://www.ncbi.nlm.nih.gov/pubmed/34659702
http://dx.doi.org/10.1039/d1sc02263f
Descripción
Sumario:Until now the reactions of organic peroxy radicals (RO(2)) with alkenes in the gas phase have been essentially studied at high temperature (T ≥ 360 K) and in the context of combustion processes, while considered negligible in the Earth's atmosphere. In this work, the reactions of methyl-, 1-pentyl- and acetylperoxy radicals (CH(3)O(2), C(5)H(11)O(2), and CH(3)C(O)O(2), respectively) with 2-methyl-2-butene, 2,3-dimethyl-2-butene and for the first time the atmospherically relevant isoprene, α-pinene, and limonene were studied at room temperature (298 ± 5 K). Monitoring directly the radicals with chemical ionization mass spectrometry led to rate coefficients larger than expected from previous combustion studies but following similar trends in terms of alkenes, with (in molecule(−1) cm(3) s(−1)) [Image: see text] = 10(−18) to 10(−17) × 2/2 and [Image: see text] = 10(−14) to 10(−13) × 5/5. While these reactions would be negligible for CH(3)O(2) and aliphatic RO(2) at room temperature, this might not be the case for acyl-, and perhaps hydroxy-, allyl- and other substituted RO(2). Combining our results with the Structure–Activity Relationship (SAR) predicts k(II)(298 K) ∼10(−14) molecule(−1) cm(3) s(−1) for hydroxy- and allyl-RO(2) from isoprene oxidation, potentially accounting for up to 14% of their sinks in biogenic-rich regions of the atmosphere and much more in laboratory studies.