2011
DOI: 10.1016/j.pecs.2010.06.006
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Kinetics of elementary reactions in low-temperature autoignition chemistry

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Cited by 606 publications
(554 citation statements)
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“…Considerable work has been performed on the phenyl radical (C 6 H 5 ) and its reactions with O 2 . 1-10 Notably, phenyl oxidation does not follow the ROO -QOOH isomerisation route often encountered when rationalising hydrocarbon radical oxidation; 11 instead, more elaborate peroxyl radical isomerisation channels are accessed. For substituted phenyl radicals there remains significant uncertainty around the key mechanisms and dominant reaction products in their oxidation.…”
Section: Introductionmentioning
confidence: 99%
“…Considerable work has been performed on the phenyl radical (C 6 H 5 ) and its reactions with O 2 . 1-10 Notably, phenyl oxidation does not follow the ROO -QOOH isomerisation route often encountered when rationalising hydrocarbon radical oxidation; 11 instead, more elaborate peroxyl radical isomerisation channels are accessed. For substituted phenyl radicals there remains significant uncertainty around the key mechanisms and dominant reaction products in their oxidation.…”
Section: Introductionmentioning
confidence: 99%
“…The subsequent fuel radical, "R", can then react with molecular oxygen. The details of this reaction, and in particular the branching among the possible product channels, is the basis of most of the fuel effects in autoignition (Zádor, Taatjes et al 2010). The formation of an OH radical in the R + O 2 reaction is particularly important, both because OH is an excellent chain carrier and because OH production is kinetically linked to the formation of hydroperoxyalkyl radicals, whose reactions are responsible for low-temperature chain branching (Battin-Leclerc, Herbinet et al 2010).…”
Section: Fundamental Chemistry Experimentsmentioning
confidence: 99%
“…Methyl peroxy (CH 3 O 2 ) radicals are critical intermediates in the atmospheric oxidation (Orlando and Tyndall, 2012) and combustion of hydrocarbons (Zador et al, 2011). In the remote atmosphere, CH 3 O 2 is mainly formed by the reaction of methane with the OH radical via abstraction of an H atom (Reaction R1), followed by the reaction of the produced CH 3 radical with O 2 (Reaction R2).…”
Section: Introductionmentioning
confidence: 99%