Geophysical Research Letters · 2000 · 36 citations · 21 references
Natural SciencesChemistryAtmospheric ChemistryChemical KineticsInorganic ChemistryAtmospheric Oxidation ProcessesChemical Reaction KineticsGas-phase Reaction KineticsKinetic Isotope EffectsKinetic ModelingReactive Oxygen SpeciesAbstractionActivation EnergyActivation Energy AnalysisActivation Energy DeterminationActivation Free EnergyIsoprene Oxidation ChemistryOxidationRadical Reaction Kinetics
Absolute rate coefficients have been determined for the reaction OH + C 5 H 8 (1) and two of its isotopomeric variants. Reaction (1) was studied as a function of temperature and pressure in N 2 , N 2 /O 2 and He buffer gases. At room temperature, a rate coefficient, k 1 , of (8.56±0.26) * 10 −11 cm³ s −1 independent of pressure and buffer gas identity was obtained. An Arrhenius fit to data over the temperature range 250 – 340 K gave a negative activation energy of −666±150 cal/mol. HO 2 production was inferred from observations of radical regeneration in the presence of NO. The absence of a kinetic isotope effect, together with the specificity of radical regeneration, indicates that reaction proceeds via an addition channel with no significant abstraction component. Our rate coefficient for reaction (1) is 15% lower than the value currently recommenced for atmospheric modeling.
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Roger Atkinson, D. L. Baulch, R. A. Cox et al. · Journal of Physical and Chemical Reference Data · 1997 · 1K citations · Full text
Evidence for marine production of isoprene
B. Bonsang, Claude Polle, Gérard Lambert · Geophysical Research Letters · 1992 · 233 citations · Full text