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The Kinetic Coefficient of the C2H4 + O Reaction Over Extended Pressure and Temperature Ranges

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Physico-Chemical Behaviour of Atmospheric Pollutants

Summary

A model suggested by Hunziker et al. (6) to explain the pressure dependence of the product distribution of the C2H4 + O reaction also implies pressure dependence of the total rate constant k1 of the reaction. The aim of the present study was to measure the rate constant k in the pressure ränge of 0.5 to 5 torr, at temperatures from 300 to 850 K and to compare the results with those obtained at 26–200 torr by other investigators. Using the discharge-flow technique, the rate constant was determined from the exponential decay of C2H4 at a large excess of O-atoms. Species concentrations were monitored by mass spectrometry using line-of-sight sampling; the sensitivity for 0 was determined on the basis of the NO + N reaction. Our k1 results show no evidence for pressure dependence in the 0.5 to 5 torr ränge; moreover they agree very closely with the values obtained by other workers at 26–200 torr. The experimental results are at variance with the Hunziker model, which, as shown by RRKM calculations, would imply marked fall-off of k1 in the 0.5 to 200 torr range, at least at higher temperatures.

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© 1984 ECSE, EEC, EAEC, Brussels and Luxembourg

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Fonderie, V., Maes, D., Peeters, J. (1984). The Kinetic Coefficient of the C2H4 + O Reaction Over Extended Pressure and Temperature Ranges. In: Versino, B., Angeletti, G. (eds) Physico-Chemical Behaviour of Atmospheric Pollutants. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-6505-8_29

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  • DOI: https://doi.org/10.1007/978-94-009-6505-8_29

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-009-6507-2

  • Online ISBN: 978-94-009-6505-8

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