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High-Temperature Reactions of Ozone with Bromine Behind Shock Waves. Rate Constant for the Reaction BrO+BrO→2Br+O2

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Abstract

A mixture of ozone and bromine, diluted by argon, was heated by reflected shock waves in a shock tube to the temperature range of 600–1100 K and the pressure range of 3.5–5.5 atm. From the concentration profiles of the BrO radical, the rate constant k 1 for the reaction BrO+BrO→2Br+O2 was determined as

$${k_1}/c{m^3}molecul{e^{ - 1}}{s^{ - 1}} = (1.9 \pm 0.1) \times {10^{ - 12}}\exp [ + (42 \pm 13)/T]$$

.

A model calculation was carried out for the reactions of ozone with bromine. The results showed that bromine catalytically decomposed ozone in the chain cycle formed by the reactions BrO+BrO→2Br+O2 and O3+Br→-BrO+O2, but that this acceleration effect of bromine fell with increasing temperature.

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© 1995 Springer-Verlag Berlin Heidelberg

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Takahashi, K., Honda, J., Inomata, T., Jinno, H. (1995). High-Temperature Reactions of Ozone with Bromine Behind Shock Waves. Rate Constant for the Reaction BrO+BrO→2Br+O2 . In: Brun, R., Dumitrescu, L.Z. (eds) Shock Waves @ Marseille II. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-78832-1_11

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  • DOI: https://doi.org/10.1007/978-3-642-78832-1_11

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-78834-5

  • Online ISBN: 978-3-642-78832-1

  • eBook Packages: Springer Book Archive

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