Summary
The rate constant of the title reaction has been measured at 298 K using the discharge flow - mass spectrometry method: k1 = (1.13 ± 0.15) X 10-11 cm3 molecule-1s-1. The measurement of the products has led to the determination of the branching ratios: (0.43 ± 0.10) for the 0C10 channel and (0.12 ± 0.05) for the BrC1 one at 298 K.
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© 1990 ECSC, EEC, EAEC, Brussels and Luxembourg
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Poulet, G., Lancar, I.T., Laverdet, G., Le Bras, G. (1990). The BrO + C1O Reaction and the Polar Stratospheric Ozone. In: Restelli, G., Angeletti, G. (eds) Physico-Chemical Behaviour of Atmospheric Pollutants. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-0567-2_29
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DOI: https://doi.org/10.1007/978-94-009-0567-2_29
Publisher Name: Springer, Dordrecht
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