Zhuangjie Li, Randall R. Friedl and Stanley P. Sander
The reaction BrO+HO2→products is the rate-limiting step in a key catalytic ozone destruction cycle in the lower stratosphere. In this study a discharge-flow reactor coupled with molecular beam mass spectrometry has been used to study the BrO+HO2 reaction over the temperature range 233–348 K. Rate constants were measured under pseudo-first-order conditions in separate experiments with first HO2 and then BrO in excess in an effort to identify possible complications in the reaction conditions. At 298 K, the rate constant was determined to be (1.73±0.61)×10-11 cm3 molecule-1 s-1 with HO2 in excess and (2.05±0.64)×10-11 cm3 molecule-1 s-1 with BrO in excess. The combined results of the temperature-dependent experiments gave the following fit to the Arrhenius expression: k=(3.13±0.33)×10-12 exp(536±206/T) where the quoted uncertainties represent two standard deviations. The reaction mechanism is discussed in light of recent ab initio results on the thermochemistry of isomers of possible reaction intermediates.