
Journal of Physical Chemistry p. 1853 - 1858 (1988)
Update date:2022-08-24
Topics:
Hills, Alan J.
Cicerone, Ralph J.
Calvert, Jack G.
Birks, John W.
We have measured the rate constant for the reactions BrO + ClO -> Br + OClO (6a), BrO + ClO -> Br + Cl + O2 (6b), and BrO + ClO -> BrCl + O2 (6c) over the temperature range 241-408 K and found k6 = (8.2 +/- 1.0)E-12 cm3 molecule-1 s-1 independent of temperature.Measurement of the individual product branching ratios yielded values for channels 6a, 6b, and 6c equal to 0.55 +/- 0.10, 0.45 +/- 0.10, and <0.02, respectively.Measurements of ozone in the stratosphere over Antarctica have shown that the springtime ozone column has fallen 40percent from 1960 to 1985.The reaction above could account for a large fraction of the springtime ozon hole reported recently, provided that at least 20 ppt of total inorganic bromine is present, and it may provide a source of chlorine dioxide of sufficient magnitude to explain the recent measurements of this species in the Antarctic stratosphere.
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