Direct rate measurements for hydroxyl + hydroxyl -> water + atomic oxygen in the range 1200-1800 K.
Rate consts. for the disproportionation reaction OH + OH -> H2O + O at 1200-1800 K were detd. by a direct technique using shock heating of a HNO3-Ar mixt. as a source of a strongly nonequilibrated OH concn. and time-resolved UV resonance absorption as a monitor.
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