The reaction of ozone with ethane was studied in the range
24−150 °C. Added oxygen at 24 °C was found
to cause a large induction period after which the reaction occurred
rapidly accompanied by a flash of light.
The light consisted of Meinel bands from vibrationally excited OH
radicals as had been previously seen at
higher temperatures in the methane−ozone system. Induction
periods of more than 3 h were measured when
an excess of oxygen was added. Total pressure measurements
suggested a chain reaction, and several possible
chain sequences are considered. A 42-step mechanism was used to
simulate the system and found to account
for the effect of added oxygen on the induction period and on the light
emission.