Abstract
Shock‐tube interferometry has been used to observe vibrational relaxation of O2 in O2+D2 mixtures. From 300° to 850°K the present shock tube and previous ultrasonic relaxation times in atmosphere seconds are given by log10(pτO2D2)=27.3T13−8.35 . Above 1500°K the relaxation time of O2 is further shortened due to effects of chemical reaction or possibly to a resonant‐energy exchange with the more rapidly excited D2. Hydrogen vibrational relaxation is too rapid to be resolved, yielding H2<2×10−6atm·sec for T = 1400°K. The vibrational relaxation of deuterium appears to be more complex than other diatoms studied and is not yet understood. However, it is observed that D2<6×10−6atm·sec at T = 1400°K.