Abstract Mixtures of ammonia and oxygen in argon were heated by reflected shock waves to temperatures between 1600 and 2100°K, and the ultraviolet radiation from OH(2Σ+) was observed by means of monochromator and a photomultiplier. The radiation profiles showed two types of radiation: a strong spike which appeared after an induction period, and a weak and constant-level emission, which followed the spike and persisted for up to 500 μsec. The former emission was observed also in the oxidation of hydrogen, methane, and acetylene, but the latter emission was observed only in the oxidation of methane and acetylene. The temperature coefficients of the intensities of the latter emission divided by the sum of spectral emissivities were found, for the oxidation of ammonia, not large enough to be explained by the thermal excitation of the ground-state OH(2π) to the 2Σ+ state. Possible reaction processes for this chemiluminescence were proposed to explain the experimental results.