(1) or from the thermal decomposition of larger radicals formed in the degradation of oxygenated hydrocarbons, e.g., the OH-initiated oxidation of methylglyoxal [ ABSTRACT: Relative rate coefficients for the reaction of acetyl (CH 3 CO) radicals with O 2 (k 4 ) and Cl 2 (k 7 ) have been obtained at 298 K and 228 K as a function of total pressure, using FTIR/environmental chamber techniques. Measured values of k 4 /k 7 were placed on an absolute basis using k 7 ϭ 2.8 ϫ 10Ϫ11 exp(Ϫ47/ T) cm 3 molec Ϫ1 s
Ϫ1. At 298 K, the value of k 4 is constant ((7 Ϯ 2) ϫ 10 Ϫ13 cm 3 molec Ϫ1 s
Ϫ1) at pressures from 0.1 to 2 torr, then increases to a high pressure limiting value of (3.2 Ϯ 0.6) ϫ 10 Ϫ12 cm 3 molec Ϫ1 s Ϫ1 , which is approached at pressures above 300 torr. At 228 K, the low-pressure value of k 4 increases by about 20 -30%, while the high pressure value remains unchanged. Experiments designed to elucidate the products of reaction (4) as a function of pressure at 298 K indicate that the reaction occurs via a concerted mechanism in which CH 3 CO radicals combine with O 2 to give an excited acetylperoxy radical (CH 3 COO 2 *) which is increasingly stabilized at high pressure at the expense of a low pressure decomposition channel. The yield of acetylperoxy radicals from reaction (4) decreases from Ͼ95% at pressures above 100 torr, to about 90% at 60 torr, and 50% at 6 torr. Indirect evidence for formation of OH radicals from the low pressure decomposition is presented, although the carbon-containing coproduct(s) of this channel could not be identified.