An experimental and theoretical study of HNCO oxidation has been carri
ed out. The experiments were performed in an isothermal quartz flow re
actor, and the effects of temperature, CO concentration, and NO concen
tration were investigated at atmospheric pressure in the temperature r
ange 1025-1425 K. The reaction mechanism for RAPRENO(x) proposed by Mi
ller and Bowman (1991) has been updated based on the present results a
s well as recent advances in the understanding of important elementary
steps. Model predictions with the revised mechanism are in good agree
ment with our experimental data as well as data from the literature. O
xidation of HNCO proceeds mainly through NCO, which subsequently is ox
idized to NO or reacts with NO to form N2 and N2O. This sequence of re
actions is chain terminating, and for reaction to occur, radicals must
be generated either by alternative oxidation pathways or by the prese
nce of other combustibles. A chain-branching oxidation route initiated
by reaction of HNCO with O2 is proposed in order to explain the obser
ved HNCO decay in the absence of inlet CO. Addition of CO enhances HNC
O oxidation and the RAPRENO(x) chemistry, since CO oxidation acts to r
eplenish the radical pool. The experimental results show that the mutu
al presence of HNCO and NO strongly inhibits CO oxidation at lower tem
peratures. In addition to the chain terminating HNCO/NCO reactions, a
second inhibition mechanism involving NO is necessary to explain this
behavior. This mechanism is presently believed to be NO/NO2 interconve
rsion, but additional work is needed to confirm this. Further progress
in the understanding of the HNCO chemistry is dependent on an accurat
e determination of the rate and/or mechanism of a number of key reacti
ons, including HNCO + OH, HNCO + O2, NCO + NO and NO + O + M.