Postflame chemistry is governed largely by moist CO oxidation. During
carbon monoxide burnout, trace amounts of many other pollutants formed
in and/or surviving through the flame front may be present (e.g., SOx
, NOx, HCl, and unburned hydrocarbons). The development of accurate ch
emical models describing these final stages of pollutant destruction r
equires evaluating the potential kinetic coupling effects that exist a
mong these components. In the present investigation, the coupling betw
een NO and HCl in a moist CO oxidation bath is considered. Experiments
are performed in an atmospheric pressure flow reactor by perturbing t
he CO/H2O/O-2 reaction system with trace amounts of NO and/or HCl for
temperatures between 1000 and 1070 K and both stoichiometric (Phi = 1.
0) and fuel-lean (Phi = 0.1) mixtures. The experimental results are co
mpared with predictions from a detailed kinetic model and analyzed by
gradient sensitivity and reaction flux analyses. While the addition of
the individual perturbing agents show accelerating or inhibiting char
acteristics depending on the equivalence ratio and temperature, the co
upling between NO and HCl generates considerable synergistic inhibitio
n of the CO oxidation rate. Thus, accurate predictions of CO burnout i
n practical systems, where trace quantities of HCl and NOx are present
, can be achieved only if these kinetic interactions are considered.