In view of the uncertainty of the origin of the secular increase of N20, we studied heterogeneous processes that contribute to formation of N20 in an environment that comes as close as possible to exhaust conditions containing NO and SOZ, among other constituents. The N20 formation was followed using electron capture gas chromatography (ECD-GC). The other reactants and intermediates (SOZ, NO, NO2 and HONO) were monitored using gas phase UV-VIS absorption spectroscopy. Experiments were conducted at 298 and 368 K as well as at dry and high humidity (approaching 100% rh) conditions. There is a significant heterogeneous rate of N20 formation at conditions that mimic an exhaust plume from combustion processes. The simultaneous presence of NO, SO2,02 in the gas phase and condensed phase water, either in the bulk liquid or adsorbed state has been confirmed to be necessary for the production of significant levels of N20. The stoichiometry of the overall reaction is: 2 NO + SO2 + Hz0 -+ N20 + H2S04. The maximum rate of N20 formation occurred at the beginning of the reaction and scales with the surface area of the condensed phase and is independent of its volume. A significant rate of N20 formation at 368 K at 100% rh was also observed in the absence of a bulk substrate. The diffusion of both gas and liquid phase reactants is not rate limiting as the reaction kinetics is dominated by the rate of N20 formation under the experimental conditions used in this work. The simultaneous presence of high humidity (90-100% rh at 368 K) and bulk condensed phase results in the maximum rate andfinal yield of N20 approaching 60% and 100% conversion after one hour in the presence of amorphous carbon and fly-ash, respectively.