Abstract This paper presents new experimental results on NO reduction by CH4 under both N2 and CO2 atmospheres in a jet-stirred rector (JSR). The experiments are simulated using an updated… Click to show full abstract
Abstract This paper presents new experimental results on NO reduction by CH4 under both N2 and CO2 atmospheres in a jet-stirred rector (JSR). The experiments are simulated using an updated reaction mechanism, and simulations are consistent with experiments. Both experiments and simulations suggest that there is a critical equivalence ratio (Φ) to achieve the maximum NO reduction at a fixed reaction temperature (T), and the critical Φ is increased with the increase of T. The maximum NO reduction in the CO2 atmosphere is achieved at T ≈ 1300 K, Φ ≈ 1.4, and CH4/NO ratio = 20 with a maximum reduction efficiency of 63%. When the CH4/NO ratio ≤5, relative to the N2 atmosphere, the NO reburning in the CO2 atmosphere is reduced by around 40%–60% at temperatures above 1100 K. Interestingly, at 1100 K the maximum NO reduction does not occur at fuel-rich environments but at Φ ≈ 0.7 due to the low reactivity to produce hydrocarbon radicals at low temperatures. Moreover, at 1300 K, as CO2 concentration increases from 30% to 60%, the critical Φ is reduced from 1.4 to 1.2 and the NO reduction efficiency is reduced by around 7% owing to the enhanced inhibition of CH4 oxidation. To improve reburning in oxy-fuel combustion, it is recommended to operate reburn zone at moderate temperatures (i.e., 1300–1400 K), the critical Φ (e.g., Φ ≈ 1.4 if T = 1300 K), long residence times (τ ≥ 2 s), and large reburning fuel/NO ratio (≥15).
               
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