Abstract

The effects of air preheat on flame structure are studied in counterflow methane–air diffusion flames, considering air temperatures in the range 300 to 560 K. Species concentrations for H 2, O 2, N 2, CH 4, CO, CO 2, C 2H 2, and C 2H 4 were measured using sampling and gas chromatography. Concentrations of NO were measured using sampling and chemiluminescence analysis. Results of numerical calculations using GRI-Mech 2.11 were compared with the measurements. The results of the numerical calculations and the measurements show excellent agreement for O 2, N 2, CH 4, and good agreement for CO 2, H 2, and CO. However, they show poor agreement for C 2H 2 and C 2H 4. Independent of the air temperature in the range 300 to 560 K, measured and predicted concentrations of CH 4, CO 2, O 2, and N 2 collapse reasonably well when plotted against the local equivalence ratio. The peak CO and H 2 concentrations increase with increasing air preheat. The peak CO concentrations increase because of enhanced dissociation of CO 2. The peak H 2 concentrations increase because of an increase in H atom concentrations causing enhanced rates of the reaction CH 4 + H → CH 3 + H 2. Both the measured and the predicted NO profiles showed approximately a 70% increase in the peak mole fractions with the increase in air temperature. The predictions of NO mole fractions in the fuel-lean region and near the peak are within 10% of the measurements. However, in the fuel-rich region, the predicted NO mole fractions are lower by up to 70% than the measured NO mole fractions. The increase in peak NO mole fractions with air preheat occurs primarily through the enhanced reaction rate of the prompt initiation reaction N 2 + CH → HCN + N. The NO production by the thermal mechanism increases significantly with air preheat, but still remains a very small portion of the total. The effects of air preheat on many species and reaction rates manifest through the increased H atom concentrations.

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