Abstract
Nitrous oxide (N2O) concentrations in the atmosphere increase at an estimated rate of 0.7–0.8 ppb per year. The combustion of solid fuels and waste at lower temperatures (750–900 °C) constitutes a significant source of N2O. During stages of a coal particle combustion (pyrolysis-devolatilisation and char combustion) both volatile-N and char- N are mainly transformed to N2 + NO and partly to N2O. HCN was recognised as the main precursor for N2O in volatile combustion. Char-N conversion to N2O (through various mechanisms) is affected by “in situ” reduction of N2O by the carbon surface and CO.
The temperature is a key parameter for N2O emissions in combustion. At temperatures over 1000 °C, N2O emissions are negligible. In practical combustion systems char and CaO are the most effective catalysts for the thermal decomposition of N2O.
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Svoboda, K., Cermák, J., Veselý, V. (2000). NOx Chemistry and Emissions - II. In: Vovelle, C. (eds) Pollutants from Combustion. NATO Science Series, vol 547. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-4249-6_9
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DOI: https://doi.org/10.1007/978-94-011-4249-6_9
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