Experimental characterization of diffusive-thermal instabilities in CO2-diluted H2-CH4-CO unstrained diffusion flames

The combustion of multi-fuel mixtures is experimentally studied for the first time in unstrained diffusion flames, where the parasitic hydrodynamic effects present in common research burners are negligible. A broad range of H2 -CO -CH4 fuels highly diluted in CO2 is investigated to provide an understanding of the intrinsic diffusive-thermal instabilities (DTIs) that onset in low calorific biomass-derived syngas. For each fuel blend, the burning intensity or the Damkohler number (Da) is gradually reduced, going through the marginal stability state where DTIs first appear, down to the lean extinction limit. Flame stability limits are provided. From the large difference between the Lewis numbers of the multiple fuel species (Lei), the cells that onset due to H2 are seen to interact and compete with the pulsations from CO and CH4, leading to superimposed cellular-pulsating instabilities. These are thoroughly characterized by measuring the pulsations amplitude, frequency, cell size, number of cells, and fraction of the flame sheet actively burning. An effective fuel Lewis number (LeF,eff) calculated from the fuel mixture composition is introduced and used along with the Damkohler number to map the DTIs observed. At lower LeF,eff and Da, the cellular attributes of the superimposed instabilities dominate, while at larger Lewis numbers and the near marginal stability state, pulsations prevail.(c) 2023 The Combustion Institute. Published by Elsevier Inc. All rights reserved.

Automated summary

The combustion of multi-fuel mixtures is experimentally studied in unstrained diffusion flames for the first time, eliminating parasitic hydrodynamic effects. The study investigates H2-CO-CH4 fuels diluted in CO2 to understand diffusive-thermal instabilities. Flame stability and properties of cellular-pulsating instabilities are characterized by measuring various parameters. Effective fuel Lewis number and Damkohler number are used to map the observed instabilities.