Transition in the propagation mechanism during flame acceleration in porous media

G Ciccarelli, C Johansen, M Parravani - Proceedings of the Combustion …, 2011 - Elsevier
G Ciccarelli, C Johansen, M Parravani
Proceedings of the Combustion Institute, 2011Elsevier
The combustion of stoichiometric hydrogen-air at various initial pressures was investigated
in a 7.62 cm square cross-section channel filled with 1.27 cm diameter beads. The flame
time-of-arrival and pressure time history along the channel were obtained by ionization
probes and piezoelectric pressure transducers. Flame acceleration was found to be very
rapid, eg at an initial pressure of 45kPa the flame achieves a velocity of over 600m/s in
roughly 0.3 m. It was determined that at this high speed a well defined planar shock wave …
The combustion of stoichiometric hydrogen-air at various initial pressures was investigated in a 7.62cm square cross-section channel filled with 1.27cm diameter beads. The flame time-of-arrival and pressure time history along the channel were obtained by ionization probes and piezoelectric pressure transducers. Flame acceleration was found to be very rapid, e.g. at an initial pressure of 45kPa the flame achieves a velocity of over 600m/s in roughly 0.3m. It was determined that at this high speed a well defined planar shock wave precedes a thick reaction zone. It was also shown that there is a transition in the flame propagation mechanism, similar to that observed in an obstacle laden channel [G. Ciccarelli and C. Johansen, The role of shock-flame interactions on flame acceleration in an obstacle laden channel, Proc. 22nd International Colloquium on the Dynamics of Explosions and Reactive Systems, Minsk, 2009]. By varying the initial pressure of the mixture, changes in the axial location of the transition between combustion propagation regimes was also observed. A soot foil technique was used to identify the transition in the propagation mechanism, as well as to provide information concerning the local flow field around the beads and the overall average flow direction.
Elsevier
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