ABSTRACT
Particle formation and emission in the combustion of four (orujillo, eucalyptus, oak and chestnut tree) pulverized biomass fuels have been studied. The fuels have been burned in an entrained flow reactor, under controlled and realistic conditions. In all the cases, the final emission distributions contained at least two modes, one of them peaking at 30–200 nm, and the other being in the supermicron range. Alkali sulphates and chlorides account for most of the mass of the fine particles in all cases, while coarse particles essentially retain the inorganic matter properties of the original fuel. K2SO4 is experimentally found to start nucleation over 900°C for orujillo, while KCl is not observed at this temperature. Condensation of KCl on these nuclei is observed in a sample taken at 560°C and in a greater amount at 360°C. The same formation schema was found for the other biomass fuels; the much lower ash content of the latter is thought to cause a “delay” in the onset of these nucleation/condensation steps along the gas cooling process. In spite of these differences, the global similarities observed among the studied fuels confirm the generality of the fine particle formation process in biomass combustion.
The authors would like to acknowledge the support of the Aerosol Technology Group at the CIEMAT (Madrid, Spain) and L. Ojeda in the fulfillment of the experiments. This work was funded by the Spanish Ministry of Science and Technology through grant BFM2001-1314-C03-03.
Notes
a Normalized (i.e., the sum of the elements in the list is 100).