ABSTRACT. The morphology of submicron ame-generated inorganic aerosols is known to be fractal-like with reported fractal exponents ranging from 1.1 -2.5 for different materials. This wide range represents a correspondingly broad variation in structure and suggests that chemical composition might affect the nal structure of ame-generated materials, a prospect of considerable importance in studies of submicron particulate penetration through electrostatic precipitators. To investigate this, the morphology of ame-generated submicron aerosols was studied by characterizing both y ash generated in a pilot scale coal combustor and controlled composition inorganic aerosols generated in a bench scale at ame burner. Fly ash generated during combustion of 2 bituminous coals at 2 different ame temperatures was found to be fractal-like with fractal exponents of 1.9 -2 and fractal prefactors of 1.1 -1.5. In addition, y ash samples collected at the inlet and outlet of an attached pilot scale electrostatic precipitator yielded no difference in particle morphology, indicating a lack of structure-dependent penetration. Flame-generated silica, magnesia, sodium-doped silica, and magnesium-doped silica produced under identical conditions in an invariant premixed ame were also fractal-like in structure with fractal exponents of 1.7 -1.8 and fractal prefactors of 1.6 -1.8. No dependence of these structural parameters on chemical composition, ame residence time, or particle number density was observed over the ranges considered. Changing chemical composition did, however, lead to order of magnitude changes in primary particle diameter without any corresponding change in aggregate structure. Findings from both systems are consistent with a growth process governed in the late stages by cluster-cluster aggregation and indicate that for ame synthesized materials produced in the overall decreasing temperature gradient characteristic of coal combustors and industrial ame reactors, the aerosol aggregate structure will not be affected by changes in chemical composition under conditions of coalescence-limited growth.¤ Corresponding author.
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B. B. Liu et al.