Science Inventory

INVESTIGATION OF PRIMARY FINE PARTICULATE MATTER FROM COAL COMBUSTION BY COMPUTER-CONTROLLED SCANNING ELECTRON MICROSCOPY

Citation:

Chen, Y., N. Shah, F. E. Huggins, G. P. Huffman, W P. Linak*, AND C A. Miller*. INVESTIGATION OF PRIMARY FINE PARTICULATE MATTER FROM COAL COMBUSTION BY COMPUTER-CONTROLLED SCANNING ELECTRON MICROSCOPY. FUEL PROCESSING TECHNOLOGY 85(6-7):743-761, (2004).

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Description:

The particle size distributions, morphologies, and chemical composition distributions of 14 coal fly ash (CFA) samples produced by the combustion of four western U.S. coals (two subbituminous, one lignite, and one bituminous) and three eastern U.S. coals (all bituminous) have been examined by computer-controlled scanning electron microscopy (CCSEM). The samples were obtained from a 50-kW combustor using an isokinetic sampler and separated aerodynamically using a cyclone into PM fractions that were nominally <2.5 μm in mean diameter (PM2.5) and >2.5 μm in mean diameter (PM2.5+). However, the CCSEM particle size distribution results show that particles with mean diameter <2.5 μm typically constitute more than 80% of the total number of particles and particles with mean diameter >2.5 μm account for over 80% of the total particle volume for both the PM2.5 and the PM2.5+ fractions. The samples contained from 0.5 to 11.0 wt.% of unburned carbon and carbonaceous PM was the dominant form of PM <1 μm in mean size. Typically, over 80% of carbon-rich PM was <1 μm and over 95% was <2.5 μm in mean size. The dominant carbonaceous PM morphology consisted of roughly spherical carbon particulates 10–50 nm in diameter bonded together in complex chains and clusters that were usually <1 μm in size. Glassy phases with rounded and frequently spherical morphologies were the dominant species observed for the inorganic PM. Particle compositions for several hundred inorganic particles are presented as ternary diagrams, which appear to be useful for source attribution. The inorganic PM derived from combustion of western low-rank coals, which are rich in carboxyl-bound Ca, is dominated by Ca–Si–Al glass phases, while that from eastern bituminous coals, which are rich in pyrite, is dominated by Fe–Si–Al glass phases. Important secondary signature glass phases that are also revealed by the ternary diagrams are Na–Si–Al for western CFA and K–Si–Al for eastern CFA.

Record Details:

Record Type:DOCUMENT( JOURNAL/ PEER REVIEWED JOURNAL)
Product Published Date:04/20/2004
Record Last Revised:05/21/2009
OMB Category:Other
Record ID: 81817