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Characterization of individual fly ash particles emitted from coal- and oil-fired power plants
Institution:1. Department of Earth Sciences, University of Minnesota, Minneapolis, MN 55455, USA;2. Department of Soil, Water, and Climate, University of Minnesota, St. Paul, MN 55108, USA;3. Department of Geosciences, State University of New York at Stony Brook, Earth and Space Science Building, Stony Brook, NY 11794, USA;4. Bigelow Laboratory for Ocean Sciences, East Boothbay, ME 04544, USA;5. Department of Oceanography, Texas A&M University, College Station, TX 77843, USA;6. Department of Marine and Coastal Sciences and Department of Earth and Planetary Sciences, Rutgers University, Piscataway, NJ, USA;7. Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA;8. Department of Ocean Sciences, UC Santa Cruz, Santa Cruz, CA 95064, USA
Abstract:Individual particles from coal- and oil-fired power plants were analyzed by scanning electron microscope equipped with an energy dispersive X-ray spectrometer to investigate size, morphology, and composition. Samples were collected on filters by dichotomous sampler in the fine ( <2.5 μm aerodynamic diameter) and coarse (2.5 to 5–10 μm) fractions. In both fractions coal fly ash particles were predominantly ( > 95%) smooth, mineral spheres. No cenospheres (perforated hollow spheres) were detected, and almost 90% of the mass concentrations occurred in the coarse fraction. Sulfur as lared as a surface layer on the mineral core; the abundances of Fe and S were highly variable. The Al/Si ratio was fairly constant for most of the spheres but not for the relatively few Fe-rich or non-spherical coal fly ash particles. Over 90% of the mass of oil fly ash occurred in the fine fraction. The size distribution of chemical and morphological properties of individual oil fly ash particles was found to be trimodal. Oil fly ash particles smaller than 0.7 μ (geometric diameter) were non-spherical and relatively pure in sulfate, and 90% of such particles were smaller than 0.5 μm; V or Ni could be detected in 50% to 60% of such particles larger than 0.3 μm. Those particles in the 0.7–3 μm range of geometric diameters were predominantly spherical and of mineral composition, highly variable in Al, Si, P, Ca, Ti and Fe; 50–60% of them contained detectable amounts of V or Ni. Larger oil fly ash particles had a lacy morphology and consisted of carbonaceous material and sulfur.
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