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U.S. Department of Energy
Office of Scientific and Technical Information

Mineralogical properties of coal ash

Conference ·
OSTI ID:6085599
Studies of the mineral phases of fly ash and the distribution of elements among them have been made. Three main phases have been categorized: (1) magnetic spinel, (2) mullite-quartz, and (3) glass. Each of these contains dissolved trace elements. The chemical species of the trace elements are determined by the phases within which they are dissolved. Elements are usually distributed preferentially, but not exclusively, in certain phases; e.g., Ni is more concentrated in the magnetic spinel matrix by factors as high as 100. Most of the trace elements are contained in the glass phase. Long-term leaching effects are therefore determined by mechanics of breakdown of the glass. Both the mullite-quartz and the magnetic spinel phases are potential resource recovery items. Mullite is used extensively as a commercial ceramic. The feasibility of its refinement from fly ash should be explored. Magnetite is an improper designation of the magnetic spinel phase, x-ray diffraction and transmission electron microscopy show that the magnetic spinel phase is a ferrite, having large amounts of aluminum substitution for iron. Recent studies of fly ash particles in human lung tissue indicate that lung fluids rapidly break down the glass phases, causing accelerated release of trace elements, leaving mullite residues permanently imbedded in the tissue. 3 figures.
Research Organization:
Oak Ridge National Lab., TN (USA)
DOE Contract Number:
W-7405-ENG-26
OSTI ID:
6085599
Report Number(s):
CONF-8206173-2; ON: DE83014132
Country of Publication:
United States
Language:
English