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Chemical and toxicological properties of coal fly ash - University of ...

Chemical and toxicological properties of coal fly ash - University of ...

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The overall purpose <strong>of</strong> this investigation was to provide information thatmay be <strong>of</strong> assistance in predicting the environmental impacts <strong>of</strong> <strong>coal</strong> <strong>fly</strong><strong>ash</strong> disposal. Data resulting from this investigation should be useful toutilities, consultants, <strong>and</strong> state, local, <strong>and</strong> federal agencies concernedwith <strong>fly</strong> <strong>ash</strong> <strong>and</strong> its disposal.The objectives <strong>of</strong> the study were to:Review the ecological <strong>and</strong> health literature concerning <strong>fly</strong> <strong>ash</strong>.Assess the variability in terms <strong>of</strong> chemical composition <strong>and</strong>aqueous solubility <strong>of</strong> <strong>fly</strong> <strong>ash</strong>es derived from Illinois Basin <strong>coal</strong>s,<strong>and</strong> compare these <strong>fly</strong> <strong>ash</strong>es to those generated from western U.S.<strong>coal</strong> s.Determine if the extracts generated from <strong>fly</strong> <strong>ash</strong> were acutelytoxic to fishes.- Determine if the soluble trace metals in the <strong>fly</strong> <strong>ash</strong>extracts were accumul ated by fishes under 1 aboratoryconditions.Nine <strong>fly</strong> <strong>ash</strong> samples generated from Illinois Basin <strong>coal</strong>s--predominantly silts (USDA classification)--varied in color from verydark grayish brown (10YR Munsell soil colors) to gray (2.5Y - 5Y). Theaverage specific gravity <strong>of</strong> the nine samples was about 2.4. Two <strong>fly</strong><strong>ash</strong>es generated by the combustion <strong>of</strong> western U.S. lignite <strong>coal</strong>s werelighter in color (light gray) <strong>and</strong> had greater specific gravities (about3.05), whereas a western subbituminous <strong>coal</strong> <strong>fly</strong> <strong>ash</strong> had a darker gray(10YR) color <strong>and</strong> a specific gravity <strong>of</strong> 2.2.The general mineralogical composition <strong>of</strong> the Illinois Basin <strong>fly</strong> <strong>ash</strong>eswas comparable to that <strong>of</strong> <strong>fly</strong> <strong>ash</strong>es generated from eastern 1J.S.bituminous <strong>coal</strong>s, as reported elsewhere. They were essentiallyspherical particles composed <strong>of</strong> an amorphous alumino-silicate glass,quartz, mu1 1 i te (A16Si 2013), <strong>and</strong> iron oxides. The subbi tuminouswestern <strong>ash</strong> was similar in mineralogical composition to the Illinoissamples, except for the presence <strong>of</strong> calcite in the western <strong>ash</strong>. The twowestern lignite samples had higher concentrations <strong>of</strong> some alkalinemetals <strong>and</strong> matrix sulfur, primarily in the form <strong>of</strong> anhydrite (CaS04)<strong>and</strong> pericl ase ( MgD) .Most <strong>of</strong> the matrix sulfur in all 12 samples existed as sulfatecompounds. The average ratio <strong>of</strong> sulfate S to sulfide S in the Illinoissamples was about 5:l.The trace constituent concentrations in the samples were highlyvariable, but the Illinois <strong>fly</strong> <strong>ash</strong> samples generally had greaterconcentrat ions <strong>of</strong> (in decreasing order <strong>of</strong> concentrat ion) Zn , N i , Rb,Cs, Cr, Co, U, Ge, Mo, V, Li, Cd, TI, Sm, Pb, Be, Eu, Tb, Ga, Ce, As,

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