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

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Table 7. Fly <strong>ash</strong> sample classifications.SampleTypealkaline Modic siltacid C-Modic silt loamalkaline Modic siltalkaline Modic siltalkaline Modic siltalkaline Modic siltacid C, Zn-Fersic siltalkaline Modic siltalkaline Modic silta1 kal ine Ba-Modic si 1 talkaline B, Ba, Sr-Calsialicaalkaline 8, Ba, Sr-Calcica--aTexture was not determinedbituminous <strong>coal</strong>s, one from a German bituminous <strong>coal</strong> <strong>and</strong> the other 17, samples were derived from subbituminous <strong>and</strong> lignite <strong>coal</strong>s from the westernUS., India, <strong>and</strong> Australia.Fly <strong>ash</strong>es from eastern U.S. bituminous <strong>coal</strong>s tended to fall on the leftside <strong>of</strong> the diagram in the Modic <strong>and</strong> Fersic fields (Fig. 5): this patternis reasonable, because the eastern U.S. <strong>coal</strong>s generally have higherconcentrations <strong>of</strong> Fe than do western <strong>coal</strong>s (Gluskoter et al., 1977). Fly<strong>ash</strong>es from western U.S. lignite <strong>and</strong> subbituminous <strong>coal</strong>s tended to plot onthe right side <strong>of</strong> the diagram in the Modic, Calsialic, <strong>and</strong> Calcic fields.Western U.S. <strong>coal</strong>s are generally associated with higher levels <strong>of</strong> Ca, Mg,<strong>and</strong> Na than are eastern <strong>coal</strong>s (Abernathy, 1969; Furr et al., 1977;Gluskoter et al., 1977). Near the Sialic- odic boundary are three f 1 y<strong>ash</strong>es generated from lignite <strong>coal</strong>s in India. Indian lignite <strong>coal</strong> ischaracteristically low in Ca (Chopra et al., 1979); therefore, these <strong>fly</strong><strong>ash</strong>es did not fit the general pattern fordhe U.S. <strong>ash</strong>es. Additional workwith high-iron <strong>fly</strong> <strong>ash</strong>es is needed to provide a clearer indication <strong>of</strong> thedistribution <strong>of</strong> Ferrics <strong>and</strong> Fercalcics; few such <strong>fly</strong> <strong>ash</strong>es are completelycharacterized in the literature. However, the magnetic fractions <strong>of</strong> someFersics <strong>and</strong> Modics can be classified as Ferrics, as shown in Figure 5.Solvent extractionFive <strong>fly</strong> <strong>ash</strong>es were extracted with benzene. An amount <strong>of</strong> elemental sulfurequivalent to about 10% <strong>of</strong> the total extractable material in each <strong>ash</strong> wasco-extracted with the organic matter <strong>and</strong> interfered with the quantification

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