2008
DOI: 10.1016/j.coal.2007.09.002
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Assessment of elements, speciation of As, Cr, Ni and emitted Hg for a Canadian power plant burning bituminous coal

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Cited by 139 publications
(74 citation statements)
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“…Nickel was mostly found in oxide form in Canadian coal (Goodarzi et al, 2008), and Ni-bearing minerals (spinels and illites) are common in coalfields close to ultramafic bodies (Ruppert et al, 1996), whilst sulphide minerals containing Ni have been also reported (Finkelman, 1995). Whatever the association in coal, Ni seems to be distributed between the silicate fraction and the magnetic fraction of fly ash during combustion.…”
Section: Nickelmentioning
confidence: 99%
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“…Nickel was mostly found in oxide form in Canadian coal (Goodarzi et al, 2008), and Ni-bearing minerals (spinels and illites) are common in coalfields close to ultramafic bodies (Ruppert et al, 1996), whilst sulphide minerals containing Ni have been also reported (Finkelman, 1995). Whatever the association in coal, Ni seems to be distributed between the silicate fraction and the magnetic fraction of fly ash during combustion.…”
Section: Nickelmentioning
confidence: 99%
“…Chromium appears to occur in most bituminous coals as Cr 3+ in organic association and primarily as Cr 3+ in illite (Goodarzi et al, 2008;Huggins and Huffman, 2004;Huggins et al, 2000a;Ruppert et al, 1996), whereas there is little evidence for the presence of Cr 6+ (Huggins et al, 1999). The occurrence in illite gives rise to an aluminosilicate association (primarily in glass) in fly ash, remaining as Cr 3+ (Goodarzi et al, 2008;Spears, 2004;Spears and MartinezTarrazona, 2004).…”
Section: Chromiummentioning
confidence: 99%
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