240 Coal Geology (Posters): New Developments in Environmental and Geochemical Coal Research
Wednesday, 12 October 2011
9:00 AM - 6:00 PM
Hall C
SPECIATION AND RELEASE OF SELENIUM IN COAL ASH FROM THE TENNESSEE VALLEY AUTHORITY KINSTON FOSSIL PLANT
Paper number: 240-3
Program: Technical Sessions
Time: 9:00 AM – 6:00 PM
Authors
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William Greer MackebeeDuke University, Durham, NC
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Heileen Hsu-KimDuke University, Durham, NC
Abstract
In general, dissolved Se in leachates showed a minimum concentration at pH 5 to 6, and increased as pH decreased below 5 and as pH increased above 6. The pH-dependent Se leaching pattern was relatively similar for all materials tested. The release of Se at low pH could be presumably ascribed to the dissolution of coal ash materials under acidic conditions. The increase in Se in leachates at pH > 6 was likely caused by the desorption of Se oxyanions (e.g. selenite and selenate) and the release of organo-Se (e.g. selenocystine and selenomethionine) as indicated by the results of HPLC-ICP-MS analysis. With an exception of one fly ash sample (out of 6), the XANES results showed that the sum of selenite, selenate, selenocystine, and selenomethionine in original coal ash materials is positively correlated (r2 = 0.92) with the total concentration of Se released at their natural pH condition (pH 7.6 – 9.5). Our results demonstrated that both Se oxyanions and organo-Se should be considered as labile Se. Conclusively, Se speciation is a potential method to evaluate the environmental risk pertaining to Se release from coal ash spills.