219-9 Speciation of Selenium and Other Heavy Metals Using X-Ray Absorption Spectroscopy in Coal Fly Ash at the Kingston Fossil Plant Site.

See more from this Division: S02 Soil Chemistry
See more from this Session: Chemistry of Metal(loids) and Trace Elements in Soils
Tuesday, November 2, 2010: 10:30 AM
Long Beach Convention Center, Room 202B, Second Floor
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Jennifer Seiter1, Mark Chappell2, Anthony Bednar1, Jacob Stanley1, Alan Kennedy1, Daniel Averett1 and Jeffery Steevens1, (1)Environmental Laboratory, U.S. Army Corps of Engineers, Vicksburg, MS
(2)Engineer Research and Development Center, US Army Corps of Engineers, Vicksburg, MS
The U.S. Army Engineer Research & Development Center (ERDC) conducted geochemical investigations of the coal fly ash spilled in the Emory River at the Kingston Fossil Plant.  Commissioned by the Tennessee Valley Authority (TVA), these investigations were designed to characterize the fly ash, in order to distinguish any changes or transformations that may have occurred during its submersion in the Emory River that would promote release of hazardous metals during cleanup dredging operations.  Fly ash samples were collected from the original source pile, the Emory River, and the ash recovery ditch, and brought back to the ERDC laboratory in Vicksburg, MS.  X-ray absorption spectroscopy (XAS) was used to identify metal(loid) speciation in the fly ash.  C and N profiles showed the ash had accumulated humics from the Emory River.  Fly ash manganese reduced to Mn (II) while Fe and other metals changed nominally, with the exception of fly ash selenium, which transformed from mostly selenite (Se(IV)) in the source pile to organoselenium (Se(II)) or thiol-bound forms.  A series of extended elutriate tests were performed by suspending collected samples in background Emory River water and bubbling extensively with either nitrogen (anoxic regime) or air (oxic regime) for 10 days.  These tests were designed to push the ash to redox and perturbation extremes to release metals, particularly selenium.  Metal species were identified using high-performace liquid chromatography inductively coupled plasma mass spectroscopy (HPLC-ICP-MS).  Both anoxic and oxic regimes released similarly low concentrations of metals through dissolution driven by the prolonged gas bubbling.  Liquid speciation of the solution phase measured low concentrations of selenite, while on the solid phase, selenium was dominated by a mixture of selenite and organoselenium.  The results indicate that while the fly ash exhibits geochemical stability, it is undergoing kinetically slow transformations while submerged in the Emory River. 
See more from this Division: S02 Soil Chemistry
See more from this Session: Chemistry of Metal(loids) and Trace Elements in Soils