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Natural attenuation of coal combustion waste in river sediments
Authors:James T Markwiese  William J Rogers  Neil E Carriker  David I Thal  Rock J Vitale  Jacob G Gruzalski  Erin E Rodgers  Carol M Babyak  Randall T Ryti
Institution:1. Environmental Standards, Inc., 8331 E. Walker Springs Lane, Suite 402, Knoxville, TN, 37923, USA
2. Tennessee Valley Authority, Kingston, TN, USA
3. Environmental Standards, Inc., Valley Forge, PA, USA
4. A.R. Smith Department of Chemistry, Appalachian State University, Boone, NC, USA
5. Neptune and Company, Inc., Los Alamos, NM, USA
Abstract:The weathering of coal combustion products (CCPs) in a lotic environment was assessed following the Tennessee Valley Authority (Kingston, TN) fly ash release of 2008 into surrounding rivers. Sampled materials included stockpiled ash and sediment collected from 180 to 880 days following the release. Total recoverable concentrations of heavy metals and metalloids in sediment were measured, and percent ash was estimated visually or quantified by particle counts. Arsenic and selenium in sediment were positively correlated with percent ash. For samples collected 180 days after the release, total concentrations of trace elements downstream of the release were greater than reference levels but less than concentrations measured in stockpiled ash. Total concentrations of trace elements remained elevated in ash-laden sediment after almost 2.5 years. A sequential extraction procedure (SEP) was used to speciate selected fractions of arsenic, copper, lead, nickel, and selenium in decreasing order of bioavailability. Concentrations of trace elements in sequentially extracted fractions were one to two orders of magnitude lower than total recoverable trace elements. The bulk of sequentially extractable trace elements was associated with iron-manganese oxides, the least bioavailable fraction of those measured. By 780 days, trace element concentrations in the SEP fractions approached reference concentrations in the more bioavailable water soluble, ion exchangeable, and carbonate-bound fractions. For each trace element, the percentage composition of the bioavailable fractions relative to the total concentration was calculated. These SEP indices were summed and shown to significantly decrease over time. These results document the natural attenuation of leachable trace elements in CCPs in river sediment as a result of the loss of bioavailable trace elements over time.
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