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Plutonium Association with Selected Solid Phases in Soils of Rocky Flats, Colorado, Using Sequential Extraction Technique
Author(s) -
Litaor M. Iggy,
Ibrahim S. A.
Publication year - 1996
Publication title -
journal of environmental quality
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.888
H-Index - 171
eISSN - 1537-2537
pISSN - 0047-2425
DOI - 10.2134/jeq1996.00472425002500050030x
Subject(s) - environmental chemistry , plutonium , soil water , extraction (chemistry) , vadose zone , groundwater , tracer , environmental science , radionuclide , contamination , dissolution , chemistry , soil science , geology , radiochemistry , ecology , physics , geotechnical engineering , chromatography , quantum mechanics , biology , nuclear physics
Plutonium contamination in the soil environs of Rocky Flats, CO, has been a potential health risk to the public since the late 1960s. Although the measurement of total activity of Pu‐239 + 240 in the soil is important information in appraising this risk, total activity does not provide the information required to characterize the geochemical behavior that affects the transport of Pu from the soil and vadose zone to groundwater. A sequential extraction experiment was conducted to assess the geochemical association of Pu with selected mineralogical and chemical phases of the soil. In the surface horizons, Pu‐239 + 240 was primarily associated with the organic C (45–65%), sesquioxides (20–40%), and the residual fraction (10–15%). A small portion of Pu‐239 + 240 was associated with soluble (0.09–0.22%), exchangeable (0.04–0.08%), and carbonates (0.57–7.0%) phases. These results suggest that under the observed pH and oxic conditions, relatively little Pu‐239 + 240 is available for geochemically induced transport processes. Uncommon hydrogeochemical conditions were observed during the spring of 1995, which may have facilitated a partial dissolution of sesquioxides followed by desorption of Pu resulting in increased Pu mobility. Systematic errors in the sequential extraction experiment due to postextraction readsorption were evaluated using Np‐237 tracer as a surrogate to Pu‐239. The results suggested that postextraction readsorption rates were insignificant during the first 30 min after extraction for most chemical and mineralogical phases under study.