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AbstractAbstract
[en] The behavior of plutonium in soil--water systems was studied by measuring its apparent diffusion coefficient in the aqueous and solid phases and by finding the adsorption--desorption relationships between soil and solution. Apparent diffusion coefficients of plutonium in soil were measured using a quick-freeze method. Aqueous diffusion was studied in a capillary-tube diffusion cell. Adsorption studies were done by equilibrating a tagged soil--water mixture on a rotary shaker before centrifuging and sampling. As expected from high adsorption coefficients (Kd) (300--10,000), the apparent diffusion coefficients were low compared with normal soil cations (1.4 x 10-8 cm2/sec in a sandy soil to less than 2.4 x 10-11 cm2/sec in a silt loam). The Kd of plutonium in aqueous solution containing the chelate ethylenediaminetetraacetic acid (EDTA) was reduced compared with the Kd in dilute HNO3. As the EDTA concentration was increased, the Kd was decreased. The chelate diethylenetriaminepentaacetic acid (DTPA) reduced the Kd more than EDTA at comparable concentrations. The aqueous diffusion coefficients varied from 3.1 x 10-7 cm2/sec in a solution extracted from the silt loam up to 2.7 x 10-5 cm2/sec in a solution extracted from the sandy soil
Original Title
238Pu
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Source
Adriano, D.C.; Brisbin, I.L. Jr. (eds.); Department of Energy, Oak Ridge, TN (USA). Technical Information Center; p. 479-494; 1978; p. 479-494; 2. mineral cycling symposia on environmental chemistry and cycling processes; Augusta, GA, USA; 28 Apr - 1 May 1976
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Report
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Conference
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