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Assessing the fate of radioactive nickel in cultivated soil cores
Authors:Sbastien Denys  Guillaume Echevarria  Louis Florentin  Elisabeth Leclerc  Jean-Louis Morel
Institution:aLaboratoire Sols et Environnement, UMR 1120 ENSAIA-INPL/INRA, 2, av. de la Forêt de Haye, BP. 172, 54 505 Vandoeuvre-lès-Nancy, France;bAndra, Agence Nationale pour la gestion des déchets radioactifs, 1-7 rue Jean Monnet, 92 290 Chatenay-Malabry, France
Abstract:Parameters regarding fate of 63Ni in the soil–plant system (soil: solution distribution coefficient, Kd and soil plant concentration ratio, CR) are mostly determined in controlled pot experiments or from simple models involving a limited set of soil parameters. However, as migration of pollutants in soil is strongly linked to the water migration, variation of soil structure in the field and seasonal variation of evapotranspiration will affect these two parameters. The aim of this work was to explore to what extent the downward transfer of 63Ni and its uptake by plants from surface-contaminated undisturbed soil cores under cultivation can be explained by isotopic dilution of this radionuclide in the pool of stable Ni of soils. Undisturbed soil cores (50 cm × 50 cm) were sampled from a brown rendzina (Rendzic Leptosol), a colluvial brown soil (Fluvic Cambisol) and an acidic brown soil (Dystric Cambisol) using PVC lysimeter tubes (three lysimeters sampled per soil type). Each core was equipped with a leachate collector. Cores were placed in a greenhouse and maize (DEA, Pioneer®) was sown. After 44 days, an irrigation was simulated at the core surfaces to supply 10 000 Bq 63NiCl2. Maize was harvested 135 days after 63Ni input and radioactivity determined in both vegetal and water samples. Effective uptake of 63Ni by maize was calculated for leaves and kernels. Water drainage and leaching of 63Ni were monitored over the course of the experiment. Values of Kd in surface soil samples were calculated from measured parameters of isotopic exchange kinetics. Results confirmed that 63Ni was strongly retained at the soil surface. Prediction of the 63Ni downward transfer could not be reliably assessed using the Kd values, since the soil structure, which controls local water fluxes, also affected both water and Ni transport. In terms of 63Ni plant uptake, the effective uptake in undisturbed soil cores is controlled by isotope dilution as previously shown at the pot experiment scale.
Keywords:Risk assessment  Nickel-63  Distribution coefficient  Concentration ratio  Undisturbed soil cores  Maize  Water drainage
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