Abstract
We have developed a sequential extraction technique for determining the geochemical partitioning of Am, Pu, and U in soils and sediments. Stable element analyses were combined with radiometric measurements to determine the most probable geochemical host phases of these actinides in reference sediment IAEA-135.241 Am results indicate an association with carbonate minerals and organic matter. The extraction profile of238U was similar to that of refractory elements Al, Ti, and K.239/240Pu data suggest a fractionation of Pu into Fe-bearing phases of varying solubility. The reproducibility of the method was quite good (replicates agreed to within 10% at a 95% confidence level).
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Schultz, M.K., Burnett, W., Inn, K.G.W. et al. Geochemical partitioning of actinides using sequential chemical extractions: Comparison to stable elements. J Radioanal Nucl Chem 234, 251–256 (1998). https://doi.org/10.1007/BF02389780
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DOI: https://doi.org/10.1007/BF02389780