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234U238U and 230Th234U activity ratios in mineral phases of a lateritic weathered zone
Affiliation:1. Institute of Marine Sciences, National Research Council, Arsenale — Tesa 104, Castello 2737/F, 30122 Venezia, Italy;3. Dept. of Civil, Architectural and Environmental Engineering, University of Padova, Via Trieste 63, 35121 Padova, Italy
Abstract:A selective phase extraction procedure was developed for the identification of the significant phases of a typical deep soil profile sampled in the vicinity of the Ranger No. 1 uranium ore body, Alligator Rivers region, N.T., Australia. The significant phases were identified as amorphous iron oxide, crystalline iron oxide and a clay/quartz resistate. The distribution of 238U, 234U, 230Th and 226Ra between the phases was measured. The results indicated that the amorphous iron oxide phase is in adsorption/desorption equilibrium with the ground water. The crystalline iron oxide phase contains a chemical control, the kinetics of which are commensurate with or less than the half-life of 230Th (7.52 × 104 y). The clay/quartz resistate is enriched in 238U descendants in such a way that they are not readily accessible to the ground water.
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