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Radionuclide Transport by Groundwater Colloids at the Koongarra Uranium Deposit
Published online by Cambridge University Press: 25 February 2011
Abstract
Groundwater and entrained particles were sampled from several boreholes at the Koongarra uranium deposit in the Northern Territory of Australia. Conventional filtration techniques, hollow fibre ultrafiltration, and stirred-cell ultrafiltration were used to separate dissolved species, large particles (> 1 μm) and colloids (< 1 μm). The colloids and particles included clay minerals, particularly kaolinite, and chlorite, together with fine quartz grains. Iron was present as particle coatings, and in a separate colloidal form. The amount of 238U associated with colloids (expressed as a percentage of the total 238U which passed through the 1.0 μm filter) ranged up to 6.5%. The corresponding figures for Th were 10-85%. However, the amount of 230Th which passed through the 1.0 μm filter was extremely small, and 230Th was associated to a much greater extent with larger particles, which are unlikely to be mobile in natural groundwaters. In some fine particle and colloidal fractions, the 227Th/230Th activity ratio in the thorium alpha spectrum was unusually high, indicating the presence of substantial quantities of 227Ac. This suggested that actinium could be present as a mobile colloid phase. Overall, there was very little colloidal material in these groundwaters, with only iron, uranium, actinium, and thorium showing a significant association with colloids.
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- Copyright © Materials Research Society 1992
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