Abstract
The spatial distribution of U-238-series radionuclides, specifically U-238, U-234, Th-230 and Ra-226, has been determined in stream sediments from Edale, Derbyshire, United Kingdom, to explore the behaviour of U-series radionuclides during weathering. For uranium and thorium, two different extraction methods were used, total dissolution with HNO3/HF in a microwave and leaching with aqua regia. This was followed by radiochemical separation using extraction chromatography, then alpha spectrometry measurement. The total radium contents in the sediments were measured using gamma spectrometry, while the leached fraction was measured in the same way as for uranium and thorium. The total sediment content of uranium and thorium ranges from similar to 10 up to similar to 200 Bq kg(-1), while the radium specific activity lies between-15 and 180 Bq kg(-1). In the aqua regia extractions, the uranium and thorium contents are in the range of similar to 5 to similar to 100 Bq kg(-1), while the radium specific activities are similar to those measured by total dissolution. All the radionuclides show no correlation with organic matter content. The activity ratios U-234/U-238, Th-230/U-238 and Ra-226/U-238 were used to determine the degree of radioactive disequilibrium. The data show disequilibrium in most of the sediments, with activity ratios of U-234/U-238, Th-230/U-238 and Ra-226/U-238 > 1, inconsistent with evolution through straightforward weathering processes. Multivariate cluster analysis based on five variables, the specific activities of U-238, U-234, Th-230, Ra-226 and loss on ignition, was employed to group the data and identify five distinct clusters. There seems to be a link between high radionuclide concentrations and proximity to landslips.