Hydrogeochemical modelling of an active system of uranium fixation by organic soils and sediments (Needle's Eye,Scotland) |
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| Authors: | P Jamet P J Hooker J M Schmitt E Ledoux P Escalier Des Orres |
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| Institution: | (1) Ecole des Mines de Paris, Centre d'Informatique Géologique, 35 rue Saint-Honoré, F-77305 Fontainebleau Cedex, France;(2) Fluid Processes Research Group, British Geological Survey, NG12 5GG Keyworth, Nottingham, UK;(3) Commissariat à l'Energie Atomique, Institut de Protection et de Sûreté Nucléaire, BP 6, F-92265 Fontenay-aux-Roses, France |
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| Abstract: | Uranium accumulation in organic-rich sediments can be closely modelled by assuming that the dominant effect of the uranium-organic matter interaction is the direct or indirect reduction of uranyl compounds to form U(IV) minerals, especially uraninite-pitchblende. Application of this model to the Needle's Eye (Scotland) site where uranium is actively accumulating in Quaternary sediments demonstrates that uranium accumulation is both effective and rapid in environments involving shallow, organic-rich, reducing horizons. The period of uranium deposit formation at Needle's Eye is estimated to be as short as 5000 years. The transport of uranium to the site of deposition by oxidizing groundwaters and the channelling of these oxidizing uraniferous groundwaters are identified as important factors involved in the rapid accumulation of uranium. The regional hydrogeological model indicates that a fault in the area appears to act as a hydraulic screen for the uraniferous groundwaters. On one side of the fault the Quaternary sediments are well drained whilst on the other the flow of groundwater seeps out creating a major flux just at the bottom of the organic-rich layers. The local hydrogeological model shows that the groundwater flow is vertical in this area. A third significant factor in the development of these uranium accumulations is the presence of a significant nearby source of leachable primary uranium. In the case of the Needle's Eye site this is in the form of some thirty 185 ±20 Ma, pitchblende-bearing veins. |
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