An approach to the mathematical modelling of the uranium series redistribution within ore bodies. [Australia]
The distributions of the uranium series isotopes in the Koongarra ore body were predicted by a simple one-dimensional model of isotopic migration parameters. Controlling the predictions were the retardation factors and the groundwater flow rates. The conditions modelled were a groundwater flow rate of 1 meter per year, retardation factors of 1 x 10/sup 4/ for /sup 238/U and of 1.2 x 10/sup 4/ for /sup 234/U, and /sup 230/Th is immobile. For this set of conditions, an exceptionally good agreement was observed between field-measured isotope ratios and ''predicted'' isotope ratios. A multiphase model adequately describes the redistribution of uranium and daughter radionuclides in the weathered zone of the ore bodies. It redistributes U, Th and Ra isotopes among an aqueous phase, an amorphous iron phase, a crystalline phase and a phase of clay and quartz. 28 refs., 26 figs., 8 tabs.
- Research Organization:
- Australian Atomic Energy Commission, Lucas Heights. Lucas Heights Research Labs.
- OSTI ID:
- 5599597
- Report Number(s):
- NUREG/CR-5060; AAEC/C-49; ON: TI88900260
- Country of Publication:
- United States
- Language:
- English
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RADIONUCLIDE MIGRATION
MATHEMATICAL MODELS
URANIUM ORES
ANALOG SYSTEMS
AUSTRALIA
COMPUTERIZED SIMULATION
FLOW RATE
GROUND WATER
HIGH-LEVEL RADIOACTIVE WASTES
NORTHERN TERRITORY
RADIOACTIVE WASTE DISPOSAL
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ORES
OXYGEN COMPOUNDS
RADIOACTIVE MATERIALS
RADIOACTIVE WASTES
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