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U.S. Department of Energy
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Radionuclide transport as vapor through unsaturated fractured rock. [Contains glossary]

Technical Report ·
OSTI ID:6215481
Transport mechanisms potentially important at larger distances include ordinary diffusion, viscous flow, and free convection. Ordinary diffusion includes self and binary diffusion, Knudsen flow, and surface diffusion. Pressure flow and slip flow comprise viscous flow. Free convective flow results from a gas density contrast. Transport mechanisms or processes dominant near the repository include ordinary diffusion, viscous flow plus several mechanisms whose driving forces arise from the non-isothermal, radioactive nature of high-level waste. The additional mechanisms include forced diffusion, aerosol transport, thermal diffusion and thermophoresis. Near a repository, vapor transport mechanisms and processes can provide a significant means of transport from a failed canister to the geologic medium from which other processes can transport radionuclides to the accessible environment. These issues are believed to be important factors that must be addressed in the assessment of specific engineering designs and site selection of any proposed high-level waste repository. 95 refs., 43 figs., 10 tabs.
Research Organization:
Arizona Univ., Tucson (USA). Dept. of Hydrology and Water Resources; Nuclear Regulatory Commission, Washington, DC (USA). Div. of Engineering
OSTI ID:
6215481
Report Number(s):
NUREG/CR-4654; ON: DE87900916
Country of Publication:
United States
Language:
English

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