HR: 0830h
AN: H11G-0948    [PDF]
TI: Mountain-Scale Transport of Radioactive Solutes and Colloids Through the Unsaturated Zone of Yucca Mountain, Nevada
AU: * Moridis, G J
EM: gjmoridis@lbl.gov
AF: Lawrence Brekeley National Laboratory, 1 Cyclotron Rd., ESD, MS 90-1116, Berkeley, CA 94720 United States
AU: Seol, Y
EM: YSeol@lbl.gov
AF: Lawrence Brekeley National Laboratory, 1 Cyclotron Rd., ESD, MS 90-1116, Berkeley, CA 94720 United States
AB: The US Department of Energy is actively investigating the technical feasibility of permanent disposal of high-level nuclear waste in an appropriate repository to be situated in the unsaturated zone (UZ) at Yucca Mountain (YM), Nevada. The objectives of this study are to evaluate the transport of radioactive solutes and colloids under ambient conditions from the potential repository horizon to the water table and to determine processes and geohydrologic features that significantly affect radionuclide transport. The radionuclide transport model considers the site hydrology, and the effects of the spatial distribution of hydraulic and transport properties in the fractured rocks of the YM subsurface. Several radionuclides (solutes and colloids) with varying properties are investigated. The results of the study indicate that the most important factors affecting radionuclide transport are the subsurface geology and site hydrology, i.e., the presence of faults (they dominate and control transport), fractures (the main migration pathways), and the relative distribution of zeolitic and vitric tuffs. Radioactive decay, diffusion from the fractures into the matrix, and subsequent sorption (for solutes) or filtration (for colloids) onto, are the main retardation processes. For solutes, arrival times at the watertable increase with the sorption distribution coefficients of the various species, and may have to account for contributions from the decay daughters of certain radionuclides. Changes in future climatic conditions can have a significant effect on transport, as increasing infiltration leads to faster transport to the water table. The transport of colloids is strongly influenced by their size (as it affects diffusion into the matrix, straining at hydrogeologic unit interfaces and transport velocity) and by the fracture attributes.
DE: 1829 Groundwater hydrology
DE: 1831 Groundwater quality
DE: 1832 Groundwater transport
SC: Hydrology [H]
MN: 2003 Fall Meeting