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The north ramp of the exploratory studies facility at Yucca Mountain provides access to a site characterization testing area for the proposed repository. The ramp is also used for site characterization data collection. If Yucca Mountain is found to be suitable for the disposal of radioactive material, the ramp will become part of the repository. |
The CNWRA aids the NRC in developing criteria with which to assess the adequacy of the license application to be submitted by the U.S. Department of Energy (DOE) for designing, constructing, operating, and ultimately closing an underground repository for spent nuclear reactor fuel and high-level nuclear wastes. Current emphasis is on a repository at Yucca Mountain, Nevada. Through a variety of research, inspection, and analysis activities, the CNWRA assists the NRC in formulating and providing guidance to the DOE, evaluating repository site characterization and design activities, and efficiently implementing the repository licensing process. These efforts will help determine whether the planned repository can adequately protect the radiological health and safety of the public in future millennia.
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A digital elevation map of the Yucca Mountain region is combined with a schematic cross section of the layers of volcanic rocks beneath the crest of the mountain. Plans call for excavation of the repository within the rock layers, which are cut by faults and dikes that have fed magma to Quaternary volcanoes like the Red and Black Cones (two larger cones at lower right). |
The CNWRA completed a multiyear laboratory and analytical investigation of cation exchange, the reaction kinetics and solubility of selected minerals, and conceptual and numerical geochemical modeling of repository systems. The investigation demonstrated that a simple thermodynamics formulation, the Margules equation, was adequate to predict ion exchange between aqueous solutions and a zeolite mineral that is commonly found in the Yucca Mountain vicinity.
Experimental and modeling studies continued on the chemical behavior of mineral phases important to radionuclide sorption. Scientists compared three mathematical models with laboratory data to assess the models' abilities to predict the effects of changing system chemistry on sorption rates. The models were found to match the experimental data well. Because the models are based on accepted geochemical principles, it is believed they will be effective in predicting most geochemical conditions of interest at Yucca Mountain.
Scale-model experiments, dimensional analyses, and numerical modeling were completed for a thermohydrology project. Results indicated that, for nonlinear thermohydrologic processes, dimensional analysis was not generally applicable. It was concluded that thermohydrologic experiments would have to be conducted at different scales to develop appropriate rules for scaling.
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An aerial view of the southwestern flank of Bare Mountain, Nevada, 15 km west of Yucca Mountain, shows a series of extensional faults (offset gray and white sedimentary layers). The Bare Mountain Fault, which forms the eastern boundary of Bare Mountain (cross section), is the most active fault in the immediate vicinity of Yucca Mountain. Styles of faulting and fault-related deformation in surface outcrops at Bare Mountain provide important constraints on interpretations of fault geometry and deformation mechanisms of the larger Bare Mountain Fault and related faults in the deep subsurface. Understanding such processes at Bare Mountain will lead to a more complete understanding of potential faulting and seismic hazards at Yucca Mountain. |
As part of an effort to understand the complex coupling of thermal, hydrological, chemical, and mechanical processes, a study of mechanical-hydrological coupling was initiated under the aegis of an international cooperative study on the development and validation of coupled models. Preliminary results indicate significant channeling of flow within rock joints and relatively large changes in permeability when the joints are subjected to normal and shear displacements.
To assess certain aspects of underground facility design, CNWRA research has focused on the effects of repeated seismic loads on the response of jointed rock masses. Reports published this year addressed the characterization of rock joints using a novel fractal approach, displacements near underground openings and changes in groundwater level caused by nearby mining-induced seismic events, and laboratory studies of single rock joints and scale-model underground openings.
Scientists completed a three-dimensional geologic framework model using EarthVision" software. This preliminary model includes eight stratigraphic units at Yucca Mountain, three potentially important faults, and the water table. Appropriate data are also being incorporated into an extensive geographic information system database to use during review of critical geochemical, hydrological, seismic, tectonic, and volcanological features of the proposed repository site.
The behavior of faults in the Yucca Mountain area will be important to repository performance. Studies this year examined factors influencing deformation in curved fault systems. In addition, software was developed to evaluate the tendency of faults and fractures to dilate or slip, depending on the orientation and magnitude of in situ stresses. Efforts to integrate this software into a three-dimensional dynamic simulation code are under way.
Because of its potentially significant consequences, the probability of volcanism in the vicinity of a repository continues to be a focus of investigation. The spatial distribution and timing of basaltic volcanism near the Yucca Mountain site were modeled using three nonhomogeneous methods to obtain nonparametric estimates of spatial and spatio-temporal recurrence rates. Active volcanoes are also being studied to evaluate the range of consequences of volcanic eruptions.
Engineers completed an experimental investigation of localized corrosion, stress corrosion cracking, materials thermal stability, and hydrogen embrittlement. The primary objective was to identify a critical parameter for predicting corrosion rates in waste container materials. It was found that the electrical potential below which corrosion stops can provide bounding values for long-term pitting, crevice corrosion, and stress corrosion cracking in nickel-based alloys. In addition, the CNWRA began to assess microbial effects on corrosion.
The CNWRA developed a computer code to demonstrate the ability to evaluate waste package containment in the context of regulatory requirements. In addition, a relatively simple repository geometry was used to simulate the evolution of potential waste-package environments. A two-phase flow model was used to calculate relative humidity in the vicinity of waste packages and to calculate the degree of saturation above and below the waste-emplacement horizon.
Studies were initiated under the third phase of the joint CNWRA-NRC iterative performance assessment effort. Investigations were selected based on previous studies that indicated either large uncertainty or high impact on repository performance. These include infiltration of water from natural sources, identification of key radionuclides, and assessment of exposure to future generations.
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