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Salt Disposal of Heat-Generating Nuclear Waste

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6. Damage Induced Permeability. Mechanically or hydraulically<br />

induced permeability is based on the same microphysical process <strong>of</strong><br />

percolation flow along grain boundaries after exceeding a threshold. In<br />

both cases the induced permeability is created by removal <strong>of</strong> intergranular<br />

cohesion.<br />

7. Consolidation <strong>of</strong> Hot Granular <strong>Salt</strong>. Crushed salt used as backfill<br />

may be an important element in a potential HLW repository. Relatively<br />

little elevated temperature mechanical testing has been conducted for<br />

crushed salt. The accelerating effect <strong>of</strong> moisture on consolidation needs<br />

further investigation. Modeling concerned with long-term, low-porosity,<br />

two-phase flow is likely required.<br />

8. Solubility and Transport. The salt repository community continues to<br />

research radionuclide solubility as if there will be ample brine available<br />

within the salt to dissolve and transport the waste. There are at least two<br />

parts to this important issue: one concerns brine sources and volume, and<br />

the other concerns existence <strong>of</strong> a pressure gradient capable <strong>of</strong> driving the<br />

soluble radionuclides to the biosphere.<br />

9. Degradation. This research area addresses the underlying hypothesis that<br />

waste forms placed in salt will degrade sufficiently that the residue can be<br />

removed readily by a human drilling intrusion.<br />

10. Radiolysis. Radiation is known to liberate hydrogen but further data are<br />

needed on the effect <strong>of</strong> combining radiation and temperature on the waste<br />

materials, waste packages, and the salt.<br />

11. Climate Changes. The radioactivity <strong>of</strong> nuclear waste will decay over a<br />

period <strong>of</strong> time (100,000 years or longer) in which major environmental<br />

changes are possible. Climate driven changes such as glaciation,<br />

permafrost, and changes in sea level could affect the subsurface<br />

environment <strong>of</strong> a salt formation and must therefore be considered in<br />

performance and safety assessments.<br />

4.7.2 Future Direction<br />

The topics given above pertain to specific phenomena, several <strong>of</strong> which could be<br />

incorporated into the next generation <strong>of</strong> repository performance assessment and<br />

supporting models. Future directions for research collaborations could be tw<strong>of</strong>old:<br />

(1) exploring fundamental processes using laboratory investigations and<br />

(2) exercising powerful new computational tools.<br />

Stone et al. (2010) have completed fully coupled, three-dimensional (3-D),<br />

thermal-mechanical simulations for a generic salt disposal scheme. These<br />

calculations demonstrate the available tools for coupled, multiphysics modeling<br />

and repository systems engineering. Several aspects <strong>of</strong> this nonlinear, thermalmechanical<br />

analysis are especially important. Past analyses <strong>of</strong> salt creep and room<br />

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