Principle
Waste is placed in rooms 2,150 feet (655 m) underground that have been excavated within a 3,000 foot (1000 m) thick salt formation (Salado and Castile Formations) where salt tectonics has been stable for more than 250 million years. Because of plasticity effects, salt and water will flow to any cracks that develop, a major reason why the area was chosen as a host medium for the WIPP project. Because drilling or excavation in the area will be hazardous long after the area is actively used, there are plans to construct markers to deter inadvertent human intrusion for the next ten thousand years.
The Salado Formation is a massive bedded salt deposit (>99% NaCl) that has a simple hydrogeology. Because massive NaCl is somewhat plastic and holes close under pressure, the rock becomes non-porous by effectively closing pores and fractures. This has a significant effect on the overall hydraulic conductivities (water permeabilities) and molecular diffusion coefficients. These are on the order of ≤10−14 m/s and ≤10−15 m2/s respectively.
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Storage of radioactive waste at WIPP
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Labeled 100-gallon drums staged for downloading and emplacement in the repository
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The DOSCO rotary head mining machine at WIPP
Read more about this topic: Waste Isolation Pilot Plant
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