Performance Assessment Model for the National Radioactive Waste Repository in Mochovce, Slovakia


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Background

This model is a very simple draft model for initial evaluation of the feasibility of disposing low- and intermediate-level radioactive waste (LILW) and very-low-level waste (VLLW) at the Mochovce National Repository. These waste are produced by nuclear power plant operations and decomissioning.

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The Conceptual Site Model

This simple model assumes that the LILW is disposed in specialized fiber/concrete containers, and that the VLLW is disposed in bulk. Both of these forms of disposal are down eithin the larger, highly-engineered vaults that constitute the rectangular footprint of the repository. Water that infiltrates into the waste will remove contaminants, draining to a local creek, or to groundwater, which itself eventually drains to surface water as well.

Hypothetical receptor scenarios have not yet been developed, but a simple dose calculation for a future resident has been done to include a drinking water exposure pathway, as an example.

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The GoldSim Model

repository calculations The CSM is translated into a mathematical representation, focused on following the fate and transport of the radiological constituents from the waste form to hypothetical receptor locations. Meteoric waters migrate slowly through the engineered cap and into the zone containing the wastes. The VLLW, which is not in the specialized concrete containers, is more easily leached than the LILW, which is containerized. Both are placed within large concrete vaults, which are underlain by a transmissive layer of gravel. All of these features are accounted for in the GoldSim model.

environmental calculations Once the contaminant-bearing water has reached the bottom of the repository, it migrates into the environmental system. This is modeled as "columns" of GoldSim Cell pathways, representing the aquifer below. Single Cell pathways are used to represent surface water conveyances, since the trnapsort in these is rapid. These two pathways merge at the point that the groundwater emerges at a spring, and surface waters carry contamination, diluted by local hydrologic phenomena, to a small lake.

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Last modified: 9 July 2007