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Architecture and management of a geological repository - Andra

Architecture and management of a geological repository - Andra

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5 – Repository ModulesFigure 5.3.14Longitudinal section through type CU1 <strong>and</strong> CU2 cellsThe temperature change <strong>of</strong> the wall <strong>of</strong> the clay buffer between 0 <strong>and</strong> 600 years (see Figure 5.3.15)shows that, for the dimensioning indicated in the table above, the temperature returns below the 70°Cthreshold well before 1 000 years, which meets the long-term thermal criterion.Température (C°)90807060504030CU2CU1 court shortCU1 long200 40 80 120 160 200 240 280 320 360 400 440 480 520 560 600Nombre Number d'années <strong>of</strong> aprés years after la mise disposal en stockageFigure 5.3.15Clay buffer wall temperature for spent fuelsThe dimensioning shown leads to a more rapid decrease in the temperature inside the argilite than intype C waste. This result may appear paradoxical, given the slower decrease in the heat rating <strong>of</strong> spentfuels; it is due to the large distances between packages imposed by the short-term thermal criterion.• Specific mechanical <strong>and</strong> thermo-mechanical dimensioning characteristics <strong>of</strong> spentfuel cellsThe sleeves <strong>of</strong> cells must maintain functional clearances that retain the capability to withdraw thepackages, for a period in the order <strong>of</strong> a few centuries. The dimensioning calculation is identical to thatfor type C waste, in both its purpose <strong>and</strong> assumptions. The only difference is the larger diameter <strong>of</strong> thecells.DOSSIER 2005 ARGILE -ARCHITECTURE AND MANAGEMENT OF A GEOLOGICAL DISPOSAL SYSTEM245/495

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