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Architecture and management of a geological repository - Andra

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5 – Repository ModulesIn terms <strong>of</strong> time, the conditions which in the short term govern evacuation <strong>of</strong> the heat produced by thepackages are different from those characterising the thermal behaviour <strong>of</strong> the <strong>repository</strong> in the longerterm. In the short term, the cells are in fact thermally independent <strong>of</strong> each other, while in the longerterm (more than three centuries), the "overall" heating <strong>of</strong> the <strong>repository</strong> zone leads to thermal couplingbetween the various units.To deal with this problem, a 3D finite-elements model was produced on the basis <strong>of</strong> three "nested"models (see Figure 5.1.10). Each <strong>of</strong> the three models is characterised by its own validity range:- the overall model on the scale <strong>of</strong> the site,- the median model on the scale <strong>of</strong> the <strong>repository</strong> module,- the local module on the scale <strong>of</strong> the disposal cell.The overall model (kilometre scale) represents the <strong>geological</strong> medium from the surface down to adepth <strong>of</strong> 3,500 m. The thermo-physical properties <strong>of</strong> the various <strong>geological</strong> layers are taken intoaccount. This general model can be used to calculate temperature evolutions over a period <strong>of</strong>10,000 years at numerous points located more than 50 m from the disposal packages. Over a periodsuch as this, the heat given <strong>of</strong>f by the packages has an influence over a distance <strong>of</strong> a kilometre <strong>and</strong> thevarious <strong>repository</strong> modules interact thermally with each other. This general model thus represents allthe <strong>repository</strong> modules <strong>and</strong> covers a lateral distance <strong>of</strong> 2,000 m around the <strong>repository</strong>.The median model is on the scale <strong>of</strong> the <strong>repository</strong> module (metre scale). Its geometricalrepresentation is less detailed than the local model but it does include the structures surrounding thecell (access drifts, seals, etc). The calculation is made by applying to the edges the limit conditionsobtained on the overall model.The local model allows a detailed representation <strong>of</strong> the various cell components with a high degree <strong>of</strong>geometrical precision (centimetre scale). It enables the temperature evolution to be evaluated for theimmediate environment <strong>of</strong> the cell for all types <strong>of</strong> packages in the <strong>repository</strong>. There are as many localmodels as there are exothermic type packages. This model is used by applying to the edges the limitconditions obtained on the previous median model. It represents all the cell components, the functionalclearances, the spacers <strong>and</strong> the access structures.Scale <strong>of</strong>the siteScale <strong>of</strong>severaldisposal cellsTemperaturesat the limits <strong>of</strong>the model aregiven by thelarger modelScale <strong>of</strong> onedisposal cellFigure 5.2.10"Nested" modelling principle usedDOSSIER 2005 ARGILE -ARCHITECTURE AND MANAGEMENT OF A GEOLOGICAL DISPOSAL SYSTEM205/495

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