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Tome Architecture and management of a geological repository - Andra

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7 - Spent fuel <strong>repository</strong> zoneevent, it is possible to reverse the process, backtracking to an earlier stage, right back to packageretrieval, even if the deconstruction <strong>of</strong> more substantial closure structures is required as closureprogresses further.7.7 Functions <strong>of</strong> the <strong>repository</strong> components over timeThe previous sections describe the various components <strong>of</strong> a spent fuel <strong>repository</strong>. They specify themeans used to construct a reversible disposal system. They expose the principles at the basis <strong>of</strong> theirdesign <strong>and</strong> dimensioning for long-term safety.The following table summarises how the various components contribute to the main functions <strong>of</strong> a<strong>repository</strong> during the various <strong>repository</strong> phases (§ 1.1).Table 7.7.1Functions <strong>of</strong> the <strong>repository</strong> components over timeCOMPONENTPERIODMAIN REPOSITORYFUNCTIONSPROPERTIES HARNESSEDPart <strong>of</strong> the graniterock where a disposalcell is installedGranite "block"where the disposalmodule is installedDuringoperation<strong>and</strong> thereversibilityphaseAfter closureAfter closure1. GEOLOGICAL MEDIUM: GRANITEEmplacing (<strong>and</strong> being able toretrieve) the packages in thecellsProtecting the disposal cellsfrom water circulationDelaying <strong>and</strong> reducingradionuclides migration to theenvironmentProtecting the disposal cellsfrom water circulationDelaying <strong>and</strong> reducingradionuclides migration to theenvironmentMechanical strengthVery low permeabilityChemical properties <strong>of</strong> the granitewater that tend to delay radionuclidemigration (reducing environment,pH, etc.)Low permeability (at a distance fromthe significant water-conductingfractures)Low underground hydraulic gradientsChemical properties <strong>of</strong> the granitewater that tend to delay radionuclidemigrationUnderground installation <strong>of</strong> the<strong>repository</strong> (500 m taken as reference)Protecting the disposal cellsfrom water circulationLow permeability (at a distance fromthe major faults, the main vectors <strong>of</strong>water in the massif)Low underground hydraulicgradientsThe <strong>repository</strong> part<strong>of</strong> the host granitemassifAfter closureDelaying <strong>and</strong> reducingradionuclides migration to theenvironmentChemical properties <strong>of</strong> the granitewater that tend to delay radionuclidemigrationGeo-dynamic context that ensuresfavourable <strong>repository</strong> conditions aremaintained in the long term,particularly in relation to erosionphenomenaIsolating the waste from humanactivitiesDossier 2005 granite - ARCHITECTURE AND MANAGEMENT OF A GEOLOGICAL REPOSITORY218/228

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