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Architecture and management of a geological repository - Andra

Architecture and management of a geological repository - Andra

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Figure 10.2.4Diagrammatic representation <strong>of</strong> the principal phenomena within a type B wastedisposal cell after closing.• Evolution <strong>of</strong> the access drift <strong>and</strong> sealIn the access drift, stopping the ventilation, as in the cell, causes very slow re-saturation <strong>of</strong> the rock.Over several centuries, the wall rock <strong>and</strong> liner concrete are again significantly de-saturated, as is thesealing clay [8], [66]. The swelling <strong>of</strong> the sealing clay caused by re-saturation thus remains verylimited, or even non-existent, during the operation <strong>of</strong> the <strong>repository</strong>.In the access drifts to cells containing only slightly exothermic waste, sealing considerably slowsdown heat propagation; the temperature at the downstream end <strong>of</strong> the seal in the accessible zoneincreases by only a few degrees. Furthermore, as with the cell liner concrete, the concrete either side<strong>of</strong> the clay seal remain intact for several centuries or much longer.The small change to the seal over a period <strong>of</strong> several centuries [85] facilitates its eventual dismantlingin the event <strong>of</strong> reversing the disposal process in order to retrieve the packages or simply to return tooperating conditions close to those <strong>of</strong> a storage facility.• Possibilities available for taking action <strong>and</strong> possible duration <strong>of</strong> the stageAt this stage, it remains technically possible to retrieve the packages using means similar to those usedwhen inserting the packages, thanks to having maintained the functional clearances in the cell, as longas the latter is mechanically stable, i.e. for several centuries after its construction. It would howeverrequire preparatory work whose technical content, as described in section 10.4, could be adaptedaccording to the condition <strong>of</strong> the cell, established by analysing the results <strong>of</strong> observation.The observation <strong>of</strong> the liner <strong>and</strong> the terrain thrust on the liner, associated with temperaturemeasurements within the cell, can be carried out for as long as possible in order to establish soundknowledge <strong>of</strong> the effective condition <strong>of</strong> the cell.Monitoring <strong>of</strong> the quantities <strong>of</strong> gas actually emitted in the cell <strong>and</strong> evacuated by ventilation during theprevious stage, make it possible to detail the precise gas production kinetics <strong>and</strong>, thus, more accuratelypredict the quantities <strong>of</strong> gas trapped in the cell after closing.DOSSIER 2005 ARGILE -ARCHITECTURE AND MANAGEMENT OF A GEOLOGICAL DISPOSAL SYSTEM374/495

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