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Tome Architecture and management of a geological repository - Andra

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4 - General architecture <strong>of</strong> the <strong>repository</strong> in a granite mediumAmong available technical solutions, construction <strong>of</strong> low permeability seals combined with the use <strong>of</strong>slightly "tamped" backfilling materials is currently considered.Seals <strong>of</strong> a similar design to those used in the <strong>repository</strong> connecting drifts are installed in all driftsserving an access structure (shaft <strong>and</strong>/or ramp). The shaft base is cemented to a height <strong>of</strong> about twentymetres above the upper level <strong>of</strong> the <strong>repository</strong>. The volume over this concrete filling is entirelybackfilled up to a level about twenty metres below the leak-tight lining emplaced at the top <strong>of</strong> the shaftwhere a seal is constructed. The backfilling <strong>of</strong> the upper part, above the seal, completes the closureoperation.• Seals in the access structuresAt the current stage <strong>of</strong> the study the seals comprise a swelling clay core mechanically confined by twoconcrete abutments anchored in the formation.The seals are installed in the portions <strong>of</strong> the shaft or ramp excavated with methods limiting walldamage.The concrete lining <strong>and</strong> damaged zone at the edge <strong>of</strong> the drifts <strong>and</strong> right above each seal are cut out(diamond-tipped cable or disk sawing). Cutting is continued in the granite beyond the damaged zonethrough a thickness <strong>of</strong> about 1 m.The coupling between the seal core <strong>and</strong> the "sound" granite develops as the clay swells. The seal core,tens <strong>of</strong> metres high, also includes a buffer thickness to compensate for any deferred tamping <strong>of</strong> thebackfill, in the event <strong>of</strong> concrete abutment failure. Two solutions are envisaged for clay coreemplacement: tailored stacking <strong>of</strong> pre-compacted bricks or in situ filling with compacted pellets. Inboth cases, provision is made for inserting a device to collect any sweeping water on the shaft wall(gutters, weepholes), upstream <strong>of</strong> the sealing zone, in order to maintain favourable conditions for theconstruction <strong>of</strong> the clay core.The core is mechanically limited by two concrete abutments, dimensioned to withst<strong>and</strong> the swellingpressure <strong>of</strong> the clay <strong>and</strong> the effective mass <strong>of</strong> the backfill materials emplaced higher up inside theshaft. Dimensioning these retaining plugs (shape <strong>and</strong> height) has yet to be made.The seal for the ramp is similar to those planned for the <strong>repository</strong> drifts• Backfilling the access structuresOnly mechanical performance is envisaged at this stage for the access structures backfill. The particlesize <strong>of</strong> the granite aggregate should minimise the voids after in situ compacting.The addition <strong>of</strong> a fraction <strong>of</strong> swelling clay to compensate for the deferred tamping efects may beenvisaged. Resort to this option should consider a draining water collection system upstream <strong>of</strong> thecompacting worksite.4.3 Disposal processThe industrial commissioning <strong>of</strong> the installations starts with the reception <strong>of</strong> the first packages on thesite <strong>and</strong> their emplacement in the first constructed disposal cells. Simultaneously, construction work <strong>of</strong>new structures could gradually start while packages are emplaced in disposal cells. Operation <strong>of</strong> areversible disposal facility is characterised by the coexistence <strong>of</strong> construction activities (including ongoing<strong>geological</strong> surveying) <strong>and</strong> package emplacement, <strong>and</strong> also by the progressive feature <strong>of</strong> theseactivities.Dossier 2005 Granite - ARCHITECTURE AND MANAGEMENT OF A GEOLOGICAL REPOSITORY77/228

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