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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 Modules• Particular case <strong>of</strong> the resaturation periodDuring resaturation <strong>of</strong> a structure, flows in the argilite converge towards this structure. If theresaturation periods <strong>of</strong> adjacent structures are different, they can lead to transfer <strong>of</strong> water from onestructure to the next. If the cells reach saturation first, flows can occur towards the as yet unsaturatedaccess drift <strong>and</strong> are liable to transport any radionuclides released by the packages.The disposal concept presented here comprises a number <strong>of</strong> factors which contribute to limiting thepossibility <strong>of</strong> convective transport in the cell: hydraulic closure <strong>of</strong> the cell, cell dimensions limiting theintercepted water flow, elongation limiting the axial rate <strong>of</strong> the water for a given intercepted flow.• Production <strong>and</strong> fate <strong>of</strong> gases (corrosion hydrogen) in the C cellsWhen decided on as part <strong>of</strong> reversible <strong>management</strong>, closure <strong>of</strong> the structures leads to them beinggradually resaturated by the water from the argilites <strong>and</strong> that <strong>of</strong> the surrounding rock, if there wasdesaturation during the operating phase. Given the low permeability <strong>of</strong> argilites, this is a slow process.It is accompanied by the production <strong>of</strong> hydrogen as a result <strong>of</strong> corrosion <strong>of</strong> the metal components,which delays the return to complete saturation.The very slow corrosion rates (a few microns/year, or probably even a few tenths <strong>of</strong> a micron/year)lead to a period <strong>of</strong> several thous<strong>and</strong> years (about 5,000 years) for the main hydrogen production phase.The modelling conducted on the basis <strong>of</strong> experimental work with samples <strong>and</strong> a borehole led to anassessment <strong>of</strong> the properties <strong>of</strong> hydrogen transfer in the argilites. It shows that hydrogen transfer takesplace first <strong>of</strong> all by dissolution, <strong>and</strong> then by diffusion through the Callovo-Oxfordian. When the wateris saturated with hydrogen, this then follows two-phase migration, principally through areas with thelowest gas inlet pressures (close to 2 to 3 MPa for the initial ruptured/damaged zone, as compared with5 to 7 MPa for sound argilites). If hydrogen production is faster than its migration, this is expressed ingaseous form <strong>and</strong> the gas pressure can reach the porosity threshold <strong>of</strong> the argilites (micro-fissures) or<strong>of</strong> the swelling clay engineered components (cell plugs). Opening up <strong>of</strong> micro-fissures enables the gasto escape <strong>and</strong> the pressure may drop. It was found on the samples <strong>and</strong> during a borehole test that themicro-fissures close up after the gas passes, without altering the properties <strong>of</strong> the rock (the waterpermeability <strong>of</strong> the argilite remains unchanged) ([62] <strong>and</strong> [6] - Tome 2). Finally, when the pressurehas dropped enough for the hydrogen to be no longer able to enter the porosity <strong>of</strong> the variouscomponents, it slowly evacuates in dissolved form.5.2.1.4 Module separationThe design <strong>of</strong> the C waste disposal zones involves division into about ten subassemblies, in order tominimise the consequences <strong>of</strong> an altered situation (failure or intrusion). These subassemblies areisolated from each other by seals in their access drifts.The sealing <strong>of</strong> each cell also contributes to limiting the impact <strong>of</strong> any such altered situation.5.2.1.5 ReversibilityReversibility is designed to maintain flexible <strong>management</strong> <strong>of</strong> the <strong>repository</strong> packages, cells <strong>and</strong>modules. At the beginning <strong>of</strong> the disposal process, this flexibility is comparable to storage; thepackages can be simply retrieved over a period <strong>of</strong> from one to a few centuries.The option <strong>of</strong> retrieving the packages depends on the durability <strong>of</strong> the packages, cells <strong>and</strong> accessdrifts. This covers the integrity <strong>of</strong> the disposal packages, the components <strong>of</strong> the cell containing them,as well as ensuring that a minimum functional clearance is maintained around the packages to enablethem to be retrieved over this same period <strong>of</strong> centuries. The integrity <strong>of</strong> the various elements for aperiod <strong>of</strong> at least a century implies a mechanical design taking account <strong>of</strong> the evolution <strong>of</strong> thematerials <strong>and</strong>, in particular in the case <strong>of</strong> C cells, <strong>of</strong> corrosion <strong>of</strong> the metal parts. Similarly,maintaining the access drifts implies mechanical sizing <strong>of</strong> the concrete lining for an identical period.Finally, the modularity <strong>of</strong> the C waste <strong>repository</strong> zone provides it with overall <strong>management</strong> flexibility.DOSSIER 2005 ARGILE -ARCHITECTURE AND MANAGEMENT OF A GEOLOGICAL DISPOSAL SYSTEM192/495

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