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Architecture and management of a geological repository - Andra

Architecture and management of a geological repository - Andra

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6 – Overall underground architectureIn the B waste zone, each module comprises one cell <strong>and</strong> one drift that provides access to it <strong>and</strong>corresponds to an operating unit. In C waste (or spent fuel) <strong>repository</strong> zones, each module comprisesseveral dozens <strong>of</strong> cells. In the architecture presented here, one module is subdivided into twooperating units.Operating units are constructed <strong>and</strong> operated as <strong>repository</strong> space is required at a rate <strong>of</strong> one unit every1 to 2 years depending on the zone. When the construction or operating periods exceed thisperiodicity, several operating units can be under construction or in operation simultaneously in thesame zone.Details <strong>of</strong> the layout <strong>of</strong> the various <strong>repository</strong> zones is given in Sections 6.2.5 <strong>and</strong> 6.2.6 below.In order to ensure compartmentization, each module is isolated from the rest <strong>of</strong> the undergroundinstallations by one or more seals at the time <strong>of</strong> closure.6.2.3 Access to <strong>repository</strong> zones6.2.3.1 Repository access shaftsThe surface installations are connected to the underground installations by means <strong>of</strong> a group <strong>of</strong> shaftscommon to all <strong>repository</strong> zones. The layout used facilitates control <strong>of</strong> the long-term hydraulicfunctioning <strong>of</strong> the <strong>repository</strong>:- The shafts are all located together in the same zone, which has a radius <strong>of</strong> approximately200 meters <strong>and</strong> is <strong>of</strong>fset from the <strong>repository</strong> zones;- The shaft zone is connected to the <strong>repository</strong> connecting infrastructures by a group <strong>of</strong> drifts thatrun parallel to the main geotechnical stress. These parallel drifts shall be sealed when the<strong>repository</strong> is closed.A detailed description <strong>of</strong> the shafts is given in Section 7.3.6.2.3.2 Connecting driftsThe <strong>repository</strong> modules are connected to the shafts by connection infrastructure made up <strong>of</strong> clusters <strong>of</strong>parallel connection drifts that vary in number depending on the size <strong>of</strong> the flow to be managed. Theseare all hierarchised into main connection drifts, which connect the shaft zone to the various <strong>repository</strong>sub-zones, <strong>and</strong> secondary connection drifts, inside each sub-zone. This hierarchisation makes theconstruction <strong>and</strong> operation <strong>of</strong> the <strong>repository</strong> more flexible <strong>and</strong> means that the various sub-zones areindependent from each other. Distinguishing between dedicated package transfer drifts, constructiondrifts <strong>and</strong>, depending on requirements, air exhaust drifts facilitates the <strong>management</strong> <strong>of</strong> coactivitybetween nuclear activities <strong>and</strong> civil engineering activities.A detailed description <strong>and</strong> design <strong>of</strong> the connection drifts can be found in Section 7.4.6.2.4 General <strong>repository</strong> layout6.2.4.1 Positioning in the clay formationAt this point, <strong>Andra</strong> used the layout <strong>of</strong> all the <strong>repository</strong> modules in the median part <strong>of</strong> the Callovo-Oxfordian formation. This option ensures the same undisturbed argillite thickness between the<strong>repository</strong> <strong>and</strong> the over- <strong>and</strong> underlying carbonate formations 105 . There is no significant verticalvariation in the parameters that govern the retention <strong>and</strong> solubility <strong>of</strong> the radionuclides between thedifferent lith<strong>of</strong>acies <strong>of</strong> the formation; the Callovo-Oxfordian conceptual model therefore adoptsidentical values to these parameters for different lithological horizons [75] <strong>and</strong> [76] – Chapter 6).105 From an optimisation viewpoint, this option could be reviewed taking into account (i) the geomechanical behaviour <strong>of</strong> the differentlith<strong>of</strong>acies <strong>of</strong> the formation, <strong>and</strong> (ii) the migration times <strong>of</strong> toxic elements into the surrounding formations.DOSSIER 2005 ARGILE -ARCHITECTURE AND MANAGEMENT OF A GEOLOGICAL DISPOSAL SYSTEM260/495

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