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Architecture and management of a geological repository - Andra

Architecture and management of a geological repository - Andra

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Due to the high thermal conductivity <strong>of</strong> the metal components, the temperature very quickly reachesthe same level within the sleeve over the entire length <strong>of</strong> the cell. It increases almost simultaneouslywithin the rock: after a year in disposal, the temperature <strong>of</strong> the rock wall reaches almost 40°C for typeC0 packages <strong>and</strong> over 50°C 136 for type C1 to C4 packages. Thermal interaction between adjacent cellsis already marked by a 5°C increase at the mid-distance between type C waste cells. In spent fueldisposal cells, the heat transfer is slowed down by the swelling clay as it has a lower thermalconductivity than that <strong>of</strong> argilites. Thus the heating <strong>of</strong> the wall rock is slowed <strong>and</strong> reduced by the clayring that maintains a temperature difference <strong>of</strong> around 30°C between its internal <strong>and</strong> external facesduring the temperature rise.The maximum temperature on the surface <strong>of</strong> the packages, <strong>of</strong> between 90°C <strong>and</strong> 100°C, is due to thedimensioning <strong>of</strong> the architecture <strong>of</strong> each <strong>repository</strong> zone for a given package age (see § 5.2 <strong>and</strong> 5.3).This maximum temperature is reached after 10 to 20 years for all type C or spent fuel waste packages.At the same time, the argilites or swelling clay in contact with the sleeve reach a temperature <strong>of</strong>between 80°C <strong>and</strong> 90°C.This temperature rise within the cells would not be significantly changed by sealing them immediatelyafter they have been filled. Given that the temperature rise is relatively rapid (from 10 to 20 years),maintaining the cell unsealed during this transitional evolutionary phase could be considered in orderto allow the fullest possible monitoring to be carried out without placing major constraints on thetransmission <strong>of</strong> measurement data (see 10.3.8.3). Furthermore, a sound knowledge <strong>of</strong> the temperature<strong>of</strong> the packages <strong>and</strong> the cell is needed in order to check that the cell behaves as expected <strong>and</strong>, inparticular, in order to establish the actual conditions inside the cell in case it is decided to retrieve thepackages.Propagation <strong>of</strong> heat from the cells leads to heating in the access drifts within the module. Thetemperature <strong>of</strong> the wall rock remains below 60°C in the vicinity <strong>of</strong> the cells. Ventilation is maintainedconstantly in the drifts with reduced flow. In the event <strong>of</strong> intervention by personnel, this flow can beincreased in order to keep the air temperature at a value below regulation limits. The thermomechanicaleffects on the sleeve induced by this heating are taken into consideration whendimensioning <strong>and</strong> do not reduce the durability <strong>of</strong> the structures (see sections 5.2, 5.3 <strong>and</strong> [13]).One <strong>of</strong> the principal effects induced by the heating <strong>of</strong> the cell is the expansion <strong>of</strong> the packages, thesleeve, the swelling clay for spent fuel disposal cells <strong>and</strong> <strong>of</strong> the rock. Thanks to the functionalclearances between the packages on the one h<strong>and</strong> <strong>and</strong> between the packages <strong>and</strong> the sleeve on theother 137 , the thermal expansion <strong>of</strong> the packages, spacers <strong>and</strong> sleeve do not create notable thermomechanicalstresses within the packages 138 <strong>and</strong> the deformations induced are sufficiently small so asnot to block the packages or the spacers, at the same time as they reach their maximum amplitude. It istherefore possible to retrieve packages at any time, whatever the amplitude <strong>of</strong> the expansiondeformation, in the cell.The heating <strong>of</strong> the rock also accelerates the delayed deformation <strong>of</strong> the argilites (by a factor <strong>of</strong> 2 to 3).For type C waste cells, this acceleration encourages the closing <strong>of</strong> the functional clearance for fittingthe sleeve <strong>and</strong> accentuates the terrain pressure on the sleeve after closing <strong>of</strong> this functional clearance.However, the dimensioning <strong>of</strong> the sleeve makes it possible, as soon as the functional clearance hasclosed, to ensure the durability <strong>of</strong> the sleeve <strong>and</strong> the maintenance <strong>of</strong> the geometry within the sleeve forat least two or three hundred years, <strong>and</strong> probably longer.136 The temperatures <strong>and</strong> durations indicated in this section correspond to the reference dimensioning used for the studies (see chapters 5<strong>and</strong> 6)137 The low level <strong>of</strong> corrosion during the heating phase does not significantly change the width <strong>of</strong> these clearances.138 Constructive provisions having been taken in order to limit these stresses locally in the area in which the package touches the sleeve, forexample by placing friction pads between the packages <strong>and</strong> the sleeve.DOSSIER 2005 ARGILE -ARCHITECTURE AND MANAGEMENT OF A GEOLOGICAL DISPOSAL SYSTEM376/495

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