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Tome Architecture and management of a geological repository - Andra

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3 – Design study <strong>of</strong> a <strong>repository</strong> in a granite formation3.2.2.2 Main analysis information: variability <strong>of</strong> French granites properties for the<strong>repository</strong> design <strong>and</strong> safety analysis• Variability <strong>of</strong> mechanical propertiesMechanical resistance <strong>of</strong> granite rock differs according to the types <strong>of</strong> granite, mainly depending ontheir hydrothermal alteration. However, generally these variations are not likely to cause anysignificant differences in the granite response to structure excavation. Differences for <strong>repository</strong>architectural design are thus minor <strong>and</strong> only affect detailed dimensioning <strong>of</strong> undergroundstructures.[6].• Considerations relating to the variability <strong>of</strong> thermal propertiesThe initial temperature <strong>of</strong> underground granite cannot be directly measured without a borehole.Modelling was thus based on thermal flux mapping in France <strong>and</strong> thermal conductivity <strong>of</strong> rocksdepending on their quartz content. Estimations made for a depth <strong>of</strong> 500 metres have led touncertainties concerning initial temperatures <strong>of</strong> between ± 2.8°C <strong>and</strong> ± 3.5°C depending on themassifs [7].The graph (Figure 3.2.5) illustrates the relatively contrasting situations between the different types <strong>of</strong>French granite on this issue. Initial temperatures at a depth <strong>of</strong> 500 metres vary between 17 <strong>and</strong> 30°C.Rock conductivity has a value <strong>of</strong> between 2.4 <strong>and</strong> 3.8 W/m.K.Figure 3.2.5Correlation between thermal conductivity <strong>and</strong> temperature for granite massifsin FranceVariability in the thermal properties <strong>of</strong> French granites influences the dimensioning <strong>of</strong> underground<strong>repository</strong> installations for highly exothermic waste (C waste <strong>and</strong> spent fuel). From this st<strong>and</strong>point, thedifference is significant with respect to Fenno-Sc<strong>and</strong>inavian granites where underground temperatureis lower by around 10°C.For the least exothermic waste such as B5 <strong>and</strong> B1, this variability has little influence on <strong>repository</strong>dimensioning.Dossier 2005 Granite - ARCHITECTURE AND MANAGEMENT OF A GEOLOGICAL REPOSITORY39/228

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