Fig. 22From: Implementation of the full-scale emplacement (FE) experiment at the Mont Terri rock laboratoryTime series plot showing how the surface temperature of the ‘deepest’ heater H1 reacted to the selected turn-on sequence. The calculated temperature prediction for an initially (with a water content of approximately 5%) relatively dry GBM with a thermal conductivity of 0.3 W/mK is represented as a dashed grey line in the backgroundBack to article page