Fig. 14From: Optimizing scenarios of a deep geothermal aquifer storage in the southern Upper Rhine GrabenRecovery factors calculated with the COMSOL model for different scenarios, i.e., flow rates (10 L s−1, 40 L s−1, 100 L s−1), filter section length L (250 m, 500 m, 1000 m), and distance between horizontal wells D (100 m, 400 m), and for 10 cyclesBack to article page