Fig. 18From: Numerical modeling of reinjection and tracer transport in a shallow aquifer, Nesjavellir Geothermal System, IcelandEvolution of temperature in 2030 and 2040 if injection and production continue at the same average flow rate and temperature from 2018 to 2020 observed in layer 1 (a), layer 3 (b) and layer 13 (c). Cross section along the most permeable fault (FAU10) for 2030 (e) and 2040 (d)Back to article page