Fig. 19From: Numerical modeling of reinjection and tracer transport in a shallow aquifer, Nesjavellir Geothermal System, IcelandEvolution of temperature for 2030 and 2040 if all injection and production is stopped in layer 1 (a), layer 3 (b) and layer 13 (c). Cross section shows temperature distribution along the most permeable fault (FAU10) for 2030 (d) and 2040 (e)Back to article page