Research Article

A Macroscale Hydrogeological Numerical Model of the Suio Hydrothermal System (Central Italy)

Figure 4

A 2D finite element model derived from the hydrogeological section in Figure 1(c). The model shows the location of the temperature measurement points of the Suio springs and at the bottom of the Gallo well and the Suio water wells along the Garigliano river. The area bordered by the green dashed polygon represents the deep reservoir. The dashed blue line represents the piezometric level inside the carbonates. The two red segments (a and b) represent the modelled discrete fractures. For the nomenclature of each layer, please refer to the caption of Figure 1.