GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 3.1 GNGTS 2024 results of the EMI-ERT constrained inversion and was not incorporated into the inversion process itself. Figure 2 - Horizontal sectons of the GPR and of the resistvity volumes obtained with and without constrain. Each row corresponds to a diferent depth: ( a ) 0.3 m; ( b ) 1.6 m; ( c ) 2.1 m; ( d ) 2.6 m and ( e ) 5.0 m. The locaton of the ERT secton (and its geoelectrical interpretaton) is shown as a green solid line. The assumed positon of a pipe is ploted in purple. The red contours are shown as references to the GPR anomalies; their purpose is merely to make the comparisons easier, and they are not necessarily connected to any specifc geological features.