2D Electrical resistivity tomography (ERT) or electrical resistivity imaging (ERI) is a geophysical technique for imaging sub-surface structures from electrical resistivity measurements made at the surface.
In electric resistivity imaging (ERI) electric currents are injected into the ground and the resulting potential differences are measured at the surface, yielding information about the distribution of electrical resistivity below the surface. Finally, this gives an indication of the lithological and structural variation of the subsoil (since resistivity depends on sediment porosity and pore water)
The process of conducting a 2D ERI survey typically involves the following steps:
Implementing 2D ERI surveys offers several key advantages over conventional subsurface exploration methods: