
In-hole geoelectric surveys are based on measuring the apparent resistivity and apparent chargeability of the subsurface using electrodes installed inside one or more boreholes.
This methodology makes it possible to obtain a geoelectrical characterization of the subsurface with high vertical resolution, representing a valuable extension of traditional surface ERT/IP surveys, especially in contexts where the stratigraphy is complex or covered by low conductivity materials.
The principle of operation is similar to that of multielectrode surface surveys: data acquisition is by means of a georesistivimeter, which manages the sequential activation of electrodes, installed at different depths along the borehole walls. The holes can be single (for vertical down-hole type measurements) or multiple (for 2D and 3D cross-hole configurations), allowing direct exploration of the investigated volume horizontally and vertically. Electrodes can be temporarily lowered or permanently installed, depending on monitoring needs. Finally, performing repeated measurements over time (timelapse), especially in 3D configuration, is a powerful tool for dynamic monitoring.
Fields of Application:
Electro-stratigraphic reconstruction
Verification of presence or search for aquifers
Study of pollution phenomena in soils or groundwater
Definition of contaminated volumes
Search for hidden cavities
Stratigraphic research
Detection of subsurface leaks
Study of landslides
Mineral prospecting
Fields of Application:
Electro-stratigraphic reconstruction
Verification of presence or search for aquifers
Study of pollution phenomena in soils or groundwater
Definition of contaminated volumes
Search for hidden cavities
Stratigraphic research
Detection of subsurface leaks
Study of landslides
Mineral prospecting
Discover the other electrical methods:
We are able to offer our partners multiple solutions in the field of Geoelectrical Investigations. Discover how we can meet your needs.