Geoelectrical and electromagnetical techniques

In order to distinguish between layers and bodies of different electrical conductivity and specific resistivity, respectively, we use the following methods:

vertical cut dike
Data and model of resistivity mapping on a dike , ©GGD mbH 2016
Interpretation of a resistivity sounding, ©GGD mbH 2016

The above-mentioned methods are primarily used to address the following questions and problems:

For geoelectrical and electromagnetical surveys we hold diverse multi-electrode equipment (Geosys and Syscal) as well as EM31, EM34, MaxMin and measurement devices for T-VLF.