(ERT) Electrical Resistivity Tomography

The ERT method allows for more effective interpretation of geological structures by collecting high resolution data.
It allows to quickly obtain geological parameters such as possible aquifer points, karstic structures, fractured cracked points, fault discontinuities, salinity ratio, groundwater level along the line.

ERT Survey Application Areas

Fractures, fault and karst mapping
Space perception in urban environments
Determination of bedrock depth
Determination of landslide structures
Dam and embankment evaluation
Soil and bedrock lithology
Fresh water, salt water distinction
Aquifer characterisation
Water table depth
Contaminated areas

Equipments

Elrec Terra 96 /SuperSting R8 84 Channel
12 Volt Akü / Generator
TIP 6000 Transmitter
CORS – RTK – GNSS

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