Electrical Resistivity Tomography (ERT)
Subsurface Imaging

Electrical Resistivity Tomography (ERT)

2D and 3D resistivity imaging of complex subsurface conditions.

Overview

Electrical Resistivity Tomography is a powerful geophysical method that images the subsurface by measuring how electrical current flows through the ground. RIIM's ERT surveys produce detailed 2D and 3D resistivity cross-sections that reveal geological layering, groundwater, contamination plumes, voids, and buried structures with exceptional spatial resolution.

How It Works

An array of electrodes is deployed along a survey line or grid. Current is injected between pairs of electrodes and the resulting voltage is measured at other electrode pairs. This process is repeated for many electrode combinations to build a comprehensive dataset. The data is then inverted using specialist software to produce a 2D or 3D resistivity model of the subsurface.

Applications

  • Groundwater exploration and aquifer mapping
  • Contamination plume delineation and monitoring
  • Void, cavity, and karst feature detection
  • Geological mapping and stratigraphic profiling
  • Landfill and waste body characterisation
  • Slope stability and embankment assessment

Deliverables

  • 2D resistivity inversion sections
  • 3D resistivity volume models (on request)
  • Geological and hydrogeological interpretation
  • Time-lapse ERT monitoring results (on request)
  • Integrated geophysical investigation report

Common Questions

Frequently Asked Questions