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Field

Geophysical investigations

See the subsurface before you drill: aquifer geometry, fractures and saline zones from resistivity imaging.

Electrical Resistivity Tomography (2D and 3D) and Vertical Electrical Sounding map aquifer thickness, weathered and fractured zones, clay layers and saline water. We use them to site productive wells, to define layers for groundwater models, and to locate seepage paths around mines and water bodies.

What you get

  • 2D and 3D Electrical Resistivity Tomography
  • Vertical Electrical Sounding
  • Well and piezometer siting
  • Seepage path mapping near mine pits and reservoirs
  • Integrated interpretation with borehole logs

Who it is for

Mines, industries siting new wells, recharge projects, and model builders who need layer geometry.

Common questions

How deep can ERT see?

Depth depends on the array and spread length. We design the survey for the depth your question needs.

Have a water question at your site?

Tell us about your site and what you need to know. A senior hydrogeologist replies within one working day.

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