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Geophysical Techniques PDF Print E-mail
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Saturday, 01 March 2008 13:32
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Geophysical Techniques
Seismic Surveying
Spectral Analysis of Surface Waves • SASW
Crosshole Sonic Logging • CSL
Ground Penetrating Radar • GPR
Electromagnetic Induction • EM
Bedrock Mapping
Borehole Geophysics
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Electrical Resistivity Surveying

ATS International, Inc. is proficient in the application of surface electrical resistivity imaging. Electrical resistivity is a versatile tool that offers the ability to obtain high-density subsurface data quickly and cost-effectively.

Electrical resistivity is the characteristic of earth materials to inhibit the flow of an electrical current. Electrical resistivity is a medium property that is effected primarily by:
  • Water Saturation
  • Ionic Strength of Pore Water
  • Grain Size
  • Porosity
  • Clay Content

Geologic information obtainable by electrical resistivity include:


  • Water Table Surface
  • Preferential Flow Paths
  • Lithology Changes
  • Geologic Structures
  • Contaminant Plumes
Electronic Resistivity  

Electrical resistivity is measured by inducing a current between two electrodes and measuring the resulting potential at other electrodes. The more widely spaced the electrodes, the deeper the sampling depth.

The raw data collected from a resistivity profile are the apparent resistivities in a cross-section of the earth. Apparent resistivities are different than the actual resistivities of the profile because of changes in the electric current that result from its pathway through various earth materials. Therefore, the apparent resistivities often require inversion modeling to convert the raw data to actual resistivities.

After the resistivity profiles are interpreted in cross-section, multiple resistivity profile data can be laterally interpolated to provide three-dimensional geologic models.



Last Updated on Sunday, 22 June 2008 03:21