Process / pipelineElectromagnetic inversion

Electrical Resistivity Tomography

Electrical Resistivity Tomography (ERT) is an active-source geophysical method that maps the spatial distribution of electrical resistivity in the subsurface by injecting current between two electrodes and measuring potential differences across an array of receiver electrodes. Advanced as a practical technique by Loke and Barker in 1996, ERT has become standard for hydrogeological, environmental, and structural characterization due to its sensitivity to fluid saturation and salt content.

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Sources

  1. Loke, M. H., & Barker, R. D. (1996). Rapid least-squares inversion of apparent resistivity pseudosections by a quasi-Newton method. Geophysical Prospecting, 44(1), 131-152. DOI: 10.1111/j.1365-2478.1996.tb00142.x
  2. Telford, W. M., Geldart, L. P., & Sheriff, R. E. (1990). Applied geophysics (2nd ed.). Cambridge University Press. link

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ScholarGateElectrical Resistivity Tomography (Electrical Resistivity Tomography). Retrieved 2026-06-04 from https://scholargate.app/en/geophysics/electrical-resistivity-tomography