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Study on geometric factor and sensitivity of subsurface for different electrical resistivity Tomography Arrays

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Abstract

The present study focused on the sensitivity and geometric factor of the subsurface employing Schlumberger array, Wenner array, and dipole–dipole array configurations. This allows to investigate the most and least sensitive subsurface depth of region and categorizes subsurface material. Sensitivity and geometric factor values are also compared, obtained by these array configurations at different depths. The geometric factor of an electrode array can be explained with reference to an ideal electrode array in which current intensity is constant throughout the subsurface strata. The constant amount of current was injected into the subsurface for all array configurations, and geometric factor is used to calculate apparent resistivity for homogeneous subsurface. Results indicate that the value of a geometric factor is smaller for the Wenner array configuration, and strong signal strength was observed. Sensitivity along the survey line in both Schlumberger and Wenner arrays is quite similar at different depths, but sensitivity in the dipole–dipole array showed differences along with the subsurface depth.

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Acknowledgements

The authors are grateful to The Editor, Arabian Journal of Geosciences, and the anonymous reviewers whose constructive reviews and suggestions have immensely enhanced the clarity of the manuscript. The authors also appreciate the support received from the Indian Institute of Technology Roorkee, Roorkee, India.

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Correspondence to Uttam Singh.

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The authors declare no competing interests.

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Responsible Editor: Narasimman Sundararajan

Highlights

• Sensitivity along the ERT survey line for both the Schlumberger array and Wenner array configuration is similar. However, the sensitivity of the Dipole–dipole array is different along with the subsurface depth.

• The values of geometric factor are smaller for the Wenner array in comparison with the Schlumberger and Dipole–dipole array.

• The average apparent resistivity value at 1.65-m depth is 460 Ohm-m. It means pebbles and sandy subsoil are available, which was also observed during augur sampling.

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Singh, U., Sharma, P.K. Study on geometric factor and sensitivity of subsurface for different electrical resistivity Tomography Arrays. Arab J Geosci 15, 560 (2022). https://doi.org/10.1007/s12517-022-09844-3

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  • DOI: https://doi.org/10.1007/s12517-022-09844-3

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