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Journal of the Australian Society of Exploration Geophysicists
RESEARCH ARTICLE

Calculation of conductivity and depth correction factors for the S-layer differential transform *

Magdel Combrinck
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121 Rosen Office Park, 37 Invicta Rd, Halfway Gardens, Gauteng 1685, South Africa. Email: magdel@geotechairborne.com

Exploration Geophysics 39(2) 133-138 https://doi.org/10.1071/EG08014
Submitted: 5 December 2007  Accepted: 27 April 2008   Published: 16 June 2008

Abstract

The VTEM system developed and operated by Geotech Limited and Geotech Airborne Limited is a central loop configuration system lending itself to many traditional ground interpretation strategies. One of these is the S-layer (thin, conductive layer) differential transform that is used to generate resistivity-depth sections. An empirical study indicated that delineating conductors in a conductive half space necessitates the implementation of a scale factor in order to obtain the correct depths and conductivity values when applying the S-layer differential transform.

Based on an empirical approach, there was found to be an infinite number of depth correction factors that will still yield acceptable conductivity values, and the need arose to explain the origin of this discrepancy and to find the correct depth correction factor. A correction strategy was followed, based on scaling results to yield exact conductivities when applied to half-space models. Assuming that the equivalent filament for the S-layer behaviour, as with the equivalent filament for the half-space behaviour, does not coincide with the electric field maxima in the subsurface led to a plausible depth correction factor which was validated on various synthetic models.

Key words: TDEM, S-layer, depth, conductivity, correction factors, CDI, VTEM.


Acknowledgments

I gratefully acknowledge Prof. Willem Botha (and Kumba Resources) for the use of MARCO software and for many insightful discussions on TDEM. Also my sincere gratitude to Michael Zhdanov and Peter Wolfgram for their constructive contributions in reviewing this paper.


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* *Presented at the 19th ASEG Geophysical Conference & Exhibition, November 2007.