1887
Volume 18, Issue 3
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

The transient magnetic fields in a borehole near a plate-like conductor can be simulated with a simple current loop in the plane of the conductor. The shape of the response with depth in the hole is related to the position and orientation of the current loop, so that characteristics of the response such as the zero-crossing separation can be used to predict the location of the current loop and therefore the location of the conductor in which the current circulates. Physical model results verify the application of the characteristics in this way.

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/content/journals/10.1071/EG987349
1987-06-01
2026-01-13
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References

  1. Barnett, C. T. (1984)—‘Simple inversion of time-domain electromagnetic data’, Geophysics49, 925-933.
  2. Buselli, G. & O2019;Neill, B. (1977)—‘SIROTEM. A new portable instrument for multichannel transient electromagnetic measurements’, Bull.Aust. Soc. Explor. Geophys.8, 82-87.
  3. Grant, F. S. & West, G. F. (1965)—‘Interpretation theory in appliedgeophysics’, New York, McGraw Hill Book Co., Inc., 583 pp.
  4. Nabighian, M. N. (1979)—‘Quasi-static transient response of a conducting halfspace — An approximate representation’, Geophysics44, 1700-1705.
  5. Parums, R. (1984)—‘ Downhole electromagnetic modelling’, B.Sc. (Hons) report, University of Melbourne, Melbourne, Victoria.
  6. Smythe, W. R. (1968)—‘Static and dynamic electricity’, New York, McGraw Hill Book Co., Inc., 623 pp.
  7. Woods, D. V. (1975)—‘A model study of. the Crone borehole pulseelectromagnetic (PEM) system’, M.Sc. thesis, Queen’s University, Kingston, Ontario.
/content/journals/10.1071/EG987349
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  • Article Type: Research Article
Keyword(s): current filament; downhole EM; nomograms; scale modeling

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