1887
Volume 29, Issue 1-2
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

We derive a closed-form solution for the transient magnetic field developed by a magnetic source located above a thin conductive layer. The solution extends the solution found by J.C. Maxwell for a conductive thin sheet. In addition to Maxwell’s expression, the new solution explicitly depends on the thickness of the conductive layer. It can be used in a rapid inversion algorithm. The new solution allows an interpreter to estimate the thickness and conductivity of the conductive layer in addition to its conductance.

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/content/journals/10.1071/EG998195
1998-03-01
2026-01-13
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References

  1. Goldman, M.M., and Fitterman, D.V., 1987, Direct time-domain calculation of the transient response for a rectangular loop over a two-layer medium: Geophysics 52, 997–1006.
  2. Macnae, J., and Lamontagne, Y., 1987, Imaging quasi-layered conductive structures by simple processing of transient electromagnetic data: Geophysics 52, 545–554.
  3. Maxwell, J.C., 1981, A treatise on electricity and magnetism: Clarendon Press, 2.
  4. Schmidt, A., 1918, Besitzt die tagliche erdmagnetische Schwankung in der Erdoberflache ein Potential: Physik Zeitsch 19, 349–355.
  5. Vasseur and Weidelt., P., 1977, Bimodal electromagnetic induction in non-uniform thin sheet with application to the northern Pyrenean induction anomaly: Geophys. J. R. Astr. Soc. 51, 669–690.
/content/journals/10.1071/EG998195
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  • Article Type: Research Article

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