1887
Volume 40 Number 6
  • E-ISSN: 1365-2478

Abstract

A

The induced polarization response for a 2D horizontal cylinder embedded in a half‐space is calculated for a uniform electric source. Response curves, in the form of apparent charge‐ability taking into account the effect of the air‐earth interface, exhibit a sharp decrease in amplitude with an increase in depth of burial of the target. The resistivity contrast between the cylinder and the host plays a dominant role in determining the IP response, i.e. the amplitude decreases considerably with the increase in resistivity contrast. The decrease is due to the defocusing effect caused by the resistive cylinder. The current lines tend to deviate away from the cylindrical target. In the case of a highly conducting cylinder, apparent defocusing takes place as current lines are confined to the surface of the conducting cylinder. An increase in chargeability contrast is reflected as a steady rise in the response. The peak response at the centre is reduced by about half the magnitude when the air–earth interface is not considered. The variation of response along the profile, though noticeable, is not as high as that obtained at the centre.

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2006-04-27
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References

  1. Aiken, C.L., Hastings, D.A. and Sturgul, J.R.1973. Physical and computer modelling of induced polarization. Geophysical Prospecting21, 763–782.
    [Google Scholar]
  2. Barnett, C.I.1972. Theoretical modelling of induced polarization effects due to arbitrarily shaped bodies . Ph.D. thesis, Colorado School of Mines, USA.
  3. Bertin, J. and Loeb, J.1976. Experimental and Theoretical Aspects of Induced Polarization, 1 and 2. Gebruder and Borntraeger, Berlin .
    [Google Scholar]
  4. Bhattacharya, B.B. and Biswas, D.1988. Induced polarization response over a three‐dimensional horizontal cylinder for gradient array. Gerlands Beitr Geophysik15, 273–286.
    [Google Scholar]
  5. Bhattacharya, B.B. and Datta, I.1982. Depth of investigation studies for gradient arrays over homogeneous isotropic half‐space. Geophysics47, 1198–1203.
    [Google Scholar]
  6. Coggon, J.H.1971. Electromagnetic and electrical modelling by the finite element method. Geophysics36, 132–155.
    [Google Scholar]
  7. Dieter, K., Paterson, N.R. and Grant, F.S.1969. I.P. and resistivity type curves for three dimensional bodies. Geophysics34, 615–632.
    [Google Scholar]
  8. Dodds, A.R., Raiche, A.P. and Vozoff, K.1977. A parametric study of induced polarization models. Geophysics42, 623–641.
    [Google Scholar]
  9. Eskola, L.1978. Comments on papers discussing the principles underlying the computation of IP parameters in a heterogeneous medium. Geophysical Prospecting26, 644–653.
    [Google Scholar]
  10. Eskola, L. and Hattula, A.1974. A method to calculate the frequency effect and charge‐ability of induced polarization in an inhomogeneous medium. Geological Survey Finland Report, Invest. 5.
    [Google Scholar]
  11. Hohman, G.W.1975. Three‐dimensional induced polarization and electromagnetic modelling. Geophysics40, 309–324.
    [Google Scholar]
  12. Komarov, V.A.1984. Elektrorazvedka Metodom Vyzvannoi Polyrizatsii (Electrical Prospecting by Induced Polarization Method), 2nd edn.Nedra, Leningrad (in Russian).
    [Google Scholar]
  13. Lee, T.1975. An integral equation and its solution for some two‐ and three‐dimensional problems in resistivity and induced polarization. Geophysical Journal of Royal Astronomical Society42, 81–95.
    [Google Scholar]
  14. Quick, D.H.1974. The interpretation of gradient array chargeability anomalies. Geophysical Prospecting22, 736–746.
    [Google Scholar]
  15. Sampaio, E.E.S.1982. Magnetic anomalies of two‐dimensional bodies in a magnetic half‐space. Geophysics47, 1229–1254.
    [Google Scholar]
  16. Seigel, H.O.1959. Mathematical formulation and type curves for induced polarization. Geophysics24, 547–566.
    [Google Scholar]
  17. Seigel, H.O.1978. Reply to comments by L. Eskola. Geophysical Prospecting26, 654–657.
    [Google Scholar]
  18. Spiegel, M.R.1959. Theory and Problems of Vector Analysis. McGraw‐Hill Book Co.
    [Google Scholar]
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