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On measuring electromagnetic surface impedance-discussions with Professor James R. Wait
Electromagnetic (EM) surface impedance, defined as the ratio of the horizontal electric field to the horizontal magnetic field perpendicular to the plane of incidence, has been used in geophysics since the early 1950s for subsurface earth mapping. Traditionally, the electric field component has been...
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Published in: | IEEE transactions on antennas and propagation 2000-10, Vol.48 (10), p.1517-1520 |
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description | Electromagnetic (EM) surface impedance, defined as the ratio of the horizontal electric field to the horizontal magnetic field perpendicular to the plane of incidence, has been used in geophysics since the early 1950s for subsurface earth mapping. Traditionally, the electric field component has been measured using a staked voltage probe. In 1989, Wu and Thiel suggested that an insulated wire dipole without the stakes was a more reliable measurement technique. Wait (1989) responded to this paper and the discussion continued until Wait's last comments were published in 1999. In this paper, the final arguments are summarized. The major conclusion reached is that either technique can be used provided caution is exercised, particularly at higher frequencies. |
doi_str_mv | 10.1109/8.899667 |
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subjects | Antennas Earth Electric fields Electric potential Electric variables measurement Electric wire Electromagnetic fields Electromagnetic measurements Geophysical measurements Geophysics Horizontal Impedance measurement Magnetic field measurement Magnetic fields Surface impedance Voltage |
title | On measuring electromagnetic surface impedance-discussions with Professor James R. Wait |
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