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Russian Geology and Geophysics

2020 year, number 2

RECORDING THE VERTICAL COMPONENT OF THE ELECTRIC FIELD IN MAGNETOTELLURIC SOUNDING

V.V. Plotkin1, V.S. Mogilatov1,2
1Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia
2Novosibirsk State University, ul. Pirogova 1, Novosibirsk, 630090, Russia
Keywords: Magnetotelluric sounding, electrical conductivity, circular electric dipole, distortion of apparent resistivity curves, vertical component of the electric field

Abstract

Magnetotelluric sounding (MTS) usually records variations in five components of the electromagnetic field. Interpretation of distorted MT responses of an inhomogeneous earth may be problematic. The problem can be solved by recording additionally the vertical component Ez of the electric field in order to improve the quality of inversion and to gain more information. Currently Ez variations are estimated by measuring voltage on a vertical line immersed in water. The land measurements of this kind require special drilling or using the existing boreholes, which is not always feasible. Otherwise, a circular electric dipole (CED) can be used as a receiver to record the electric field behavior along the vertical component. Its applicability to MT soundings is analyzed in this paper.

DOI: 10.15372/RGG2019097