Standard

Recording the vertical component of the electric field in magnetotelluric sounding. / Plotkin, V. V.; Mogilatov, V. S.

In: Russian Geology and Geophysics, Vol. 61, No. 2, 01.02.2020, p. 234-240.

Research output: Contribution to journal › Article › peer-review

Harvard

Plotkin, VV & Mogilatov, VS 2020, 'Recording the vertical component of the electric field in magnetotelluric sounding', Russian Geology and Geophysics, vol. 61, no. 2, pp. 234-240. https://doi.org/10.15372/RGG2019097

APA

Plotkin, V. V., & Mogilatov, V. S. (2020). Recording the vertical component of the electric field in magnetotelluric sounding. Russian Geology and Geophysics, 61(2), 234-240. https://doi.org/10.15372/RGG2019097

Vancouver

Plotkin VV, Mogilatov VS. Recording the vertical component of the electric field in magnetotelluric sounding. Russian Geology and Geophysics. 2020 Feb 1;61(2):234-240. doi: 10.15372/RGG2019097

Author

Plotkin, V. V. ; Mogilatov, V. S. / Recording the vertical component of the electric field in magnetotelluric sounding. In: Russian Geology and Geophysics. 2020 ; Vol. 61, No. 2. pp. 234-240.

BibTeX

@article{f4c7bbdbe11a448dbedb85a42f568311,
title = "Recording the vertical component of the electric field in magnetotelluric sounding",
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.",
keywords = "Circular electric dipole, Distortion of apparent resistivity curves, Electrical conductivity, Magnetotelluric sounding, Vertical component of electric field",
author = "Plotkin, {V. V.} and Mogilatov, {V. S.}",
year = "2020",
month = feb,
day = "1",
doi = "10.15372/RGG2019097",
language = "English",
volume = "61",
pages = "234--240",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Фонд {"}Центр поддержки науки и культуры{"}",
number = "2",

}

RIS

TY - JOUR

T1 - Recording the vertical component of the electric field in magnetotelluric sounding

AU - Plotkin, V. V.

AU - Mogilatov, V. S.

PY - 2020/2/1

Y1 - 2020/2/1

N2 - 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.

AB - 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.

KW - Circular electric dipole

KW - Distortion of apparent resistivity curves

KW - Electrical conductivity

KW - Magnetotelluric sounding

KW - Vertical component of electric field

UR - http://www.scopus.com/inward/record.url?scp=85089088444&partnerID=8YFLogxK

U2 - 10.15372/RGG2019097

DO - 10.15372/RGG2019097

M3 - Article

AN - SCOPUS:85089088444

VL - 61

SP - 234

EP - 240

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 2

ER -

ID: 24986043