Research output: Contribution to journal › Article › peer-review
Influences of the earth’s magnetic field on the transient electromagnetiprocess in the geoelectric field: An experimental study. / Mogilatov, V. S.; Potapov, V. V.; Shein, N. et al.
In: Russian Geology and Geophysics, Vol. 62, No. 12, 8, 12.2021, p. 1430-1439.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Influences of the earth’s magnetic field on the transient electromagnetiprocess in the geoelectric field: An experimental study
AU - Mogilatov, V. S.
AU - Potapov, V. V.
AU - Shein, N.
AU - Gur’ev, V.
N1 - Funding Information: The research was supported by the Russian Foundation for Basic Research, Grant No. 17-05-00083. Publisher Copyright: Russian Geology and Geophysics © 2021, Novosibirsk State University.
PY - 2021/12
Y1 - 2021/12
N2 - A mathematical model of the influence of the Earth’s magnetic field (the Hall effect) on results of the controlled source transient electromagnetic (TEM) method has been elaborated. For identification of this effect, we propose a schematic layout of the experimental grounded system with a pulsed loop source and signals recording by radial receive lines equally spaced relative to the loop. The 2018–2019 special field experiments were conducted in the Tatar region of the West Siberian Lowland with an aim to estimate the Hall effect contributions to the TEM method. To detect the Hall effect, transient electromagnetic responses were measured mainly by four receive lines radiating from a 500×500 m square loop. Analysis of the TEM results processing aimed at improving the signal quality and reducing the interference revealed a great similarity in signals from the radial lines, which is theoretically possible only under the Hall effect. Comparison of the field signals with the theoretical ones enabled estimation of the components caused by the Hall effect, in particular, conductivity at ~0.002 S/m.
AB - A mathematical model of the influence of the Earth’s magnetic field (the Hall effect) on results of the controlled source transient electromagnetic (TEM) method has been elaborated. For identification of this effect, we propose a schematic layout of the experimental grounded system with a pulsed loop source and signals recording by radial receive lines equally spaced relative to the loop. The 2018–2019 special field experiments were conducted in the Tatar region of the West Siberian Lowland with an aim to estimate the Hall effect contributions to the TEM method. To detect the Hall effect, transient electromagnetic responses were measured mainly by four receive lines radiating from a 500×500 m square loop. Analysis of the TEM results processing aimed at improving the signal quality and reducing the interference revealed a great similarity in signals from the radial lines, which is theoretically possible only under the Hall effect. Comparison of the field signals with the theoretical ones enabled estimation of the components caused by the Hall effect, in particular, conductivity at ~0.002 S/m.
KW - Controlled source transient electromagnetic (TEM) method
KW - Electrical prospecting
KW - Geomagnetic field
KW - Hall eff
UR - http://www.scopus.com/inward/record.url?scp=85121386416&partnerID=8YFLogxK
UR - https://www.elibrary.ru/item.asp?id=47546570
UR - https://www.mendeley.com/catalogue/64fa452e-9d89-38e2-9ec5-cf6f1bdff038/
U2 - 10.2113/RGG20204192
DO - 10.2113/RGG20204192
M3 - Article
AN - SCOPUS:85121386416
VL - 62
SP - 1430
EP - 1439
JO - Russian Geology and Geophysics
JF - Russian Geology and Geophysics
SN - 1068-7971
IS - 12
M1 - 8
ER -
ID: 35258923