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Magnetic viscosity effect on TEM data of an array with a fixed transmitter loop. / Kozhevnikov, N. O.; Antonov, E. Yu.

In: Russian Geology and Geophysics, Vol. 59, No. 6, 01.06.2018, p. 690-696.

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Kozhevnikov NO, Antonov EY. Magnetic viscosity effect on TEM data of an array with a fixed transmitter loop. Russian Geology and Geophysics. 2018 Jun 1;59(6):690-696. doi: 10.1016/j.rgg.2018.05.007

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Kozhevnikov, N. O. ; Antonov, E. Yu. / Magnetic viscosity effect on TEM data of an array with a fixed transmitter loop. In: Russian Geology and Geophysics. 2018 ; Vol. 59, No. 6. pp. 690-696.

BibTeX

@article{a4869d94cc5b4463a11bc3cbb9a00bd7,
title = "Magnetic viscosity effect on TEM data of an array with a fixed transmitter loop",
abstract = "In this paper, we present and discuss the results of modeling of the transient induction processes observed at different distances from the center of a transmitter loop in studies of a two-layer earth in which the magnetic susceptibility of the top layer or the base depends on frequency. Profiling graphs (the offset is plotted on the abscissa, and the EMF induced in the receiver coil at a fixed time is plotted on the ordinate) show that the polarity of the EMF changes as the offset increases. For the model with a magnetic layer of any thickness, the polarity of the EMF reverses immediately after the receiver crosses the loop wire. For the model with a magnetic base, the offset at which the EMF polarity reversal occurs is the larger the greater the thickness of the layer. For both models, the EMF at a fixed time depends on the thickness of the layer and the offset. Particularly strong dependence of the EMF on layer thickness or offset is observed near the loop side. Therefore, measurements near the wire make it possible to determine the thickness of the layer in the case where it is much less than the length of the loop side. The overall effect of magnetic relaxation and transient eddy currents leads to the fact that small changes in the layer thickness or offset can lead to a dramatic change in the transient response.",
keywords = "fixed source array, magnetic viscosity, TEM method, two-layer model, RELAXATION",
author = "Kozhevnikov, {N. O.} and Antonov, {E. Yu}",
year = "2018",
month = jun,
day = "1",
doi = "10.1016/j.rgg.2018.05.007",
language = "English",
volume = "59",
pages = "690--696",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "6",

}

RIS

TY - JOUR

T1 - Magnetic viscosity effect on TEM data of an array with a fixed transmitter loop

AU - Kozhevnikov, N. O.

AU - Antonov, E. Yu

PY - 2018/6/1

Y1 - 2018/6/1

N2 - In this paper, we present and discuss the results of modeling of the transient induction processes observed at different distances from the center of a transmitter loop in studies of a two-layer earth in which the magnetic susceptibility of the top layer or the base depends on frequency. Profiling graphs (the offset is plotted on the abscissa, and the EMF induced in the receiver coil at a fixed time is plotted on the ordinate) show that the polarity of the EMF changes as the offset increases. For the model with a magnetic layer of any thickness, the polarity of the EMF reverses immediately after the receiver crosses the loop wire. For the model with a magnetic base, the offset at which the EMF polarity reversal occurs is the larger the greater the thickness of the layer. For both models, the EMF at a fixed time depends on the thickness of the layer and the offset. Particularly strong dependence of the EMF on layer thickness or offset is observed near the loop side. Therefore, measurements near the wire make it possible to determine the thickness of the layer in the case where it is much less than the length of the loop side. The overall effect of magnetic relaxation and transient eddy currents leads to the fact that small changes in the layer thickness or offset can lead to a dramatic change in the transient response.

AB - In this paper, we present and discuss the results of modeling of the transient induction processes observed at different distances from the center of a transmitter loop in studies of a two-layer earth in which the magnetic susceptibility of the top layer or the base depends on frequency. Profiling graphs (the offset is plotted on the abscissa, and the EMF induced in the receiver coil at a fixed time is plotted on the ordinate) show that the polarity of the EMF changes as the offset increases. For the model with a magnetic layer of any thickness, the polarity of the EMF reverses immediately after the receiver crosses the loop wire. For the model with a magnetic base, the offset at which the EMF polarity reversal occurs is the larger the greater the thickness of the layer. For both models, the EMF at a fixed time depends on the thickness of the layer and the offset. Particularly strong dependence of the EMF on layer thickness or offset is observed near the loop side. Therefore, measurements near the wire make it possible to determine the thickness of the layer in the case where it is much less than the length of the loop side. The overall effect of magnetic relaxation and transient eddy currents leads to the fact that small changes in the layer thickness or offset can lead to a dramatic change in the transient response.

KW - fixed source array

KW - magnetic viscosity

KW - TEM method

KW - two-layer model

KW - RELAXATION

UR - http://www.scopus.com/inward/record.url?scp=85048184469&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2018.05.007

DO - 10.1016/j.rgg.2018.05.007

M3 - Article

AN - SCOPUS:85048184469

VL - 59

SP - 690

EP - 696

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 6

ER -

ID: 14103157