Measurements of Geomagnetic Field Variations in the Low Frequency Range

The article presents the results of measurements of geomagnetic field variations obtained using magnetometers with different frequency range (0.01–200 Hz and 0.01–30 Hz) developed at the Institute of Geophysics of Uro RAS. The measurements showed that the sensitivity and resolution of the equipment...

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Main Author: Тягунов Д.С.
Format: Article
Language:Russian
Published: Institute of Volcanology and Seismology FEB RAS 2019-10-01
Series:Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле
Subjects:
Online Access:http://www.kscnet.ru/journal/kraesc/article/view/260
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spelling doaj-98bffa888e0f46079f81ed3052de22ba2020-11-24T21:53:43ZrusInstitute of Volcanology and Seismology FEB RASВестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле1816-55241816-55322019-10-014339910810.31431/1816-5524-2019-3-43-99-108267Measurements of Geomagnetic Field Variations in the Low Frequency RangeТягунов Д.С.0Institute of Geophysics of Ural Branch of Russian Academy of Sciences, Ekaterinburg, RussiaThe article presents the results of measurements of geomagnetic field variations obtained using magnetometers with different frequency range (0.01–200 Hz and 0.01–30 Hz) developed at the Institute of Geophysics of Uro RAS. The measurements showed that the sensitivity and resolution of the equipment used in the work is sufficient to study the variations of the geomagnetic field at low frequencies. It is shown that magnetometers used by magnetic modulation converter with auto-parametric amplification of the signal are capable of recording variations of the geomagnetic field that do not exceed the level of geomagnetic noise of 0.2 pT at a frequency of 2 Hz and 1 pT at lower frequencies. The average amplitude of the variations in the geomagnetic field of the magnetic induction components recorded by the device with a frequency range of 0.01–200 Hz in the entire bandwidth is twofold higher than the average amplitude of the magnetic induction components recorded by the device with a frequency range of 0.01–30 Hz, but the spectral composition shows close values.http://www.kscnet.ru/journal/kraesc/article/view/260the geomagnetic noisemagnetic inductionmagnetic field
collection DOAJ
language Russian
format Article
sources DOAJ
author Тягунов Д.С.
spellingShingle Тягунов Д.С.
Measurements of Geomagnetic Field Variations in the Low Frequency Range
Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле
the geomagnetic noise
magnetic induction
magnetic field
author_facet Тягунов Д.С.
author_sort Тягунов Д.С.
title Measurements of Geomagnetic Field Variations in the Low Frequency Range
title_short Measurements of Geomagnetic Field Variations in the Low Frequency Range
title_full Measurements of Geomagnetic Field Variations in the Low Frequency Range
title_fullStr Measurements of Geomagnetic Field Variations in the Low Frequency Range
title_full_unstemmed Measurements of Geomagnetic Field Variations in the Low Frequency Range
title_sort measurements of geomagnetic field variations in the low frequency range
publisher Institute of Volcanology and Seismology FEB RAS
series Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле
issn 1816-5524
1816-5532
publishDate 2019-10-01
description The article presents the results of measurements of geomagnetic field variations obtained using magnetometers with different frequency range (0.01–200 Hz and 0.01–30 Hz) developed at the Institute of Geophysics of Uro RAS. The measurements showed that the sensitivity and resolution of the equipment used in the work is sufficient to study the variations of the geomagnetic field at low frequencies. It is shown that magnetometers used by magnetic modulation converter with auto-parametric amplification of the signal are capable of recording variations of the geomagnetic field that do not exceed the level of geomagnetic noise of 0.2 pT at a frequency of 2 Hz and 1 pT at lower frequencies. The average amplitude of the variations in the geomagnetic field of the magnetic induction components recorded by the device with a frequency range of 0.01–200 Hz in the entire bandwidth is twofold higher than the average amplitude of the magnetic induction components recorded by the device with a frequency range of 0.01–30 Hz, but the spectral composition shows close values.
topic the geomagnetic noise
magnetic induction
magnetic field
url http://www.kscnet.ru/journal/kraesc/article/view/260
work_keys_str_mv AT tâgunovds measurementsofgeomagneticfieldvariationsinthelowfrequencyrange
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