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...
Main Author: | |
---|---|
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 |
id |
doaj-98bffa888e0f46079f81ed3052de22ba |
---|---|
record_format |
Article |
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 |
_version_ |
1725870509323714560 |