Frequency electromagnetic sounding with industrial power lines on Karelia-Kola geotraverse
The paper describes theory, method and first experimental results of research on the interaction between electromagnetic waves of extremely low and ultra low frequency (0.1-200 Hz), the Earth crust and ionosphere in the field of two mutually orthogonal industrial power lines, 109 and 120 km long, in...
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Saint-Petersburg Mining University
2017-04-01
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doaj-1b68dfd426e645a9b20c9228d33f99072020-11-25T00:00:38ZengSaint-Petersburg Mining UniversityZapiski Gornogo Instituta2411-33362541-94042017-04-01224210.18454/pmi.2017.2.1785216Frequency electromagnetic sounding with industrial power lines on Karelia-Kola geotraverseА. Н. Шевцов0А. А. Жамалетдинов1В. В. Колобов2М. Б. Баранник3Geological Institute of the Kola Science Centre of the RASGeological Institute of the Kola Science Centre of the RASCentre for Physical and Technological Problems of Energy in Northern Areas of the Kola Science Centre of the RASCentre for Physical and Technological Problems of Energy in Northern Areas of the Kola Science Centre of the RASThe paper describes theory, method and first experimental results of research on the interaction between electromagnetic waves of extremely low and ultra low frequency (0.1-200 Hz), the Earth crust and ionosphere in the field of two mutually orthogonal industrial power lines, 109 and 120 km long, in the course of FENICS experiment (Fennoscandian Electrical conductivity from Natural and Induction Control Source soundings). The main focus was on the observation results along the line of Karelia-Kola geotraverse over a distance of 700 km from the source. High horizontal homogeneity of geoelectrical lithosphere section has been detected in the eastern part of the Baltic shield at depth range from 10-15 to 50-70 km. Parameters of «regular» lithosphere section have been specified to the depth of 60-70 km. As a result of inverse problem solution for the western part of Karelia and Central Finland, a zone of decreased transverse resistivity has been detected at the depth of 50-60 km, corresponding to the area, detected by seismic methods, where Moho boundary reaches the same depth.http://pmi.spmi.ru/index.php/pmi/article/view/5236electromagnetismdeep soundingcontrolled sourcesindustrial power lineselectrical resistivityinterpretation |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
А. Н. Шевцов А. А. Жамалетдинов В. В. Колобов М. Б. Баранник |
spellingShingle |
А. Н. Шевцов А. А. Жамалетдинов В. В. Колобов М. Б. Баранник Frequency electromagnetic sounding with industrial power lines on Karelia-Kola geotraverse Zapiski Gornogo Instituta electromagnetism deep sounding controlled sources industrial power lines electrical resistivity interpretation |
author_facet |
А. Н. Шевцов А. А. Жамалетдинов В. В. Колобов М. Б. Баранник |
author_sort |
А. Н. Шевцов |
title |
Frequency electromagnetic sounding with industrial power lines on Karelia-Kola geotraverse |
title_short |
Frequency electromagnetic sounding with industrial power lines on Karelia-Kola geotraverse |
title_full |
Frequency electromagnetic sounding with industrial power lines on Karelia-Kola geotraverse |
title_fullStr |
Frequency electromagnetic sounding with industrial power lines on Karelia-Kola geotraverse |
title_full_unstemmed |
Frequency electromagnetic sounding with industrial power lines on Karelia-Kola geotraverse |
title_sort |
frequency electromagnetic sounding with industrial power lines on karelia-kola geotraverse |
publisher |
Saint-Petersburg Mining University |
series |
Zapiski Gornogo Instituta |
issn |
2411-3336 2541-9404 |
publishDate |
2017-04-01 |
description |
The paper describes theory, method and first experimental results of research on the interaction between electromagnetic waves of extremely low and ultra low frequency (0.1-200 Hz), the Earth crust and ionosphere in the field of two mutually orthogonal industrial power lines, 109 and 120 km long, in the course of FENICS experiment (Fennoscandian Electrical conductivity from Natural and Induction Control Source soundings). The main focus was on the observation results along the line of Karelia-Kola geotraverse over a distance of 700 km from the source. High horizontal homogeneity of geoelectrical lithosphere section has been detected in the eastern part of the Baltic shield at depth range from 10-15 to 50-70 km. Parameters of «regular» lithosphere section have been specified to the depth of 60-70 km. As a result of inverse problem solution for the western part of Karelia and Central Finland, a zone of decreased transverse resistivity has been detected at the depth of 50-60 km, corresponding to the area, detected by seismic methods, where Moho boundary reaches the same depth. |
topic |
electromagnetism deep sounding controlled sources industrial power lines electrical resistivity interpretation |
url |
http://pmi.spmi.ru/index.php/pmi/article/view/5236 |
work_keys_str_mv |
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