Effect of the electromagnetic environment in pipes in Yakutia

The results of measurements of telluric currents flowing through pipelines laid in the cryolithozone in Yakutia are presented during geomagnetic storms and lightning discharges occurring in the 10 km zone around the pipeline. The currents reach tens of amperes. Construction of a lightning density di...

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Main Authors: Kozlov Vladimir I., Abzaletdinova Larisa M., Tarabukina Lena D., Korsakov Alexey A., Grigoryev Yuri M.
Format: Article
Language:English
Published: EDP Sciences 2017-01-01
Series:E3S Web of Conferences
Online Access:https://doi.org/10.1051/e3sconf/20172001006
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spelling doaj-74c383e510f94e3cbbbddb5a431d15e52021-02-02T02:48:34ZengEDP SciencesE3S Web of Conferences2267-12422017-01-01200100610.1051/e3sconf/20172001006e3sconf_strpep2017_01006Effect of the electromagnetic environment in pipes in YakutiaKozlov Vladimir I.Abzaletdinova Larisa M.Tarabukina Lena D.Korsakov Alexey A.Grigoryev Yuri M.The results of measurements of telluric currents flowing through pipelines laid in the cryolithozone in Yakutia are presented during geomagnetic storms and lightning discharges occurring in the 10 km zone around the pipeline. The currents reach tens of amperes. Construction of a lightning density distribution map. The effect of a direct current flowing in a 150 m long pipeline with a diameter of 110 mm laid in permafrost on the change in the pipe-to-ground potential is measured. Based on the analysis of variations in the horizontal component of the magnetic activity in the current 24th cycle of solar activity, it is established that the frequency of occurrence of a certain level of the rate of change in geomagnetic activity can be expressed by a power law with an order of magnitude of about two at low values. The exponent decreases to unity as the geomagnetic activity increases. The probability of occurrence of time intervals with given threshold values of the rate of change of geomagnetic activity is determined.https://doi.org/10.1051/e3sconf/20172001006
collection DOAJ
language English
format Article
sources DOAJ
author Kozlov Vladimir I.
Abzaletdinova Larisa M.
Tarabukina Lena D.
Korsakov Alexey A.
Grigoryev Yuri M.
spellingShingle Kozlov Vladimir I.
Abzaletdinova Larisa M.
Tarabukina Lena D.
Korsakov Alexey A.
Grigoryev Yuri M.
Effect of the electromagnetic environment in pipes in Yakutia
E3S Web of Conferences
author_facet Kozlov Vladimir I.
Abzaletdinova Larisa M.
Tarabukina Lena D.
Korsakov Alexey A.
Grigoryev Yuri M.
author_sort Kozlov Vladimir I.
title Effect of the electromagnetic environment in pipes in Yakutia
title_short Effect of the electromagnetic environment in pipes in Yakutia
title_full Effect of the electromagnetic environment in pipes in Yakutia
title_fullStr Effect of the electromagnetic environment in pipes in Yakutia
title_full_unstemmed Effect of the electromagnetic environment in pipes in Yakutia
title_sort effect of the electromagnetic environment in pipes in yakutia
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2017-01-01
description The results of measurements of telluric currents flowing through pipelines laid in the cryolithozone in Yakutia are presented during geomagnetic storms and lightning discharges occurring in the 10 km zone around the pipeline. The currents reach tens of amperes. Construction of a lightning density distribution map. The effect of a direct current flowing in a 150 m long pipeline with a diameter of 110 mm laid in permafrost on the change in the pipe-to-ground potential is measured. Based on the analysis of variations in the horizontal component of the magnetic activity in the current 24th cycle of solar activity, it is established that the frequency of occurrence of a certain level of the rate of change in geomagnetic activity can be expressed by a power law with an order of magnitude of about two at low values. The exponent decreases to unity as the geomagnetic activity increases. The probability of occurrence of time intervals with given threshold values of the rate of change of geomagnetic activity is determined.
url https://doi.org/10.1051/e3sconf/20172001006
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