Modelling of geomagnetic induction in pipelines

Geomagnetic field variations induce telluric currents in pipelines, which modify the electrochemical conditions at the pipe/soil interface, possibly contributing to corrosion of the pipeline steel. Modelling of geomagnetic induction in pipelines can be accomplished by combining several techn...

Full description

Bibliographic Details
Main Authors: L. Trichtchenko, D. H. Boteler
Format: Article
Language:English
Published: Copernicus Publications 2002-07-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/20/1063/2002/angeo-20-1063-2002.pdf
id doaj-c1ab1604731b42779b5211bd89a1f7b7
record_format Article
spelling doaj-c1ab1604731b42779b5211bd89a1f7b72020-11-24T23:42:40ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762002-07-01201063107210.5194/angeo-20-1063-2002Modelling of geomagnetic induction in pipelinesL. Trichtchenko0L. Trichtchenko1L. Trichtchenko2D. H. Boteler3Correspondence to: L. TrichtchenkoGeomagnetic Laboratory, Geological Survey of Canada, 7 Observatory Crescent, Ottawa, Ontario K1A 0Y3, Canada(ltrichtc@NRCan.gc.ca)Geomagnetic Laboratory, Geological Survey of Canada, 7 Observatory Crescent, Ottawa, Ontario K1A 0Y3, CanadaGeomagnetic field variations induce telluric currents in pipelines, which modify the electrochemical conditions at the pipe/soil interface, possibly contributing to corrosion of the pipeline steel. Modelling of geomagnetic induction in pipelines can be accomplished by combining several techniques. Starting with geomagnetic field data, the geoelectric fields in the absence of the pipeline were calculated using the surface impedance derived from a layered-Earth conductivity model. The influence of the pipeline on the electric fields was then examined using an infinitely long cylinder (ILC) model. Pipe-to-soil potentials produced by the electric field induced in the pipeline were calculated using a distributed source transmission line (DSTL) model. The geomagnetic induction process is frequency dependent; therefore, the calculations are best performed in the frequency domain, using a Fourier transform to go from the original time domain magnetic data, and an inverse Fourier transform at the end of the process, to obtain the pipe-to-soil potential variation in the time domain. Examples of the model calculations are presented and compared to observations made on a long pipeline in the auroral zone.<br><br><b>Key words. </b>Geomagnetism and paleomagnetism (geo-magnetic induction)https://www.ann-geophys.net/20/1063/2002/angeo-20-1063-2002.pdf
collection DOAJ
language English
format Article
sources DOAJ
author L. Trichtchenko
L. Trichtchenko
L. Trichtchenko
D. H. Boteler
spellingShingle L. Trichtchenko
L. Trichtchenko
L. Trichtchenko
D. H. Boteler
Modelling of geomagnetic induction in pipelines
Annales Geophysicae
author_facet L. Trichtchenko
L. Trichtchenko
L. Trichtchenko
D. H. Boteler
author_sort L. Trichtchenko
title Modelling of geomagnetic induction in pipelines
title_short Modelling of geomagnetic induction in pipelines
title_full Modelling of geomagnetic induction in pipelines
title_fullStr Modelling of geomagnetic induction in pipelines
title_full_unstemmed Modelling of geomagnetic induction in pipelines
title_sort modelling of geomagnetic induction in pipelines
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2002-07-01
description Geomagnetic field variations induce telluric currents in pipelines, which modify the electrochemical conditions at the pipe/soil interface, possibly contributing to corrosion of the pipeline steel. Modelling of geomagnetic induction in pipelines can be accomplished by combining several techniques. Starting with geomagnetic field data, the geoelectric fields in the absence of the pipeline were calculated using the surface impedance derived from a layered-Earth conductivity model. The influence of the pipeline on the electric fields was then examined using an infinitely long cylinder (ILC) model. Pipe-to-soil potentials produced by the electric field induced in the pipeline were calculated using a distributed source transmission line (DSTL) model. The geomagnetic induction process is frequency dependent; therefore, the calculations are best performed in the frequency domain, using a Fourier transform to go from the original time domain magnetic data, and an inverse Fourier transform at the end of the process, to obtain the pipe-to-soil potential variation in the time domain. Examples of the model calculations are presented and compared to observations made on a long pipeline in the auroral zone.<br><br><b>Key words. </b>Geomagnetism and paleomagnetism (geo-magnetic induction)
url https://www.ann-geophys.net/20/1063/2002/angeo-20-1063-2002.pdf
work_keys_str_mv AT ltrichtchenko modellingofgeomagneticinductioninpipelines
AT ltrichtchenko modellingofgeomagneticinductioninpipelines
AT ltrichtchenko modellingofgeomagneticinductioninpipelines
AT dhboteler modellingofgeomagneticinductioninpipelines
_version_ 1725503665704271872