High-resolution electrical resistivity tomography applied to patterned ground, Wedel Jarlsberg Land, south-west Spitsbergen

This article presents results of two-dimensional electrical resistivity tomography (ERT) applied to three types of patterned ground in Wedel-Jarlsberg Land (Svalbard), carried out in late July 2012. The structures investigated include sorted circles, non-sorted polygons and a net with sorted coarser...

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Published in:Polar Research
Main Author: Kasprzak, Marek
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2015
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/3233
https://doi.org/10.3402/polar.v34.25678
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spelling ftjpolarres:oai:journals.openacademia.net:article/3233 2024-09-09T20:02:45+00:00 High-resolution electrical resistivity tomography applied to patterned ground, Wedel Jarlsberg Land, south-west Spitsbergen Kasprzak, Marek 2015-06-18 application/pdf text/html application/epub+zip application/xml https://polarresearch.net/index.php/polar/article/view/3233 https://doi.org/10.3402/polar.v34.25678 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/3233/pdf_29 https://polarresearch.net/index.php/polar/article/view/3233/html_22 https://polarresearch.net/index.php/polar/article/view/3233/_23 https://polarresearch.net/index.php/polar/article/view/3233/xml_21 https://polarresearch.net/index.php/polar/article/view/3233 doi:10.3402/polar.v34.25678 Polar Research; Vol 34 (2015) 1751-8369 Patterned ground permafrost active layer electrical imaging Svalbard info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftjpolarres https://doi.org/10.3402/polar.v34.25678 2024-06-20T23:33:17Z This article presents results of two-dimensional electrical resistivity tomography (ERT) applied to three types of patterned ground in Wedel-Jarlsberg Land (Svalbard), carried out in late July 2012. The structures investigated include sorted circles, non-sorted polygons and a net with sorted coarser material. ERT was used to recognize the internal ground structure, the shape of permafrost table below the active layer and the geometric relationships between permafrost, ground layering and surface patterns. Results of inversion modelling indicate that the permafrost table occurs at a depth of 0.5–1 m in a mountain valley and 1–2.5 m on raised marine terraces. The permafrost table was nearly planar beneath non-sorted deposits and wavy beneath sorted materials. The mutual relationships between the permafrost table and the shape of a stone circle are different from those typically presented in literature. Ground structure beneath the net with sorted coarser materials is complex as implied in convective models. In non-sorted polygons, the imaging failed to reveal vertical structures between them.Keywords: Patterned ground; permafrost; active layer; electrical imaging; Svalbard.(Published: 18 June 2015)Citation: Polar Research 2015, 34, 25678,http://dx.doi.org/10.3402/polar.v34.25678 Article in Journal/Newspaper permafrost Polar Research Svalbard Wedel Jarlsberg Land Spitsbergen Polar Research Svalbard Wedel Jarlsberg Land ENVELOPE(15.362,15.362,77.201,77.201) Wedel-Jarlsberg ENVELOPE(-165.133,-165.133,-85.650,-85.650) Polar Research 34 1 25678
institution Open Polar
collection Polar Research
op_collection_id ftjpolarres
language English
topic Patterned ground
permafrost
active layer
electrical imaging
Svalbard
spellingShingle Patterned ground
permafrost
active layer
electrical imaging
Svalbard
Kasprzak, Marek
High-resolution electrical resistivity tomography applied to patterned ground, Wedel Jarlsberg Land, south-west Spitsbergen
topic_facet Patterned ground
permafrost
active layer
electrical imaging
Svalbard
description This article presents results of two-dimensional electrical resistivity tomography (ERT) applied to three types of patterned ground in Wedel-Jarlsberg Land (Svalbard), carried out in late July 2012. The structures investigated include sorted circles, non-sorted polygons and a net with sorted coarser material. ERT was used to recognize the internal ground structure, the shape of permafrost table below the active layer and the geometric relationships between permafrost, ground layering and surface patterns. Results of inversion modelling indicate that the permafrost table occurs at a depth of 0.5–1 m in a mountain valley and 1–2.5 m on raised marine terraces. The permafrost table was nearly planar beneath non-sorted deposits and wavy beneath sorted materials. The mutual relationships between the permafrost table and the shape of a stone circle are different from those typically presented in literature. Ground structure beneath the net with sorted coarser materials is complex as implied in convective models. In non-sorted polygons, the imaging failed to reveal vertical structures between them.Keywords: Patterned ground; permafrost; active layer; electrical imaging; Svalbard.(Published: 18 June 2015)Citation: Polar Research 2015, 34, 25678,http://dx.doi.org/10.3402/polar.v34.25678
format Article in Journal/Newspaper
author Kasprzak, Marek
author_facet Kasprzak, Marek
author_sort Kasprzak, Marek
title High-resolution electrical resistivity tomography applied to patterned ground, Wedel Jarlsberg Land, south-west Spitsbergen
title_short High-resolution electrical resistivity tomography applied to patterned ground, Wedel Jarlsberg Land, south-west Spitsbergen
title_full High-resolution electrical resistivity tomography applied to patterned ground, Wedel Jarlsberg Land, south-west Spitsbergen
title_fullStr High-resolution electrical resistivity tomography applied to patterned ground, Wedel Jarlsberg Land, south-west Spitsbergen
title_full_unstemmed High-resolution electrical resistivity tomography applied to patterned ground, Wedel Jarlsberg Land, south-west Spitsbergen
title_sort high-resolution electrical resistivity tomography applied to patterned ground, wedel jarlsberg land, south-west spitsbergen
publisher Norwegian Polar Institute
publishDate 2015
url https://polarresearch.net/index.php/polar/article/view/3233
https://doi.org/10.3402/polar.v34.25678
long_lat ENVELOPE(15.362,15.362,77.201,77.201)
ENVELOPE(-165.133,-165.133,-85.650,-85.650)
geographic Svalbard
Wedel Jarlsberg Land
Wedel-Jarlsberg
geographic_facet Svalbard
Wedel Jarlsberg Land
Wedel-Jarlsberg
genre permafrost
Polar Research
Svalbard
Wedel Jarlsberg Land
Spitsbergen
genre_facet permafrost
Polar Research
Svalbard
Wedel Jarlsberg Land
Spitsbergen
op_source Polar Research; Vol 34 (2015)
1751-8369
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container_title Polar Research
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