Vertical electric resistivity sounding of natural and anthropogenically affected cryosols of Fildes Peninsula, Western Antarctica

Natural and anthropogenically-affected Cryosols of the Fildes Peninsula (King George Island, NWAntarcticPeninsula) from the surroundings of Russian polar station Bellingshausen were investigated by vertical electric sounding. The aim of the study was to asses the thawing depth and active layer thick...

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Main Author: Abakumov, Evgeny
Format: Article in Journal/Newspaper
Language:English
Published: Masaryk Univerzity 2017
Subjects:
Online Access:http://journals.muni.cz/CPR/article/view/12996
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spelling ftmasarykunivojs:oai:ojs.journals.muni.cz:article/12996 2023-05-15T13:03:05+02:00 Vertical electric resistivity sounding of natural and anthropogenically affected cryosols of Fildes Peninsula, Western Antarctica Abakumov, Evgeny 2017-06-01 application/pdf http://journals.muni.cz/CPR/article/view/12996 eng eng Masaryk Univerzity http://journals.muni.cz/CPR/article/view/12996/11243 http://journals.muni.cz/CPR/article/view/12996 Copyright (c) 2020 Czech Polar Reports https://creativecommons.org/licenses/by-nc-nd/4.0 CC-BY-NC-ND Czech Polar Reports; Vol 7 No 2 (2017); 109-122 Czech Polar Reports; Vol. 7 No. 2 (2017); 109-122 1805-0697 1805-0689 soils Antarctic Vertical Electric Sounding (VERS) Wastes Polygons (WP) info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2017 ftmasarykunivojs 2022-06-26T10:16:39Z Natural and anthropogenically-affected Cryosols of the Fildes Peninsula (King George Island, NWAntarcticPeninsula) from the surroundings of Russian polar station Bellingshausen were investigated by vertical electric sounding. The aim of the study was to asses the thawing depth and active layer thickness. Natural Turbic Croysols showed lesser thickness of active layer than the soils of former reclaimed wastes disposals. Average thickness of the active layer was 0.3-0.4 m in natural soil and 1.3-1.4 m in anthropogenically-affected ones. This was affected by the change in the temperature regime of soils, and related to the destruction of upper organic layer and mechanical disturbance of the active soil layer on the waste polygons. Itwasshown,thattheuseof vertical electric soundingmethodologyinthesoilsurveysisusefulfor the identificationofthe permafrostdepthwithoutdiggingofsoilpit.Thismethodallowstheidentificationofsoilheterogeneity, because the electric resistivity (ER) values are strongly affected by soil properties. ER also intensively changes on the border of differentgeochemicalregimes,i.e.ontheborderoftheactivelayerandthepermafrost. The lowest ER values were found for the upper organic horizons, the highest for permafrost table. Technogenic Superficial Formations exhibit lower resistivity values than natural soils. Therefore, disposition of WP and disturbance of the soil surface, results in permafrost degradation and an increase in the active layer thickness. Article in Journal/Newspaper Active layer thickness Antarc* Antarctic Antarctica King George Island permafrost Masaryk University Journals Antarctic King George Island Fildes ENVELOPE(-58.817,-58.817,-62.217,-62.217) Fildes peninsula ENVELOPE(-58.948,-58.948,-62.182,-62.182)
institution Open Polar
collection Masaryk University Journals
op_collection_id ftmasarykunivojs
language English
topic soils
Antarctic
Vertical Electric Sounding (VERS)
Wastes Polygons (WP)
spellingShingle soils
Antarctic
Vertical Electric Sounding (VERS)
Wastes Polygons (WP)
Abakumov, Evgeny
Vertical electric resistivity sounding of natural and anthropogenically affected cryosols of Fildes Peninsula, Western Antarctica
topic_facet soils
Antarctic
Vertical Electric Sounding (VERS)
Wastes Polygons (WP)
description Natural and anthropogenically-affected Cryosols of the Fildes Peninsula (King George Island, NWAntarcticPeninsula) from the surroundings of Russian polar station Bellingshausen were investigated by vertical electric sounding. The aim of the study was to asses the thawing depth and active layer thickness. Natural Turbic Croysols showed lesser thickness of active layer than the soils of former reclaimed wastes disposals. Average thickness of the active layer was 0.3-0.4 m in natural soil and 1.3-1.4 m in anthropogenically-affected ones. This was affected by the change in the temperature regime of soils, and related to the destruction of upper organic layer and mechanical disturbance of the active soil layer on the waste polygons. Itwasshown,thattheuseof vertical electric soundingmethodologyinthesoilsurveysisusefulfor the identificationofthe permafrostdepthwithoutdiggingofsoilpit.Thismethodallowstheidentificationofsoilheterogeneity, because the electric resistivity (ER) values are strongly affected by soil properties. ER also intensively changes on the border of differentgeochemicalregimes,i.e.ontheborderoftheactivelayerandthepermafrost. The lowest ER values were found for the upper organic horizons, the highest for permafrost table. Technogenic Superficial Formations exhibit lower resistivity values than natural soils. Therefore, disposition of WP and disturbance of the soil surface, results in permafrost degradation and an increase in the active layer thickness.
format Article in Journal/Newspaper
author Abakumov, Evgeny
author_facet Abakumov, Evgeny
author_sort Abakumov, Evgeny
title Vertical electric resistivity sounding of natural and anthropogenically affected cryosols of Fildes Peninsula, Western Antarctica
title_short Vertical electric resistivity sounding of natural and anthropogenically affected cryosols of Fildes Peninsula, Western Antarctica
title_full Vertical electric resistivity sounding of natural and anthropogenically affected cryosols of Fildes Peninsula, Western Antarctica
title_fullStr Vertical electric resistivity sounding of natural and anthropogenically affected cryosols of Fildes Peninsula, Western Antarctica
title_full_unstemmed Vertical electric resistivity sounding of natural and anthropogenically affected cryosols of Fildes Peninsula, Western Antarctica
title_sort vertical electric resistivity sounding of natural and anthropogenically affected cryosols of fildes peninsula, western antarctica
publisher Masaryk Univerzity
publishDate 2017
url http://journals.muni.cz/CPR/article/view/12996
long_lat ENVELOPE(-58.817,-58.817,-62.217,-62.217)
ENVELOPE(-58.948,-58.948,-62.182,-62.182)
geographic Antarctic
King George Island
Fildes
Fildes peninsula
geographic_facet Antarctic
King George Island
Fildes
Fildes peninsula
genre Active layer thickness
Antarc*
Antarctic
Antarctica
King George Island
permafrost
genre_facet Active layer thickness
Antarc*
Antarctic
Antarctica
King George Island
permafrost
op_source Czech Polar Reports; Vol 7 No 2 (2017); 109-122
Czech Polar Reports; Vol. 7 No. 2 (2017); 109-122
1805-0697
1805-0689
op_relation http://journals.muni.cz/CPR/article/view/12996/11243
http://journals.muni.cz/CPR/article/view/12996
op_rights Copyright (c) 2020 Czech Polar Reports
https://creativecommons.org/licenses/by-nc-nd/4.0
op_rightsnorm CC-BY-NC-ND
_version_ 1766327850233757696