Repeated Electrical Resistivity Tomographies in a CALM Site in Livingston Island, Maritime Antarctica

During the years of 2009, 2012, and 2013 several electrical resistivity tomographies (ERTs) were done in a CALM (Circumpolar Active Layer Monitoring) site near the Bulgarian Antarctic Base of St. Kliment Ohridski. The main objective of the ERTs was to try to identify permafrost zones and their exten...

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Main Authors: Correia, António M., Rocha, João, Vieira, Gonçalo
Format: Article in Journal/Newspaper
Language:English
Published: European Association of Geoscientists and Engineers 2013
Subjects:
Online Access:http://hdl.handle.net/10174/9719
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record_format openpolar
spelling ftunivevora:oai:dspace.uevora.pt:10174/9719 2023-09-05T13:11:08+02:00 Repeated Electrical Resistivity Tomographies in a CALM Site in Livingston Island, Maritime Antarctica Correia, António M. Rocha, João Vieira, Gonçalo 2013 http://hdl.handle.net/10174/9719 eng eng European Association of Geoscientists and Engineers http://hdl.handle.net/10174/9719 Earthdoc coreia@uevora.pt jrocha@uevora.pt vieira@campus.ul.pt 393 openAccess Electrical Resistivity Tomography Maritime Antarctica article 2013 ftunivevora 2023-08-14T17:32:51Z During the years of 2009, 2012, and 2013 several electrical resistivity tomographies (ERTs) were done in a CALM (Circumpolar Active Layer Monitoring) site near the Bulgarian Antarctic Base of St. Kliment Ohridski. The main objective of the ERTs was to try to identify permafrost zones and their extension, as well as their time and space evolution. Geoelectrical methods, in particular ERTs, are very useful for permafrost studies because of the significant increase of the electrical resistivity when the ground is partially or totally frozen and when temperature is lower than 0 degrees celcius. For each ERT made, 40 electrodes in line, spaced by 2 metres each, were used and the apparent electrical resistivity measurements were mathematically inverted to obtain two-dimensional geoelectrical models for each of them. All models show high electrical resistivity values (of the order of tens of thousands of Ω.m). In the CALM site the high electrical resistivities probably correspond to patches of frozen ground but it is not possible to indicate whether it is sporadic permafrost or remnants of seasonally frozen ground yet. Article in Journal/Newspaper Active layer monitoring Antarc* Antarctic Antarctica Livingston Island permafrost Repositório Científico da Universidade de Évora Antarctic Livingston Island ENVELOPE(-60.500,-60.500,-62.600,-62.600)
institution Open Polar
collection Repositório Científico da Universidade de Évora
op_collection_id ftunivevora
language English
topic Electrical Resistivity Tomography
Maritime Antarctica
spellingShingle Electrical Resistivity Tomography
Maritime Antarctica
Correia, António M.
Rocha, João
Vieira, Gonçalo
Repeated Electrical Resistivity Tomographies in a CALM Site in Livingston Island, Maritime Antarctica
topic_facet Electrical Resistivity Tomography
Maritime Antarctica
description During the years of 2009, 2012, and 2013 several electrical resistivity tomographies (ERTs) were done in a CALM (Circumpolar Active Layer Monitoring) site near the Bulgarian Antarctic Base of St. Kliment Ohridski. The main objective of the ERTs was to try to identify permafrost zones and their extension, as well as their time and space evolution. Geoelectrical methods, in particular ERTs, are very useful for permafrost studies because of the significant increase of the electrical resistivity when the ground is partially or totally frozen and when temperature is lower than 0 degrees celcius. For each ERT made, 40 electrodes in line, spaced by 2 metres each, were used and the apparent electrical resistivity measurements were mathematically inverted to obtain two-dimensional geoelectrical models for each of them. All models show high electrical resistivity values (of the order of tens of thousands of Ω.m). In the CALM site the high electrical resistivities probably correspond to patches of frozen ground but it is not possible to indicate whether it is sporadic permafrost or remnants of seasonally frozen ground yet.
format Article in Journal/Newspaper
author Correia, António M.
Rocha, João
Vieira, Gonçalo
author_facet Correia, António M.
Rocha, João
Vieira, Gonçalo
author_sort Correia, António M.
title Repeated Electrical Resistivity Tomographies in a CALM Site in Livingston Island, Maritime Antarctica
title_short Repeated Electrical Resistivity Tomographies in a CALM Site in Livingston Island, Maritime Antarctica
title_full Repeated Electrical Resistivity Tomographies in a CALM Site in Livingston Island, Maritime Antarctica
title_fullStr Repeated Electrical Resistivity Tomographies in a CALM Site in Livingston Island, Maritime Antarctica
title_full_unstemmed Repeated Electrical Resistivity Tomographies in a CALM Site in Livingston Island, Maritime Antarctica
title_sort repeated electrical resistivity tomographies in a calm site in livingston island, maritime antarctica
publisher European Association of Geoscientists and Engineers
publishDate 2013
url http://hdl.handle.net/10174/9719
long_lat ENVELOPE(-60.500,-60.500,-62.600,-62.600)
geographic Antarctic
Livingston Island
geographic_facet Antarctic
Livingston Island
genre Active layer monitoring
Antarc*
Antarctic
Antarctica
Livingston Island
permafrost
genre_facet Active layer monitoring
Antarc*
Antarctic
Antarctica
Livingston Island
permafrost
op_relation http://hdl.handle.net/10174/9719
Earthdoc
coreia@uevora.pt
jrocha@uevora.pt
vieira@campus.ul.pt
393
op_rights openAccess
_version_ 1776197764765450240