Thermal conductivity and thermal diffusivity of cores from a 26 meter deep borehole drilled in Livingston Island, Maritime Antarctic

Detalhes bibliográficos
Autor(a) principal: Correia, António
Data de Publicação: 2012
Outros Autores: Vieira, Gonçalo, Ramos, Miguel
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10174/6561
https://doi.org/http://dx.doi.org/10.1016/j.geomorph.2011.12.012
Resumo: During the month of January of 2008 a borehole (Permamodel-Gulbenkian 1 — PG1) 26 m deep was drilled on the top of Mount Reina Sofia (275 m a.s.l.) near the Spanish Antarctic Station of Livingston Island, South Shetland Islands. Cores from1.5 mto about 26mdeepwere collected formeasuring several physical properties. The objective of the present work is to report the values of the thermal conductivity and the thermal diffusivity that were measured in the cores fromthe borehole and the heat production thatwas estimated for the geological formations intercepted by it. Seven coreswere selected to measure the thermal conductivity and the thermal diffusivity. The measured values for the thermal conductivity vary from2.6W/mK to 3.3 W/mKwhile the measured values for the thermal diffusivity vary from 1.1×10−6 m2/s to 1.6×10−6 m2/s. Both thermal conductivity and thermal diffusivity, on average, show a slight increase with depth. Average heat production was also estimated for two portions of the borehole: one from2 to 12mand the other from12 to 25 m. A gamma-ray spectrometer was used to estimate the concentrations of uranium, thorium, and potassium of the cores, from which the heat production per unit volume was calculated. The estimated heat production for the first half of the borehole is 2.218 μW/m3 while for the second half it is 2.173 μW/m3; these heat production values are compatiblewith acidic rock types. Porosity and density were also estimated for the same cores.
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spelling Thermal conductivity and thermal diffusivity of cores from a 26 meter deep borehole drilled in Livingston Island, Maritime AntarcticThermal conductivityThermal diffusivityLivingston IslandAntarctica PeninsulaDuring the month of January of 2008 a borehole (Permamodel-Gulbenkian 1 — PG1) 26 m deep was drilled on the top of Mount Reina Sofia (275 m a.s.l.) near the Spanish Antarctic Station of Livingston Island, South Shetland Islands. Cores from1.5 mto about 26mdeepwere collected formeasuring several physical properties. The objective of the present work is to report the values of the thermal conductivity and the thermal diffusivity that were measured in the cores fromthe borehole and the heat production thatwas estimated for the geological formations intercepted by it. Seven coreswere selected to measure the thermal conductivity and the thermal diffusivity. The measured values for the thermal conductivity vary from2.6W/mK to 3.3 W/mKwhile the measured values for the thermal diffusivity vary from 1.1×10−6 m2/s to 1.6×10−6 m2/s. Both thermal conductivity and thermal diffusivity, on average, show a slight increase with depth. Average heat production was also estimated for two portions of the borehole: one from2 to 12mand the other from12 to 25 m. A gamma-ray spectrometer was used to estimate the concentrations of uranium, thorium, and potassium of the cores, from which the heat production per unit volume was calculated. The estimated heat production for the first half of the borehole is 2.218 μW/m3 while for the second half it is 2.173 μW/m3; these heat production values are compatiblewith acidic rock types. Porosity and density were also estimated for the same cores.Elsevier2012-12-06T18:27:08Z2012-12-062012-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://hdl.handle.net/10174/6561https://doi.org/http://dx.doi.org/10.1016/j.geomorph.2011.12.012http://hdl.handle.net/10174/6561eng7-11155 - 156Geomorphologycorreia@uevora.ptndnd247Correia, AntónioVieira, GonçaloRamos, Miguelinfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2024-01-03T18:43:17Zoai:dspace.uevora.pt:10174/6561Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T01:00:03.601971Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv Thermal conductivity and thermal diffusivity of cores from a 26 meter deep borehole drilled in Livingston Island, Maritime Antarctic
title Thermal conductivity and thermal diffusivity of cores from a 26 meter deep borehole drilled in Livingston Island, Maritime Antarctic
spellingShingle Thermal conductivity and thermal diffusivity of cores from a 26 meter deep borehole drilled in Livingston Island, Maritime Antarctic
Correia, António
Thermal conductivity
Thermal diffusivity
Livingston Island
Antarctica Peninsula
title_short Thermal conductivity and thermal diffusivity of cores from a 26 meter deep borehole drilled in Livingston Island, Maritime Antarctic
title_full Thermal conductivity and thermal diffusivity of cores from a 26 meter deep borehole drilled in Livingston Island, Maritime Antarctic
title_fullStr Thermal conductivity and thermal diffusivity of cores from a 26 meter deep borehole drilled in Livingston Island, Maritime Antarctic
title_full_unstemmed Thermal conductivity and thermal diffusivity of cores from a 26 meter deep borehole drilled in Livingston Island, Maritime Antarctic
title_sort Thermal conductivity and thermal diffusivity of cores from a 26 meter deep borehole drilled in Livingston Island, Maritime Antarctic
author Correia, António
author_facet Correia, António
Vieira, Gonçalo
Ramos, Miguel
author_role author
author2 Vieira, Gonçalo
Ramos, Miguel
author2_role author
author
dc.contributor.author.fl_str_mv Correia, António
Vieira, Gonçalo
Ramos, Miguel
dc.subject.por.fl_str_mv Thermal conductivity
Thermal diffusivity
Livingston Island
Antarctica Peninsula
topic Thermal conductivity
Thermal diffusivity
Livingston Island
Antarctica Peninsula
description During the month of January of 2008 a borehole (Permamodel-Gulbenkian 1 — PG1) 26 m deep was drilled on the top of Mount Reina Sofia (275 m a.s.l.) near the Spanish Antarctic Station of Livingston Island, South Shetland Islands. Cores from1.5 mto about 26mdeepwere collected formeasuring several physical properties. The objective of the present work is to report the values of the thermal conductivity and the thermal diffusivity that were measured in the cores fromthe borehole and the heat production thatwas estimated for the geological formations intercepted by it. Seven coreswere selected to measure the thermal conductivity and the thermal diffusivity. The measured values for the thermal conductivity vary from2.6W/mK to 3.3 W/mKwhile the measured values for the thermal diffusivity vary from 1.1×10−6 m2/s to 1.6×10−6 m2/s. Both thermal conductivity and thermal diffusivity, on average, show a slight increase with depth. Average heat production was also estimated for two portions of the borehole: one from2 to 12mand the other from12 to 25 m. A gamma-ray spectrometer was used to estimate the concentrations of uranium, thorium, and potassium of the cores, from which the heat production per unit volume was calculated. The estimated heat production for the first half of the borehole is 2.218 μW/m3 while for the second half it is 2.173 μW/m3; these heat production values are compatiblewith acidic rock types. Porosity and density were also estimated for the same cores.
publishDate 2012
dc.date.none.fl_str_mv 2012-12-06T18:27:08Z
2012-12-06
2012-01-01T00:00:00Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://hdl.handle.net/10174/6561
https://doi.org/http://dx.doi.org/10.1016/j.geomorph.2011.12.012
http://hdl.handle.net/10174/6561
url http://hdl.handle.net/10174/6561
https://doi.org/http://dx.doi.org/10.1016/j.geomorph.2011.12.012
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 7-11
155 - 156
Geomorphology
correia@uevora.pt
nd
nd
247
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
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dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
dc.source.none.fl_str_mv reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
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instname_str Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação
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reponame_str Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
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repository.name.fl_str_mv Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação
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