Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica

The historic site and monument n° 38, Nordenskjöld Hut, is located on Snow Hill Island, James Ross archipelago, Antarctica. This is a place of a great historic and heritage value because there are very few centennial buildings in Antarctica. This building was built in February 1902 as a refuge by th...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Silva Busso, A., Yermolin, Y.
Formato: JOUR
Materias:
Antarctica
Historic site and monument
Nordenskjöld hut
Permafrost
Snow hill island
climate effect
embankment
erosion
heritage conservation
historic building
monument
permafrost
preservation
warming
James Ross Island
Snow Hill Island
West Antarctica
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_03660176_v128_n1_p207_SilvaBusso
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires
id todo:paper_03660176_v128_n1_p207_SilvaBusso
record_format dspace
spelling todo:paper_03660176_v128_n1_p207_SilvaBusso2023-10-03T15:28:07Z Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica Silva Busso, A. Yermolin, Y. Antarctica Historic site and monument Nordenskjöld hut Permafrost Snow hill island climate effect embankment erosion heritage conservation historic building monument permafrost preservation warming Antarctica James Ross Island Snow Hill Island West Antarctica The historic site and monument n° 38, Nordenskjöld Hut, is located on Snow Hill Island, James Ross archipelago, Antarctica. This is a place of a great historic and heritage value because there are very few centennial buildings in Antarctica. This building was built in February 1902 as a refuge by the Swedish expedition directed by Otto Nordenskjöld, between 1901 and1904. The building is located over an embankment with ice-rich permafrost, which produces unstable conditions for the foundation. In the past anthropic factors accelerated this process, for example the use of the hut as refuge and garage for other field campaigns. Intensive and potentially destructive signs are observed as a consequence of the thermokarst and erosion active processes in the last decades, in relation with climate warming. Around the embankment the erosion processes are connected with underground icethaw occurring in the top of the permafrost. The embankment area contains 17-20% of underground ice and the mean active layer depth is 1.2 m. A potential maximum settlement of the embankment top surface between 0.15-0.25m has been estimated. The above mentioned processes are consequence of ice thaw in the permafrost table. This would modify the natural surface and could produce significant damages. This study analyzes contingency and mitigation strategies to prevent or reduce the rate of settlement and avoid altering the top of the embankment. The goal is to protect the slopes and foundation from surface erosion and thermo-erosion. We propose increasing the thickness of the embankment, making a frame on the shoulder of the embankment and carrying out a retaining wall or socket in the foundation. © 2017, Instituto Geologico y Minero de Espana. All rights reserved. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_03660176_v128_n1_p207_SilvaBusso
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Antarctica
Historic site and monument
Nordenskjöld hut
Permafrost
Snow hill island
climate effect
embankment
erosion
heritage conservation
historic building
monument
permafrost
preservation
warming
Antarctica
James Ross Island
Snow Hill Island
West Antarctica
spellingShingle Antarctica
Historic site and monument
Nordenskjöld hut
Permafrost
Snow hill island
climate effect
embankment
erosion
heritage conservation
historic building
monument
permafrost
preservation
warming
Antarctica
James Ross Island
Snow Hill Island
West Antarctica
Silva Busso, A.
Yermolin, Y.
Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica
topic_facet Antarctica
Historic site and monument
Nordenskjöld hut
Permafrost
Snow hill island
climate effect
embankment
erosion
heritage conservation
historic building
monument
permafrost
preservation
warming
Antarctica
James Ross Island
Snow Hill Island
West Antarctica
description The historic site and monument n° 38, Nordenskjöld Hut, is located on Snow Hill Island, James Ross archipelago, Antarctica. This is a place of a great historic and heritage value because there are very few centennial buildings in Antarctica. This building was built in February 1902 as a refuge by the Swedish expedition directed by Otto Nordenskjöld, between 1901 and1904. The building is located over an embankment with ice-rich permafrost, which produces unstable conditions for the foundation. In the past anthropic factors accelerated this process, for example the use of the hut as refuge and garage for other field campaigns. Intensive and potentially destructive signs are observed as a consequence of the thermokarst and erosion active processes in the last decades, in relation with climate warming. Around the embankment the erosion processes are connected with underground icethaw occurring in the top of the permafrost. The embankment area contains 17-20% of underground ice and the mean active layer depth is 1.2 m. A potential maximum settlement of the embankment top surface between 0.15-0.25m has been estimated. The above mentioned processes are consequence of ice thaw in the permafrost table. This would modify the natural surface and could produce significant damages. This study analyzes contingency and mitigation strategies to prevent or reduce the rate of settlement and avoid altering the top of the embankment. The goal is to protect the slopes and foundation from surface erosion and thermo-erosion. We propose increasing the thickness of the embankment, making a frame on the shoulder of the embankment and carrying out a retaining wall or socket in the foundation. © 2017, Instituto Geologico y Minero de Espana. All rights reserved.
format JOUR
author Silva Busso, A.
Yermolin, Y.
author_facet Silva Busso, A.
Yermolin, Y.
author_sort Silva Busso, A.
title Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica
title_short Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica
title_full Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica
title_fullStr Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica
title_full_unstemmed Geologic - geotechnical characteristics and preservation proposals for the Historic Site and Monument n° 38, Nordenskjöld’s Hut, Antarctica
title_sort geologic - geotechnical characteristics and preservation proposals for the historic site and monument n° 38, nordenskjöld’s hut, antarctica
url http://hdl.handle.net/20.500.12110/paper_03660176_v128_n1_p207_SilvaBusso
work_keys_str_mv AT silvabussoa geologicgeotechnicalcharacteristicsandpreservationproposalsforthehistoricsiteandmonumentn38nordenskjoldshutantarctica
AT yermoliny geologicgeotechnicalcharacteristicsandpreservationproposalsforthehistoricsiteandmonumentn38nordenskjoldshutantarctica
_version_ 1807314958339276800

Ejemplares similares