A permafrost test on intact gneiss rock

Changes in permafrost conditions in high mountain rocks have increased the risk of dangerous instabilities. Ice segregation within the rock mass has been interpreted as one of the mechanisms involved in high mountain bedrock degradation. A long term laboratory test on a cube of intact gneiss has bee...

Full description

Bibliographic Details
Published in:International Journal of Rock Mechanics and Mining Sciences
Main Authors: Duca, S, Alonso Pérez de Agreda, Eduardo, Scavia, Claudio
Other Authors: Universitat Politècnica de Catalunya. Departament d'Enginyeria Civil i Ambiental, Universitat Politècnica de Catalunya. MSR - Mecànica del Sòls i de les Roques
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2015
Subjects:
Ice
Online Access:http://hdl.handle.net/2117/81089
https://doi.org/10.1016/j.ijrmms.2015.02.003
id ftupcatalunyair:oai:upcommons.upc.edu:2117/81089
record_format openpolar
spelling ftupcatalunyair:oai:upcommons.upc.edu:2117/81089 2023-10-09T21:52:16+02:00 A permafrost test on intact gneiss rock Duca, S Alonso Pérez de Agreda, Eduardo Scavia, Claudio Universitat Politècnica de Catalunya. Departament d'Enginyeria Civil i Ambiental Universitat Politècnica de Catalunya. MSR - Mecànica del Sòls i de les Roques 2015-07 10 p. application/pdf http://hdl.handle.net/2117/81089 https://doi.org/10.1016/j.ijrmms.2015.02.003 eng eng Elsevier http://www.sciencedirect.com/science/article/pii/S1365160915000404 Duca, S., Alonso, E., Scavia, C. A permafrost test on intact gneiss rock. "International journal of rock mechanics and mining sciences", Juliol 2015, vol. 77, p. 142-151. 1365-1609 http://hdl.handle.net/2117/81089 doi:10.1016/j.ijrmms.2015.02.003 http://creativecommons.org/licenses/by-nc-nd/3.0/es/ Open Access Àrees temàtiques de la UPC::Enginyeria civil::Geotècnia::Mecànica de roques Gneiss Ice segregation Laboratory test THM modeling Fracturing Wave propagation SLOPE STABILITY SALINE MEDIA FORMULATION MECHANISMS FRACTURE REGIONS FROZEN CURVE SOILS Roques metamòrfiques Article 2015 ftupcatalunyair https://doi.org/10.1016/j.ijrmms.2015.02.003 2023-09-12T23:08:38Z Changes in permafrost conditions in high mountain rocks have increased the risk of dangerous instabilities. Ice segregation within the rock mass has been interpreted as one of the mechanisms involved in high mountain bedrock degradation. A long term laboratory test on a cube of intact gneiss has been designed to reproduce field temperature gradients and water supply conditions. Test results demonstrate that ice crystallization in a permafrost fringe (T=0 degrees C to -3 degrees C) leads to the formation of continuous ice-filled cracks which explain the loss of rock continuity and the observed rock failures. A coupled thermo-hydro-mechanical model which incorporates the thermodynamics of ice-water mixtures has been used to reproduce test results. The model, which follows existing formulations for unsaturated porous media, was capable of capturing the main observations derived from the experiment. Calculated tensile stresses are close to the gneiss tensile strength. The analysis performed is a step forward in understanding field observations and in the application of computational tools to real cases. (C) 2015 Elsevier Ltd. All rights reserved. Peer Reviewed Postprint (author's final draft) Article in Journal/Newspaper Ice permafrost Universitat Politècnica de Catalunya, BarcelonaTech: UPCommons - Global access to UPC knowledge International Journal of Rock Mechanics and Mining Sciences 77 142 151
institution Open Polar
collection Universitat Politècnica de Catalunya, BarcelonaTech: UPCommons - Global access to UPC knowledge
op_collection_id ftupcatalunyair
language English
topic Àrees temàtiques de la UPC::Enginyeria civil::Geotècnia::Mecànica de roques
Gneiss
Ice segregation
Laboratory test
THM modeling
Fracturing
Wave propagation
SLOPE STABILITY
SALINE MEDIA
FORMULATION
MECHANISMS
FRACTURE
REGIONS
FROZEN
CURVE
SOILS
Roques metamòrfiques
spellingShingle Àrees temàtiques de la UPC::Enginyeria civil::Geotècnia::Mecànica de roques
Gneiss
Ice segregation
Laboratory test
THM modeling
Fracturing
Wave propagation
SLOPE STABILITY
SALINE MEDIA
FORMULATION
MECHANISMS
FRACTURE
REGIONS
FROZEN
CURVE
SOILS
Roques metamòrfiques
Duca, S
Alonso Pérez de Agreda, Eduardo
Scavia, Claudio
A permafrost test on intact gneiss rock
topic_facet Àrees temàtiques de la UPC::Enginyeria civil::Geotècnia::Mecànica de roques
Gneiss
Ice segregation
Laboratory test
THM modeling
Fracturing
Wave propagation
SLOPE STABILITY
SALINE MEDIA
FORMULATION
MECHANISMS
FRACTURE
REGIONS
FROZEN
CURVE
SOILS
Roques metamòrfiques
description Changes in permafrost conditions in high mountain rocks have increased the risk of dangerous instabilities. Ice segregation within the rock mass has been interpreted as one of the mechanisms involved in high mountain bedrock degradation. A long term laboratory test on a cube of intact gneiss has been designed to reproduce field temperature gradients and water supply conditions. Test results demonstrate that ice crystallization in a permafrost fringe (T=0 degrees C to -3 degrees C) leads to the formation of continuous ice-filled cracks which explain the loss of rock continuity and the observed rock failures. A coupled thermo-hydro-mechanical model which incorporates the thermodynamics of ice-water mixtures has been used to reproduce test results. The model, which follows existing formulations for unsaturated porous media, was capable of capturing the main observations derived from the experiment. Calculated tensile stresses are close to the gneiss tensile strength. The analysis performed is a step forward in understanding field observations and in the application of computational tools to real cases. (C) 2015 Elsevier Ltd. All rights reserved. Peer Reviewed Postprint (author's final draft)
author2 Universitat Politècnica de Catalunya. Departament d'Enginyeria Civil i Ambiental
Universitat Politècnica de Catalunya. MSR - Mecànica del Sòls i de les Roques
format Article in Journal/Newspaper
author Duca, S
Alonso Pérez de Agreda, Eduardo
Scavia, Claudio
author_facet Duca, S
Alonso Pérez de Agreda, Eduardo
Scavia, Claudio
author_sort Duca, S
title A permafrost test on intact gneiss rock
title_short A permafrost test on intact gneiss rock
title_full A permafrost test on intact gneiss rock
title_fullStr A permafrost test on intact gneiss rock
title_full_unstemmed A permafrost test on intact gneiss rock
title_sort permafrost test on intact gneiss rock
publisher Elsevier
publishDate 2015
url http://hdl.handle.net/2117/81089
https://doi.org/10.1016/j.ijrmms.2015.02.003
genre Ice
permafrost
genre_facet Ice
permafrost
op_relation http://www.sciencedirect.com/science/article/pii/S1365160915000404
Duca, S., Alonso, E., Scavia, C. A permafrost test on intact gneiss rock. "International journal of rock mechanics and mining sciences", Juliol 2015, vol. 77, p. 142-151.
1365-1609
http://hdl.handle.net/2117/81089
doi:10.1016/j.ijrmms.2015.02.003
op_rights http://creativecommons.org/licenses/by-nc-nd/3.0/es/
Open Access
op_doi https://doi.org/10.1016/j.ijrmms.2015.02.003
container_title International Journal of Rock Mechanics and Mining Sciences
container_volume 77
container_start_page 142
op_container_end_page 151
_version_ 1779315399173603328