Study on fine soil behaviour in function of temperature in the context of climate change

One of the expected effects of global warming is the gradual melting of permafrost. Its melting will significantly impact soil material properties, potentially causing instability of infrastructures and triggering natural hazards. The objective of this experimentation is to quantify the effect of th...

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Main Authors: Torche, Jérémy, Howald, Erika Prina
Format: Text
Language:English
Published: Granarolo dell'Emilia (BO), Prof. Riccardo PÃ tron & C. S.r.l. 2024
Subjects:
Online Access:https://doi.org/10.19199/2023.169.1121-9041.036
https://arodes.hes-so.ch/record/14622/files/Torche_2023_study_fine_soil_behaviour_function_temperature_context_climate_change.pdf
http://arodes.hes-so.ch/record/14622
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spelling fthessoch:oai:hesso.tind.io:14622 2024-09-30T14:41:14+00:00 Study on fine soil behaviour in function of temperature in the context of climate change Torche, Jérémy Howald, Erika Prina 2024-08-21T06:44:05Z https://doi.org/10.19199/2023.169.1121-9041.036 https://arodes.hes-so.ch/record/14622/files/Torche_2023_study_fine_soil_behaviour_function_temperature_context_climate_change.pdf http://arodes.hes-so.ch/record/14622 eng eng Granarolo dell'Emilia (BO), Prof. Riccardo Pà tron & C. S.r.l. doi:10.19199/2023.169.1121-9041.036 https://arodes.hes-so.ch/record/14622/files/Torche_2023_study_fine_soil_behaviour_function_temperature_context_climate_change.pdf http://arodes.hes-so.ch/record/14622 http://arodes.hes-so.ch/record/14622 Text 2024 fthessoch https://doi.org/10.19199/2023.169.1121-9041.036 2024-09-01T23:35:00Z One of the expected effects of global warming is the gradual melting of permafrost. Its melting will significantly impact soil material properties, potentially causing instability of infrastructures and triggering natural hazards. The objective of this experimentation is to quantify the effect of thawing on the geomechanical strength of a reconstituted fine soil. More specifically, it is intended to qualify the initial frozen state and compare it to the state after thawing. This study was carried out in three steps. To begin, soil samples were identified by the usual parameters. Then, artificial samples were sheared at a temperature of –5°C in our temperature controlled triaxial press in order to determine the soil’s parameters. Finally, identical tests were carried out at a temperature of +5°C in order to thaw the soil completely before the shearing. In total, three tests for each temperature were compared and discussed. The expected results aim at a better understanding and quantification of soil strength reduction after the thawing phase. As many infrastructures are now built on permafrost, such as infrastructures, or alpine chalets, they will be affected by this phenomenon in the near future. A better understanding of (geo)mechanical consequences might facilitate risk analysis, evaluation and mitigation Text permafrost Hes-so: ArODES Open Archive (University of Applied Sciences and Arts Western Switzerland)
institution Open Polar
collection Hes-so: ArODES Open Archive (University of Applied Sciences and Arts Western Switzerland)
op_collection_id fthessoch
language English
description One of the expected effects of global warming is the gradual melting of permafrost. Its melting will significantly impact soil material properties, potentially causing instability of infrastructures and triggering natural hazards. The objective of this experimentation is to quantify the effect of thawing on the geomechanical strength of a reconstituted fine soil. More specifically, it is intended to qualify the initial frozen state and compare it to the state after thawing. This study was carried out in three steps. To begin, soil samples were identified by the usual parameters. Then, artificial samples were sheared at a temperature of –5°C in our temperature controlled triaxial press in order to determine the soil’s parameters. Finally, identical tests were carried out at a temperature of +5°C in order to thaw the soil completely before the shearing. In total, three tests for each temperature were compared and discussed. The expected results aim at a better understanding and quantification of soil strength reduction after the thawing phase. As many infrastructures are now built on permafrost, such as infrastructures, or alpine chalets, they will be affected by this phenomenon in the near future. A better understanding of (geo)mechanical consequences might facilitate risk analysis, evaluation and mitigation
format Text
author Torche, Jérémy
Howald, Erika Prina
spellingShingle Torche, Jérémy
Howald, Erika Prina
Study on fine soil behaviour in function of temperature in the context of climate change
author_facet Torche, Jérémy
Howald, Erika Prina
author_sort Torche, Jérémy
title Study on fine soil behaviour in function of temperature in the context of climate change
title_short Study on fine soil behaviour in function of temperature in the context of climate change
title_full Study on fine soil behaviour in function of temperature in the context of climate change
title_fullStr Study on fine soil behaviour in function of temperature in the context of climate change
title_full_unstemmed Study on fine soil behaviour in function of temperature in the context of climate change
title_sort study on fine soil behaviour in function of temperature in the context of climate change
publisher Granarolo dell'Emilia (BO), Prof. Riccardo PÃ tron & C. S.r.l.
publishDate 2024
url https://doi.org/10.19199/2023.169.1121-9041.036
https://arodes.hes-so.ch/record/14622/files/Torche_2023_study_fine_soil_behaviour_function_temperature_context_climate_change.pdf
http://arodes.hes-so.ch/record/14622
genre permafrost
genre_facet permafrost
op_source http://arodes.hes-so.ch/record/14622
op_relation doi:10.19199/2023.169.1121-9041.036
https://arodes.hes-so.ch/record/14622/files/Torche_2023_study_fine_soil_behaviour_function_temperature_context_climate_change.pdf
http://arodes.hes-so.ch/record/14622
op_doi https://doi.org/10.19199/2023.169.1121-9041.036
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