One- and two-dimensional finite element modelling of thaw consolidation
Coupled thermo-hydro-mechanical finite element (FE) modelling of thaw consolidation is presented. One-dimensional FE analyses are performed for thaw consolidation of a soil column due to self-weight and with a combination of self-weight and surcharge, with the linear and nonlinear void ratio–effecti...
Main Authors: | , , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2022
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Subjects: | |
Online Access: | https://figshare.com/articles/journal_contribution/One-_and_two-dimensional_finite_element_modelling_of_thaw_consolidation/27551553 |
_version_ | 1821681995188535296 |
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author | R. Dayarathne B. Hawlader Ryan Phillips Dilan Robert |
author_facet | R. Dayarathne B. Hawlader Ryan Phillips Dilan Robert |
author_sort | R. Dayarathne |
collection | Research from RMIT University |
description | Coupled thermo-hydro-mechanical finite element (FE) modelling of thaw consolidation is presented. One-dimensional FE analyses are performed for thaw consolidation of a soil column due to self-weight and with a combination of self-weight and surcharge, with the linear and nonlinear void ratio–effective stress–hydraulic conductivity relationships of thawed soil. The nonlinear behaviour of thawed soil is modelled using a modified Drucker–Prager Cap model, while the hydraulic conductivity is varied with the void ratio. Finally, two-dimensional FE modelling of thaw consolidation around a warm pipeline buried in permafrost is performed. The rapid reduction of the void ratio with consolidation, especially at the low-stress level, results in a wide variation of hydraulic conductivity within the thawed zone. The significantly large hydraulic conductivity of soil elements along the curved thaw front, as compared to that of thaw consolidated soil, causes the flow of water along the thaw front, instead of a vertical flow, as assumed in previous 1-D thaw consolidation modelling of buried pipelines. |
format | Article in Journal/Newspaper |
genre | permafrost |
genre_facet | permafrost |
id | ftrmitunivfig:oai:figshare.com:article/27551553 |
institution | Open Polar |
language | unknown |
op_collection_id | ftrmitunivfig |
op_relation | 10779/rmit.27551553.v1 |
op_rights | All rights reserved |
publishDate | 2022 |
record_format | openpolar |
spelling | ftrmitunivfig:oai:figshare.com:article/27551553 2025-01-17T00:15:46+00:00 One- and two-dimensional finite element modelling of thaw consolidation R. Dayarathne B. Hawlader Ryan Phillips Dilan Robert 2022-01-01T00:00:00Z https://figshare.com/articles/journal_contribution/One-_and_two-dimensional_finite_element_modelling_of_thaw_consolidation/27551553 unknown 10779/rmit.27551553.v1 All rights reserved Civil geotechnical engineering finite element modelling nonlinear thawed soil behaviour permafrost thaw consolidation warm pipeline Text Journal contribution 2022 ftrmitunivfig 2025-01-03T08:17:24Z Coupled thermo-hydro-mechanical finite element (FE) modelling of thaw consolidation is presented. One-dimensional FE analyses are performed for thaw consolidation of a soil column due to self-weight and with a combination of self-weight and surcharge, with the linear and nonlinear void ratio–effective stress–hydraulic conductivity relationships of thawed soil. The nonlinear behaviour of thawed soil is modelled using a modified Drucker–Prager Cap model, while the hydraulic conductivity is varied with the void ratio. Finally, two-dimensional FE modelling of thaw consolidation around a warm pipeline buried in permafrost is performed. The rapid reduction of the void ratio with consolidation, especially at the low-stress level, results in a wide variation of hydraulic conductivity within the thawed zone. The significantly large hydraulic conductivity of soil elements along the curved thaw front, as compared to that of thaw consolidated soil, causes the flow of water along the thaw front, instead of a vertical flow, as assumed in previous 1-D thaw consolidation modelling of buried pipelines. Article in Journal/Newspaper permafrost Research from RMIT University |
spellingShingle | Civil geotechnical engineering finite element modelling nonlinear thawed soil behaviour permafrost thaw consolidation warm pipeline R. Dayarathne B. Hawlader Ryan Phillips Dilan Robert One- and two-dimensional finite element modelling of thaw consolidation |
title | One- and two-dimensional finite element modelling of thaw consolidation |
title_full | One- and two-dimensional finite element modelling of thaw consolidation |
title_fullStr | One- and two-dimensional finite element modelling of thaw consolidation |
title_full_unstemmed | One- and two-dimensional finite element modelling of thaw consolidation |
title_short | One- and two-dimensional finite element modelling of thaw consolidation |
title_sort | one- and two-dimensional finite element modelling of thaw consolidation |
topic | Civil geotechnical engineering finite element modelling nonlinear thawed soil behaviour permafrost thaw consolidation warm pipeline |
topic_facet | Civil geotechnical engineering finite element modelling nonlinear thawed soil behaviour permafrost thaw consolidation warm pipeline |
url | https://figshare.com/articles/journal_contribution/One-_and_two-dimensional_finite_element_modelling_of_thaw_consolidation/27551553 |