A generalized stress correction scheme for the Maxwell elasto-brittle rheology: impact on the fracture angles and deformations

The Maxwell elasto-brittle (MEB) rheology uses a damage parameterization to represent the brittle fracture of sea ice without involving plastic laws to constrain the sea ice deformations. The conventional MEB damage parameterization is based on a correction of super-critical stresses that binds the...

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Published in:The Cryosphere
Main Authors: Plante, Mathieu, Tremblay, L. Bruno
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/tc-15-5623-2021
https://tc.copernicus.org/articles/15/5623/2021/
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spelling ftcopernicus:oai:publications.copernicus.org:tc91608 2023-05-15T15:16:36+02:00 A generalized stress correction scheme for the Maxwell elasto-brittle rheology: impact on the fracture angles and deformations Plante, Mathieu Tremblay, L. Bruno 2021-12-10 application/pdf https://doi.org/10.5194/tc-15-5623-2021 https://tc.copernicus.org/articles/15/5623/2021/ eng eng doi:10.5194/tc-15-5623-2021 https://tc.copernicus.org/articles/15/5623/2021/ eISSN: 1994-0424 Text 2021 ftcopernicus https://doi.org/10.5194/tc-15-5623-2021 2021-12-13T17:22:30Z The Maxwell elasto-brittle (MEB) rheology uses a damage parameterization to represent the brittle fracture of sea ice without involving plastic laws to constrain the sea ice deformations. The conventional MEB damage parameterization is based on a correction of super-critical stresses that binds the simulated stress to the yield criterion but leads to a growth of errors in the stress field. A generalized damage parameterization is developed to reduce this error growth and to investigate the influence of the super-critical stress correction scheme on the simulated sea ice fractures, deformations and orientation of linear kinematic features (LKFs). A decohesive stress tensor is used to correct the super-critical stresses towards different points on the yield curve. The sensitivity of the simulated sea ice fractures and deformations to the decohesive stress tensor is investigated in uniaxial compression experiments. Results show that the decohesive stress tensor influences the growth of residual errors associated with the correction of super-critical stresses, the orientation of the lines of fracture and the short-term deformation associated with the damage, but it does not influence the long-term post-fracture sea ice deformations. We show that when ice fractures, divergence first occurs while the elastic response is dominant, and convergence develops post-fracture in the long term when the viscous response dominates – contrary to laboratory experiments of granular flow and satellite imagery in the Arctic. The post-fracture deformations are shown to be dissociated from the fracture process itself, an important difference with classical viscous plastic (VP) models in which large deformations are governed by associative plastic laws. Using the generalized damage parameterization together with a stress correction path normal to the yield curve reduces the growth of errors sufficiently for the production of longer-term simulations, with the added benefit of bringing the simulated LKF intersection half-angles closer to observations (from 40–50 to 35–45 ∘ , compared to 15–25 ∘ in observations). Text Arctic Sea ice Copernicus Publications: E-Journals Arctic The Cryosphere 15 12 5623 5638
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The Maxwell elasto-brittle (MEB) rheology uses a damage parameterization to represent the brittle fracture of sea ice without involving plastic laws to constrain the sea ice deformations. The conventional MEB damage parameterization is based on a correction of super-critical stresses that binds the simulated stress to the yield criterion but leads to a growth of errors in the stress field. A generalized damage parameterization is developed to reduce this error growth and to investigate the influence of the super-critical stress correction scheme on the simulated sea ice fractures, deformations and orientation of linear kinematic features (LKFs). A decohesive stress tensor is used to correct the super-critical stresses towards different points on the yield curve. The sensitivity of the simulated sea ice fractures and deformations to the decohesive stress tensor is investigated in uniaxial compression experiments. Results show that the decohesive stress tensor influences the growth of residual errors associated with the correction of super-critical stresses, the orientation of the lines of fracture and the short-term deformation associated with the damage, but it does not influence the long-term post-fracture sea ice deformations. We show that when ice fractures, divergence first occurs while the elastic response is dominant, and convergence develops post-fracture in the long term when the viscous response dominates – contrary to laboratory experiments of granular flow and satellite imagery in the Arctic. The post-fracture deformations are shown to be dissociated from the fracture process itself, an important difference with classical viscous plastic (VP) models in which large deformations are governed by associative plastic laws. Using the generalized damage parameterization together with a stress correction path normal to the yield curve reduces the growth of errors sufficiently for the production of longer-term simulations, with the added benefit of bringing the simulated LKF intersection half-angles closer to observations (from 40–50 to 35–45 ∘ , compared to 15–25 ∘ in observations).
format Text
author Plante, Mathieu
Tremblay, L. Bruno
spellingShingle Plante, Mathieu
Tremblay, L. Bruno
A generalized stress correction scheme for the Maxwell elasto-brittle rheology: impact on the fracture angles and deformations
author_facet Plante, Mathieu
Tremblay, L. Bruno
author_sort Plante, Mathieu
title A generalized stress correction scheme for the Maxwell elasto-brittle rheology: impact on the fracture angles and deformations
title_short A generalized stress correction scheme for the Maxwell elasto-brittle rheology: impact on the fracture angles and deformations
title_full A generalized stress correction scheme for the Maxwell elasto-brittle rheology: impact on the fracture angles and deformations
title_fullStr A generalized stress correction scheme for the Maxwell elasto-brittle rheology: impact on the fracture angles and deformations
title_full_unstemmed A generalized stress correction scheme for the Maxwell elasto-brittle rheology: impact on the fracture angles and deformations
title_sort generalized stress correction scheme for the maxwell elasto-brittle rheology: impact on the fracture angles and deformations
publishDate 2021
url https://doi.org/10.5194/tc-15-5623-2021
https://tc.copernicus.org/articles/15/5623/2021/
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-15-5623-2021
https://tc.copernicus.org/articles/15/5623/2021/
op_doi https://doi.org/10.5194/tc-15-5623-2021
container_title The Cryosphere
container_volume 15
container_issue 12
container_start_page 5623
op_container_end_page 5638
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