Non-basal dislocations should be accounted for in simulating ice mass flow

Prediction of ice mass flow and associated dynamics is pivotal at a time of climate change. Ice flow is dominantly accommodated by the motion of crystal defects – the dislocations. In the specific case of ice, their observation is not always accessible by means of the classical tools such as X-ray d...

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Main Authors: Chauve, T, Montagnat, M, Piazolo, S, Journaux, B, Wheeler, J, Barou, F, Mainprice, D, Tommasi, A
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:http://livrepository.liverpool.ac.uk/3008474/
http://livrepository.liverpool.ac.uk/3008474/1/WBV_ChauveEtAl_asPublished_Perso.pdf
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spelling ftunivliverpool:oai:livrepository.liverpool.ac.uk:3008474 2023-05-15T16:41:01+02:00 Non-basal dislocations should be accounted for in simulating ice mass flow Chauve, T Montagnat, M Piazolo, S Journaux, B Wheeler, J Barou, F Mainprice, D Tommasi, A 2017-09-01 text http://livrepository.liverpool.ac.uk/3008474/ http://livrepository.liverpool.ac.uk/3008474/1/WBV_ChauveEtAl_asPublished_Perso.pdf en eng http://livrepository.liverpool.ac.uk/3008474/1/WBV_ChauveEtAl_asPublished_Perso.pdf Chauve, T, Montagnat, M, Piazolo, S, Journaux, B, Wheeler, J orcid:0000-0002-7576-4465 , Barou, F, Mainprice, D and Tommasi, A (2017) Non-basal dislocations should be accounted for in simulating ice mass flow. Earth and Planetary Science Letters, 473. 247 - 255. Article NonPeerReviewed 2017 ftunivliverpool 2022-04-25T09:04:47Z Prediction of ice mass flow and associated dynamics is pivotal at a time of climate change. Ice flow is dominantly accommodated by the motion of crystal defects – the dislocations. In the specific case of ice, their observation is not always accessible by means of the classical tools such as X-ray diffraction or transmission electron microscopy (TEM). Part of the dislocation population, the geometrically necessary dislocations (GNDs) can nevertheless be constrained using crystal orientation measurements via electron backscattering diffraction (EBSD) associated with appropriate analyses based on the Nye (1950) approach. The present study uses the Weighted Burgers Vectors, a reduced formulation of the Nye theory that enables the characterization of GNDs. Applied to ice, this method documents, for the first time, the presence of dislocations with non-basal or Burgers vectors. These or dislocations represent up to of the GNDs observed in laboratory-deformed ice samples. Our findings offer a more complex and comprehensive picture of the key plasticity processes responsible for polycrystalline ice creep and provide better constraints on the constitutive mechanical laws implemented in ice sheet flow models used to predict the response of Earth ice masses to climate change. Article in Journal/Newspaper Ice Sheet The University of Liverpool Repository
institution Open Polar
collection The University of Liverpool Repository
op_collection_id ftunivliverpool
language English
description Prediction of ice mass flow and associated dynamics is pivotal at a time of climate change. Ice flow is dominantly accommodated by the motion of crystal defects – the dislocations. In the specific case of ice, their observation is not always accessible by means of the classical tools such as X-ray diffraction or transmission electron microscopy (TEM). Part of the dislocation population, the geometrically necessary dislocations (GNDs) can nevertheless be constrained using crystal orientation measurements via electron backscattering diffraction (EBSD) associated with appropriate analyses based on the Nye (1950) approach. The present study uses the Weighted Burgers Vectors, a reduced formulation of the Nye theory that enables the characterization of GNDs. Applied to ice, this method documents, for the first time, the presence of dislocations with non-basal or Burgers vectors. These or dislocations represent up to of the GNDs observed in laboratory-deformed ice samples. Our findings offer a more complex and comprehensive picture of the key plasticity processes responsible for polycrystalline ice creep and provide better constraints on the constitutive mechanical laws implemented in ice sheet flow models used to predict the response of Earth ice masses to climate change.
format Article in Journal/Newspaper
author Chauve, T
Montagnat, M
Piazolo, S
Journaux, B
Wheeler, J
Barou, F
Mainprice, D
Tommasi, A
spellingShingle Chauve, T
Montagnat, M
Piazolo, S
Journaux, B
Wheeler, J
Barou, F
Mainprice, D
Tommasi, A
Non-basal dislocations should be accounted for in simulating ice mass flow
author_facet Chauve, T
Montagnat, M
Piazolo, S
Journaux, B
Wheeler, J
Barou, F
Mainprice, D
Tommasi, A
author_sort Chauve, T
title Non-basal dislocations should be accounted for in simulating ice mass flow
title_short Non-basal dislocations should be accounted for in simulating ice mass flow
title_full Non-basal dislocations should be accounted for in simulating ice mass flow
title_fullStr Non-basal dislocations should be accounted for in simulating ice mass flow
title_full_unstemmed Non-basal dislocations should be accounted for in simulating ice mass flow
title_sort non-basal dislocations should be accounted for in simulating ice mass flow
publishDate 2017
url http://livrepository.liverpool.ac.uk/3008474/
http://livrepository.liverpool.ac.uk/3008474/1/WBV_ChauveEtAl_asPublished_Perso.pdf
genre Ice Sheet
genre_facet Ice Sheet
op_relation http://livrepository.liverpool.ac.uk/3008474/1/WBV_ChauveEtAl_asPublished_Perso.pdf
Chauve, T, Montagnat, M, Piazolo, S, Journaux, B, Wheeler, J orcid:0000-0002-7576-4465 , Barou, F, Mainprice, D and Tommasi, A (2017) Non-basal dislocations should be accounted for in simulating ice mass flow. Earth and Planetary Science Letters, 473. 247 - 255.
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