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...

Full description

Bibliographic Details
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: Elsevier 2017
Subjects:
Online Access:https://eprints.whiterose.ac.uk/118692/
https://eprints.whiterose.ac.uk/118692/1/WBV_ChauveEtAl_asPublished_Perso.pdf
id ftleedsuniv:oai:eprints.whiterose.ac.uk:118692
record_format openpolar
spelling ftleedsuniv:oai:eprints.whiterose.ac.uk:118692 2023-05-15T16:41:03+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 https://eprints.whiterose.ac.uk/118692/ https://eprints.whiterose.ac.uk/118692/1/WBV_ChauveEtAl_asPublished_Perso.pdf en eng Elsevier https://eprints.whiterose.ac.uk/118692/1/WBV_ChauveEtAl_asPublished_Perso.pdf Chauve, T, Montagnat, M, Piazolo, S orcid.org/0000-0001-7723-8170 et al. (5 more authors) (2017) Non-basal dislocations should be accounted for in simulating ice mass flow. Earth and Planetary Science Letters, 473. pp. 247-255. ISSN 0012-821X Article NonPeerReviewed 2017 ftleedsuniv 2023-01-30T21:56:45Z 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 [c][c] or 〈c+a〉〈c+a〉 Burgers vectors. These [c][c] or 〈c+a〉〈c+a〉 dislocations represent up to 35% 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 White Rose Research Online (Universities of Leeds, Sheffield & York)
institution Open Polar
collection White Rose Research Online (Universities of Leeds, Sheffield & York)
op_collection_id ftleedsuniv
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 [c][c] or 〈c+a〉〈c+a〉 Burgers vectors. These [c][c] or 〈c+a〉〈c+a〉 dislocations represent up to 35% 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
publisher Elsevier
publishDate 2017
url https://eprints.whiterose.ac.uk/118692/
https://eprints.whiterose.ac.uk/118692/1/WBV_ChauveEtAl_asPublished_Perso.pdf
genre Ice Sheet
genre_facet Ice Sheet
op_relation https://eprints.whiterose.ac.uk/118692/1/WBV_ChauveEtAl_asPublished_Perso.pdf
Chauve, T, Montagnat, M, Piazolo, S orcid.org/0000-0001-7723-8170 et al. (5 more authors) (2017) Non-basal dislocations should be accounted for in simulating ice mass flow. Earth and Planetary Science Letters, 473. pp. 247-255. ISSN 0012-821X
_version_ 1766031483908128768