Dislocation pile-ups in Fe at high temperature

Dislocation 'pile-ups' occur in crystals when a number of similar dislocations, gliding in a common slip plane, are driven by an applied stress towards an obstacle that they cannot overcome. In contrast to dislocation walls, pile-ups give rise to a long-range stress field, and their proper...

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المؤلفون الرئيسيون: Fitzgerald, S, Dudarev, S
التنسيق: Journal article
اللغة:English
منشور في: 2008
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author Fitzgerald, S
Dudarev, S
author_facet Fitzgerald, S
Dudarev, S
author_sort Fitzgerald, S
collection OXFORD
description Dislocation 'pile-ups' occur in crystals when a number of similar dislocations, gliding in a common slip plane, are driven by an applied stress towards an obstacle that they cannot overcome. In contrast to dislocation walls, pile-ups give rise to a long-range stress field, and their properties strongly influence the plastic behaviour of the crystal as a whole. In this paper, we apply the analytic model of a pile-up (due to Eshelby, Frank and Nabarro) to a cubic crystal. Full anisotropic elasticity is used, and the model is extended to predict the plastic displacement generated by a dislocation source during the formation of a pile-up. The results are applied to Fe close to the temperature of the α-γ phase transition, where the inclusion of anisotropy leads to a strikingly different prediction from that of the isotropic approximation. © 2008 The Royal Society.
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spelling oxford-uuid:cf1f19d9-173f-43c3-a99d-c75d30f107cc2022-03-27T07:40:17ZDislocation pile-ups in Fe at high temperatureJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:cf1f19d9-173f-43c3-a99d-c75d30f107ccEnglishSymplectic Elements at Oxford2008Fitzgerald, SDudarev, SDislocation 'pile-ups' occur in crystals when a number of similar dislocations, gliding in a common slip plane, are driven by an applied stress towards an obstacle that they cannot overcome. In contrast to dislocation walls, pile-ups give rise to a long-range stress field, and their properties strongly influence the plastic behaviour of the crystal as a whole. In this paper, we apply the analytic model of a pile-up (due to Eshelby, Frank and Nabarro) to a cubic crystal. Full anisotropic elasticity is used, and the model is extended to predict the plastic displacement generated by a dislocation source during the formation of a pile-up. The results are applied to Fe close to the temperature of the α-γ phase transition, where the inclusion of anisotropy leads to a strikingly different prediction from that of the isotropic approximation. © 2008 The Royal Society.
spellingShingle Fitzgerald, S
Dudarev, S
Dislocation pile-ups in Fe at high temperature
title Dislocation pile-ups in Fe at high temperature
title_full Dislocation pile-ups in Fe at high temperature
title_fullStr Dislocation pile-ups in Fe at high temperature
title_full_unstemmed Dislocation pile-ups in Fe at high temperature
title_short Dislocation pile-ups in Fe at high temperature
title_sort dislocation pile ups in fe at high temperature
work_keys_str_mv AT fitzgeralds dislocationpileupsinfeathightemperature
AT dudarevs dislocationpileupsinfeathightemperature