Formation of I1 stacking fault by deformation defect evolution from grain boundaries in Mg

I1 stacking faults (SFs) in Mg alloys are regarded as the nucleation sites of 〈c+a〉 dislocations that are critical for these alloys to achieve high ductility. Previously it was proposed that the formation of I1 SFs requires the accumulations of a large number of vacancies, which are difficult to ach...

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Main Authors: Yong-Jie Hu, Vaidehi Menon, Liang Qi
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2022-10-01
Series:Journal of Magnesium and Alloys
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2213956722001591
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author Yong-Jie Hu
Vaidehi Menon
Liang Qi
author_facet Yong-Jie Hu
Vaidehi Menon
Liang Qi
author_sort Yong-Jie Hu
collection DOAJ
description I1 stacking faults (SFs) in Mg alloys are regarded as the nucleation sites of 〈c+a〉 dislocations that are critical for these alloys to achieve high ductility. Previously it was proposed that the formation of I1 SFs requires the accumulations of a large number of vacancies, which are difficult to achieve at low temperatures. In this study, molecular dynamics (MD) and molecular statics (MS) simulations based on empirical interatomic potentials were applied to investigate the deformation defect evolutions from the symmetric tilt grain boundaries (GBs) in Mg and Mg-Y alloys under external loading along 〈c〉-axis. The results show the planar faults (PFs) on Pyramidal I planes first appear due to the nucleation and glide of 〈12c+p〉 partial dislocations from GBs, where 〈p〉=13〈101¯0〉. These partial dislocations with pyramidal PFs interact with other defects, including pyramidal PFs themselves, GBs, and 〈p〉 partial dislocations, generating a large amount of I1 SFs. Detailed analyses show the nucleation and growth of I1 SFs are achieved by atomic shuffle events and deformation defect reactions without the requirements of vacancy diffusion. Our simulations also suggest the Y clusters at GBs can reduce the critical stress for the formation of pyramidal PFs and I1 SFs, which provide a possible reason for the experimental observations that Y promotes the 〈c+a〉 dislocation activities.
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spelling doaj.art-6a98d1613887470daf99836677a34e092022-12-22T04:38:49ZengKeAi Communications Co., Ltd.Journal of Magnesium and Alloys2213-95672022-10-01101027172729Formation of I1 stacking fault by deformation defect evolution from grain boundaries in MgYong-Jie Hu0Vaidehi Menon1Liang Qi2Department of Materials Science and Engineering, University of Michigan, Ann Arbor 48109, USA; Department of Materials Science and Engineering, Drexel University, Philadelphia 19104, USADepartment of Materials Science and Engineering, University of Michigan, Ann Arbor 48109, USACorresponding author.; Department of Materials Science and Engineering, University of Michigan, Ann Arbor 48109, USAI1 stacking faults (SFs) in Mg alloys are regarded as the nucleation sites of 〈c+a〉 dislocations that are critical for these alloys to achieve high ductility. Previously it was proposed that the formation of I1 SFs requires the accumulations of a large number of vacancies, which are difficult to achieve at low temperatures. In this study, molecular dynamics (MD) and molecular statics (MS) simulations based on empirical interatomic potentials were applied to investigate the deformation defect evolutions from the symmetric tilt grain boundaries (GBs) in Mg and Mg-Y alloys under external loading along 〈c〉-axis. The results show the planar faults (PFs) on Pyramidal I planes first appear due to the nucleation and glide of 〈12c+p〉 partial dislocations from GBs, where 〈p〉=13〈101¯0〉. These partial dislocations with pyramidal PFs interact with other defects, including pyramidal PFs themselves, GBs, and 〈p〉 partial dislocations, generating a large amount of I1 SFs. Detailed analyses show the nucleation and growth of I1 SFs are achieved by atomic shuffle events and deformation defect reactions without the requirements of vacancy diffusion. Our simulations also suggest the Y clusters at GBs can reduce the critical stress for the formation of pyramidal PFs and I1 SFs, which provide a possible reason for the experimental observations that Y promotes the 〈c+a〉 dislocation activities.http://www.sciencedirect.com/science/article/pii/S2213956722001591Magnesium alloysI1 stacking faults〈c+a〉 dislocationsGrain boundariesDefect nucleation and evolutionMolecular dynamics simulations
spellingShingle Yong-Jie Hu
Vaidehi Menon
Liang Qi
Formation of I1 stacking fault by deformation defect evolution from grain boundaries in Mg
Journal of Magnesium and Alloys
Magnesium alloys
I1 stacking faults
〈c+a〉 dislocations
Grain boundaries
Defect nucleation and evolution
Molecular dynamics simulations
title Formation of I1 stacking fault by deformation defect evolution from grain boundaries in Mg
title_full Formation of I1 stacking fault by deformation defect evolution from grain boundaries in Mg
title_fullStr Formation of I1 stacking fault by deformation defect evolution from grain boundaries in Mg
title_full_unstemmed Formation of I1 stacking fault by deformation defect evolution from grain boundaries in Mg
title_short Formation of I1 stacking fault by deformation defect evolution from grain boundaries in Mg
title_sort formation of i1 stacking fault by deformation defect evolution from grain boundaries in mg
topic Magnesium alloys
I1 stacking faults
〈c+a〉 dislocations
Grain boundaries
Defect nucleation and evolution
Molecular dynamics simulations
url http://www.sciencedirect.com/science/article/pii/S2213956722001591
work_keys_str_mv AT yongjiehu formationofi1stackingfaultbydeformationdefectevolutionfromgrainboundariesinmg
AT vaidehimenon formationofi1stackingfaultbydeformationdefectevolutionfromgrainboundariesinmg
AT liangqi formationofi1stackingfaultbydeformationdefectevolutionfromgrainboundariesinmg