Interaction of a dislocation pileup with {332} tilt grain boundary in bcc metals studied by MD simulations

The sustainability and capacity of macroscopic deformation by polycrystalline metals and metallic alloys is controlled by the propagation of dislocation-mediated slip through grains. In this paper, the interaction of a pileup of 1/2¿111¿ dislocations with the {332} tilt grain boundary (GB) is studie...

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Detalles Bibliográficos
Autores: Kvashin, Nikolai|||0000-0002-6924-0083, Anento Moreno, Napoleón|||0000-0002-4643-7270, Terentyev, Dimitry, Bakaev, A., Serra Tort, Ana María|||0000-0002-8754-5649
Tipo de recurso: artículo
Fecha de publicación:2021
País:España
Institución:Universitat Politècnica de Catalunya (UPC)
Repositorio:UPCommons. Portal del coneixement obert de la UPC
Idioma:inglés
OAI Identifier:oai:upcommons.upc.edu:2117/346611
Acceso en línea:https://hdl.handle.net/2117/346611
https://dx.doi.org/10.1103/PhysRevMaterials.5.013605
Access Level:acceso abierto
Palabra clave:Metals--Plastic properties--Mathematical models
Molecular dynamics
Grain boundary
Dislocation pileup
Disconnection
Plastic deformation
Metalls -- Propietats plàstiques
Àrees temàtiques de la UPC::Enginyeria dels materials::Materials compostos
Àrees temàtiques de la UPC::Enginyeria dels materials::Metal·lúrgia
Descripción
Sumario:The sustainability and capacity of macroscopic deformation by polycrystalline metals and metallic alloys is controlled by the propagation of dislocation-mediated slip through grains. In this paper, the interaction of a pileup of 1/2¿111¿ dislocations with the {332} tilt grain boundary (GB) is studied as a function of temperature in three bcc metals: iron (Fe), chromium (Cr), and tungsten (W). The interaction results in the transformation of the crystal dislocation into GB dislocations. The {332} tilt GB absorbs the crystal dislocations of the pileup, neither the transmission nor reflection of dislocations was observed. The reaction product at the GB is determined by the crystallography of the GB and the features of the crystal dislocations involved, specifically, the orientation of the Burgers vector and the glide plane of the dislocation. In general, the decomposition results in the formation of a sessile GB dislocation with a riser that facets the GB and several elementary disconnections that glide away. In some cases, the riser increases its length with the number of dislocations absorbed and a new asymmetrical grain boundary of {112}/{110} type is created. For a given external shear stress, the number of dislocations absorbed depends on the orientation of the Burgers vector, glide plane of the pileup, and material.