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Multiscale Modeling of Grain-Boundary Fracture: Cohesive Zone Models Parameterized from Atomistic Simulations
Author(s) -
E. H. Glaessgen,
Erik Saether,
David H. Phillips,
V. Yamakov
Publication year - 2006
Publication title -
nasa technical reports server (nasa)
Language(s) - English
Resource type - Conference proceedings
DOI - 10.2514/6.2006-1674
Subject(s) - grain boundary , cohesive zone model , materials science , multiscale modeling , parameterized complexity , crystallite , fracture (geology) , molecular dynamics , deformation (meteorology) , constitutive equation , nanoscopic scale , mechanics , grain boundary strengthening , finite element method , boundary (topology) , composite material , metallurgy , thermodynamics , physics , nanotechnology , microstructure , computer science , mathematics , mathematical analysis , computational chemistry , chemistry , algorithm , quantum mechanics
A multiscale modeling strategy is developed to study grain boundary fracture in polycrystalline aluminum. Atomistic simulation is used to model fundamental nanoscale deformation and fracture mechanisms and to develop a constitutive relationship for separation along a grain boundary interface. The nanoscale constitutive relationship is then parameterized within a cohesive zone model to represent variations in grain boundary properties. These variations arise from the presence of vacancies, interstitials, and other defects in addition to deviations in grain boundary angle from the baseline configuration considered in the molecular-dynamics simulation. The parameterized cohesive zone models are then used to model grain boundaries within finite element analyses of aluminum polycrystals.

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