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Quantitative study of the effect of grain boundary parameters on the slip system level Hall-Petch slope for basal slip system in Mg-4A1

ACTA MATERIALIA(2020)

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Abstract
Several theoretical studies have reported that the geometry and structure of grain boundaries in polycrystalline materials could impose a significant effect on the Hall-Petch slope. However, experimental observations are primarily limited by the ability of the techniques to accurately quantify the grain boundary strength and validate these theoretical models. Using high-resolution electron backscatter diffraction (HR-EBSD), the local stress tensor ahead of a slip band blocked by a grain boundary was quantified and coupled with a continuum dislocation pile-up model to assess the barrier strength of specific grain boundaries to specific slip systems, referred to as micro-Hall-Petch coefficient. For basal slip system in a deformed Mg-4A1 alloy, the micro-Hall-Petch coefficient (k basal mu) varied significantly, from 0.054 to 0.184 MPa - m(1/2) for nine different grain boundaries. These results were correlated with geometric descriptors of the respective grain boundaries, with three-dimensional GB profile additionally measured via focused ion beam milling. It was found that the angle between the two slip plane traces on the grain boundary plane was the most sensitive parameter affecting kbifsal, followed by the angle between the slip directions. A functional form for calculation of kbifsal depending on these two angles is proposed to augment crystal plasticity constitutive models with slip resistance dependent on some measure of the grain size. The method allows a new pathway to calibrate grain size strengthening parameters in crystal plasticity models, allowing further computational investigations of the interrelationship between texture, grain morphology, and the Hall Petch effect. (C) 2020 Acta Materialia Inc. Published by Elsevier Ltd. All rights reserved.
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Key words
Mg alloy,Electron backscattering diffraction (EBSD),Micro-hall-petch coefficient,Grain Boundary,Crystal Plasticity
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