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

材料科学 电子背散射衍射 晶界强化 晶界 打滑(空气动力学) 凝聚态物理 粒度 微晶 晶体塑性 位错 可塑性 复合材料 几何学 结晶学 冶金 微观结构 热力学 物理 数学 化学
作者
Mohsen Taheri Andani,Aaditya Lakshmanan,Veera Sundararaghavan,J. Allison,Amit Misra
出处
期刊:Acta Materialia [Elsevier]
卷期号:200: 148-161 被引量:42
标识
DOI:10.1016/j.actamat.2020.08.079
摘要

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-4Al alloy, the micro-Hall-Petch coefficient (kμbasal)varied significantly, from 0.054 to 0.184 MPa−m1/2for 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 kμbasal, followed by the angle between the slip directions. A functional form for calculation of kμbasaldepending 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.
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