4.7 Article

Modeling peak-aged precipitate strengthening in Al-Mg-Si alloys

Journal

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.jmps.2021.104378

Keywords

Al-Mg-Si alloy; Peak aging; Precipitation strengthening; Orowan mechanism; Precipitate shear mechanism; Dislocation precipitate interaction; Discrete Dislocation Dynamics

Funding

  1. NCCR MARVEL - Swiss National Science Foundation

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Strengthening in Al-Mg-Si alloys by needle-shaped beta'' precipitates is crucial, with computational studies showing that Orowan looping only sets an upper bound for the CRSS even at peak aging. Further quantitative progress in understanding the strengthening mechanism requires detailed modeling of precipitate shearing.
Strengthening by needle-shaped beta'' precipitates is critical in Al-Mg-Si alloys. Here, the strengthening is studied computationally at the peak-aged condition where precipitate shearing and Orowan looping are usually considered to have equal strengths. Pseudo-random precipitate microstructures are constructed based on experimental precipitate dimensions and volume fractions at peak aging. A Discrete Dislocation Dynamics method is then adapted to compute the Critical Resolved Shear Stress (CRSS) for Orowan looping of dislocations moving through the non-shearable precipitate field. The CRSS for Orowan looping is determined by a typical in-situ precipitate spacing that is smaller than the average spacing and by the dislocation core energy within a radius of approximate to 5b, a factor rarely considered. The matrix misfit stresses, volume fraction, and precipitate shape have small effects on the CRSS. With microstructure and property details introduced as faithfully as possible, the CRSS for Orowan looping using atomistically-calibrated core energies at room temperature is nonetheless approximate to 33% higher than experiments. This suggests that precipitate shearing controls strength, and analyses of (i) forces acting on the precipitates, (ii) misfit stresses inside the precipitates, (iii) first-principles results for the relevant precipitate fault energies, and (iv) simulations that mimic precipitate shearing indicate a shearing CRSS closer to experiments. Thus, Orowan looping only sets an upper bound for the CRSS even at peak aging, and further quantitative progress requires detailed modeling of precipitate shearing.

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