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Stefan Zaefferer

Researcher at Max Planck Society

Publications -  186
Citations -  9821

Stefan Zaefferer is an academic researcher from Max Planck Society. The author has contributed to research in topics: Electron backscatter diffraction & Grain boundary. The author has an hindex of 43, co-authored 174 publications receiving 8021 citations.

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On the role of non-basal deformation mechanisms for the ductility of Mg and Mg–Y alloys

TL;DR: In this paper, the authors focused on understanding the mechanisms for ductility improvement by microstructure analysis, texture analysis and slip trace analysis based on electron backscatter diffraction and transmission electron microscopy.
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The effect of grain size and grain orientation on deformation twinning in a Fe-22 wt.% Mn-0.6 wt.% C TWIP steel

TL;DR: In this article, the effect of grain size and grain orientation on deformation twinning in a Fe-22-wt.% Mn-0.6-c TWIP steel was investigated.
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The relation between ductility and stacking fault energies in Mg and Mg–Y alloys

TL;DR: In this article, the intrinsic stacking fault I1 energy (I1 SFE) was investigated by transmission electron microscopy and density functional theory, and the influence of the SFE on the relative activation of different competing deformation mechanisms (basal, prismatic, pyramidal slip) was discussed.
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Micromechanical and macromechanical effects in grain scale polycrystal plasticity experimentation and simulation

TL;DR: In this article, a polycrystalline aluminum sample with a quasi-2D single layer of coarse grains is plastically deformed in a channel die plane strain set-up at ambient temperature and low strain rate.
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A study of microstructure, transformation mechanisms and correlation between microstructure and mechanical properties of a low alloyed TRIP steel

TL;DR: In this article, differently heat treated samples of a low alloyed TRIP steel have been investigated using electron diffraction techniques in SEM and TEM, and the results showed that the mechanical properties of these samples are most strongly influenced by the amount and distribution of carbon in the retained austenite and by the degree of recovery in bainite and martensite.