Formation Mechanism for the Orientation Relationship between {110}〈001〉 and {111}〈112〉 Grains during Twinning in Fe-3 Pct Si Alloy

Formation Mechanism for the Orientation Relationship between {110}〈001〉 and {111}〈112〉 Grains during Twinning in Fe-3 Pct Si Alloy

A hypothesis is advanced about the origin of areas having close to Goss orientation as a result of secondary twinning in the Fe-3 pct Si alloy. This hypothesis does not contradict available experimental data for single and polycrystals of the Fe-3 pct Si alloy .

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Veröffentlicht in:Metallurgical and materials transactions. A, Physical metallurgy and materials science Physical metallurgy and materials science, 2008-10, Vol.39 (10), p.2278-2280
Hauptverfasser: Rusakov, G.M., Redikultsev, A.A., Lobanov, M.L.
Format: Artikel
Sprache:eng
Schlagworte:
Characterization and Evaluation of Materials
Chemistry and Materials Science
Communication
Materials Science
Metallic Materials
Nanotechnology
Structural Materials
Surfaces and Interfaces
Thin Films
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Zusammenfassung:A hypothesis is advanced about the origin of areas having close to Goss orientation as a result of secondary twinning in the Fe-3 pct Si alloy. This hypothesis does not contradict available experimental data for single and polycrystals of the Fe-3 pct Si alloy .
ISSN:1073-5623
1543-1940
DOI:10.1007/s11661-008-9575-5