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- W2017039872 abstract "A number of intermetallic phases have been found in commercial pure aluminium, e.g. θ-Al13Fe4, Al6Fe, b.c.c. α-AlFeSi, AlmFe, q1-AlFeSi and q2-AlFeSi. Crystallographic orientation relationships between θ-Al13Fe4 and Al; b.c.c. α-AlFeSi and Al; q1-AlFeSi and b.c.c. α-AlFeSi; q1-AlFeSi and Al and q2-AlFeSi and b.c.c. α-AlFeSi were determined by electron diffraction. The orientation relationships are discussed in terms of lattice matching. The number of variants for each relationship was determined from group theory. The orientation relationships between θ-Al13Fe4 and Al are explained by the close matching of metal atoms on the interfacial surface between the two phases. Plusieurs phases intermétalliques ont été identifiées dans l'aluminium pur commercial, telles que Al13Fe4 θ, Al6Fe, AlFeSi α cubique centré, AlmFe, AlFeSi q1 et AlFeSi q2. Nous avons déterminé par diffraction électronique les relations d'orientation cristallographique entre Al13Fe4 θ et Al, entre AlFeSi α cubique centré et Al, entre AlFeSi q1 et AlFeSi α cubique centré, entre AlFeSi q1 et Al, et entre AlFeSi q2 et AlFeSi α cubique centré. Nous discutons ces relations en fonction du désaccord réticulaire, et nous déterminons le nombre de variantes pour chaque relation à partir de la théorie des groupes. Nous expliquons les relations d'orientation entre Al13Fe4 θ et Al à partir de la coïncidence parfaite des atomes métalliques à l'interface entre les deux phases. Mehrere intermetallische Phasen wurden in kommerziellem Reinaluminium aufgefunden: θ-Al13Fe4, Al6Fe, krz. α-AlFeSi, AlmFe, q1-AlFeSi und q2-AlFeSi. Mit Elektronenbeugung wurden die kristallografischen Orientierungsbeziehungen zwischen θ-Al13Fe4 und Al, krz. α-AlFeSi und Al, q1-AlFeSi und krz. α-AlFeSi, q1-AlFeSi und Al, q2-AlFeSi und krz. α-AlFeSi bestimmt. Die erhaltenen Beziehungen werden im Hinblick auf die Gitterpassung diskutiert. Die Anzahl der Varianten bei jeder Orientierungsbeziehung ergeben sich gruppentheoretisch. Die Orientierungsbeziehungen zwischen θ-Al13Fe4 und Al werden mit der genauen Passung der Metallatome an der Grenzfläche zwischen den beiden Phasen erklärt." @default.
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- W2017039872 date "1988-06-01" @default.
- W2017039872 modified "2023-10-14" @default.
- W2017039872 title "Crystallographic orientation relationships for Al-Fe and Al-Fe-Si precipitates in aluminium" @default.
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- W2017039872 doi "https://doi.org/10.1016/0001-6160(88)90215-5" @default.
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