Formation condition of the icosahedral phase in rapidly quenched Ag-In-RE (rare earth) alloys
Formation of icosahedral (i) phases in rapidly quenched Ag-In-RE (rare earth) (RE = Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb) ternary alloys is investigated. It is found that the relative magnitude of the quasilattice constant is well explained by the atomic radius of the RE elements for Ag-In-RE allo...
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Published in | Philosophical magazine (2003. Print) Vol. 86; no. 3-5; pp. 435 - 441 |
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Main Authors | , , , |
Format | Journal Article Conference Proceeding |
Language | English |
Published |
Abingdon
Taylor & Francis Group
21.01.2006
Taylor and Francis |
Subjects | |
Online Access | Get full text |
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Summary: | Formation of icosahedral (i) phases in rapidly quenched Ag-In-RE (rare earth) (RE = Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb) ternary alloys is investigated. It is found that the relative magnitude of the quasilattice constant is well explained by the atomic radius of the RE elements for Ag-In-RE alloys with trivalent RE elements, and the formation of the i phase is governed by the atomic radius of the RE element. Moreover, the i phase is found to be formed in a wide composition range for the Ag/In atomic ratio but in a very narrow range for the RE concentration, which suggests that the RE concentration plays a crucial role in the formation, i.e. the stability, of the i phase rather than the average electrons-per-atom ratio. Furthermore, it is suggested that the structural change caused by the variation of the Ag/In concentration ratio in the i phase cannot be understood as a consequence of simple mutual replacement between Ag and In. |
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Bibliography: | ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 23 |
ISSN: | 1478-6435 1478-6443 |
DOI: | 10.1080/14786430500253984 |