Stoichiometric icosahedral phase in the Zn–Mg–Y system View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

1997-06

AUTHORS

A. P. Tsai, A. Niikura, A. Inoue, T. Masumoto

ABSTRACT

Stoichiometric composition and formation process of the icosahedral phase in the Zn–Mg–Y system have been studied. The icosahedral phase exhibit a stoichiometric composition in the vicinity of Zn 60 Mg 30 Y 10 . During cooling, (Zn, Mg) 5 Y phase primarily crystallizes from the melt at ∼960 K and then undergoes a peritectic reaction with the residual Mg-enriched melt (∼820 K) to form the icosahedral phase. The melt with a constant composition close to Mg 7 Zn 3 is in equilibrium with the (Zn, Mg) 5 Y phase above the peritectic temperature in a wide compositional range. More... »

PAGES

1468-1471

References to SciGraph publications

Identifiers

URI

http://scigraph.springernature.com/pub.10.1557/jmr.1997.0202

DOI

http://dx.doi.org/10.1557/jmr.1997.0202

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1030298130


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