Y-Fe-Al ternary system: partial isothermal section at 1070 K Powder X-ray diffraction and Mossbauer spectroscopy study

Citation
Jc. Waerenborgh et al., Y-Fe-Al ternary system: partial isothermal section at 1070 K Powder X-ray diffraction and Mossbauer spectroscopy study, J ALLOY COM, 323, 2001, pp. 78-82
Citations number
9
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science
Journal title
JOURNAL OF ALLOYS AND COMPOUNDS
ISSN journal
09258388 → ACNP
Volume
323
Year of publication
2001
Pages
78 - 82
Database
ISI
SICI code
0925-8388(20010712)323:<78:YTSPIS>2.0.ZU;2-H
Abstract
Phase equilibria were established in the Y-Fe-Al ternary system within the concentration region 50-100 at.% Al for an isothermal section at 1070 K by means of scanning electron microscopy and powder X-ray diffraction, Two ter nary aluminides were observed, YFexAl12-x (4 less than or equal tox less th an or equal to5.6) with the ThMn12-type structure, a = 8.6467(9)-8.7603(7) Angstrom, c = 5.0374(6)-5.0504(5) Angstrom and YFe2Al10, YbFe2Al10-type str ucrure, a = 8.9649(6) Angstrom, b = 10.1568(6) Angstrom, c = 9.0113(6) Angs trom. The only binary which forms a prolonged solid solution range is YAl2. The unit cell edge of the YFexAl2-x compounds, MgCu2-type structure, decre ases with Fe content from 7.834(9) Angstrom for x = 0 down to 7.689(4) Angs trom for x = 0.5. Fe-57 Mossbauer spectroscopy data of YFe2Al10 show an unu sually large isomer shift for Fe in Al-containing intermetallics and confir m that no magnetic ordering occurs down to 5 K. (C) 2001 Elsevier Science B .V. All rights reserved.