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- W2067022461 abstract "In the present work, results obtained by differential thermal analysis (DTA) and X-ray diffraction (XRD) confirm [5, 8] that the icosahedral phase (i-phase) is formed by a peritectic reaction. A single i-phase can be obtained after annealing around the compositions Al64Cu24Fe12Al61.75Cu25.5Fe12.75. For the composition Al62Cu25.5Fe12.5, the XRD lines of the i-phase are narrow whatever the annealing temperature (800 °C or 600 °C). Thus, this result establishes that there exists a single phase domain where the i-phase is perfect (without phasons) and remains stable at 600 °C. A provisional vertical section along the line Al70Cu20Fe10Al64Cu24Fe12Al58CuPin28Fe14 is proposed and shows the phases that exist equilibrium at various temperatures in this range of compositions." @default.
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- W2067022461 date "1991-03-01" @default.
- W2067022461 modified "2023-10-14" @default.
- W2067022461 title "About the AlCuFe icosahedral phase formation" @default.
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- W2067022461 doi "https://doi.org/10.1016/0921-5093(91)90093-3" @default.
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