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Precipitation in the iron--beryllium system

Journal Article · · Acta Met., v. 22, no. 2, pp. 201-217
Resu1ts are reported for an electron microscope study of precipitation in 12 and 18 at.% Be alloys. The reaction sequence is shown to be (at low temperatures): Spinodal decomposition- FeBe ordering of Be-rich regions - intermediate tetragonal precipitate in Be-rich regions - equilibrium FeBe/sub 2/. The spinodal reaction and ordering were separated by direct quenching experiments and the ordering process observed directly. Coarsening of the composition modulations followed a t1/2 law and gave an activation energy of 251 plus or minus 16 kJ/mole. The modulation solvus (spinodal) was found by these direct quenching experiments which also gave the ordering temperature. Direct quenching to temperatures above the spinodal caused nucleation of FeBe/sub 2/ which in turn led to the formation of intermediate precipitate in adjacent regions. This followed a nodular, branching mode until all regions had transformed. Further aging gave FeBe/sub 2. The solvas for the intermediate precipitate was found by direct quenching. The various precipitation regimes are summed up in a complete metastable phase diagram and the various products discussed in detail. (21 figres) (auth)
Research Organization:
Univ. of Manchester, Eng.
Sponsoring Organization:
USDOE
NSA Number:
NSA-29-013217
OSTI ID:
4364056
Journal Information:
Acta Met., v. 22, no. 2, pp. 201-217, Journal Name: Acta Met., v. 22, no. 2, pp. 201-217; ISSN AMETA
Country of Publication:
Country unknown/Code not available
Language:
English

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