Giant magnetostrictive material Terfenol-D (TbxDy1-xFe2-y, 0.27 less than o
r equal to x less than or equal to 0.30, 0.05 less than or equal to y less
than or equal to 0.1) was directionally solidified by vertical Bridgman met
hod within a sealed quartz crucible. Macrosegregation of RE elements along
the growth axis occurred in an abnormal way. RE elements concentration decr
eased significantly with increasing axial distance, which is different from
the typical macrosegregation with a distribution coefficient, ii, less tha
n unity. This was due to the compositional inhomogeneity of the initial mel
t. During the melting of the prealloyed ingot in the quartz crucible, eutec
tic RE-rich phase melted first and flowed out into the gap between the cruc
ible and the ingot. This RE-rich phase which flowed to the bottom did not m
ix well with the melt by convection because the temperature distribution in
the melt is quite stable and the density of the RE-rich phase is higher th
an that of the REFe2 phase. Macrosegregation was reduced very much in the r
od grown after the homogenization of the initial melt. Even though the magn
etostrictive strain was very different from part to part in the as-grown ro
d due to the macrosegregation, each specimen came to have a similar magneto
striction after the heat treatment above the eutectic temperature (890 degr
ees C). During the high-temperature annealing, excess RE-rich phase was obs
erved to be melted and flowed out from the specimen leaving pores between R
EFe2 matrices. Therefore, composition of the crystal approached to the stoi
chiometic value regardless of the initial composition. That makes magnetost
riction of the samples similar to one another. Melt extraction during the a
nnealing is thought to be the result of poor wetting between the two phases
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