1982 Volume 51 Issue 8 Pages 2487-2492
The Mössbauer effect of 57Fe in amorphous and crystalline YFe2 was measured from 77 K to 700 K. The average value of the quadrupole splitting in amorphous YFe2 below 400 K is nearly equal to the extrapolated value from the paramagnetic state of crystalline YFe2. The temperature dependence of absorption intensity follows the Debye model in amorphous YFe2. The ratio of the Debye temperature in amorphous state to crystalline state is 0.80±0.05 for YFe2. The isomer shift in amorphous state is smaller than that in crystalline state and increases with increasing temperature up to the value of the crystalline state.
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