Impurity diffusion, and the isotope effect, for Co in -Fe were studied by using a serial radio-frequency sputter-microsectioning method and the radioactive tracers, 57Co and 60Co, at temperatures ranging from 859 to 1173K (table 3). A larger effect of magnetic spin ordering upon Co diffusion, than upon self-diffusion, in -Fe was observed. In ferromagnetic -Fe, the Co diffusion coefficient was equal to about 50% of the self-diffusion coefficient. Above the Curie temperature, the Arrhenius plot for Co diffusion approached the linear Arrhenius line, for self-diffusion, with increasing temperature; as if the latter was the asymptote of the former. The increase in the isotope effect coefficient, due to magnetic spin ordering, for Co diffusion in -Fe was found to be larger than that for self-diffusion. It was suggested that the increase in the migration energy of a Co atom, due to magnetic spin ordering, in -Fe was larger than that in the case of self-diffusion.

Y.Iijima, K.Kimura, C.G.Lee, K.Hirano: Materials Transactions, 1993, 34[1], 20-6

Table 3

Diffusivity of Co in -Fe

 

Temperature (K)

Diffusivity, D57(m2/s)

1173

2.16 x 10-15

1160

1.74 x 10-15

1133

7.53 x 10-16

1093

2.02 x 10-16

1075

1.12 x 10-16

1053

4.46 x 10-17

1043

3.31 x 10-17

1030

1.33 x 10-17

1023

1.75 x 10-17

1012

7.22 x 10-18

993

2.12 x 10-18

973

8.94 x 10-19

963

5.41 x 10-19

934

1.22 x 10-19

914

4.07 x 10-20

873

5.10 x 10-21

859

2.57 x 10-21