Grain-boundary grooving methods were used to study the diffusion of Ag at 973 to 1073K. The results could be described by:
D (m2/s) = 2.49 x 10-1 exp[-166(kJ/mol)/RT]
at an O partial pressure of 10-11Pa, and by:
D (m2/s) = 1.71 x 10-3 exp[-106(kJ/mol)/RT]
at an O partial pressure of 105Pa.
K.Yoshihara, K.Nii: Transactions of the Japan Institute of Metals, 1979, 20[9], 533-42
Table 3
Volume Diffusivity of 110mAg in Ag Polycrystals
Temperature (K) | D (m2/s) |
911 | 7.56 x 10-16 |
776 | 1.53 x 10-17 |
751 | 6.43 x 10-18 |
723 | 2.23 x 10-18 |
701 | 9.18 x 10-19 |
672 | 2.60 x 10-19 |
622 | 2.27 x 10-20 |
565 | 8.29 x 10-22 |
564 | 7.78 x 10-22 |
560 | 6.00 x 10-22 |
554 | 4.05 x 10-22 |
544 | 2.06 x 10-22 |
537 | 1.26 x 10-22 |
497 | 5.91 x 10-24 |
478 | 1.19 x 10-24 |
452 | 9.43 x 10-26 |
424 | 5.03 x 10-27 |
423 | 4.64 x 10-27 |
394 | 1.29 x 10-28 |