Abstract
The rate of diffusion of Zn into Fe in solid Fe/Zn diffusion couples is found to be two to four orders of magnitude greater than would be predicted by lattice diffusion. The penetration depth varies markedly from sample to sample. It is achieved primarily in an initial transient, and then stops even though a steep concentration gradient persists in the ferrite. The maximum concentration of Zn in the ferrite surface layer often exceeds the published solubility of the first intermetallic phase, gamma, in ferrite. The initial Zn penetration seems to occur by DIGM. The mechanism for continued penetration is less clear. The variability in percent Zn in the ferrite, and possibly the variation in penetration depth, must stem from the delay in the nucleation of the most iron rich intermetallic phase, gamma.
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He was a Visiting Scholar at OSU at the time this work was done.
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Shewmon, P., Abbas, M. & Meyrick, G. Anomalously fast diffusion in the Fe-Zn System. Metall Trans A 17, 1523–1527 (1986). https://doi.org/10.1007/BF02650088
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DOI: https://doi.org/10.1007/BF02650088