Abstract
The precipitation of Au-rich precipitates on the external surfaces of Fe-Au alloys has been studied by scanning and transmission electron microscopy. The surface precipitates formed at elevated temperatures are found to self-organize in regular patterns and their growth rate is determined quantitatively. The observed surface precipitation at a free surface is compared to the precipitation at the internal surface of grain boundary cavities induced by creep loading. A close agreement between both processes is observed.
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Sun, W.W., Fang, H., van Dijk, N.H. et al. Linking Surface Precipitation in Fe-Au Alloys to Its Self-healing Potential During Creep Loading. Metall Mater Trans A 48, 2109–2114 (2017). https://doi.org/10.1007/s11661-017-4025-x
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DOI: https://doi.org/10.1007/s11661-017-4025-x