Abstract
The effect of grain boundaries on the formation of oxide scale was investigated for two different Fe-Cr alloys at 1073 K in H2-H2O atmosphere: typical stainless steel (SUS430) and Laves-phase forming Fe-Cr alloy. Identified oxide scale phases were Cr-Mn-(Fe) spinel and Cr2O3 on both surfaces of the Fe-Cr alloys. A relatively fast diffusion of elements was observed at the grain boundaries of SUS430 with a formation of ridges on the oxide scale surface. On the other hand, the diffusion of elements was controlled by precipitating a Laves-phase (Fe2(Nb, Mo) phase) at the alloy grain boundaries in the Laves-phase forming alloy. The oxide scale growth rates of the Laves-phase forming alloy was 9.8 × 10- 15 cm2 s- 1, which was much smaller than that of SUS430 (4.5 × 10- 14 cm2 s- 1) in the same condition. This was due to the lower diffusivity of elements at the grain boundaries of alloy. The control of elemental diffusivity at the alloy grain boundary (Laves-phase forming alloy) is effective to form stable and thin oxide scales on the Fe-Cr alloy surface in H2-H2O.
| Original language | English |
|---|---|
| Pages (from-to) | 1320-1324 |
| Number of pages | 5 |
| Journal | Solid State Ionics |
| Volume | 179 |
| Issue number | 27-32 |
| DOIs | |
| State | Published - 30 Sep 2008 |
| Externally published | Yes |
Keywords
- Fe-Cr alloy
- Grain boundary
- Interconnect
- Oxide scale
- Solid oxide fuel cells (SOFCs)
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