Abstract

Early stages of the evolution of Al 2O 3 scales formed on a FeCrAlRE alloy (Kanthal AF) have been investigated by analytical TEM. The samples were oxidized isothermally at 900 °C in dry O 2 or O 2 + 40% H 2O for 1 h or 24 h. All oxide scales exhibited a two-layered structure, with a continuous inward growing α-Al 2O 3 inner layer and an outward growing outer layer. After 1 h, the outer oxide layer consisted of γ-Al 2O 3 in both environments. After 24 h exposure in dry O 2, the γ-Al 2O 3 in the outer oxide layer was partly transformed to α-Al 2O 3 and spinel oxide (Mg 1− x Fe x Al 2O 4). In contrast, the γ-Al 2O 3 in the outer layer was not transformed after 24 h in O 2 + 40% H 2O, showing that water vapour stabilizes γ-Al 2O 3. All oxide scales contained a Cr-rich band, a product of the initial oxidation. The inner α-Al 2O 3 layer is suggested to nucleate on Cr 2O 3 or Cr 2− x Fe x O 3 in the initial oxide.

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