Abstract

The base oxide scales on a commercial FeCrAl alloy oxidized isothermally at 900°C in dry O2 or O2 with 40% H2O were studied in detail using analytical electron microscopy. Electron transparent cross-section foils prepared with a FIB/SEM in-situ lift-out technique were investigated using STEM/EDX and CBED. The oxide scales on the samples exposed to dry O2 are slightly thinner than the scales formed in O2+H2O. The oxide scales exhibit a multilayered structure, with a Cr-rich layer in the middle, indicating the original metal/gas interface. An almost pure inner α-Al2O3 layer, containing columnar grains, was formed by inward oxygen diffusion, after exposures in both the dry and wet atmospheres. The outer oxide layer consisted of γ-Al2O3 in the wet case and of α-Al2O3/MgAl2O4 in the dry case. It is suggested that the α-Al2O3/MgAl2O4 phases resulted from a phase transformation of initially grown γ-Al2O3. The observations indicate that water vapour may stabilize the γ-Al2O3 phase.

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