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Original Articles

Influence of the oxidation environment on scale morphology and oxidation rate of Fe–22Cr

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Pages 223-229 | Published online: 02 Jan 2014
 

Abstract

The oxidation behaviour of a commercial Fe–Cr alloy with 22 wt% Cr was investigated at 1173K in Ar–9 H2 with 1% H2O (pO2 = 9.8 × 10−19), in air with 1% H2O (pO2 = 0.208), and in a combination of the two atmospheres. The oxide morphology was investigated with X-ray diffraction and scanning electron microscopy. The oxide layer consisted of MnCr2O4 on top of Cr2O3.

Small oxide whiskers were present at the surface after oxidation in Ar–9 H2 with 1% H2O but not after oxidation in air with 1% H2O. For samples initially oxidised in air with 1% H2O, the oxide/alloy interface was wrinkled and covered with a SiO2 layer. SiO2 particles had developed at a rather flat oxide/alloy interface for samples initially oxidised in Ar–9% H2 with 1% H2O. The results obtained can be explained assuming that oxide growth occurs by cation diffusion only in Ar–9 H2 with 1% H2O, whereas both cation and anion diffusion contribute to the growth in air/H2O.

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