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The Initial Oxide Scale Development on a Model FeNiCrAl Alloy at 900 °C in Dry and Humid Atmosphere: A Detailed Investigation

机译:FeNiCrAl合金在干燥潮湿环境中在900°C时的初始氧化皮发展:详细研究

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摘要

The investigated alumina forming FeNiCrAl model alloy shows protective oxidation behavior in dry and humid environment at 900 °C. Hence, this type of alloy may replace conventional chromia forming austenitic alloys in aggressive oxidizing/reducing environments. A detailed investigation of the oxide scale development reveals a complex initial scale development. Firstly, at alloy grain boundaries, a thin AI rich oxide forms which is replaced by transient alumina platelets in dry and equiaxed α-Al_2O_3 crystallites in humid atmosphere. The scale at alloy grain centers develops via a layered scale of external chromia:Fe/Ni metal inclusions internal alumina to a layered external spinel: internal alumina scale in dry atmosphere. In humid condition an additional oxide feature appears on the center of large alloy grains i.e. thick oxide protrusions. Despite the initially different phase compositions a continuous protective α-Al_2O_3 scale forms both atmospheres.
机译:研究的氧化铝成型FeNiCrAl模型合金在900°C的干燥和潮湿环境中显示出保护性氧化行为。因此,这种类型的合金可以在侵蚀性氧化/还原环境中代替常规的形成氧化铬的奥氏体合金。对氧化物垢发展的详细研究揭示了复杂的初始垢发展。首先,在合金晶界处,会形成一层薄薄的富含AI的氧化物,在潮湿的大气中,在干燥和等轴的α-Al_2O_3微晶中,瞬态氧化铝片晶会代替它。合金晶粒中心的氧化皮是通过外部氧化铬:Fe / Ni金属夹杂物内部氧化铝的分层氧化皮发展为分层外部尖晶石:内部氧化铝在干燥气氛中的氧化皮。在潮湿条件下,在大合金晶粒的中心会出现一个附加的氧化物特征,即厚的氧化物突起。尽管最初的相组成不同,但连续的保护性α-Al_2O_3垢形成了两种气氛。

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