超纯铁素体不锈钢的高温氧化行为和氧化层形貌演变模拟研究

    Simulation on High Temperature Oxidation Behavior and Oxidation Layer Morphology Evolution for High-purity Ferritic Stainless Steel

    • 摘要: 耦合Cr2O3金属氧化物形核与长大热力学、动力学以及元胞自动机模型,建立了描述较大尺度下超纯铁素体不锈钢高温氧化层形貌演变过程的数值模型,与文献的实验结果对比,验证了本模型的合理性与准确性。采用该模型模拟了超纯Fe-Cr不锈钢的高温氧化行为及氧化层形貌演变过程,研究了Cr含量对超纯Fe-Cr合金高温氧化动力学行为的影响。结果表明,不锈钢高温氧化层稳定增厚前由3个阶段组成,即金属氧化物初始形核阶段、氧化物粒子快速长大与元素扩散相互竞争阶段、表面致密氧化层的缓慢形成阶段,最终形成的超纯Fe-Cr不锈钢表面高温氧化层致密度与厚度沿纵向呈现严重的不均匀性。当Cr含量<29.0wt%时,界面前沿氧化物长大速度随氧化时间的增加逐渐增大并最终保持稳定;当Cr含量≥29.0wt%时,界面前沿氧化物长大速度随氧化时间的增加先达到最大值,之后逐渐减小最终达到稳定值。

       

      Abstract: A numerical model for morphological evolution of high-temperature oxide scales of high-purity ferritic stainless steel at large scales was developed by coupling nucleation and growth thermodynamics-kinetics of Cr2O3 and cellular automaton model. The rationality and accuracy of the proposed model were verified by comparison with experimental results reported in literatures. The microstructure evolution and dynamics behaviors of high-temperature oxidation for high-purity Fe-Cr alloys were simulated by using the model, the effect of Cr content on the high-temperature oxidation kinetics of the high-purity Fe-Cr alloys was investigated. It demonstrates that the high-temperature oxidation process can be divided into three stages before the stable growth of oxide layer, including the initial nucleation stage of metal oxides, the stage of competition between rapid growth of oxide particles and elemental diffusion and the stage of slow formation of dense oxide layers. Finally, the density and thickness of the high-temperature oxide layer formed on the surface of the stainless steel exhibit a severe inhomogeneous distribution along the longitudinal direction. When the Cr content is lower than 29.0 wt%, the growth rate of the interface front of oxides increases gradually with the increase of time and remains stable eventually. When the Cr content is higher than 29.0 wt%, the growth rate of the interface front of oxides firstly reaches its maximum with the increase of time, then decreases gradually and levels off finally.

       

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