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Initial stage of isothermal decomposition of austenite to ferrite and graphite in spheroidal graphite cast iron

机译:球墨铸铁中奥氏体等温分解为铁素体和石墨的初始阶段

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The isothermal decomposition of austenite to ferrite and graphite in a spheroidal graphite cast iron was investigated by dilatometry metallography, and image analysis. The results gave quantitative, although indirect, information on the kineticsof carbon transfer from austenite to graphite, as well as on the kinetics of the austenite to ferrite and graphite transformation. The relationship between the kinetics and the graphite nodule count was highlighted. The incubation period before ferritegrowth was found to be associated with a global contraction of the material, in spite of the related increase in the graphite volume fraction. Calculations showed good agreement with experimental results, except for the rate of carbon transfer which wasfound to be much slower experimentally than predicted by calculations based on the volume diffusion of carbon. Possible reasons for this discrepancy are discussed.
机译:通过膨胀金相学和图像分析研究了球墨铸铁中奥氏体的等温分解为铁素体和石墨。结果提供了关于碳从奥氏体到石墨的转移动力学以及奥氏体到铁素体和石墨相变动力学的定量信息,尽管是间接的。动力学和石墨结核计数之间的关系被突出。尽管石墨体积分数相应增加,但发现铁素体生长之前的潜伏期与材料的整体收缩有关。计算结果与实验结果吻合良好,只是碳的转移速率在实验上比基于碳的体积扩散的计算预测的要慢得多。讨论了这种差异的可能原因。

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