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The Formation of Abnormal Ferrite in Hypereutectoid Steels Revisitedand Its Analogy to the Formation of Austenite and Ferrite ShellsAround Graphite in Cast Irons

机译:过度切开钢中异常铁素体的形成重新探测其对铸铁奥氏体和铁氧体壳星石墨的形成

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Abnormal ferrite, defined by large regions of ferrite covering coarse cementite, has been reported in hyper-eutectoid plain carbon, carburised and alloy steels. The early studies suggested that this abnormal ferrite might be a result of the coarsening of pearlite. A more radical view, expressed by Hillert in 1962, was that abnormal ferrite formed by nucleation and growth from cementite. In 2000, we reported further microstructural evidence for the occurrence of abnormal ferrite in hyper-eutectoid carbon steels and proposed an explanation based upon carbon redistribution accommodating concurrent growth of both cementite and abnormal ferrite. This explanation will be revisited and a comparison made with the formation of graphite and austenite in cast irons.
机译:通过覆盖粗渗透石的大型铁氧体区域定义的异形铁氧体,已在超凝胶酸盐普通碳,碳化和合金钢中报道。早期的研究表明,这种异常的铁素体可能是珠光体粗化的结果。由1962年的Hillert表示的更自然的观点是通过渗透凝聚和生长形成的异常铁素体。 2000年,我们报告了超凝胶碳钢中异常铁素体发生的进一步微观结构证据,并提出了基于碳酸盐和异常铁氧体的同时生长的碳再分布的解释。将重新审视该解释,并在铸造熨斗中形成石墨和奥氏体的比较。

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