铁碳体系:超硬质合金共晶的成因和形态

Vladyslav Mazur
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摘要

已开发出一种对铁-碳熔体进行热循环处理的直接技术,可在结晶前引起显著的过冷。在显著过冷条件下,原共晶合金的共晶结晶是一个复杂的过程,包括几个部分结晶过程和结晶相的同步溶解:奥氏体和两种可转移碳化物(Fe3C 和 Fe7C3)。我们对 L→L+Fe7C3 共晶转变的显微和热成像(DSC)动力学进行了研究。一般来说,结晶按照 L→L+Fe7C3+γ→L+Fe7C3+γ+Fe3C→ Fe7C3+γ+Fe3C 的方案进行。因此,形成了以奥氏体为基体的板状共晶(Fe7C3+γ)和以雪明体为基体的斑晶(Fe3C+γ)。图中提供了 Fe-C 体系中蜕变相平衡的示意图。在所进行的实验中,相变发生在两个子系统中:Fe-Fe3C(在低过冷度时)和 Fe-Fe7C3(在高过冷度时的第二种较高蜕变度的蜕变平衡子系统)。碳化物相的置换以及与每种碳化物处于可转移平衡状态的奥氏体的不同平衡浓度证实了这一点。
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The Iron-Carbon System: Genesis and Morphology of the Eutectic Involving Hyper-Cementite Carbide
A straightforward technology for the thermal cyclic processing of the Fe-C melt has been developed to induce significant super-cooling before crystallization. Eutectic crystallization of pro-eutectic alloys under substantial super-cooling is demonstrated to be a complex process, comprising several partial crystallization processes and the synchronous dissolution of crystalline phases: austenite and two metastable carbides, Fe3C and Fe7C3. The kinetics of the eutectic transformation L→L+Fe7C3 in its microscopic and thermal (DSC) imaging has been studied. In general, crystallization proceeds according to the scheme L→L+Fe7C3+γ→L+Fe7C3+γ+Fe3C→ Fe7C3+γ+Fe3C. Consequently, plate-like eutectic (Fe7C3+γ) with an austenite matrix and ledeburite (Fe3C+γ) with a cementite matrix are formed. A schematic diagram of the metastable phase equilibria in the Fe-C system is provided. In the conducted experiments, phase transformations occur in two subsystems: Fe-Fe3C (at low supercooling) and Fe-Fe7C3 (a subsystem of metastable equilibria of the second, higher degree of metastability at large supercooling). This is confirmed by the replacement of the carbide phase and different equilibrate concentrations of austenite in metastable equilibrium with each of the carbides.
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