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首页> 外文期刊>International Journal of Refractory Metals & Hard Materials >About one stable and three metastable eutectic microconstituents in the Fe-W-C system
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About one stable and three metastable eutectic microconstituents in the Fe-W-C system

机译:Fe-W-C系统中约有一种稳定的和三种亚稳态的共晶微成分

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The Fe-W-C system has been the subject of numerous investigations and the findings have led to quite different interpretations in the iron-rich corner, justifying the need for new experimental studies. In the present study, some 12 compositions are prepared using both the powder metallurgy technique and the casting of melted alloys. DTA experiments, long time annealing supplemented by the phase separation technique and controlled solidification experiments are carried out. The micrographs of the corresponding specimens reveal significant sedimentation of WC carbides, an observation which must be carefully taken into account in interpreting the micrographs. The liquid/solid equilibria between 1423 and 1543 K are investigated and the corresponding partial isothermal sections of the Fe-W-C system are compared to the calculated phase equilibria based on thermochemical models. Four ternary eutectic microconstituents gamma/M_6C/ cementite, gamma/WC/cementite, gamma/M_6C/graphite and gamma/WC/graphite, are observed by experiments. The microstructures are characterised and the four eutectic temperatures are established both experimentally and by calculations. The experimental eutectic temperatures lie within a range of 10 K but well below the temperatures predicted by thermodynamic modelling and the calculated temperatures within a range of 20 K. This explains why metastable microconstituents can so readily be formed.
机译:Fe-W-C系统一直是众多研究的主题,这些发现导致在铁含量高的角落产生了截然不同的解释,从而证明需要进行新的实验研究。在本研究中,使用粉末冶金技术和熔融合金铸造制备了约12种成分。进行了DTA实验,补充了相分离技术的长时间退火以及受控的凝固实验。相应样品的显微照片显示WC碳化物有大量沉积,在解释显微照片时必须仔细考虑这一观察结果。研究了1423至1543 K之间的液/固平衡,并将Fe-W-C系统的相应部分等温截面与基于热化学模型计算出的相平衡进行了比较。通过实验观察到了四种三元共晶微成分γ/ M_6C /渗碳体,γ/ WC /硅藻土,γ/ M_6C /石墨和γ/ WC /石墨。表征了微结构,并通过实验和计算确定了四个共晶温度。实验的共晶温度在10 K的范围内,但远低于热力学建模预测的温度和计算的温度在20 K的范围内。这解释了为什么可以如此容易地形成亚稳态的微成分。

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