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Monte Carlo Simulation of NbC Precipitation Kinetics in α-Fe

机译:α-Fe中Nbc降水动力学的Monte Carlo仿真

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Using a vacancy diffusion mechanism for substitutional elements and an interstitial mechanism for carbon atoms, we propose a Monte Carlo method for simulating the coherent precipitation of niobium carbide in α-iron. Iron, niobium, and carbon atoms are distributed on a rigid, simple cubic lattice which describes both the bcc ferrite structure and the fcc NaCl-type structure of NbC. The Monte-Carlo parameters have been fitted with good accuracy to the experimental diffusion and equilibrium data. A residence time algorithm has been adapted in order to handle both the fast interstitial C diffusion and the slow substitutional Nb and Fe diffusion. Depending on the concentration and temperature, the simulations exhibit two kinds of kinetic paths: formation of transient iron carbides at high supersaturation, and nucleation of NbC precipitates at low supersaturation. Not only can the resulting kinetics of nucleation be compared with the classical theory but the simulations also provide information on cluster size, shape and density on the atomic scale which can then be directly compared with tomographic atom probe (TAP) results.
机译:利用用于碳原子的空位扩散机制和用于碳原子的间质机制,提出了一种用于模拟α-铁中碳化铌的相干沉淀的蒙特卡罗方法。铁,铌和碳原子分布在刚性的简单立方晶格上,所述立方格晶格,其描述了BCC铁氧体结构和NBC的FCC NaCl型结构。 Monte-Carlo参数已经适用于实验扩散和平衡数据的良好精度。已经调整了停留时间算法以处理快速的间隙C扩散和缓慢的替代NB和Fe扩散。取决于浓度和温度,模拟表现出两种动力学路径:在高过饱和度下形成瞬时铁碳化物,并在低过饱和下沉淀NBC沉淀。与经典理论相比,不仅可以将导致的成核动力学与经典理论进行比较,但是模拟还提供有关集群大小,形状和密度的信息,然后可以与断层图像探测(TAP)结果直接比较。

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