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Carbon Diffusion Measurement in Austenite in the Temperature Range 500 °C to 900 °C

机译:在500°C至900°C温度范围内的奥氏体中碳扩散测量

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摘要

Carbon diffusion in austenite plays a critical role in phase transformation in steel. However, it can only be estimated in the fully austenitic range and has then to be extrapolated to the temperature range of the phase transformation. Therefore, published data are limited to temperatures above 750 °C. In this study, new experiments are carried out to determine the carbon diffusion coefficient in austenite at temperatures as low as 500 °C. Carburization experiments are performed in the austenitic range for a Fe-1.5 pct Mn 0.13 pct C and a Fe-31 pct Ni alloy (wt pct). Composition profile measurements, which are done using glow discharge optical emission spectrometry (GDOES), show that the surface composition is not constant with time. A methodology has been developed to assess the diffusion coefficient of carbon in austenite combining the measured carbon profiles and a numerical method to compute the diffusion profile taking into account the time evolution of the boundary condition. This method is first validated on the Fe-C-Mn steel. Carburization experiments are carried out on a Fe-31 pct Ni alloy at 900 °C, 800 °C, 700 °C, 600 °C, and 500 °C. The carbon diffusion coefficient is assessed using the method described above and fitted with the following expression (T in Kelvin): $ D = 1.23cdot10^{{ - 6}} cdot e^{{ - frac{{15,050}} {{T{left( {text{K}} right)}}}}} ({text{m}}^{{text{2}}} {text{/s}}) $ . The new expression is compared with previous experimental results measured for comparable nickel content at higher temperatures, and it shows a reasonable agreement. The model proposed by ?gren for carbon diffusion has been modified to take into account the thermodynamic contribution of nickel. This model also shows good agreement with the present experimental results, even if it was fitted to experiments performed at higher temperatures.
机译:奥氏体中的碳扩散在钢的相变中起关键作用。但是,只能在完全奥氏体范围内进行估算,然后必须将其外推至相变的温度范围。因此,公开的数据仅限于高于750°C的温度。在这项研究中,进行了新的实验以确定在低至500°C的温度下奥氏体中的碳扩散系数。 Fe-1.5 pct Mn 0.13 pct C和Fe-31 pct Ni合金(wt pct)在奥氏体范围内进行了渗碳实验。使用辉光放电光发射光谱法(GDOES)进行的成分分布测量表明,表面成分不是随时间变化的。已经开发出一种方法,结合测得的碳分布和结合边界条件随时间变化的数值方法来计算碳在奥氏体中的扩散系数。该方法首先在Fe-C-Mn钢上得到验证。在900°C,800°C,700°C,600°C和500°C的Fe-31 pct Ni合金上进行渗碳实验。使用上述方法评估碳扩散系数,并拟合以下表达式(开尔文中的T):$ D = 1.23cdot10 ^ {{{-6}} cdot e ^ {{-frac {{15,050}} {{T {left({text {K}}右)}}}}}({text {m}} ^ {{text {2}}} {text {/ s}})$。将该新表达式与之前在较高温度下测得的镍含量可比较的实验结果进行了比较,结果显示出合理的一致性。菲伦提出的碳扩散模型已经过修改,以考虑到镍的热力学贡献。即使适合在较高温度下进行的实验,该模型也与当前的实验结果显示出良好的一致性。

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  • 来源
    《Metallurgical and Materials Transactions A》 |2007年第6期|1169-1176|共8页
  • 作者单位

    Arcelor Research Industry Gent/OCAS N.V B-9060 Zelzate Belgium;

    Materials Science Department Ecole Polytechnique Universitaire de Lille Lille France;

    Arcelor Research Industry Gent/OCAS N.V B-9060 Zelzate Belgium;

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