铁碳奥氏体高温晶格参数的偏摩尔体积

N. Ridley, H. Stuart
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引用次数: 50

摘要

摘要在1200°C (1473 K)温度下测量了几种铁碳合金的奥氏体晶格参数,通过外推和内插,确定了奥氏体晶格参数随碳浓度在较宽温度范围内的变化,并用于计算奥氏体中铁和碳的偏摩尔体积。两种组分的偏摩尔量变化不大,但V c、γ随温度升高而减小,而V Fe、γ随温度升高而增大。得到的奥氏体中碳的偏摩尔体积值明显低于前面引用的值。在727°C (1000 K)时,压力对奥氏体与渗碳体平衡组成的影响的测量值与计算值之间的差异可能主要是由于在计算奥氏体中碳的偏摩尔体积时使用了过高的值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Partial Molar Volumes from High-Temperature Lattice Parameters of Iron–Carbon Austenites
AbstractThe lattice parameters of a number of iron–carbon alloys have been measured in the austenite field for temperatures up to 1200° C (1473 K). By extrapolation and interpolation of these data the variation with carbon concentration of the lattice parameter of austenite has been determined for a wide range of temperatures, and used to calculate partial molar volumes of iron and carbon in austenite. Both partial molar quantities show little variation with composition but V c, γ decreases with increasing temperature, while V Fe, γ increases. The values obtained for the partial molar volume of carbon in austenite are appreciably lower than those cited earlier. It is probable that the differences previously reported between the measured and calculated effect of pressure on the composition of austenite in equilibrium with cementite at 727° C (1000 K), are due primarily to the use in the calculations of too high a value for the partial molar volume of carbon in austenite.
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