马氏体形态的平行多层截面法研究
收稿日期: 2010-01-05
修回日期: 2010-05-19
网络出版日期: 2010-08-10
基金资助
国家自然科学基金资助项目50871082
A STUDY OF MARTENSITIC MORPHOLOGY BY PARALLEL MULTIPLE–LAYERS SECTIONING
Received date: 2010-01-05
Revised date: 2010-05-19
Online published: 2010-08-10
Supported by
Supported by National Natural Science Foundation of China (No.50871082)
设计了一种平行截面原位观察方法, 并研究了一种C含量(质量分数)为1.37%的高碳钢的马氏体形态. 采用激光打孔定位、超细抛光多层减薄方法原位追踪测量了目标马氏体的长度、宽度与减薄厚度的变化. 以厚度累加变化为横坐标, 测量的长度与宽度对称分布为纵坐标, 还原出的马氏体空间形态为扁椭球体, 而不是传统教科书中描述的透镜体, 椭球的几何参数为a/b≈3, a/c≈20.热力学分析表明: 形核能量除了与材料的物理特性有关外, 还与新相的形状有关. 在同等晶粒尺寸条件下, 扁椭球状新相的形核功明显低于透镜状新相的形核功.含C量降低会导致相变驱动力降低, 并使形核功增加, 马氏体新相晶核为板条形态时可弥补因含C量下降导致的形核功增加.
柳永宁 , 张贵一 , 李伟 . 马氏体形态的平行多层截面法研究[J]. 金属学报, 2010 , 46(8) : 930 -934 . DOI: 10.3724/SP.J.1037.2010.00007
In metallography the shape of high carbon martensite is commonly considered to be ens–like in three dimensions, which is of needle or bamboo leaf on the OM micrographs of section lanes. However, a round martensite on OM micrographs have never been seen so far. This question as not been answered over the years. It has not been theoretically explanined why is martensite ath–like for low carbon steels and lens–like for high carbon steels on OM micrographs. For answering hese questions, the martensitic morphology of a steel with carbon content 1.37% was observed in the ame view by OM using a method of multiple sectioning of one sample. The length, width of the aimed artensite and sectioned thickness of samples were measured before observing. It is found that the artensite is a flat ellipsoid rather than lens–like as described in traditional textbooks. The ratio of a/b is about 3 and a/c is abot 20 for the martensite ellisoid. The thermal dynamic analyss ndicates hat the nucleation energy for a martenste s closely related to its shape. Ithe austenite with the ame grain size, the nucleation energy (ΔG∗) of martensite will be lower with ellipsoid shape than with lens shape. The drvng force for martensitic transformation will reduce with the decrease of carbon ontent, resulting n the formation of lath–like martensite in steels with low carbon content.
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