Study on tempering behaviour of AISI 410 stainless steel

被引:67
作者
Chakraborty, Gopa [1 ]
Das, C. R. [1 ]
Albert, S. K. [1 ]
Bhaduri, A. K. [1 ]
Paul, V. Thomas [1 ]
Panneerselvam, G. [2 ]
Dasgupta, Arup [1 ]
机构
[1] Indira Gandhi Ctr Atom Res, Met & Mat Grp, Kalpakkam 603102, Tamil Nadu, India
[2] Indira Gandhi Ctr Atom Res, Chem Grp, Kalpakkam 603102, Tamil Nadu, India
关键词
Martensite; Tempering; Embrittlement; Carbide; XRD; TEM; EMBRITTLEMENT; MICROSTRUCTURE;
D O I
10.1016/j.matchar.2014.12.015
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Martensitic stainless steels find extensive applications due to their optimum combination of strength, hardness and wear-resistance in tempered condition. However, this class of steels is susceptible to embrittlement during tempering if it is carried out in a specific temperature range resulting in significant reduction in toughness. Embrittlement of as-normalised AISI 410 martensitic stainless steel, subjected to tempering treatment in the temperature range of 673-923 K was studied using Charpy impact tests followed by metallurgical investigations using field emission scanning electron and transmission electron microscopes. Carbides precipitated during tempering were extracted by electrochemical dissolution of the matrix and identified by X-ray diffraction. Studies indicated that temper embrittlement is highest when the steel is tempered at 823 K. Mostly iron rich carbides are present in the steel subjected to tempering at low temperatures of around 723 K, whereas chromium rich carbides (M23C6) dominate precipitation at high temperature tempering. The range 773-823 K is the transition temperature range for the precipitates, with both Fe2C and M23C6 types of carbides coexisting in the material. The nucleation of Fe2C within the martensite lath, during low temperature tempering, has a definite role in the embrittlement of this steel. Embrittlement is not observed at high temperature tempering because of precipitation of M23C6 carbides, instead of Fe2C, preferentially along the lath and prior austenite boundaries. Segregation of S and P, which is widely reported as one of the causes for temper embrittlement, could not be detected in the material even through Auger electron spectroscopy studies. (C) 2014 Elsevier Inc. All rights reserved.
引用
收藏
页码:81 / 87
页数:7
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