Characterization of Precipitation Behavior and Fracture Toughness along Thickness Direction in SA508 Gr.3 Mn-Mo-Ni low alloy steels

被引:4
作者
Song, Jaemin [1 ,2 ]
Kim, Min-Chul [1 ]
Hong, Seokmin [1 ]
Lee, Bong-Sang [1 ]
机构
[1] Korea Atom Energy Res Inst, Nucl Mat Safety Res Div, Daejeon 34057, South Korea
[2] Univ Sci & Technol, Quantum Energy Chem Engn, Daejeon 34113, South Korea
来源
KOREAN JOURNAL OF METALS AND MATERIALS | 2015年 / 53卷 / 10期
关键词
low alloy steels; forging; fracture toughness; mechanical properties; SA508; Gr.3; CLEAVAGE FRACTURE; MASTER CURVE; TEMPERATURE;
D O I
10.3365/KJMM.2015.53.10.700
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
SA 508 Gr.3 Mn-Mo-Ni low alloy steel forgings thicker than 200 mm are used for reactor pressure vessels in nuclear power plants. The cooling rate difference along the thickness direction during the quenching process causes variation in the microstructure and mechanical properties. The microstructural variation and its influence on the fracture toughness of RPV steels were investigated in this study. The cleavage fracture toughness in the transition region were evaluated with the ASTM E1921 master curve method for samples at different locations from the inner surface to the center thickness of the RPV steel. The microstructural features, such as the area fraction, and the size and distribution of precipitates were quantitatively evaluated at each sampling position. Microstructure observations showed that at near the surface position, bainite laths are finer, and furthermore, the carbides are smaller and homogeneously distributed. The fracture toughness at the surface was better than those at deeper positions. The reference temperature To showed a linear relationship with the area fraction of the carbides bigger than a certain critical size. It is concluded that the size of the precipitates caused by the cooling rate gradient may have a dominant role in controlling the cleavage fracture toughness variation along the thickness direction for a very thick RPV steel.
引用
收藏
页码:700 / 710
页数:11
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