基于原位TEM拉伸的稀土H13钢塑性形变行为和断裂机制
朱健1, 张志豪1,2(
), 谢建新1,2
), 谢建新1,2
Plastic Deformation Behavior and Fracture Mechanism of Rare Earth H13 Steel Based on In Situ TEM Tensile Study
ZHU Jian1, ZHANG Zhihao1,2(), XIE Jianxin1,2
), XIE Jianxin1,2
图10. 稀土H13钢原位拉伸试样主裂纹边缘G1和G2选区的马氏体和母相奥氏体取向重构计算结果
Color online
(a, d) boundary distributions (b, e) parent austenite orientation reconstructions (c, f) grain maps
Fig.10. Orientation reconstruction results of martensite and parent austenite of selected areas G1 (a~c) and G2 (d~f) near main crack of in situ tensile specimen of rare earth H13 steel (green line: block boundary, red line: packet boundary, black line: parent austenite grain boundary, PAGB)
