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异种钢焊接接头熔合区马氏体层断裂韧性的模拟研究

A STUDY OF THE FRACTURE TOUGHNESS OF THE MARTENSITE LAYER IN AUSTENITIC-FERRITIC DISSIMILAR METAL JOINTS

  • 摘要: 奥氏体/铁素体异种钢焊接接头的熔合区中合金成分连续地变化,由奥氏体过渡为铁素体成分,Ni含量不足使该区生成马氏体层。曾有人采用实际接头冲击韧性试验方法研究接头的韧性,认为马氏体层是接头韧性的薄弱环节。本文采用模拟马氏体成分熔化炼钢的方法,在均匀的马氏体组织上研究了马氏体层的断裂韧性,同时也对接头其它区域的断裂韧性进行了研究。结果表明:在Cr25-Ni13/13CrMo44异种钢接头中,接头韧性的薄弱区并不在马氏体层上,而是与马氏体层相毗邻的热影响区的过热区;该区粗大的贝氏体组织使得这一区域的断裂呈准解理型,而马氏体层的断裂主要呈韧性撕开型。

     

    Abstract: In the austenitic-ferritic dissimilar metal welded joints the content of alloying elements in the transition zone varies continuously from HAZ to weld. Due to the low level of Ni content, a martensite layer is formed in this zone during the welding process.The Charpy impact test made before indicated that the martensite layer was the weakest zone in toughness in the joints. In this paper, the simulating lest, in which specimens were prepared by casting steels in accordance with the compositions in the martensite layer respectively,was conducted to evaluate the fracture toughness of the martensite layer in the homogeneous structure. The experiments were alse made to investigate the variation in toughness in the different regions of the joint.The results show that the weakest region in toughness in the dissimilar metal joints is not the martensite layer but the overheated zone in the HAZ. The fracture in the overheated zone is caused by the coarse-grained bainite, and it appears as a quasicleavage fracture; however, in the martensite elayer, it appears as a tear fracture.

     

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