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Microstructure evolution mechanism near the fracture lip of 4Cr5MoSiV1 steel during deforming at 580°C

机译:在580°C变形期间,4Cr5Mosiv1钢断裂唇附近的微观结构演化机制

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The failure mechanisms under thermal-mechanical conditions have always been a critical issue in hot work steels. However, previous studies mainly focused on the mechanical properties of hot work materials, while the underlying deformation mechanism remains largely unclear. Here, we investigate the crack morphology and microstructure evolution mechanism near the fracture surfaces of 4Cr5MoSiV1 hot work die steels subjected to the uniaxial tension at 580°C. An evident deformation band was observed consisting of refined α-Fe grains with a width of about 100nm along both sides of the intergranular fracture surface. Additionally, characteristic slip band rings formed frequently, presumably due to the grain rotation near the crack. Finally, carbides (including MC, M7C3and M23C6) were also considered as possible crack nucleation sources due to the existence of incoherent boundary between these carbides and the ferrite matrix.
机译:热电机械条件下的故障机制一直是热工作钢中的关键问题。然而,之前的研究主要集中在热工作材料的机械性能上,而底层变形机制仍然很大程度上不清楚。在这里,我们研究了在580℃下对高轴张力进行单轴张力的4Cr5MOSiv1热工作钢的断裂表面附近的裂纹形态和微观结构演化机制。观察到明显的变形带,由宽度约100nm的精制α-Fe晶粒组成,沿骨间骨折表面的两侧。另外,经常形成的特征滑槽环,可能是由于裂缝附近的颗粒旋转。最后,由于这些碳化物和铁氧体基质之间存在着阴离子边界,还认为碳化物(包括MC,M7C3和M23C6)也被认为是可能的裂缝成核来源。

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