This study systematically investigated the deformation behavior and fracture mechanisms of AISI 430 ferritic stainless steel (FSS) following dual-phase zone annealing with varying martensite contents, using quasi in-situ tensile testing. In 430 FSS with a low martensite volume fraction, significant deformation occurred through dislocation slip in the ferrite phase, involving the activation of multiple slip systems and dislocation transmission at grain boundaries. In contrast, in sample with high martensite fraction, dislocation slip within the ferrite was restricted, leading to an overall decrease in plasticity. During the tensile process, ferrite grains exhibited different responses under external stress. Additionally, strain concentration mainly occurred at ferrite-martensite phase boundaries and at interfaces between large and small grains. As deformation progressed, strain distribution gradually homogenized in the low martensite fraction sample. However, in the high martensite fraction sample, fracture occurred before strain distribution could become uniform. Weak bonding at ferrite-martensite phase boundaries renders these interfaces critical sites for crack initiation. The combined effects of dislocation accumulation and strain incompatibility lead to the initiation and propagation of cracks, ultimately causing material failure. Optimizing the dual-phase zone annealing processes enables ferrite grains to achieve moderate and uniform sizes while maintaining the continuous distribution of ferrite and the discontinuous distribution of martensite. This microstructural control can effectively reduce interphase stress concentration, enhance the coordinated deformation capabilities of ferrite, and thereby significantly improve the overall performance of 430 FSS.
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