Uncovering the role of heterogeneous microstructure in the mechanical anisotropy of ultra-high-strength steel fabricated by directed energy deposition–arc
The anisotropic properties of components produced by directed energy deposition–arc (DED-Arc) markedly limit their use in engineering. Thus, it is crucial to elucidate the mechanism that regulates this anisotropic phenomenon in DED-Arc components to ensure the reliable application of this technology in high-performance components. In this study, 300M steel was fabricated by DED-Arc with controlled interlayer temperature, and a critical phenomenon was observed. At an interlayer temperature of 200 °C, the strength was isotropic, while the ductility exhibited a certain degree of anisotropy. When the interlayer temperature increased above the martensite start temperature to 300 °C, a unique anisotropy in mechanical properties emerged. The vertical specimens exhibited higher ultimate tensile strength and elongation but lower yield strength than the horizontal specimens. At an interlayer temperature of 200 °C, the microstructure was relatively uniform and consisted entirely of tempered martensite. The plastic anisotropy mainly originated from directional grain growth. At an interlayer temperature of 300 °C, the microstructure evolved into a heterogeneous structure consisting of alternating soft and hard zones, caused by the uneven distribution of soft phases (tempered martensite and needle‑like bainite) and hard phases (untempered martensite). In this case, the spatial arrangement of the heterogeneous structure governed the anisotropy. Under horizontal tension, the soft and hard zones are alternately stacked perpendicular to the tensile direction, and the deformation compatibility was constrained by the hard zones, resulting in higher yield strength but lower ductility. Under vertical tension, the soft and hard zones are stacked parallel to the tensile direction, offering better deformation compatibility. Moreover, the Orowan strengthening effect induced by the interlayer regions was more pronounced, leading to a higher ultimate tensile strength than that of the horizontal specimens. This study elucidates the microscale mechanism of heterogeneous structure formation upon exceeding the martensite start temperature, thereby producing this unique anisotropy.

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