Suppression and reactivation of transformation and twinning induced plasticity in laser powder bed fusion additively manufactured Ti-10V-2Fe-3Al
Suppression and reactivation of transformation and twinning induced plasticity in laser powder bed fusion additively manufactured Ti-10V-2Fe-3Al
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DOI:
10.1016/j.addma.2021.102406
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发表时间:
2021-12-01
影响因子:
11
通讯作者:
Banerjee, R.
中科院分区:
文献类型:
--
作者:
Mantri, S. A.;Nartu, M. S. K. K. Y.;Banerjee, R.
Laser powder bed fusion (LBPF) was employed to fabricate a strain-transformable beta-Ti alloy, Ti-10V-2Fe-3Al (wt %). While the alloy is known to exhibit transformation induced plasticity (TRIP), the as-fabricated alloy, under tensile loading, did not show the same TRIP effects, even though it exhibits the same beta + omega microstructure. The repeated heating-cooling cycles experienced during the LBPF process leads to the early stages of rejection of solute elements (Fe, V, and Al), forming isothermal omega (omega) precipitates, which were captured via detailed investigations coupling transmission electron microscopy (TEM) and three-dimensional atom probe tomography (APT). While these homogeneously distributed isothermal omega precipitates lead to a higher yield strength, the TRIP/TWIP effects within the beta matrix were suppressed, leading to very low ductility and virtually no strainhardenability. Interestingly, after a simple beta-solution heat treatment followed by quenching, leading to a beta + omega (athermal) microstructure, the TRIP/TWIP effects were reactivated in the same LPBF Ti-10 V-2Fe-3Al alloy. The alloy exhibited substantial recovery of tensile ductility and a very large strain hardening (tensile strength minus yield strength -500 MPa), with a high average strain hardening rate -15000. Such a very high strain hardening rate in case of LBPF processed Ti-10 V-2Fe-3Al, appears to arise from a rapid strain-induced transformation from beta to alpha" at the early stages of plastic deformation, leading to a high-volume fraction of the martensitic phase, coupled with hierarchical twinning within the martensite plates.