Origin of phase stability in Fe with long-period stacking order as an intermediate phase in cyclic γ−ε martensitic transformation
Origin of phase stability in Fe with long-period stacking order as an intermediate phase in cyclic γ−ε martensitic transformation
复制标题
具有长周期堆垛顺序的 Fe 作为循环 γ−ε 马氏体相变中间相的相稳定性起源
DOI:
10.1103/physrevresearch.3.033215
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发表时间:
2021
影响因子:
4.2
通讯作者:
Takahiro Sawaguchi
中科院分区:
文献类型:
--
作者:
Takao Tsumuraya;Ikumu Watanabe;Takahiro Sawaguchi
A class of Fe-Mn-Si–based alloys exhibit a reversible martensitic transformation between thephase with a face-centered cubic (fcc) structure and anphase with a hexagonal close-packed (hcp) structure. During the deformation-inducedtransformation, we identified a phase that is different from thephase. In this phase, the electron diffraction spots are located at the 1/3 positions that correspond to theplane of the(hcp) phase with 2H structure, which suggests long-period stacking order (LPSO). To understand the stacking pattern and explore the possible existence of an LPSO phase as an intermediate between theandphases, the phase stability of various structural polytypes of iron was examined using first-principles calculations with a spin-polarized form of the generalized gradient approximation in density functional theory. We found that an antiferromagnetic orderedstructure is the most stable among the candidate LPSO structures and is energetically closest to thephase, which suggests that the observed LPSO-like phase adopts thestructure. Furthermore, we determined that the phase stability can be attributed to the valley depth in the density of states, close to the Fermi level.