TY - JOUR
T1 - Kink Formation Process in Long-Period Stacking Ordered Mg-Zn-Y Alloy
AU - Yamasaki, Shigeto
AU - Tokuzumi, Tsubasa
AU - Li, Wansong
AU - Mitsuhara, Masatoshi
AU - Hagihara, Koji
AU - Fujii, Toshiyuki
AU - Nakashima, Hideharu
N1 - Funding Information:
This work was supported by the Japan Society for the Promotion of Science ( JSPS ) KAKENHI for Scientific Research on Innovative Areas " MFS Materials Science (Grant Number: JP18H05481 , JP18H05478 , JP18H05254 and JP18H05475 )".
Funding Information:
This work was supported by the Japan Society for the Promotion of Science (JSPS) KAKENHI for Scientific Research on Innovative Areas "MFS Materials Science (Grant Number: JP18H05481, JP18H05478, JP18H05254 and JP18H05475)".
Publisher Copyright:
© 2020 Acta Materialia Inc.
PY - 2020/8/15
Y1 - 2020/8/15
N2 - The formation process of the kink bands in a directionally solidified, polycrystalline, long-period stacking ordered (LPSO) Mg85Zn6Y9 phase during compression deformation was investigated. In-situ compression observations by scanning electron microscopy and electron backscattered diffraction analysis revealed that regions with localized crystal orientation rotation appeared before ridge kinks formed as surface relief. In this paper, it is called as pre-kink The observed pre-kinks were composed of two separate regions rotated in opposite directions to each other and distinguished from one another by the three boundaries. A transmission electron microscopy observation revealed that the boundaries of the pre-kink are sub-boundaries consisting of edge dislocation array, and both its ends are terminated within the matrix. These characteristics match the reported that of regular ridge kink boundaries. In addition, while pre-kinks do not possess the ability of complete reversibility, its boundaries are capable of moving elastically.
AB - The formation process of the kink bands in a directionally solidified, polycrystalline, long-period stacking ordered (LPSO) Mg85Zn6Y9 phase during compression deformation was investigated. In-situ compression observations by scanning electron microscopy and electron backscattered diffraction analysis revealed that regions with localized crystal orientation rotation appeared before ridge kinks formed as surface relief. In this paper, it is called as pre-kink The observed pre-kinks were composed of two separate regions rotated in opposite directions to each other and distinguished from one another by the three boundaries. A transmission electron microscopy observation revealed that the boundaries of the pre-kink are sub-boundaries consisting of edge dislocation array, and both its ends are terminated within the matrix. These characteristics match the reported that of regular ridge kink boundaries. In addition, while pre-kinks do not possess the ability of complete reversibility, its boundaries are capable of moving elastically.
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U2 - 10.1016/j.actamat.2020.04.051
DO - 10.1016/j.actamat.2020.04.051
M3 - Article
AN - SCOPUS:85085964135
SN - 1359-6454
VL - 195
SP - 25
EP - 34
JO - Acta Materialia
JF - Acta Materialia
ER -