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A microstructural and crystallographic investigation of the precipitation behaviour of a primary Al 3 Zr phase under a high magnetic field
Author(s) -
Li Lei,
Zhang Yudong,
Esling Claude,
Qin Ke,
Zhao Zhihao,
Zuo Yubo,
Cui Jianzhong
Publication year - 2013
Publication title -
journal of applied crystallography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.429
H-Index - 162
ISSN - 1600-5767
DOI - 10.1107/s0021889813001258
Subject(s) - crystallography , precipitation , phase (matter) , magnetocrystalline anisotropy , layer (electronics) , materials science , anisotropy , field (mathematics) , magnetic field , chemical physics , magnetic anisotropy , composite material , chemistry , magnetization , optics , physics , organic chemistry , mathematics , quantum mechanics , meteorology , pure mathematics
The effects of a high magnetic field on the precipitation behaviour of the primary Al 3 Zr phase are investigated. With and without the field, the primary Al 3 Zr crystals possess three morphologies – small tabular crystals in the deposit layer, long bars and dendritic crystals. The dendritic crystals are probably those surviving from the initial material. The tabular crystals in the deposit layer are those surviving from the heating stage, whereas the long bars are those formed during cooling. With the field, the tabular crystals in the deposit layer and the long bars tend to orient with the 〈110〉 direction parallel to the field direction, but the orientation of the dendritic crystals is less affected. The orientation of the crystals in the deposit layer arises from their magnetocrystalline anisotropy, but that of the long bars and dendritic crystals is disturbed by gravity and the formation of compound twins, respectively. Increased Zr content raises the precipitation amount of the primary Al 3 Zr crystals but weakens the alignment tendency of the tabular ones in the deposit layer. The weakness of the alignment arises from interaction between the crystals.