Crystal structure of the orthorhombic U2-Al4Mg4Si4 precipitate in the Al-Mg-Si alloy system and its relation to the β′ and β" phases

被引:190
作者
Andersen, SJ [1 ]
Marioara, CD
Froseth, A
Vissers, R
Zandbergen, HW
机构
[1] SINTEF, Mat Technol, Appl Phys, N-7465 Trondheim, Norway
[2] NTNU, Dept Phys, N-7491 Trondheim, Norway
[3] Delft Univ Technol, Natl Ctr HRTEM, Mat Sci Lab, NL-2628 AL Delft, Netherlands
来源
MATERIALS SCIENCE AND ENGINEERING A-STRUCTURAL MATERIALS PROPERTIES MICROSTRUCTURE AND PROCESSING | 2005年 / 390卷 / 1-2期
关键词
Al-Mg-Si alloys; U2-Al4Mg4Si4; precipitates; high-resolution transmission electron microscopy; precipitate coherency relations;
D O I
10.1016/j.msea.2004.09.019
中图分类号
TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
The atomic structure of a common precipitate in the Al-Mg-Si system has been determined. It is isotypic with TiNiSi (space group Pnma) and contains four units of MgAlSi in a unit cell of size a = 0.675 nm, b = 0.405 nm, c = 0.794 nm. EDS analyses support the composition. A model was based on the atomic structure of the beta' precipitate, electron diffraction and high-resolution transmission electron microscopy (HRTEM) images. A quantum mechanical refinement of the model removed discrepancies between simulated and experimental diffraction intensities. Finally, a multi-slice least square refinement confirmed the structure. The structural relation with beta" is investigated. A similar Mg-Si plane also existing in beta" and beta', can explain most coherency relations between the precipitate phases and with matrix. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:127 / 138
页数:12
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