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© 2024 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.

Abstract

The effect of a high static magnetic field (HSMF) on the evolution of cube texture in directionally solidified Fe-3.0 wt. % Si alloy was studied. The results show that the <001> crystal orientation of an α-Fe single crystal was parallel to the direction of the HSMF, and a sharp cube texture was successfully formed in the final ingot. With the increase in growth speed, the main texture of the Fe-3.0 wt. % Si alloy evolved in the way of <001>→<081>→<120> along the pulling direction when an HSMF was applied. The orientation transition was attributed to the magnetocrystalline anisotropy of the α–Fe crystal during the directional solidification process. As a result of texture optimization, the specimens with an HSMF had higher saturation magnetization and permeability than the sample without an HSMF. Furthermore, a new creative method to tailor the cube texture of Fe-based alloys during the directional solidification process assisted by an HSMF is proposed.

Details

Title
The Evolution of Cube Texture in Directionally Solidified Fe-3.0 wt. % Si Alloy Assisted by a High Static Magnetic Field
Author
Liu, Chunmei; Chen, Zijian; Li, Hongyu; Lin, Wenhao; Feng, Meilong; Zheng, Tianxiang  VIAFID ORCID Logo  ; Zhou, Bangfei; Zhong, Yunbo
First page
1264
Publication year
2024
Publication date
2024
Publisher
MDPI AG
e-ISSN
20754701
Source type
Scholarly Journal
Language of publication
English
ProQuest document ID
3133350739
Copyright
© 2024 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.