Shozo Hiramoto
;
Satoshi Okamoto
;
Jun Uzuhashi
;
Tadakatsu Ohkubo
;
Akihiko Toda
;
Sangwook Kim
;
Chikako Moriyoshi
;
Yoshihiro Kuroiwa
Description:
(abstract)To explore the impact of annealing temperature on the nucleation and subsequent growth of nanocrystalline α-Fe grains in a high saturation magnetization soft magnetic Fe84.8Si0.5B9.4P3.5Cu0.8C1.0 alloy, we conducted multiprobe analyses of the isothermal crystallization process within the 633 K to 733 K temperature range. Transmission electron microscopy and atom probe tomography observations for the samples isothermally annealed at 733 K and 633 K revealed distinct differences in microstructure. For the higher isothermal temperature, Cu clusters were larger, and α-Fe grains were finer. In contrast, for the lower isothermal temperature, Cu clusters were smaller, and α-Fe grains were coarser. Time-resolved synchrotron X-ray diffraction measurements provided a direct evidence of sporadic nucleation mechanism, highlighting the significant effect of isothermal temperature on the formation of α-Fe grains. To achieve an optimal microstructure for lower coercivity, it is crucial to control the Cu clustering and α-Fe nanocrystallization by annealing at higher temperatures for shorter durations.
Rights:
This version of the article has been accepted for publication, after peer review (when applicable) and is subject to Springer Nature’s AM terms of use, but is not the Version of Record and does not reflect post-acceptance improvements, or any corrections. The Version of Record is available online at: https://doi.org/10.1007/s10853-025-10696-x
Keyword: atom probe tomography, transmission electron microscopy, nanocrystalline soft magnetic material
Date published: 2025-02-10
Publisher: Springer Science and Business Media LLC
Journal:
Funding:
Manuscript type: Author's version (Accepted manuscript)
MDR DOI: https://doi.org/10.48505/nims.5341
First published URL: https://doi.org/10.1007/s10853-025-10696-x
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Updated at: 2026-02-11 08:30:29 +0900
Published on MDR: 2026-02-10 18:03:07 +0900
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