4.6 Article

Magnetic domain structure across the austenite-martensite interface in Ni50Mn25Ga20Fe5 single crystalline thin foil

期刊

APPLIED PHYSICS LETTERS
卷 119, 期 21, 页码 -

出版社

AIP Publishing
DOI: 10.1063/5.0066983

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资金

  1. Czech Science Foundation (Czech Republic) [19-09882S]
  2. Operational Programme Research, Development and Education - European Structural and Investment Funds
  3. Czech Ministry of Education, Youth and Sports (MEYS CR Project) [SOLID21 CZ.02.1.01/0.0/0.0/16_019/0000760]
  4. MEYS CR [LM2018110]

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The study used Lorentz transmission electron microscopy to investigate the magnetic domain structure at the martensite transformation interface in a Ni50Mn25Ga20Fe5 alloy. By reducing the thickness of the foil, the stability of the magnetic domain structure was achieved, with dense labyrinth structures in thicker regions and broader domains in thinner regions. The interface consists of a nanosized laminated structure of austenite and martensite, where the two distinct magnetic domain structures interpenetrate and transition within the interface region.
The magnetic domain structure (MDS) at the martensite transformation interface is relevant for the complete understanding of functionalities in magnetic shape memory alloys. We study the MDS in Ni50Mn25Ga20Fe5 single crystalline foil using Lorentz transmission electron microscopy. The transformation interface is stabilized by decreasing foil thickness at a thickness of about 40 nm. The martensite in the thicker region contains no twin domains and exhibits dense labyrinth MDS with magnetization out-of-plane. The austenite in the thinner region exhibits broad magnetic domains with magnetization in-plane. The transformation interface is about 1 mu m broad, formed by an unusual nanosized laminated structure of austenite and martensite. Within the interface region, the two distinct MDSs interpenetrate each other, with a labyrinth MDS of martensite changing suddenly to broad magnetic domains of austenite. The changes from dense to broad domains do not follow the underlying phase changes exactly but occur on antiphase boundaries, revealing their role in the overall MDS formation.

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