TY - JOUR
T1 - Spontaneous creation of exchange bias in epitaxially self-assembled nanostructures driven by inhomogeneous structural transformation
AU - Bhukta, Anjan
AU - Kumar Patel, Akhilesh
AU - Horvitz, Dror
AU - Kohn, Amit
AU - Goldfarb, Ilan
N1 - Publisher Copyright:
© 2022 Elsevier B.V.
PY - 2023/2/1
Y1 - 2023/2/1
N2 - Ternary silicide nanostructures were grown by solid phase epitaxy of Ni80Fe20 Permalloy on a vicinal Si(0 0 1) surface, with the aim of increasing magnetic anisotropy and stability in assemblies of epitaxial islands. The first nanostructures to form were ternary Fe(Ni)Si2 disilicide islands crystallized in a CaF2-prototype structure, with well-defined flat-top and ridge geometry above the substrate surface and pyramidally faceted interfaces below the surface. Under higher temperature and Permalloy coverage conditions, most of the ridge islands had their shape transformed into the more energetically favorable flat-tops. This shape transition, was driven by vertical interdiffusion and structural phase transformation at the top part of the nanostructures above the surface: the Fe-rich top parts transformed from the CaF2-based γ-disilicide to a CsCl-based c-monosilicide, while the Ni-rich sub-surface part of the islands retained its original CaF2-γ structure. The γ-phase is known to exhibit ferromagnetic order, whereas the c-phase has been identified as antiferromagnetic. As a result of such self-formed coupling between the antiferromagnetic top and ferromagnetic bottom part of the islands, an exchange bias was created, evident from magnetometry.
AB - Ternary silicide nanostructures were grown by solid phase epitaxy of Ni80Fe20 Permalloy on a vicinal Si(0 0 1) surface, with the aim of increasing magnetic anisotropy and stability in assemblies of epitaxial islands. The first nanostructures to form were ternary Fe(Ni)Si2 disilicide islands crystallized in a CaF2-prototype structure, with well-defined flat-top and ridge geometry above the substrate surface and pyramidally faceted interfaces below the surface. Under higher temperature and Permalloy coverage conditions, most of the ridge islands had their shape transformed into the more energetically favorable flat-tops. This shape transition, was driven by vertical interdiffusion and structural phase transformation at the top part of the nanostructures above the surface: the Fe-rich top parts transformed from the CaF2-based γ-disilicide to a CsCl-based c-monosilicide, while the Ni-rich sub-surface part of the islands retained its original CaF2-γ structure. The γ-phase is known to exhibit ferromagnetic order, whereas the c-phase has been identified as antiferromagnetic. As a result of such self-formed coupling between the antiferromagnetic top and ferromagnetic bottom part of the islands, an exchange bias was created, evident from magnetometry.
KW - Magnetic exchange bias
KW - Phase transformation in epitaxial nanostructures
KW - Scanning tunneling microscopy
KW - Ternary iron-nickel silicide
UR - http://www.scopus.com/inward/record.url?scp=85141547383&partnerID=8YFLogxK
U2 - 10.1016/j.apsusc.2022.155525
DO - 10.1016/j.apsusc.2022.155525
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AN - SCOPUS:85141547383
SN - 0169-4332
VL - 610
JO - Applied Surface Science
JF - Applied Surface Science
M1 - 155525
ER -