1996
DOI: 10.1002/pssa.2211580125
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Experimental Verification of Theoretical Relations for the Domain Structure of Uniaxial Ferromagnets

Abstract: Precise measurements of stripe domain periods and of bubble domain collapse field in two garnets over a wide thickness range are reported along with a comparison with existing theories and attempts to determine from them the material parameters. Domain periods obey the Kittel half-power law in an intermediate sample thickness range, increase more steeply at larger sample thickness in accordance with the Szymczak theory, and also increase with decreasing sample thickness (below a 'critical' value) as earlier pr… Show more

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Cited by 9 publications
(7 citation statements)
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“…It has been known since 1960's that as the crystal thickness increases, magnetic domains at the surface become more complex, and show corrugations and even fractalizations to further screen the surface magnetic charges on larger scales [26−30]. Such wavy or branched flower-like domain textures have been observed in a broad range of uniaxial ferromagnets such as Co [26,28], Nd-Fe-B alloys [26,30,31], hexagonal ferrites [28,32] and garnet ferrites [29]. In spite of such a long history of domain wall physics over 60 years, the anisotropic sawtooth pattern governed by 4 ̅ symmetry as observed in this antiskyrmion material has never been reported so far, and thus must be exclusively attributed to the anisotropic DMI in the S4 crystal lattice.…”
Section: Mfm Observation Of Sawtooth Domain Patternsmentioning
confidence: 99%
“…It has been known since 1960's that as the crystal thickness increases, magnetic domains at the surface become more complex, and show corrugations and even fractalizations to further screen the surface magnetic charges on larger scales [26−30]. Such wavy or branched flower-like domain textures have been observed in a broad range of uniaxial ferromagnets such as Co [26,28], Nd-Fe-B alloys [26,30,31], hexagonal ferrites [28,32] and garnet ferrites [29]. In spite of such a long history of domain wall physics over 60 years, the anisotropic sawtooth pattern governed by 4 ̅ symmetry as observed in this antiskyrmion material has never been reported so far, and thus must be exclusively attributed to the anisotropic DMI in the S4 crystal lattice.…”
Section: Mfm Observation Of Sawtooth Domain Patternsmentioning
confidence: 99%
“…The Kittel model is limited to systems with small quality ratios. However, in many strongly anisotropic materials Q is large and no critical thickness is observed [4,18,23]. [6,7], it separates the homogeneous state without domains from the weak stripe phase.…”
Section: Critical Thickness and Critical Anisotropymentioning
confidence: 99%
“…We adopt a sinewave magnetization profile in the wall and we take into account the magnetostatic interaction between the top and bottom surfaces of the film. Our model applies to hexagonal Co, for which a critical thickness between 25 nm [15,16] and 40 nm [17] has been reported, as well as to materials with high magneto-crystalline anisotropy, such as FePd(001) or garnet films [4,17,18]. Another possible application concerns ferromagnetic thin films of Mn 5 Ge 3 that were recently synthesized [19,20].…”
Section: Introductionmentioning
confidence: 99%
“…However, investigations were limited by using the magneto-optic Faraday and Kerr effect in the past 12,13 and type-I contrast in SEM more recently. [14][15][16] Measurement in domain size using TEM can provide high spatial resolution for a range of thickness through which electrons can penetrate, although determining the thickness of a TEM sample is not trivial. 17 Figure 1͑a͒ is a Lorentz image revealing the configuration of magnetic domains from a Nd 2 Fe 14 B single crystal with its surface normal near the ͓001͔ easy axis.…”
Section: A Measurements Of Domain Width As a Function Of Crystal Thimentioning
confidence: 99%