2018
DOI: 10.1002/pssa.201700762
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Strain Mediated in‐Plane Uniaxial Magnetic Anisotropy in Amorphous CoFeB Films Based on Structural Phase Transitions of BaTiO3 Single‐Crystal Substrates

Abstract: The uniaxial in-plane magnetic anisotropy constants (K 1 ) of amorphous Co 10 Fe 74 B 16 (CoFeB) films deposited on BaTiO 3 (BTO) single-crystal substrates are characterized using a vibrating sample magnetometer. As a result, a significant increase in K 1 with temperature is observed by a factor of 26, from 0.267 Â 10 5 erg cm À3 at 300 K to 6.88 Â 10 5 erg cm À3 at 230 K, and the thermal/K 1 cycling was reproduced. Estimation of the magnetoelastic effect at the CoFeB/ BTO interface demonstrated that the exter… Show more

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Cited by 8 publications
(4 citation statements)
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“…The strains in the a 1 (a 2 ) domains change by u xx /u xx ≈ 124% (−46%) and u yy /u yy ≈ −46% (124%). agree with previous studies considering similar systems [25,57]. Figures 4(a), 4(c), and 4(d) show the calculated field dependence of the change of the equilibrium angle ψ eff between H eff and the x axis under laser excitation.…”
Section: B Laser-induced Change Of Magnetoelastic Anisotropysupporting
confidence: 89%
“…The strains in the a 1 (a 2 ) domains change by u xx /u xx ≈ 124% (−46%) and u yy /u yy ≈ −46% (124%). agree with previous studies considering similar systems [25,57]. Figures 4(a), 4(c), and 4(d) show the calculated field dependence of the change of the equilibrium angle ψ eff between H eff and the x axis under laser excitation.…”
Section: B Laser-induced Change Of Magnetoelastic Anisotropysupporting
confidence: 89%
“…1(e)]. The magnetoelastic anisotropy energy associated with the 90°in-plane magnetization rotation B 1 (u yy − u xx ) = −2.17 • 10 4 mJ/cm 3 and the magnetostriction coefficient λ = 8 • 10 −6 agree with previous works considering similar systems [25,61].…”
supporting
confidence: 87%
“…In general, variations in H c indicate that the pinning effects of the magnetic domain movements are present or absent owing to substrate roughness or impurities [40]. Additionally, variations in M r /M s imply that multi-grains or magnetic domains are composed of magnetic anisotropies of various orientations [43,44]. These values (H c and M r /M s ) can be used to qualitatively evaluate the magnetic anisotropy of a sample [38,45,46].…”
Section: Magnetic Properties With Deformable Substratesmentioning
confidence: 99%