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The inverted hysteresis loops in the exchange-coupled multilayers such as the Co/Pt/Gd/Pt/films are explained by a combination between the antiferromagnetic coupling among the layers and the magnetic anisotropy acting on only the side layer (Refs. Conversely, those in the heteroepitaxial Fe films on W(001) or Si(111) originate from the competition between the cubic and uniaxial magnetic anisotropy in the isolated Fe microcrystallines (Refs., and
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The inverted hysteresis loops in the exchange-coupled multilayers such as the Co/Pt/Gd/Pt/films are explained by a combination between the antiferromagnetic coupling among the layers and the magnetic anisotropy acting on only the side layer (Refs. 12131415). Conversely, those in the heteroepitaxial Fe films on W(001) or Si(111) originate from the competition between the cubic and uniaxial magnetic anisotropy in the isolated Fe microcrystallines (Refs. 16 and 17).
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Sm, 9.4; Gd, 26.7; Cr, 12.1 Calculated for (formula presented) 18.2; Gd, 17.2; Cr, 12.0, and found: Sm, 18.7; Gd, 17.5; Cr, 12.8
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The (formula presented) powders were prepared by reacting an aqueous solution containing mixtures of (formula presented) and (formula presented) with a (formula presented) aqueous solution at 55 °C to yield a light yellow precipitate. Elemental analyses for Sm, Gd, and Cr were obtained by inductively coupled plasma mass spectrometry, e.g., Calculated for (formula presented) 9.3; Gd, 26.4; Cr, 11.9, and found: Sm, 9.4; Gd, 26.7; Cr, 12.1 Calculated for (formula presented) 18.2; Gd, 17.2; Cr, 12.0, and found: Sm, 18.7; Gd, 17.5; Cr, 12.8. Calculated for. (formula presented) 20.5; Gd, 14.9; Cr, 12.0, and found: Sm, 20.8; Gd, 14.5; Cr, 12.1.
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Calculated for. (formula presented) 20.5; Gd, 14.9; Cr, 12.0, and found: Sm, 20.8; Gd, 14.5; Cr
, vol.12
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