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Magnetic anisotropy ofSm2Fe17single crystals

Diop, L. V. B. ; Kuz'min, M. D. ; Skokov, K. P. ; Karpenkov, D. Yu. ; Gutfleisch, O. (2016)
Magnetic anisotropy ofSm2Fe17single crystals.
In: Physical Review B, 94 (14)
doi: 10.1103/PhysRevB.94.144413
Artikel, Bibliographie

Kurzbeschreibung (Abstract)

The previously accepted notion that the spontaneous magnetization of Sm2Fe17 lies in the basal plane of the crystal is true only approximately, and then only around room temperature. At low temperatures the magnetization, whose orientation is not fixed by the symmetry, is found to deviate from the basal plane by as much as 10 degrees. The threefold symmetry axis is a hard direction; to magnetize the crystal in this direction, a magnetic field of about 9 T is required. The hard-axis magnetization arrives at saturation discontinuously, by way of a first-order phase transition. The behavior is a general one for trigonal ferromagnets where K-1 < 0 and the leading trigonal anisotropy constant is nonzero, K-2' not equal 0. Although of universal occurrence, the first-order transition is only visible at low temperatures, where it is accompanied by a magnetization anomaly of sufficient size.

Typ des Eintrags: Artikel
Erschienen: 2016
Autor(en): Diop, L. V. B. ; Kuz'min, M. D. ; Skokov, K. P. ; Karpenkov, D. Yu. ; Gutfleisch, O.
Art des Eintrags: Bibliographie
Titel: Magnetic anisotropy ofSm2Fe17single crystals
Sprache: Englisch
Publikationsjahr: 12 Oktober 2016
Verlag: American Physical Society
Titel der Zeitschrift, Zeitung oder Schriftenreihe: Physical Review B
Jahrgang/Volume einer Zeitschrift: 94
(Heft-)Nummer: 14
DOI: 10.1103/PhysRevB.94.144413
Kurzbeschreibung (Abstract):

The previously accepted notion that the spontaneous magnetization of Sm2Fe17 lies in the basal plane of the crystal is true only approximately, and then only around room temperature. At low temperatures the magnetization, whose orientation is not fixed by the symmetry, is found to deviate from the basal plane by as much as 10 degrees. The threefold symmetry axis is a hard direction; to magnetize the crystal in this direction, a magnetic field of about 9 T is required. The hard-axis magnetization arrives at saturation discontinuously, by way of a first-order phase transition. The behavior is a general one for trigonal ferromagnets where K-1 < 0 and the leading trigonal anisotropy constant is nonzero, K-2' not equal 0. Although of universal occurrence, the first-order transition is only visible at low temperatures, where it is accompanied by a magnetization anomaly of sufficient size.

Fachbereich(e)/-gebiet(e): 11 Fachbereich Material- und Geowissenschaften > Materialwissenschaft > Fachgebiet Funktionale Materialien
11 Fachbereich Material- und Geowissenschaften > Materialwissenschaft
11 Fachbereich Material- und Geowissenschaften
Hinterlegungsdatum: 18 Nov 2016 10:07
Letzte Änderung: 18 Nov 2016 10:07
PPN:
Sponsoren: The financial support by the German federal state of Hessen through its excellence programme LOEWE "RESPONSE" is acknowledged.
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