Magnetic anisotropy of the spin-ice compound Dy2Ti2O7 -: art. no. 054410

被引:176
|
作者
Fukazawa, H [1 ]
Melko, RG
Higashinaka, R
Maeno, Y
Gingras, MJP
机构
[1] Kyoto Univ, Dept Phys, Kyoto 6068502, Japan
[2] Univ Waterloo, Dept Phys, Waterloo, ON N2L 3G1, Canada
[3] Kyoto Univ, Int Innovat Ctr, Kyoto 6068501, Japan
[4] Japan Sci & Technol Corp, CREST, Kawaguchi, Saitama 3320012, Japan
[5] Univ Waterloo, Dept Phys, Waterloo, ON N2L 3G1, Canada
[6] Canadian Inst Adv Res, Toronto, ON M5G 1Z8, Canada
关键词
D O I
10.1103/PhysRevB.65.054410
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
We report magnetization and ac susceptibility of single crystals of the spin-ice compound Dy2Ti2O7. Saturated moments at 1.8 K along the characteristic axes [100] and [110] agree with the expected values for an effective ferromagnetic nearest-neighbor Ising pyrochlore with local (111) anisotropy, where each magnetic moment is constrained to obey the "ice rule." At high enough magnetic fields along the [111] axis, the saturated moment exhibits a breaking of the ice rule; it agrees with the value expected for a three-in, one-out spin configuration. Assuming the realistic magnetic interaction between Dy ions given by the dipolar spin ice model, we completely reproduce the results at 2 K by Monte Carlo calculations. However, down to at least 60 mK, we have not found any experimental evidence of the long-range magnetic ordering predicted by this model to occur at around 180 mK. Instead, we confirm the spin freezing of the system below 0.5 K.
引用
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页码:1 / 6
页数:6
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