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Magnetic anisotropy of the spin ice compound Dy2Ti2O7

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arxiv cond-mat/0108129 v1 pith:HJWF6CE5 submitted 2001-08-08 cond-mat.str-el cond-mat.stat-mech

Magnetic anisotropy of the spin ice compound Dy2Ti2O7

classification cond-mat.str-el cond-mat.stat-mech
keywords magneticspinalonganisotropycompounddy2ti2o7expectedice-rule
verification ladder T0 review T1 audit T2 compute T3 formal T4 reserved
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We report magnetization and ac susceptibility of single crystals of the spin ice compound Dy2Ti2O7. Saturated moments at 1.8 K along the charasteristic 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 beaking 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.

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