Magnetic anisotropy of the spin-ice compound Dy2Ti2O7
By H. Fukazawa, Roger G. Melko, R. Higashinaka, Y. Maeno, Michel J. P. Gingras. 2001
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We report magnetization and ac susceptibility of single crystals of the spin-ice compound ${\mathrm{Dy}}_{2}{\mathrm{Ti}}_{2}{\mathrm{O}}_{7}.$ 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.
Subfields: Condensed Matter Physics, Electronic, Optical and Magnetic Materials
View Paper: https://www.semanticscholar.org/paper/b3e1ab239c5b1e9947ae36c8831e02b416b80764
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In Condensed Matter Physics
In Electronic, Optical and Magnetic Materials
Citations in the corpus
- Magnetic Pyrochlore Oxides (2009, background): “Measurements of the AC magnetic susceptibility χ(ω) of Dy2Ti2O7 down to 60 mK (Fukazawa et al., 2002a) and 100 mK (Matsuhira et al., 2001) find that the real part of χ, χ′, drops precipitously below a temperature of roughly 1 K for a frequency of the order of 10 Hz (see Fig.”