The low-temperature magnetic properties of the pyrochlore compound Dy 2 Ti 2 O 7 in magnetic fields applied along the [111] direction are reported. Below 1 K, a clear plateau has been observed in the magnetization process in the field range 2–9 kOe, followed by a sharp moment jump at around 10 kOe that corresponds to a breaking of the spin ice state. We found that the plateau state is disordered, with a residual entropy of nearly half the value for the zero-field state, whose macroscopic degeneracy comes from a frustration of the spins on the Kagomé layers perpendicular to the magnetic field.
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Matsuhira et al. (2002) studied this question.
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