We describe magnetization measurements on the heavy rare earth titanate pyrochlores R2Ti2O7, where R = Gd, Dy, Ho, Er, Yb, in the temperature range 1.8-300 K, and the field range 0-70000 Oe. In these materials magnetism arises from the rare earth ions, while Ti is non-magnetic. Analysis of the low field susceptibility versus temperature curves shows that Gd2Ti2O7 has antiferromagnetic coupling (θ ≈ -9 K), which suggests that it is an example of a frustrated antiferromagnet on the pyrochlore lattice. Er2Ti2O7 is likewise found to have a large negative Curie-Weiss temperature, θ ≈ -22 K, which we argue is indicative of antiferromagnetic coupling. Ho2Ti2O7, Dy2Ti2O7 and Yb2Ti2O7 are found to have weak ferromagnetic coupling (θ ≈ 2K, l K and 1 K respectively) which may be largely dipolar in origin. Fitting of the high field magnetization versus field curves suggests a strong (1, 1, 1) single ion anisotropy that identifies these three materials as possible realizations of the ferromagnetic 'spin ice' model.
CITATION STYLE
Bramwell, S. T., Field, M. N., Harris, M. J., & Parkin, I. P. (2000). Bulk magnetization of the heavy rare earth titanate pyrochlores - A series of model frustrated magnets. Journal of Physics Condensed Matter, 12(4), 483–495. https://doi.org/10.1088/0953-8984/12/4/308
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