Dipolar-Octupolar Ising Antiferromagnetism in SmTiO: A Moment Fragmentation Candidate
arXiv:1805.09472 · doi:10.1103/PhysRevB.98.100401
Abstract
Over the past two decades, the magnetic ground states of all rare earth titanate pyrochlores have been extensively studied, with the exception of SmTiO. This is, in large part, due to the very high absorption cross-section of naturally-occurring samarium, which renders neutron scattering infeasible. To combat this, we have grown a large, isotopically-enriched single crystal of SmTiO. Using inelastic neutron scattering, we determine that the crystal field ground state for Sm is a dipolar-octupolar doublet with Ising anisotropy. Neutron diffraction experiments reveal that SmTiO orders into the all-in, all-out magnetic structure with an ordered moment of 0.44(7) below K, consistent with expectations for antiferromagnetically-coupled Ising spins on the pyrochlore lattice. Zero-field muon spin relaxation measurements reveal an absence of spontaneous oscillations and persistent spin fluctuations down to 0.03 K. The combination of the dipolar-octupolar nature of the Sm moment, the all-in, all-out ordered state, and the low-temperature persistent spin dynamics make this material an intriguing candidate for moment fragmentation physics.
arXiv comment5 pages, 4 figures. Supplemental Material
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