Dipolar-octupolar Ising antiferromagnetism in Sm2Ti2O7: A moment fragmentation candidate

C. Mauws, A. M. Hallas, G. Sala, A. A. Aczel, P. M. Sarte, J. Gaudet, D. Ziat, J. A. Quilliam, J. A. Lussier, M. Bieringer, H. D. Zhou, A. Wildes, M. B. Stone, D. Abernathy, G. M. Luke, B. D. Gaulin, C. R. Wiebe

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23 Scopus citations

Abstract

Over the past two decades, the magnetic ground states of all rare-earth titanate pyrochlores have been extensively studied, with the exception of Sm2Ti2O7. 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 Sm2Ti2O7. Using inelastic neutron scattering, we determine that the crystal field ground state for Sm3+ is a dipolar-octupolar doublet with Ising anisotropy. Neutron diffraction experiments reveal that Sm2Ti2O7 orders into the all-in, all-out magnetic structure with an ordered moment of 0.44(7)μB below TN=0.35 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 Sm3+ 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.

Original languageEnglish
Article number100401
JournalPhysical Review B
Volume98
Issue number10
DOIs
StatePublished - Sep 5 2018

Funding

This research was supported by NSERC of Canada. A portion of this research used resources at the High Flux Isotope Reactor and Spallation Neutron Source, a DOE Office of Science User Facility operated by the Oak Ridge National Laboratory. C.R.W. thanks the Canada Research Chair program (Tier II) and the CFI. C.M. thanks the Manitoba Government for support through the MGS. J.A.Q. acknowledges technical support from M. Lacerte and S. Fortier and funding from FRQNT and CFREF. G.S. thanks J. Lin and A. T. Savici for useful discussions, and support in the analysis. H.D.Z. acknowledges support from NSF DMR through Grant No. DMR-1350002. P.M.S. acknowledges financial support from the CCSF, the RSC and the University of Edinburgh through the GRS and PCDS.

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