Quantum paramagnetism in a non-Kramers rare-earth oxide: Monoclinic
arXiv:2211.06758 · doi:10.1103/PhysRevMaterials.7.063401
Abstract
Little is so far known about the magnetism of the monoclinic layered perovskites that replace the spin-ice supporting pyrochlore structure for . We show that high quality monoclinic PrTiO single crystals with a three-dimensional network of non-Kramers Pr ions that interact through edge-sharing super-exchange interactions, form a singlet ground state quantum paramagnet that does not undergo any magnetic phase transitions down to at least 1.8 K. The chemical phase stability, structure, and magnetic properties of the layered perovskite PrTiO were investigated using x-ray diffraction, transmission electron microscopy, and magnetization measurements. Synthesis of polycrystalline samples with the nominal compositions of PrTiO () showed that deviations from the PrTiO stoichiometry lead to secondary phases of related, structures including the perovskite phase PrTiO and the orthorhombic phases PrTiO and PrTiO. No indications of site disordering (stuffing and anti-stuffing) or vacancy defects were observed in the PrTiO majority phase. A procedure for growth of high-structural-quality, stoichiometric single crystals of PrTiO by the traveling solvent floating zone (TSFZ) method is reported. Thermo-magnetic measurements of single-crystalline PrTiO reveal an isolated singlet ground state that we associate with the low symmetry crystal electric field environments that split the -fold degenerate spin-orbital multiplets of the four differently coordinated Pr ions into 36 isolated singlets resulting in an anisotropic temperature independent van-Vleck susceptibility at low . A small isotropic Curie term is associated with 0.96(2)\% non-interacting Pr impurities.
18 pages, 7 figures, 6 tables
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