Abstract
We report a comprehensive study on the magnetic ground state of combining single crystal neutron diffraction and resonant magnetic x-ray scattering at the edges. Three single-crystal samples obtained from the same boule were investigated exhibiting magnetic phase transitions from a high-temperature paramagnetic phase to an antiferromagnetic phase at . Single crystal neutron diffraction reveals that the crystal structure at room temperature shows an orthorhombic -centered lattice but with and axes almost equal in length. The structural phase transition (charge-ordering-like) from the parent tetragonal cell takes place above 523 K into the space group where two nonequivalent compressed and expanded octahedra are ordered showing a checkerboard pattern in the plane. The charge segregation between the nonequivalent Co sites is about 0.4(1) electrons. Resonant magnetic x-ray reflections indexed as , , and in the parent tetragonal cell were observed at low temperature at the -edge energy range. The resonant spectral shape, with a noticeable absence of any resonant enhancement at the edge, indicates that only -like ions participate in the magnetic ordering. The polarization analysis discloses that the orientation of Co magnetic moments is the same for the three magnetic orders and they are long-range ordered along the diagonal in the plane of the parent tetragonal cell with a slight tilt in the axis. Despite the onset temperatures for the three resonant magnetic reflections being the same, , different thermal behavior is observed between and () reflections whose intensities maximize at different temperatures, suggesting the coexistence of two magnetic arrangements. Moreover, the intensity of the magnetic reflection is at least ten times larger than that of the ones. On the other hand\, neutron diffraction measurements only detect a single type of antiferromagnetic ordering following the propagation vector that involves half of the Co atoms in the unit cell. We conclude that the bulk magnetic order in corresponds then to this propagation vector while and magnetic reflections correspond to a minority magnetic phase that must be due to changes in the oxygen stoichiometry near the surface.
2 More- Received 22 January 2021
- Revised 24 March 2021
- Accepted 5 May 2021
DOI:https://doi.org/10.1103/PhysRevB.103.184422
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