Evolution of the nuclear and magnetic structures of TlFe1.6Se2 with temperature
Huibo Cao, Claudia Cantoni, Andrew F. May, Michael A. McGuire, Bryan, C. Chakoumakos, Stephen J. Pennycook, Radu Custelcean, Athena S. Sefat, and, Brian C. Sales

TL;DR
This study investigates how the nuclear and magnetic structures of TlFe$_{1.6}$Se$_2$ evolve with temperature, revealing changes in magnetic ordering, layer corrugation, and lattice parameters, with implications for magnetic-lattice coupling.
Contribution
It provides detailed temperature-dependent structural and magnetic data for TlFe$_{1.6}$Se$_2$, highlighting differences from alkali-metal counterparts and showing strong magneto-lattice interactions.
Findings
Magnetic structure transitions around 100-150 K.
Layer corrugation increases with temperature.
Magnetic and structural properties are strongly coupled.
Abstract
The evolution of the nuclear and magnetic structures of TlFeSe was determined in the temperature range of 5-450\,K using single crystal neutron diffraction. The Fe layers in these materials develop a corrugation in the magnetically ordered state. A canting away from the block checkerboard magnetic structure is observed in the narrow temperature range between approximately 100 and 150\,K. In this same temperature range, an increase in the corrugation of the Fe layers is observed. At lower temperatures, the block checkerboard magnetic structure is recovered with a suppressed magnetic moment and abrupt changes in the lattice parameters. Microstructure analysis at 300\,K using atomic-resolution Z-contrast scanning transmission electron microscopy reveals regions with ordered and disordered Fe vacancies, and the iron content is found to be uniform across the crystal. These…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
