Ikeda Osamu, Yamamoto Hajime, Sano-Furukawa Asami, Sakamaki Tatsuya, Kuribayashi Takahiro, Noda Yukio, Suzuki Akio
Department of Earth Science, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan.
Institute of Multidisciplinary Research for Advanced Materials, Tohoku University, Sendai 980-8577, Japan.
J Am Chem Soc. 2025 Feb 5;147(5):4005-4016. doi: 10.1021/jacs.4c11982. Epub 2025 Jan 23.
The compression behavior of iron oxyhydroxide ε-FeOOH is complex, with variations in its magnetic property and bonding character. In this study, in situ powder neutron diffraction experiments were conducted on ε-FeOOH and ε-FeOOD up to pressures exceeding 20 GPa to investigate a spin-reorientation (spin-flop) transition, hydrogen-bond (H-bond) symmetrization, and their correlation. The magnetic transition was observed at 8 GPa in both ε-FeOOH and ε-FeOOD. The Fe-spins aligned in an A-type antiferromagnetic order and reoriented from the -direction to the -direction above 8 GPa. The crystal symmetry and H-bonds of ε-FeOOH transitioned from 2 with asymmetric H-bonds to with disordered H-bonds at 17.90 GPa, while ε-FeOOD remained asymmetric. The pressure evolution of the interatomic angles and distances indicates that the coordinate geometry of Fe transitioned toward H-bond symmetrization and would have affected the magnetic anisotropy. This study provides insights into the pressure effect of the magnetic transition on compounds containing hydrogen bonds.
羟基氧化铁ε-FeOOH的压缩行为很复杂,其磁性和键合特性会发生变化。在本研究中,对ε-FeOOH和ε-FeOOD进行了原位粉末中子衍射实验,压力超过20 GPa,以研究自旋重取向(自旋翻转)转变、氢键(H键)对称化及其相关性。在ε-FeOOH和ε-FeOOD中均在8 GPa处观察到磁性转变。Fe自旋以A型反铁磁顺序排列,并在8 GPa以上从-方向重新取向至-方向。ε-FeOOH的晶体对称性和H键在17.90 GPa时从具有不对称H键的2转变为具有无序H键的,而ε-FeOOD保持不对称。原子间角度和距离的压力演化表明,Fe的配位几何向H键对称化转变,这可能影响了磁各向异性。本研究为含氢键化合物中磁性转变的压力效应提供了见解。