2D to 3D Magnetism in Synthetic Micas

Fe-based mica minerals usually display two opposing magnetic ground states, either they behave as spin-glasses or as layered ferrimagnets. No definite reason has been proposed as an explanation for this duality. This conundrum is unraveled by comparing the synthetic micas KFe<sub>3</sub>[MGe<sub>3</sub>]O<sub>10</sub>X<sub>2</sub> with M═Fe and Ga, X═OH<sup>-</sup> and F<sup>-</sup>. Neutron diffraction demonstrates a 2D to 3D magnetic transition in KFe<sub>3</sub>[FeGe<sub>3</sub>]O<sub>10</sub>(OH)<sub>2</sub> while just hints or no order at all are observed for the fluorides with M═Fe and Ga respectively. The 3D transition is triggered by the presence of iron in the intralayer tetrahedra. DFT+U calculations show that the magnetic exchange couplings between the previously believed solely magnetic octahedral layers would otherwise be frustrated without this intralayer iron.

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Publication Details

Journal
Advanced Science
Published
2024-09-20
DOI
https://doi.org/10.1002/advs.202408266
Citations
1
Primary Topic
Advanced Condensed Matter Physics
Type
article
Field-Weighted Citation Impact
0.31

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article

2D to 3D Magnetism in Synthetic Micas

Óscar Fabelo, Claire Minaud, Olivier Mentré, C. Ritter et al.
1 citations
Advanced Science
Advanced Condensed Matter Physics
0.31
article

2D to 3D Magnetism in Synthetic Micas

Óscar Fabelo, Claire Minaud, Olivier Mentré, C. Ritter, Ángel M. Arévalo‐López, J.L. Rosas-Huerta, Jonas Wolber
article en
1 citations

Abstract

Fe-based mica minerals usually display two opposing magnetic ground states, either they behave as spin-glasses or as layered ferrimagnets. No definite reason has been proposed as an explanation for this duality. This conundrum is unraveled by comparing the synthetic micas KFe<sub>3</sub>[MGe<sub>3</sub>]O<sub>10</sub>X<sub>2</sub> with M═Fe and Ga, X═OH<sup>-</sup> and F<sup>-</sup>. Neutron diffraction demonstrates a 2D to 3D magnetic transition in KFe<sub>3</sub>[FeGe<sub>3</sub>]O<sub>10</sub>(OH)<sub>2</sub> while just hints or no order at all are observed for the fluorides with M═Fe and Ga respectively. The 3D transition is triggered by the presence of iron in the intralayer tetrahedra. DFT+U calculations show that the magnetic exchange couplings between the previously believed solely magnetic octahedral layers would otherwise be frustrated without this intralayer iron.

Advanced ScienceVol. 11(42)
Rutherford Appleton Laboratory (GB), Centre National de la Recherche Scientifique (FR), École Nationale Supérieure de Chimie de Lille (FR), Université de Lille (FR), Research Complex at Harwell (GB), Institut Laue-Langevin (FR), Unité de catalyse et de chimie du solide de Lille (FR), École Centrale de Lille (FR)
Secretaría de Educación Pública, Indo-French Centre for the Promotion of Advanced Research, Secretaría de Estado de Ciencia, Tecnología e Innovación, Institut Chevreul
Openalex Percentile: Top 43%
Advanced Condensed Matter Physics
0.31
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2D to 3D Magnetism in Synthetic Micas — Óscar Fabelo, Claire Minaud, et al. · Advanced Science (2024) | TGRS Research Map | TGRS