High‐Entropy Magnetism of Murunskite

Abstract Murunskite (K 2 FeCu 3 S 4 ) bridges the two known families of high‐temperature superconductors, cuprates and iron‐pnictides, structurally and electronically. Like these families, murunskite exhibits an antiferromagnetic (AF)‐like response with an ordered phase below 97 K. The magnetic iron atoms are randomly distributed over one‐quarter of the sites in two‐dimensional planes, while the remaining sites are occupied by non‐magnetic copper, evoking the notion of a high‐entropy magnetic alloy. This intriguing magnetic transition is studied by neutron, Mössbauer, and X‐ray photoelectron spectroscopy (XPS) measurements on single crystals. The AF order has a nearly commensurate quarterzone wave vector. In the paramagnetic state, Mössbauer spectroscopy identifies two iron sites, associated with Fe 3 + or Fe 2 + oxidation states as observed by XPS, which merge into a third site upon cooling, indicating an orbital transition. This cascade of local transitions transforms iron atoms from a fully orbitally and magnetically disordered state to a homogeneously ordered state in inverse space, while still being randomly distributed in real space. This finding challenges the traditional paradigm of magnetism in insulators, which relies on a direct connection between crystal structure and the location of magnetic moments.

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Publication Details

Journal
Advanced Functional Materials
Published
2025-05-02
DOI
https://doi.org/10.1002/adfm.202500099
Citations
3
Primary Topic
High-pressure geophysics and materials
Type
article
Field-Weighted Citation Impact
5.60

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High‐Entropy Magnetism of Murunskite

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article

High‐Entropy Magnetism of Murunskite

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article en
3 citations

Abstract

Abstract Murunskite (K 2 FeCu 3 S 4 ) bridges the two known families of high‐temperature superconductors, cuprates and iron‐pnictides, structurally and electronically. Like these families, murunskite exhibits an antiferromagnetic (AF)‐like response with an ordered phase below 97 K. The magnetic iron atoms are randomly distributed over one‐quarter of the sites in two‐dimensional planes, while the remaining sites are occupied by non‐magnetic copper, evoking the notion of a high‐entropy magnetic alloy. This intriguing magnetic transition is studied by neutron, Mössbauer, and X‐ray photoelectron spectroscopy (XPS) measurements on single crystals. The AF order has a nearly commensurate quarterzone wave vector. In the paramagnetic state, Mössbauer spectroscopy identifies two iron sites, associated with Fe 3 + or Fe 2 + oxidation states as observed by XPS, which merge into a third site upon cooling, indicating an orbital transition. This cascade of local transitions transforms iron atoms from a fully orbitally and magnetically disordered state to a homogeneously ordered state in inverse space, while still being randomly distributed in real space. This finding challenges the traditional paradigm of magnetism in insulators, which relies on a direct connection between crystal structure and the location of magnetic moments.

Advanced Functional MaterialsVol. 35(40)
University of Notre Dame (US), Agency for Science, Technology and Research (SG), Jagiellonian University (PL), Johns Hopkins University (US), TU Wien (AT), University of Zagreb (HR), University of Zurich (CH), Paul Scherrer Institute (CH), Institute of Nuclear Physics, Polish Academy of Sciences (PL), Institut Laue-Langevin (FR), Ruđer Bošković Institute (HR), École Polytechnique Fédérale de Lausanne (CH), AGH University of Krakow (PL)
National Science Foundation, Technische Universitat Wien, Sveučilište u Zagrebu, European Commission, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, Austrian Science Fund, Narodowym Centrum Nauki, Hrvatska Zaklada za Znanost, Narodowa Agencja Wymiany Akademickiej, Direktion für Entwicklung und Zusammenarbeit, European Regional Development Fund
Openalex Percentile: Top 5%
High-pressure geophysics and materials
5.60
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