Discovery of the soft electronic modes of the trimeron order in magnetite

• Published in: Nature physics Vol. 16; no. 5; pp. 541 - 545
• Main Authors: Baldini, Edoardo, Belvin, Carina A., Rodriguez-Vega, Martin, Ozel, Ilkem Ozge, Legut, Dominik, Kozłowski, Andrzej, Oleś, Andrzej M., Parlinski, Krzysztof, Piekarz, Przemysław, Lorenzana, José, Fiete, Gregory A., Gedik, Nuh
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 01-05-2020; Nature Publishing Group; Nature Publishing Group (NPG)
• Subjects: 639/766/119/2795; 639/766/119/995; Atomic; Classical and Continuum Physics; Complex Systems; Condensed Matter Physics; Energy; Equilibrium; Excitation; Iron oxides; Lasers; Letter; Low temperature; Magnetite; Mathematical and Computational Physics; Metal-insulator transition; Molecular; Optical and Plasma Physics; Physics; Physics and Astronomy; Polarons; Signatures; Theoretical
• ISSN: 1745-2473; 1745-2481
• DOI: 10.1038/s41567-020-0823-y

The Verwey transition in magnetite (Fe
3
O
4
) is the first metal–insulator transition ever observed
1
and involves a concomitant structural rearrangement and charge–orbital ordering. Owing to the complex interplay of these intertwined degrees of freedom, a complete characterization of the low-temperature phase of magnetite and the mechanism driving the transition have long remained elusive. It was demonstrated in recent years that the fundamental building blocks of the charge-ordered structure are three-site small polarons called trimerons
2
. However, electronic collective modes of this trimeron order have not been detected to date, and thus an understanding of the dynamics of the Verwey transition from an electronic point of view is still lacking. Here, we discover spectroscopic signatures of the low-energy electronic excitations of the trimeron network using terahertz light. By driving these modes coherently with an ultrashort laser pulse, we reveal their critical softening and hence demonstrate their direct involvement in the Verwey transition. These findings shed new light on the cooperative mechanism at the origin of magnetite’s exotic ground state.
Spectroscopic study of the low-energy excitations in magnetite Fe
3
O
4
shows the signatures of its charge-ordered structure involved in the metal–insulator transition, whose building blocks are the three-site small polarons, termed trimerons.