Observation of universal strong orbital-dependent correlation effects in iron chalcogenides

M. Yi, Z. K. Liu, Y. Zhang, R. Yu, J. X. Zhu, J. J. Lee, R. G. Moore, F. T. Schmitt, W. Li, S. C. Riggs, J. H. Chu, B. Lv, J. Hu, M. Hashimoto, S. K. Mo, Z. Hussain, Z. Q. Mao, C. W. Chu, I. R. Fisher, Q. SiZ. X. Shen, D. H. Lu

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Abstract

Establishing the appropriate theoretical framework for unconventional superconductivity in the iron-based materials requires correct understanding of both the electron correlation strength and the role of Fermi surfaces. This fundamental issue becomes especially relevant with the discovery of the iron chalcogenide superconductors. Here, we use angle-resolved photoemission spectroscopy to measure three representative iron chalcogenides, FeTe 0.56 Se 0.44, monolayer FeSe grown on SrTiO3 and K0.76 Fe1.72 Se2. We show that these superconductors are all strongly correlated, with an orbital-selective strong renormalization in the d xy bands despite having drastically different Fermi surface topologies. Furthermore, raising temperature brings all three compounds from a metallic state to a phase where the dxy orbital loses all spectral weight while other orbitals remain itinerant. These observations establish that iron chalcogenides display universal orbital-selective strong correlations that are insensitive to the Fermi surface topology, and are close to an orbital-selective Mott phase, hence placing strong constraints for theoretical understanding of iron-based superconductors.

Original languageEnglish
Article number7777
JournalNature Communications
Volume6
DOIs
StatePublished - Jul 23 2015
Externally publishedYes

Funding

ARPES experiments were performed at the Stanford Synchrotron Radiation Lightsource and the Advanced Light Source, which are both operated by the Office of Basic Energy Sciences, U.S. Department of Energy. The Stanford work is supported by the US DOE, Office of Basic Energy Science, Division of Materials Science and Engineering, under award number DE-AC02-76SF00515. The work at Rice is supported by NSF Grant DMR-1309531 and the Robert A. Welch Foundation Grant No. C-1411. The work at Renmin University is supported by the National Science Foundation of China Grant number 11374361, and the Fundamental Research Funds for the Central Universities and the Research Funds of Remnin University of China. The work at Tulane is supported by the NSF under grant DMR-1205469. The work at Los Alamos was supported by the U.S. DOE Office of Basic Energy Sciences.

FundersFunder number
Division of Materials Science and EngineeringDE-AC02-76SF00515
Office of Basic Energy Science
Remnin University of ChinaDMR-1205469
Robert A. Welch Foundation
U.S. DOE Office of Basic Energy Sciences
National Science FoundationDMR-1309531
U.S. Department of Energy
Directorate for Mathematical and Physical Sciences1309531
National Natural Science Foundation of China11374361
Renmin University of China
Fundamental Research Funds for the Central Universities

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