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Origin of ARPES Dirac cones in TBTANG/Au(111) honeycomb–kagome COF

Determine whether the Dirac cone observed by angle-resolved photoemission spectroscopy in the mesoscale honeycomb–kagome covalent organic framework formed by tribromotrioxaazatriangulene (TBTANG) molecules on an Au(111) surface originates from the kagome sublattice or from the honeycomb sublattice, by attributing the measured Dirac dispersion to a specific lattice-derived band.

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Background

A mesoscale honeycomb–kagome lattice was grown from TBTANG molecules on Au(111) under UHV, where ARPES revealed both a Dirac cone and a flat band. Since honeycomb lattices can also generate Dirac cones, distinguishing whether the observed Dirac dispersion is due to the kagome part or the honeycomb part of the structure is essential for interpreting the band topology and for validating kagome-specific physics in this COF system.

References

A Dirac cone (Fig. 4b) and a flat band residing at 1.8 eV below the Fermi level were observed using ARPES [77]. However, since a honeycomb lattice also contributes Dirac cones, the exact origin of the experimental observed Dirac cones remains unclear.

Two-dimensional Kagome Materials: Theoretical Insights, Experimental Realizations, and Electronic Structures (2409.03214 - Zhang et al., 5 Sep 2024) in Section 3.1.4 (Kagome COF monolayers on metal–vacuum interfaces), page 15