New Journal of Physics (Jan 2024)

Bi-intercalated epitaxial graphene on SiC(0001)

  • Susanne Wolff,
  • Mark Hutter,
  • Philip Schädlich,
  • Hao Yin,
  • Monja Stettner,
  • Sabine Wenzel,
  • F Stefan Tautz,
  • François C Bocquet,
  • Thomas Seyller,
  • Christian Kumpf

DOI
https://doi.org/10.1088/1367-2630/ad7f7d
Journal volume & issue
Vol. 26, no. 10
p. 103009

Abstract

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The intercalation of graphene with suitable atomic species is one of the most frequently applied methods to decouple the graphene layer from the substrate in order to establish the classical electronic properties of graphene. In this context, we studied the bismuth (Bi) intercalation of the $\left(6\sqrt{3}\times6\sqrt{3}\right)R30^\circ$ reconstructed so-called ‘zeroth layer graphene’ on SiC $\left(0001\right)$ . As reported earlier by Sohn et al (2021 J. Korean Phys. Soc. 78 157) two phases are formed depending on the amount of intercalated Bi, which in turn is controlled by the annealing temperature: The α phase, showing a $(1\times1)$ periodicity with respect to the substrate, and, at higher temperatures, the $(\sqrt{3}\times\sqrt{3})$ reconstructed β phase. We characterise both phases and the transformation from the α to the β phase by photoelectron spectroscopy, normal incidence x-ray standing waves, electron diffraction and electron microscopy. We clearly see an almost complete intercalation of the graphene layers in both phases, with strong (covalent) interaction between the topmost Si atoms of the substrate and the Bi intercalant, but only weak (van der Waals) interaction between Bi and the graphene layer. The n-doping of the graphene found for the α phase decreases continuously during the phase transformation, in agreement with a reduced density of the Bi intercalating layer. Missing core level shifts of the surface species as well as the normal incidence x-ray standing waves results indicate that all surface Si atoms remain saturated during the transition and no dangling bonds are formed. Low energy electron microscopy and diffraction reveal the coexistance of both phases after annealing to intermediate temperatures and allow a quantitative analysis of island sizes and numbers.

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