Materials Today Advances (Aug 2023)

Structural, vibrational, and electronic behavior of two GaGeTe polytypes under compression

  • E. Bandiello,
  • S. Gallego-Parra,
  • A. Liang,
  • J.A. Sans,
  • V. Cuenca-Gotor,
  • E. Lora da Silva,
  • R. Vilaplana,
  • P. Rodríguez-Hernández,
  • A. Muñoz,
  • D. Diaz-Anichtchenko,
  • C. Popescu,
  • F.G. Alabarse,
  • C. Rudamas,
  • C. Drasar,
  • A. Segura,
  • D. Errandonea,
  • F.J. Manjón

Journal volume & issue
Vol. 19
p. 100403

Abstract

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GaGeTe is a layered topological semimetal that has been recently found to exist in at least two different polytypes, α-GaGeTe (R3¯m) and β-GaGeTe (P63mc). Here we report a joint experimental and theoretical study of the structural, vibrational, and electronic properties of these two polytypes in high-pressure conditions. Both polytypes show anisotropic compressibility and two phase transitions, above 7 and 15 GPa, respectively, as confirmed by XRD and Raman spectroscopy measurements. Although the nature of the high-pressure phases could not be confirmed, comparison with other chalcogenides and total-energy calculations allow us to propose possible high-pressure phases for both polytypes with an increase in coordination for Ga and Ge atoms from 4 to 6. In particular, the simplification of the X-ray pattern for both polytypes above 15 GPa suggests a transition to a structure of relatively higher symmetry than the original one. This result is consistent with the rocksalt-like high-pressure phases observed in parent III-VI semiconductors, such as GaTe, GaSe, and InSe. Pressure-induced amorphization is observed upon pressure release. The electronic band structures of α-GaGeTe and β-GaGeTe and their pressure dependence also show similarities to III-VI semiconductors, thus suggesting that the germanene-like sublayer induces a semimetallic character in both GaGeTe polytypes. Above 3 GPa, both polytypes lose their topological features, due to the opening of the direct band gap, while the reduction of the interlayer space increases the thermal conductivity at high pressure.