Prediction of Fe2P-type TiTe2 under pressure

Kai Hu, Jichun Lian, Li Zhu, Qinjun Chen, and Sheng-Yi Xie
Phys. Rev. B 101, 134109 – Published 17 April 2020

Abstract

Fe2P-type dioxides are significant both for geoscience and condensed-matter physics. For example, Fe2P-type SiO2 has been proposed to be one of the dominant components in the mantles of super-Earths and Fe2P-type TiO2 has been shown to have a large visible absorbance. Here we report the discovery of an Fe2P-type phase in a typical transition-metal dichalcogenide (TMD), TiTe2, using crystal structure prediction and first-principles calculations. Ambient layered TiTe2 will first transform to a monoclinic C2/m phase and then finally to the hexagonal Fe2P-type phase above 33 GPa. Fe2P-type TiTe2 is predicted to be metallic, contrasting with the semiconductivity of Fe2P-type TiO2. The same high-pressure phase (Fe2P type) appears both in transition-metal dioxides and TMDs, indicating that the stacking patterns of anions and cations play an increasingly important role in determining the high-pressure phase.

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  • Received 13 December 2019
  • Revised 12 March 2020
  • Accepted 25 March 2020

DOI:https://doi.org/10.1103/PhysRevB.101.134109

©2020 American Physical Society

Physics Subject Headings (PhySH)

Condensed Matter, Materials & Applied Physics

Authors & Affiliations

Kai Hu1, Jichun Lian1, Li Zhu2, Qinjun Chen1,*, and Sheng-Yi Xie1,†

  • 1School of Physics and Electronics, Hunan University, Changsha, 410082, China
  • 2Geophysical Laboratory, Carnegie Institution for Science, Washington, DC 20015, USA

  • *chenqj@hnu.edu.cn
  • shengyi_xie@hnu.edu.cn

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Issue

Vol. 101, Iss. 13 — 1 April 2020

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