A new polymorph of germanium

ORAL

Abstract

The behavior of germanium under high pressure has been studied for many decades using diamond-anvil cells (DACs). A series of metal-metal transitions has been observed after the initial transition to the metallic $\beta $-Sn structure at $\sim$10 GPa. More recently, evidence for the semiconductor-metal transition has also been reported from point loading (indentation) experiments. Particularly pure amorphous Ge as starting material can be reliably phase transformed. These transitions are not reversible however, and meta-stable crystalline phases can be recovered upon pressure release. In this study we report experimental evidence from both point loading and in-situ DAC experiments for a new polymorph of Ge with the r8 structure, the same as observed for silicon. In the point loading case, the final phases after unloading are characterized using Raman spectroscopy in conjunction with computations employing density functional theory. In the DAC case, in-situ X-ray diffraction using synchrotron radiation was employed. This combination of two such very different methods for pressure application yields a more comprehensive picture of the phase behavior of Ge.

Authors

  • Bianca Haberl

    Australian National University, Australia

  • Malcolm Guthrie

    Geophysical Laboratory, Washington, DC, USA, Geophysical Laboratory, Carnegie Institution of Washington, USA

  • Brett C. Johnson

    University of Melbourne, Australia

  • Guoyin Shen

    HP-CAT, Geophysical Laboratory, Carnegie Institution of Washington, USA, HPCAT, Geophysical Laboratory, Carnegie Institution of Washington, HPCAT, Carnegie Institution of Washington

  • Brad D. Malone

    Harvard University, USA

  • Marvin L. Cohen

    University of California-Berkeley, USA and Lawrence Berkeley National Laboratory, USA

  • Jim S. Williams

    Australian National University, Australia

  • Jodie E. Bradby

    Australian National University, Australia