Ultrahigh-pressure disordered eight-coordinated phase of Mg 2 GeO 4 : Analogue for super-Earth mantles

Author:

Dutta Rajkrishna12,Tracy Sally June1,Cohen R. E.1ORCID,Miozzi Francesca1ORCID,Luo Kai1ORCID,Yang Jing1,Burnley Pamela C.3,Smith Dean4,Meng Yue4,Chariton Stella5,Prakapenka Vitali B.5,Duffy Thomas S.2ORCID

Affiliation:

1. Earth and Planets Laboratory, Carnegie Institution for Science, Washington, DC 20015

2. Department of Geosciences, Princeton University, Princeton, NJ 08544

3. Department of Geoscience, University of Nevada, Las Vegas, NV 89154

4. High-Pressure Collaborative Access Team (HPCAT), X-Ray Science Division, Argonne National Laboratory, Argonne, IL 60439

5. Center for Advanced Radiation Sources, The University of Chicago, Chicago, IL 60637

Abstract

Significance This work presents experimental evidence for the formation of a phase with eightfold coordination of germanium by oxygen in Mg 2 GeO 4 , a well-known analogue of Mg 2 SiO 4 at extreme pressure and temperatures. Using both experiments and theoretical computations, we have determined the structure, equation of state, and phase stability of this phase at pressures above 200 GPa. The existence of this phase in the silicate counterpart may play an important role in the structure and dynamics of the deep interiors of large, rocky exoplanets.

Funder

Carnegie Institution of Washington

National Science Foundation

Gauss Centre for Supercomputing

Publisher

Proceedings of the National Academy of Sciences

Subject

Multidisciplinary

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