High-pressure polymeric phases of carbon dioxide
- Jian Suna,b,1,
- Dennis D. Kluga,
- Roman Martoňákc,d,
- Javier Antonio Montoyad,e,f,
- Mal-Soon Leef,
- Sandro Scandolof,g and
- Erio Tosattid,f,g
- aSteacie Institute for Molecular Sciences, National Research Council of Canada, Ottawa, K1A 0R6, Canada;
- bLehrstuhl für Theoretische Chemie, Ruhr-Universität Bochum, 44780 Bochum, Germany;
- cDepartment of Experimental Physics, Comenius University, Mlynská dolina F2, 842 48 Bratislava, Slovakia;
- dInternational School for Advanced Studies, Trieste, Italy;
- eGeophysical Laboratory, Carnegie Institution of Washington DC, Washington, DC, 20015;
- fThe Abdus Salam International Centre for Theoretical Physics, Trieste, Italy; and
- gIstituto Nazionale di Fisica della Materia, Consiglio Nazionale delle Ricerche “Democritos” National Simulation Center, Trieste, Italy
-
Edited by Russell J. Hemley, Carnegie Institution of Washington, Washington, DC, and approved February 24, 2009 (received for review December 11, 2008)
Abstract
Understanding the structural transformations of solid CO2 from a molecular solid characterized by weak intermolecular bonding to a 3-dimensional network solid at high pressure has challenged researchers for the past decade. We employ the recently developed metadynamics method combined with ab initio calculations to provide fundamental insight into recent experimental reports on carbon dioxide in the 60–80 GPa pressure region. Pressure-induced polymeric phases and their transformation mechanisms are found. Metadynamics simulations starting from the CO2-II (P42/mnm) at 60 GPa and 600 K proceed via an intermediate, partially polymerized phase, and finally yield a fully tetrahedral, layered structure (P-4m2). Based on the agreement between calculated and experimental Raman and X-ray patterns, the recently identified phase VI [Iota V, et al. (2007) Sixfold coordinated carbon dioxide VI. Nature Mat 6:34–38], assumed to be disordered stishovite-like, is instead interpreted as the result of an incomplete transformation of the molecular phase into a final layered structure. In addition, an α-cristobalite-like structure (P41212), is predicted to be formed from CO2-III (Cmca) via an intermediate Pbca structure at 80 GPa and low temperatures (<300 K). Defects in the crystals are frequently observed in the calculations at 300 K whereas at 500 to 700 K, CO2-III transforms to an amorphous form, consistent with experiment [Santoro M, et al. (2006) Amorphous silica-like carbon dioxide. Nature 441:857–860], but the simulation yields additional structural details for this disordered solid.
- solid CO2
- first-principles molecular dynamics
- metadynamics
- phase transition
- density functional theory
Footnotes
- 1To whom correspondence should be addressed. E-mail: jian.sun{at}theochem.rub.de
-
Author contributions: J.S., D.D.K., R.M., S.S., and E.T. designed research; J.S., R.M., J.A.M., and M.-S.L. performed research; J.S., D.D.K., R.M., J.A.M., M.-S.L., and S.S. analyzed data; and J.S., D.D.K., R.M., S.S., and E.T. wrote the paper.
-
The authors declare no conflict of interest.
-
This article is a PNAS Direct Submission.
-
This article contains supporting information online at www.pnas.org/cgi/content/full/0812624106/DCSupplemental.




