Folio Bioscience, clinical sample procurement  Sign up for PNAS Online eTocs
Link: Info for AuthorsLink: Editorial BoardLink: AboutLink: SubscribeLink: AdvertiseLink: ContactLink: Sitemap Link: PNAS Home
Proceedings of the National Academy of Sciences
Link: Current Issue "" Link: Archives "" Link: Online Submission ""  Link: Advanced Search

Published online on May 1, 2008, 10.1073/pnas.0711925105
PNAS | May 6, 2008 | vol. 105 | no. 18 | 6526-6530


This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Supporting Information
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a colleague
Right arrow Similar articles in this journal
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Add to My File Cabinet
Right arrow Download to citation manager
Right arrow Request Copyright Permission
Citing Articles
Right arrow Citing Articles via CrossRef
Google Scholar
Right arrow Articles by Umemoto, K.
Right arrow Articles by Wentzcovitch, R. M.
PubMed
Right arrow PubMed Citation
Right arrow Articles by Umemoto, K.
Right arrow Articles by Wentzcovitch, R. M.
Social Bookmarking
 Add to CiteULike   Add to Complore   Add to Connotea   Add to Del.icio.us   Add to Digg  
What's this?

 Previous Article  | Table of Contents |  Next Article 

PHYSICAL SCIENCES / GEOPHYSICS
Prediction of an U2S3-type polymorph of Al2O3 at 3.7 Mbar

Koichiro Umemoto* and Renata M. Wentzcovitch

Minnesota Supercomputing Institute and Department of Chemical Engineering and Materials Science, University of Minnesota, 421 Washington Avenue SE, Minneapolis, MN 55455

Edited by Ho-kwang Mao, Carnegie Institution of Washington, Washington, DC, and approved February 27, 2008 (received for review December 18, 2007)

We predict by first principles a phase transition in alumina at {approx}3.7 Mbar and room temperature from the CaIrO3-type polymorph to another with the U2S3-type structure. Because alumina is used as window material in shock-wave experiments, this transformation should be important for the analysis of shock data in this pressure range. Comparison of our results on all high-pressure phases of alumina with shock data suggests the presence of two phase transitions in shock experiments: the corundum to Rh2O3(II)-type structure and the Rh2O3(II)-type to CaIrO3-type structure. The transformation to the U2S3-type polymorph is in the pressure range reached in the mantle of recently discovered terrestrial exoplanets and suggests that the multi-megabar crystal chemistry of planet-forming minerals might be related to that of the rare-earth sulfides.

alumina | first-principles calculation | high-pressure phase transition | postperovskite | rare-earth sulfide structure


Author contributions: K.U. designed research; K.U. performed research; K.U. and R.M.W. analyzed data; and K.U. and R.M.W. 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/0711925105/DCSupplemental.

{dagger} The NdYbS3-type structure was first reported to have the B2212 symmetry which is a subgroup of the Cmcm group of the CaIrO3-type structure (42, 43). However the NdYbS3-type structure refined in the B2212 symmetry is nearly indistinguishable from the CaIrO3-type structure. The difference between them is very tiny; in the B2212 NdYbS3-type structure, the cation at the B site and one kind of sulfur are just slightly shifted from the 4a and 8f Wyckoff positions in the Cmcm CaIrO3-type structure. A recent x-ray diffraction study suggested the NdYbS3-type structure should have the Cmcm symmetry and be the same as the CaIrO3-type structure (44).

*To whom correspondence should be addressed. E-mail: umemoto{at}cems.umn.edu

© 2008 by The National Academy of Sciences of the USA


Add to CiteULike CiteULike   Add to Complore Complore   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us   Add to Digg Digg    What's this?