Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
American Mineralogist Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

American Mineralogist; April; v. 94; no. 4; p. 461-466; DOI: 10.2138/am.2009.3071
© 2009 Mineralogical Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
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 friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Yu, Y. G.
Right arrow Articles by Wentzcovitch, R. M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Low-pressure clino- to high-pressure clinoenstatite phase transition: A phonon-related mechanism

Yonggang G. Yu1,* and Renata M. Wentzcovitch2,{dagger}

1 Department of Chemistry, Minnesota Supercomputing Institute, University of Minnesota, Minneapolis, Minnesota 55455, U.S.A.
2 Department of Chemical Engineering and Materials Sciences, Minnesota Supercomputing Institute, University of Minnesota, Minneapolis, Minnesota 55455, U.S.A.

Correspondence: {dagger} E-mail: wentzcov{at}cems.umn.edu

We have investigated by first principles the compressional behavior of low-pressure (LP) and high-pressure (HP) MgSiO3 clinoenstatite. We have carefully examined unit-cell shapes, chain angles, and polyhedral volume responses, such as angle variances and quasi-elongations, under pressure at room temperature. We have observed opposite behavior of the tetrahedra in the S-rotated and O-rotated chains with pressure in the LP phase, with a slight increase (decrease) in angle variance and quasi-elongation in the former (latter). Inspection of zone center modes of both phases under pressure reveals a transition path that converts the S-rotated chain in the LP phase into the O-rotated chain in the HP phase. This conversion is related to a slight softening of an Ag "metastable" Raman mode under pressure.

Key Words: Phase transition mechanism • low-pressure clinoenstatite • high-pressure clinoenstatite • Raman • IR • phonon frequency







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Mineralogical Society of America