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Crystal structure of sinhalite MgAlBO4 under high pressure
Authors
A. L. J. Pereira
A. Muñoz
+50 more
Andrault D.
Birch F.
Blochl P. E.
C. Popescu
Capponi J. J.
Claringbull G. F.
D. Errandonea
D. Santamarı́a-Pérez
Downs R. T.
Errandonea D.
F. J. Manjón
Fang J. H.
Fauth F.
Finger L. W.
Hammersley A. P.
Hayward C. L.
Hazen R. M.
Hazen R. M.
Hyde B. G.
J. A. Sans
Katsura T.
Kiefer B.
Kresse G.
Kresse G.
Lumpkin G. R.
Mao H. K.
Mujica A.
Nolze G.
O. Gomis
P. Rodrı́guez-Hernández
Perdew J. P.
Recio J. M.
Robinson K.
Rodriguez-Carvajal J.
Santamaria-Perez D.
Santamaria-Perez D.
Santamaria-Perez D.
Santamaria-Perez D.
Sharp Z. D.
Smyth J. R.
Sung C. M.
Sung C. M.
Vegas A.
Vegas A.
Vegas A.
Vegas A.
Wentzcovitch R. M.
Werding G.
Yang H.
Zhang L.
Publication date
26 March 2015
Publisher
'American Chemical Society (ACS)'
Doi
Abstract
This document is the Accepted Manuscript version of a Published Work that appeared in final form in Journal of Physical Chemistry C, copyright © American Chemical Society after peer review and technical editing by the publisher. To access the final edited and published work see http://dx.doi.org/10.1021/jp512131eWe report on high-pressure angle-dispersive X-ray diffraction data up to 27 GPa for natural MgAlBO4 sinhalite mineral and ab initio total energy calculations. The experimental bulk modulus of sinhalite is B-0 = 171(3) GPa with a first-pressure derivative of B-0' = 4.2(3). A comparison with other olivine-type compounds shows that the value for B0 is 27% larger than that of Mg2SiO4 forsterite and 29% smaller than that of Al2BeO4 chrysoberyl. These differences are interpreted, on the basis of our ab initio calculations, in terms of the relative incompressibility of Al-O bonds in AlO6 octahedra (with a calculated bulk modulus of 250(1) GPa) as compared to Mg-O bonds in MgO6 octahedra (with a calculated bulk modulus of 130(1) GPa). The spatial cation distribution in the Pbnm orthorhombic unit cell and different polyhedral compressibilities entails a strong anisotropic compression comparable to that of forsterite. The axial compressibilities are 1.06(2) x 10(-3), 2.17(2) x 10(-3), and 1.30(3) x 10(-3) GPa(-1) for a, b, and c axes, respectively. The crystal chemistry of sinhalite under compression is compared to that of other olivine-like compounds. Compressibility trends and possible high-pressure phases are discussed.This study was supported by the Spanish government MEC under Grants No: MAT2010-21270-C04-01/03/04, MAT2013-46649-C4-1/2/3-P, and CTQ2009-14596-C02-01, by the Comunidad de Madrid and European Social Fund (S2009/PPQ1551 4161893), by MALTA Consolider Ingenio 2010 project (CSD2007-00045), and by Generalitat Valenciana (GVA-ACOMP-2013-1012 and GVA-ACOMP-2014-243). Experiments were performed at MSPD beamline at ALBA Synchrotron Light Facility with the collaboration of ALBA staff A.M. and P.R-H. acknowledge computing time provided by Red Espanola de Supercomputacion (RES) and MALTA-Cluster. J.A.S. acknowledges financial support through the Juan de la Cierva fellowship. We are particularly grateful to Angel Vegas for stimulating discussions and critical reading of this manuscript.Santamaría Pérez, D.; Errandonea, D.; Gomis, O.; Sans Tresserras, JÁ.; Pereira, ALJ.; Manjón Herrera, FJ.; Popescu, C.... (2015). Crystal structure of sinhalite MgAlBO4 under high pressure. Journal of Physical Chemistry C. 119(12):6777-6784. https://doi.org/10.1021/jp512131eS677767841191
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info:doi/10.1021%2Fjp512131e
Last time updated on 02/01/2020