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Isostructural Second-Order Phase Transition of β-Bi2O3 at High Pressures: An Experimental and Theoretical Study
dc.contributor.author | Pereira, André L. J. | |
dc.contributor.author | Sans, Juan A. | |
dc.contributor.author | Villaplana, Rosario | |
dc.contributor.author | Gomis Hilario, Óscar | |
dc.contributor.author | Manjón, F. J. | |
dc.contributor.author | Rodríguez Hernández, P. | |
dc.contributor.author | Muñoz, Alfonso | |
dc.contributor.author | Popescu, Catalin | |
dc.contributor.author | Beltran, Armando | |
dc.date.accessioned | 2015-07-31T09:39:40Z | |
dc.date.available | 2015-07-31T09:39:40Z | |
dc.date.issued | 2014-09 | |
dc.identifier.citation | PEREIRA, A. L. J., et al. Isostructural Second-Order Phase Transition of β-Bi2O3 at High Pressures: An Experimental and Theoretical Study. The Journal of Physical Chemistry C, 2014, 118.40: 23189-23201. | ca_CA |
dc.identifier.uri | http://hdl.handle.net/10234/129805 | |
dc.description.abstract | We report a joint experimental and theoretical study of the structural and vibrational properties of synthetic sphaerobismoite (β-Bi2O3) at high pressures in which room-temperature angle-dispersive X-ray diffraction (XRD) and Raman scattering measurements have been complemented with ab initio total-energy and lattice dynamics calculations. Striking changes in Raman spectra were observed around 2 GPa, whereas X-ray diffraction measurements evidence no change in the tetragonal symmetry of the compound up to 20 GPa; however, a significant change exists in the compressibility when increasing pressure above 2 GPa. These features have been understood by means of theoretical calculations, which show that β-Bi2O3 undergoes a pressure-induced isostructural phase transition near 2 GPa. In the new isostructural β′ phase, the Bi3+ and O2– environments become more regular than those in the original β phase because of the strong decrease in the activity of the lone electron pair of Bi above 2 GPa. Raman measurements and theoretical calculations provide evidence of the second-order nature of the pressure-induced isostructural transition. Above 20 GPa, XRD measurements suggest a partial amorphization of the sample despite Raman measurements still show weak peaks, probably related to a new unknown phase, which remains up to 27 GPa. On pressure release, XRD patterns and Raman spectra below 2 GPa correspond to elemental Bi–I, thus evidencing a pressure-induced decomposition of the sample during downstroke. | ca_CA |
dc.format.extent | 12 p. | ca_CA |
dc.format.mimetype | application/pdf | ca_CA |
dc.language.iso | eng | ca_CA |
dc.publisher | American Chemical Society | ca_CA |
dc.relation.isPartOf | J. Phys. Chem. C, 2014, 118 (40) | ca_CA |
dc.rights | opyright © 2014 American Chemical Society | ca_CA |
dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | * |
dc.subject | high pressure | ca_CA |
dc.subject | isostructural | ca_CA |
dc.subject | second-order phase transition | ca_CA |
dc.subject | theoretical study | ca_CA |
dc.title | Isostructural Second-Order Phase Transition of β-Bi2O3 at High Pressures: An Experimental and Theoretical Study | ca_CA |
dc.type | info:eu-repo/semantics/article | ca_CA |
dc.identifier.doi | http://dx.doi.org/10.1021/jp507826j | |
dc.rights.accessRights | info:eu-repo/semantics/restrictedAccess | ca_CA |
dc.relation.publisherVersion | http://pubs.acs.org/doi/abs/10.1021/jp507826j | ca_CA |
dc.type.version | info:eu-repo/semantics/publishedVersion | ca_CA |
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