Combined experimental and computational study of oxide ion conduction dynamics in Sr2Fe2O5 brownmillerite
dc.contributor.author | Auckett, JE | en_AU |
dc.contributor.author | Studer, AJ | en_AU |
dc.contributor.author | Pellegrini, E | en_AU |
dc.contributor.author | Ollivier, J | en_AU |
dc.contributor.author | Johnson, MR | en_AU |
dc.contributor.author | Schober, H | en_AU |
dc.contributor.author | Miiller, W | en_AU |
dc.contributor.author | Ling, CD | en_AU |
dc.date.accessioned | 2014-04-22T04:08:45Z | en_AU |
dc.date.available | 2014-04-22T04:08:45Z | en_AU |
dc.date.issued | 2013-08-13 | en_AU |
dc.date.statistics | 2014-04-23 | en_AU |
dc.description.abstract | We report a detailed study of the dynamics of oxide ionic conduction in brownmillerite-type Sr2Fe2O5, including lattice anisotropy, based on neutron scattering studies of a large (partially twinned) single crystal in combination with ab initio molecular dynamics simulations. Single-crystal diffraction reveals supercell peaks due to long-range ordering among chains of corner-sharing FeO4 tetrahedra, which disappears on heating above 540 °C due to confined local rotations of tetrahedra. Our simulations show that these rotations are essentially isotropic, but are a precondition for the anisotropic motion that moves oxide ions into the tetrahedral layers from the octahedral layers, which we observe experimentally as a Lorentzian broadening of the quasielastic neutron scattering spectrum. This continual but incoherent movement of oxide ions in turn creates conduction pathways and activates long-range diffusion at the interface between layers, which appears to be largely isotropic in two dimensions, in contrast with previously proposed mechanisms that suggest diffusion occurs preferentially along the c axis.© 2013, American Chemical Society. | en_AU |
dc.identifier.citation | Auckett, J.E., Studer, A.J., Pellegrini, E., Ollivier, J., Johnson, M.R., Schober, H., Miiller, W., & Ling, C.D. (2013). Combined experimental and computational study of oxide ion conduction dynamics in Sr2Fe2O5 brownmillerite. Chemistry of Materials, 25(15), 3080-3087. doi:10.1021/cm401278m | en_AU |
dc.identifier.govdoc | 5448 | en_AU |
dc.identifier.issn | 0897-4756 | en_AU |
dc.identifier.issue | 15 | en_AU |
dc.identifier.journaltitle | Chemistry of Materials | en_AU |
dc.identifier.pagination | 3080-3087 | en_AU |
dc.identifier.uri | http://dx.doi.org/10.1021/cm401278m | en_AU |
dc.identifier.uri | http://apo.ansto.gov.au/dspace/handle/10238/5462 | en_AU |
dc.identifier.volume | 25 | en_AU |
dc.language.iso | en | en_AU |
dc.publisher | American Chemical Society | en_AU |
dc.subject | Oxides | en_AU |
dc.subject | Ionic conductivity | en_AU |
dc.subject | Scattering | en_AU |
dc.subject | Simulation | en_AU |
dc.subject | Crystals | en_AU |
dc.subject | Ions | en_AU |
dc.title | Combined experimental and computational study of oxide ion conduction dynamics in Sr2Fe2O5 brownmillerite | en_AU |
dc.type | Journal Article | en_AU |
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