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dc.creatorREGUERA, B. Y E.-
dc.creatorYEE-MADEIRA, H.-
dc.creatorDEMESHKO, S.-
dc.creatorECKOLD, G.-
dc.creatorJIMENEZ GALLEGOS, J.-
dc.date2012-03-27T01:48:05Z-
dc.date2012-03-27T01:48:05Z-
dc.date2009-
dc.date.accessioned2013-01-16T11:53:37Z-
dc.date.available2013-01-16T11:53:37Z-
dc.date.issued2013-01-16-
dc.identifierZ. Phys. Chem. 223 (2009) 701–711-
dc.identifierhttp://hdl.handle.net/123456789/531-
dc.identifier.urihttp://www.repositoriodigital.ipn.mx/handle/123456789/11018-
dc.descriptionThe material under study belongs to the Prussian blue analogues family, which are coordination compounds with a porous framework appropriate for the storage of small molecules, among them hydrogen. The porous framework results from systematic vacancies for the octahedral building block, [M(CN)6], in a 3D structure. Mössbauer spectroscopy is a powerful tool to obtain structural information on the local environment for the iron nucleus in these materials. Mössbauer spectra of iron (2+) hexacyanometallates (III) show two slightly asymmetric quadrupole splitting doublets. These two doublets correspond to two non-equivalent structural sites for the iron atom in the framework related with a non-random vacancy distribution. The observed asymmetry was ascribed to a vibrational anisotropy for these iron sites. The asymmetry decreases on the sample cooling and for 7 K it practically disappears. The iron atom is found at the cavities surface with a mixed coordination sphere, Fe(NC)6–x(H2O)x. Such anisotropic coordination environment could explain the presence of certain vibrational anisotropy detected as asymmetric quadrupole splitting doublets.-
dc.languageen-
dc.publisherZ. Phys. Chem.-
dc.titleNature of the Observed Asymmetry in Mössbauer Spectra of Iron (2+) Hexacyanometallates (III)-
dc.typeArticle-
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