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dc.contributor.authorMellini, Marcello
dc.contributor.authorWeiss, Zdeněk
dc.contributor.authorRieder, Milan
dc.contributor.authorDrábek, Milan
dc.date.accessioned2007-09-13T08:53:18Z
dc.date.available2007-09-13T08:53:18Z
dc.date.issued1996
dc.identifier.citationEuropean Journal of Mineralogy. 1996, vol. 8, no. 6, p. 1265-1271.en
dc.identifier.issn0935-1221
dc.identifier.urihttp://hdl.handle.net/10084/62759
dc.language.isoenen
dc.publisherE. Schweizerbart'sche Verlagsbuchhandlungen
dc.relation.ispartofseriesEuropean Journal of Mineralogyen
dc.relation.urihttps://dx.doi.org/10.1127/ejm/8/6/1265en
dc.subjectCs-ferrianniteen
dc.subjectcrystal structureen
dc.subjectcation orderingen
dc.subjectbond strengthen
dc.subjectradwasteen
dc.titleCs-ferriannite as a possible host for waste cesium: crystal structure and synthesisen
dc.typearticleen
dc.identifier.locationNení ve fondu ÚKen
dc.description.abstract-enCs-ferriannite, ideally CsFe32+ (Fe3+Si3)O-10(OH)(2), was synthesized as euhedral crystals, starting from an oxide mix, at 550 degrees C and 0.1 GPa water pressure. Using 860 independent reflections, the crystal structure of its 1M polytype was refined in the C2/m space group with R equal to 5.5%. All octahedral positions as well as 23% tetrahedral positions are occupied by iron. Its octahedral sheet is geometrically homooctahedral with all octahedra the same in size. The tetrahedral and octahedral sheets are nearly undistorted. Cs-ferriannite is the 1M mica with the largest unit cell known to date: a = 5.487(1) Angstrom, b = 9.506(2) Angstrom, c = 10.826(6) Angstrom, beta = 99.83(3)degrees, Z = 2. The mica appears to be a stable crystalline phase that may serve for fixation and storage of radioactive cesium isotopes in its interlayer.en
dc.identifier.doi10.1127/ejm/8/6/1265
dc.identifier.wosA1996WB92300005


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