Zobrazit minimální záznam

dc.contributor.authorJaneba, Daniel
dc.contributor.authorČapková, Pavla
dc.contributor.authorWeiss, Zdeněk
dc.contributor.authorSchenk, Henk
dc.date.accessioned2007-08-21T12:37:46Z
dc.date.available2007-08-21T12:37:46Z
dc.date.issued1998
dc.identifier.citationEuropean Powder Diffraction 5 : Fifth European Powder Diffraction Conference (EPDIC 5), May 1997, Parma, Italy. Proceedings. 1998, p. 139-144. Materials science forum, vol. 278-281.en
dc.identifier.isbn0-87849-807-9
dc.identifier.issn0255-5476
dc.identifier.urihttp://hdl.handle.net/10084/62117
dc.language.isoenen
dc.publisherTrans Tech Publicationsen
dc.relation.ispartofseriesEuropean Powder Diffraction 5 : Fifth European Powder Diffraction Conference (EPDIC 5), May 1997, Parma, Italy. Proceedingsen
dc.subjectXRD profile analysisen
dc.subjectlayered structuresen
dc.subjectintercalatesen
dc.titleXRD profile analysis of clay mineralsen
dc.typearticleen
dc.identifier.locationNení ve fondu ÚKen
dc.description.abstract-enXRD profile analysis of smectites is usually limited to the apparent d-spacing estimated from the peak maxima from the raw data. This can lead to the wrong d-spacing and consequently to the wrong conclusions about mixed layering (interstratification) and wrong structural model of interlayer. The interference function is modulated by the angle dependent instrumental factors (Lorentz-polarization, diffraction geometry) and physical factors (structural factor, volume absorption, surface roughness absorption) which lead to profile distortions and to the shift of the peak maxima. This effect is especially significant at low diffraction angles and for broadened diffraction lines (FWHM>1 degrees). Present work deals with detailed analysis of these effects, their corrections and their consequences for the interpretation of diffraction patterns. The proposed methodology and effect of all corrections is shown on the example of montmorillonite intercalated with Al-hydroxy complexes.en
dc.identifier.wos000074945400022


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