Zobrazit minimální záznam

dc.contributor.authorSimha Martynková, Gražyna
dc.contributor.authorValášková, Marta
dc.contributor.authorŠupová, Monika
dc.date.accessioned2007-08-31T06:49:18Z
dc.date.available2007-08-31T06:49:18Z
dc.date.issued2007
dc.identifier.citationphysica status solidi (a). 2007, vol. 204, issue 6, p. 1870-1875.en
dc.identifier.issn0031-8965
dc.identifier.issn1521-396X
dc.identifier.urihttp://hdl.handle.net/10084/62386
dc.language.isoenen
dc.publisherWileyen
dc.relation.ispartofseriesphysica status solidi (a)en
dc.relation.urihttp://dx.doi.org/10.1002/pssa.200675345en
dc.titleOrgano-vermiculite structure ordering after PVAc introductionen
dc.typearticleen
dc.identifier.locationNení ve fondu ÚKen
dc.description.abstract-enNatural vermiculite served as a host for intercalation with quaternary ammonium salt (QUAT) followed by in-situ polymerization of polyvinyl acetate (PVAc). We studied the structural changes of organo-vermiculite and its PVAc nanocomposite with the help of X-ray diffraction analysis. The mean crystallite size of PVAc nanocomposite is double compared to that of organo-vermiculite and its distribution of crystallite sizes presents a broader region but more uniform values than the curve calculated for organo-vermiculite. Molecular dynamic calculation proved a monolayer arrangement of QUAT guests and a bilayer-like system of guest organic molecules in the vermiculite gallery.en
dc.identifier.doi10.1002/pssa.200675345
dc.identifier.wos000247542500043


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