Zobrazit minimální záznam

dc.contributor.authorSimha Martynková, Gražyna
dc.contributor.authorBuchtík, Ondřej
dc.contributor.authorPlevová, Eva
dc.contributor.authorBarabaszová, Karla
dc.contributor.authorHolešová, Sylva
dc.contributor.authorValášková, Marta
dc.date.accessioned2010-11-04T13:11:20Z
dc.date.available2010-11-04T13:11:20Z
dc.date.issued2010
dc.identifier.citationJournal of Scientific Conference Proceedings. 2010, vol. 2, no. 1, p. 42-44.en
dc.identifier.issn1937-6456
dc.identifier.urihttp://hdl.handle.net/10084/83288
dc.description.abstractThe demand of nanocomposites for filler properties which is expected utilization. Natural minerals are keeping one of the prior positions in that significance. The thermal properties and strength of the requested properties expected to be improved for polymeric materials. Modification of that layered materials is still necessary to assure the compatibility of the filler with polymer with non-polar character. The organically modified montmorillonite is still the most frequently studied mineral for the application as the filler. Comparing montmorillonite and vermiculite we can note the difference in layer charge of silicate layer. Thus the vermiculite with higher charge could be more stable. Modification of jet milled vermiculite with amine and phosphonium salts using thermal treatment was performed using 10% of organic amount. The changes of interlayer space of samples after intercalation and nanocomposites were studied using X-ray diffraction analysis. Higher degradation temperature for nanocomposites with vermiculite was defined using thermogravimetry.en
dc.language.isoenen
dc.publisherAmerican Scientific Publishersen
dc.relation.ispartofseriesJournal of Scientific Conference Proceedingsen
dc.relation.urihttps://doi.org/10.1166/jcp.2010.1008en
dc.subjectnanocompositeen
dc.subjectnanofilleren
dc.subjectvermiculiteen
dc.subjectpolystyreneen
dc.titleVermiculite filler for polymeric nanocomposites: thermal and dispersion studyen
dc.typeproceedings paperen
dc.identifier.locationNení ve fondu ÚKen
dc.identifier.doi10.1166/jcp.2010.1008
dc.identifier.wos000282747300008


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Zobrazit minimální záznam