dc.contributor.author | Weiss, Zdeněk | |
dc.contributor.author | Valášková, Marta | |
dc.contributor.author | Křístková, Monika | |
dc.contributor.author | Čapková, Pavla | |
dc.contributor.author | Pospíšil, Miroslav | |
dc.date.accessioned | 2006-10-24T14:19:03Z | |
dc.date.available | 2006-10-24T14:19:03Z | |
dc.date.issued | 2003 | |
dc.identifier.citation | Clays and Clay Minerals. 2003, vol. 51, no. 5, p. 555-565. | en |
dc.identifier.issn | 0009-8604 | |
dc.identifier.uri | http://hdl.handle.net/10084/57360 | |
dc.description.abstract | Octadecylamine (ODA) was used to intercalate a fine-grained and a coarse-grained fraction of natural Mg-vermiculite (VER) using a low-temperature melting procedure. Mixtures of Mg-vermiculite fractions and powdered ODA in the molar ratios of 2:1, 1:1, 1:2 and 1:6 were homogenized and heated for 1, 3, 15 and 30 h at 80ºC to prepare intercalated samples. X-ray powder diffraction analysis of intercalated samples was combined with molecular modeling to investigate their interlayer structure. Significant amounts of non-intercalated vermiculite and diffuse peaks with very low intensity and basal spacings close to 29 Åwere identified when the lowest concentration (molar ratio VER:ODA = 2:1) was used. According to molecular modeling, this indicates the initial stage of a one-layer arrangement of distorted ODA molecules in the interlayer. If the concentration of ODA molecules and treatment time were increased, a two-layer arrangement of ODA molecules with a different ODA chain-disorder and interlayer-space saturation was identified. Interlayer ODA molecules were inclined to the vermiculite basal plane with an inclination angle for two-layer arrangements that ranged from 76 to 95º. Experimental basal spacings with these two-layer arrangements varied from 52 to 58 A˚and were in agreement with molecular modeling results. A fully-saturated 58 Å two-layer ODA arrangement was identified when higher ODA concentrations (VER:ODA = 1:2 and 1:6) and 15 and 30 h treatment times were used. There was no significant difference between ODA-intercalated samples prepared using fine-grained and coarse-grained Mg-vermiculite fractions. A grafted ODA-chain nano-layer with a 49.6(2.1) Å average height was observed on the surface of thin ODA-intercalated micro-flakes using atomic force microscopy. Grafted ODA chains not only created an homogeneous surface nano-layer, but also variable-width channels between the ODA molecules. | en |
dc.language.iso | en | en |
dc.publisher | Clay Minerals Society | en |
dc.relation.ispartofseries | Clays and Clay Minerals | en |
dc.relation.uri | https://doi.org/10.1346/CCMN.2003.0510509 | en |
dc.subject | atomic force microscopy | en |
dc.subject | intercalation | en |
dc.subject | low-temperature melting | en |
dc.subject | molecular modeling | en |
dc.subject | octadecylamine | en |
dc.subject | vermiculite | en |
dc.subject | X-ray powder diffraction | en |
dc.title | Intercalation and grafting of vermiculite with octadecylamine using low-temperature melting | en |
dc.type | article | en |
dc.identifier.location | Ve fondu ÚK | en |
dc.identifier.doi | 10.1346/CCMN.2003.0510509 | |
dc.identifier.wos | 000185878600009 | |