dc.contributor.author | Čapková, Pavla | |
dc.contributor.author | Driessen, Rene A.J. | |
dc.contributor.author | Numan, Milco | |
dc.contributor.author | Schenk, Henk | |
dc.contributor.author | Weiss, Zdeněk | |
dc.contributor.author | Klika, Zdeněk | |
dc.date.accessioned | 2007-08-22T08:08:36Z | |
dc.date.available | 2007-08-22T08:08:36Z | |
dc.date.issued | 1998 | |
dc.identifier.citation | Clays and Clay Minerals. 1998, vol. 46, no. 3, p. 240-244. | en |
dc.identifier.issn | 0009-8604 | |
dc.identifier.uri | http://hdl.handle.net/10084/62156 | |
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.1998.0460303 | en |
dc.subject | Al-cation | en |
dc.subject | gibbsite-like polymers | en |
dc.subject | intercalation | en |
dc.subject | molecular simulations | en |
dc.subject | montmorillonite | en |
dc.title | Molecular Simulations of Montmorillonite Intercalated with Aluminum Complex Cations. Part II: Intercalation with Al(OH)3-Fragment Polymers | en |
dc.type | article | en |
dc.identifier.location | Ve fondu ÚK | en |
dc.description.abstract-en | The Crystal Packer module in the Cerius 2 modeling environment has been used to study the
structure of montmorillonite intercalated with Al(OH)3-fragment (gibbsite-like) polymers. Basal spacings
in gibbsite-like polymers arranged in 2 layers in the interlayer of montmorillonite varied in the range
19.54-20.13 Å, depending on the type and arrangement of AI(OH)3 fragments. The inhomogeneous
distribution of intercalating species in the interlayer and, consequently, the turbostratic stacking of layers
has been found for gibbsite-like polymers as well as in the case of Keggin cations (Capková et al. 1998).
The dominating contribution to the total sublimation energy comes from electrostatic interactions for both
intercalating species, gibbsite-like polymers and Keggin cations. | en |
dc.identifier.doi | 10.1346/CCMN.1998.0460303 | |
dc.identifier.wos | 000075523200003 | |