Приказ основних података о документу

dc.creatorStojaković, D.
dc.creatorRajić, Nevenka
dc.date.accessioned2021-03-10T09:57:00Z
dc.date.available2021-03-10T09:57:00Z
dc.date.issued2001
dc.identifier.issn1380-2224
dc.identifier.urihttp://TechnoRep.tmf.bg.ac.rs/handle/123456789/378
dc.description.abstractThe lattice energies of the as-synthesized fluoride-containing chabazite-like aluminophosphate (AlPO4-34F) and of the corresponding metal-substituted materials [MeAPO-34F, Me = Mn(II), Co(II), Ni(II)] have been calculated in order to investigate the Al-site preference the transition metal substitution in the AlPO4-34F. The calculations show that the transition metal ions in MeAPO-34F should preferentially occupy octahedral Al3+ sites, and kinetic reasons are suggested as an explanation for the actual preference of tetrahedral sites. The lattice energies have also been calculated for the calcined AlPO4-34F material (AlPO4-34) and the rehydrated-calcined product (AlPO4-34h). The AlPO4-34 is found to be less stable than either AlPO4-34F or AlPO4-34h, which is consistent with the fact that AlPO4-34 can only be prepared starting from AlPO4-34F.en
dc.publisherKluwer Academic Publ, Dordrecht
dc.rightsrestrictedAccess
dc.sourceJournal of Porous Materials
dc.subjectchabazite zeoliteen
dc.subjectaluminophosphatesen
dc.subjectGULP programen
dc.subjectcatalysten
dc.titleComputational studies in the AlPO4-34 systemen
dc.typearticle
dc.rights.licenseARR
dc.citation.epage242
dc.citation.issue3
dc.citation.other8(3): 239-242
dc.citation.rankM22
dc.citation.spage239
dc.citation.volume8
dc.identifier.doi10.1023/A:1012296908560
dc.identifier.scopus2-s2.0-0035482852
dc.identifier.wos000171486400008
dc.type.versionpublishedVersion


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Приказ основних података о документу