Please use this identifier to cite or link to this item: https://olympias.lib.uoi.gr/jspui/handle/123456789/14227
Full metadata record
DC FieldValueLanguage
dc.contributor.authorKarakassides, M. A.en
dc.contributor.authorGournis, D.en
dc.contributor.authorSimopoulos, T.en
dc.contributor.authorPetridis, D.en
dc.date.accessioned2015-11-24T17:36:16Z-
dc.date.available2015-11-24T17:36:16Z-
dc.identifier.issn0009-8604-
dc.identifier.urihttps://olympias.lib.uoi.gr/jspui/handle/123456789/14227-
dc.rightsDefault Licence-
dc.subjectcms clay swa-1en
dc.subjectdehydroxylationen
dc.subjectinfrared spectraen
dc.subjectlithium migrationen
dc.subjectmossbauer spectraen
dc.subjectnontroniteen
dc.subjectsuperparamagnetic behavioren
dc.subjectmagnetic-propertiesen
dc.subjectlayer silicatesen
dc.subjectx-rayen
dc.subjectspectraen
dc.subjectironen
dc.titleMossbauer and infrared study of heat-treated nontroniteen
heal.typejournalArticle-
heal.type.enJournal articleen
heal.type.elΆρθρο Περιοδικούel
heal.identifier.primaryDoi 10.1346/Ccmn.2000.0480109-
heal.identifier.secondary<Go to ISI>://000085533900009-
heal.languageen-
heal.accesscampus-
heal.recordProviderΠανεπιστήμιο Ιωαννίνων. Σχολή Θετικών Επιστημών. Τμήμα Μηχανικών Επιστήμης Υλικώνel
heal.publicationDate2000-
heal.abstractThe Mossbauer and infrared spectra of Li- and Rb-saturated nontronites from Washington, USA (SWa-1), heat treated at different temperatures, were measured. The Mossbauer results show that diffusion of Li+ into the 2:1 layer by heat treatment at 250-300 degrees C does nor affect the magnetic hyperfine interactions of the octahedral iron centers. In contrast, significant changes were observed by calcination at temperatures >300 degrees C for Li-saturated nontronites. The main features of the Mossbauer spectra recorded at different temperatures reveal superparamagnetic behavior with a blocking temperature of similar to 5 K. The superparamagnetic behavior is related to small magnetic domains created by partially broken Fe-O-Fe bonds upon hear treatment. The infrared spectra of Li-rich nontronite, heat treated at 300 degrees C, show changes attributed to Li migration into the hexagonal cavities. Heating to higher temperatures, produced changes in the spectra of the Li- and Rb-saturated nontronites owing to the dehydroxylation of the layer structure. The dehydroxylation process begins with the loss of OH groups in the FeOHFe bridges and is completed with the disruption of the Al-O bonds at >600 degrees C.en
heal.publisherThe Clay Minerals Societyen
heal.journalNameClays and Clay Mineralsen
heal.journalTypepeer reviewed-
heal.fullTextAvailabilityTRUE-
Appears in Collections:Άρθρα σε επιστημονικά περιοδικά ( Ανοικτά)

Files in This Item:
File Description SizeFormat 
Gournis-2000-Mos.pdf627.58 kBAdobe PDFView/Open


This item is licensed under a Creative Commons License Creative Commons