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https://olympias.lib.uoi.gr/jspui/handle/123456789/14075Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Karakassides, M. A. | en |
| dc.contributor.author | Petridis, D. | en |
| dc.contributor.author | Gournis, D. | en |
| dc.date.accessioned | 2015-11-24T17:35:06Z | - |
| dc.date.available | 2015-11-24T17:35:06Z | - |
| dc.identifier.issn | 0009-8604 | - |
| dc.identifier.uri | https://olympias.lib.uoi.gr/jspui/handle/123456789/14075 | - |
| dc.rights | Default Licence | - |
| dc.subject | cs-montmorillonite | en |
| dc.subject | li-montmorillonite | en |
| dc.subject | longitudinal-optic (lo) mode | en |
| dc.subject | migration | en |
| dc.subject | reflectivity | en |
| dc.subject | transverse-optic (to) mode | en |
| dc.subject | synthetic fluorine micas | en |
| dc.subject | ir-spectra | en |
| dc.subject | glasses | en |
| dc.subject | silica | en |
| dc.subject | charge | en |
| dc.subject | spectroscopy | en |
| dc.subject | migration | en |
| dc.subject | lithium | en |
| dc.subject | water | en |
| dc.subject | sites | en |
| dc.title | Infrared reflectance study of thermally treated Li- and Cs-montmorillonites | en |
| heal.type | journalArticle | - |
| heal.type.en | Journal article | en |
| heal.type.el | Άρθρο Περιοδικού | el |
| heal.identifier.secondary | <Go to ISI>://A1997YJ80800004 | - |
| heal.language | en | - |
| heal.access | campus | - |
| heal.recordProvider | Πανεπιστήμιο Ιωαννίνων. Σχολή Θετικών Επιστημών. Τμήμα Μηχανικών Επιστήμης Υλικών | el |
| heal.publicationDate | 1997 | - |
| heal.abstract | The structure of Li-and Cs-montmorillonites was studied using infrared (IR) reflectance spectroscopy. The spectra of heat-treated clays between 80 and 220 degrees C were analyzed by Kramers-Kronig inversion in order to obtain the optical and dielectric properties of the clays. The analysis revealed the transverse-optic (TO) and longitudinal-optic (LO) components of the asymmetric stretching vibration of Si-O-Si bridges. Major differences, in particular the systematic development of new bands, were found in the Li-montmorillonite LO and TO spectra with increasing temperature. These changes were attributed to the migration of the Li-cations into the layer structure. | en |
| heal.publisher | Clay Minerals Society | en |
| heal.journalName | Clays and Clay Minerals | en |
| heal.journalType | peer reviewed | - |
| heal.fullTextAvailability | TRUE | - |
| Appears in Collections: | Άρθρα σε επιστημονικά περιοδικά ( Ανοικτά) | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| Karakassides-1997-Infrared reflectance study.pdf | 681.28 kB | Adobe PDF | View/Open |
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