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dc.contributor.authorGournis, D.en
dc.contributor.authorKarakassides, M. A.en
dc.contributor.authorPetridis, D.en
dc.date.accessioned2015-11-24T17:34:29Z-
dc.date.available2015-11-24T17:34:29Z-
dc.identifier.issn0342-1791-
dc.identifier.urihttps://olympias.lib.uoi.gr/jspui/handle/123456789/13975-
dc.rightsDefault Licence-
dc.subjectsmectite claysen
dc.subjecthydroxyl radicalen
dc.subjectsuperoxideen
dc.subjectspin trappingen
dc.subjectepren
dc.subjecthydrogen-peroxideen
dc.subjectlipid-peroxidationen
dc.subjectasbestosen
dc.subjectsuperoxideen
dc.subjectironen
dc.subjecttoxicityen
dc.subjectinhibitionen
dc.subjectfibersen
dc.subjectdustsen
dc.titleFormation of hydroxyl radicals catalyzed by clay surfacesen
heal.typejournalArticle-
heal.type.enJournal articleen
heal.type.elΆρθρο Περιοδικούel
heal.identifier.primaryDOI 10.1007/s002690100215-
heal.identifier.secondary<Go to ISI>://000174990600007-
heal.languageen-
heal.accesscampus-
heal.recordProviderΠανεπιστήμιο Ιωαννίνων. Σχολή Θετικών Επιστημών. Τμήμα Μηχανικών Επιστήμης Υλικώνel
heal.publicationDate2002-
heal.abstractThe formation of superoxide and hydroxyl radicals at the surface of smectite clays due to oxygen reduction is demonstrated by electron paramagnetic resonance spectroscopy. The yield of hydroxyl radicals is mainly a function of particle size of the clays and depends, to a lesser extent, on the clay lattice iron. Synthetic laponite clay with small platelet size (similar to20 nm) and without lattice iron is leading in the formation of hydroxyl radicals followed by montmorillonite (similar to200 nm). Fluorohectorite (similar to2000 nm) was inactive to hydroxyl radical formation by oxygen reduction.en
heal.publisherSpringer-Verlagen
heal.journalNamePhysics and Chemistry of Mineralsen
heal.journalTypepeer reviewed-
heal.fullTextAvailabilityTRUE-
Appears in Collections:Άρθρα σε επιστημονικά περιοδικά ( Ανοικτά)

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