Please use this identifier to cite or link to this item: https://olympias.lib.uoi.gr/jspui/handle/123456789/9648
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dc.contributor.authorSklari, S.en
dc.contributor.authorRahiala, H.en
dc.contributor.authorStathopoulos, V.en
dc.contributor.authorRosenholm, J.en
dc.contributor.authorPomonis, P.en
dc.date.accessioned2015-11-24T16:50:49Z-
dc.date.available2015-11-24T16:50:49Z-
dc.identifier.issn1387-1811-
dc.identifier.urihttps://olympias.lib.uoi.gr/jspui/handle/123456789/9648-
dc.rightsDefault Licence-
dc.subjectmesoporousen
dc.subjectwateren
dc.subjectfreezingen
dc.subjecth-1-nmren
dc.subjectsurface acidityen
dc.subjectnuclear-magnetic-resonanceen
dc.subjectneutron-scatteringen
dc.subjectporous silicaen
dc.subjectsizeen
dc.subjectporeen
dc.subjectnmren
dc.subjectdiffractionen
dc.subjectdynamicsen
dc.subjecth-1-nmren
dc.subjectglassen
dc.titleThe influence of surface acid density on the freezing behavior of water confined in mesoporous MCM-41 solidsen
heal.typejournalArticle-
heal.type.enJournal articleen
heal.type.elΆρθρο Περιοδικούel
heal.identifier.secondary<Go to ISI>://000172090500001-
heal.identifier.secondaryhttp://ac.els-cdn.com/S1387181101003717/1-s2.0-S1387181101003717-main.pdf?_tid=8da267a1de2c940bb0c9e68cc7609ef6&acdnat=1333036704_35446bc50c23a1b5b16a80f7ee27fbcf-
heal.languageen-
heal.accesscampus-
heal.recordProviderΠανεπιστήμιο Ιωαννίνων. Σχολή Θετικών Επιστημών. Τμήμα Χημείαςel
heal.publicationDate2001-
heal.abstractThe freezing behavior of water confined in the pores of five mesoporous MCM-41 materials of controlled acidity has been studied using H-1-NMR. The surface acidity of Si, Si/Al and Si/Ti-based MCM-41 solids was determined using NH3 temperature programmed desorption experiments. The Full Width at Half Maximum of the H-1-NMR signal in the temperature range 300 K > T > 200 K, corresponding to the spin-spin re:laxation time 1/T-2 was recorded at 5 degrees intervals. The 1/T-2 values for all samples show a smooth increase as temperature drops down to T approximate to 225-230 K. At this region the core water in the pores freezes leaving a layer of water between the pore wall and the core ice unfreezable. This shell of unfreezable water undergoes a continuous transition as temperature drops, Below T < 225-230 K the slope d(1/T-2)/dT depends on the surface acid density. An energy relationship (1/T-2) = A exp(Q/RT) was used to calculate the Q and A values which show a compensation effect. The energy parameter Q assumes values between 14-19 kJ mol(-1) and depends on the acid-acid site distance. A model of water molecules bridging the acid surface sites is proposed. The number N of water molecules bridging these sites is suggested to be related to Q via a charge - hopping mechanism. The Q value becomes zero when the distance between the acid sites is similar to5.5 Angstrom which corresponds to the unfreezable shell water layer in the pores. (C) 2001 Elsevier Science B.V. All rights reserved.en
heal.publisherElsevieren
heal.journalNameMicroporous and Mesoporous Materialsen
heal.journalTypepeer reviewed-
heal.fullTextAvailabilityTRUE-
Appears in Collections:Άρθρα σε επιστημονικά περιοδικά ( Ανοικτά). ΧΗΜ

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