Structural characterization of aniline-bentonite composite by FTIR, DTA/TG, and PXRD analyses and BET measurement

ArticleAçık Erişim

Özet

The aniline species incorporated into the acid-activated bentonite matrices leads to the decay of the skeletal stretches centered at 1041 cm-1 and the rise of new features in the phenyl ring frequency region, 1700-1400 cm-1, demonstrates clearly the influence of the acid activation on the Lewis sites necessary for coordination of aniline to bentonite. The exothermic DTA features at 507, 684, and 725°C indicate the release of both the clusters and the decomposed fragments of the aniline-clay composite, and the highly stable carbonaceous residue, respectively. The basal difference by ∼1.0 nm and the much smaller surface area (33.8 m2/g) than that of the nonintercalated bentonite (129.2 m2/g) prove the presence of the tilted aniline species between the interlamellar grooves of the bentonite framework. Copyright © Taylor & Francis Group, LLC.

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RDL Kalıcı Bağlantı (PID)
https://rdlopen.rawdatalibrary.net/r/ebyu/15754Resmi atıflarda kullanılan kalıcı adres
DOI
https://doi.org/10.1080/00387010903555953Yayıncı resmi DOI adresi
Tam Kayıt
AlanDeğerDil
dc.contributor.authorKoksal, E.
dc.contributor.authorAfsin, B.
dc.contributor.authorTabak, A.
dc.contributor.authorCaglar, B.
dc.date.accessioned2026-10-18T20:30:36.032945015Z
dc.date.available2026-10-18T20:30:36.032945015Z
dc.date.issued2011
dc.description.abstractThe aniline species incorporated into the acid-activated bentonite matrices leads to the decay of the skeletal stretches centered at 1041 cm-1 and the rise of new features in the phenyl ring frequency region, 1700-1400 cm-1, demonstrates clearly the influence of the acid activation on the Lewis sites necessary for coordination of aniline to bentonite. The exothermic DTA features at 507, 684, and 725°C indicate the release of both the clusters and the decomposed fragments of the aniline-clay composite, and the highly stable carbonaceous residue, respectively. The basal difference by ∼1.0 nm and the much smaller surface area (33.8 m2/g) than that of the nonintercalated bentonite (129.2 m2/g) prove the presence of the tilted aniline species between the interlamellar grooves of the bentonite framework. Copyright © Taylor & Francis Group, LLC.
dc.description.sponsorshipThe authors are grateful to the Research Foundation of Ondokuz Mayis University for the financial support of this work under Project F238. We also thank Professor Ugur Cevik of Karadeniz Technical University for performing the chemical analysis of the activated clay sample.
dc.identifier.doi10.1080/00387010903555953
dc.identifier.endpage82
dc.identifier.issn1532-2289
dc.identifier.issue2
dc.identifier.scopus2-s2.0-79951932562
dc.identifier.startpage77
dc.identifier.urihttps://rdlopen.rawdatalibrary.net/r/ebyu/15754
dc.identifier.volume44
dc.identifier.wosWOS:000287490500001
dc.language.isoen
dc.publisherTAYLOR & FRANCIS INC
dc.relation.ispartofSpectroscopy Letters
dc.rightsinfo:eu-repo/semantics/openAccess
dc.subjectanline species
dc.subjectbentonite
dc.subjectintercalation
dc.subjectsurface properties
dc.subjectthermal analysis
dc.titleStructural characterization of aniline-bentonite composite by FTIR, DTA/TG, and PXRD analyses and BET measurement
dc.typeArticle
dspace.entity.typePublication
rdl.citation.scopus20
rdl.citation.wos19
rdl.source.indexSCOPUS
rdl.source.indexWOS
rdl.wos.indexScience Citation Index Expanded (SCI-EXPANDED)