Investigation of the Orientation of CTA+ Ions in the Interlayer of CTAB Pillared Montmorillonite

The orientation of CTA+ in the interlayer of organic pillared montmorillonite prepared by adding different amounts of surfactant corresponding to the CEC of the pristine clay mineral has been studied using X-ray diffraction (XRD), Fourier Transform Infrared (FTIR) spectra. Morphology of the samples...

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Main Authors: Semra Karaca, Ahmet Gürses, Mehtap Ejder Korucu
Format: Article
Language:English
Published: Hindawi Limited 2013-01-01
Series:Journal of Chemistry
Online Access:http://dx.doi.org/10.1155/2013/274838
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spelling doaj-b24a17b0c11343dabad808e007106b772020-11-24T22:25:17ZengHindawi LimitedJournal of Chemistry2090-90632090-90712013-01-01201310.1155/2013/274838274838Investigation of the Orientation of CTA+ Ions in the Interlayer of CTAB Pillared MontmorilloniteSemra Karaca0Ahmet Gürses1Mehtap Ejder Korucu2Department of Chemistry, Faculty of Science, Atatürk University, 25240 Erzurum, TurkeyDepartment of Chemistry, K.K. Education Faculty, Atatürk University, 25240 Erzurum, TurkeyDepartment of Chemistry, Faculty of Science, Atatürk University, 25240 Erzurum, TurkeyThe orientation of CTA+ in the interlayer of organic pillared montmorillonite prepared by adding different amounts of surfactant corresponding to the CEC of the pristine clay mineral has been studied using X-ray diffraction (XRD), Fourier Transform Infrared (FTIR) spectra. Morphology of the samples was examined by scanning electron microscopy (SEM). The results are supported by the measurements of zeta potentials and contact angles of pristine clay and organoclay samples. From the XRD results, a series of arrangement models of CTA+ in the interlayer of montmorillonite have been proposed as lateral-bilayer, pseudotrilayer, paraffin-type-monolayer and pseudotrilayer, paraffin-type-bilayer and pseudotrilayer for 0.5, 1, 1.5, and 2.0 CEC, respectively. FTIR spectrum and contact angle measurements of pristine montmorillonite and organoclays indicated the incorporation of surfactant and the changing of hydrophility in the different OMts. This study demonstrates that not only the arrangement model of surfactant, but also the morphology of organoclay strongly depends on the surfactant packing density within the montmorillonite interlayer space. In addition, it can be also proposed that, the magnitude of surface charge or its distribution on clay mineral might be an important factor for expansion characteristics of organoclay.http://dx.doi.org/10.1155/2013/274838
collection DOAJ
language English
format Article
sources DOAJ
author Semra Karaca
Ahmet Gürses
Mehtap Ejder Korucu
spellingShingle Semra Karaca
Ahmet Gürses
Mehtap Ejder Korucu
Investigation of the Orientation of CTA+ Ions in the Interlayer of CTAB Pillared Montmorillonite
Journal of Chemistry
author_facet Semra Karaca
Ahmet Gürses
Mehtap Ejder Korucu
author_sort Semra Karaca
title Investigation of the Orientation of CTA+ Ions in the Interlayer of CTAB Pillared Montmorillonite
title_short Investigation of the Orientation of CTA+ Ions in the Interlayer of CTAB Pillared Montmorillonite
title_full Investigation of the Orientation of CTA+ Ions in the Interlayer of CTAB Pillared Montmorillonite
title_fullStr Investigation of the Orientation of CTA+ Ions in the Interlayer of CTAB Pillared Montmorillonite
title_full_unstemmed Investigation of the Orientation of CTA+ Ions in the Interlayer of CTAB Pillared Montmorillonite
title_sort investigation of the orientation of cta+ ions in the interlayer of ctab pillared montmorillonite
publisher Hindawi Limited
series Journal of Chemistry
issn 2090-9063
2090-9071
publishDate 2013-01-01
description The orientation of CTA+ in the interlayer of organic pillared montmorillonite prepared by adding different amounts of surfactant corresponding to the CEC of the pristine clay mineral has been studied using X-ray diffraction (XRD), Fourier Transform Infrared (FTIR) spectra. Morphology of the samples was examined by scanning electron microscopy (SEM). The results are supported by the measurements of zeta potentials and contact angles of pristine clay and organoclay samples. From the XRD results, a series of arrangement models of CTA+ in the interlayer of montmorillonite have been proposed as lateral-bilayer, pseudotrilayer, paraffin-type-monolayer and pseudotrilayer, paraffin-type-bilayer and pseudotrilayer for 0.5, 1, 1.5, and 2.0 CEC, respectively. FTIR spectrum and contact angle measurements of pristine montmorillonite and organoclays indicated the incorporation of surfactant and the changing of hydrophility in the different OMts. This study demonstrates that not only the arrangement model of surfactant, but also the morphology of organoclay strongly depends on the surfactant packing density within the montmorillonite interlayer space. In addition, it can be also proposed that, the magnitude of surface charge or its distribution on clay mineral might be an important factor for expansion characteristics of organoclay.
url http://dx.doi.org/10.1155/2013/274838
work_keys_str_mv AT semrakaraca investigationoftheorientationofctaionsintheinterlayerofctabpillaredmontmorillonite
AT ahmetgurses investigationoftheorientationofctaionsintheinterlayerofctabpillaredmontmorillonite
AT mehtapejderkorucu investigationoftheorientationofctaionsintheinterlayerofctabpillaredmontmorillonite
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