Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Clay Minerals Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Clay Minerals; June 2005; v. 40; no. 2; p. 233-243; DOI: 10.1180/0009855054020169
© 2005 Mineralogical Society of Great Britain and Ireland
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (8)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by KOOLI, F.
Right arrow Articles by MAGUSIN, P. C. M. M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Adsorption of cetyltrimethylammonium ions on an acid-activated smectite and their thermal stability

F. KOOLI1,* and P. C. M. M. MAGUSIN2

1 Institute of Chemical and Engineering Sciences, 1 Pesek Road, Jurong Island, Singapore 627833 and 2 Eindhoven University of Technology, Laboratory of Inorganic Chemistry and Catalysis, P.O. Box 513, 5600 MB Eindhoven, The Netherlands

* E-mail: fethi_kooli{at}ices.a-star.edu.sg

(Received 10 June 2004; revised 29 November 2004)

The intercalation of the cationic surfactant cetyltrimethylammonium (C16TMA) into the interlayer of an acid-activated clay in the presence of different anions has been studied in detail. When Br or OH anions were used, the basal spacing increased significantly, the increase being related to the loading concentration of the surfactant solution. For intercalated compounds prepared from the hydroxide form, the basal spacing at room temperature varied from 1.6 to 3.8 nm. However, for organoclays prepared from the surfactant bromide, the basal spacing is almost loading-independent (1.9 nm). The use of hydroxide and bromide at higher pH is crucial to intercalating larger amounts of C16TMA cations and, hence, to improving the exfoliation of the silicate sheets. Magic-angle spinning 13C nuclear magnetic resonance spectroscopy indicates that the intercalated surfactants exhibit a significant degree of gauche conformation. According to in situ powder X-ray diffraction, an increase of the basal spacing to 4.08 nm is observed at intermediate temperatures of 50 to 150°C for organoclay with an initial basal spacing of 3.7 nm. At higher temperatures, decomposition of the surfactant occurs and the basal spacing decreases to ~1.4 nm.

KEYWORDS: adsorption, cetyltrimethylammonium, smectite, organoclay, MAS-NMR




This article has been cited by other articles:


Home page
Clays and Clay MineralsHome page
J. Madejova, H. Palkova, M. Pentrak, and P. Komadel
NEAR-INFRARED SPECTROSCOPIC ANALYSIS OF ACID-TREATED ORGANO-CLAYS
Clays and Clay Minerals, June 1, 2009; 57(3): 392 - 403.
[Abstract] [Full Text] [PDF]


Home page
Clays and Clay MineralsHome page
Z. Li and W.-T. Jiang
INTERLAYER CONFORMATIONS OF INTERCALATED DODECYLTRIMETHYLAMMONIUM IN RECTORITE AS DETERMINED BY FTIR, XRD, AND TG ANALYSES
Clays and Clay Minerals, April 1, 2009; 57(2): 194 - 204.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Mineralogical Society of Great Britain and Ireland