Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Clays and Clay Minerals Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Clays and Clay Minerals; August 2006; v. 54; no. 4; p. 456-465; DOI: 10.1346/CCMN.2006.0540406
© 2006 Clay Minerals Society
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 (5)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Harris, R. G.
Right arrow Articles by Johnson, B. B.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

MODELING THE ADSORPTION OF ORGANIC DYE MOLECULES TO KAOLINITE

Rodney G. Harris{dagger}, John D. Wells*, Michael J. Angove and Bruce B. Johnson

Colloid and Environmental Chemistry Laboratory, La Trobe University, PO Box 199, Bendigo, Victoria 3552, Australia

* E-mail address of corresponding author: j.wells{at}latrobe.edu.au

Simple extended constant capacitance surface complexation models have been developed to represent the adsorption of polyaromatic dyes (9-aminoacridine, 3,6-diaminoacridine, azure A and safranin O) to kaolinite, and the competitive adsorption of the dyes with Cd. The formulation of the models was based on data from recent publications, including quantitative adsorption measurements over a range of conditions (varying pH and concentration), acid-base titrations and attenuated total reflectance-Fourier transform infrared spectroscopic data. In the models the dye molecules adsorb as aggregates of three or four, forming outer-sphere complexes with sites on the silica face of kaolinite. Both electrostatic and hydrophobic interactions are implicated in the adsorption processes. Despite their simplicity, the models fit a wide range of experimental data, thereby supporting the underlying hypothesis that the flat, hydrophobic, but slightly charged silica faces of kaolinite facilitate the aggregation and adsorption of the flat, aromatic, cationic dye molecules.

Key Words: 9-aminoacridine • 3,6-diaminoacridine • Azure A • Dye • Hydrophobic Interactions • Kaolin • Safranin O • Surface Complexation Models




This article has been cited by other articles:


Home page
Clays and Clay MineralsHome page
R. G. Harris, B. B. Johnson, and J. D. Wells
STUDIES ON THE ADSORPTION OF DYES TO KAOLINITE
Clays and Clay Minerals, August 1, 2006; 54(4): 435 - 448.
[Abstract] [Full Text] [PDF]


Home page
Clays and Clay MineralsHome page
R. G. Harris, B. B. Johnson, and J. D. Wells
COMPETITIVE ADSORPTION OF Cd AND DYES TO KAOLINITE
Clays and Clay Minerals, August 1, 2006; 54(4): 449 - 455.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Clay Minerals Society