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; June 2004; v. 52; no. 3; p. 321-333; DOI: 10.1346/CCMN.2004.0520307
© 2004 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 (19)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Strawn, D. G.
Right arrow Articles by Kukkadapu, R. K.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

COPPER SORPTION MECHANISMS ON SMECTITES

Daniel G. Strawn1,*, Noel E. Palmer1, Luca J. Furnare1, Carmen Goodell1, James E. Amonette2 and Ravi K. Kukkadapu2

1 Department of Plant, Soil and Entomological Sciences, University of Idaho, Moscow, ID 83844-2339, USA
2 Pacific Northwest National Laboratory, Richland, Washington, USA

* E-mail address of corresponding author: dgstrawn{at}uidaho.edu

Due to the importance of clay minerals in metal sorption, many studies have attempted to derive mechanistic models that describe adsorption processes. These models often include several different types of adsorption sites, including permanent charge sites and silanol and aluminol functional groups on the edges of clay minerals. To provide a basis for development of adsorption models it is critical that molecular-level studies be done to characterize sorption processes. In this study we conducted X-ray absorption fine structure (XAFS) and electron paramagnetic resonance (EPR) spectroscopic experiments on copper (II) sorbed on smectite clays using suspension pH and ionic strength as variables. At low ionic strength, results suggest that Cu is sorbing in the interlayers and maintains its hydration sphere. At high ionic strength, Cu atoms are excluded from the interlayer and sorb primarily on the silanol and aluminol functional groups of the montmorillonite or beidellite structures. Interpretation of the XAFS and EPR spectroscopy results provides evidence that multinuclear complexes are forming. Fitting of extended X-ray absorption fine structure spectra revealed that the Cu-Cu atoms in the multinuclear complexes are 2.65 Å apart, and have coordination numbers near one. This structural information suggests that small Cu dimers are sorbing on the surface. These complexes are consistent with observed sorption on mica and amorphous silicon dioxide, yet are inconsistent with previous spectroscopic results for Cu sorption on montmorillonite. The results reported in this paper provide mechanistic data that will be valuable for modeling surface interactions of Cu with clay minerals, and predicting the geochemical cycling of Cu in the environment.

Key Words: Copper • EPR • EXAFS • Montmorillonite • Smectite • Sorption




This article has been cited by other articles:


Home page
Eur J MineralHome page
K. A. Hudson-Edwards, A. M.L. Smith, W. E. Dubbin, A. J. Bennett, P. J. Murphy, and K. Wright
Comparison of the structures of natural and synthetic Pb-Cu-jarosite-type compounds
European Journal of Mineralogy, April 1, 2008; 20(2): 241 - 252.
[Abstract] [Full Text] [PDF]




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