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

Clays and Clay Minerals; October 2000; v. 48; no. 5; p. 495-502
© 2000 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 Di Leo, P.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

A NUCLEAR MAGNETIC RESONANCE (NMR) AND FOURIER-TRANSFORM INFRARED (FTIR) STUDY OF GLYCINE SPECIATION ON A Cd-RICH MONTMORILLONITE

Paola Di Leo

Istituto di Ricerca sulle Argille, CNR, Area di Ricerca di Potenza, Via S. Loja, 85050 Tito Scalo (PZ), Italy

E-mail of corresponding author: pdileo{at}ira.pz.cnr.it

As a consequence of treatments with glycine solutions, glycine molecules enter the interlayer of both Ca- and Cd-rich montmorillonite. Measurements of d value suggest that at low glycine concentration (0.01 and 0.1 M glycine solutions) a "flat" arrangement of the glycine molecules occurs in the interlayer. In contrast, intercalation of more than one monolayer of glycine molecules occurs for the montmorillonite treated with a higher concentration of glycine (1 M glycine solution).

Interlayer complexation of glycine occurs only for the Cd-rich form of montmorillonite, whereas no complexation is observed for Ca-rich montmorillonite. Both nuclear magnetic resonance (NMR) and Fourier-transform infrared (FTIR) results suggest that the adsorbed glycine, which fully protonates in the interlayer of montmorillonite to give the GlyH2+ species, interacts with the interlayer Cd2+ to form the CdGlyx complex mainly through the carboxylate group. The interlayer cadmium, present as both Cd2+ and CdCl+, is complexed by the ligand glycine. In contrast, the cadmium adsorbed on the external surfaces of montmorillonite does not interact with the ligand. Complexation of CdCl+ only occurs for large amounts of adsorption of glycine (e.g., for samples treated with 1 M glycine solution).

Key Words: Adsorption • Amino Acids • Cadmium • Glycine • Montmorillonite • Speciation




This article has been cited by other articles:


Home page
Clays and Clay MineralsHome page
P. Di Leo, P. Di Leo, and J. Cuadros
113Cd, 1H MAS NMR AND FTIR ANALYSIS OF Cd2+ ADSORPTION ON DIOCTAHEDRAL AND TRIOCTAHEDRAL SMECTITE
Clays and Clay Minerals, August 1, 2003; 51(4): 403 - 414.
[Abstract] [Full Text] [PDF]


Home page
ScienceHome page
M. J. Kennedy, D. R. Pevear, and R. J. Hill
Mineral Surface Control of Organic Carbon in Black Shale
Science, January 25, 2002; 295(5555): 657 - 660.
[Abstract] [Full Text] [PDF]




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