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Interactions of ammonium smectite with low-molecular-weight carboxylic acids

Published online by Cambridge University Press:  09 July 2018

M. Gautier*
Affiliation:
CNRS/INSU, Institut des Sciences de la Terre d'Orléans (ISTO), Université d'Orléans-Université de Tours, 1A rue de la Férollerie, 45071 Orléans Cedex 2, France
F. Muller
Affiliation:
CNRS/INSU, Institut des Sciences de la Terre d'Orléans (ISTO), Université d'Orléans-Université de Tours, 1A rue de la Férollerie, 45071 Orléans Cedex 2, France
J.-M. Beny
Affiliation:
CNRS/INSU, Institut des Sciences de la Terre d'Orléans (ISTO), Université d'Orléans-Université de Tours, 1A rue de la Férollerie, 45071 Orléans Cedex 2, France
L. Le Forestier
Affiliation:
CNRS/INSU, Institut des Sciences de la Terre d'Orléans (ISTO), Université d'Orléans-Université de Tours, 1A rue de la Férollerie, 45071 Orléans Cedex 2, France
P. Alberic
Affiliation:
CNRS/INSU, Institut des Sciences de la Terre d'Orléans (ISTO), Université d'Orléans-Université de Tours, 1A rue de la Férollerie, 45071 Orléans Cedex 2, France
P. Baillif
Affiliation:
CNRS/INSU, Institut des Sciences de la Terre d'Orléans (ISTO), Université d'Orléans-Université de Tours, 1A rue de la Férollerie, 45071 Orléans Cedex 2, France

Abstract

The percolation of water through waste landfill sites produces leachates with large amounts of pollutants. Clay barriers are often used to limit soil and underground water pollution. A better understanding of the interaction between ammonium smectite and carboxylic acids would contribute significantly to our understanding of such systems. The SWy-2 (Wyoming smectite) was exchanged with NH4+ and then batched with carboxylic acids (acetic, formic, chloroacetic and oxalic) in concentrations between 0.01 M and 1 M. The solid phases obtained were analysed chemically and characterized by infrared absorption spectroscopy (IR) and powder X-ray diffraction (XRD). Ionic chromatography was used for the quantitative measurement of ammonium ions in the solution after the interaction. For the four acids, the interaction was characterized by a cationic exchange of NH4+ to H3O+. A partial exchange to Al3+ due to a partial dissolution of the sample in strong acidic medium was observed with chloroacetic and oxalic acids for which adsorption of molecules on the clay sample occurs, mainly through H-bonding with the cation. Moreover, the intercalation of oxalic acid in the interlayer space was highlighted.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2009

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