Adsorption of a C10E3 non-ionic surfactant on a Ca-smectite
Guegan, Regis (Centre national de la recherche scientifique (França). Institut des Sciences de la Terre d'Orléans)
Gautier, Mathieu (Centre national de la recherche scientifique (França). Institut des Sciences de la Terre d'Orléans)
Beny, Jean-Michel (Centre national de la recherche scientifique (França). Institut des Sciences de la Terre d'Orléans)
Muller, Fabrice (Centre national de la recherche scientifique (França). Institut des Sciences de la Terre d'Orléans)

Date:	2009
Abstract:	The transformation of clay minerals into organo-clays by surfactant intercalation is of great environmental and industrial importance because it causes the clay to attract hydrophobic contaminants and other non-polar organic compounds, but a better understanding is needed of the mechanisms by which different classes of surfactants are intercalated. The purpose of this study was to synthesize and characterize an organo-clay comprising triethylene glycol monodecyl ether (CE) non-ionic surfactant, which has a lamellar phase at room temperature, intercalated into Ca-montmorillonite from Wyoming (SWy-2). The CE non-ionic surfactant differed from previous non-ionic surfactants used in the formation of a lamellar phase in that it consisted of the stacking of molecules by hydrophobic interaction. CE-clay composites were characterized by complementary techniques (adsorption isotherms, X-ray diffraction, and infrared spectroscopy) and were compared to benzyldimethyltetradecyl ammonium chloride (BDTAC) cationic surfactant-clay composites for different loadings of the surfactant. For large loadings, the amount of CE adsorbed, which can be described by the Langmuir equation, seemed to reach a steady state close to that of the cationic surfactant. The adsorption processes of the two surfactants were different. For the cationic surfactant, the adsorption, as described in the literature, was due to ion exchange between organic cations and Ca counterions. The adsorption of CE did not depend on electrostatic interaction but rather was due to several interaction mechanisms (H-bonding, ion-dipole, and hydrophobic interaction). For both surfactants, the expansion was limited to two adsorbed monolayers parallel to the clay surface. The expansion of the basal spacing to 17 Å suggested a complete dissociation of the CE lamellar phase when adsorbed on the Ca-smectite. Organo-clays made using the non-ionic surfactant were stable, changing the chemical nature of clay to hydrophobic, and allowing for other cations to be exchanged, which has importance in the manufacture of new nanocomposites or geochemical barriers.
Rights:	Tots els drets reservats.
Language:	Anglès
Document:	Article ; recerca ; Versió publicada
Subject:	Ca-smectite ; Infrared Spectroscopy ; Organo-clay ; Surfactant ; X-ray Diffraction
Published in:	Clays and Clay Minerals, Vol. 57, Núm. 4 (2009) , p. 502-509, ISSN 1552-8367

DOI: 10.1346/CCMN.2009.0570411

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