Deuterium and oxygen-17 nuclear magnetic resonance of aqueous clay suspensions.
Properties of interfacial water have been studied in saponite, hectorite and montmorillonite suspensions. These data, together with our previous results are explained by the presence of two water interfacial sites or by a fast exchange between them.
Grandjean
J
J
University of Liege, Institute of Chemistry B6, Sart Tilman, Belgium.
Laszlo
P
P
D000538:Aluminum Silicates; D001546:Bentonite; D000077215:Clay; D003903:Deuterium; D009682:Magnetic Resonance Spectroscopy; D010103:Oxygen Isotopes; D017640:Silicates; D013535:Suspensions
D000538:Aluminum Silicates; D010103:Oxygen Isotopes; D017640:Silicates; D013535:Suspensions; C013547:hectorite; D001546:Bentonite; D003903:Deuterium; D000077215:Clay