Far infrared analysis of the structural environment of interlayer K+, NH4+, Rb+ and Cs+ selectively retained by vermiculite

Clays and Clay Minerals

Volumn 50, Issue 2, 2002, Pages 284-293

  Diaz, M ^a   Huard, E ^a   Prost, R ^a  

^a Science du Sol   (France)

Author keywords

Cation clay interactions; Far infrared spectroscopy; Retention; Selectivity; Vermiculite

Indexed keywords

HYDRATION; INFRARED SPECTROSCOPY; ION EXCHANGE; ISOTHERMS; POSITIVE IONS; STRUCTURE (COMPOSITION); X RAY DIFFRACTION;

INTERLAMELLAR SPACES;

CLAY MINERALS;

AMMONIA; CESIUM; MAGNESIUM CHLORIDE; POTASSIUM; RUBIDIUM; VERMICULITE;

CATION EXCHANGE CAPACITY; CLAY MINERAL; INFRARED SPECTROSCOPY; RETENTION; VERMICULITE;

CLAY; DESORPTION; HYDRATION; INFRARED SPECTROSCOPY; ISOTHERM; PHYSICAL CHEMISTRY; SOIL STRUCTURE; X RAY DIFFRACTION;

ABIES;

EID: 0036553893     PISSN: 00098604     EISSN: None     Source Type: Journal    
DOI: 10.1346/000986002760832883     Document Type: Article

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