Particle properties of hydrothermal ammonium-bearing illite-smectite
Šucha, Vladimír (Comenius University. Faculty of Natural Sciences)
Uhlík, Peter (Comenius University. Faculty of Natural Sciences)
Madejová, Jana (Slovak Academy of Sciences. Institute of Inorganic Chemistry)
Petit, Sabine (Université de Poitiers)
Kraus, Ivan (Comenius University. Faculty of Natural Sciences)
Puškelová, L'Ubica (Slovak Academy of Sciences. Geological Institute)

Data:	2007
Resum:	Mixed-layer illite-smectite with high degree of ordering (rectorite-like clay) and with three types of interlayer cations - K, Na and NH , was detenrimed in the high-sulfide epithermal mineralization of the Western Carpathian Mountains. The tobelitic portion of the clay comprises 5-10%. Ammonium was detected both by chemical analysis and by Fourier transform infrared analysis. Some of the ammonium can be assigned to a poorly bound form, not fully fixed in the illitic interlayer. The finest size fraction separated from the samples behaves differently from the rest of the sample. It contains two layers of water molecules in the expandable interlayers as determined by X-ray diffraction, whereas coarser fractions have only one water layer in the interlayers.
Drets:	Aquest material està protegit per drets d'autor i/o drets afins. Podeu utilitzar aquest material en funció del que permet la legislació de drets d'autor i drets afins d'aplicació al vostre cas. Per a d'altres usos heu d'obtenir permís del(s) titular(s) de drets.
Llengua:	Anglès
Document:	Article ; recerca ; Versió publicada
Matèria:	Ammonium Illite-smectite ; Carpathian Mountains ; Hydrothermal Activity, Particle ; Properties ; Rectorite-like Mineral
Publicat a:	Clays and Clay Minerals, Vol. 55, Núm. 1 (2007) , p. 36-44, ISSN 1552-8367

DOI: 10.1346/CCMN.2007.0550103

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