Particle properties of hydrothermal ammonium-bearing illite-smectite

Authors: Šucha, Vladimír; Uhlík, Peter; Madejová, Jana; Petit, Sabine; Kraus, Ivan; Puškelová, L'ubica

Source: Clays and Clay Minerals, Volume 55, Number 1, February 2007 , pp. 36-44(9)

Publisher: The Clay Minerals Society

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Abstract:

Mixed-layer illite-smectite with high degree of ordering (rectorite-like clay) and with three types of interlayer cations - K+, Na+ and NH4+, was determined 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.
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  • The JOURNAL publishes articles of interest to the international community of clay scientists, including but not limited to areas in mineralogy, crystallography, geology, geochemistry, sedimentology, soil science, agronomy, physical chemistry, colloid chemistry, ceramics, petroleum engineering, foundry engineering, and soil mechanics. Clays and Clay Minerals exists to disseminate to its worldwide readership the most recent developments in all of these aspects of clay materials. Manuscripts are welcome from all countries.

    Clays and Clay Minerals is the official publication of The Clay Minerals Society.

    The Editor-in-Chief is Professor Joseph W. Stucki jstucki@illinois.edu

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