Mineralogical and physico-chemical characterizations of ferruginous beidellite-rich clay from Agadir Basin (Morocco)

The mechanism of formation of detrital, beidellite-rich clay occurring in the Agadir basin (Morocco) is well documented, but its detailed characterization is incomplete which limits its application. The aim of the present study was to provide further details of the mineralogical and physico-chemical...

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Veröffentlicht in:	Clays and clay minerals 2012-06, Vol.60 (3), p.278-290
Hauptverfasser:	Bouna, L, Rhouta, B, Daoudi, L, Maury, F, Amjoud, M, Senocq, F, Lafont, M. C, Jada, A, Ait Aghzzaf, A
Format:	Artikel
Sprache:	eng
Schlagworte:	Africa Agadir Basin Aluminum Basins Beidellite Biogeosciences Charge Chemical Sciences clastic sediments Clay clay mineralogy Clay minerals Dioctahedral Earth and Environmental Science Earth Sciences Earth, ocean, space Exact sciences and technology Ferruginous ferruginous composition Geochemistry Greene-Kelly Test Hofmann-Klemen Effect Inorganic chemistry Medicinal Chemistry mineral composition Mineralogy Minerals Morocco Nanoscale Science and Technology North Africa Petrology of sedimentary rocks except quaternary rocks physicochemical properties Raw rock, sediment, soil sed rocks, sediments Sedimentary petrology Sedimentary rocks sediments sheet silicates Silicates Soil Science & Conservation Specific surface Spectra Tetrahedral-Octahedral Charge Magnitude
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Beschreibung
Zusammenfassung:	The mechanism of formation of detrital, beidellite-rich clay occurring in the Agadir basin (Morocco) is well documented, but its detailed characterization is incomplete which limits its application. The aim of the present study was to provide further details of the mineralogical and physico-chemical characteristics of this clay. Bulk raw clay and its Na+-saturated,
ISSN:	0009-8604 1552-8367
DOI:	10.1346/CCMN.2012.0600305