2011
DOI: 10.1016/j.clay.2011.05.021
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Kinetic and equilibrium studies for the adsorption of acid nucleic bases onto K10 montmorillonite

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Cited by 50 publications
(33 citation statements)
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“…Water molecules are allocated in the interlayer sheet and are coordinated by the exchangeable cations. The size of the cations influences the (001) basal space of the structure (Sciascia et al, 2011). The inorganic-organic ion exchange between the desired organic cations and exchangeable inorganic cations in the interlayers of clays allows to obtain organoclays, which are effective adsorbents for organic and aromatic contaminants in pollution treatment (Meng et al, 2009).…”
Section: Introductionmentioning
confidence: 99%
“…Water molecules are allocated in the interlayer sheet and are coordinated by the exchangeable cations. The size of the cations influences the (001) basal space of the structure (Sciascia et al, 2011). The inorganic-organic ion exchange between the desired organic cations and exchangeable inorganic cations in the interlayers of clays allows to obtain organoclays, which are effective adsorbents for organic and aromatic contaminants in pollution treatment (Meng et al, 2009).…”
Section: Introductionmentioning
confidence: 99%
“…Among them are the nanoclays, like imogolite and halloysite that both have a hollow tubular shape, which have a particular relevance for materials design. Imogolite, Al 2 SiO 3 (OH) 4, possesses an external diameter of ca. 25 Å and an internal diameter of ca.…”
Section: ■ Introductionmentioning
confidence: 99%
“…The different chemistry at each surface offers the opportunity to control the selective interaction with ionic molecules. 3,4 Recent studies proved that HNTs are ecological, biocompatible, and dispersible in water even at very high concentrations where they can form liquid crystalline phases. 5,6 HNTs are abundant all over the world and consequently are available at low cost.…”
Section: ■ Introductionmentioning
confidence: 99%
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“…Sillitoe 2010; Kadir et al 2011;Premović et al 2012) and weathering pathways controlling processes of clay-mineral formation in acidic soils (Uzarowicz et al 2011). Many studies were devoted to acid treatment of bentonites or smectites (Fijał et al 1975;Číčel & Novák 1976;Stoch et al 1977;Novák & Číčel 1978;Komadel et al 1993Komadel et al , 1996Tkáč et al 1994;Breen et al 1997;Madejová et al 1998;Rožić et al 2010Rožić et al , 2011Sciascia et al 2011), illites, micas or kaolinites (Bahranowski et al 1993;Ganor et al 1995;Kalinowski & Schweda 1996;Dubíková et al 2002;Hradil et al 2002;Jozefaciuk & Bowanko 2002;Pentrák et al 2009Pentrák et al , 2010Nguetnkam et al 2011;Valášková et al 2011;Worasith et al 2011 Al) in octahedral sheets leads to enhancement of the clay mineral dissolution due to higher negative layer charge density (Pentrák et al 2012). The tetrahedra are rearranged from layered into three-dimensional adjustment.…”
Section: Acidification Of the Claysmentioning
confidence: 99%