2012
DOI: 10.1007/978-1-4471-4108-2_3
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Clays and Clay Minerals as Layered Nanofillers for (Bio)Polymers

Abstract: This introductory chapter presents the most relevant structural, physical, and chemical properties of clay minerals for the formation of nanocomposites with polymers. The general principles of silicates classification are outlined in order to better understand the structures of the various types of clay minerals as phyllosilicates. Cation exchange capacity (CEC), surface area, porosity, and rheological properties of clay minerals are briefly discussed. The physico-chemical properties of clay mineral layers, in… Show more

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Cited by 27 publications
(20 citation statements)
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“…The layer is the result of the condensation of tetrahedral sheets (T) and octahedral sheets (O) (Bergaya et al 2012). Phyllosilicates are often referred to as 1:1 or 2:1.…”
Section: Nanofillersmentioning
confidence: 99%
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“…The layer is the result of the condensation of tetrahedral sheets (T) and octahedral sheets (O) (Bergaya et al 2012). Phyllosilicates are often referred to as 1:1 or 2:1.…”
Section: Nanofillersmentioning
confidence: 99%
“…In fact, the lath-like fragments of T-O-T structure extend along the c axis, being connected by siloxane bridges (Fig. 8) (Bergaya et al 2012;Duquesne et al 2007). Some isomorphic substitutions occur inside these central layers creating a negative charge naturally counterbalanced by the presence of inorganic cations (Na + , Ca 2+ , etc.).…”
Section: Nanofillersmentioning
confidence: 99%
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“…Among the smectite groups, montmorillonite (Mt) has held the limelight in the preparation of OC because of its moderate charge density and cation exchange capacity (CEC), interlayer swelling ability, and propensity for intercalating simple and polymeric organic compounds (Bergaya et al, 2011b(Bergaya et al, , 2012Murray, 2000;SwartzenAllen and Matijevic, 1974;Theng, 1974Theng, , 2012, not to mention its availability and low cost. At the same time, quaternary ammonium halides bearing long alkyl chains have been widely used for modifying clay minerals because of the ease with which the QAC can exchange the inorganic compensator exchangeable cation in the interlayer space of Mt.…”
Section: Introductionmentioning
confidence: 99%