Geochemistry of Colloid Systems 1979
DOI: 10.1007/978-3-642-67041-1_8
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Colloid Geochemistry of Clay Minerals

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Cited by 8 publications
(5 citation statements)
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“…It should be noted, however, that perlite is in principle a negatively charged aluminosilicate (unbound terminal –SiO – groups and isomorphous substitutions) and that the balancing cations are very labile, i.e., easily exchangeable. Thus, adsorption of AB 1 in patches onto perlite unravels, besides the structural diversity, the charge heterogeneity in perlite possibly accompanying the “broken-bond” or “edge” existing surfaces where the unsatisfied atoms may bring positive charges (Yariv & Cross, 1979 ).…”
Section: Resultsmentioning
confidence: 99%
“…It should be noted, however, that perlite is in principle a negatively charged aluminosilicate (unbound terminal –SiO – groups and isomorphous substitutions) and that the balancing cations are very labile, i.e., easily exchangeable. Thus, adsorption of AB 1 in patches onto perlite unravels, besides the structural diversity, the charge heterogeneity in perlite possibly accompanying the “broken-bond” or “edge” existing surfaces where the unsatisfied atoms may bring positive charges (Yariv & Cross, 1979 ).…”
Section: Resultsmentioning
confidence: 99%
“…In addition, negative surface charge in layers may be accounted for by broken bonds at the edges of the sheets, on noncleavage surfaces [ 117 ]. This second source of charge is generally negative and pH dependent [ 21 ].…”
Section: Natural Mineral Catalystsmentioning
confidence: 99%
“…This second source of charge is generally negative and pH dependent [ 21 ]. The unsatisfied charges may be balanced by the sorption of cations and anions, either specifically by chemisorption or nonspecifically by electrostatic attraction, the latter ions being easily exchangeable [ 117 ].…”
Section: Natural Mineral Catalystsmentioning
confidence: 99%
“…are the well-studied phyllosilicate minerals in different fields. Because the Al atoms in pyrophyllite exist within the structure of the octahedral sheet, they do not appear on cleavage surfaces during grinding in mill (Yariv and Cross, 1979). Cleavage occurs between two tetrahedral sheets in adjacent layers, resulting in lower free energy on the exposed surface of the ground pyrophyllite particles and increased hydrophobicity of the particles (Newton and Sposito, 2015).…”
Section: Introductionmentioning
confidence: 99%