1965
DOI: 10.1039/tf9656102024
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Adsorption of amino-acids and peptides by montmorillonite and illite. Part 2.—Physical adsorption

Abstract: The adsorption of four naturally occurring a-amino-acids on calcium montmorillonite and sodium and calcium illite has been studied and compared with that of glycine and its di-, tri-and tetra-peptides. Linear isotherms were obtained for adsorption by the calcium clays. These have been treated in terms of a constant partition of solute between the solution and the Stern layer of the adsorbent. Free energies of adsorption were obtained from the selectivity coefficients for the partition reaction. The relative ma… Show more

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Cited by 75 publications
(47 citation statements)
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“…Greenland et al (1962,1965) investigated the interactions of various amino acids with H-, Na-, and Ca-montmorillonites [19,20]. Arginine, histidine, and lysine adsorbed to Na-and Ca-montmorillonites by cation exchange.…”
Section: Adsorption Of Amino Acids By Clay Mineralsmentioning
confidence: 99%
“…Greenland et al (1962,1965) investigated the interactions of various amino acids with H-, Na-, and Ca-montmorillonites [19,20]. Arginine, histidine, and lysine adsorbed to Na-and Ca-montmorillonites by cation exchange.…”
Section: Adsorption Of Amino Acids By Clay Mineralsmentioning
confidence: 99%
“…In addition, the solubility of tetra-gly is much smaller than mono-and other oligo-glys. However, the slope of the isotherm for adsorption of tetra-gly was not so steep, as compared with those of mono-, di-, tri-and tetra-gly by Ca2+-montmorillonite by Greenland (1965). [7] For that, the adsorption of tetra-gly might be affected by the mesopore for FSM-16.…”
Section: Introductionmentioning
confidence: 99%
“…More recently, Lee et al (1989), Smith et al (1990), and Jaynes and Boyd ( 199 l) attributed this mechanism to the enhanced sorption of neutral organic molecules on soils and clays exchanged with organic cations with one or more long alkyl groups. Because clay minerals saturated with metal cations contain negligible amounts of organic matter, the sorption of neutral organic molecules on these clays only involves the partition mechanism proposed by the earlier investigators (Greenland et al, 1962(Greenland et al, , 1965Theng, 1972;Theng and Scharpenseel, 1976).…”
mentioning
confidence: 99%
“…It should be noted that two types of partition mechanisms have been proposed. Earlier, Greenland et al (1962Greenland et al ( , 1965, Theng (1972), and Theng and Scharpenseel (1976) proposed that the linear sorption isotherm observed with clay minerals can be characterized by a partition of a solute between the bulk and intercrystalline water. Later, Chiou et al (1979Chiou et al ( , 1983 proposed that the sorption of neutral organic chemicals is essentially a partition process between the soil organic matter and soil water.…”
mentioning
confidence: 99%