1964
DOI: 10.1016/0016-7037(64)90009-2
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Cation exchange properties of humic acids and their importance in the geochemical enrichment of UO2++ and other cations

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Cited by 201 publications
(54 citation statements)
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“…Uranium is not reduced by interaction with humic acids, but rather is strongly adsorbed (Nash et al, 1981). Szalay (1964) likened humic acids to cation exchange columns, and found that Langmuir iso-pH curves described well the adsorption equilibrium of humic acids (see section on Modelling). The Langmuir equation is characterized by two constants representing a geochemical enrichment factor (GEF) and the adsorption capacity.…”
Section: Adsorptionmentioning
confidence: 85%
See 1 more Smart Citation
“…Uranium is not reduced by interaction with humic acids, but rather is strongly adsorbed (Nash et al, 1981). Szalay (1964) likened humic acids to cation exchange columns, and found that Langmuir iso-pH curves described well the adsorption equilibrium of humic acids (see section on Modelling). The Langmuir equation is characterized by two constants representing a geochemical enrichment factor (GEF) and the adsorption capacity.…”
Section: Adsorptionmentioning
confidence: 85%
“…The interaction of humic substances with U binding to algal cells was also studied by Szalay (1964). The adsorptive properties of humic acids probably relate to the carboxyl and hydroxyl groups associated with the breakdown of lignin.…”
Section: Adsorptionmentioning
confidence: 99%
“…At ambient temperatures (-25 OC), U is adsorbed to humic substances through rapid ion-exchange and complexation processes with carboxylic and other acidic functional groups (Idiz et al 1986 Borovec et al 1979, Szalay 1964 without reduction to the U(IV) species. It has been suggested that U(VI) adsorbed (or fixed) to organic matter may undergo reduction to U(IV) followed by precipitation of UO, (Andreyev and Chumachenko 1964).…”
Section: Sorptionmentioning
confidence: 99%
“…The source of UO 2 +2 is probably apatite, which is a known host for U in igneous rocks. However, uranium in sedimentary rocks is invariably associated with organic matter (Abdel-Gawad and Kerr, 1961;Szalay, 1964;Mohan et al, 1982;Drew Ilger et al, 1987) or with accessory detrital minerals such as zircon (ZrSiO 4 ). Humic acids within the organic matter sequester UO 2 +2 through complexation on carboxyl functional groups (R-COOH) (Szalay, 1964;Drew Ilger et al, 1987) Nefedov et al, 1998) leading to enrichment factors over contacting groundwaters by a factor as high as 10,000 (Szalay, 1964 + although direct microbial reduction of U(VI) to U(IV) has also been observed under anaerobic conditions (Suzuki et al, 2005).…”
Section: Mercurymentioning
confidence: 99%