2015
DOI: 10.1071/en14157
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Interaction of humic acids with soil minerals: adsorption and surface aggregation induced by Ca2+

Abstract: Environmental context Humic acids, important components of natural organic matter in soils, sediments and aquatic media, can interact with the surface of minerals affecting key environmental processes. In the presence of calcium, humic acids can also interact among themselves leading to molecular aggregates. We demonstrate that a solid mineral surface facilitates the formation of humic acid aggregates, and thus surface aggregation occurs under conditions where normal aggregation in solution does not occur. A… Show more

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Cited by 45 publications
(20 citation statements)
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“…According to the literature, Ca 2+ has the ability of producing aggregation of alginate molecules above a certain cation concentration due to the complexation of the carboxylic groups (Kloster and Avena 2015). Thus, the above quantitative comparison of the amounts of adsorbed alginate and the unadsorbed alginate allows us to hypothesize a heterocoagulation mechanism between the alginate-covered CuO NPs and the unabsorbed alginate under high concentration of Ca(NO 3 ) 2 in this study.…”
Section: Hetero-coagulation Mechanism Between Cuo Nps and The Unabsormentioning
confidence: 93%
“…According to the literature, Ca 2+ has the ability of producing aggregation of alginate molecules above a certain cation concentration due to the complexation of the carboxylic groups (Kloster and Avena 2015). Thus, the above quantitative comparison of the amounts of adsorbed alginate and the unadsorbed alginate allows us to hypothesize a heterocoagulation mechanism between the alginate-covered CuO NPs and the unabsorbed alginate under high concentration of Ca(NO 3 ) 2 in this study.…”
Section: Hetero-coagulation Mechanism Between Cuo Nps and The Unabsormentioning
confidence: 93%
“…Humic and fulvic acids possess similar structures, but have different molecular weights and contents in functional groups; humic acids have higher molecular weight and less oxygen-containing functional groups than fulvic acids [9]. These chemical differences make humic acids less soluble than fulvic acids, decreasing their solubility at higher polyvalent cation contents, and lower pH due to aggregation of humic molecules themselves by cation bridging and their adsorption onto soil particles by reduced electrostatic repulsion [12][13][14][15]. Humic and fulvic acids present in humic substances contain a great variety of functional groups that are very active adsorption sites-especially carboxyl and phenolic OH (acidic groups)-and have strong complexation ability with metal ions [8,9,11,16].…”
Section: Introductionmentioning
confidence: 99%
“…The decrease in calcium content is in accordance with the decrease in lime content. Kloster and Avena (2015) reported that the addition of a small dose of humic acid resulted in a little increase in calcium content but that adding a large dose of humic acid decreased the calcium content.…”
Section: Discussionmentioning
confidence: 99%