MODELING THE BINDING OF FULVIC ACID BY GOETHITE: THE SPECIATION OF ADSORBED FA MOLECULES

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dc.contributor.author Filius J.D.
dc.contributor.author Meeussen J.C.L.
dc.contributor.author Lumsdon D.G.
dc.contributor.author Hiemstra T.
dc.contributor.author van Riemsdijk W.H.
dc.date.accessioned 2021-12-24T05:12:37Z
dc.date.available 2021-12-24T05:12:37Z
dc.date.issued 2003
dc.identifier https://www.elibrary.ru/item.asp?id=1469668
dc.identifier.citation Geochimica et Cosmochimica Acta, 2003, 67, 8, 1463-1474
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/33782
dc.description.abstract Under natural conditions, the adsorption of ions at the solid-water interface may be strongly influenced by the adsorption of organic matter. In this paper, we describe the adsorption of fulvic acid (FA) by metal(hydr)oxide surfaces with a heterogeneous surface complexation model, the ligand and charge distribution (LCD) model. The model is a self-consistent combination of the nonideal competitive adsorption (NICA) equation and the CD-MUSIC model. The LCD model can describe simultaneously the concentration, pH, and salt dependency of the adsorption with a minimum of only three adjustable parameters. Furthermore, the model predicts the coadsorption of protons accurately for an extended range of conditions. Surface speciation calculations show that almost all hydroxyl groups of the adsorbed FA molecules are involved in outer sphere complexation reactions. The carboxylic groups of the adsorbed FA molecule form inner and outer sphere complexes. Furthermore, part of the carboxylate groups remain noncoordinated and deprotonated.
dc.title MODELING THE BINDING OF FULVIC ACID BY GOETHITE: THE SPECIATION OF ADSORBED FA MOLECULES
dc.type Статья


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