ADSORPTION OF FULVIC ACID ON GOETHITE - EFFECTS OF PHYSICAL AND CHEMICAL HETEROGENEITY

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dc.contributor.author Filius J.D.
dc.contributor.author Lumsdon D.G.
dc.contributor.author Meeussen J.C.L.
dc.contributor.author Hiemstra T.
dc.contributor.author van Riemsdijk W.H.
dc.date.accessioned 2021-01-21T08:45:00Z
dc.date.available 2021-01-21T08:45:00Z
dc.date.issued 2000
dc.identifier https://elibrary.ru/item.asp?id=200780
dc.identifier.citation Geochimica et Cosmochimica Acta, 2000, 64, 1, 51-60
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/23462
dc.description.abstract The adsorption of fulvic acid by goethite was determined experimentally as a function of concentration, pH, and ionic strength. The data were described with the CD-MUSIC model of Hiemstra and Van Riemsdijk (1996), which allows the distribution of charge of the bound fulvate molecule over a surface region. Simultaneously, the concentration, pH, and salt dependency of the binding of fulvic acid can be described. Using the same parameters, the basic charging behavior of the goethite in the absence of fulvic acid could be described well. The surface species used in the model indicate that inner sphere coordination of carboxylic groups of the fulvate molecule is important at low pH, whereas at high pH the outer sphere coordination with reactive groups of the fulvate molecule with high proton affinity is important.
dc.title ADSORPTION OF FULVIC ACID ON GOETHITE - EFFECTS OF PHYSICAL AND CHEMICAL HETEROGENEITY
dc.type Статья


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