DISSOLUTION OF FE(III) (HYDR) OXIDES BY METAL-EDTA COMPLEXES

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dc.contributor.author Nowack B.
dc.contributor.author Sigg L.
dc.date.accessioned 2020-12-16T04:09:08Z
dc.date.available 2020-12-16T04:09:08Z
dc.date.issued 1997
dc.identifier https://elibrary.ru/item.asp?id=274950
dc.identifier.citation Geochimica et Cosmochimica Acta, 1997, , 5, 951-963
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/20943
dc.description.abstract The dissolution of Fe(III) (hydr)oxides (goethite and hydrous ferric oxide) by metal-EDTA complexes occurs by ligand-promoted dissolution. The process is initiated by the adsorption of metal-EDTA complexes to the surface and is followed by the dissociation of the complex at the surface and the release of Fe(III)EDTA into solution. The dissolution rate is decreased to a great extent if EDTA is complexed by metals in comparison to the uncomplexed EDTA. The rate decreases in the order EDTA # CaEDTA > PbEDTA > ZnEDTA > CuEDTA > Co(II)EDTA > NiEDTA. Two different rate-limiting steps determine the dissolution process: (1) detachment of Fe(III) from the oxide-structure and (2) dissociation of the metal-EDTA complexes. In the case of goethite, step 1 is slower than step 2 and the dissolution rates by various metals are similar. In the case of hydrous ferric oxide, step 2 is rate-limiting and the effect of the complexed metal is very pronounced.
dc.title DISSOLUTION OF FE(III) (HYDR) OXIDES BY METAL-EDTA COMPLEXES
dc.type Статья


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