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dc.contributor.authorNoubactep, Chicgoua
dc.date.accessioned2010-11-24T15:58:39Z
dc.date.available2010-11-24T15:58:39Z
dc.date.issued2009
dc.identifier.citationJournal of hazardous materials; Vol. 164.2009, No. 2/3, p. 835-837
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-33F4-A
dc.description.abstractThe validity of the specific reaction rate constants (kSA) in modelling contaminant removal in Fe0/H2O systems is questioned. It is shown that the current kSA-model does not consider the large reactive surface area provided by the in-situ formed oxide film, and thus the adsorptive interactions between contaminants and film materials. Furthermore, neither the dynamic nature of film formation nor the fact that Fe0 surface is shielded by the film is considered. Suggestions are made how the kSA-model could be further developed to possibly meet its original goal.
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.relation.ispartofseriesJournal of hazardous materials
dc.rights.urihttp://goedoc.uni-goettingen.de/goescholar/rights
dc.subject.ddc551.9
dc.subject.gokVJF 000
dc.titleOn the validity of specific rate constants (kSA) in Fe0/H2O systems
dc.typearticle
dc.subject.gokverbalUmweltgeochemie insgesamt
dc.bibliographicCitation.volume164
dc.bibliographicCitation.issue2/3
dc.bibliographicCitation.firstPage835
dc.bibliographicCitation.lastPage837
dc.identifier.doi10.23689/fidgeo-831
dc.identifier.ppn587488255
dc.type.versiondraft
dc.relation.issn0304-3894
dc.bibliographicCitation.journalJournal of hazardous materials
dc.relation.collectionGeologische Wissenschaften
dc.description.typeresearch
dc.identifier.otherdoi10.1016/j.jhazmat.2008.08.074


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