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dc.contributorHydroQual, Inc.-
dc.contributorWater Quality Research Program (U.S.)-
dc.contributor.authorDi Toro, Dominic M.-
dc.contributor.authorLowe, Scott.-
dc.contributor.authorFitzpatrick, James F.-
dc.contributor.authorIsleib, Richard R.-
dc.descriptionContract Report-
dc.descriptionAbstract: Iron and manganese were installed as state variables in a previously developed sediment diagenesis model. The comprehensive model now incorporates nutrients, oxygen and sulfide, and iron and manganese. The model was initially calibrated using long-term mesocosm data The mesocosms contained water and sediments removed from Narragansett Sound, an estuarine environment. Validation of the model was conducted using in situ data from two freshwater systems, Onondaga Lake and Croton Reservoir. NOTE: This.pdf file is large. Allow your browser several minutes to download the file.-
dc.publisherEnvironmental Laboratory (U.S.)-
dc.publisherEngineer Research and Development Center (U.S.)-
dc.rightsApproved for public release; distribution is unlimited.-
dc.sourceThis Digital Resource was created from scans of the Print Resource-
dc.subjectEstuarine sediments-
dc.subjectMarine sediments-
dc.subjectLake sediments-
dc.subjectSediment flux-
dc.subjectMathematical models-
dc.subjectNumerical models-
dc.titleSediment flux model for manganese and iron-
Appears in Collections:Contract Report

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