Hydromorphology of Piedmont Floodplain Soils

dc.contributor.advisorRabenhorst, Martin Cen_US
dc.contributor.authorCastenson, Karen Lynnen_US
dc.contributor.departmentPlant Science and Landscape Architecture (PSLA)en_US
dc.date.accessioned2004-06-04T05:16:15Z
dc.date.available2004-06-04T05:16:15Z
dc.date.issued2004-05-07en_US
dc.description.abstractAlluvial soils situated on middle locations along Mid-Atlantic Piedmont floodplains lack characteristic redoximorphic features that allow them to meet a current field indicator of hydric soil. Although these soils appear to be located in wetlands based on their hydrologic, vegetative, and electrochemical status; there is no hydric soil indicator that accurately includes soils on these landscapes. Two research sites in Maryland and one in Delaware were instrumented along a hydrosequence. Depth to water table, redox potential, and soil temperature were measured. Redox potential measurements of the hydric and possible hydric soil conclude that Fe(III) is predicted to be reduced to Fe(II) for a significant period of time during the growing season. Based on data collected over three years, the possible hydric soil was confirmed hydric. An alternate hydric soil indicator has been proposed for these landscapes.en_US
dc.format.extent3863916 bytes
dc.format.mimetypeapplication/pdf
dc.identifier.urihttp://hdl.handle.net/1903/1354
dc.language.isoen_US
dc.relation.isAvailableAtDigital Repository at the University of Marylanden_US
dc.relation.isAvailableAtUniversity of Maryland (College Park, Md.)en_US
dc.subject.pqcontrolledAgriculture, Soil Scienceen_US
dc.subject.pquncontrolledhydric soilen_US
dc.subject.pquncontrolledwetlanden_US
dc.subject.pquncontrolledfloodplainen_US
dc.subject.pquncontrolledPiedmonten_US
dc.subject.pquncontrolledredoximorphic featuresen_US
dc.titleHydromorphology of Piedmont Floodplain Soilsen_US
dc.typeThesisen_US

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