Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5714
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dc.contributor.authorallGiraldi, D.; Department of Civil Engineering – University of Pisa, Pisa, Italyen
dc.contributor.authorallDe' Michieli Vitturi, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallZaramella, M.; Department of Hydraulic, Maritime, Environmental and Geotechnical Engineering – University of Padua, Padova, Italyen
dc.contributor.authorallMarion, A.; Department of Hydraulic, Maritime, Environmental and Geotechnical Engineering – University of Padua, Padova, Italyen
dc.contributor.authorallIannelli, R.; Department of Civil Engineering – University of Pisa, Pisa, Italyen
dc.date.accessioned2010-01-21T13:56:46Zen
dc.date.available2010-01-21T13:56:46Zen
dc.date.issued2009-02-09en
dc.identifier.urihttp://hdl.handle.net/2122/5714en
dc.description.abstractTypical unsteady unsaturated conditions can profoundly affect the hydrodynamics of vertical subsurface flow constructed wetlands. In this study we analyzed the hydrodynamics of a 33 m2 vertical flow pilot plant, treating municipal secondary effluents. Three different saturation conditions were analyzed under several constant flux regimes: complete saturation, partial saturation with the free water table 20 cm over the bottom of the bed, and complete drainage. Tracer tests were performed in steady state conditions by dosing rhodamine WT as square input signals. Breakthrough curves were analyzed by means of both a classical residence time distribution analysis and an originally developed numerical plug-flow model with longitudinal dispersion adapted to the unsaturated conditions. We found that the degree of global mixing in the vertical flow constructed wetland increased as the water content increased; this effect was controlled by the hydraulic residence time of the system. Conversely, the degree of local mixing was inversely affected by water content; the dispersivity was 4.5, 10, and 14 cm for fully saturated, partially saturated and draining conditions, respectively. We explain the dependency of dispersivity on water content in physical terms; however, further studies are needed to mathematically include this relationship in numerical models that describe the behaviour of vertical flow constructed wetlands.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofEcological Engineeringen
dc.relation.ispartofseries2/35(2009)en
dc.relation.isversionofhttp://hdl.handle.net/2122/4540en
dc.subjectConstructed wetlandsen
dc.subjectVertical flowen
dc.subjectHydrodynamicsen
dc.subjectTracer testsen
dc.subjectRhodamine WTen
dc.subjectModellingen
dc.subjectUnsaturated flowen
dc.subjectDispersivityen
dc.titleHydrodynamics of vertical subsurface flow constructed wetlands: Tracer tests with rhodamine WT and numerical modellingen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber265-273en
dc.subject.INGV03. Hydrosphere::03.02. Hydrology::03.02.06. Water resourcesen
dc.subject.INGV05. General::05.01. Computational geophysics::05.01.99. General or miscellaneousen
dc.subject.INGV05. General::05.08. Risk::05.08.01. Environmental risken
dc.identifier.doi10.1016/j.ecoleng.2008.06.004en
dc.description.obiettivoSpecifico3.8. Geofisica per l'ambienteen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorGiraldi, D.en
dc.contributor.authorDe' Michieli Vitturi, M.en
dc.contributor.authorZaramella, M.en
dc.contributor.authorMarion, A.en
dc.contributor.authorIannelli, R.en
dc.contributor.departmentDepartment of Civil Engineering – University of Pisa, Pisa, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentDepartment of Hydraulic, Maritime, Environmental and Geotechnical Engineering – University of Padua, Padova, Italyen
dc.contributor.departmentDepartment of Hydraulic, Maritime, Environmental and Geotechnical Engineering – University of Padua, Padova, Italyen
dc.contributor.departmentDepartment of Civil Engineering – University of Pisa, Pisa, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptDepartment of Civil Engineering, University of Pisa, Pisa, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptDepartment of Hydraulic, Maritime, Environmental and Geotechnical Engineering – University of Padua, Padova, Italy-
crisitem.author.deptDepartment of Hydraulic, Maritime, Environmental and Geotechnical Engineering, University of Padova, Padova, Italy-
crisitem.author.deptDepartment of Civil Engineering, University of Pisa, Pisa, Italy-
crisitem.author.orcid0000-0002-6750-9245-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent05. General-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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