Hydrodynamics of vegetated channels

This paper highlights some recent trends in vegetation hydrodynamics, focusing on conditions within channels and spanning spatial scales from individual blades, to canopies or vegetation patches, to the channel reach. At the blade scale, the boundary layer formed on the plant surface plays a role in...

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Vydané v:	Journal of hydraulic research Ročník 50; číslo 3; s. 262 - 279
Hlavný autor:	Nepf, Heidi M.
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Delft Taylor & Francis 01.06.2012 International Association for Hydraulic Research Taylor & Francis Ltd
Predmet:	blade boundary layer Boundary layer Boundary layers Canopies channel resistance Earth sciences Earth, ocean, space Exact sciences and technology Flow resistance Hydrodynamics Hydrology Hydrology. Hydrogeology Nutrient flow Nutrient uptake sediment transport Studies turbulence Vegetation stress channel resistance boundary layer mixing vegetation hydrodynamics turbulence blade boundary layer nutrients surface water hydraulics sediment transport channels geometry methodology
ISSN:	0022-1686, 1814-2079
On-line prístup:	Získať plný text
Tagy:	Pridať tag Žiadne tagy, Buďte prvý, kto otaguje tento záznam!

Abstract	This paper highlights some recent trends in vegetation hydrodynamics, focusing on conditions within channels and spanning spatial scales from individual blades, to canopies or vegetation patches, to the channel reach. At the blade scale, the boundary layer formed on the plant surface plays a role in controlling nutrient uptake. Flow resistance and light availability are also influenced by the reconfiguration of flexible blades. At the canopy scale, there are two flow regimes. For sparse canopies, the flow resembles a rough boundary layer. For dense canopies, the flow resembles a mixing layer. At the reach scale, flow resistance is more closely connected to the patch-scale vegetation distribution, described by the blockage factor, than to the geometry of individual plants. The impact of vegetation distribution on sediment movement is discussed, with attention being paid to methods for estimating bed stress within regions of vegetation. The key research challenges of the hydrodynamics of vegetated channels are highlighted.
AbstractList	This paper highlights some recent trends in vegetation hydrodynamics, focusing on conditions within channels and spanning spatial scales from individual blades, to canopies or vegetation patches, to the channel reach. At the blade scale, the boundary layer formed on the plant surface plays a role in controlling nutrient uptake. Flow resistance and light availability are also influenced by the reconfiguration of flexible blades. At the canopy scale, there are two flow regimes. For sparse canopies, the flow resembles a rough boundary layer. For dense canopies, the flow resembles a mixing layer. At the reach scale, flow resistance is more closely connected to the patch-scale vegetation distribution, described by the blockage factor, than to the geometry of individual plants. The impact of vegetation distribution on sediment movement is discussed, with attention being paid to methods for estimating bed stress within regions of vegetation. The key research challenges of the hydrodynamics of vegetated channels are highlighted. This paper highlights some recent trends in vegetation hydrodynamics, focusing on conditions within channels and spanning spatial scales from individual blades, to canopies or vegetation patches, to the channel reach. At the blade scale, the boundary layer formed on the plant surface plays a role in controlling nutrient uptake. Flow resistance and light availability are also influenced by the reconfiguration of flexible blades. At the canopy scale, there are two flow regimes. For sparse canopies, the flow resembles a rough boundary layer. For dense canopies, the flow resembles a mixing layer. At the reach scale, flow resistance is more closely connected to the patch-scale vegetation distribution, described by the blockage factor, than to the geometry of individual plants. The impact of vegetation distribution on sediment movement is discussed, with attention being paid to methods for estimating bed stress within regions of vegetation. The key research challenges of the hydrodynamics of vegetated channels are highlighted. [PUBLICATION ABSTRACT]
Author	Nepf, Heidi M.
Author_xml	– sequence: 1 givenname: Heidi M. surname: Nepf fullname: Nepf, Heidi M. email: hmnepf@mit.edu organization: Department of Civil and Environmental Engineering , Massachusetts Institute of Technology
BackLink	http://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=26122025$$DView record in Pascal Francis
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Snippet	This paper highlights some recent trends in vegetation hydrodynamics, focusing on conditions within channels and spanning spatial scales from individual...
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SubjectTerms	blade boundary layer Boundary layer Boundary layers Canopies channel resistance Earth sciences Earth, ocean, space Exact sciences and technology Flow resistance Hydrodynamics Hydrology Hydrology. Hydrogeology Nutrient flow Nutrient uptake sediment transport Studies turbulence Vegetation
Title	Hydrodynamics of vegetated channels
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