Application of a simple space-time averaged porous media model to flow in densely vegetated channels

M.R. Hoffmann

Research output: Contribution to journalArticleAcademicpeer-review

31 Citations (Scopus)

Abstract

Traditional flow modeling in open channels uses time-averaged turbulence models. These models are valid in clear fluid, but not if dense obstructions are present in the flow field. In this article we show that newly developed flow models can describe open channel flow as flow in a porous medium. Clear fluid models do not take into account drag due to the presence of the obstacles. Flow in rivers, channels, estuaries, and irrigation networks is often obstructed by vegetation, and coarse bedrock. In computer modeling applications, appropriate turbulence resistance models are either absent or empirically based In this article we develop a space-time averaged form of the Navier-Stokes equations, in order to improve modeling of flow in densely obstructed channels. We use a combination of Reynolds averaging for the turbulent flow and volume averaging in order to take into account the dense obstructions. We show that the obstacle density can be modeled by a porosity term if structural parameters of the vegetation are taken into account. In order to take these into account we develop a representative unit cell (RUC) concept, borrowed from volume averaging in porous media. Inside the RUC, local flow solutions for the Navier-Stokes equations are developed and used as closure terms in the space-time-averaged form of the Navier-Stokes equations. Our expression depends on measurable quantities such as average porosity and average vegetation diameter. It can be used in computational models to include vegetation characteristics directly, instead of approximate resistance factors. As an application, we use our theoretically derived model to compute resistance factors for Manning's equation from the structural properties of the vegetation modeled as a porous medium.
Original languageEnglish
Pages (from-to)183-191
JournalJournal of Porous Media
Volume7
Issue number3
DOIs
Publication statusPublished - 2004

Fingerprint

Porous Media
Porous materials
Vegetation
vegetation
Space-time
Navier-Stokes equation
Navier Stokes equations
Averaging
Navier-Stokes Equations
R Factors
Porosity
Obstruction
Reynolds averaging
open channel flow
Model
Open Channel Flow
porosity
Open channel flow
Open Channel
irrigation

Keywords

  • emergent vegetation
  • incompressible-flow
  • turbulence model
  • resistance

Cite this

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abstract = "Traditional flow modeling in open channels uses time-averaged turbulence models. These models are valid in clear fluid, but not if dense obstructions are present in the flow field. In this article we show that newly developed flow models can describe open channel flow as flow in a porous medium. Clear fluid models do not take into account drag due to the presence of the obstacles. Flow in rivers, channels, estuaries, and irrigation networks is often obstructed by vegetation, and coarse bedrock. In computer modeling applications, appropriate turbulence resistance models are either absent or empirically based In this article we develop a space-time averaged form of the Navier-Stokes equations, in order to improve modeling of flow in densely obstructed channels. We use a combination of Reynolds averaging for the turbulent flow and volume averaging in order to take into account the dense obstructions. We show that the obstacle density can be modeled by a porosity term if structural parameters of the vegetation are taken into account. In order to take these into account we develop a representative unit cell (RUC) concept, borrowed from volume averaging in porous media. Inside the RUC, local flow solutions for the Navier-Stokes equations are developed and used as closure terms in the space-time-averaged form of the Navier-Stokes equations. Our expression depends on measurable quantities such as average porosity and average vegetation diameter. It can be used in computational models to include vegetation characteristics directly, instead of approximate resistance factors. As an application, we use our theoretically derived model to compute resistance factors for Manning's equation from the structural properties of the vegetation modeled as a porous medium.",
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Application of a simple space-time averaged porous media model to flow in densely vegetated channels. / Hoffmann, M.R.

In: Journal of Porous Media, Vol. 7, No. 3, 2004, p. 183-191.

Research output: Contribution to journalArticleAcademicpeer-review

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