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Grant: Discovery Grants Program - Individual

University of Regina

$31,500.00

Modeling flow and pressure distribution by multilayer averaged equations

FY 2006-07

Summary
A multilayer model is in fact the solution of layer averaged momentum equations (which are similar to depth averaged equations) in a number of layers. One of the advantages of a multi-layer system is that due to this similarity, a three-dimensional multilayer model can be developed from any two-dimensional depth-averaged program. To upgrade any depth-averaged model, additional terms should be added to the momentum equations to account for friction and mass transfer between the layers. The momentum equations can be solved in a similar manner for each layer. Following this step, the flow depth is updated and the iteration process continues until convergence is achieved. A few researchers have also applied the multilayer method in open channels with the same assumption of horizontal layers of constant thickness. This assumption causes some restriction in channel flows since the top layer must accommodate all of the water surface variation, it may become too thick and model accuracy is reduced in different locations. An additional complication occurs when the lower layers of flow intersect the bed topography and the imposing boundary conditions become very complicated.  The proposed model proposed herein incorporates the multilayer modeling and depth-averaged equations to become the multilayer depth averaged model with modifications in layer selection and turbulence model. The model differs from classical multilayer models and classical depth averaged models so that the proposed model will simulate not only the averaged velocities and flow depth but also predict the velocity and shear profiles over the depth. The model will be modified and expanded for simulations of hydraulic jump and flow in curved open channels. Modeling results will be compared with experimental data and numerical results by other three-dimensional hydrodynamatic models. These will verify whether the model has the capability to predict flows in complex three-dimensional flow conditions.
Program
Discovery Grants Program - Individual
Location
Saskatchewan, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data

As published

Application id
109585-2006
Name nom
Jin, YeeChung
Department département
Engineering, Faculty of
Organization id
17
Institution établissement
University of Regina
Province en
Saskatchewan
Province fr
Saskatchewan
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2006
Competition year année de concours
2006
Award amount
31500
Program id
RGPIN
Program name en
Discovery Grants Program - Individual
Program name fr
Programme de subventions à la découverte - individuelles
Group en
Discovery grants programs
Group fr
Programmes de subventions à la découverte
Committee code
6
Committee name en
Civil Engineering
Committee name fr
Génie civil
Area of application code
405
Area of application group en
Environment
Area of application group fr
Environnement
Area of application en
Modelling and mathematical simulation of natural processes
Area of application fr
Modélisation et simulation mathématique des processus naturels
Research subject code
1005
Research subject group en
Civil engineering
Research subject group fr
Génie civil
Research subject en
Hydraulic engineering
Research subject fr
Génie hydraulique
Partie
1
Nb partie
5
Application title
Modeling flow and pressure distribution by multilayer averaged equations
Keyword
NA
Application summary
A multilayer model is in fact the solution of layer averaged momentum equations (which are similar to depth averaged equations) in a number of layers. One of the advantages of a multi-layer system is that due to this similarity, a three-dimensional multilayer model can be developed from any two-dimensional depth-averaged program. To upgrade any depth-averaged model, additional terms should be added to the momentum equations to account for friction and mass transfer between the layers. The momentum equations can be solved in a similar manner for each layer. Following this step, the flow depth is updated and the iteration process continues until convergence is achieved. A few researchers have also applied the multilayer method in open channels with the same assumption of horizontal layers of constant thickness. This assumption causes some restriction in channel flows since the top layer must accommodate all of the water surface variation, it may become too thick and model accuracy is reduced in different locations. An additional complication occurs when the lower layers of flow intersect the bed topography and the imposing boundary conditions become very complicated.  The proposed model proposed herein incorporates the multilayer modeling and depth-averaged equations to become the multilayer depth averaged model with modifications in layer selection and turbulence model. The model differs from classical multilayer models and classical depth averaged models so that the proposed model will simulate not only the averaged velocities and flow depth but also predict the velocity and shear profiles over the depth. The model will be modified and expanded for simulations of hydraulic jump and flow in curved open channels. Modeling results will be compared with experimental data and numerical results by other three-dimensional hydrodynamatic models. These will verify whether the model has the capability to predict flows in complex three-dimensional flow conditions.