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Computational Modeling of Flow over a Spillway In Vatnsfellsstífla Dam in Iceland. Master’s Thesis Presentation Chalmers University of Technology 2007 – 02 - 02. Presentation Schedule. Introduction and background Method Theory Results Conclusions and future work.
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Computational Modeling of Flow over a SpillwayIn Vatnsfellsstífla Dam in Iceland Master’s Thesis Presentation Chalmers University of Technology 2007 – 02 - 02
Presentation Schedule • Introduction and background • Method • Theory • Results • Conclusions and future work
The spillway – characteristics • Function: cope with accidental flooding • Height above stilling basin bottom: 27.5 m • Lenght of spillway crest: 50 m • Equipped with a splitter wall and cover to prevent overtopping of the chute sidewalls • The velocity of the water is above 20 m/s (=72 km/hour!) where it flows into the stilling basin
The stilling basin – characteristics • Function: Decrease flow velocity in order to decrease risk for erosion in the river wally downstream the basin • Equipped with 28 energy dissipating baffles (height from 1.5 to 2.0 m) • Length ca. 33 m and the width increasing from 22 m in the upstream part to 33 m in the downstream part, depth ca. 7 m • Downstream the stilling basin is a 35 m long rock rip-rap made of rocks with diameter of 0.4 – 1.2 m
Background and goals • In 1999 Vattenfall in Sweden did hydraulic experiments for the spillway with a 1:30 model • In the experiments flow was investigated over the spillway, through the bottom outlet and in the stilling basin • Goals of the present study: • investigate flow over the spillway and in the stilling basin with computational methods (CFD) • compare CFD-results with experimental results
Aspects • Spillway: • water head in the reservoir vs. the discharge capacity of the spillway • Water level along the chute sidewalls • Pressure acting on the chute bottom • Stilling basin: • Water level • Pressure acting on the baffles and the end sill • Flow velocity out of the basin
Method • Identify the computational domain to be modeled (according to the goals!) • Draw the computational domain in 3D in Autodesk INVENTOR • Import the geometry into the mesh making software GAMBIT and divide the computational domain into computational cells of different size in GAMBIT • Import the mesh into the CFD-solver FLUENT, set up the numerical model, compute and monitor the solution • Postprocessing with FLUENT and MATLAB; examine the results and consider revisions to the model
The computational domain • Three different domains: • One for head vs. flow discharge • One for water level and pressure in the spillway chute • One for water level, pressure and flow velocity in the stilling basin • Why different domains? • to spare computational power and get more precise results
Grids nr. 1 – 7 as seen from above- one grid for each of the seven different cases with flow discharge of 50 – 350 m3/s, ca. 653 000 cells/grid
Cut through grids nr. 1 and 7 in the downstream end of the reservoir by the spillway crest – different water levels • Grid to the left: designed for flow discharge of 50 m3/s • Grid to the right: designed for flow discharge of 350 m3/s
Grid nr. 8: finer in the chute than grids nr. 1 – 7, ca. 1393 000 cells • The mesh in the spillway bottom • To the left: mesh 7 which is NOT specifically designed to investigate pressure and water level in the spillway chute • To the right: mesh 8 which is specifically designed to investigate pressure and water level in the spillway chute
Mesh nr. 8: finer in the chute than meshes nr. 1 - 7 • The grid perpendicular to the splitter wall • To the left: mesh 7 which is NOT specifically designed to investigate pressure and water level in the spillway chute • To the right: mesh 8 which is specifically designed to investigate pressure and water level in the spillway chute
Grid nr. 9: different types of mesh; consisting of both hexahedron cells and tetrahedron cellsca. 498 000 cells
Grid nr. 9 includes the stilling basinthough coarse in view of the size of the computational domain
Grid nr. 9: includes a simplified rock rip-rap downstream the basin
Setting up the numerical model • Define • Material properties (air, water, concrete) • Boundary conditions (inlet, outlet, walls, air pressure,...) • Operating conditions (air pressure, gravity, temperature...) • Turbulence model (standard k-ε) • Initial solution (nB: steady flow) • Convergence criteria
Theory – equations of motion and the VOF method • The continuity equation for incompressible flow: • The momentum equation for incompressible flow: • VOF method in FLUENT • assumes that the two phases (air and water) are not interpenetrating • denoting αq as the volume fraction of the q-th phase three possibilities for a given cell can be noted: • i) : the cell is empty of the q-th phase, • ii) : the cell is full of the q-th phase, • iii) : the cell contains the interphase between the q-th phase and one or more phases.
Water reservoir head vs. flow discharge; Q=CBH3/2where Q= flow discharge, C= discharge coefficient, B = length of crest, H=head
Pressure on the chute bottom – location of investigation points
Pressure on the chute bottom point A: 23 % deviation from exp-results
Pressure on the chute bottom point B: 16 % deviation from exp-results
Pressure on the chute bottom point C: 9 % deviation from exp-results
Water level in the left upstream corner of the stilling basin
Volume fraction of water in the basin (longitudinal profile) – determines the water level
Pressure on two baffles in the first row (deviations from experimental results in parantheses)
Total pressure on the basin end sill- a view under the water surface in the downstream end of the basin