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The morphodynamics of super- and transcritical flow
Yves Zech Sandra Soares Frazão Benoit Spinewine, Mourad Bellal, Céline Savary Université catholique de Louvain, Belgium
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Morphodynamics and floods
Sudden changes in discharge and levels Regime discontinuities Supercritical flow Intense transport Instabilities and bed forms Transcritical flow Boundary conditions RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Overview The basic model: Saint-Venant - Exner Regime and solid transport Two-layer model Supercritical flow and bed forms Transcritical flow and boundary conditions RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Overview The basic model: Saint-Venant - Exner Regime and solid transport Two-layer model Supercritical flow and bed forms Transcritical flow and boundary conditions RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The basic model : St-Venant - Exner
RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The basic model : St-Venant - Exner
Closure Friction slope Sf Solid discharge qs RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Overview The basic model: Saint-Venant - Exner Regime and solid transport Two-layer model Supercritical flow and bed forms Transcritical flow and boundary conditions RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Regime and solid transport
Grain mobilization : Shields - van Rijn RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Regime and solid transport
Solid discharge RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Regime and solid transport
High transport intensity Common formulae (range of applicability) If interaction between grains > interaction grains / liquid flow debris flow Sudden changes in transport intensity Acceleration and deceleration: lag exchanges of momentum two-layer model Two-layer model instead of time and space lag RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Overview The basic model: Saint-Venant - Exner Regime and solid transport Two-layer model The model Uniform flow and calibration Application to dam-break wave Supercritical flow and bed forms Transcritical flow and boundary conditions RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Overview The basic model: Saint-Venant - Exner Regime and solid transport Two-layer model The model Uniform flow and calibration Application to dam-break wave Supercritical flow and bed forms Transcritical flow and boundary conditions RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model Distinct velocities Distinct concentrations pure water mixture u z RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model Closure : Erosion Shear stresses and Shear stress RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Overview The basic model: Saint-Venant - Exner Regime and solid transport Two-layer model The model Uniform flow and calibration Application to dam-break wave Supercritical flow and bed forms Transcritical flow and boundary conditions RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model Uniform flow conditions : RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model Uniform flow conditions : RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model Uniform flow conditions : RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model Uniform flow conditions : 8 equations 12 variables RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model Uniform flow conditions : calibration RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model Uniform flow conditions : RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model Uniform flow conditions : RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model Uniform flow conditions : RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Two-layer model Uniform flow conditions : qs (m3/s/m) hw : Manning qs : Meyer-Peter - Müller hw : 2-layers qs : MPM hw and qs : 2-layer model Fr RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Overview The basic model: Saint-Venant - Exner Regime and solid transport Two-layer model The model Uniform flow and calibration Application to dam-break wave Supercritical flow and bed forms Transcritical flow and boundary conditions RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Dam-break wave t = 0.0 s t = 0.2 s t = 0.4 s RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Dam-break wave Physical description RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Dam-break wave : flat bed
Flat bed case PVC Gates moving up h0 hs RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Dam-break wave : flat bed
Sediment layer underestimated: the concentration is the same in the sediment layer although this one has to de-bulk for moving t = 0.2 s RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Dam-break wave : flat bed
Sediment layer underestimated: the concentration is the same in the sediment layer although this one has to de-bulk for moving t = 0.4 s RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Dam-break wave : flat bed
Sediment layer underestimated: the concentration is the same in the sediment layer although this one has to de-bulk for moving t = 0.6 s RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Dam-break wave : flat bed
Sediment layer underestimated: the concentration is the same in the sediment layer although this one has to de-bulk for moving t = 0.8 s RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Dam-break wave : flat bed
Sediment layer underestimated: the concentration is the same in the sediment layer although this one has to de-bulk for moving t = 1.0 s RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Dam-break wave : stepped bed
Stepped-bed case Materials PVC Sand Louvain new flume Gates moving down RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Dam-break wave : stepped bed
RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Experimental set-up RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Dam-break wave : stepped bed
PVC - t = 3 t0 z/h0 x/h0 RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Dam-break wave : stepped bed
PVC - t = 4 t0 z/h0 x/h0 RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Dam-break wave : stepped bed
PVC - t = 6 t0 z/h0 x/h0 RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Dam-break wave : stepped bed
PVC - t = 8 t0 z/h0 x/h0 RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Overview The basic model: Saint-Venant - Exner Regime and solid transport Two-layer model Supercritical flow and bed forms Antidune modeling Transcritical flow and boundary conditions RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Supercritical flow and bed forms
Stepped bed z/h0 x/h0 RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Supercritical flow and bed forms
2D two-layer model Sediment layer underestimated: the concentration is the same in the sediment layer although this one has to de-bulk for moving RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Supercritical flow and antidunes
Two-layer shallow-water computation Flow H. Capart D.L. Young 2002 Two-layer shallow water computations of torrential geomorphic flows The paper applies a two-layer shallow water approach to the simulation of torrential geomorphic flows. The description endows water and slurry layers with their own velocity and inertia, and accounts for both mass and momentum exchanges across sharp interfaces. This allows rather general patterns of water and sediment motion to emerge from interactions between torrential currents and loose sand beds. The description is implemented into a 2D computational scheme based on direction and operator splitting. A Godunov algorithm is used for the hyperbolic operator, and an implicit backwards Euler scheme for the frictional and geomorphic source terms. A bank failure operator can further be nested inside the time-stepping loop. To explore its capabilities, we test the approach on three geomorphological features associated with miniature rivers on intertidal beaches: crescent marks, antidune trains, and runnel bank erosion. Encouraging results are obtained, and suggest that the modelling approach could be extended to torrential geomorphic flows at larger scales. Computed Measured Antidunes RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Overview The basic model: Saint-Venant - Exner Regime and solid transport Two-layer model Supercritical flow and bed forms Transcritical flow and boundary conditions Saint-Venant - Exner approach Limitations 2-layer approach : jump over mobile bed RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Overview The basic model: Saint-Venant - Exner Regime and solid transport Two-layer model Supercritical flow and bed forms Transcritical flow and boundary conditions Saint-Venant - Exner approach Limitations 2-layer approach : jump over mobile bed RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Boundary conditions Saint-Venant - Exner in unit width RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Boundary conditions De Vries analysis : characteristics RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Boundary conditions 2 upstream, 1 downstream boundary conditions x t RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Overview The basic model: Saint-Venant - Exner Regime and solid transport Two-layer model Supercritical flow and bed forms Transcritical flow and boundary conditions Saint-Venant - Exner approach Limitations 2-layer approach : jump over mobile bed RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : aggradation
Steep-sloped aggradation q (qs) zb h = hc RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump over mobile bed Initial conditions : steep slope RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump over mobile bed Raise of a gate downstream RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump over mobile bed Stabilisation of the surge RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Water and bed level RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Initial condition : supercritical flow x t zw q (qs) zb RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump on fixed bed zw zw q RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump on fixed bed : upstream zw q Upstream RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump on fixed bed : downstream zw q Downstream RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump on mobile bed zw zw q (qs) RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump on mobile bed zw zw q RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump on mobile bed : upstream zw q x t Upstream RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump on mobile bed : downstream zw q x t Downstream RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump on mobile bed zw zw q x t RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump on mobile bed zw zw q RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump on mobile bed zw zw q RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump on mobile bed zw zw q RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Boundary conditions : hydraulic jump
Hydraulic jump on mobile bed zw zw q ? RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Overview The basic model: Saint-Venant - Exner Regime and solid transport Two-layer model Supercritical flow and bed forms Transcritical flow and boundary conditions Saint-Venant - Exner approach Limitations : jump over mobile bed 2-layer approach : jump over mobile bed RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Two-layer boundary conditions
RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Two-layer boundary conditions
Re (l) (m/s) Im (l) Frw Frw uw = 1 m/s, us = 0.6 m/s, hs = 0.01 m and hw varies from 0.01 to 2.55 m RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Two-layer boundary conditions
l m/s Frw uw = 1 m/s, us = 0.6 m/s, hs = 0.1 m and hw varies from 0.01 to 2.55 m RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Two-layer boundary conditions
Supercritical flow 1 = 0 2, 3, 4, 5 > 0 1 < 2 = 0 3, 4, 5 > 0 RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Two-layer boundary conditions
Subcritical flow 1 < 2 = 0 3, 4, 5 > 0 1, 2 < 3 = 0 4, 5 > 0 RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Jump boundary conditions
1 = 0 2, 3, 4, 5 > 0 4 boundary conditions 1 < 0 2, 3, 4 = 0 5 > 0 1 boundary condition RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Hydraulic jump on mobile bed
RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Hydraulic jump on mobile bed
zw zw q (qs) RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Hydraulic jump on mobile bed
t = 9.2 s RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Hydraulic jump on mobile bed
t = 18.4 s Léger hs à gauche; pas à droite RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Hydraulic jump on mobile bed
t = 27.6 s RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Hydraulic jump on mobile bed
t = 36.8 s RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Hydraulic jump on mobile bed
t = 36.8 s Numerical sediment front a little delayed but also spread. Depending on the initial bottom. The imposed one was a straight line, which was not completely the realty where there were some discontinuities (see the last experimental point below the theoretical one) No measurement before since too fast for digital imaging with a little frame (< 1 m) RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Hydraulic jump on mobile bed
zw zw q (qs) RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Hydraulic jump on mobile bed
t = 140 s Water level too high. In the realty a part of kinetic energy due to recirculation is not modelled. Front a little delayed, but also little transport downstream the front contrarily to the realty. Probably linked to the water level and the critical bottom shear stress (disappears after). RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Hydraulic jump on mobile bed
t = 290 s Now the threshold is clearly exceeded, thus no more problem downstream. Too low: no measurement of the upstream point, thus maybe too high upstream. In the realty deposition of solid discharge is not so clearly defined. RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Hydraulic jump on mobile bed
t = 545 s RCEM, October 2005 The morphodynamics of super- and transcritical flow
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Hydraulic jump on mobile bed
t = 630 s RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Conclusions Floods Regime discontinuities Supercritical flow Intense transport Instabilities and bed forms Transcritical flow Acceleration / deceleration : lag Boundary conditions RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Conclusions Floods Regime discontinuities Supercritical flow Intense transport Instabilities and bed forms Transcritical flow Acceleration / deceleration : lag Boundary conditions Two layer model… to be improved RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Conclusions Floods Regime discontinuities Supercritical flow Intense transport Instabilities and bed forms Transcritical flow Acceleration / deceleration : lag Boundary conditions Two-layer model… to be improved RCEM, October 2005 The morphodynamics of super- and transcritical flow
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The morphodynamics of super- and transcritical flow
Yves Zech Sandra Soares Frazão Benoit Spinewine, Mourad Bellal, Céline Savary Université catholique de Louvain, Belgium Thank you for your attention
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