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Fluid Dynamics with Erosion

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Fluid Dynamics with Erosion Brandon Lloyd COMP 259 May 2003 Overview Sediment transport in open channels Bed-load transport Suspensed transport Sediment transport ... – PowerPoint PPT presentation

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Title: Fluid Dynamics with Erosion


1
Fluid Dynamics with Erosion
  • Brandon Lloyd
  • COMP 259
  • May 2003

2
Overview
  • Sediment transport in open channels
  • Bed-load transport
  • Suspensed transport
  • Sediment transport models
  • Model used for this project
  • Implementation issues
  • Future work

3
Sediment Transport
  • Bed-load transport sliding, rolling, saltating
  • Suspended transport sediment moves through the
    fluid

Suspension
Sediment
Bed-load
Bed
4
Bed-load transport
Once the forces acting on particles are
strong enough to intiate motion
Figure from Chanson, p. 200
particles slide, roll, and saltate down the
river bed at a steady rate.
Figure from Chanson, p. 180
5
Suspended Transport
  • Particles entrained at the bed-load layer
  • Transported by convection, diffusion, and
    turbulence

Suspension occurs here
Figure from Chanson, p. 200
6
Sediment Transport Models
  • Difficult problem most models are empirical.
  • Usually make simplifying assumptions about flow.
  • Many different formulas exist.

Table from Chanson, p. 198
7
My Model
  • Simplified version of model used in Haupt et al.
    1999
  • Transport occurs above critical velocity.
  • Fluid has a transport capacity related to
    velocity.
  • Concentration of sediment relative to capacity
    determines change in terrain

8
Implementation Issues
zero concentration
  • Semi-Lagrangian advection causes mass loss in the
    presence of eddies.
  • What to do at boundaries?

backward tracing does not see wall ? mass loss.
9
Implementation Issues
  • Semi-Lagrangian advection causes mass loss in the
    presence of eddies.
  • What to do at boundaries?

Recycle concentration(limits the time-step)
10
Results
  • Nice swirls of sediment with erosion and
    deposition at interactive rates (on a fast
    machine ?.)

11
Future Work
  • Add bed-load transport
  • Add instability based on slope
  • Add variable material properties
  • Fix spikes and improve robustness
  • Better handling of velocities near heightfield.
  • Experiment with and compare different
    fluid/advection models
  • Add a free surface
  • Implement on GPU

12
References
  • CHANSON, H. 1999. The Hydraulics of Open Channel
    Flow An Introduction. Arnold.
  • HAUPT, B. J., SEIDOV, D. AND STATTEGGER, K. 1999.
    SEDLOB and PATLOB Two numerical tools for
    modeling climatically forced sediment and water
    volume transport in large ocean basins. In
    Computerized Modeling of Sedimentary Systems.
    Springer-Verlag, Berlin.
  • WU, W., RODI, W. AND THOMAS, W. 2000. 3D numerial
    modeling of flow and sediment transport in open
    channels. Journal of Hydraulic Engineering, 4-15.
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