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VELOCITY PROFILE AND SHEAR STRESSES CALCULATION IN HIGH VOLUME RELATIVE BED ROUGHNESS FLOW

Krakow Agriculture University. VELOCITY PROFILE AND SHEAR STRESSES CALCULATION IN HIGH VOLUME RELATIVE BED ROUGHNESS FLOW. Wojciech Bartnik Andrzej Struzynski. Presentation Schedule. Flow zones – Introduction Laboratory measurements Bed roughness measurements Log-law velocity distribution

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VELOCITY PROFILE AND SHEAR STRESSES CALCULATION IN HIGH VOLUME RELATIVE BED ROUGHNESS FLOW

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  1. Krakow Agriculture University VELOCITY PROFILE AND SHEAR STRESSES CALCULATION IN HIGH VOLUME RELATIVE BED ROUGHNESS FLOW Wojciech Bartnik Andrzej Struzynski

  2. Presentation Schedule • Flow zones – Introduction • Laboratory measurements • Bed roughness measurements • Log-law velocity distribution • Calculation of velocity and shear stresses • Conclusions

  3. Flow zones Bed roughness and water surface acts on the flowing water

  4. Flow zones • I - laminar flow • II - log-law velocity distribution • III - wake region • IV - free surface region

  5. IV III II I Flow zones • flat bed

  6. IV Flow zones • rough bed IV III II I

  7. Flow zones [Williams J.J., 1996]

  8. Flow zones Bed roughness and water surface acts on the shape of flowing water velocity profile.

  9. Flow zones Fr = 0.074 Fr = 1.38 The shape of velocity profile depend on: flow depth, av. velocity of flowing water, bed roughness, relative roughness ... For hydraulically rough flow conditions I and IV flow zone decreases 4D

  10. Laboratory measurements • Flume dimensions: l2.0 x 0.5 x 0.6 m (glass walls) • Flume rig: • micro-propeller • flow-meter • slope measurements • Bed slope, water surface slope • Discharge: max 0.13 qm s-1 • Artificial grains Ø – 4 to 8 cm

  11. Bed roughness measurements homogeneous roughness ks = K (1.926 SF2 – 0.488 SF + 4.516) Profile-meter AG-1

  12. Log-law velocity distribution flat bed Maximum velocity moves with relative roughness change

  13. Log-law velocity distribution rough bed Maximum velocity moves with relative roughness change

  14. Log-law velocity distribution flat bed For the same bed roughness curves are parallel

  15. Log-law velocity distribution grains 4M For the same bed roughness curves are parallel

  16. Log-law velocity distribution grains 4D For the same bed roughness curves are parallel

  17. Log-law velocity distribution grains 6D For the same bed roughness curves are parallel

  18. Log-law velocity distribution grains 8D For the same bed roughness curves are parallel

  19. Calculation of velocity and shear stresses Modified Prandtl equation Log-law velocity distribution for whole profile is used U/Umax = A log (y/Y) + B B becomes constant- B = 1.12±3%

  20. Calculation of velocity and shear stresses U/Umax = A log (y/Y) + B A value changes with relative depth Y/K

  21. Calculation of velocity and shear stresses U/Umax = A log (y/Y) + B Comparison of measured to calculated A constant

  22. Calculation of velocity and shear stresses Velocity profile reflects shear stresses Use of logarithmic equation allow calculating t0 for rough flow conditions t0 = 2.303 K UM

  23. Calculation of velocity and shear stresses

  24. Conclusions • Near bed the velocity and velocity profile slope calculations (in logarithmic scale) are correct within the second and third flow zone. The use of equation (4) makes the bed level (zero velocity) estimation error negligible (B=1.12). • The use of mentioned method is limited to the rough flow conditions where the maximum velocity lays close to the water surface (the near surface region decreases to 20% of water depth). • The measurements of surface velocity, water depth and bed roughness can be used for calculation of water velocity profile and bed shear stresses for rough flow conditions.

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