Post on 24-Feb-2016
description
transcript
Fereshteh Bagherimiyab
Ulrich Lemmin
Effects of bed form structure on particle-turbulence interaction in unsteady suspended sediment-laden
laboratory open-channel flows
Introduction Experimental set-up Procedure Results Conclusion
Introduction
Turbulence plays an essential role in
suspended sediment transport
Suspension of fine sediments
Generates bed forms
Affects Water quality in rivers
Impacts on the environment
Experimental set-up
side walls = transparent glass gravel layer= 0.1 m thick gravel size range = 3 to 8 mmD50 = 5.5 mm
L=17mh = 0.8m
B = 0.6m
ADVP with housing
Experimental procedure
Constant discharge ?
Range of variations of discharge, water depth, mean velocity and Reynolds number
Results
Hydrograph: Low High
Pump discharge Q (l sec-1) 10 35Water depth h (cm) 10 15
Mean velocity u (cm s-1) 17 39
Reynolds Number 1.5 104 5.3 104
ResultsVelocity measurements without sediment
Longitudinal mean velocity and mean velocity from log fit during the unsteady flow stages against depth changes
Results
Friction velocity u* distribution for the unsteady ranges of 30s and 60 s
Flow with particle motion Sediment suspension
D50 = 0.16 mm
1 m
Thickness = 6 mm
Results
Mean particle velocities during the accelerating and the peak flow stages
Particle velocity with ADVP
Results
a) b)
PTV results during the (a) initial and (b) final phase of the accelerating stage. Arrows indicate particle velocity vectors
Mean particle velocities in ten image slices for the (a) initial and (b) final phases of the accelerating stage
suspension is nearly uniform in a shallow layer above the bed
Suspension into the water column above occurs in burst-like events in the final phase, strongest near the ripple crest
Particle velocity
profiles extend higher into the water column in the final phase
Particle Tracing Velocimetry (PTV)
Particle concentrations in the same image slices
The highest concentration is found near the bottom
total suspension, increase in the final phase. This confirms the importance of burst structures with strongest bursts near the ripple crests
concentration (gr cm-3)
ResultsExample of PTV results during the final phase of the accelerating flow range. Arrows indicate particle velocity vectors
a) b)
Particle velocities in six positions of images
Particle concentrations in six positions of images
Bed form formation during the final phase of the accelerating flow range
The highest concentration is found in the position where ripples are formed (x = 10.2 cm with a strong gradient towards the trough
This confirms the burst structure pattern with strongest bursts near the ripple crests
Results
L= 0.8 water depth h=5 mm
fine particles rolled along ripples
ripples were observed
Ripples formed quickly, within about 3 sec after fine sediment particle saltation started
Results
Close-up view of sediment particle trajectories related to ripple formation
during the initial saltation of particles, the upper layer of the whole bed began to move (Fig. a)
Particles may rise about 1 cm above the bed
Saltation above the bed level occurs in bursts
The ripple started forming 2.5 s after (Fig. b)
vortex is formed in the lee side of the crest
the vertical velocity component is strong in the near bottom layer
Results
Large scale image of ripple formation, seen from the top. Mean spacing of the
ripples is about 6 cm
ripples are formed from some
instability on the bed
towards the end of the acceleration
range, ripples occurred nearly
simultaneously along the whole bed and
quickly formed a pattern
The whole pattern slowly moves in the
direction of the flow, but the distribution
does not change significantly
Over time during the steady peak flow
of about 3 minutes, the colour of the
dark area changes little
Remains of the initial reference bed level
Sediment suspension strongly characterized by burst events and the presence of
ripples on the bed
High sediment suspension continued to occur during the decelerating flow even
though the flow velocity decreased
Sediment suspension in unsteady flow is controlled by the same large scale
turbulence processes as in steady flow
The wavelength of the ripples depended on the rate of acceleration
Faster acceleration produced shorter ripples due to a much stronger friction velocity
The shorter ripples produced stronger and higher suspension
Ripples did not change in appearance or dimension for the duration of the
experiments
Conclusion