Incipient Motionpierre/ce_old/Projects/linkfiles/... · Colorado State University, Fort Collins, CO...

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1 Sedimentation Engineering… Incipient Motion and Bedforms Pierre Y. Julien Professor of Civil and Environmental Engineering Colorado State University, Fort Collins, CO 80523 [email protected] January 15, 2008 UiTM, Shah Alam, Malaysia Incipient Motion

Transcript of Incipient Motionpierre/ce_old/Projects/linkfiles/... · Colorado State University, Fort Collins, CO...

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Sedimentation Engineering…Incipient Motion and Bedforms

Pierre Y. JulienProfessor of Civil and Environmental EngineeringColorado State University, Fort Collins, CO 80523

[email protected]

January 15, 2008UiTM, Shah Alam, Malaysia

Incipient Motion

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Shields Parameter• Ratio of

Hydrodynamic Forces to Submerged Weight

( ) ( ) ss

m

ss

o

du

d γγρ

γγττ

−=

−=

2*

*

Beginning of Motion• Critical Shields Parameter(τ*c)

– beginning of motion (τo = τc) ( ) ss

cc dγγ

ττ−

=*

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Calculating Critical Shear Stress

Bedforms and Resistance to Flow

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What are bedforms?Initiation of Bedforms on a flat bed

Wind Blown Ripples on Dunes

Antidunes

Ripples

Dunes

Lower Regime - Ripples• Small Grain Diameter

– d50 < 0. 6mm• Manning n

– 0.018 to 0.028• Concentration

– 10 to 200 mg/L• Small Features

– Less than 20 cm long – A few cm high

• Dominant Roughness– Form

Linguoid current ripples Kennetcook River

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Lower Regime - Dunes• Coarser Grain Diameter

– d50 < 2 mm• Manning n

– 0.02 to 0.04• Concentration

– 200 to 3000 mg/L• Large Features

– Up to tens of meters in height

• Dominant Roughness– Form

• Field Characteristic– Boils on the water surface

Transition - Washed Out Dunes

• Manning n– 0.014-0.025

• Concentration – 1,000 to 4,000 mg/L

• Water Surface Profile– Out of Phase

• Dominant Roughness– Form or Grain

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Upper Regime - Plane Bed• Manning n

– 0.010 to 0.013• Concentration

– 2,000 to 4,000 mg/L• Water Surface Profile

– Parallel• Dominant Roughness

– Grain

Upper Regime – Antidunes• Manning n

– 0.010 to 0.020• Concentration

– 2,000 to 5,000 mg/L• Water Surface Profile

– In Phase• Dominant Roughness

– Grain

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Upper Regime – Chutes and Pools

• Manning n– 0.018 to 0.035

• Concentration – 5,000 to 50,000 mg/L

• Water Surface Profile– In Phase

• Dominant Roughness– Variable

Bedform Classification• Bedforms are

classified based on:– Shape– Resistance to Flow

(Energy Dissipation)– Sediment Transport– Relationship between

the bed and water surface Forms of bed roughness in sand channels

(Simons and Richardson 1963, 1966)

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Based on Transport-Stage Parametervan Rijn, 1984b

Study Area of the Rhine River

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Field Surveys on the Rhine River

Bedform Profiles

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Dune Height during the Flood

Manning n during the Flood

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Resistance to Flow

Sedimentation Engineering

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Total rainfall of Typhoon Maemi from 9/8/2003 to 9/13/2003)

South Korea

Mangun mountain, South Korea

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Imha Reservoir, South Korea

Annual average: 3,450 tons/km2/year.

Soil loss maps

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CSU Watershed Model TREX

Flow Depth [ft] 100 yr Storm

Logarithmic Velocity Profile

o

x

zz

uv ln1

* κ=

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Turbulent Flow Equations

{{

4444 34444 2143421

3214444 34444 21nfluctuatioturbulent

zzzyzx

viscous

zm

gradientpressure

mnalgravitatioz

convective

zz

zy

zx

local

z

yzyyyxym

my

yz

yy

yx

y

xzxyxxxm

mx

xz

xy

xx

x

zvv

yvv

xvv

vzpg

zvv

yvv

xvv

tv

zvv

yvv

xvv

vypg

zv

vyv

vxv

vt

v

zvv

yvv

xvv

vxpg

zv

vyv

vxv

vt

v

⎥⎥⎦

⎢⎢⎣

∂∂

+∂

∂+

∂∂

−∇+∂∂

−=∂∂

+∂∂

+∂∂

+∂∂

⎥⎥⎦

⎢⎢⎣

∂+

∂+

∂−∇+

∂∂

−=∂

∂+

∂+

∂+

⎥⎥⎦

⎢⎢⎣

∂∂

+∂

∂+

∂∂

−∇+∂∂

−=∂∂

+∂∂

+∂∂

+∂∂

++++++

++++++

++++++

2

2

2

1

1

1

υρ

υρ

υρ

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Riprap Design

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Hapcheon Re-regulation Dam

South Korea

0

10

20

30

40

50

60

70

80

90

100

0 10 20 30 40 50 60 70 80 90 100

time (hr)

wat

er d

epth

(m)

Degradation and armouring

40 km

37

39

41

43

45

47

49

0 100 200 300 400 500 600

width (m)

bed

elev

atio

n (m

)

19832003

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River changes below Hapcheon dam

2004

2007

1983

Before

After

Nakdong River and NREB Unsteady modeling for the upstream of NREB

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Nakdong River Estuary Barrage

Case-Study:Gupo Bridge during Typhoon Maemi in 2003

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Erosion and River Mechanics Textbooks

Acknowledgments• Dr. Sang Kil Park (PNU)• Dr. Un Ji (Myongji U. )• Hyeon Sik Kim (KOWACO)• Young Ho Shin (KOWACO)• Byungdal Kim (KOWACO)• A.F. Embi (DID-Malaysia)• Dr. N.A. Zakaria (USM)• Dr. A. Ab. Ghani (USM)• Dr. J.Ariffin (UiTM-Malaysia)• James Halgren (CSU)• Seema Shah (CSU)

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Terima Kasih!

[email protected]