Lecture 9-River Dynamics 3 Flashcards

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1
Q

Froude number purpose

A

Will water continue downstream or go back upstream when it hits an obstacle

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2
Q

How to solve for mean velocity when water is flowing at critical velocity

A

Velocity = Fr x sqrt(gY)
Where fr=1 at critical velocity
And g=9.8
Y= depth.

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3
Q

Changes in space and time of the profile (4)

A

Steady flow
Uniform flow
Varied flow
Unsteady flow

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4
Q

Uniform flow

A

Steady and uniform

  • velocity is constant in space (reach of interest)
  • depth is constant in space
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5
Q

Steady flow

A
  • Velocity is constant through time

- depth is constant through time

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6
Q

Varied flow

A

Depth and velocity are not constant in time and space.

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7
Q

Unsteady flow

A

Velocity and depth are not constant through time (flood wave)

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8
Q

Significance of uniform flow

A
  • flow is steady if average velocity doesn’t change over time
  • acceleration =0, velocity does notchange
  • can be laminar
  • or turbulent (our focus)
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9
Q

Prandtl’s velocity profile

A

What is the distribution of velocity in turbulent flow?
In turbulent flow, turbulent forces > viscous forces
Eddy viscosity depends on flow characteristics and varies in space within a flow

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10
Q

τ =ε ( dv /dy)

A
Prandtl's velocity profile formula
τ = shear stress
ε = eddy viscosity (not a constant)
v = velocity at a point
y = distance above bed
d = change in
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11
Q

ε = ρι2 (dv/dy)

A

ε = Eddy viscosity
ρ = mass density
ι (squared) = mixing length

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12
Q

Eddy viscosity assumptions (2)

A
1. ι = ky
The mixing length is proportional to distance from the bed
2. τ =τ0 =γ y S0
The shear stress is constant throughout flow and equal to boundary shear stress given by laminar flow.
τ0 = shear stress at the base
γ = weight density
y = depth
S0 = slope at the base
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13
Q

v = 2.5 V* ln ( 30y / ks )

A

Final velocity profile equation
Velocity related to friction V* =(gyS0) to power of 1/2
y =depth
ks = constant for effective roughness length (grain size at the bed)

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14
Q

v= 2.5 V* ln(by/y0)

A

Formula to calculate the mean velocity

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