Lecture 9-River Dynamics 3 Flashcards
Froude number purpose
Will water continue downstream or go back upstream when it hits an obstacle
How to solve for mean velocity when water is flowing at critical velocity
Velocity = Fr x sqrt(gY)
Where fr=1 at critical velocity
And g=9.8
Y= depth.
Changes in space and time of the profile (4)
Steady flow
Uniform flow
Varied flow
Unsteady flow
Uniform flow
Steady and uniform
- velocity is constant in space (reach of interest)
- depth is constant in space
Steady flow
- Velocity is constant through time
- depth is constant through time
Varied flow
Depth and velocity are not constant in time and space.
Unsteady flow
Velocity and depth are not constant through time (flood wave)
Significance of uniform flow
- flow is steady if average velocity doesn’t change over time
- acceleration =0, velocity does notchange
- can be laminar
- or turbulent (our focus)
Prandtl’s velocity profile
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
τ =ε ( dv /dy)
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
ε = ρι2 (dv/dy)
ε = Eddy viscosity
ρ = mass density
ι (squared) = mixing length
Eddy viscosity assumptions (2)
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
v = 2.5 V* ln ( 30y / ks )
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)
v= 2.5 V* ln(by/y0)
Formula to calculate the mean velocity