Exam 2 Flashcards
Uniform Flow
No change in velocity over a distance
Steady Flow
No change in velocity over time
hydraulic Radius
Area/wetted perimeter (Wp)
Hydraulic Depth
Area/B (top width)
Continuity equation
Q = Q
F =?
P*A
P = ?
gamma *Hc
Normal Depth
The equilibrium depth
The equation used to derive manning equations
Chezy Equation
Assumptions for uniform depth
a fixed geometry
a fixed flow rate
fixed roughness coefficient
fixed slope
What are alternate depths
Two depths with the same specific energy
Specific Energy
The total energy in the flow at a cross-section when Function of its kinetic and potential energy terms when you use the bottom of the channel as a datum
Critical depth
the depth that critical flow occurs
Critical flow
Flow with minimum energy, froudes number = 1
Subcritical flow
Froudes <1
Deep water and slow
Supercritical flow
Froudes > 1
Shallow water and fast