Velocity Distribution Formula:
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Velocity distribution in rough turbulent flow describes how fluid velocity varies with height above a rough boundary in turbulent flow conditions. This mathematical model helps predict flow characteristics in various engineering applications.
The calculator uses the velocity distribution formula:
Where:
Explanation: This formula calculates the average velocity at a given height above a rough boundary in turbulent flow, accounting for the logarithmic velocity profile characteristic of turbulent boundary layers.
Details: Accurate velocity distribution calculation is crucial for hydraulic engineering, sediment transport studies, river morphology analysis, and designing water conveyance systems.
Tips: Enter shear velocity in m/s, height above bed in meters, and equivalent sand-grain roughness in meters. All values must be positive numbers greater than zero.
Q1: What is shear velocity?
A: Shear velocity, also called friction velocity, is a form by which shear stress may be re-written in units of velocity, representing the flow's ability to transport sediment.
Q2: How is equivalent sand-grain roughness determined?
A: Equivalent sand-grain roughness is an empirical parameter that represents the roughness characteristics of a surface, typically determined through experimental measurements.
Q3: When is this formula applicable?
A: This formula applies to fully developed turbulent flow over rough boundaries, typically in open channel flow and boundary layer flow situations.
Q4: What are the limitations of this formula?
A: The formula assumes fully turbulent flow, homogeneous roughness, and may not accurately represent flow very close to the boundary or in transitional flow regimes.
Q5: How does roughness affect velocity distribution?
A: Increased roughness typically reduces flow velocities near the boundary and alters the velocity profile, affecting overall flow resistance and sediment transport capacity.