Friction Velocity Equation:
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Friction velocity (u*) is a fundamental parameter in fluid dynamics that characterizes the shear stress at a boundary. It represents the velocity scale associated with turbulent flow near surfaces and is crucial for understanding boundary layer dynamics.
The calculator uses the friction velocity equation:
Where:
Explanation: The equation relates the square of friction velocity to the ratio of shear stress to fluid density, providing a velocity scale that characterizes turbulent flow properties.
Details: Friction velocity is essential for predicting sediment transport, calculating turbulent energy dissipation, modeling atmospheric boundary layers, and designing hydraulic structures. It serves as a scaling parameter in many turbulence models.
Tips: Enter shear stress in Pascals (Pa) and fluid density in kg/m³. Both values must be positive. For water at 20°C, density is approximately 998 kg/m³; for air at sea level, density is approximately 1.225 kg/m³.
Q1: What is the physical significance of friction velocity?
A: Friction velocity represents the characteristic velocity scale in the turbulent boundary layer and is proportional to the square root of the wall shear stress.
Q2: How is friction velocity related to Reynolds stress?
A: Friction velocity squared is equal to the Reynolds stress divided by density in simple shear flows, making it a direct measure of turbulent momentum transport.
Q3: What are typical values of friction velocity?
A: In atmospheric flows, u* typically ranges from 0.1-1.0 m/s; in hydraulic engineering, values depend on flow conditions but generally range from 0.01-0.5 m/s.
Q4: Can friction velocity be measured directly?
A: While not directly measurable, it can be determined from velocity profile measurements, shear stress measurements, or pressure drop calculations in pipes.
Q5: How does friction velocity affect sediment transport?
A: Friction velocity is crucial for determining the critical shear stress for sediment motion and calculating sediment transport rates in rivers and coastal environments.