Shear stress velocity
The shear velocity is in the hydrodynamics a measure of the shear stress , a layer of a flowing fluid on an adjacent layer or a boundary surface exerts. It is calculated from the amount of the shear stress vector and the density of the fluid:
In turbulent media , the shear stress is dominated by the turbulent transport. The components of the shear stress vector are then calculated from the elements of Reynolds' shear stress tensor :
in which
- and the two velocity components parallel (x- and y-direction) and perpendicular (z-direction) to the interface as well
- canceled quantities such as the deviations from the mean.
The two covariances and can also be interpreted as the turbulent flows in the z direction of the momentum in the x or y direction.
The shear stress velocity is the square root of the amount of this vector:
When deriving the logarithmic wind profile using the mixing path length approach according to Ludwig Prandtl , the coordinate system is defined so that the x-axis is parallel to the mean wind direction ( ), and it is assumed that the mean wind direction and the direction of the shear stress coincide ( ). In this case:
See also
literature
- Erich Truckenbrodt: Fundamentals and elementary flow processes of density-stable fluids . In: Fluid Mechanics . 4th edition. tape 1 . Springer-Verlag, Berlin / Heidelberg 1996, ISBN 978-3-540-79017-4 .