Abstract
Detailed measurements have been taken for the longitudinal turbulent intensities of flow in a gravel-bed flume. The experimental results indicate that the distribution of turbulent intensity greatly depends on the relative roughness. In comparison with the smooth-bed results, the roughness makes the flow turbulence become well-distributed, especially in the region near the bed and in the case of smaller H/K s values. In addition, the cross sectional average of turbulent intensity is also discussed in this paper, and the results show that the roughness makes flow turbulence much more intense.
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Abbreviations
- D u :
-
empirical constant
- H :
-
flow depth
- K s :
-
roughness height
- N :
-
\(N = \frac{1}{H}\int\limits_0^H {\frac{{u\prime }}{{\bar U}}} {\text{ }}dy\), the mean turbulence intensity over the cross section
- Re * :
-
\(Re* = \frac{{k_s u_* }}{\nu }\), roughness Reynolds number
- u′ :
-
the RMS of streamwise fluctuating velocity
- u * :
-
friction velocity
- Ū :
-
mean bulk velocity
- x :
-
coordinate alined with mainstream velocity (x = 0 is channel entrance)
- y :
-
vertical coordinate to the rough bed (y = 0 is the top of the rough elements)
- y + \(\frac{{yu_* }}{\nu }\) :
-
λ u empirical constant
- v :
-
kinematic viscosity
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Wang, JJ. Distribution of turbulent intensity in a gravel-bed flume. Experiments in Fluids 11, 201–202 (1991). https://doi.org/10.1007/BF00190303
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DOI: https://doi.org/10.1007/BF00190303