Abstract
The effect of particle density on the turbulent open-channel flow carrying dilute particle suspensions is investigated using two specific gravities and three concentrations of solid particles. The particles, identical in size and similar in shape, were natural sand and a neutrally buoyant plastic. The particles were fully suspended, and formed no particle streaks on the channel’s bed. Accordingly, the changes in the flow are attributed to the interactions between suspended particles and flow turbulence structures. Measurements were obtained by means of image velocimetry enabling simultaneous, but distinct, measurement of liquid and particle velocities. The experimental results show that, irrespective of particle specific gravity, particle suspension influences bulk velocity of flow and the Kármán coefficient, while friction velocity essentially remains constant. The results also show that particles in suspension modify local water turbulence over the flow depth, but in ways not accurately predicted using the customary parameters for characterizing turbulence modification.
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Abbreviations
- C :
-
Depth averaged sediment concentration
- D 50 :
-
Median diameter of sediment particle
- D s :
-
Sediment particle diameter
- D + s :
-
Dimensionless sediment particle diameter \({\left( {\equiv {D_s u_\ast}\mathord{\left/ {\vphantom {{D_s u_\ast }\nu }}\right.\kern-\nulldelimiterspace}\nu }\right)}\)
- Fr:
-
Froude number
- N :
-
Total number of particles
- N + :
-
Number of upward-moving particles
- N − :
-
Number of downward-moving particles
- q s :
-
Total unit sediment discharge
- U :
-
Mean streamwise velocity
- V :
-
Mean vertical velocity
- \({\overline{U}}\) :
-
Depth averaged streamwise velocity of water
- \({{\overline{U}_s}}\) :
-
Depth averaged streamwise velocity of sediment
- u L :
-
Average velocity lag
- u * :
-
Shear velocity
- u′:
-
Root-mean square of fluctuation component of streamwise velocity\({\left({\equiv \sqrt {\overline {{u}'{u}'}} }\right)}\)
- V MLT :
-
Equivalent vertical velocity by McLaughlin and Tiederman
- υ ′:
-
Root-mean square of fluctuation component of vertical velocity\({\left( {\equiv \sqrt {\overline {{\upsilon }'{\upsilon }'}} }\right)}\)
- υ s :
-
Fall velocity of sediment particle
- v :
-
Kinematic viscosity of water
- h :
-
Flow depth
- y :
-
Distance from the channel bed
- y + :
-
Dimensionless distance from the channel bed \({\left( {\equiv {yu_\ast }\mathord{\left/ {\vphantom {{yu_\ast }\nu }}\right.\kern-\nulldelimiterspace}\nu }\right)}\)
- Re:
-
Reynolds number
- Re p :
-
Particle Reynolds number
- \({{\varepsilon _m}}\) :
-
Turbulent momentum diffusion coefficient
- St :
-
Stokes number
- λ T :
-
Taylor microscale
- ξ:
-
The rate of turbulent energy dissipation
- \({{\kappa}}\) :
-
von Kármán coefficient/constant
- τ p :
-
Particle response time
- τ f :
-
Representative flow time scale
- τ K :
-
Kolmogorov time scale \({\left( {\equiv \sqrt {\nu \mathord{\left/{\vphantom {\nu \xi }}\right. \kern-\nulldelimiterspace}\xi }}\right)}\)
- ℓ e :
-
Length scale of the energy containing eddies
- η:
-
Dimensionless height \({\left( {\equiv y \mathord{\left/ {\vphantom {yh}}\right. \kern-\nulldelimiterspace} h}\right)}\)
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Muste, M., Yu, K., Fujita, I. et al. Two-phase flow insights into open-channel flows with suspended particles of different densities. Environ Fluid Mech 9, 161–186 (2009). https://doi.org/10.1007/s10652-008-9102-7
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DOI: https://doi.org/10.1007/s10652-008-9102-7