Abstract
AbstractGlass beads were used to model permeable beds and boulders (simulated by plastic spherical balls) placed on the centre section of the bed. Flume experiments were conducted to investigate the hydrodynamics through a boulder array over impermeable and permeable beds (i.e. IMPB and PB). For background reference, hydrodynamics investigation was made over smooth beds (SB) with the boulder array. Through measuring the instantaneous velocity field, the major flow characteristics such as mean flow velocity, turbulence intensity, turbulent kinetic energy (TKE) and instantaneous Reynolds stresses (through quadrant analysis) were presented. The results show that the increase in bed permeability through decreasing the exposure height of boulders has little impact on the magnitude of streamwise velocity, but tends to decrease the near-bed velocity gradient, thus affecting the bed shear-stress. For turbulence, similar to the previous studies, the bed permeability is identified to enable a downward shift of the peak of turbulence intensity. The TKE budget analysis shows that bed permeability tends to inhibit the transport and diffusion processes of TKE generation. Finally, the quadrant analysis of turbulence structure clearly shows that the ejections (Q2) and sweeps (Q4) with and without the boulder array are dominated by turbulence structure of different scales.
Highlights
In mountain rivers, immobile boulders are regarded as large bed obstacles, largely influencing the spatial and temporal variability in flow and topographic dynamics (Euler et al ; Afzalimehr et al )
This study aims to investigate the impacts of the coexistence of boulders and bed permeability on the hydrodynamics
To construct the permeable configuration, the second layer of beads was well packed on the IMPB, which was able to enhance the vertical motion of flows
Summary
Immobile boulders are regarded as large bed obstacles, largely influencing the spatial and temporal variability in flow and topographic dynamics (Euler et al ; Afzalimehr et al ). The investigation of the effects of boulders on flow structures is difficult to perform due to the complexity of the bed surface geometry configuration. A far-wake region beyond the near-wake region enables flow to return to a normal state near the bed as upstream. Multiple arrays of isolated boulders in a regular
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