4.6 Article

Effects of Submerged Vegetation Arrangement Patterns and Density on Flow Structure

Journal

WATER
Volume 15, Issue 1, Pages -

Publisher

MDPI
DOI: 10.3390/w15010176

Keywords

deflected vegetation; non-bending vegetation; vegetation density; Reynolds shear stress; turbulence kinetic energy; flow structure

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This study investigates the effects of submerged vegetation arrangement patterns and density on flow structure through experiments. The results show that the staggered configuration leads to intensified streamwise velocity, turbulence kinetic energy, and Reynolds shear stress compared to the square configuration. Additionally, the wake zone produced by low vegetation density is more expansive than that produced by high vegetation density.
Aquatic vegetation appears very often in rivers and floodplains, which significantly affects the flow structure. In this study, experiments have been conducted to investigate the effects of submerged vegetation arrangement patterns and density on flow structure. Deflected and non-bending vegetation is arranged in square and staggered configurations in the channel bed of a large-scale flume. Results showed that the staggered configuration leads to intensified streamwise velocity, turbulence kinetic energy (TKE), and Reynolds shear stress (RSS) compared to the square configuration. When vegetation density is low (lambda = 0.04 and lambda = 0.07), the produced wake in the rear of the vegetation is more expansive than that with high vegetation density (lambda = 0.09 and lambda = 0.17) because the velocity in the center of four vegetation elements is lower than that in the middle of two vegetation elements with low vegetation density. Results of TKE in the wake zone of the deflected vegetation indicate that the maximum root-mean-square velocity fluctuations of flow occur at the sheath section (z/H = 0.1) and the top of the vegetation (z/H = 0.4). In the wake zone behind the vegetation elements, the maximum value of the RSS occurred slightly above the interface between deflected vegetation and the non-vegetation layer, showing the Kelvin-Helmholtz instability that is associated with inflectional points of the longitudinal velocity. Within the range of vegetation density in this study (0.04 < lambda approximate to< 0.23), as the vegetation density increases, the negative and positive values of RSS throughout the flow depth increase.

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