Effects of Submerged Vegetation Density on Turbulent Flow Characteristics in an Open Channel
The vegetation density <i>λ</i> affects turbulent flow type in the submerged vegetated river. This laboratory study investigates different types of vegetated turbulent flow, especially the flow at 0.04 < <i>λ</i> < 0.1 and <i>λ&l...
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doaj-9625eae10358483792a3de55820637f32020-11-25T00:10:07ZengMDPI AGWater2073-44412019-10-011110215410.3390/w11102154w11102154Effects of Submerged Vegetation Density on Turbulent Flow Characteristics in an Open ChannelHanqing Zhao0Jing Yan1Saiyu Yuan2Jiefu Liu3Jinyu Zheng4State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, ChinaState Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, ChinaState Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, ChinaState Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, ChinaHenan Water Conservancy Survey, Ltd., Zhengzhou 450008, ChinaThe vegetation density <i>λ</i> affects turbulent flow type in the submerged vegetated river. This laboratory study investigates different types of vegetated turbulent flow, especially the flow at 0.04 < <i>λ</i> < 0.1 and <i>λ</i> = 1.44 by setting the experimental <i>λ</i> within a large range. Vertical distributions of turbulent statistics (velocity, shear stress and skewness coefficients), turbulence kinetic generation rate and turbulence spectra in different <i>λ</i> conditions have been presented and compared. Results indicate that for flow at 0.04 < <i>λ</i> < 0.1, the profiles of turbulent statistics manifest characteristics that are similar to those of both the bed-shear flow and the free-shear flow, and the turbulence spectral curves are characterized with some slight humps within the low-frequency range. For <i>λ</i> = 1.44, the turbulent statistics above the vegetation top demonstrate the characteristics of boundary-shear flow. The spectral curves fluctuate intensely within the low-frequency range, and the spectra of low-frequency eddies above vegetation top are significantly larger than the values below. The change of turbulent flow type induced by an increase of <i>λ</i> would increase the maximum value of turbulence kinetic generation rate <i>G</i><sub>S</sub> and change the point where <i>G</i><sub>S</sub> is vertically maximum upwards to the vegetation top.https://www.mdpi.com/2073-4441/11/10/2154open channelsubmerged vegetation densityturbulent flow typeturbulent statisticsturbulence spectra |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Hanqing Zhao Jing Yan Saiyu Yuan Jiefu Liu Jinyu Zheng |
spellingShingle |
Hanqing Zhao Jing Yan Saiyu Yuan Jiefu Liu Jinyu Zheng Effects of Submerged Vegetation Density on Turbulent Flow Characteristics in an Open Channel Water open channel submerged vegetation density turbulent flow type turbulent statistics turbulence spectra |
author_facet |
Hanqing Zhao Jing Yan Saiyu Yuan Jiefu Liu Jinyu Zheng |
author_sort |
Hanqing Zhao |
title |
Effects of Submerged Vegetation Density on Turbulent Flow Characteristics in an Open Channel |
title_short |
Effects of Submerged Vegetation Density on Turbulent Flow Characteristics in an Open Channel |
title_full |
Effects of Submerged Vegetation Density on Turbulent Flow Characteristics in an Open Channel |
title_fullStr |
Effects of Submerged Vegetation Density on Turbulent Flow Characteristics in an Open Channel |
title_full_unstemmed |
Effects of Submerged Vegetation Density on Turbulent Flow Characteristics in an Open Channel |
title_sort |
effects of submerged vegetation density on turbulent flow characteristics in an open channel |
publisher |
MDPI AG |
series |
Water |
issn |
2073-4441 |
publishDate |
2019-10-01 |
description |
The vegetation density <i>λ</i> affects turbulent flow type in the submerged vegetated river. This laboratory study investigates different types of vegetated turbulent flow, especially the flow at 0.04 < <i>λ</i> < 0.1 and <i>λ</i> = 1.44 by setting the experimental <i>λ</i> within a large range. Vertical distributions of turbulent statistics (velocity, shear stress and skewness coefficients), turbulence kinetic generation rate and turbulence spectra in different <i>λ</i> conditions have been presented and compared. Results indicate that for flow at 0.04 < <i>λ</i> < 0.1, the profiles of turbulent statistics manifest characteristics that are similar to those of both the bed-shear flow and the free-shear flow, and the turbulence spectral curves are characterized with some slight humps within the low-frequency range. For <i>λ</i> = 1.44, the turbulent statistics above the vegetation top demonstrate the characteristics of boundary-shear flow. The spectral curves fluctuate intensely within the low-frequency range, and the spectra of low-frequency eddies above vegetation top are significantly larger than the values below. The change of turbulent flow type induced by an increase of <i>λ</i> would increase the maximum value of turbulence kinetic generation rate <i>G</i><sub>S</sub> and change the point where <i>G</i><sub>S</sub> is vertically maximum upwards to the vegetation top. |
topic |
open channel submerged vegetation density turbulent flow type turbulent statistics turbulence spectra |
url |
https://www.mdpi.com/2073-4441/11/10/2154 |
work_keys_str_mv |
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1725409326479179776 |