Effect of Flume Width on the Hydraulic Properties of Overland Flow from Laboratory Observation

The effect of flume width (b) on overland flow dynamics was investigated in this study. Experiments were conducted with five different flow discharges and five flume widths (0.05–0.30 m, with an interval of 0.05 m). The findings revealed that a narrow flume had a noticeable impact on flow accelerati...

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Main Authors: Ye Tian, Yue Xu, Maojin Yang, Fangshi Jiang, Yue Zhang, Yanhe Huang, Jinshi Lin
Format: Article
Language:English
Published: MDPI AG 2023-09-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/15/19/3416
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author Ye Tian
Yue Xu
Maojin Yang
Fangshi Jiang
Yue Zhang
Yanhe Huang
Jinshi Lin
author_facet Ye Tian
Yue Xu
Maojin Yang
Fangshi Jiang
Yue Zhang
Yanhe Huang
Jinshi Lin
author_sort Ye Tian
collection DOAJ
description The effect of flume width (b) on overland flow dynamics was investigated in this study. Experiments were conducted with five different flow discharges and five flume widths (0.05–0.30 m, with an interval of 0.05 m). The findings revealed that a narrow flume had a noticeable impact on flow acceleration as the slope length increased. Relative average deviation (RAD) was calculated to evaluate the influence of sidewall effects on flow velocity. The coefficient of variation in the RAD ranged from 1.90% to 3.65%. The RAD has extremely significant differences between different widths when the flow is 0.02–0.08 m<sup>2</sup>/min. The significant differences in the RAD at different widths decrease as the flow rate increases. The flow regime was evaluated using the ratio of the thickness of the viscous sublayer to the water depth (<i>δ</i>/<i>h</i>), which proved to be a better indicator than the Reynolds number for studying flow regimes in different flume widths. Furthermore, it was observed that the energy variation was smaller in narrow flumes (b = 0.5–0.10 m) compared to wider flumes (b = 0.25–0.30 m). When the flume width ranged from 0.15 to 0.30 m, the specific energy change increased. These results contribute to further understanding of the hydraulic characteristics of overland flow and provide theoretical references for optimizing experimental design.
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spelling doaj.art-e0c3d398bf5847b8be3707bee32c21b42023-11-30T20:49:48ZengMDPI AGWater2073-44412023-09-011519341610.3390/w15193416Effect of Flume Width on the Hydraulic Properties of Overland Flow from Laboratory ObservationYe Tian0Yue Xu1Maojin Yang2Fangshi Jiang3Yue Zhang4Yanhe Huang5Jinshi Lin6Jinshan Soil and Water Conservation Research Center, Fujian Agriculture and Forestry University, Fuzhou 350002, ChinaJinshan Soil and Water Conservation Research Center, Fujian Agriculture and Forestry University, Fuzhou 350002, ChinaJinshan Soil and Water Conservation Research Center, Fujian Agriculture and Forestry University, Fuzhou 350002, ChinaJinshan Soil and Water Conservation Research Center, Fujian Agriculture and Forestry University, Fuzhou 350002, ChinaJinshan Soil and Water Conservation Research Center, Fujian Agriculture and Forestry University, Fuzhou 350002, ChinaJinshan Soil and Water Conservation Research Center, Fujian Agriculture and Forestry University, Fuzhou 350002, ChinaJinshan Soil and Water Conservation Research Center, Fujian Agriculture and Forestry University, Fuzhou 350002, ChinaThe effect of flume width (b) on overland flow dynamics was investigated in this study. Experiments were conducted with five different flow discharges and five flume widths (0.05–0.30 m, with an interval of 0.05 m). The findings revealed that a narrow flume had a noticeable impact on flow acceleration as the slope length increased. Relative average deviation (RAD) was calculated to evaluate the influence of sidewall effects on flow velocity. The coefficient of variation in the RAD ranged from 1.90% to 3.65%. The RAD has extremely significant differences between different widths when the flow is 0.02–0.08 m<sup>2</sup>/min. The significant differences in the RAD at different widths decrease as the flow rate increases. The flow regime was evaluated using the ratio of the thickness of the viscous sublayer to the water depth (<i>δ</i>/<i>h</i>), which proved to be a better indicator than the Reynolds number for studying flow regimes in different flume widths. Furthermore, it was observed that the energy variation was smaller in narrow flumes (b = 0.5–0.10 m) compared to wider flumes (b = 0.25–0.30 m). When the flume width ranged from 0.15 to 0.30 m, the specific energy change increased. These results contribute to further understanding of the hydraulic characteristics of overland flow and provide theoretical references for optimizing experimental design.https://www.mdpi.com/2073-4441/15/19/3416flow patternflume widthoverland flowsoil erosionspecific energy
spellingShingle Ye Tian
Yue Xu
Maojin Yang
Fangshi Jiang
Yue Zhang
Yanhe Huang
Jinshi Lin
Effect of Flume Width on the Hydraulic Properties of Overland Flow from Laboratory Observation
Water
flow pattern
flume width
overland flow
soil erosion
specific energy
title Effect of Flume Width on the Hydraulic Properties of Overland Flow from Laboratory Observation
title_full Effect of Flume Width on the Hydraulic Properties of Overland Flow from Laboratory Observation
title_fullStr Effect of Flume Width on the Hydraulic Properties of Overland Flow from Laboratory Observation
title_full_unstemmed Effect of Flume Width on the Hydraulic Properties of Overland Flow from Laboratory Observation
title_short Effect of Flume Width on the Hydraulic Properties of Overland Flow from Laboratory Observation
title_sort effect of flume width on the hydraulic properties of overland flow from laboratory observation
topic flow pattern
flume width
overland flow
soil erosion
specific energy
url https://www.mdpi.com/2073-4441/15/19/3416
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