Exploring coupling effects of rainfall and surface roughness on the sheet flow velocity

Accurately describing the path of sheet flow (SF) is crucial in soil erosion. Raindrop impact and underlying surface conditions can affect the SF velocity by changing the velocity profile. However, since this information is rarely known, the estimation of SF velocity is inaccurate. A series of upstr...

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Main Authors: Enshuai Shen, Gang Liu, Qiong Zhang, Chenxi Dan, Chang Liu, Hairu Li, Ya Liu, Xueming Qu, Xiaolin Xia, Dandan Liu, Zhen Guo, Xining Zhao
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2025-03-01
Series:International Soil and Water Conservation Research
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Online Access:http://www.sciencedirect.com/science/article/pii/S2095633924000662
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author Enshuai Shen
Gang Liu
Qiong Zhang
Chenxi Dan
Chang Liu
Hairu Li
Ya Liu
Xueming Qu
Xiaolin Xia
Dandan Liu
Zhen Guo
Xining Zhao
author_facet Enshuai Shen
Gang Liu
Qiong Zhang
Chenxi Dan
Chang Liu
Hairu Li
Ya Liu
Xueming Qu
Xiaolin Xia
Dandan Liu
Zhen Guo
Xining Zhao
author_sort Enshuai Shen
collection DOAJ
description Accurately describing the path of sheet flow (SF) is crucial in soil erosion. Raindrop impact and underlying surface conditions can affect the SF velocity by changing the velocity profile. However, since this information is rarely known, the estimation of SF velocity is inaccurate. A series of upstream inflow and rainfall experiments were carried out on an impermeable flume to determine the coupling effects of rainfall and rough bed surfaces on the SF velocity and correction factor (α). The results showed that the roughness of the bed surface had a more pronounced effect on reducing the mean velocity compared to the surface velocity in both cases with and without raindrop impact. The raindrop impact notably reduced the flow velocity near the water surface, while the mean velocity slightly decreased or remained almost constant with increasing rainfall intensity. The reduction in SF velocity can be explained by the combined effects of the roughness reducing the mean velocity (up to 33.52%) and the raindrop impact reducing the surface velocity (up to 25.43%). In addition, α was not a constant when the SF was subjected to raindrop impact. The rainfall was found to increase α, while the roughness of the bed surface reduced α for all cases. Finally, a model was created to forecast α based on the ratio of water depth to roughness height, hydraulic slope, and rain Reynolds number. The results are valuable in soil erosion by providing accurate α for estimating the surface and mean velocities of SF.
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spelling doaj-art-5445fe47ccd745a3bb254410547996f02025-01-07T04:17:16ZengKeAi Communications Co., Ltd.International Soil and Water Conservation Research2095-63392025-03-01131164176Exploring coupling effects of rainfall and surface roughness on the sheet flow velocityEnshuai Shen0Gang Liu1Qiong Zhang2Chenxi Dan3Chang Liu4Hairu Li5Ya Liu6Xueming Qu7Xiaolin Xia8Dandan Liu9Zhen Guo10Xining Zhao11State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, College of Soil and Water Conservation Science and Engineering (Institute of Soil and Water Conservation), Northwest A&F University, Yangling, 712100, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, College of Soil and Water Conservation Science and Engineering (Institute of Soil and Water Conservation), Northwest A&F University, Yangling, 712100, China; Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, 712100, China; Corresponding author. Institute of Soil and Water Conservation, Northwest A&F University, No. 26, Xinong Road, Yangling, Shaanxi Province, 712100, China.State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, College of Soil and Water Conservation Science and Engineering (Institute of Soil and Water Conservation), Northwest A&F University, Yangling, 712100, China; Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, 712100, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, College of Soil and Water Conservation Science and Engineering (Institute of Soil and Water Conservation), Northwest A&F University, Yangling, 712100, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, College of Soil and Water Conservation Science and Engineering (Institute of Soil and Water Conservation), Northwest A&F University, Yangling, 712100, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, College of Soil and Water Conservation Science and Engineering (Institute of Soil and Water Conservation), Northwest A&F University, Yangling, 712100, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, College of Soil and Water Conservation Science and Engineering (Institute of Soil and Water Conservation), Northwest A&F University, Yangling, 712100, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, College of Soil and Water Conservation Science and Engineering (Institute of Soil and Water Conservation), Northwest A&F University, Yangling, 712100, ChinaKey Laboratory of Water Conservancy and Water Resources of Anhui Province, Bengbu, 233000, ChinaKey Laboratory of Water Conservancy and Water Resources of Anhui Province, Bengbu, 233000, ChinaSichuan Huabiaoce Testing Technology Co. Ltd., Chengdu, 610097, ChinaState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, College of Soil and Water Conservation Science and Engineering (Institute of Soil and Water Conservation), Northwest A&F University, Yangling, 712100, China; Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, 712100, ChinaAccurately describing the path of sheet flow (SF) is crucial in soil erosion. Raindrop impact and underlying surface conditions can affect the SF velocity by changing the velocity profile. However, since this information is rarely known, the estimation of SF velocity is inaccurate. A series of upstream inflow and rainfall experiments were carried out on an impermeable flume to determine the coupling effects of rainfall and rough bed surfaces on the SF velocity and correction factor (α). The results showed that the roughness of the bed surface had a more pronounced effect on reducing the mean velocity compared to the surface velocity in both cases with and without raindrop impact. The raindrop impact notably reduced the flow velocity near the water surface, while the mean velocity slightly decreased or remained almost constant with increasing rainfall intensity. The reduction in SF velocity can be explained by the combined effects of the roughness reducing the mean velocity (up to 33.52%) and the raindrop impact reducing the surface velocity (up to 25.43%). In addition, α was not a constant when the SF was subjected to raindrop impact. The rainfall was found to increase α, while the roughness of the bed surface reduced α for all cases. Finally, a model was created to forecast α based on the ratio of water depth to roughness height, hydraulic slope, and rain Reynolds number. The results are valuable in soil erosion by providing accurate α for estimating the surface and mean velocities of SF.http://www.sciencedirect.com/science/article/pii/S2095633924000662RunoffErosion assessmentCorrection factorHillslope hydrologyHydraulic parameter
spellingShingle Enshuai Shen
Gang Liu
Qiong Zhang
Chenxi Dan
Chang Liu
Hairu Li
Ya Liu
Xueming Qu
Xiaolin Xia
Dandan Liu
Zhen Guo
Xining Zhao
Exploring coupling effects of rainfall and surface roughness on the sheet flow velocity
International Soil and Water Conservation Research
Runoff
Erosion assessment
Correction factor
Hillslope hydrology
Hydraulic parameter
title Exploring coupling effects of rainfall and surface roughness on the sheet flow velocity
title_full Exploring coupling effects of rainfall and surface roughness on the sheet flow velocity
title_fullStr Exploring coupling effects of rainfall and surface roughness on the sheet flow velocity
title_full_unstemmed Exploring coupling effects of rainfall and surface roughness on the sheet flow velocity
title_short Exploring coupling effects of rainfall and surface roughness on the sheet flow velocity
title_sort exploring coupling effects of rainfall and surface roughness on the sheet flow velocity
topic Runoff
Erosion assessment
Correction factor
Hillslope hydrology
Hydraulic parameter
url http://www.sciencedirect.com/science/article/pii/S2095633924000662
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