Estimation of friction factor and bed shear stress considering bedform effect in rivers

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL Earth Surface Processes and Landforms Pub Date : 2024-08-08 DOI:10.1002/esp.5954
Minjae Lee, Yong Sung Park, Mikyung Lee, Yong-Sik Song, Chanho Park
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Abstract

The roughness height plays a crucial role, especially in shallow-water environments with rough-bed conditions. Specifically, it is a key parameter for predicting flow velocity and bed shear stress. Therefore, an accurate determination of roughness height is essential for precise predictions of hydraulic phenomena. In this study, we propose a method to estimate form roughness height and friction factor using bathymetry data, with a focus on cross-sectional data in the transverse direction. To overcome the limitations of using lateral direction data, we derived an empirical formula for estimating bedform length from the bed profiles in the streamwise direction. To assess the validity of bedform analysis and estimated form roughness height based on lateral direction data, we compared the characteristics of bedform and form roughness height analysed using lateral direction data with those analysed using the streamwise direction data. Furthermore, we confirmed the importance of considering the form roughness height in estimating bed shear stress through a comparison with bed shear stress calculations considering only grain roughness height.

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考虑河床形态效应的摩擦因数和河床剪应力估算
粗糙度高度起着至关重要的作用,尤其是在具有粗糙床条件的浅水环境中。具体来说,它是预测流速和床面剪应力的关键参数。因此,准确测定粗糙度高度对于精确预测水力现象至关重要。在本研究中,我们提出了一种利用水深测量数据估算形式粗糙度高度和摩擦因数的方法,重点是横向的断面数据。为了克服使用横向数据的局限性,我们推导出了一个经验公式,用于根据流向的床面剖面估算床面长度。为了评估基于横向数据的床形分析和形态粗糙度高度估算的有效性,我们将使用横向数据分析的床形特征和形态粗糙度高度与使用流向数据分析的床形特征和形态粗糙度高度进行了比较。此外,我们还通过与仅考虑颗粒粗糙度高度的床面剪应力计算结果进行比较,确认了考虑颗粒粗糙度高度对估算床面剪应力的重要性。
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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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