Experimental study on the entrainment of bed material into debris flow

S. Egashira , N. Honda , T. Itoh
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引用次数: 149

Abstract

The present study describes entraining characteristics of bed material into debris flow, based on flume tests, numerical and dimensional analyses. Flume tests are conducted to investigate influences of bed sediment size on erosion rate by supplying debris flows having unsaturated sediment concentration onto erodible beds. Experimental results show that the relative erosion rate, E/E0, decreases monotonically with increase of relative sediment size, d/d0, although E/E0 changes slightly with sediment concentration of debris flow. Herein, E is the erosion rate of bed sediment of size, d, E0 is the erosion rate when solid particle size, d0, of debris flow, are the same of the erodible bed material. According to the relation between E/E0 and d/d0, erosion rate, E, can be estimated by using Egashira's formula for E0. Therefore, the validity of erosion rate formula for E0 is tested by solving numerically for debris flow characteristics in terms of governing equations. In addition, critical size of bed sediment entrainment is discussed by introducing non-dimensional effective bed shear stress which is formulated by using fluid shear stress (total shear stress minus yield stress), bed sediment size, d, specific weight of sediment particle in water and acceleration due to gravity, and it is found that the critical non-dimensional effective shear stress takes a value similar to critical Shields parameter for bed load movement.

泥石流中床质夹带的实验研究
本研究基于水槽试验、数值分析和量纲分析,描述了河床物质进入泥石流的夹带特性。通过水槽试验,将含非饱和泥沙浓度的泥石流输送到可侵蚀河床,研究河床泥沙粒径对侵蚀速率的影响。实验结果表明,相对侵蚀速率E/E0随相对泥沙粒径d/d0的增加而单调减小,但E/E0随泥石流含沙量的增加变化不大。式中,E为粒径河床沉积物的侵蚀速率,d, E0为泥石流固体粒径d0与可蚀河床物质相同时的侵蚀速率。根据E/E0与d/d0的关系,可以用Egashira的E0公式来估算侵蚀速率E。因此,通过控制方程对泥石流特征进行数值求解,验证了E0侵蚀速率公式的有效性。此外,通过引入由流体剪切应力(总剪切应力减去屈服应力)、床质粒径、d、水中泥沙颗粒比重和重力加速度组成的无量纲有效床质剪切应力,讨论了床质夹带的临界尺寸,发现临界无量纲有效剪切应力的取值与床质运动的临界Shields参数相似。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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