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A comparative analysis of Lajeunesse model with other used bed load models - effects on river morphological changes

机译:Lajeunesse模型与其他二手床荷模型的比较分析-对河流形态变化的影响

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Among the phenomena that greatly influence the river morphology is the sediment transport, especially the bed load mode causing a significant changes in the river morphology. Indeed, the choice of a model or a methodology that can better quantify sediment transport, remains always poorly understood. In this context, a new approach to studying the morphological evolution of rivers is proposed by Charru in 2004, it is based on a model for the erosion and deposition of the particles under laminar flow. In 2006, Charru proposes an extension of this model to turbulent flow. In more advanced research, Lajeunesse in 2010, realizes an experimental study to support the erosion deposition model of Charru, and proposes a new formula to calculate the bed load transport rate. The current research focuses on the effects of bed load transport on the morphological changes in rivers. In the first part, a comparative analysis of empirical laws of bed load transport with experimental data was conducted, in order to test and validate the new bed load model proposed by Lajeunesse, then to check the grain size effect on the sediment transport capacity. In the second part, we are interested in the study of the morphological evolution in rivers. It was performed through numerical modeling using TELEMAC 2D coupled with SISYPHE. The aim is to understand and analyze the morphological changes in the channel bottom. The analysis of the results presented in this paper showed that through the calculated score, most formulas give satisfactory results. In particular at the grain scale, the new bed load transport relation of Lajeunesse, provides an excellent fit to the experimental data. Finally, we were interested in the study of the morphological changes in the channel bottom, it appers clear that the bed load transport has large impacts on river morphology.
机译:极大地影响河流形态的现象包括泥沙输送,尤其是河床荷载模式导致河流形态发生重大变化。确实,人们对如何更好地量化沉积物迁移的模型或方法的选择始终知之甚少。在这种情况下,Charru在2004年提出了一种研究河流形态演变的新方法,该方法基于层流下颗粒的侵蚀和沉积模型。 2006年,Charru提出将此模型扩展到湍流。在更高级的研究中,Lajeunesse在2010年完成了一项支持Charru侵蚀沉积模型的实验研究,并提出了计算床载运移速率的新公式。目前的研究集中在河床荷载运输对河流形态变化的影响上。在第一部分中,通过实验数据对床层负荷输送的经验规律进行了比较分析,以测试和验证Lajeunesse提出的新的床层负荷模型,然后检验粒度对沉积物输送能力的影响。在第二部分中,我们对河流形态演变的研究感兴趣。它是通过使用TELEMAC 2D和SISYPHE进行数值建模来执行的。目的是了解和分析通道底部的形态变化。对本文提出的结果进行的分析表明,通过计算出的分数,大多数公式都能得出令人满意的结果。特别是在谷物规模上,Lajeunesse的新床载运输关系非常适合实验数据。最后,我们对河床底部形态变化的研究很感兴趣,显然可以看出,河床荷载的输送对河流形态有很大的影响。

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