漫滩
沉积物
频道(广播)
流量(数学)
横截面
泥沙输移
地质学
背景(考古学)
水文学(农业)
河流形态
环境科学
机械
岩土工程
地貌学
物理
河流
计算机科学
工程类
结构工程
古生物学
计算机网络
构造盆地
作者
Shasha Han,Lianjun Zhao,Ao Chang,Baichuan Liu,Jingwen Wang,Jie Li
出处
期刊:Water
[Multidisciplinary Digital Publishing Institute]
日期:2024-04-24
卷期号:16 (9): 1213-1213
被引量:4
摘要
As a prerequisite and foundation for studying the evolution mechanism of river channels, an in-depth understanding of the cross-sectional morphology adjustment is required. As a starting point, it is crucial to systematically summarize and generalize the research findings on channel morphological adjustment obtained to date, particularly in the context of the significant changes in the water and sediment conditions of large rivers that have occurred worldwide. This paper provides a comprehensive review of the research findings on the three following aspects of the Lower Yellow River: the transverse distribution of overbank flow velocity, the transverse distribution of suspended sediment concentration, and the morphological adjustment of the river cross-section. There are various equations available to predict the lateral depth–average flow velocity distribution. These equations are classified into the two following categories: empirical and theoretical formulas. Theoretical formulas are obtained through consideration of the cross-sectional morphology, accounting for inertial force terms caused by secondary flow, and momentum transfer between the main channel and its floodplain. Similarly, empirical equations and theoretical formulas for sediment concentration transverse distribution are also summarized, given the different influencing factors and assumptions. We also discuss the morphological adjustment of river cross-sections based on the analysis of measured data, mathematical model calculation, and the physical model test. In particular, we propose the idea of revealing channel cross-section morphology evolution mechanisms from the theoretical level of water and sediment movement and distribution. This review aims to enhance understanding of overbank flow, sediment transport, and channel morphology in the Lower Yellow River and may also serve to some extent as a reference for the evolution and management of channels in other rivers.
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