Abstract

The “secondary suspended river” poses a huge threat to the safety of embankment in the lower reaches of the Yellow River. The formation of the “secondary suspended river” is mainly attributed to the “less water and more sediment, inconsistent water-sediment relationship” of the Yellow River. Through the analysis of the relationship between the evolution of the lower reaches of the Yellow River and the loss caused by disasters and flood and magnitude of sediment concentration, this paper thinks that the Yellow River must pay attention to the graded regulation of water and sediment. For small and medium-sized flood with small sediment concentration, according to the flood magnitude and the reservoir water volume in the upper and middle reaches, Impoundment and filling water to build the peak time at the right time is necessary and the flood processes which are less than 2600 m3/s should be avoided in the scheduling process. Based on the shape of river channel of high flow flood in floodplain and average flow flood in floodplain, and the difference between the sediment transport efficiency of flood and the difference between the loss to the lower floodplain area, the average flow flood in floodplain which is between 6000 m3/s should be avoided in the scheduling process as far as possible. In order to relieve the development trend of the “secondary suspended river”, the regulation of “brushing groove of silt beach” should be insisted on for large flood. But the high sediment concentration flood should be avoided because of its serious destructive effect on the lower reach. At the same time, it also calls for strengthening the research and popularization of reservoir sediment treatment and sediment resource utilization technology.

Highlights

  • The lower reaches of the Yellow River are in a state of intense sedimentation and lifting, and the river bed is higher than the two sides of the ground, forming the “suspended river”

  • Based on the evolution of the lower reaches of the Yellow River and the changes of the loss caused by disasters, the author discusses the concept of graded management of water and sediment in the lower reaches of the Yellow River, considers the influence of various factors and constructs a coordinated flood process to alleviate or contain the disadvantageous situation of the “secondary suspended river”

  • Regardless of annual sediment discharge or average sediment concentration, the Yellow River ranks first in the world’s rivers[2]. It is precisely because the flood of the Yellow River rises and falls sharply, and the peak value is high and the flow is small and the damage of the high sediment concentration flood sedimentation to the river channel is serious that the flood has caused great harm to the flood control safety of the lower reaches

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Summary

Introduction

The lower reaches of the Yellow River are in a state of intense sedimentation and lifting, and the river bed is higher than the two sides of the ground, forming the “suspended river”. The “secondary suspended river” situation is the most serious in the reach from Dongbatou to Taochengpu, and it is one of the most important flood control tasks in the lower reach of the Yellow River. The situation of “secondary suspended river” with high beach lip and lowlyling levee root is becoming more and more serious, which increases the burden of flood control and difficulty of river regulation in the lower reaches. Based on the evolution of the lower reaches of the Yellow River and the changes of the loss caused by disasters, the author discusses the concept of graded management of water and sediment in the lower reaches of the Yellow River, considers the influence of various factors and constructs a coordinated flood process to alleviate or contain the disadvantageous situation of the “secondary suspended river”

Materials and Methods
Evolution characteristics of flood in the lower reaches of the Yellow River
Different shaping effects on river channel morphology of different floods
Conclusions
Findings
Discussion
Full Text
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