DocumentCode
1989594
Title
Notice of Retraction
Evolution of the channel geomorphology and flood management countermeasures of the middle and lower Yangtze River
Author
Li Chang-an ; Shao Leiz ; Huang Chang-Sheng ; Kang Chun-guo
Author_Institution
Key Lab. of Biogeology & Environ. Geol. of Minist. of Educ., China Univ. of Geosci., Wuhan, China
Volume
4
fYear
2010
fDate
17-18 July 2010
Firstpage
446
Lastpage
448
Abstract
Notice of Retraction
After careful and considered review of the content of this paper by a duly constituted expert committee, this paper has been found to be in violation of IEEE´s Publication Principles.
We hereby retract the content of this paper. Reasonable effort should be made to remove all past references to this paper.
The presenting author of this paper has the option to appeal this decision by contacting TPII@ieee.org.
River channel geomorphologic evolution is the basis of flood control and regulation. With the information of satellite images and field investigation, the article emphatically analyzes the geomorphologic evolution characteristics and stability of meandering channels and gooseneck-bifurcated channel, both of which are the most typical and unstable types in the middle and lower Yangtze River. Evolution of meandering channels has characteristics of periodicity and length constraint. The fractal dimension of Lower-Jingjiang is between 1.078 and 1.23. When it reaches a value between 1.19 and 1.23, river channel goes to an unstable status, in that case the fractal dimension will have mutation from big to small, because of the channel cutoff. Stone serving as node, heart-shape beach, branch inflow are the main conditions of the forming of gooseneck-bending channel. Most gooseneck-bifurcated channel has the characteristics of periodicity integer nested translation. Recently most of the left branches are at the stage of bankrupt-siltation-bank combined Lower-Jingjiang meandering channel has the characteristics of variability at the transverse direction and linkage at the vertical direction, so river regulation should be based on the whole part of the river. Bifurcated channel below Chenglingji should be governed from different units according to the node. More branches, more unstable the channel will become, besides, the branch also has the characteristics of linkage, and so all branches should be treated as an entirety w- en having the river regulation.
After careful and considered review of the content of this paper by a duly constituted expert committee, this paper has been found to be in violation of IEEE´s Publication Principles.
We hereby retract the content of this paper. Reasonable effort should be made to remove all past references to this paper.
The presenting author of this paper has the option to appeal this decision by contacting TPII@ieee.org.
River channel geomorphologic evolution is the basis of flood control and regulation. With the information of satellite images and field investigation, the article emphatically analyzes the geomorphologic evolution characteristics and stability of meandering channels and gooseneck-bifurcated channel, both of which are the most typical and unstable types in the middle and lower Yangtze River. Evolution of meandering channels has characteristics of periodicity and length constraint. The fractal dimension of Lower-Jingjiang is between 1.078 and 1.23. When it reaches a value between 1.19 and 1.23, river channel goes to an unstable status, in that case the fractal dimension will have mutation from big to small, because of the channel cutoff. Stone serving as node, heart-shape beach, branch inflow are the main conditions of the forming of gooseneck-bending channel. Most gooseneck-bifurcated channel has the characteristics of periodicity integer nested translation. Recently most of the left branches are at the stage of bankrupt-siltation-bank combined Lower-Jingjiang meandering channel has the characteristics of variability at the transverse direction and linkage at the vertical direction, so river regulation should be based on the whole part of the river. Bifurcated channel below Chenglingji should be governed from different units according to the node. More branches, more unstable the channel will become, besides, the branch also has the characteristics of linkage, and so all branches should be treated as an entirety w- en having the river regulation.
Keywords
bifurcation; floods; fractals; geomorphology; rivers; Chenglingji; China; Lower-Jingjiang; branch inflow; channel cutoff; flood control; flood management countermeasures; fractal dimension; gooseneck-bending channel; gooseneck-bifurcated channel; heart-shape beach; length constraint; lower Yangtze River; lower-Jingjiang meandering channel; middle Yangtze River; periodicity; river channel geomorphologic evolution; river regulation; satellite images; transverse direction; vertical direction; Artificial intelligence; Navigation; flood management countermeasures; gooseneck bifurcated channel; meandering channel; middle and lower Yangtze River; river channel geomorphologic evolution;
fLanguage
English
Publisher
ieee
Conference_Titel
Environmental Science and Information Application Technology (ESIAT), 2010 International Conference on
Conference_Location
Wuhan
Print_ISBN
978-1-4244-7387-8
Type
conf
DOI
10.1109/ESIAT.2010.5567402
Filename
5567402
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