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三峡水库运行初期的泥沙淤积特点

李文杰 杨胜发 付旭辉 肖毅

水科学进展2015,Vol.26Issue(5):676-685,10.
水科学进展2015,Vol.26Issue(5):676-685,10.DOI:10.14042/j.cnki.32.1309.2015.05.009

三峡水库运行初期的泥沙淤积特点

Sedimentation characteristics in the Three Gorges Reservoir during the initial operation stage

李文杰 1杨胜发 1付旭辉 2肖毅2

作者信息

  • 1. 重庆交通大学国家内河航道整治工程技术研究中心, 重庆 400074
  • 2. 重庆交通大学水利水运工程教育部重点实验室, 重庆 400074
  • 折叠

摘要

Abstract

The sedimentation characteristics in the Three Gorges Reservoir ( TGR) are studied by analyzing measured sediment load and cross section data. Results indicate that the total deposition amount and effective sediment export ra-tio from 2003 to 2013 are 1. 531 billion tons and 24. 5%, respectively, and both are less than those estimated during design. The sediment is primarily deposited in the wide and curved reaches in the permanent backwater region. It dis-tributes evenly over the cross sections in the wide reaches and on the side of the sections with low velocity in the curved reaches. No deposition occurs in gorges. The deposition rates near the dam tend to decrease, while those of the upper reaches are increasing. The longitudinal particle size variation is not obvious, and the median particle diameters of the deposition in the permanent backwater region are mostly less than 0. 01 mm. The thalweg of the gorge reaches have no changes, and the deposition delta is not found. The deposition in the backwater zone and the associated in-creasing of the tail water level are less than previous estimations. These suggest that the gorge reaches play a role of a local erosion base level due to their sufficient sediment carrying capacities, and it is unlikely that a unified equilibrium bed slope will be developed in the TGR.

关键词

泥沙/淤积/挟沙力/平衡比降/三峡水库

Key words

sediment/deposition/sediment carrying capacity/equilibrium bed slope/Three Gorges Reservoir

分类

建筑与水利

引用本文复制引用

李文杰,杨胜发,付旭辉,肖毅..三峡水库运行初期的泥沙淤积特点[J].水科学进展,2015,26(5):676-685,10.

基金项目

国家自然科学基金资助项目( 51209241) ( 51209241)

交通运输部应用基础研究项目( 2014329814310)The study is financially supported by the National Natural Science Foundation of China ( No. 51209241) and the Basic Research Project of China Ministry of Transport ( No. 2014329814310) . ( 2014329814310)

水科学进展

OA北大核心CSCDCSTPCD

1001-6791

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