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黄河宁夏河段河道演变分析

马云 包淑萍 陈丹 李淑霞 王生鑫 于慧黎

人民黄河Issue(9):38-40,3.
人民黄河Issue(9):38-40,3.DOI:10.3969/j.issn.1000-1379.2014.09.012

黄河宁夏河段河道演变分析

Analysis of the Channel Evolution in Ningxia Reach of the Yellow River

马云 1包淑萍 1陈丹 1李淑霞 1王生鑫 1于慧黎1

作者信息

  • 1. 宁夏回族自治区水文水资源勘测局,宁夏银川750001
  • 折叠

摘要

Abstract

Through the analysis of Ningxia reaches of the channel evolution of the Yellow River,it researched on the erosion and scour and river re-gime changes of the river section in Ningxia. The results show that in the period of 1993-2009,in Ningxia section of the Yellow River Xiaheyan to Qingtongxia river channel erosion and deposition of average balance to Qingtongxia to Shizuishan reach of the river is in silting status. Ningxia section of river channel scouring and silting variation depend largely on the conditions of water and sediment,water and sediment and flood in,full of sediment siltation in the river main channel within the main channel siltation shrink,small and medium water level significantly inflated. River in Ningxia section of the Yellow River canyon and pebble river bed scour and less mainstream swing,the rest of river beds scour and mainstream swing are greater. The implementation of river training works on the controlling river regime changes has an effect. Ningxia section of the Yellow River water and sediment conditions,river boundary condition and river bed texture are the causes to influence the channel evolution.

关键词

河道演变/河势变化/水沙变化/黄河宁夏河段

Key words

channel evolution/change of river regime/water and sediment variation/Ningxia river reach of Yellow River

分类

建筑与水利

引用本文复制引用

马云,包淑萍,陈丹,李淑霞,王生鑫,于慧黎..黄河宁夏河段河道演变分析[J].人民黄河,2014,(9):38-40,3.

人民黄河

OA北大核心

1000-1379

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