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流滑型崩岸河岸侧蚀模式初探

假冬冬 张幸农 应强 陈长英 张思和

水科学进展2011,Vol.22Issue(6):813-817,5.
水科学进展2011,Vol.22Issue(6):813-817,5.DOI:32.1309.P.20110911.1135.014

流滑型崩岸河岸侧蚀模式初探

Preliminary study on the analytical model for slide collapse of riverbanks

假冬冬 1张幸农 1应强 1陈长英 1张思和1

作者信息

  • 1. 南京水利科学研究院水文水资源与水利工程科学国家重点实验室,江苏南京210029
  • 折叠

摘要

Abstract

The slide collapse of riverbanks with fast -developing, large rates of bank erosion, and strong destructive powers is a common type of riverbank collapses in alluvial rivers. This type of failure is mainly caused by the direct impact of flow water, as well as resulting from the fact that water level is too close to the top of riverbanks in the course of collapse. An analytical model for the slide collapse of riverbanks is presented based on the analysis of scouring effects on the riverbanks. The model structures and parameters are evaluated using the flume experiments and centrifugal tests. The erosion coefficient of river bank is calibrated using the experimental data. The model result is in good agreement with the experiments. The analytical model contains only a few parameters and is easy to apply . The model result can be used as a reference for the prediction of riverbank erosion and channel migration.

关键词

流滑型崩岸/河岸侧蚀/计算模式/冲积河流/试验研究

Key words

slide collapse of riverbank/ riverbank erosion/ analytical model/ alluvial rivers/ experiment study

分类

建筑与水利

引用本文复制引用

假冬冬,张幸农,应强,陈长英,张思和..流滑型崩岸河岸侧蚀模式初探[J].水科学进展,2011,22(6):813-817,5.

基金项目

国家自然科学基金资助项目(50779038 ()

51109140) ()

水科学进展

OA北大核心CSCDCSTPCD

1001-6791

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