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无粘性土堤漫顶溃决水流运动试验研究

魏红艳 余明辉 梁艳洁

水科学进展2011,Vol.22Issue(4):532-538,7.
水科学进展2011,Vol.22Issue(4):532-538,7.DOI:32.1309.P.20110709.1622.019

无粘性土堤漫顶溃决水流运动试验研究

Experimental study on overtopping flow of non-cohesive embankments

魏红艳 1余明辉 1梁艳洁1

作者信息

  • 1. 武汉大学水资源与水电工程科学国家重点实验室,湖北武汉430072
  • 折叠

摘要

Abstract

Correctly describing the flow process near the breach site and the variation of breach discharge is essential to the prediction of overtopping flow and flood propagation, which provide valuable information for breach blocking and disaster preparation, as well as flood damage assessment. Based on the observational result from a series of bend flume experiments, the erosion process during overtopping breaching of non-cohesive embankments can be divided into four stages, overtopping, groove formation, breach stretching and stability. The analysis involves the variation in water levels and flood discharge in the river after overtopping breaching, the water-level difference between the inner and outer river, and the influence of embankment materials on water-level changes near the breach site. Finally, the study summarizes the relationship among the breaching discharge, the breach width and the water head near the site.

关键词

无粘性土堤漫顶溃决/弯道水槽试验/溃口处水流形态/溃决流量

Key words

overtopping breaching of non-cohesive embankments/ bend flume experiments/ flow patterns near the breach/ breaching discharge

分类

建筑与水利

引用本文复制引用

魏红艳,余明辉,梁艳洁..无粘性土堤漫顶溃决水流运动试验研究[J].水科学进展,2011,22(4):532-538,7.

基金项目

国家重点基础研究发展计划(973)资助项目(2007CB714100) (973)

国家自然科学基金资助项目(11072180) (11072180)

水科学进展

OA北大核心CSCDCSTPCD

1001-6791

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