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淤地坝冲蚀特性研究

曹喜

广东水利水电Issue(3):17-22,6.
广东水利水电Issue(3):17-22,6.

淤地坝冲蚀特性研究

Experimental Study on the Tracing Mechanism of Steep Slopes in Silt Dams

曹喜1

作者信息

  • 1. 新疆兵团勘测设计院集团股份有限公司,乌鲁木齐 830002
  • 折叠

摘要

Abstract

A silt dam is a soil and water conservation project constructed in the Loess Plateau region to reduce the inflow of sediment into the Yellow River,retain floodwaters and silt,and reclaim farmland from silt.In recent years,the frequent occurrence of water damage disasters in silt dams has made it necessary to conduct research on the mechanism of silt dam failure.This study analyzes the erosion mechanism of the"steep slope"of silt dams in the Loess Plateau region through indoor experiments.The results indicate that the moisture content is the decisive factor determining the erosion morphology.When the moisture content is low,layered erosion is dominant,while when the moisture content is high,it transforms into block instability erosion.The compaction degree and inflow have an impact,but their effect is limited.The research results can provide reference for the design of local silt dams and disaster prevention and control.

关键词

於地坝/漫顶/溃坝机理

Key words

check dam/overtopping/dam breach mechanism

分类

建筑与水利

引用本文复制引用

曹喜..淤地坝冲蚀特性研究[J].广东水利水电,2026,(3):17-22,6.

广东水利水电

1008-0112

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