粉质黏土堤防漫溢溃决试验

魏红艳; 余明辉; 李义天; 吴松柏

doi:10.14042/j.cnki.32.1309.2015.05.008

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粉质黏土堤防漫溢溃决试验

魏红艳, 余明辉, 李义天, 吴松柏

文章导航 > 水科学进展 > 2015 > 26(5): 668-675

魏红艳, 余明辉, 李义天, 吴松柏. 粉质黏土堤防漫溢溃决试验[J]. 水科学进展, 2015, 26(5): 668-675. doi: 10.14042/j.cnki.32.1309.2015.05.008

引用本文:

魏红艳, 余明辉, 李义天, 吴松柏. 粉质黏土堤防漫溢溃决试验[J]. 水科学进展, 2015, 26(5): 668-675. doi: 10.14042/j.cnki.32.1309.2015.05.008

WEI Hongyan, YU Minghui, LI Yitian, WU Songbai. Experimental study on overflow breaching of embankments constructed with silty clay[J]. Advances in Water Science, 2015, 26(5): 668-675. doi: 10.14042/j.cnki.32.1309.2015.05.008

Citation:

WEI Hongyan, YU Minghui, LI Yitian, WU Songbai. Experimental study on overflow breaching of embankments constructed with silty clay[J]. Advances in Water Science, 2015, 26(5): 668-675. doi: 10.14042/j.cnki.32.1309.2015.05.008

粉质黏土堤防漫溢溃决试验

doi: 10.14042/j.cnki.32.1309.2015.05.008

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

基金项目: 国家自然科学基金资助项目(11272240;11502174)

详细信息

作者简介:
魏红艳(1985—),女,山东济南人,博士后,主要从事河流动力学研究.E-mail:weihongyan@whu.edu.cn

通讯作者:
余明辉,E-mail:mhyu@whu.edu.cn

中图分类号: TV145

Experimental study on overflow breaching of embankments constructed with silty clay

State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan 430072, China

摘要: 为研究粉质黏土堤防漫溢溃决破坏过程及其对水流要素和土体性质的响应规律,以河道流量、筑堤土体含水率和孔隙率为变量,在弯道水槽中开展了9组堤防漫溢溃决概化试验.通过试验发现,粉质黏土堤漫溢溃决溃口发展过程可分为垂向侵蚀和横向扩宽两个阶段,垂向侵蚀阶段以"陡坎"后退为主要形式;筑堤土体含水率与孔隙率不仅影响了溃口垂向侵蚀以及横向扩宽速度,而且决定了溃口最终形态,河道流量主要影响堤防溃口的横向扩宽速度;溃口处流速以及下游水位变化受溃口高度的制约.拟合得到土体黏聚力与土体含水率、孔隙率的相关关系式;通过试验数据提出了由土体黏聚力和水流参数表达的"陡坎"侵蚀后退速度计算公式,证明具有一定合理性.
- 粉质黏土堤防 /
- 漫溢溃决 /
- 含水率 /
- 孔隙率 /
- 黏聚力 /
- "陡坎"侵蚀
Abstract: The purpose of this study is aims to investigate overflow breaching process of embankments constructed with silty clay and their as well as its response to flow and soil characteristics. Nine groups of experiments were conducted on the overflow breaching of cohesive embankments were conducted in a bend flume. Factors considered included inflow discharge, water content, and porosity of the embankment materials. Results showed: It has been found that the breach process can be categorized into a vertical erosion stage and lateral widening stage, with headcut retreat as the main form of erosion form during the vertical erosion stage. The soil water content and porosity not only affected the breach development rate, but also determined the final breach type. The inflow discharge, however, only affected has impact on the breach widening rate. The flow velocities and water level close to the breach were both restricted by the breach height. The relationship between the soil water content, soil porosity, and soil cohesion force was fitted using by the experiment data. A formula expressed by the soil cohesion force and flow parameters for computing the headcut retreat rate was proposed and was proved to be reasonable.
- embankments constructed with silty clay /
- overflow breaching /
- soil water content /
- soil porosity /
- cohesion force /
- headcut erosion

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粉质黏土堤防漫溢溃决试验

doi: 10.14042/j.cnki.32.1309.2015.05.008

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

基金项目: 国家自然科学基金资助项目(11272240;11502174)

作者简介:
魏红艳(1985—),女,山东济南人,博士后,主要从事河流动力学研究.E-mail:weihongyan@whu.edu.cn

通讯作者: 余明辉,E-mail:mhyu@whu.edu.cn

收稿日期: 2014-10-15
刊出日期: 2015-09-25

中图分类号: TV145

关键词:

粉质黏土堤防 /

漫溢溃决 /

含水率 /

孔隙率 /

黏聚力 /

"陡坎"侵蚀

摘要: 为研究粉质黏土堤防漫溢溃决破坏过程及其对水流要素和土体性质的响应规律,以河道流量、筑堤土体含水率和孔隙率为变量,在弯道水槽中开展了9组堤防漫溢溃决概化试验.通过试验发现,粉质黏土堤漫溢溃决溃口发展过程可分为垂向侵蚀和横向扩宽两个阶段,垂向侵蚀阶段以"陡坎"后退为主要形式;筑堤土体含水率与孔隙率不仅影响了溃口垂向侵蚀以及横向扩宽速度,而且决定了溃口最终形态,河道流量主要影响堤防溃口的横向扩宽速度;溃口处流速以及下游水位变化受溃口高度的制约.拟合得到土体黏聚力与土体含水率、孔隙率的相关关系式;通过试验数据提出了由土体黏聚力和水流参数表达的"陡坎"侵蚀后退速度计算公式,证明具有一定合理性.

English Abstract

Experimental study on overflow breaching of embankments constructed with silty clay

State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan 430072, China

Received Date: 2014-10-15
Publish Date: 2015-09-25

Keywords:

embankments constructed with silty clay /
overflow breaching /
soil water content /
soil porosity /
cohesion force /
headcut erosion

Abstract: The purpose of this study is aims to investigate overflow breaching process of embankments constructed with silty clay and their as well as its response to flow and soil characteristics. Nine groups of experiments were conducted on the overflow breaching of cohesive embankments were conducted in a bend flume. Factors considered included inflow discharge, water content, and porosity of the embankment materials. Results showed: It has been found that the breach process can be categorized into a vertical erosion stage and lateral widening stage, with headcut retreat as the main form of erosion form during the vertical erosion stage. The soil water content and porosity not only affected the breach development rate, but also determined the final breach type. The inflow discharge, however, only affected has impact on the breach widening rate. The flow velocities and water level close to the breach were both restricted by the breach height. The relationship between the soil water content, soil porosity, and soil cohesion force was fitted using by the experiment data. A formula expressed by the soil cohesion force and flow parameters for computing the headcut retreat rate was proposed and was proved to be reasonable.

魏红艳, 余明辉, 李义天, 吴松柏. 粉质黏土堤防漫溢溃决试验[J]. 水科学进展, 2015, 26(5): 668-675. doi: 10.14042/j.cnki.32.1309.2015.05.008

引用本文:

魏红艳, 余明辉, 李义天, 吴松柏. 粉质黏土堤防漫溢溃决试验[J]. 水科学进展, 2015, 26(5): 668-675. doi: 10.14042/j.cnki.32.1309.2015.05.008

Citation:

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粉质黏土堤防漫溢溃决试验

doi: 10.14042/j.cnki.32.1309.2015.05.008

作者简介: 魏红艳(1985—),女,山东济南人,博士后,主要从事河流动力学研究.E-mail:weihongyan@whu.edu.cn

通讯作者: 余明辉,E-mail:mhyu@whu.edu.cn

Experimental study on overflow breaching of embankments constructed with silty clay

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出版历程

粉质黏土堤防漫溢溃决试验

doi: 10.14042/j.cnki.32.1309.2015.05.008

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

作者简介: 魏红艳(1985—),女,山东济南人,博士后,主要从事河流动力学研究.E-mail:weihongyan@whu.edu.cn

通讯作者: 余明辉,E-mail:mhyu@whu.edu.cn

English Abstract

Experimental study on overflow breaching of embankments constructed with silty clay

State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan 430072, China

全文HTML

目录

作者简介:
魏红艳(1985—),女,山东济南人,博士后,主要从事河流动力学研究.E-mail:weihongyan@whu.edu.cn

通讯作者:
余明辉,E-mail:mhyu@whu.edu.cn

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

作者简介:
魏红艳(1985—),女,山东济南人,博士后,主要从事河流动力学研究.E-mail:weihongyan@whu.edu.cn