A Numerical Analysis of the Leakage Characteristics of an Embankment Dam Slope With Internal Erosion

被引:5
作者
Jia, Yu [1 ]
Ding, Yu [1 ]
Wang, Xuan [1 ,2 ]
Zhang, Jiasheng [1 ,2 ]
Chen, Xiaobin [1 ,2 ]
机构
[1] Cent South Univ, Sch Civil Engn, Changsha, Peoples R China
[2] Cent South Univ, Natl Engn Res Ctr High Speed Railway Construction, Changsha, Peoples R China
基金
中国国家自然科学基金;
关键词
embankment dam slope; internal erosion; two-phase seepage characteristics; deformation characteristics; porosity; permeability; migrated fine particles; SOIL;
D O I
10.3389/feart.2022.866238
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Leakage is a common defect of embankment dam slopes, and is usually accompanied by internal erosion. This study establishes a mathematical two-phase seepage coupling model that explicitly considers the effects of internal erosion. With the help of finite element software COMSOL Multiphysics((R)), we use this model to study the characteristics of fluid seepage, the fraction of leakage volume that is made up of migrated fine particles (migrated fine particles volume fraction), porosity, permeability, and displacement in the leakage process of a three-dimensional embankment dam slope, as well as to study the influence of the water level and leakage outlet size on the aforementioned features. Our results show that water seepage velocity gradually increases with time, especially at the downstream leakage outlet. Therefore, the erosion and migration of fine particles occur primarily at the downstream leakage outlet, resulting in a significant increase in the migrated fine particles volume fraction, porosity, and permeability. In addition, the maximum migrated fine particles volume fraction, the maximum porosity, and the maximum permeability in the slope increase nonlinearly with time. Curves for maximum displacement with a strength reduction factor can be divided into three stages: the early stable stage, the midterm nonlinear growth stage (creeping state), and the later rapid growth stage (instability state). We also find that the rise of the water level promotes the erosion and migration of fine particles on the slope and that the maximum migrated fine particles volume fraction and the maximum porosity increase with the water level. The values of the strength reduction factor for the creeping state decrease as the water level rises. Furthermore, the larger the size of the downstream leakage outlet, the larger the maximum migrated fine particles volume fraction and maximum porosity. However, the relationship between maximum displacement and strength reduction factor is nearly unaffected by the size of the leakage outlet.
引用
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页数:14
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