A simplified method to estimate saturated and unsaturated seepage through dikes under steady-state conditions

被引:34
作者
Chapuis, RP [1 ]
Aubertin, M [1 ]
机构
[1] Ecole Polytech, Dept Civil Geol & Min Engn, Montreal, PQ H3C 3A7, Canada
关键词
dams; dikes; seepage; saturated soil; unsaturated soil; numerical modeling;
D O I
10.1139/cgj-38-6-1321
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The seepage rate through homogeneous or zoned dikes includes saturated and unsaturated flow. The latter is often neglected but should be considered to obtain the positions of the water table and the seepage face that may develop either on the downstream slope of a homogeneous dike or within the filter layer behind the core of a zoned dike. Different dikes with heights of 5, 10, 20, and 50 m have been analyzed numerically with a two-dimensional finite element code. The cases investigated include the most frequent types of small dikes designed to retain municipal or industrial wastewater. Solutions are proposed to solve numerically two difficulties related to the representation of saturated and unsaturated physical flow conditions. One difficulty is treating a downstream seepage face. The other is treating the passage of water from the core into a draining layer. The paper presents simple expressions to predict the total (saturated and unsaturated) seepage flow rate through a dike and discusses precautions to be taken.
引用
收藏
页码:1321 / 1328
页数:8
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