Design of hydraulic structures with two intermediate filters

被引:13
|
作者
Farouk, MI [1 ]
Smith, IM [1 ]
机构
[1] Univ Manchester, Sch Engn, Dept Civil Engn, Manchester M13 9PL, Lancs, England
关键词
hydraulic structures; conformal mapping; intermediate filters;
D O I
10.1016/S0307-904X(00)00017-2
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The problem of steady-state seepage flow underneath two intermediate filters located anywhere between two end cutoffs of a flat floor of a hydraulic structure on a permeable soil of a finite depth has not been previously solved. Conformal mapping has been applied in this paper to investigate the exact solution. Companion papers (M.I. Farouk, I.M. Smith, Journal of Hydraulic Division, ASCE (2000), submitted for publication; M.I. Farouk, I.M. Smith, Proceedings of the European Geophysical Society on Millennium Conference on Earth, Planetary and Solar Systems Sciences, Nice, France, April 2000) use numerical (finite element) techniques to study a wider range of practical problems involving anisotropy, arbitrary geometries and so on. These solutions are subject to idealization and discretization errors and it was of great value to have the exact results presented herein for comparison purposes. Equations for pore water pressures at key points and hydraulic exit gradient downstream of the hydraulic structure have been derived. Since these equations are not explicit, they are calculated numerically. Results are employed to create design charts in easy-to-use form. These charts indicate that potential heads along the entire floor and the hydraulic exit gradient downstream of the structure are considerably decreased by the provision of two filters even with very small length. Uplift pressures along the door between the two filters are controlled by the location of both filters. Potential heads along the upstream floor are controlled by the upstream filter location and potential heads downstream, and the hydraulic exit gradient downstream by the downstream filter location. Potential heads downstream of the second filter and the hydraulic exit gradient are decreased with decreases in depth of the permeable strata. Pore water pressures upstream of the second filter are decreased with increases in depth of the upstream cut-off. The results clearly indicate that the use of more than one filter in these situations is worth practical consideration. (C) 2000 Elsevier Science Inc. All rights reserved.
引用
收藏
页码:779 / 794
页数:16
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