scholarly journals Impact of inclined double-cutoff walls under hydraulic structures on uplift forces, seepage discharge and exit hydraulic gradient

Author(s):  
Asaad M. Armanuos ◽  
Abdelazim M. Negm ◽  
Akbar A. Javadi ◽  
John Abraham ◽  
Tamer A. Gado
Water SA ◽  
2019 ◽  
Vol 45 (1 January) ◽  
Author(s):  
Rasool Ghobadian ◽  
Hamed Shekari ◽  
Parisa Koochak

Although the impervious layer under a hydraulic structure is rarely flat, the effect of the impervious layer’s slope, under the hydraulic structure, on seepage characteristics has not been studied to date. Therefore, this study investigated the effect of the downhill and uphill impervious layer’s slope (downhill/uphill foundation slopes) on the uplift pressure, seepage discharge and exit gradient under hydraulic structures. In order to reach this goal, a numerical model has been developed in which the general equation of fluid flow in non-uniform; anisotropic soil is solved by the finite volume method on a structured grid. The model validation was performed using the measured data from experimental tests. The results of the model validation indicated that the model calculates the seepage discharge and uplift pressure with a maximum error of less than 3.79% and 3.25%, respectively. The results also indicated that by increasing the downhill foundation slope (DFS) the uplift force decreases, but the exit gradient and seepage discharge increase. Moreover, by increasing the uphill foundation slope (UFS), the uplift force increases but the exit gradient and seepage discharge decrease. In addition, the results demonstrate that by increasing the length of the cut-off wall the effect of the DFS on decreasing and UFS on increasing the uplift pressure force becomes more severe. However, the effect of the DFS on increasing the seepage discharge and UFS on decreasing the seepage discharge becomes milder as the length of the cut-off wall increases. By increasing the DFS, from zero to −15%, the exit gradient increases 19.75% and 14.4% for 1 m and 6 m cut-off lengths, respectively.


2014 ◽  
Vol 33 (1) ◽  
pp. 95-103 ◽  
Author(s):  
Abdolreza Moharrami ◽  
Gholam Moradi ◽  
Masoud Hajialilue Bonab ◽  
Javad Katebi ◽  
Gholamreza Moharrami

2010 ◽  
Vol 13 (2) ◽  
pp. 23-35
Author(s):  
Duc Van Le

Amplitude of osillation of water table surface and hydraulic gradient under tidal effect, tend to decrease while the seepage flow enters the earthen dam. Therefore, there exists a Dangerous Seepage Triangular Area (DSTA) where hydraulic gradient obtains maximum values. Based on the continuity equation and an assumption on the transmission of seepage oscillation, this DSTA can be specified. Finite Difference Method (FDM), analytical and DSTA methods were programmed using EXCEL software for computation and evaluation of simulated results. The numerical experiments show that the error of total seepage discharge during a tidal cycle between FDM and DSTA methods is less than 1.3%; and the error of maximum hydraulic gradient is not greater than 12%. Besides, the analysis on the earth dam slope stability shows that the most dangerous seepage case occurs when the minimum tidal water level exists as well as maximum hydraulic gradient of out-seepage flow is reached. This is one of the important reasons that explain plenty of tidal river bank erosions in Mekong River Delta.


1979 ◽  
Vol 16 (2) ◽  
pp. 351-362 ◽  
Author(s):  
O. Dascal

The hydraulic efficiency of a double-wall cutoff built through 126 m (420 ft) of pervious alluvial deposit filling a V-shaped canyon and under a 107 m (350 ft) high earthfill dam is discussed. The cutoff walls are made up of cast-in-place concrete interlocking piles and panels and are intended primarily to minimize the danger of piping, by controlling the pore pressures in the downstream zone of the dam. The behaviour of the cutoff, monitored by a comprehensive instrumentation program, indicated after [Formula: see text] years a relatively high hydraulic efficiency (over 92%). During this period the cutoff has exhibited a very slight decrease in its efficiency (less than 1%), probably due to leaching of the grout at the rock-wall contact in the grout curtain, and probably also due to some removal of the bentonite from between the piles and panels. The analysis of the efficiency of each wall considered individually (using Casagrande's latest recommendation) indicates a lower efficiency for the upstream wall as compared to that of the downstream wall, probably because of the migration of bentonite particles downstream under the hydraulic gradient. The double-wall cutoff exhibits an efficiency about 18–30% higher than that for a similar single-wall cutoff.


Water ◽  
2018 ◽  
Vol 10 (12) ◽  
pp. 1757
Author(s):  
V. Kirca ◽  
R. Kilci

Coastal and hydraulic structures, such as revetments, embankments and levees—as well as their underlying soil—may experience piping when exposed to outward pressure gradients. The aim of the present study is twofold: (1) to derive the force-balance equation for soils with a sloping surface exposed to a steady hydraulic gradient (relevant to hydraulic structures) and to seek a criterion for piping, including the friction terms; (2) to study the case of unsteady hydraulic gradient forcing (relevant to coastal structures) by means of a series of experiments. The derived force-balance equation is compared with the available experimental and numerical model data from the literature and extended to soils protected by a filter/armour layer or rip rap. The experiments conducted to study the mechanism of piping under unsteady hydraulic gradients involved two types of loadings; sudden and oscillatory. The results show that although the mechanism of steady and unsteady piping has some similar aspects, the soil is generally more prone to piping in the unsteady hydraulic loading compared to the steady case, attributed to the inertia terms. The hydraulic conductivity of the soil becomes more distinctive for the unsteady piping case. Finally, remarks are made about practical applications.


2006 ◽  
Vol 14 (2) ◽  
pp. 639-644
Author(s):  
G.M. Thomas ◽  
J.F. Morgan ◽  
M.J. Gefell ◽  
J. Shi
Keyword(s):  

2020 ◽  
pp. 109-116
Author(s):  
N.P. KARPENKO ◽  
◽  
M.A. SHIRYAEVA

The purpose of the work is to consider methods for calculating the forecast of groundwater backwater in the zone of influence of hydraulic structures. The analysis of analytical dependences of calculation of the forecast of groundwater backwater for various calculation schemes is carried out. For a homogeneous scheme of the geofiltration structure, a numerical model is proposed and a computational program for calculating the groundwater backwater is developed. It allows calculating the groundwater backwater from the channel at any time in the discrete mode. To simplify the solution of the problem of calculating the groundwater backwater, a computer program was created in the programming language Phyton Version 8.3 which quickly solves this hydrogeological problem. A possible range of geofiltration parameters is proposed for calculating the groundwater backwater near main channels. The adaptation and implementation of the software model was carried out for a specific object – the Bolshoy Stavropol channel-5, for which forecast calculations were made. The results of predictive calculations of groundwater backwater are the basis for the assessment of areas of possible flooding – the territory within which the level of ground water increases as a result of their backup by a hydraulic structure.


10.29007/2k64 ◽  
2018 ◽  
Author(s):  
Pat Prodanovic ◽  
Cedric Goeury ◽  
Fabrice Zaoui ◽  
Riadh Ata ◽  
Jacques Fontaine ◽  
...  

This paper presents a practical methodology developed for shape optimization studies of hydraulic structures using environmental numerical modelling codes. The methodology starts by defining the optimization problem and identifying relevant problem constraints. Design variables in shape optimization studies are configuration of structures (such as length or spacing of groins, orientation and layout of breakwaters, etc.) whose optimal orientation is not known a priori. The optimization problem is solved numerically by coupling an optimization algorithm to a numerical model. The coupled system is able to define, test and evaluate a multitude of new shapes, which are internally generated and then simulated using a numerical model. The developed methodology is tested using an example of an optimum design of a fish passage, where the design variables are the length and the position of slots. In this paper an objective function is defined where a target is specified and the numerical optimizer is asked to retrieve the target solution. Such a definition of the objective function is used to validate the developed tool chain. This work uses the numerical model TELEMAC- 2Dfrom the TELEMAC-MASCARET suite of numerical solvers for the solution of shallow water equations, coupled with various numerical optimization algorithms available in the literature.


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