Abstract
Filters managed in zoned dams are designed according to criteria based on the grain size distribution of both filter and eroded soil. However, the constriction size distribution of the filter is the key parameter which governs the filter retention process of flowing eroded particles. To assess the filter efficiency regarding eroded particles, several filters and base soils are tested in a vertical cell with a configuration coupling erosion and filtration processes. For setting the boundary condition of eroded particles at the filter inlet, hole erosion test (HET) was performed on the base soil. The investigation of the evolution of filter behavior shows that the void ratio and the grain shape are of a great influence on filter efficiency. A new approach of filter clogging was proposed by evaluating a damage index which is affected by various parameters such as the ratio D15/d85 and the size of eroded particles. An approach linking the geometrical parameters (damage index) to the hydraulic conductivity leads to an estimation of the filter performance which provides a more quantifiable and realistic criterion. The results indicate that even existing criteria were not met; the tested filters remain efficient as regards to experimental data. An analytical approach based on constrictions size distribution was used and pore reduction was matched with experimental results.
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Acknowledgements
This work was carried out in the framework of the doctorate mobility toward Le Havre Normandy university (France), supported by ERASMUS MUNDUS program “BATTUTA”.
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Appendix: Analytical Model of the Constriction Size Distribution
Appendix: Analytical Model of the Constriction Size Distribution
The most common definition of the pore size is the diameter of the inscribed sphere between tangential particles. Comparisons with the void volumes are made possible by associating a constriction diameter with each pore. The analytical approach aims to compute the CSD from essential information about the PSd of the granular material. It consists of applying a probabilistic schema to an assumed geometrical packing structure within the filter. A further basic concept based on a probabilistic approach is shown in Fig. 9 for two cases, i.e., the loosest and densest filters. The fine particles sequentially flow from one pore to another, passing through the constrictions. Actually, the occurrence of a given constriction size is related to the possibility of particle contact to create such a constriction. This design criterion was based on the probability of the grains’ arrangement in the filter matrix in order to form the largest voids. The size of these voids is dependent on the size and packing geometry of the filter particles.
Silveira et al. (1975) assumed that for the densest geometric configuration, the constriction size Dc3 is made up of three tangent spheres of diameters Di, Dj, Dk. The size of Dc3 can be deduced as follows:
The probability of the occurrence Pc3 by the surface of the constriction size Dc3 is provided by Eq. 9.
where ri, rj and rk are the numbers of times that the diameters Di, Dj and Dk appear in the three particle groups, respectively; ri, rj, rk = 0, 1, 2, 3 and ri + rj + rk = 3; pi, pj and pk are the percentage (probability of occurrence by area) of Di, Dj and Dk, respectively.
It was assumed that in the loosest state the area SV formed by four tangent spheres with respective diameters Di, Dj, Dk and Dm and respective probabilities of occurrence by area pi, pj,pk and pm (Fig. 1a), the constriction size Dc4 can be expressed by Eq. 10.
where SVmax is the maximum area formed among the four tangent particles. The probability of the occurrence by area Pc4 of the constriction size Dc4 is computed from Eq. 11 as follows:
where ri, rj, rk and rm are the numbers of times that the diameters Di, Dj, Dk and Dm appear in the four particles groups, respectively; ri, rj, rk, rm = 0, 1, 2, 3, 4 and ri + rj + rk + rm = 4; pi, pj, pk and pm are the percentage (probability of occurrence by area) of Di, Dj, Dk and Dm respectively.
The constriction area SV can be computed (Fig. 9) from Eq. 12 below:
The two geometrical cases shown in Fig. 9 represent the extreme cases (loosest and densest) of the relative density. Real filters are unlikely to exist either as densest or loosest states, but rather at some intermediate state or relative density. Locke et al. (2001) and Indraratna et al. (2007) proposed that a more realistic pore model should also consider the filter relative density. They suggested that a combination of two cases gives the constriction size dc, which is computed using the relative density Dr as provided by Eq. 13:
where:
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dc: the constriction size at the relative density Dr;
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Pc: the probability of occurrence by area of the constriction size dc.
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Azirou, S., Benamar, A. & Tahakourt, A. Evaluation of Combined Base Soil Erodibility and Granular Filter Efficiency. Geotech Geol Eng 39, 4181–4194 (2021). https://doi.org/10.1007/s10706-021-01747-6
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DOI: https://doi.org/10.1007/s10706-021-01747-6