Abstract
This paper presents results from a series of filtration tests to investigate geometrical and hydromechanical factors controlling the erosion of base particles and their subsequent capture into sand-gravel filters subjected to uniaxial static loading. The analysis revealed that the effectiveness of a filter, apart from its geometry (i.e. particles and constriction sizes), is also controlled by unique combinations of associated hydromechanical factors such as applied hydraulic gradients and the resulting effective stresses. Furthermore, it is observed that the base soil experiences a significant and continuous reduction in effective stress during internal flow (seepage), and the migration of base particles into the filter initiates after localised fluidisation in the base soil (i.e. at very low effective stress levels). Based on limit equilibrium considerations, a novel theoretical approach, different from all other existing methods, is proposed to estimate the critical hydraulic gradient for base soil erosion into granular filter and hence the retention capacity of filters. The current methodology is subsequently validated using experimental data from the published literature and promising results were obtained.
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Abbreviations
- ∆y i, δ z :
-
base particle penetration depth and elemental pore channel (mm)
- ∅′ :
-
drained angle of internal friction
- γ w and μ w :
-
viscosity (Pa.s) and unit weight of water (kN/m3)
- σ′vm, σ′vt, σ′vb :
-
mean, top and bottom vertical effective stresses respectively (kPa)
- Ɲ m :
-
dimensionless mechanical number
- d b, D cm :
-
base particle and mean constriction size of the filter media (mm)
- F d, F h, F b, F w, F f :
-
drag, hydrodynamics, buoyancy, gravity and friction forces (kN)
- F bm, F bmh, F bmr :
-
various factor of safety against base particle migration
- G s and γ s :
-
specific gravity and specific unit weight of soil (kN/m3)
- h f and h f, p :
-
filter thickness, predicted filter thickness (mm)
- h h :
-
upstream hydraulic head in dams (m)
- i cr, 0 :
-
theoretical critical hydraulic gradient for soil piping (Terzaghi 1922)
- i c0, i and i c0, t :
-
hydraulic gradient for base particle erosion under no-load condition for unit step erosion and total erosion, respectively
- i cp :
-
hydraulic gradient for base particle erosion into loaded filters
- i a and i max :
-
average and maximum applied hydraulic gradients, respectively
- i cr :
-
observed critical hydraulic gradient for particle migration into filter
- i ct :
-
theoretical hydraulic gradient for particle migration into loaded filter
- k fc :
-
contact friction factor
- n f :
-
filter porosity
- p w :
-
applied water pressure (kPa)
- q s :
-
effective overburden surcharge pressure (kPa)
- Q f, V f :
-
volumetric flow rate (lit/min), macroscopic fluid velocity (cm/s)
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Acknowledgements
Supports received by the corresponding author in the form of Helan Mountain Research Scholar Program of Ningxia University China, and FDP & IPTA scholarships from University of Engineering and Technology Lahore Pakistan and University of Wollongong Australia, respectively, are acknowledged. Private discussions and consultations of the authors with the Distinguished Professor Buddhima Indraratna, previously at University of Wollongong Australia, are heartily appreciated.
Funding
This study received financial supports from Helan Research Scholar Program of Ningxia University China, Key R&D Program of Ningxia Hui Autonomous Region China (No. 2018BFH03010) and National Natural Science Foundation of China (No. 51768059).
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Responsible Editor: Zeynal Abiddin Erguler
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Zhang, G., Israr, J. Semi empirical hydromechanical model for quantifying effectiveness of loaded granular filters. Arab J Geosci 14, 1488 (2021). https://doi.org/10.1007/s12517-021-07875-w
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DOI: https://doi.org/10.1007/s12517-021-07875-w