Effects of the Erosion and Transport of Fine Particles due to Seepage Flow
Author: Sterpi, Donatella | Size: 0.25 MB | Format: PDF | Quality: Original preprint | Publisher: International Journal of Geomechanics; Vol. 3 Issue 1/2 | Year: Sep2003 | pages: p111-122
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The gradual erosion and transport of fine particles are among the possible consequences to the subsoil of a severe seepage flow, such as the seepage induced by the artificial lowering of the water table by means of pumping wells. The erosion, in turn, could induce local effects, in terms of reductions in the soil volume and variations in the soil mechanical characteristics, that could be non-negligible when working in an urban area. In this paper, some laboratory tests are presented aimed at investigating the erosion of fine particles from soil samples subjected to a controlled seepage flow. The phenomenon of erosion and transport is then modeled by combining, in a single governing equation, the conservation of mass of moving particles with a suitable law of erosion, which is calibrated on the basis of the seepage tests. This equation, coupled with the equation governing the seepage problem, permits one to evaluate the quantity of particles eroded and transported from the soil mass. The effects of the loss of fine material on the stress-strain distribution within the soil mass are estimated by a finite-element analysis. The proposed model is then adopted for the evaluation of the surface settlements induced by the water pumping from a drainage trench.
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Seepage-Induced Erosion in Granular Soil and Consequent Settlements.
Author: Cividini, A., Bonomi, S., Vignati, G., and Gioda, G. | Size: 0.84 MB | Format: PDF | Quality: Original preprint | Publisher: International Journal of Geomechanics; Vol. 9 Issue 4, | Year: Aug 2009 | pages: p187-194
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The erosion of the fine fraction of granular soils due to seepage is a possible cause of the settlements of shallow foundations. Here the problem is tackled with reference to deep pumping wells to be installed in an urban area. First, the results of laboratory tests on reconstituted soil samples are illustrated that provide the quantity of eroded particles during time depending on the imposed hydraulic gradient. Based on the experimental data, an incremental erosion law is proposed that has been implemented in a finite-element code for erosion-transport analysis. After describing the steps of the numerical solution procedure, the results of two- and three-dimensional finite-element calculations are discussed. They provide an estimation of the quantity of eroded material in the vicinity of the pumping wells and of the possible consequent settlements of nearby buildings.
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