2019
DOI: 10.1016/j.compgeo.2019.103145
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Modelling electro-osmosis–surcharge preloading combined consolidation of unsaturated soils

Abstract: After the embargo period via non-commercial hosting platforms such as their institutional repository  via commercial sites with which Elsevier has an agreement In all cases accepted manuscripts should: link to the formal publication via its DOI  bear a CC-BY-NC-ND licensethis is easy to do  if aggregated with other manuscripts, for example in a repository or other site, be

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Cited by 17 publications
(9 citation statements)
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“…Several assumptions related to the mathematical model presented in this research are: The unsaturated soil layer is homogeneous, in which the compression of water or soil particles during consolidation is negligible. The strain occurring in the soil during consolidation is small. Ohm's law and Darcy's law are applicable to the water flow 13,32,33 ; Fick's law is effective for the air flow, 34 and both flows are independent and continuous. The voltage distribution, normalΦfalse(rfalse)$\Phi ( r )$, is assumed to follow the law of charge conservation in the radial direction, which is independent of time 4,35 The coefficient of volume change, electro‐osmotic permeability k e , 18, 36 and permeability coefficient k a* ( k w* ) are constants 24,26,29 …”
Section: Mathematical Modelmentioning
confidence: 99%
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“…Several assumptions related to the mathematical model presented in this research are: The unsaturated soil layer is homogeneous, in which the compression of water or soil particles during consolidation is negligible. The strain occurring in the soil during consolidation is small. Ohm's law and Darcy's law are applicable to the water flow 13,32,33 ; Fick's law is effective for the air flow, 34 and both flows are independent and continuous. The voltage distribution, normalΦfalse(rfalse)$\Phi ( r )$, is assumed to follow the law of charge conservation in the radial direction, which is independent of time 4,35 The coefficient of volume change, electro‐osmotic permeability k e , 18, 36 and permeability coefficient k a* ( k w* ) are constants 24,26,29 …”
Section: Mathematical Modelmentioning
confidence: 99%
“…This makes the two techniques, electro‐osmosis and surcharge preloading, reinforce each other. However, the soil will change from fully saturated 12 to unsaturated as the water collects toward the cathode during electro‐osmotic consolidation 13 . The electro‐osmosis applications have also been investigated in unsaturated soils, for example: enhancing the stability of slopes, 14 reducing the moisture content of “over‐wet soil fill,” 15 and strengthening the ground 16,17 .…”
Section: Introductionmentioning
confidence: 99%
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“…During the electroosmosis drainage process, the soil gradually changed from the initial saturated state to the unsaturated state, so the saturation changed. e electroosmotic consolidation model considering the change of saturation is proposed [13], which makes the calculation results closer to the real situation. On the basis of the above saturation changes, the large deformation theory is introduced to improve the influence of soil properties changes in the process of electroosmotic consolidation by Deng and Zhou [14] and Zhou et al [15][16][17]; the change of soil saturation also attracted the attention of Wang et al [18].…”
Section: Introductionmentioning
confidence: 99%