1968
DOI: 10.1061/jsfeaq.0001178
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Pore Pressures, Consolidation, and Electrokinetics

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Cited by 205 publications
(29 citation statements)
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“…the pore water pressure, accessibility to atmosphere and soil permeability. At the outset, the negative pore water pressure, as per [6], emerges but is small, and its presence is restricted to the locations near the anode. The emerged pore water pressure needs to be balanced in terms of Eqs.…”
Section: Simulation Resultsmentioning
confidence: 99%
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“…the pore water pressure, accessibility to atmosphere and soil permeability. At the outset, the negative pore water pressure, as per [6], emerges but is small, and its presence is restricted to the locations near the anode. The emerged pore water pressure needs to be balanced in terms of Eqs.…”
Section: Simulation Resultsmentioning
confidence: 99%
“…The farther from the entry point of the anode, the less noticeable the pressure reduction, if the pore water pressure keeps increasing. The fact is that the pore water pressures reach equilibrium, whereas the voltage gradient remains unchanged [6]. The continuous inflow of air is able to occupy, progressively downward, the pore space and reduce the pore air pressure, which explains the gradual flat-outs of pore air pressure isochrones.…”
Section: Simulation Resultsmentioning
confidence: 99%
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“…In 1968, Esrig proposed a one-dimensional electroosmotic consolidation theory under the assumption that the flow caused by the voltage and head differences can be superimposed. is theory is used to explain the phenomena of excess pore water pressure increase and dissipation in the electroosmosis process [15]. In 1976, based on Esrig's onedimensional electroosmotic consolidation theory, Wan proposed a one-dimensional electroosmotic consolidation theory considering external loads.…”
Section: Introductionmentioning
confidence: 99%