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Analysis on Nonlinear Flowing Consolidation of Clay
It exist non-linear flow in soft clay, which is caused by the shear flow situation of bounded-water. In this case, permeability coefficient is a nonlinear function of hydraulic gradient. With the discharge of pore water, the effective stress is increasing, and part of weakly bound-water begins flow, while the porosity and permeability are became lower. By taking into the characteristics of the pore water, it is established a model, which is explained the nonlinear flow of clay, and shown that, with the increasing of and , the consolidation time is obviously increased
Analysis on Nonlinear Flowing Consolidation of Clay
It exist non-linear flow in soft clay, which is caused by the shear flow situation of bounded-water. In this case, permeability coefficient is a nonlinear function of hydraulic gradient. With the discharge of pore water, the effective stress is increasing, and part of weakly bound-water begins flow, while the porosity and permeability are became lower. By taking into the characteristics of the pore water, it is established a model, which is explained the nonlinear flow of clay, and shown that, with the increasing of and , the consolidation time is obviously increased
Analysis on Nonlinear Flowing Consolidation of Clay
Advanced Materials Research ; 168-170 ; 175-180
06.12.2010
6 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch
Analysis on Nonlinear Flowing Consolidation of Clay
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