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A fully coupled finite element analysis of water-table fluctuation and land deformation in partially saturated soils due to surface loading

✍ Scribed by Jun-Mo Kim


Publisher
John Wiley and Sons
Year
2000
Tongue
English
Weight
260 KB
Volume
49
Category
Article
ISSN
0029-5981

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✦ Synopsis


A fully coupled numerical model is presented for the water-table uctuation and land deformation in partially saturated soils due to surface loading. This numerical model is developed based on the poroelastic governing equations for groundwater ow in deforming variably saturated porous media and the Galerkin ÿnite element method. The numerical model is veriÿed and validated against a one-dimensional consolidation problem concerning surface loading on a soil column which has six di erent initial water-table elevations. The numerical model is then applied to a two-dimensional consolidation problem of surface loading on a partially saturated soil at a construction site. Results from the numerical simulations of both problems show that the water table uctuates in the partially saturated soils, and the unsaturated zone above the water table has signiÿcant e ects on the consolidation behaviour of the partially saturated soils under surface loading. Such e ects are caused by the permanent absorption of a portion of the mechanical loading stress and the weak hydromechanical coupling between the solid skeleton deformation ÿeld and the groundwater ow ÿeld in the unsaturated zone due to its partial saturation.