2015
DOI: 10.1061/(asce)gt.1943-5606.0001270
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Kinematic Bending of Fixed-Head Piles in Nonhomogeneous Soil

Abstract: Kinematic bending of piles in inhomogeneous soil is explored in static and dynamic regime. The system under consideration consists of a fixed-head pile embedded in a continuously inhomogeneous viscoelastic soil layer resting on a rigid base. A generalized parabolic function is employed to describe the variable shear modulus in the inhomogeneous stratum. The problem is treated numerically by means of rigorous elastodynamic finite-element analyses and Beam-on-Dynamic-Winkler-Foundation (BDWF) formulations. A des… Show more

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Cited by 78 publications
(56 citation statements)
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“…e superstructure is simulated by beam, pipe, and mass elements, whereas the raft, piles, and soil are modeled with solid elements (continuum elements). During the simulation of the soil medium, to reduce the effect of boundary conditions on the dynamic response of the system, the lateral model boundary is chosen as approximately 4 times the lateral size of the raft in the x and y directions [32], and the bottom of which is 5 m below the top of the bedrock. e final size of the 3D soil model is set as 322 m × 223 m × 53 m, as shown in Figure 5.…”
Section: Modeling Of the Soil-pile-structurementioning
confidence: 99%
“…e superstructure is simulated by beam, pipe, and mass elements, whereas the raft, piles, and soil are modeled with solid elements (continuum elements). During the simulation of the soil medium, to reduce the effect of boundary conditions on the dynamic response of the system, the lateral model boundary is chosen as approximately 4 times the lateral size of the raft in the x and y directions [32], and the bottom of which is 5 m below the top of the bedrock. e final size of the 3D soil model is set as 322 m × 223 m × 53 m, as shown in Figure 5.…”
Section: Modeling Of the Soil-pile-structurementioning
confidence: 99%
“…Perfect contact (ie, no gap nor slippage) is considered at the soil‐pile interface. The soil layer of thickness H (= L ) is described by a constant Poisson ratio ν s and a depth‐varying shear modulus G s ( z ) ( z being the vertical coordinate) expressed by the following power‐law function Gsfalse(zfalse)=GsH2.05482pt[]b+false(1bfalse)0.1em()zHn and b=()Gs0GsH1false/n, where G s H corresponds to the soil shear modulus at the base of the layer ( z = H ) and n and b are dimensionless inhomogeneity parameters. It is evident that b = 0 corresponds to zero stiffness at the soil surface and b = 1 (or n = 0) to constant stiffness along the thickness of the layer (eg, a heavily over‐consolidated clay).…”
Section: Proposed Analytical Modelmentioning
confidence: 99%
“…Formulas are derived for idealised soil conditions, and the application to inhomogeneous soils generally requires an engineering judgement, based on equivalence criteria in terms of parameters adopted to describe the non‐dimensional problem. (eg, Laora and Rovithis and Karatzia and Mylonakis).…”
Section: Formulas For Estimating Lpm Parametersmentioning
confidence: 99%