2013
DOI: 10.1002/nag.2206
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Dynamic response of road pavement resting on a layered poroelastic half‐space to a moving traffic load

Abstract: SUMMARY This paper is dedicated to study the dynamic response of a thin‐plate resting on a layered poroelastic half‐space under a moving traffic load. Based on the dynamic poroelastic theory of Biot, the general solutions of the homogeneous poroelastic foundation are obtained by Fourier translation. By using the transmission and reflection matrices method in the frequency domain, the equivalent stiffness of the layered poroelastic half‐space is presented. Kirchhoff's hypotheses are applied to obtain the vertic… Show more

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Cited by 21 publications
(4 citation statements)
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“…In which E, and v p are the elastic modulus and Poison's ratio of the plate, respectively. For each layer of the poroelastic layered half-space [30],…”
Section: Formulation and Statement Of The Problemmentioning
confidence: 99%
“…In which E, and v p are the elastic modulus and Poison's ratio of the plate, respectively. For each layer of the poroelastic layered half-space [30],…”
Section: Formulation and Statement Of The Problemmentioning
confidence: 99%
“…Therefore, it is more reasonable to regard the subgrade as layered transversely isotropic media than springs (Winkler model) or a homogeneous medium (half-space model). A large number of scholars have studied the dynamic behaviours of layered media subjected to moving loads and provided a series of methods, [29][30][31][32][33][34][35][36][37][38] such as Green's function method, 29 the finite layer method, 30 the spectral element method (SEM), 31 the transmission and reflection matrices (TRM) method, 32 the stiffness matrix method (SMM), [33][34][35] the analytical layer-element method (ALEM), 36 and the extended precise integration method (PIM). 37,38 References [35][36][37][38] also addressed the transverse isotropy of subgrades.…”
Section: Introductionmentioning
confidence: 99%
“…The early works inclined to define the subgrade as the Winkler foundation 34,35 or the viscoelastic elemental model. 32,36 Recently, the poroelastic continuum assumption prevails and was applied on the subgrade from 2D isotropic condition 37,38 to 3D isotropic condition 39 and to 3D transversely isotropic condition. 40 However, there is still a lack of the research that considers the unsaturated characteristics of subgrade induced by rainfall, infiltration, and evaporation, much less the stratification and the transverse isotropy of the subgrade soil, which is exactly one of our interests in this work.…”
Section: Introductionmentioning
confidence: 99%