This paper presents an analytical investigation on the excess pore-fluid pressure in a finite seabed layer by taking into account the influence of a compressible pore fluid. The seabed layer is modeled as a poroelastic layer saturated with a compressible pore fluid and resting on a rough, rigid impermeable base. The surface of the poroelastic seabed layer is either completely pervious or completely impervious, and subjected to a normal surface traction induced by offshore structures. The paper presents analytical and numerical results to illustrate the time-dependent behaviour of excess pore pressure in the poroelastic seabed. The results demonstrate that the presence of a compressible pore fluid reduces the generation of excess pore pressu...
An analytical solution of the fully coupled system of equations governing the plane strain deformati...
The evaluation of the wave-induced seabed response (including pore pressures and effective stresses)...
ABSTRACT: Fluid pressures in argillaceous sediments depend on, inter alia, mechanical stresses, temp...
This paper presents an analytical investigation on the excess pore-fluid pressure in a finite seabed...
This paper examines stresses and excess pore fluid pressure that are induced in a saturated poroelas...
A suction anchor is an appealing anchoring solution for floating production. However, the possible e...
While currently available methods of dynamic soil-foundation interaction idealize the soil as a cont...
Both transient and residual pore pressure responses are induced as ocean waves propagate over a silt...
Abstract: In this paper, a three-dimensional poro-elastoplastic model for the short-crested wave-ind...
Thermal expansion of seabed pipelinesmay generate excess pore pressure in the surrounding soil. This...
In many sedimentary basins of the world the minimum hori- zontal stress, Sh, is greater in overpress...
Periodic pressure measurements made during the depletion of oil fields and virgin pressure measureme...
While ocean waves propagating over a porous seabed, the amplitude of excess pore pressure would atte...
Instantaneous liquefaction can be induced by the upward seepage force generated in a sandy seabed un...
The evaluation of the wave-induced excess pore pressure around a buried pipeline is particularly imp...
An analytical solution of the fully coupled system of equations governing the plane strain deformati...
The evaluation of the wave-induced seabed response (including pore pressures and effective stresses)...
ABSTRACT: Fluid pressures in argillaceous sediments depend on, inter alia, mechanical stresses, temp...
This paper presents an analytical investigation on the excess pore-fluid pressure in a finite seabed...
This paper examines stresses and excess pore fluid pressure that are induced in a saturated poroelas...
A suction anchor is an appealing anchoring solution for floating production. However, the possible e...
While currently available methods of dynamic soil-foundation interaction idealize the soil as a cont...
Both transient and residual pore pressure responses are induced as ocean waves propagate over a silt...
Abstract: In this paper, a three-dimensional poro-elastoplastic model for the short-crested wave-ind...
Thermal expansion of seabed pipelinesmay generate excess pore pressure in the surrounding soil. This...
In many sedimentary basins of the world the minimum hori- zontal stress, Sh, is greater in overpress...
Periodic pressure measurements made during the depletion of oil fields and virgin pressure measureme...
While ocean waves propagating over a porous seabed, the amplitude of excess pore pressure would atte...
Instantaneous liquefaction can be induced by the upward seepage force generated in a sandy seabed un...
The evaluation of the wave-induced excess pore pressure around a buried pipeline is particularly imp...
An analytical solution of the fully coupled system of equations governing the plane strain deformati...
The evaluation of the wave-induced seabed response (including pore pressures and effective stresses)...
ABSTRACT: Fluid pressures in argillaceous sediments depend on, inter alia, mechanical stresses, temp...