Fundamental solutions for a fluid-saturated, transversely isotropic, poroelastic solid

DOI10.1002/NAG.202zbMath1051.74013OpenAlexW2016767733WikidataQ57707983 ScholiaQ57707983MaRDI QIDQ4543704

M. Kurashige, Isao Taguchi

Publication date: 8 August 2002

Published in: International Journal for Numerical and Analytical Methods in Geomechanics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1002/nag.202

zbMATH Keywords

Laplace spaceKupradze's methodtriple Fourier transforms

Mathematics Subject Classification ID

Fluid-solid interactions (including aero- and hydro-elasticity, porosity, etc.) (74F10) Soil and rock mechanics (74L10)

Related Items (8)

Three-dimensional steady-state closed form solution for multilayered fluid-saturated anisotropic finite media due to surface/internal point source ⋮ Plane strain dynamic responses of a multi-layered transversely isotropic saturated half-space ⋮ Fundamental solutions in 3D elastodynamics for the BEM: a review ⋮ Three-dimensional analytical solution for fluid-saturated transversely isotropic poroelastic multilayer formation ⋮ Time-harmonic response of transversely isotropic and layered poroelastic half-spaces under general buried loads ⋮ 3D dynamic responses of a multi-layered transversely isotropic saturated half-space under concentrated forces and pore pressure ⋮ 2D steady-state general solution and fundamental solution for fluid-saturated, orthotropic, poroelastic materials ⋮ Three-dimensional dynamic Green's functions for transversely isotropic saturated half-space subjected to buried loads

Uses Software

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Cites Work

• Point Force Solution for an Infinite Transversely Isotropic Solid

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