Time Domain Traction and Flux Fundamental Solutions for 3D Saturated Poroelastic Media with Incompressible Constituents

AbstractOne of the key factors in the time domain boundary element method (BEM) for dynamic poroelasticity is an applicable fundamental solution of the governing differential equations. With the completion of the fundamental solutions, this paper is dedicated to the simple time domain traction and f...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:International journal of geomechanics 2013-10, Vol.13 (5), p.678-685
Hauptverfasser: Sharahi, Morteza Jiryaei, Kamalian, Mohsen
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:AbstractOne of the key factors in the time domain boundary element method (BEM) for dynamic poroelasticity is an applicable fundamental solution of the governing differential equations. With the completion of the fundamental solutions, this paper is dedicated to the simple time domain traction and fluid flux fundamental solutions for the three-dimensional (3D) u-p formulation of saturated porous media where fluid and soil particles are assumed incompressible in comparison with the compressibility of the soil structure. First, the explicit Laplace transform fundamental solutions are obtained from the governing differential equations which were written in terms of solid displacements and fluid pressure. Subsequently, the closed form time domain traction and fluid volumetric flux fundamental solutions are derived by analytical inversion of the Laplace transform solutions. Finally, a set of numerical results are presented which demonstrate the accuracy and some salient features of the derived analytical transient traction and fluid flux fundamental solutions.
ISSN:1532-3641
1943-5622
DOI:10.1061/(ASCE)GM.1943-5622.0000248