EFFECT OF PORE FLUID COMPRESSIBILITY ON LOCALIZATION IN ELASTIC-PLASTIC POROUS SOLIDS UNDER UNDRAINED CONDITIONS

Citation
K. Runesson et al., EFFECT OF PORE FLUID COMPRESSIBILITY ON LOCALIZATION IN ELASTIC-PLASTIC POROUS SOLIDS UNDER UNDRAINED CONDITIONS, International journal of solids and structures, 33(10), 1996, pp. 1501-1518
Citations number
16
Categorie Soggetti
Mechanics
ISSN journal
00207683
Volume
33
Issue
10
Year of publication
1996
Pages
1501 - 1518
Database
ISI
SICI code
0020-7683(1996)33:10<1501:EOPFCO>2.0.ZU;2-N
Abstract
Conditions are derived for band-shaped localization, i.e. for the exis tence of discontinuous bifurcations of the incremental strain field, i n elastic-plastic porous materials, under undrained conditions. It is assumed that the pores are filled with nearly incompressible liquid/ga s mixture, and the significant parameter is the bulk modulus of the po re fluid. The extreme situation is complete incompressibility, which w ould correspond to full saturation of a liquid with an infinite bulk m odulus. In this case the surprising result is obtained that, for plane strain and cylindrical stress states, the critical bifurcation direct ion is always 45 degrees to a principal stress axis regardless of the adopted yield criterion. It is also shown in the paper that incompress ibility usually (although not generally) has a stabilizing effect. For example, when the how rule is associated, the critical hardening modu lus is always non-positive. A discontinuity in strain rate is always a ccompanied by discontinuous pore pressure rate across the characterist ic surface, and the magnitude of this jump is related to the strength of the displacement jump. One restrictive assumption used in the analy sis is that the gradient of the yield criterion and the flow direction are coaxial. A numerical evaluation of the critical bifurcation direc tion and the corresponding hardening modulus is given for the Mohr-Cou lomb criterion, which is representative for the behavior of cohesionle ss granular materials such as soil.