Abstract
Investigates the effects of two-phase instability on finite element (FE) solutions for porous hypoelastic solids saturated with an insterstitial fluid. Demonstrates that two-phase instability creates definite problems to the FE computations of coupled solid-fluid systems. The eigenvectors of the tangential finite element matrices which are responsible for problems are not artificial, but are the bifurcating modes of physical solutions. The investigation, although limited to the plane strain undrained compression of hypoelastic models, is relevant to the investigation of the two-phase instability of other materials and boundary value problems, and may lead towards an explanation for numerical problems in soil liquefaction analysis.
