The solution to Blot's coupled consolidation theory is usually addressed by
the finite element (FE) method thus obtaining a system of first-order diff
erential equations which is integrated by the use of an appropriate time ma
rching scheme. For small values of the time step the resulting linear syste
m may be severely ill-conditioned and hence the solution can prove quite di
fficult to achieve. Under such conditions efficient and robust projection s
olvers based on Krylov's subspaces which are usually recommended for non-sy
mmetric large size problems can exhibit a very slow convergence rate or eve
n fail. The present paper investigates the correlation between the ill-cond
itioning of FE poroelasticity equations and the time integration step Delta
t. An empirical relation is provided for a lower bound Deltat(crit) of Delt
at below which ill-conditioning may suddenly occur. The critical time step
is larger for soft and low permeable porous media discretized on coarser gr
ids. A limiting value for the rock stiffness is found such that for stiffer
systems there is no ill-conditioning irrespective of Deltat however small,
as is also shown by several numerical examples. Finally, the definition of
a different Deltat(crit) as suggested by other authors is reviewed and dis
cussed. (C) 2001 Elsevier Science Ltd. All rights reserved.