A multi-region boundary element method (BEM) is presented for the seep
age analysis in deep excavations. In the formulation, soil foundation
is regarded as a multilayered porous medium possessing the zoned inhom
ogeneous hydraulic conductivity. Based on Darcy's law, a two-dimension
al steady state differential equation with transient free surface cond
itions is adopted. With a fundamental solution of the potential proble
m, a generalized multi-region boundary element method is developed. Th
e transient boundary conditions are treated by means of the Galerkin s
cheme of the theta family approximation and are imposed into the bound
ary integral formulation. The essential features of the BEM are that i
t concerns the zoned inhomogeneous hydraulic conductivity of soil medi
a, and that the assembly of each individual region can process in the
same way as in finite element method (FEM) with much less computer mem
ory storage. Several unconfined seepage problems are solved to demonst
rate the performance of the multi-region BEM. Copyright (C) 1996 Elsev
ier Science Ltd.