The present study proposes a 1D model that describes the solids consolidati
on process occurring in a saturated sediment column due to its own weight.
The governing consolidation equation, a second order non-linear transient p
artial differential equation of the parabolic type with the effective stres
s as the dependent variable, is solved by using the finite element and fini
te difference methods. In the spatial discretization of the problem, the Pe
trov-Galerkin method is used to obtain the weak form of the equation. For t
he model's time discretization, two timing step schemes are used for the sa
ke of comparison: the Crank-Nicolson and the backward-difference schemes. T
he contribution of the non-linear terms is determined by employing the stan
dard Newton-Raphson iteration method. The present formulation and numerical
approach are examined by using the results of two consolidation tests, an
attapulgite solids column and a mixture of kaolin-bentonite solids column.
The comparison shows that the consolidation rate and the distribution of th
e volume fraction of solids within the columns can be accurately predicted
by the present model. In addition the results of the non-linear model are c
ompared with those of the corresponding linear consolidation model. It is s
hown that the linear model significantly overpredicts the rate of consolida
tion. Finally, the effect of the initial conditions on the model prediction
s is also examined. (C) 1999 Elsevier Science Inc. All rights reserved.