The numerical properties of approximation schemes for a model that sim
ulates water transport in root-soil systems are considered. The model
is derived in detail. It is based on a previously proposed model which
is reformulated completely in terms of the water potential. The syste
m of equations consists of a parabolic partial differential equation t
hat contains a nonlinear capacity term coupled to two linear ordinary
differential equations. A closed form solution is obtained for one of
the latter equations. Finite element and finite difference schemes are
defined to approximate the solution of the coupled system. Some new t
echniques which have wide applicability for analyzing the nonlinear ca
pacity term are used, and optimal order error estimates are derived. A
postprocessed water mass flux computation is also presented and shown
to be superconvergent to the true flux. Computational results which v
erify the theoretical convergence rates are given.