A method is presented for incorporating the dynamics of a well with finite
wellbore volume into finite difference models of air and water flow in vari
ably saturated porous media. The method is based on the assumption of fluid
gravity segregation with water accumulation at the bottom of the well. The
method accurately accounts for changing water levels in the well and the c
orresponding changes ill ail and water storage in the wellbore. The method
was added to a three-dimensional finite difference model for multiphase Row
and transport and tested against three-dimensional pilot scale experiments
of water injection into initially unsaturated soil. Well water levels and
soil moisture contents monitored during the course of the experiments compa
red well with the model predictions. (C) 2000 Elsevier Science Ltd. All rig
hts reserved.