A numerical model has been developed to predict the soil moisture cont
ent over the root zone depth as a function of time and to estimate the
irrigation water requirements in humid basins under various managemen
t options. An implicit finite difference model for transient one dimen
sional flow, backed up by routines for computing various components of
the field hydrological cycle such as evapotranspiration, effective ra
infall, surface runoff, capillary rise, etc. is proposed. The paper de
scribes the assumptions made, theoretical considerations of various su
bmodules; system flowchart, hardware requirements and details of input
-output. Comparison of the model predicted soil moisture profiles with
the field observations is also given along with the results of numeri
cal experiments carried out with the model in the form of sensitivity
analysis for various model parameters. Statistical error analysis is a
lso given to prove reliability of the model for estimation of irrigati
on water requirements.