A moving control volume approach was used to model the advance phase o
f a furrow irrigation system whereas a fixed control volume was used t
o model the nearly stationary phase and the runoff rate. The resulting
finite-difference equations of the kinematic-wave model were lineariz
ed and explicit algebraic expressions were obtained for computation of
advance and runoff rate. The solutions for the advance increment and
the runoff rate were compared with the nonlinear scheme, the zero-iner
tia model, and a set of field data. A close agreement was found betwee
n the models and the field data. Assuming a constant infiltration rate
, a differential equation was derived to estimate the error between th
e kinematic-wave model and the zero-inertia model in predicting the fl
ow cross-sectional area along the field length. The differential equat
ion and two dimensionless terms were used to define the limits for use
of the kinematic-wave model in furrow irrigation.