A mathematical model is developed for the analysis of spatially varied
steady flow in an irrigation canal. The spatially varied steady flow
equations are solved using the finite difference method. The model res
ults are verified with the observed water surface profiles available i
n literature. The effect of canal seepage, canal condition, turnout fl
ows, backwater and drawdown conditions are studied in terms of dischar
ge in the canals, performance of turnouts and spatial variability of f
low. It is observed that even for design roughness and seepage paramet
ers, the actual depth and discharge in the canal is significantly diff
erent from the designed ones.