In case of the Upper Indravati Hydro Electric Project in the Orissa st
ate of India, the topography of the reservoir area governed the locati
on of the water intake, which is situated about; 6.6 km from the upstr
eam edge of the water spread. The total length of the reservoir is 43
km. When the delta arrives at the intake, the water draws a heavy char
ge of sand and coarser sediment that will damage the turbines. seasona
bly accurate prediction of the period required for the sediment delta
to travel down to the intake position therefore achieved crucial impor
tance. Three different methods were used to predict the time rate of d
elta development: (1) a mathematical model; (2) the empirical procedur
e developed by the U.S. Bureau of Reclamation (USER), based on the obs
ervations about the topset slope, foreset slope, and pivot point, made
when the reservoir is in operation; and (3) a procedure based on sedi
ment distribution following the empirical area reduction method. Resul
ts achieved by each of the three methods compared well, indicating tha
t such comparative analysis increases confidence in quantitative predi
ctions and improves the predictive methods for delta profile.