Laboratory study reveals accurate empirical discharge relationships in rough stone bed channels, indicating the reliability of free overfalls for open channel flow measurement.
In the present investigation, the overfall is employed as a practical tool for measuring discharges in stone bed rectangular channels with overfalls. Fifteen stone bed rectangular channel models with a length of 240 cm and an end drop fall of 20 cm are constructed and examined. These models assess different stone sizes π· π = 0.5 cm, 1.0 cm, and 1.5 cm in horizontal bed channels as well as channels with different bed slopes π π = 0.0033, 0.005, 0.01, and 0.02. The examination of laboratory data for ratios of brink flow depth π π to critical depth π π (EDR) and to normal flow depth π π for different values of π π and π· π showed straight line relationships. The average π e / π π values varied with π π according to a quadratic formula. For the ranges of π π from 0.0033 to 0.02, Froude number πΉ π π from 0.41 to 2.78, and π π / π· π from 0.88 to 15.55, a direct empirical power correlation is presented for estimating the dimensionless discharge π π /( π π 1 / 2 β‘ π π 3 / 2 ) in terms of π e / π π , π e / π· π and π π with determination coefficient R 2 of 0.960 and Mean Percentage Error MPE = Β±0.45%. Another empirical power expression is presented for the dimensionless discharge in stone bed rectangular channels of horizontal beds with R 2 of 0.965. The correlations identified in this study shown good consistency when compared to the findings of many other researchers.
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Noori et al. (2026) studied this question.
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