Abstract
Side weirs are utilized to regulate water surface and to control discharge and water elevation in rivers and channels. Here, the discharge coefficient for trapezoidal sharp-crested side weirs (TSCSW) and their affecting parameters are numerically investigated. To simulate the hydraulic and geometric characteristics of TSCSWs, three weir crest lengths of 15 cm, 20 cm and 30 cm with lengths of 20 cm, 30 cm and 40 cm and with two different sidewall slopes are utilized. The results show that for constant P/B (P: weir height, B: main channel width), the depth of flow along the channel and weir decreases as the crest length increases. Also, with increasing P/y1 ratio (P: weir height, y1: upstream flow depth), the discharge coefficient decreases for small crest lengths and increases for large crest lengths. The results show that for constant T/L ratio (T: passing flow width, L: side weir crest length), increasing the length, height and sidewall slope of a side weir will increase the discharge coefficient. It is observed that as the upstream Froude number increases for side weirs with longer crest lengths, the intensity of deviating flow and kinetic energy over the TSCSW will increase. Finally, some relations with high correlation factors are proposed for obtaining discharge coefficients using the dimensionless parameters of P/y1, T/L and Fr1. Based on proposed relations and sensitivity analysis, it is shown that T/L and P/y1 are the most effective parameters for reducing the discharge coefficient reduction.
Highlights
To control and maintain the flow in a channel or river, some discharge control structures such as side weirs are utilized
A side weir is built on the side of a main channel, and free spatially varying flow with decreasing discharge is the dominant regime over this hydraulic structure
The results showed the impact of upstream Froude number and weir height on wide open channels
Summary
To control and maintain the flow in a channel or river, some discharge control structures such as side weirs are utilized. A side weir is built on the side of a main channel, and free spatially varying flow with decreasing discharge is the dominant regime over this hydraulic structure. Decreasing the ultimate (downstream) discharge in the main channel is the result of this action. It means if a flow with discharge (Q1) crosses a side weir, its discharge will be reduced (Q2) because of overspilling (Qw) (see Fig. 1). Inadequate assessment of a discharge coefficient and inappropriate hydraulic design of the structure may result in downstream damage or reduction in flow transmission capacity in the main channel
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