Here, k2 is the correction for the effect of curvature of flow over the weir crest (Fig. 5.15), and L is the length of the weir along the flow direction. C is obtained from Fig. 5.16 which is based on the following equation:
H
=
3 [C2 / 3 − (2/3)]1/ 2
(5.17)
H + W
(b/b ) C
1
For suppressed broad-crested weirs b = b1. Here, b1 is the width of the channel. Thus, one uses the curve for b/b1 = 1.0 in Fig. 5.16 to find C. k1 is obtained from Fig. 5.13. For broad-crested weirs with sloping upstream and downstream faces one can use Eq. (5.16) with different functional relations for k1 and k2 shown in Figs. 5.17 and 5.18, respectively.
1.2
1.1
1.0
k2 0.9
0.8
0.7
0.02
0.1
1.0
2.0
H/L
Fig. 5.15 Variation of k2 with H/L for vertical-faced weir with rounded corner
For a submerged broad-crested weir, the discharge equation is written as (7, 8)
Q = Cb g H 3 /2 k1 k2 k4
(5.18)
Assuming that C, k1, and k2 remain unaffected due to submergence, relationship for k4 is as shown in Fig. 5.19. It should be noted that the discharge on broad- crested weirs remains unaffected up to submergence (H2/H1) as high as 75 per cent. Figure 5.20 compares the discharge characteristics of submerged broad-crested weirs with those of sharp-crested weirs.
198 IRRIGATION AND WATER RESOURCES ENGINEERING
Weirs of widths smaller than that of the approach channel are termed contracted weirs. The above-mentioned relationships, Eq. (5.15) for sharp-crested rectangular weirs and Eq. (5.16) for broad-crested weirs, require some modifications for contracted weirs. Ranga Raju and Asawa (6) suggested the following equation for the actual discharge over a contracted sharp-crested rectangular weir:
Q = k k
2
[0.611 + C (H/W)] b 2gH3 /2
(5.19)
1
3
3
1
in which k3 is the correction factor for lateral contraction and C1 is a function of b/b1 as shown in Fig. 5.21. k3 should logically be a function of H/b. On analysing the experimental data, the average value of k3 was found to be 0.95 for H/b ranging from 0.1 to 1.0 (6).
Similarly, the actual discharge over a contracted broad-crested weir may be written as
(6)
Q = k
k k Cb g H 3 /2
(5.20)
1
2
3
in which k3 is a correction factor for contraction effects and the value of C for various values of b/b1, as obtained by solving Eq. (5.17), can be read from Fig. 5.16. Logically, k3should be afunction of H/b. Based on the analysis of experimental data, the value of k3can be taken as unity for H/b ranging from 0.1 to 1.0 (6).
0.68
0.66
0.64
Suppressed weir
0.62
C
0.60
0.58
0.56
0.54
0.52
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
H/(H + W)
0
.
=
1
b/b
1
0
.
9
8
.
0
0.7
.6 0
.5 0
0.4 0.2
0.8 0.9 1.0
Fig. 5.16 Variation of C with H/(H + W) and b/b1 for broad-crested weirs (6)
CANAL IRRIGATION 199
1.4
Symbol
L
W
Su
Sd
cm
cm
25
15
1.0
3
L
10
15
0.5
3
W
Su
SD
1.3
10
15
1.0
3
1
1
10
15
1.0
3
25
10
0.5
3
1.2
25
10
1.0
3
k1
1.1
1.0
0.9
2
4
6
8
2
2
4
6
8
3
2
4
10
10
.2
.6
Re
W1
Fig. 5.17 Variation of k1 for broad-crested weirs with sloping faces (7)