Hydrology Field Methods
Weirs and Flumes
WEIRS
- General Information:
- Weirs are used to measure streamflow with great precision
- The accuracy is degraded by obstructions, leaves, branches, ice, etc.
- Sediment collecting in the weir pool also degrades accuracy
- Weir Components:
- Weir Blade: vertical obstruction in stream over which water must fall.
- Weir Basin: upstream of weir blade used to calm water before falling.
- Cutoff Wall: used to prevent water from moving under or around weir blade.
- Stilling Well: used to calm water level even more than in weir basin
- Staff Gage: used to manually measure water level in weir basin or stilling basin
- Water Level Recorder: used to automatically measure water level
- Weir Equations:
- Q is discharge
- A is cross-sectional area
- v is water velocity
- g is gravitational constant
- h is water level above lowest point of weir blade
- Q = A v
- v2 = 2 g h
- A = function of weir geometry
H-FLUMES
- General Information:
- H flumes are primarily designed for measuring flows that vary widely such as seasonal runoff and overflow from dams.
- The recommended approach channel length is five times the height of the flume.
- The width of the channel should equal the width of the entrance to the flume.
- The flume crest should be set level with the approach channel.
- The approach channel slope should not exceed 2%.
- As the flow exits the flume, it must be able to spill clear or flow in a manner equivalent to spilling clear.
- The flumes may be set in concrete or earth or bolted to companion structures.
- When pouring concrete, brace the flume internally with 2" x 4" blocks cut to size to prevent bulging the walls.
- Remove the bracing when the concrete is set.
- Flume Dimensions:
| Type |
W/H |
L/H |
T/H |
| H |
1.90 |
1.35 |
0.10 |
| HS |
1.05 |
1.50 |
0.05 |
| HL |
3.20 |
1.50 |
0.20 |
- Flume Capacities:
| Type |
Flume Dimensions (feet)1 |
|
Discharge |
| Height |
Width |
Length |
Spout |
|
Min |
|
Max |
| H |
W |
L |
T |
|
(gpm) |
|
(gpm) |
(cfs) |
|
| H |
0.5 |
0.95 |
0.675 |
0.05 |
|
0.180 |
|
149 |
0.33 |
| 0.75 |
1.425 |
1.0125 |
0.075 |
|
0.269 |
|
430 |
0.96 |
| 1 |
1.9 |
1.35 |
0.1 |
|
0.314 |
|
862 |
1.92 |
| 1.5 |
2.85 |
2.025 |
0.15 |
|
0.494 |
|
2,392 |
5.33 |
| 2 |
3.8 |
2.7 |
0.2 |
|
0.628 |
|
4,928 |
11.0 |
| 2.5 |
4.75 |
3.375 |
0.25 |
|
0.808 |
|
8,618 |
19.2 |
| 3 |
5.7 |
4.05 |
0.3 |
|
0.943 |
|
13,645 |
30.4 |
| 4.5 |
8.55 |
6.075 |
0.45 |
|
1.391 |
|
37,704 |
84 |
|
| HS |
0.4 |
0.42 |
0.6 |
0.02 |
|
0.072 |
|
36 |
0.08 |
| 0.6 |
0.63 |
0.9 |
0.03 |
|
0.103 |
|
99 |
0.22 |
|
| HL |
4 |
12.8 |
6 |
0.8 |
|
2.244 |
|
52,517 |
117 |
|
- Flume Calibration Equations
- x = log10(h)
- y = log10(Q)
- h = stage, feet
- Q = discharge, cfs
- 1-foot flume:
- 2-foot flume:
- Flume Rating Curves:
- 1-Foot H-Type Flume (Stage in feet - Discharge in gpm)
| Stage |
0.00 |
0.01 |
0.02 |
0.03 |
0.04 |
0.05 |
0.06 |
0.07 |
0.08 |
0.09 |
| 0.00 |
0.00 |
0.04 |
0.31 |
0.73 |
1.24 |
1.86 |
2.58 |
3.41 |
4.36 |
5.42 |
| 0.10 |
6.60 |
7.91 |
9.34 |
10.9 |
12.6 |
14.4 |
16.4 |
18.5 |
20.7 |
23.1 |
| 0.20 |
25.6 |
28.3 |
31.1 |
34.1 |
37.3 |
40.5 |
44.0 |
47.6 |
51.3 |
55.3 |
| 0.30 |
59.4 |
63.6 |
68.0 |
72.6 |
77.4 |
82.3 |
87.5 |
92.8 |
98.2 |
104 |
| 0.40 |
110 |
116 |
122 |
128 |
135 |
142 |
149 |
156 |
163 |
171 |
| 0.50 |
179 |
187 |
195 |
203 |
212 |
221 |
230 |
239 |
249 |
258 |
| 0.60 |
268 |
278 |
289 |
300 |
310 |
322 |
333 |
345 |
357 |
369 |
| 0.70 |
381 |
394 |
407 |
420 |
433 |
447 |
461 |
475 |
490 |
505 |
| 0.80 |
520 |
535 |
551 |
567 |
583 |
600 |
617 |
634 |
652 |
669 |
| 0.90 |
688 |
706 |
725 |
744 |
764 |
784 |
804 |
825 |
845 |
867 |
| 1.00 |
888 |
910 |
933 |
956 |
979 |
1,002 |
1,026 |
1,051 |
1,075 |
1,101 |
| 1.10 |
1,126 |
1,152 |
1,178 |
1,205 |
1,233 |
1,260 |
1,288 |
1,317 |
1,346 |
1,376 |
| 1.20 |
1,405 |
1,436 |
1,467 |
1,498 |
1,530 |
1,562 |
1,595 |
1,629 |
1,662 |
1,697 |
| 1.30 |
1,732 |
1,767 |
1,803 |
1,840 |
1,877 |
1,914 |
1,953 |
1,991 |
2,031 |
2,071 |
| 1.40 |
2,111 |
2,152 |
2,194 |
2,236 |
2,279 |
2,322 |
2,367 |
2,411 |
2,457 |
2,503 |
| 1.50 |
2,550 |
2,597 |
2,645 |
2,694 |
2,744 |
2,794 |
2,845 |
2,896 |
2,949 |
3,002 |
| 1.60 |
3,056 |
3,110 |
3,166 |
3,222 |
3,279 |
3,336 |
3,395 |
3,454 |
3,514 |
3,575 |
| 1.70 |
3,637 |
3,699 |
3,763 |
3,827 |
3,892 |
3,959 |
4,026 |
4,094 |
4,162 |
4,232 |
| 1.80 |
4,303 |
4,374 |
4,447 |
4,521 |
4,595 |
4,671 |
4,747 |
4,825 |
4,904 |
4,983 |
| 1.90 |
5,064 |
5,146 |
5,229 |
5,313 |
5,398 |
5,484 |
5,571 |
5,660 |
5,749 |
5,840 |
Useful information:
Assignment:
- Working in teams of three, find additional websites documenting various control structures for measuring streamflow.