water-resources investigations report 87-4226 · the spillway (figs. 2, 5) when the headwater pool...
TRANSCRIPT
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DISCHARGE RATINGS FOR CONTROL STRUCTURES AT
McHENRY DAM ON THE POX RIVER, ILLINOIS
By Gregory G. Fisk
U.S. GEOLOGICAL SURVEY
Water-Resources Investigations Report 87-4226
Prepared in cooperation with
ILLINOIS DEPARTMENT OF TRANSPORTATION,
DIVISION OF WATER RESOURCES
Urbana, Illinois
1988
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DEPARTMENT OF THE INTERIOR
DONALD PAUL HODEL, Secretary
U.S. GEOLOGICAL SURVEY
Dallas L. Peck, Director
For additional information write to:
District ChiefU.S. Geological Survey4th Floor102 E. Main StreetUrbana, IL 61801
Copies of this report can be purchased from:
U.S. Geological SurveyBooks and Open-file Reports SectionFederal center, Bldg. 810Box 25425Denver, CO 80225
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CONTENTS
Page
Abstract................................................................ 1Introduction............................................................ 1
Background......................................................... 1Purpose and scope.................................................. 3Approach........................................................... 3Acknowledgments.................................................... 3
Description of McHenry Dam.............................................. 3Discharge ratings....................................................... 5
Spillway........................................................... 9Sluice gates....................................................... 12Evaluation of ratings.............................................. 19Computation of discharge........................................... 20
Summary and conclusions................................................. 23References cited........................................................ 24
ILLUSTRATIONS
Figure 1. Map showing location of McHenry Dam and gaging stationson the Fox River.......................................... 2
2. Diagram showing location of control structures atMcHenry Dam............................................... 4
3. Photograph showing downstream side of sluice gates.......... 6
4. Diagram showing cross section of sluice gate................ 7
5. Photographs showing downstream side of spillway andfish ladder............................................... 8
6-10. Graphs showing:
6. Relation between discharge coefficient for free weir flow and headwater depth for spillway (fish ladder included)............................... 9
7. Relation between discharge coefficient for freeweir flow and headwater depth for sluice gates....... 14
8. Relation between discharge coefficient for freeorifice flow and sluice-gate opening................. 16
9. Relation between discharge coefficient for submergedorifice flow and submergence ratio for sluice gates.. 17
10. Daily discharges for Fox River at McHenry Dam and Fox River at Algonquin for selected days during the data-collection period........................... 21
111
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TABLES
Page
Table 1. Equations of flow............................................. 52. Characteristics of discharge at McHenry Dam................... 10
3. Discharge rating table for free weir flow over spillway(fish ladder included)...................................... 13
4. Discharge rating table for free weir flow under fivesluice gates................................................ 15
5. Discharge rating table for free orifice flow under fivesluice gates set to same gate opening....................... 18
6. Summary of hydraulic conditions and discharge equations for different flow regimes at McHenry Dam control structures.................................................. 19
CONVERSION FACTORS AND ABBREVIATIONS
For the convenience of readers who prefer to use metric (International System) units, rather than the inch-pound terms used in this report, the following conversion factors may be used:
Multiply By To obtain
foot (ft) 0.3048 meter (m)
mile (mi) 1.609 kilometer (km)
square foot (ft2 ) 0.09294 square meter (m2 )9 9square mile (mi^) 2.590 square kilometer (km'2 )
O -3
cubic foot per second (ft°/s) 0.02832 cubic meter per second (irr/s)
Sea level: In this report "sea level" refers to the National Geodetic Vertical Datum of 1929 (NGVD of 1929) a geodetic datum derived from a general adjustment of the first-order level nets of both the United States and Canada, formerly called "Mean Sea Level of 1929."
iv
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SYMBOLS AND UNITS
Symbol Definition Unit
B Sluice-gate width, or spillway and fish ladder length ft
C Coefficient of discharge for free orifice flow under sluice gates
Cs Coefficient of discharge for submerged orifice flow under sluice gates
Cw Coefficient of discharge for free weir flow
Cws Coefficient of discharge for submerged weir flow
g Acceleration due to gravity (32.2) ft/s
h-j Headwater depth referenced to sluice-gate sill or spillway ft crest
113 Tailwater depth referenced to sluice-gate sill or spillway ft crest
hq Sluice-gate opening ft
Q Discharge ft3/s
v
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DISCHARGE RATINGS FOR CONTROL STRUCTURES AT McHENRY DAM
ON THE FOX RIVER, ILLINOIS
by Gregory G. Fisk
ABSTRACT
Twenty-three measurements of discharge were used to determine discharge ratings for the five adjustable sluice gates, spillway, and fish ladder at McHenry Dam on the Fox River in Illinois. Discharge ratings were determined for free weir, free orifice, and submerged orifice flow regimes.
Hydraulic conditions that identify flow regimes at McHenry Dam are defined by ratios between headwater depth (h 1 ), tailwater depth (h3 ), and gate opening (h_). Flow under the sluice gates is identified as weir flow when the ratio of gate opening to headwater depth is greater than 0.73, and as orifice flow when ha/h« is less than 0.73. Free orifice flow occurs when the ratio of tailwater depth to gate opening is less than 1.3, and submerged orifice flow occurs when h3/h is greater than 1.3. Flow under the sluice gates is identi fied as free weir flow when the ratio of tailwater depth to headwater depth is less than 0.75, and as submerged weir flow when h3/h-| is greater than 0.75. Flow over the spillway is identified as free weir flow when the ratio of tail- water depth to headwater depth is less than 0.60, and as submerged weir flow when h3/h 1 is greater than 0.60.
Discharge coefficients to be used in equations to compute discharge for various hydraulic conditions were determined. Four discharge measurements, ranging from 169 to 2,990 cubic feet per second, were used to define discharge coefficients that varied from 2.61 to 3.14 for free weir flow over the spillway,
Nineteen discharge measurements, ranging from 180 to 4,050 cubic feet per second, were used to define discharge coefficients for free weir, free orifice, and submerged orifice flow under the sluice gates. The average value of the discharge coefficient for free weir flow under the sluice gates is 3.17. Discharge coefficients for free orifice flow varied from 0.48 to 0.66 and the discharge coefficients for submerged orifice flow from the two measurements were 0.59 and 0.67.
INTRODUCTION
Background
McHenry Dam is located on the Fox River in northeastern Illinois, 42 miles northwest of Chicago and 2.5 miles south of McHenry (fig. 1). The Illinois Department of Transportation, Division of Water Resources (DWR) operates the
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88°l 5' 88°l O 1
42°25' -
42°I5' -
CHAIN O'lLAKES STATE/PARK
234 KILOMETERS
U.S. Geological Surveystream-flow gaging station
U.S. Geological Survey lake station, stage only
Figure 1. Location of McHenry Dam and gaging stations on the Fox River.
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dam for recreational and flood-control purposes. Reliable computation of discharge at McHenry Dam is needed in order to effectively operate the dam for those purposes. The U.S. Geological Survey (Survey), in cooperation with DWR, began a study in March 1985 to develop a method for computing discharge at McHenry Dam. The method was to include discharge ratings for the various flow regimes related to hydraulic conditions involving headwater depth, tailwater depth, and sluice-gate openings.
Purpose and Scope
The purpose of this report is to describe the results of a study to develop discharge ratings for the control structures at McHenry Dam. The methods are limited in scope to three types of flow free weir, free orifice, and submerged orifice that occurred during the study period.
Approach
Discharge ratings at McHenry Dam are affected by headwater and tailwater stages, and gate openings. Because it was not feasible to make measurements under all hydraulic conditions, measurements were made to determine discharge coefficients in equations that relate discharge to headwater depth, tailwater depth, and gate openings. Discharge coefficients were then related to depths and gate openings applicable to each measurement.
Standard Survey techniques (Buchanan and Somers, 1969) were used to make discharge measurements. Current-meter measurements of low flows were made by wading across the spillway crest and wading 50 feet (ft) downstream from the sluice gates. Medium and high flows were measured from a boat about 100 ft upstream from the gates and 150 ft upstream from the spillway (fig. 2).
Acknowledgments
The Illinois Department of Transportation and Bill Rice, in particular, provided historical data used in this report. McHenry Dam Lockmaster, Frank Novak, Jr., was very helpful in providing various gate openings to provide the desired flow regime. Their cooperation on this study is gratefully acknowledged.
DESCRIPTION OF McHENRY DAM
McHenry Dam is located at river mile 97.8 on the Fox River in northeastern Illinois (fig. 1). The drainage area at the dam is 1,250 square miles (mi^). The 8,900-acre reservoir created by the dam is part of the Fox Chain O 1 Lakes and is used primarily for recreation and flood control. The control struc tures at the dam consist of five sluice gates, a spillway, a fish ladder, and a navigation lock.
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Wad
ing
mea
sure
men
t se
ctio
n
D.W
.R.
tail
wa
ter
ga
ge
Fo
x
SL
UIC
E
GA
TE
S
. lad
der
SP
ILL
WA
Y
north
U.S.
G.Sl
gag
e
Bo
at
mea
sure
men
t s
ec
tio
n
/?
iv
e r N
OT
T
O
SC
AL
E
Figu
re 2. Location of control
stru
ctur
es at
McHenry
Dam.
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The sluice gates (figs. 2, 3) are operated to regulate discharge when the headwater-pool stage is below the crest of the spillway. Each sluice gate is 13.75 ft wide and can be raised to a maximum opening of 9.0 ft to regulate flow under the gate; flow over the top of the gates does not occur. The sill on which a closed gate rests (fig. 4) is at an elevation of 731.15 ft above sea level. All gates are set to similar openings, ranging from 0 to 9 ft, to maintain the headwater-pool stage at 4.00 ft during the recreational season, April through October. Headwater-pool stages are referenced to a datum of 733.00 ft above sea level. In November of each year, the sluice gates are gradually adjusted to lower the headwater pool to a stage between 1.5 and 2.0 ft to provide storage for flood control during spring runoff. The tailwater- pool stage, which is referenced to a datum of 730.15 ft above sea level, can be partially regulated during floods by adjustment of the sluice-gate openings.
The spillway is a broad-crested, concrete and stone-faced weir that is arced upstream and measures 282 ft along the arc. Water begins to flow over the spillway (figs. 2, 5) when the headwater pool rises above the weir-crest elevation of 736.68 ft. A 6-foot-long fish ladder, also having a crest eleva tion of 736.68 ft, is adjacent to and in the same approach section as the spillway (figs. 2, 5). The discharge rating for flow over the spillway includes flow over the 6-foot-long fish ladder.
DISCHARGE RATINGS
The four flow regimes that may occur at dams are discussed by Collins (1977). The flow regimes and hydraulic conditions defining each regime, along with equations for computing discharge, are listed in table 1. Collins states that the hydraulic conditions (table 1) are general criteria for defining the flow regimes.
Table 1. Equations of flow
[Equations from Collins, 1977. Q, Discharge, in cubic feet per second; C, Free orifice discharge coefficient; Cs , Submerged orifice discharge coefficient; C^, Free weir discharge coefficient; C^g, Submerged weir
discharge coefficient; hg , Gate opening; h 1 , Headwater depth; ho, Tailwater depth; B, Sluice gate width or spillway length;
g, Acceleration due to gravity; Ah equals h-j-h^]
Flow regime
Free orifice
Submerged orifice
Free weir
Submerged weir
Hydraulic condition
h <0.67h1 and h3 <h
hg<0.67h 1 and h3 >h
h^>0.67hi and h-s/h 1 <0.6 g_ i -j iha>0.67h<| and h3/h 12.0.6j
Equations
Q=C[hgB(2gh 1 )°- 5 ]
Q=Cs [h3B(2gAh)°' 5 ]
Q=Cw [Bh 1 1-5 ]
Q=CWCWS [fih^-5]
Equation number
(1)
(2)
(3)
(4)
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~f
Figure 3. Downstream side of sluice gates
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Concrete walkway Motor.for adjusting gates
Concrete pier
Datum 733.00 ft
h1 Headwater depth
hg Gate opening
h3 Tailwater depth
Sluice gateHeadwater pool stage
Tailwater pool stage
Concrete sill Elev. 731.15 ft
NOT TO SCALE
_ Datum 730. I 5 ft
Figure 4. Cross section of sluice gate.
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Figure 5. Downstream side of spillway and fish ladder.
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Spillway
Discharge measurements 5, 13, 15, and 20 (table 2) were made during free weir flow over the spillway. Free weir flow over a spillway, as defined by Collins (table 1), occurs when the ratio of tailwater depth (h3 ) to headwater depth (h-j) is less than 0.6. Both depths are referenced to the spillway crest, The greatest submergence ratio (h3/h 1 ) measured for the spillway was only 0.20, Submerged weir flow, which occurs when the submergence ratio (h3/h^) is equal to or greater than 0.6, did not occur during the study period; thus, the general submergence ratio suggested by Collins (0.6) is assumed to be appli cable for the spillway.
Upstream pool stage for the discharge measurements ranged from 4.05 to 5.90 ft, and discharge ranged from 169 to 2,990 cubic feet per second (ft3/s). The discharge coefficients for free weir flow defined by the measurements ranged from 2.61 to 3.14 (table 2). The relation between headwater depth (h-j) and free weir discharge coefficient for the spillway is shown in figure 6. The resulting equation relating the discharge coefficient for free weir flow to headwater depth is
Cw = 2.94 h-,0.087 . (5)
10.0 T I I I I I I T
15, Discharge measurement and number (table 2)
Cw=2.94h1 °-087
o
zUJo
UJo occUJ5 I
UJ UJ
J315
1.0 i i i i i I I iO.I i.o 10.0
HEADWATER DEPTH (h,), IN FEET
Figure 6. Relation between discharge coefficient for free weir flow and headwater depth for spillway (fish ladder included).
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Table 2. Characteristics of discharge
at Mc
Henr
y Dam
Measure
ment
Stru
ctur
e *
numb
er
Date
Sluice
1 03
-22-
85gates
Do.
2 03-22-85
Do.
3 03-26-85
Do.
4 03-26-85
Spillway
5 05
-16-
85
Sluice
gates
6 05
-16-
85
Do.
7 1 1-
04-8
5
Do.
8 1 1-
04-8
5
Do.
9 03
-17-
86
Do.
10
04-2
2-86
Do.
11
04-2
2-86
Do.
12
05-2
3-86
Spillway
13
08-2
8-86
Sluice
14
08-2
8-86
gates
Gate
opening
(hg
> (ft)
out of
water
73.
00
out
ofwater
73.30
7.60
83.15
82.50
out
ofwater
71.2
94@2
iei " 2 7.2
[ft,
feet;
ft3/
s,
Head
wate
r-
pool
Flow
stage3
regime2
(ft)
FW
3.51
FO
3.68
FW
2.64
FO
2.71
FW
4.05
FO
4.03
FO
3.98
FO
4.05
FW
4.31
FO
3.23
FO
3.13
FO
4.16
FW
4.23
FO
4.22
cubic feet per second]
Head
wate
r depth
(h,)
1*
(ft)
5.36
5.53
4.49
4.56 .37
5.88
5.83
5.90
6.16
5.08
4.98
6.01 .55
6.07
Tailwater-
pool
stage5
(ft)
3.90
3.70
3.45
3.42
1.35
1.35
2.82
2.75
5.03
1.71
1.85
2.25
1.05
1.05
Tailwater
dept
h (h
3)6
(ft)
2.90
2.70
2.45
2.42 ~ .35
1.82
1.75
4.03 .71
.85
1.25
.05
Measured
disc
harg
e (ft3/
s)
2,790
1,99
0
2,100
1,85
0
169
448
1,83
0
1,46
0
3,230
833
1,18
0
967
342
180
Computed
coef
fi
cient
3.27 .51
3.21 .48
2.61 .56
.54
.54
3.07 .56
.53
.60
2.91 .66
Deviation
from
rati
ng
(per
cent
)
3.0
-1.5 1.4
-7.5
-2.9
-6.1 5.7
3.5
-3.0 -.3
-1.9
6.2
4.6
1.7
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Tabl
e 2. Characteristics of discharge
at Mc
Henr
y Dam Continued
Structure
1
Spillway
Slui
cega
tes
Do*
Do.
Measure
ment
number
15 16 17 18
Gate
open
ing
<vDa
te
(ft)
09-2
7-86
09-27-86
74.0
09-27-86
out of
water
09-27-86
74.9
Flow
regime ̂
FW FO FW FO
Head
wate
r-pool
stag
e3
(ft)
5.34
5.35
5.20
5.22
Headwater
depth
(h,)"
(ft)
1.66
7.20
7.05
7.07
Tailwater-
pool
stag
e5
(ft)
6.12
6.15
6.25
6.25
Tailwater
dept
h (h
3)6
(ft) « 5.15
5.25
5.25
Measured
discharge
(ft3/
s)
1,880
3,040
4,050
3,60
0
Computed
coeffi
cient
3.05 .51
3.15 .50
Devi
atio
nfrom
rati
ng
(percent)
-1.1 1.3
-1.8 1.1
Do.
1909-27-86
74.5
FO5.26
7.11
6.30
5.30
3,320
.50
Spillway
20
09-30-86
FW
5.90
2.22
6.98
.45
2,990
3.14
-.7
Sluice
gates
Do.
21
09-30-86
74.0
SO
5.90
7.75
6.98
5.
98
2,600
22
09-30-86
74.5
SO
5.86
7.71
6.98
5.98
2,920
.59
.67
-.4 .3
Do.
23
10-15-86
out
of
FW
water
4.25
6.10
5.10
4.10
3,270
3.16
-.3
1Dat
um of spillway cr
est
and
sluice gates
are
736.68 an
d 731.15 ft
ab
ove
sea
leve
l, re
spectively.
2FW
designates fr
ee weir fl
ow,
FO designates free or
ific
e flow,
and
SO designates submerged
orif
ice
flow.
^Ref
eren
ced
to Su
rvey
ga
ge da
tum
of 733.00 ft above
sea
level.
**He
adwa
ter
dept
hs ar
e computed by applying an
adjustment factor (-
3.68
ft
for
spil
lway
; 1.
85 ft for
sluice ga
tes)
to the
headwater-pool st
ages
.
^Ref
erenced
to Survey ga
ge da
tum
of 730.15 ft
ab
ove
sea
level.
6Tailwater de
pths
are
computed by applying an
adjustment factor (-6.53 ft for
spil
lway
; -1.00
ft for
sluice gates) to
the
tailwater-pool st
ages
.
7Five gates
set
to same opening.
8Fou
r gates
in operation
set
to sa
me op
enin
g, on
e gate cl
osed
.9Fou
r ga
tes
were
set
to 2.0
ft an
d on
e gate at
1.0
ft;
the
coefficient
from
fi
gure
8
was
used to
su
btra
ct fl
ow for
a 1.0-ft
open
ing;
a
coef
fici
ent
for
a 2.0-ft op
enin
g wa
s determined from the
meas
urem
ent.
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Discharge for free weir flow over the spillway is computed by combining equation 3 in table 1 with equation 5 for the free weir coefficient (Cw ). The resulting equation of discharge is
Q = 847 (h^ 1 ' 59 (6)
where h-j is the headwater depth above the spillway crest. Discharges for free weir flow over the spillway are given in table 3 and are extrapolated to include the historical peak stage of 6.36 ft.
Sluice gates
Nineteen discharge measurements, ranging from 180 to 4,050 ft3/s, were made to describe flow under the sluice gates. Characteristics of flow and the discharge coefficient associated with each measurement are listed in table 2. Discharge coefficients, required for the equations of flow (table 1), were determined for free weir, free orifice, and submerged orifice flow. Submerged weir flow did not occur during the study period.
Nineteen measurements of discharge, stage, and gate opening provided data for identifying the flow regimes for the sluice gates at McHenry Dam. The criteria for identifying free weir flow are that the ratio of gate opening (hg) to headwater depth (h-j) is greater than 0.73, and the ratio of tailwater depth (113) to the headwater depth is less than 0.75 (fig. 4). Submerged weir flow occurs when hq/h-j is greater than 0.73, and h3/h 1 is greater than 0.75. Orifice flow occurs when hq/h-| is less than 0.73 (the bottom of the gate must be touching the water surface) and is free orifice flow when the submergence ratio (ho/hg) is less than 1.3. Submerged orifice flow occurs when the sub mergence ratio is equal to or greater than 1.3.
Free weir flow under the sluice gates occurred during measurements 1, 3, 9, 17, and 23 (table 2). The headwater-pool stage ranged from 2.64 to 5.20 ft, and the discharge ranged from 2,100 to 4,050 ft /s. A discharge coef ficient for free weir flow of 3.17 was defined by. the measurements (fig. 7). Discharge for free weir flow under five sluice gates is computed by using using equation 3 in table 1 and a coefficient of 3.17. The resulting equation of discharge is
Q = 218 (h^ 1 ' 5 (7)
where h-j is headwater depth above the sluice-gate sill. Discharges for free weir flow are given in table 4.
Measurements 2, 4, 6-8, 10-12, 14, 16, 18, and 19 were used to calculate discharge coefficients for free orifice flow. Discharge coefficients varied from 0.48 to 0.66 for free orifice flow for a range of gate openings (fig. 8) The resulting equation relating the discharge coefficient for free orifice flow to gate opening (hg ) is
C = 0.57 (hg )"°- 084 . (8)
12
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Table 3. Discharge rating table for free weir flow over spillway (f
ish
ladder included)
Headwater
pool stage,
in feet
1
3.60
3.70
3.80
3.90
4.00
4.10
4.20
4.30
4.40
4.50
4.60
4.70
4.80
4.90
5.00
5.10
5.20
5.30
5.40
5.50
5.60
5.70
5.80
5.90
6.00
6.10
6.20
6.30
Headwater pool st
age,
in hundredths of
feet
.00
1.7
29 76
138
213
299
396
502
618
742
874
1,010
1,160
1,32
01,480
1,650
1,82
02,010
2,190
2,390
2,590
2,800
3,010
3,230
3,450
3,680
3,920
.01
3.2
33 82 145
221
309
406
514
630
755
888
1,030
1,180
1,330
1,500
1,670
1,840
2,020
2,210
2,410
2,610
2,820
3,030
3,250
3,480
3,710
3,940
.02
5.1
37 88 152
230
318
417
525
642
768
898
1,04
01,190
1,350
1,510
1,680
1,860
2,040
2,230
2,430
2,630
2,840
3,050
3,270
3,500
3,730
3,960
.03
Di scharge
7.2
41 93 160
238
327
427
536
654
781
915
1,060
1,210
1,360
1,530
1,700
1,880
2,060
2,250
2,450
2,650
2,860
3,080
3,300
3,520
3,750
3,990
.04
, in cubic
9.7
46 99 167
246
334
437
547
666
794
929
1,070
1,220
1,380
1,550
1,720
1,90
02,080
2,270
2,470
2,670
2,880
3,100
3,320
3,540
3,780
4,010
.05
feet per
12 51 106
174
254
347
448
559
679
807
943
1,090
1,240
1,400
1,560
1,740
1,910
2,100
2,290
2,490
2,690
2,900
3,120
3,340
3,570
3,800
4,040
.06
second 15 55 112
182
264
356
459
571
691
820
957
1,10
01,
250
1,410
1,58
01,
750
1,930
2,120
2,310
2,510
2,710
2,920
3,140
3,360
3,590
3,820
4,060
.07
18 60 118
190
272
366
470
582
704
836
971
1, 120
1,270
1,43
01,
600
1,77
01,950
2,140
2,330
2,530
2,730
2,950
3,160
3,380
3,610
3,850
.08 0.
022 66
125
197
281
376
480
594
716
847
986
1,130
1,290
1,450
1,610
1,790
1,97
02,160
2,350
2,550
2,760
2,970
3,180
3,410
3,640
3,870
.09 0.
625 71 132
205
290
386
491
606
729
861
1,000
1,15
01,
300
1,460
1,630
1,81
01,990
2,180
2,370
2,570
2,780
2,990
3,210
3,430
3,660
3,890
1Referenced to Survey gage datum of 733.00 ft
above se
a level.
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10.0
O
UJ
gLL LL LLJ O O
ocLLI
LLI LLI
1.0
Discharge measurement and number (table 2)
23
917
HEADWATER DEPTH (h,), IN FEET
Figure 7. Relation between discharge coefficient for free weir flow and headwater depth for sluice gates.
14
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Table 4. -Discharge rating table for free weir flow under five sluice gates
Headwater pool stage, in feet 1
0.20.30.40.50.6
0.70.80.91.01.1
1.21.31.41.51.6
1.71.81.92.02.1
2.22.32.42.52.6
2.72.82.93.03.1
3.23.33.43.53.6
3.73.83.94.04.1
4.24.34.44.54.6
4.74.84.95.05.1
Headwater pool stage,
.00
640687736785836
888940994
1,0501,100
1,1601,2201,2801,3401,400
1,4601,5201,5801,6501,710
1,7801,8401,9101,9802,050
2,1202,1902,2602,3302,400
2,4702,5502,6202,7002,770
2,8502,9303,0103,0803,160
3,2403,3203,4103,4903,570
3,6503,7403,8203,9103,990
.01
645692741790841
893946
1,0001,0501,110
1,1701,2201,2801,3401,400
1,4601,5301,5901,6501,720
1,7801,8501,9201,9802,050
2,1202,1902,2602,3402,410
2,4802,5602,6302,7102,780
2,8602,9403,1013,0903,170
3,2503,3303,4103,5003,580
3,6603,7503,8303,9204,000
.02
649697746795846
898951
1,0001,0601,120
1,1701,2301,2901,3501,410
1,4701,5301,6001,6601,720
1,7901,8601,9201,9902,060
2,1302,2002,2702,3402,420
2,4902,5602,6402,7102,790
2,8702,9403,0203,1003,180
3,2603,3403,4203,5003,590
3,6703,7603,8403,9304,010
.03
Discharge
654702751800851
903956
1,0101,0701,120
1,1801,2401,2901,3501,420
1,4801,5401,6001,6701,730
1,8001,8601,9302,0002,070
2,1402,2102,2802,3502,420
2,5002,5702,6402,7202,800
2,8702,9503,0303,1103,190
3,2703,3503,4303,5103,600
3,6803,7603,8503,9304,020
.04
in hundredths of feet
.05
, in cubic feet
659707755805857
909962
1,0201,0701,130
1,1801,2401,3001,3601,420
1,4801,5501,6101,6701,740
1,8001,8701,9402,0102,070
2,1402,2102,2902,3602,430
2,5002,5802,6502,7302,800
2,8802,9603,0403,1203,200
3,2803,3603,4403,5203,600
3,6903,7703,8603,9404,030
663711760811862
914967
1,0201,0801,130
1,1901,2501,3101,3701,430
1,4901,5501,6201,6801,740
1,8101,8801,9402,0102,080
2,1502,2202,2902,3602,440
2,5102,5902,6602,7402,810
2,8902,9703,0403,1203,200
3,2803,3703,4503,5303,610
3,7003,7803,8703,9504,040
.06
per second
668716765816867
919973
1,0301,0801,140
1,2001,2501,3101,3701,430
1,5001,5601,6201,6901,750
1,8201,8801,9502,0202,090
2,1602,2302,3002,3702,440
2,5202,5902,6702,7402,820
2,9002,9703,0503,1303,210
3,2903,3703,4603,5403,620
3,7003,7903,8703,9604,050
.07
673721770821872
924978
1,0301,0901,140
1,2001,2601,3201,3801,440
1,5001,5601,6301,6901,760
1,8201,8901,9602,0302,090
2,1602,2402,3102,3802,450
2,5302,6002,6802,7502,830
2,9002,9803,0603,1403,220
3,3003,3803,4603,5503,630
3,7103,8003,8803,9704,050
.08
678726775826877
930983
1,0401,0901,150
1,2101,2701,3201,3801,450
1,5101,5701,6301,7001,760
1,8301,9001,9602,0302,100
2,1702,2402,3102,3902,460
2,5302,6102,6802,7602,830
2,9102,9903,0703,1503,230
3,3103,3903,4703,5503,640
3,7203,8103,8903,9804,060
.09
682731780831882
936989
1,0401,1001,160
1,2101,2701,3301,3901,450
1,5101,5801,6401,7001,770
1,8401,9001,9702,0402,110
2,1802,2502,3202,3902,470
2,5402,6102,6902,7702,840
2,9203,0003,0803,1603,240
3,3203,4003,4803,5603,650
3,7303,8103,9003,9904,070
15
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Table 4. Discharge rating table for free weir flow under five sluice gates Continued
Headwaterpool stage,in feet1hi .00
Headwater pool stage, in hundredths of feet
.01 .02 .03 .04 .05 .06 .07 .08 .09
Discharge, in cubic feet per second
5.25.35.45.55.6
5.75.85.96.06.1
6.26.3
4,0804,1704,2604,3404,430
4,5204,6104,7004,7904,890
4,9805,070
4,0904,1804,2604,3504,440
4,5304,6204,7104,8004,900
4,9905,080
4,1004,1904,2704,3604,450
4,5404,6304,7204,8104,910
5,0005,090
4,1104,1904,2804,3704,460
4,5504,6404,7304,8204,910
5,0105,100
4,1204,2004,2904,3804,470
4,5604,6504,7404,8304,920
5,0205,110
4,1204,2104,3004,3904,480
4,5704,6604,7504,8404,930
5,0305,120
4,1304,2204,3104,4004,490
4,5804,6704,7604,8504,940
5,0305,130
4,1404,2304,3204,4104,500
4,5904,6804,7704,8604,950
5,040
4,1504,2404,3304,4204,500
4,5904,6904,7804,8704,960
5,050
4,1604,2504,3404,4204,510
4,6004,6904,7904,8804,970
5,060
^Referenced to Survey gage datum of 733.00 ft above sea level.
1.0
O
zUJ O U. U. UJOoUJ O U. QC O
UJ UJocU.
1412
19
-0.084C= 0.57 h0
e Discharge measurement and number (table 2)
O.I i i i i I I0.1 1.0 10.0
GATE OPENING (hfl ). IN FEET
Figure 8. Relation between discharge coefficient for free orifice flow and sluice-gate opening.
16
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Discharge for free orifice flow under the five sluice gates is computed by combining equation 1 in table 1 with equation 8. The resulting equation of discharge is
Q = 314 (h)°- 916 (9)
where hg is sluice-gate opening and h1 is headwater depth above the sluice gate sill. The relation between upstream-pool stage, gate opening, and discharge is presented in table 5.
Measurements 21 and 22 were made during submerged orifice flow. The sub mergence ratio (h3/hg ) for measurement 21 was 1.50 with a coefficient of 0.59. Measurement 22 had a submergence ratio of 1.33 and a coefficient of 0.67. The relation between the discharge coefficient for submerged orifice flow and sub mergence ratio is illustrated in figure 9. The resulting equation relating the discharge coefficient for submerged orifice flow to the submergence ratio (h 3/hg ) is
Cs = 0.89 (h3/hg ) -1.00 (10)
I.O
O
UJ I-o z
O ULI UL
O UJuj OO O
CO
O.I
21
22
Discharge measurement and number (table 2)
Gate opening
Tailwater depth
Cs = 0.89 (h 3 /hg)-1.00
1.0 10.0 ORIFICE SUBMERGENCE RATIO (h3 /li9 )
Figure 9. Relation between discharge coefficient for submerged orifice flow and sub mergence ratio for sluice gates.
17
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00
Table 5. Discharge rating table for free orifice flow under five sluice gates set to same gate opening
[Fre
e orifice flow does not occur in
the areas marked by dashed li
nes]
Upstream
pool stage,
in feet
1
1.0
1.2
1.4
1.6
1.8
2.0
2.2
2.4
2.6
2.8
3.0
3.2
3.4
3.6
3.8
4.0
4.2
4.4
4.6
4.8
5.0
5.2
5.4
5.6
5.8
6.0
6.2
Gate openings, in feet
0.1 64 67 69
71 73 75 77 79
8082
84
86 87 89
91 9294
95
9798
100
0.2 121
126
130
134
137
141
145
148
152
155
158
162
165
168
171
174
177
180
183
185
188
-
0.4 229
237
244
252
259
266
273
280
286
292
299
305
311
317
322
328
334
339
344
350
355
0.6 332
343
355
365
376
386
396
406
415
424
433
442
451
459
468
476
484
492
500
507
515
_
_
0.8
432
447
462
475
489
502
515
528
540
552
564
575
586
598
609
619
630
640
650
660
670
1.0
Discharge,
530
548
566
583
600
616
632
647
663
677
691
706
719
733
746
760
772
785
798
810
822
-
1.5
in cubic
768
795
821
845
869
893
916
939
960
981
1,000
1,020
1,040
1,060
1,080
1,100
1,120
1,140
1,160
1,170
1,190
-
2.0
feet per
1,000
1,030
1,070
1,100
1,130
1,160
1,190
1,220
1,250
1,280
1,300
1,330
1,360
1,380
1,410
1,430
1,460
1,480
1,500
1,530
1,550
2.5
second
1,340
1,370
1,410
1,450
1,480
1,520
1,550
1,580
1,620
1,650
1,680
1,710
1,740
1,770
1,800
1,830
1,850
1,880
-
3.0
1,77
01,810
1,850
1,890
1,930
1,970
2,010
2,040
2,080
2,110
2,150
2,180
2,220
2,250
3.5
2,180
2,220
2,270
2,310
2,350
2,390
2,430
2,470
2,510
2,550
2,590
2,630
2,660
2,700
2,740
2,770
2,810
4.0
2,660
2,700
2,750
2,800
2,840
2,880
2,930
2,970
3,010
3,050
3,090
3,130
3,170
4.5
3,110
3,160
3,210
3,260
3,310
3,350
3,400
3,440
3,490
3,530
5.0
3,590
3,640
3,690
3,740
3,790
3,840
3,890
1Referenced
to Survey ga
ge datum
of 733.00 ft ab
ove
sea
level.
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Discharge for submerged orifice flow under five sluice gates set to the same opening is computed by combining equation 2 in table 1 with equation 10 The resulting equation of discharge is
Q = 491(Ah) 0 ' 5 (1D
where h is the gate opening and Ah equals the difference between the head water depth and tailwater depth.
Submerged orifice coefficients and the submergence ratio (h3/hg ) general ly plot on logarithmic paper as a straight line when submergence ratios are greater than 2.0 (Collins, 1977). For ratios less than 2.0, coefficients may be greater than those extrapolated from the straight line relation. The dis charge coefficients for submergence ratios greater than 2.0 may be greater than those illustrated in figure 9 because the submergence ratios for discharge measurements 21 and 22 were less than 2.0. Additional discharge measurements are needed to determine if the discharge coefficients for submerged orifice flow are applicable when submergence ratios (h3/hg ) are greater than 2.0.
Evaluation of ratings
The discharge of the Fox River over the spillway and fish ladder and through the sluice gates at McHenry Dam can be calculated from records of headwater- and tailwater-pool stages and gate openings using equations of dis charge for free weir, free orifice, and submerged orifice flow regimes which are summarized in table 6. Hydraulic conditions used to identify flow regimes are also summarized in table 6. Discharge for free weir and free orifice flow can also be obtained from tables 3, 4, and 5.
Table 6.--Summary of hydraulic conditions and discharge equations for different flow regimes at McHenry Dam control structures
[Q, Discharge, in cubic feet per second; h-|, headwater depths are computed by applyingan adjustment factor (-3.68 ft for spillway and 1.85 ft for sluice gates) to the
headwater-pool stage; h3/ tailwater depths are computed by applying anadjustment factor (-6.53 ft for spillway and -1.00 ft for sluice gates)to the tailwater-pool stage; hg, sluice-gate opening; Ah equals h1 -h3 ]
Structure
Spillway
Sluice gates
Sluice gates
Sluice gates
Flow regime
Free weir
Free weir
Free orifice
Submerged orifice
Hydraulic conditions
h3/h., <0.6
hg.^0.73 h 1 and h3/h 1 <0.75
hg<0.73 h 1 and h3 <1.3 h
hg<0.73 h1 and hjXI.3 h
Equation of discharge
Q = 847 (h.,) 1 ' 59
Q * 218 (h,) 1 - 5
Q = 3.14 (hg)°- 916 ( hl )°- !
Q = 491 h (Ah) 0 ' 5
Equation number
(6)
(7)
' (9)
(11)
19
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Submerged weir flow did not occur during the study; therefore, discharge coefficients were not determined. Based on observations of flow during the near-record flood of September-October 1986, it is probable that the occurrence of submerged weir flow is rare. On occasions when it could have occurred, the operating procedure of the dam prevented it.
Figure 10 compares daily discharge for the Fox River at McHenry Dam to discharge at the gaging station on the Fox River at Algonquin for selected days in the 1986 and 1987 water years. Daily discharge at McHenry Dam was computed from hourly records of headwater-pool stage, twice-daily readings of the tailwater-pool stage and gate opening, and equations 6, 7, 9, and 11. The gaging station at Algonquin is 16 miles downstream from McHenry Dam and has a drainage area of 1,403 mi2 , 12 percent larger than at McHenry Dam. The solid line in figure 10 represents a 1:1 ratio of discharges at McHenry Dam and Algonquin. Daily discharge at Algonquin is 10 to 12 percent larger than McHenry Dam, except during periods of rapidly increasing discharge at McHenry Dam. During these periods, the daily discharge at Algonquin is only 1 to 2 percent larger than at McHenry Dam, but, after the initial rise, the relation returns to the 10 to 12 percent range.
Computation of discharge
The following are examples of how discharge may be calculated using equa tions in table 6 and discharge from the rating tables for free orifice and free weir flow.
Example 1: The following conditions exist:
Headwater-pool stage is 5.20 ft, tailwater pool stage is 3.0 ft, and all gates are out of the water.
Flow through the sluice gates is determined by first converting the stages to depths above the sluice-gate sill. This is done by adding the difference between headwater gage datum and the elevation of the sill (1.85) to the head water stage and then subtracting the difference between the tailwater gage datum and the elevation of the sill (1.00) from the tailwater stage.
h-, = 5.20 + 1.85 = 7.05 ft
h3 = 3.00 - 1.00 = 2.00 ft
Because the gates are out of the water and h3/h^ (0.28) is less than 0.75 (table 6), free weir flow exists.
Using equation 7 from table 6, discharge is
Q = 218 (h-,) 1 * 5
= 218 (7.05) 1 * 5
= 4,080 ft3/s.
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7,000
< 6,000 Q
oczQJ
O 5,000
QZg 4,000QJ COOC QJ 0.
UJ 3,000
LL
gmoZ 2,000Qj"
O OC<
OCO | fOOOa
0
9 Discharge measurement at McHenry Dam
Steady flow
S Rapidly rising flow
1,000 2,000 3,000 4,000 5,000 6,000
DISCHARGE, IN CUBIC FEET PER SECOND, AT ALGONQUIN
7,000
Figure 10. Daily discharges for Fox River at McHenry Dam and Fox River at Algonquin for selected days during the data-collection period.
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Flow over the spillway and through the fish ladder is determined by first con verting the headwater stage to depth above the spillway crest. This is done by subtracting the difference between headwater gage datum and the elevation of the spillway crest (3.68) from the headwater stage reading,
h-, = 5.20 - 3.68 = 1.52 ft,
and using equation 6 from table 6. The discharge is
Q = 847 (h-,) 1 * 59
= 847 (1.52) 1 ' 59
= 1,650 ft3/s.
Total discharge = 4,080 + 1,650 = 5,730 ft3/s.
Alternately, the discharge may be computed from tables 3 and 4 for a headwater-pool stage of 5.20 ft.
Free weir flow over the spillway = 1,650
Free weir flow under the sluice gates = 4,080
Total discharge = 5,730 ft3/s.
Example 2: The following conditions exist:
Headwater-pool stage is 3.68 ft, tailwater-pool stage is 3.70 ft, and five gates are set to 3.0 ft each.
First, pool stages must be converted to depths above the sluice-gate sill.
h<| = 3.68 + 1.85 = 5.55 ft
h3 = 3.70 - 1.00 = 2.70 ft
Because hg/h<| (0.54) is less than 0.73 and h3/h (0.90) is less 1.30 (table 6), free orifice flow exists.
Using equation 9 in table 6, the discharge is
Q = 314 (hg )°- 916 (h,) Q ' S
Q = 314 (3.0)°* 916 (5.55) 0 * 5
Q = 2,020 ft3/s.
Alternately, the discharge may be computed from table 6 for an upstream- pool stage of 3.68 ft.
Free orifice flow under five sluice gates = 2,020 ft3/s.
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Example 3: The following conditions exist:
Headwater-pool stage is 5.90 ft, tailwater-pool stage is 6.98 ft, and five gates are set to 4.0 ft each.
First, the pool stages must be converted to depths above the sluice-gate sill.
h 1 = 5.90 + 1.85 = 7.75 ft
h3 = 6.98 - 1.00 = 5.98 ft
Ah = 1.77 ft
Because hg/h 1 (0.52) is less than 0.73 and h3/hg (1.50) is greater than 1.30 (table 6), submerged orifice flow exists.
Using equation 11 from table 6, the discharge is
Q = 491 hg (Ah) 0 - 5
= (491)(4.00)(1.77) 0 ' 5
= 2,610 ft3/s.
Flow over the spillway and fish ladder is determined by converting the headwater-pool elevation to depth above the spillway crest,
h-, = 5.90 - 3.68 = 2.22 ft,
and using equation 6 from table 6, the discharge is
Q = 847 (h-,) 1 * 59
Q = 847 (2.22) 1 ' 59
Q = 3,010 ft3/s.
Total discharge = 2,610 + 3,010 = 5,620 ft3/s.
SUMMARY AND CONCLUSIONS
Twenty-three discharge measurements were used to develop discharge ratings for the control structures at McHenry Dam on the Fox River. Discharge ratings were developed for free weir flow over the spillway and fish ladder; and free weir, free orifice, and submerged orifice flow under the sluice gates. Hydraulic conditions that identify flow regimes at McHenry Dam were defined by ratios between headwater depth (h-j), tailwater depth (h3 ), and gate opening (hg ). Flow under the sluice gates was identified as weir flow when the ratio of gate opening (hg) to headwater depth (h^) is greater than 0.73 and as orifice flow when hg/h-j is less than 0.73. Free orifice flow occurs when the ratio of tailwater depth (h 3 ) to gate opening (hg ) is less than 1.3,
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and submerged orifice flow occurs when hg/hj is greater than 1.3. Flow under the sluice gates was identified as free weir flow when the ratio of tailwater depth (113) to headwater depth (h-j) is less than 0.75 and as submerged weir flow when h3/h^ is greater than 0.75. Flow over the spillway was identified as free weir flow when the ratio of tailwater depth (h3 ) to headwater depth (h-|) is less than 0.60 and as submerged weir flow when h3/h^ is greater than 0.60.
Discharge coefficients used in equations to compute discharge were deter mined for free weir, free orifice, and submerged orifice flow. Equations that relate discharge coefficients to headwater depth, tailwater depth, gate open ing, or a combination of these, were developed. These equations were combined with equations of flow to form discharge equations for the control structures at McHenry Dam.
Additional discharge measurements are needed to determine discharge coef ficients for submerged weir flow. Additional discharge measurements are also needed to determine if the discharge coefficients for submerged orifice flow are applicable when submergence ratios (h3/hg) are greater than 2.0. Hydraulic conditions for submerged weir and submerged orifice flow occur only at very high streamflows and did not occur during the data-collection period of this project.
All of the measured flow regimes were used in a comparison of daily discharge with the Fox River at Algonquin. Computed daily discharges for Fox River at McHenry Dam are reasonable and consistent when compared with the com puted daily discharge for Fox River at Algonquin.
REFERENCES CITED
Buchanan, T. J., and Somers, W. P., 1969, Discharge measurements at gaging stations: U.S. Geological Survey Techniques of Water-Resources Investigations Book 3, Chapter A8, 65 p.
Collins, D. L., 1977, Computation of records of streamflow at controlstructures: U.S. Geological Survey Water-Resources Investigations 77-78, 57 p.
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GOVERNMENT PRINTING OFFICE 1988-543-271/62103