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DISCHARGE RATINGS FOR CONTROL GATES AT MISSISSIPPI RIVER LOCK AND DAM 14, LE CLAIRE, IOWA By Albert J. Heinitz U.S. GEOLOGICAL SURVEY Water Resources Investigations Report 85-4261 Prepared in cooperation with U.S. Army Corps of Engineers Rock Island District Rock Island, Illinois Iowa City, Iowa 1985
46

By Albert J. Heinitz - USGS

Jun 14, 2022

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Page 1: By Albert J. Heinitz - USGS

DISCHARGE RATINGS FOR CONTROL GATES

AT MISSISSIPPI RIVER LOCK AND DAM 14,

LE CLAIRE, IOWA

By Albert J. Heinitz

U.S. GEOLOGICAL SURVEY

Water Resources Investigations Report 85-4261

Prepared in cooperation with

U.S. Army Corps of Engineers Rock Island District Rock Island, Illinois

Iowa City, Iowa 1985

Page 2: By Albert J. Heinitz - USGS

UNITED STATES DEPARTMENT OF THE INTERIOR

Donald Paul Hodel, Secretary

GEOLOGICAL SURVEY

Dallas L. Peck, Director

For additional information write to

U.S. Geological Survey Water Resources Division P.O. Box 1230 Iowa City, Iowa 52244

ii

Page 3: By Albert J. Heinitz - USGS

CONTENTS

Page

T |^ 4» y* ^^ /"Ji i r* 4" i /% v\ ^_^_ ^_ ^_ ^_ ^_ ^_ ^_ ^^ ^^ ^^ ^^ ^^ _^ _^ OXJI L.L L/UlUw LX UJ1 *-. -. *. «.«.«. «.«««. «.«.«.«.«.«. «.«. ^

Purpose and Scope - 3Acknowledgements --- 3

Location of study area 4

Flow Controls 4Types of flow at Dam 14 control gates -- 7

Dam Operation - 8

Discharge and stage measurements - 11

Tainter gate flow 14Computation of gate opening 14Submerged orifice flow coefficients - 18Submerged orifice discharge equation 20

Roller gate flow 22Gate opening - 22Submerged orifice flow coefficient 22Submerged orifice discharge equation - 26Free weir flow coefficient 27Free weir discharge equation 29

Discharge equations and ratings - 30

Conclusions 37

Selected references 38

Xll

Page 4: By Albert J. Heinitz - USGS

ILLUSTRATIONS

8

9

10

11

Page

Figure 1. Map of Inland Waterway Navigation System of theUpper Mississippi River Bas: n 5

2. Map showing location of tainter and roller gatesat Lock and Dam 14 on the Mississippi River 9

3. Diagram showing sectional views of tainter androller gates on Mississippi River Lock and Dam 14- 10

4. Diagram showing details of tainter gates atMississippi River Lock and Dam 14 15

5. Graph showing gage indicator corrections and com­ parison of gate openings and discharges at 1.0 foot gage indicator settings? for tainter gates on Mississippi River Lock and Dam 14 17

6. Graph showing submerged orifice flow coefficient- submergence ratio relation for Mississippi River Lock and Dam 14 tainter gates 19

7. Graph showing comparison of discharge measurements of September 12-13, 28, 1983, to rating curves for tainter gates at Mississippi River Lock and Dam 14 21

Graph showing submerged ori submergence ratio relation Mississippi River Locks and

Diagram showing positions o:: roller gates for selected openings

Graph showing free weir flow relation for roller gates in for Mississippi River Locks

Graph showing discharge-headwater relation for free weir flow for roller gates in submerged position, Mississippi River Lock and Dams 11 and 14 - -- *

ice flow coefficient- or roller gates at Dams 11 and 14 23

25

coefficient-headwater submerged position

and Dams 11 and 14 28

29

iv

Page 5: By Albert J. Heinitz - USGS

ILLUSTRATIONS continued

Page12. Graph showing discharge ratings for submerged

orifice flow for a single tainter gate at Missis­ sippi River Lock and Dam 14 compared to hydraulic-model ratings 34

13. Graph showing discharges for submerged orifice flow for a single roller gate at Mississippi River Lock and Dam 14 compared to hydraulic- model ratings 35

TABLES

Table 1. Flow controls and their respective hydraulic equations

Summary of current-meter measurements and hydraulic control data for control gates at Mississippi River Lock and Dam 14 13

Summary of discharge equations for control gates at Mississippi River Lock and Dam 14 31

Stage-discharge rating for submerged-orifice flow for a single tainter gate at Mississipi River Lock and Dam 14 with upstream pool stage of 14.92 feet.- 32

Stage-discharge rating for submerged-orifice flow for a single roller gate at Mississippi River Lock and Dam 14 with upstream pool stage of 14.92 feet.- 33

Mississippi River Lock and Dam 14 operation sche­ dule Plan A 36

V

Page 6: By Albert J. Heinitz - USGS

SYMBOLS AND UNITS

Symbol

a

B

B s

C

C gs

Csw

Csws

C w

C ws

8

G

H,

Definition Unit

H Is

Is

3s

Elevation difference, trunnion centerline to sill ft

Lateral width of a Tainter or Roller gate ft

Length of fixed spillway ft

Free orifice flow coefficient of discharge

Submerged orifice flow coefficient of discharge

Free weir flow coefficient of discharge, fixed spillway

Submerged weir flow coefficient of discharge, fixed spillway

Free weir flow coefficient of discharge, gate crest

Submerged weir flow coefficient o:E discharge, gate crest

Acceleration due to gravity

Gage indicator reading

Total headwater head including velocity head referenced

to gate sill

Static headwater head referenced to gate sill

Static tailwater head referenced

Total headwater head including velocity head referenced

to the gate crest

Static headwater head referenced

Static tailwater head referenced

to gate sill

to gate crest

to gate crest

Vertical gate opening

Number of lockages occurring betwieen recordings

Computed discharge per gate

Computed fixed-spillway discharge

ft/s 2

ft

ft

ft

ft

ft

ft

ft

ft

ft 3 /s

ft 3 /s

vi

Page 7: By Albert J. Heinitz - USGS

SYMBOLS AND UNITS --continued

Symbol Definition Unit

R Radius from trunnion centerline to upstream face of a

Tainter gate ft

r Radius from trunnion centerline to gate R.P. ft

Ah=h 1 -h_ Static head loss through structure ftJ. «J

At Time between recordings sec

8 Included angle between radial lines from the trunnion

centerline through the R.P. and through the lower lip

of the gate deg

0 The angle measured from the horizontal to the radial

line from the trunnion centerline through the gate

R.P. with the gate in a closed position deg

< Less than

> Greater than

^ Greater than or equal to

Page 8: By Albert J. Heinitz - USGS

FACTORS FOR CONVERTING INCH-POUND UNITS TO INTERNATIONALSYSTEM UNITS (SI)

The following factors may be used to convert published herein to the International System

Multiply inch-pound units

inches (in) feet (ft) miles fmi)

acressquare miles (mi 2 )

cubic feet (ft 3 )cubic feet per second-day

(ft 3/s-day) acre-feet (acre-ft)

cubic feet per second (ftVs)

By

-Length-

25.4.3048

1.609

-Area-

4,0472.590

- Volume -

0.028322,447

1,233

-Flow-

0.02832

the inch-pound units of Units (SI)

To obtain SI units

millimeters (mm) meters (m) kilometers (tan)

square meters (m2 ) Square kilometers (km2 )

cubic meters (m3 )cubic meters (m 3 )

cubic meters (m 3 )

cubic meters per second (m 3 /s)

viii

Page 9: By Albert J. Heinitz - USGS

DISCHARGE RATINGS FOR CONTROL GATES

AT MISSISSIPPI RIVER LOCK AND DAM 14, LE CLAIRE, IOWA

By Albert J. Heinitz

ABSTRACT

The water level of the navigation pools on the Mississippi River are

maintained by the operation of tainter and roller gates at the locks and dams.

Discharge ratings for the gates on Lock and Dam 14, at Le Claire, Iowa, were

developed from current-meter discharge measurements made in the forebays of

the gate structures.

Methodology is given to accurately compute the vertical gate openings of

the tainter gates.

Discharge coefficients, in equations that express discharge as a function

of tailwater head, headwater head, and vertical height of gate opening, were

determined for conditions of submerged-orifice and free-weir flow.

A comparison of the rating discharges to the hydraulic-model rating

discharges is given for submerged orifice flow for the tainter and roller

gates.

Page 10: By Albert J. Heinitz - USGS

INTRODUCTION

The present navigation system on the Upper Mississipppi River between St.

Paul, Minnesota, and St. Louis, Missouri, was initiated in 1930 when Congress

passed the River and Harbor Act authorizing funds for its development. This

legislation provided for a navigation channel at least 9 feet deep and 400

feet wide, to be established by constructing 4 series of locks and dams, andt

maintained by channel dredging. The dams create a series of "steps" which

allow towboats or other river vessels to travel upstream or downstream. Each

dam controls the level of its pool and the locks lift or lower vessels from

one pool to the next. Lock and Dam 14 was placed in operation June 14, 1939.

This is the second in a series of reports relating to discharge ratings

and hydraulic characteristics of the control ( 5ates at locks and dams on the

Mississippi river. The report for Lock and Dam

1985) preceded this report. The discharge ratings for Locks and Dams 11, 14

and 16 were done concurrently. During the course of the studies, it was

observed that the hydraulic characteristics of

14 had some similarity. For this reason,

coefficients for the Dam 11 roller gates were

rating development in this study.

11 at Dubuque, Iowa, (Heinitz,

the roller gates at Dams 11 and

the submerged orifice flow

used to corroborate the Dam 14

Page 11: By Albert J. Heinitz - USGS

Purpose and Scope

Central to the efficient operation of the navigation system is the

availability of reliable discharge ratings for the flow control structures.

The purpose of this report is to describe the results of a study to develope

discharge ratings for the control gates at Lock and Dam 14. The ratings were

developed by using the results of current-meter discharge measurements, made

in the forebays of the control gate structures, to verify and evaluate the

discharge coefficients for the theoretical discharge equations. Discharge

ratings (U.S. Army Corps of Engineers, 1940) originally developed from

laboratory tests on hydraulic models of the gates had never been verified with

field data.

The scope of the work covered in this report includes results of current-

meter discharge measurements, methodology for computing tainter gate openings,

development of discharge coefficients and equations of discharge, definition

of rating tables of discharge for submerged orifice flow, comparison of

submerged orifice flow discharges to hydraulic-model rating discharges, and a

comparison of discharges computed from methods described in this study to

those listed in the U.S. Army Corps of Engineers gate operation schedule for

Lock and Dam 14.

Acknowledgements

This project was completed in cooperation with the U.S. Army Corps of

Engineers (U.S.C.E.). Personnel from the U.S.C.E. assisted in making current-

meter discharge measurements at the dam. Special acknowledgement is given to

the U.S.C.E. Lockmaster for arranging to have the gates adjusted as needed

for the measurements.

Page 12: By Albert J. Heinitz - USGS

LOCATION OF STUDY AREA

Lock and Dam 14, located at Le Claire, Iowa, is a unit of the Inland

Waterway Navigation System of the Upper Mississippi River Basin. Figure 1

shows a general map of the system within the 'took Island District (U.S. Army

Corps of Engineers, 1980, plate 1).

FLOW CONTROLS

Three types of flow controls are present or the structures of Lock and Dam

14. These are tainter gates, roller gates am the navigation lock. Detailed

theoretical as well as physical descriptions of these flow control structures

are beyond the scope of this report, and therefore are not included. Readers

interested in this subject are referred to Davis and Sorensen (1952), Rouse

(1949), Creager and Justin (1950), and King and Brater (1954). Table 1

summarizes the hydraulic conditions that define each regime of flow and the

corresponding generalized steady-state disc large equations. An important

parameter common to all types of flow control is the discharge coefficient,

which is discussed in the following paragraph.

The discharge coefficients (C) are functions of various independent

hydraulic control variables, of which the most significant are: the static

headwater head (h-), the static tailwater h^ad (h_), and the gate opening

(h ). A discharge coefficient is defined as (the ratio of measured dischargeO

(Q) to theoretical discharge (ASCE, 1962] i. Discharge coefficients are

determined by measuring discharge during conditions when the hydraulic control

variables are known and fixed. This procedure, referred to as calibration, may

be performed on a hydraulic model under controlled laboratory conditions or in

the field at the dam.

Page 13: By Albert J. Heinitz - USGS

DAM NO. 10(GUTTENBERG.I

DAM NO. II(DUBUQUE.IA)

WISCONSIN

ILLINOIS

DAM NO. 12(BELLEVUE, IA)

DAM NO. 13(FULTON, IL)

DAM NO. 14(LE CLAIRE, IA)

DAM NO. 15ROCK ISLAND.IL)

PROJECT LOCATION

DAM NO. 16(MUSCATINE.IA)

DAM NO. 17(NEW

DAM NO. 18(GLADSTONE, IL)

MISSOURI

DAM NO. 19(KEOKUK.IA)

DAM NO. 20(CANTON, MO)

DAM NO. 21(QUINCY, IL)

NORTH

10 20 30 MILES

10 20 30 KILOMETERS

DAM NO. 22(SAVERTON.MO)

Figure 1.--Inland Waterway Navigation System of the Upper Mississippi River Basin (modified from USCE, 1980, plate 1).

Page 14: By Albert J. Heinitz - USGS

Table

1. Flow co

ntro

ls and

their

respective hydraulic equations

Flow

control

Tainter

and

Roller

gates

Fixed

Spillway*

Flow regimes

possible

Free-orifice

Submerged orifice

Free weir

Submerged weir

Free weir

Submerged weir

Hydraulic

conditions

necessary

h <^0.67 h.

and h~<^h

g 1

J a

h0<"0.67 h, and

h-a J^ h

"

1

J-*-"

gr o

h ^0.67 h, and

h3/h,<;o.6

o

>*>x^

- ^~ 0.67 h^

and h~/h*.^Q.6

h3s

/hls<:0

-6

h3s/his^0.6

Equations

Q =

Cfh

B(2g h^

0-5]

Q =

C fh

3 B(2gAh)0-5j

Q = Cw^l

1'5]

"

Cw ^s^l

1'5]

Qg .

C fB^^

1-5]

L

_

% '

Csw Csw

s[B

shls

1-5

J

Equation

number

(1)

(2)

(3)

(A)

(5)

(6)

iocks

Ah>0

- NA Ah/At

(7)

* Same fo

r flow over gate cr

est with gate in

submerged position

The

brac

kete

d po

rtio

ns o

f eq

uati

ons

1 th

roug

h 6

repr

esen

t th

e th

eore

tica

l expression

for

disc

harg

e through

a gate B

units

in

widt

h.

The

inde

pend

ent

hydr

auli

c co

ntro

l variables

are

stat

ic h

eadwater h

ead

(hn)

, st

atic

tailwater

head

(h

^),

and

gate

opening

(h ).

Th

e va

riab

le,

Ah,

repr

esen

ts

the

difference b

etwe

en

the

headwater

and

tailwater

heads

and At,

repr

esen

ts a

tim

e interval.

N is

the

num

ber

of

lockages a

nd A i

s the

area

or

widt

h ti

mes

leng

th of th

e Lock.

The

grav

itat

iona

l constant,

g,

is

equa

l to

32

.2 f

t/s

2.

Heao

Vate

r and

tail

wate

r heads

are

the

vert

ical

dis

tanc

es f

rom

the

gate s

ill

or sp

illw

ay crest

to u

pstream

and

down

stre

am p

ool

elev

atio

ns,

respectively.

The

crit

eria

used

to s

epar

ate

orifice

flow f

rom we

ir f

low

is b

ased

on

the

fact

th

at

crit

ical

depth

of

flow

in

a rectangular

chan

nel

is e

qual

to t

wo-t

hird

s of t

he t

otal

head

in t

he a

ppro

ach

section.

As t

he g

ate

open

ing

is increased

above

crit

ical

dep

th,

the ga

te no

long

er a

cts

as a

contr

ol of d

ischarge.

Page 15: By Albert J. Heinitz - USGS

Tainter and roller gates are the only controls for which data are evaluated in

this report. Flow through the locks can be computed by multiplying the volume

of water contained in the lock times the number of lockages during a fixed

period of time.

Types of Flow at Dam 14 Control Gates

Submerged orifice flow predominates when the control gates at Dam 14 are

in operation (U.S. Army Corps of Engineers, 1980, plate 29). Free orifice

flow would very rarely occur at a low-head navigation-type structure as found

on Dam 14 and would not occur at the dam under normal operating conditions.

Calibration requires the development of a relation between the discharge

coefficient, C , in equation 2 and the gate submergence ratio, tu/h .

Free weir flow at the Dam 14 roller gates would occur primarily with the

gates in a submerged condition with flow over the crests of the gates.

Calibration of these gates requires the definition of the relation between the

discharge coefficient, C , in equation 5 and the headwater, h , over the

gate crest. The gates are operated in the submerged position in the winter

when there is no commercial navigation and the dam is out of operation.

Submerged weir flow could occur with the roller gates in a submerged condition

at a time of high flow in the river. However, the gates would normally be

raised above the water surface before submerged weir flow would occur over the

gate crests. The tainter gates are non-submergible, therefore, flow would not

occur over the gate crests. Submerged weir flow would also occur over the

tainter and roller gate sills with the gates raised above the water surface

when the dam is out of operation. This type flow is not evaluated in this

report.

Page 16: By Albert J. Heinitz - USGS

DAM OPERATION

gatesLock and Dam 14 contains 13 tainter

controlling the pool elevation upstream from

gates, located adjacent to the lock, are separated

tainter gates by the 4 roller gates, which arc;

(fig. 2). Sectional views of the tainter and

figure 3.

and 4 roller gates for

the dam. Four of the tainter

from the remainder of the

situated at about mid-channel

roller gates are shown in

The tainter gates are of the non-submergible type and close on the curved

steel channels embedded in the concrete sills. Each gate is 60 feet wide and

operates between piers with 60 feet clear openings.

The roller gates are of the submergible

submergence. Each gate is 20 feet high and 100

piers with 100 feet clear openings.

type, capable of 8 feet of

feet wide and operates between

Operation of the control gates for maintaining the pool elevation is based

on a study (U.S. Army Corps of Engineers, 1980) conducted to determine the

optimum use of the dam for river flowage, conservation interests and towboat

service. Operation "Plan A" (U.S. Army Corps of Engineers, 1980, plate 29) was

adopted and put into use on April 17, 1940 and remains in effect. "Plan A"

allows the high water levels to recede naturally until the authorized pool

elevation for lower flows is reached.

Dam 14 is a run-of-the-river dam and cannct store water for flood control

purposes. The pool is maintained between stagas 14.5 and 15.0 feet. When the

river is rising and the tailwater stage reaches 12.6 feet, the tainter and

roller gates are raised above the water surface. During flood periods, the

gates are raised out of the water allowing run-of-the-river flow to occur.

8

Page 17: By Albert J. Heinitz - USGS

600 FEET

EARTH DIKE

Figure 2.--Location of tainter and roller gates at Lock and Dam 14 on the Mississippi River (from USCE, 1980, plate 2).

Page 18: By Albert J. Heinitz - USGS

TAINTER GATE-

ROLLER GATE -SECTIONAL VIEW

Figure 3.--Sectional views of tainter and roller gates on Mississippi River Lock and Dam 14 (modified from USCE, 1980, plates 5 and 6)

10

Page 19: By Albert J. Heinitz - USGS

During winter, when there is no commercial navigation and the pools become ice

covered, the roller gates at Dam 14 are placed in the submerged position. The

tainter gates are operated the same as in summer with submerged orifice flow.

The pool is maintained within the winter operating limits of 13.9 to 14.9 feet

stage.

DISCHARGE AND STAGE MEASUREMENTS

The tainter and roller gates are built with a roadway over the structures

giving access to the forebays with standard current-meter measuring equipment.

The discharge measurements were made from the upstream edge of the roadway

which is approximately 22 feet upstream from the downstream edge of the

tainter gate sills and approximately 27 feet upstream from the roller gates.

The distance of the measuring equipment from the orifice and control structure

appeared to be adequate to allow measurements of good quality to be made. Some

vertical velocity curves were taken to verify the standard 0.2 and 0.8 method

of velocity observation. The measurements were made with equipment normally

used for measuring large streams; velocity was measured using a type AA

current meter suspended with Columbus-type sounding weights (50-150 pound)

from a collapsible crane (Rantz and others, 1982).

The concurrent pool and tailwater stages for the measurements were

obtained from the gages in the operations building. The headwater (h ) and

tailwater (h_) referenced to the sill are obtained by adding 5.08 feet to the

gage readings. The stages can be referenced to mean sea level elevation by

adding the zero gage datum, 557.08 feet (1912 adjustment), to the stages. The

gate-opening settings for the tainter gates were read from the staff-indicator

gages on the tainter gates and those for the roller gates were read from the

shaft indicator marks on the operating machinery.

11

Page 20: By Albert J. Heinitz - USGS

A total of 43 measurements of discharge ranging from 738 to 20,800 cubic

feet per second in a gate were made in the forebays of the roller and tainter

gate structures of Lock and Dam 14. Discharge coefficients for all the gates

of the same design could be developed from ipeasurements on a single gate.

However, to insure greater accuracy because of the fluctuations of the pool

and tailwater during the measurements and to account for variations in

entrance and exit conditions, several gates were selected for calibration.

Discharge through each of the gate bays was measured at least once for

submerged orifice flow. Only roller gate no. 7 was measured with the gates in

a free weir flow position. The results of thjese measurements are listed in

table 2.

Leakage, which is common to submergible jjates because of the clearance

provided between the gate and sill for lowering the gates, was not separately

determined. The flow attributable to leakage is included in the discharge

measurements.

Discharge measurements made at the Lock and Dam 11 roller gates were used

to corroborate the data for the Lock and Dam 14 roller gates in defining the

submerged-orifice discharge rating because the gates are the same type of

structure and share the same hydraulic-model discharge rating.

12

Page 21: By Albert J. Heinitz - USGS

Table 2 - Summary of current-meter discharge measurements and hydraulic control data for control gates at Mississippi River Lock and Dam 14.

Gate Pool I/ T/W 2/number Date stage stage

in feet in feet

1

2

333333

4

5

66666

777777

8

9

10

111111111111

12

13

14141414

15151515

16

1717

I/2/3/

bsw

09-13-83 14.96 4.94

09-13-83 14.96 4.94

09-13-83 14.96 4.9409-28-83 14.96 6.5009-28-83 14.96 6.4905-14-84 14.02 9.5505-14-84 14.02 9.5505-14-84 14.02 9.55

09-13-83 14.96 4.94

09-13-83 14.98 4.90

09-13-83 15.00 4.8809-28-83 14.96 6.5205-14-84 14.02 9.5505-14-84 14.02 9.5505-14-84 14.02 9.55

09-13-83 15.02 4.7211-08-83 14.95 5.0511-08-83 14.95 5.0511-08-83 14.95 5.0511-08-83 14.95 5.0511-08-83 14.95 5.05

09-13-83 15.02 4.70

09-13-83 14.98 4.94

09-13-83 14.98 4.94

09-13-83 15.02 4.7809-28-83 14.95 6.5009-28-83 14.96 6.5105-14-84 14.02 9.5505-14-84 14.02 9.5505-14-84 14.02 9.55

09-13-83 15.02 4.78

09-13-83 15.02 4.72

09-12-83 14.60 4.5705-14-84 14.02 9.5505-14-84 14.02 9.5505-14-84 14.02 9.55

09-12-83 14.60 4.5709-14-83 14.94 4.9209-28-83 14.95 6.4909-28-83 14.96 6.52

09-12-83 14.60 4.57

09-12-83 14.60 4.5709-13-83 14.95 4.94

1^ = Pool stage +5.08 feet.h3 = Tailwater (T/W) stage + 5.SO designates submerged-orificeFW designates free-weir flow.

Gagereading

G in feet

1.50

2.00

1.503.004.006.008.009.00

1.50

2.10

2.604.507.008.509.50

2.00l.OOs2.00s4.00s6.00s7.00s

2.00

1.00

1.00

1.003.004.006.008.009.00

1.00

1.00

1.006.008.009.00

1.002.003.024.00

1.00

0.501.50

08 feet.flow.

Gateopening

in

1

1

123578

1

12467

1

0

023579

0

1

0578

0123

0

01

?eet

.35

.83

.26

.84

.80

.78

.77

.79

.46

.20b

.20b

.20b

.20b

.20b

.01

.94

.95

.98

.92

.97

.97

.09

.95

.13

.96

.95

.93

.93

.99

.94

.99

.91

.83

.39

.36

Dis­charge

in ftVs

2

2

134479

2

3

477

1320

312456

3

1

1

134479

1

1

1589

1245

1

1

,060

,630

,720,520,820,740,500,580

,000

,930

,670,040,520,300,800

,460,610,100,110,990,930

,400

,510

,460

,430,610,970,760,110,210

,440

,650

,410,470,140,840

,500,670,000,140

,290

738,910

Deviationfrom

rating in percent

+ 4

+ 0

- 6- 3+ 0- 9+ 9+24

- 5

+ 9

+ 5+ 0- 5

0+ 2

0+40

0+ 2+ 0+ 0

- 1

+ 0

+ 3

0- 5+ 1-11+ 1+15

+ 0

- 2

- 1+ 2+16+25

+ 2- 3+ 4+ 4

+ 3

+19- 3

.6

.8

.5

.6

.8

.2

.2

.4

.7

.8

.2

.3

.4

.5

.0

.0

.7

.3

.5

.7

.5

.2

.0

.5

.1

.8

.7

.4

.4

.1

.3

.8

.0

.3

.7

.7

.2

.4

.5

3 9

7.42

5.48

7.954.083.042.531.881.66

6.86

4.75

3.832.582.091.721.54

4.90

4.89

9.92

10.66

10.383.892.962.451.841.61

10.38

8.67

10.052.461.841.64

9.755.153.872.97

11.63

24.747.37

C9S

0.135

0.172

0.1120.2170.2980.3190.5040.644

0.131

0.155

0.1840.2600.3030.5360.839

0.13712.24w6.43w4.78w3.88w3.59w

0.135

0.099

0.096

0.0940.2230.3070.3200.4780.619

0.095

0.109

0.0960.3670.5470.661

0.1020.1750.2470.317

0.088

0.0500.125

Flow 3/regime

SO

SO

SOSOSOSOSOSO

so

so

sososososo

soFWFWFWFWFW

SO

SO

SO

SOSOSOSOsoso

so

so

sosososo

sosososo

so

soso

Computed headwater, h, , over gate crest.Gate in submerged positionCoefficient, C , for free-weir flow.

13

Page 22: By Albert J. Heinitz - USGS

TAINTER GATE FLOW

Computation of Gate Opening

The gate opening, h , is the most important variable in calibrating theo

flow through tainter gates. In most cases the ,gate opening cannot be measured

directly in the field during operation of the

opening is computed indirectly using pertinent geometric properties of the

gates and direct measurements of the elevation of a selected reference point

on each gate. Dimensions of gate structure members that can not be measured on

the gate are obtained from the construction plans. These include the gate

radius, R, and the included angle, 8, of the gate structure (fig. 4).

structure. Therefore, the gate

The reference point (R.P.) established for [computing the gate opening, h ,o

for the tainter gates on Dam 14 is the top of

guide plate on the gate arm (fig. 4). The bolt

a slotted bolt head holding a

selected, of four bolts, is the

one closest to the pier and to the trunnion and is 18.00 feet from the

trunnion centerline. The R.P. is the same for all the gates except for gate 1

where a chiseled arrow was set on the left (as viewed facing downstream) gate

arm and gate 17 where a chiseled arrow was s^t on the right gate arm. These

R.P.'s were set 18.00 feet from the trunnion centerline. The guide plates on

gates 1 and 17 were not accessible for determining elevations. Elevations of

the R.P.'s were determined by levels from established benchmarks on the piers

between the gates (U.S. Army Corps of Engineers, 1939). The vertical gate

opening, h , is computed from the equation:O

h = 22.00 - 27.531 sin(40.622 + 8

where

<(> = sin" 1 [(574.00 - R.P. elev. )/18.00]

The terms in the equation are graphically displayed in figure 4.

14

(8)

Page 23: By Albert J. Heinitz - USGS

TR

UN

NIO

N

hg =

22.0

0'-

27.5

3l'

sin

(4

0.6

22°+

(|)u

)

^

. .1

/

574.0

0' -

R.R

e

lev

ati

on

N

wh

ere

(p

., =

sin

' ;

\ 18.0

0

/

NO

T

TO

S

CA

LE

Figure 4.

Details of tainter gates at Mississippi River Lock an

d Dam 14.

Page 24: By Albert J. Heinitz - USGS

The average gate opening (h ) computed forO

5 gates in the closed (h = 0)O

position prior to calibration of the included angle was 0.19 foot with

variations from 0.17 to 0.21 foot. The relation between the "true" gate

opening (h ) and the gage indicator readings for non-submergible gates can beO

calibrated by closing the gate (h = 0) and computing the included angle ofc>

the gate structure using the R.P. elevatior. of the gates in the closed

position. The average included angle (8) competed for the 5 gates was 40.622

degrees (fig. 4). The deviation of h for these; 5 gates is +/- 0.02 foot.O

The average adjusted gate opening (h ), with the gage indicator settingsO

at 1.00 foot for all the tainter gates, was 0.93 foot with variations from

0.76 to 1.13 feet. These differences can be attributed primarily to error in

the gage indicator settings and to the variance of the seals on the bottom

edge of the gates. Corrections for the individual gage indicators (e) and the

relation of the gate openings (h ) at the 1.00 foot gage indicator settingsc>

are shown in figure 5. Also shown is the discharge for each of the tainter

gates, these range from 1,140 to 1,650 cubic feet per second.

A gage indicator error of 0.10 foot will give about a 10 percent deviation

in discharge from the rating discharge at the 1.00 foot gage setting. This

deviation from the rating decreases at higher

at the 2.00 feet gage setting and 2.5 percent

The deviation of discharge from the rating dis

gage settings (about 4 percent

at the 4.00 feet gage setting),

charge for the individual gates

could be minimized by adjusting the gage indicators to more nearly reflect the

computed gate opening, h .O

16

Page 25: By Albert J. Heinitz - USGS

o IT

I

2-5

-

to

n O

*£.<

&-*

-o' "

"*"< >

-o<Q

o Q

-t

- <S

3<

* o

<D - T

"^

D

O

r-9

:5O

O

*/»

(DO

-* c

o O

O

"^

D O o> CO

GAT

E O

PE

NIN

G,

hg,

IN R

ELA

TIO

N T

O 1

.0FO

OT

GA

GE

RE

AD

ING

p

o

p

--

^

CQ

ID

0

L*

i

O4

o _

CO -

GA

GE

IND

ICA

TOR

C

OR

RE

CTI

ON

ro 1*4 CD

O (n

(e)

-0.1

5

-0.1

7

-0.2

4

-0.0

6

+0.

01

-0.0

6

-0.0

5

-0.0

5

+0.1

3

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4

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7

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1

ME

AS

UR

ED

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CH

AR

GE

IN R

ELA

TIO

N T

O1,

390

FT3/

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ATI

NG

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CH

AR

GE

AT

1.0

FOO

T G

AG

E R

EA

DIN

G

_

N>

c*

-is*

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^j

0000000

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o

o

o

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TO

CM

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i

Page 26: By Albert J. Heinitz - USGS

Submerged Orifice Flow Coefficients

Discharge coefficients for submerged orifice flow were computed by solving

equation (2) in table 1 for C using the results of the dischargegs

measurements (table 2) that were made with the gates in submerged orifice flow

conditions. The flow coefficients, C , are Listed in table 2 and a graph8s

defining the relationship of C to the orifice submergence ratio is shown in8s

figure 6. The resulting equation, relating the

the gate submergence ratio, h_/h , is:

discharge coefficient, C , to8s

Cgs = °' 83-0.93 (9)

The flow coefficient, C , at submergence ratios less than about 1.9 are8s

greater than those extrapolated from the curve

that a new coefficient relation may exist in this range. This trend was also

noted by Collins (1977). Discharges must be relatively high with the gates

open 8 feet or greater before submergence ratios of less than 1.9 will occur

(USCE, 1980, plate 29). This condition will ocjcur about 3 percent of the time

(USCE, 1980, plate 19), such as on the rise of a flood peak before the gates

relation (fig. 6) and indicates

are raised above the water surface and on the

the gates have been lowered back into the water.

recession of a flood peak after

18

Page 27: By Albert J. Heinitz - USGS

C 3 a> CO c

sf

</>

«t>(A

-,

*r o

H-

Q

<&

v£>

D

-*»

CL rr

t o 6 -A IB. Q

O b

SU

BM

ER

GE

D O

RIF

ICE

FLO

W C

OE

FFIC

IEN

T, C

gs

Page 28: By Albert J. Heinitz - USGS

Submerged Orifice Discharge Equation

An equation for computing discharge for submerged orifice flow in

individual tainter gate bays was developed using the submerged orifice

equation (2) and substituting the above equation (9) for the discharge

coefficient, C . The resulting equation relating the discharge (Q) to the8s I

orifice submergence ratio (h_/h ) and the static headwater (h- - 1O is:J 2 i J

Q = 400 h (h /h )"°' 93 (h j j g i

0.5(10)

where h = gage indicator reading + the individual gage indicator correctionO

(e) shown in figure 5 (the average correction, e, for all the tainter gage

indicators is -0.07 foot), h_ is the tailwater gage reading plus 5.08 feet and

is the difference between the pool and

Figure 7 shows the relation of the current-meter discharge measurements

made at the tainter gates on September 12-13,

defined by equation (10).

tailwater gage readings.

28, 1983, to the discharge curve

20

Page 29: By Albert J. Heinitz - USGS

5.0

LJ

L_ z a> .c *s

O z LJ a.

O LJ

£

O a:

4.0

3.0 2.0

1.0

Dis

charg

e m

ea

sure

me

nts

:

O S

epte

mber

12

-13

, 19

83

D S

epte

mber

28,

1983

x-6

_*

^f*/ 6

7^

&

(

^-^

ex^ N

^

3

e

A _

^ n

r\

uQ

*

*uu

it

\ w

here

h, o

/here

h, 3

X ID = 2

0.0

=

11.

6

1Q

R

.)-«

'

=

9.8

and h

g =

ga

ge

re

ad

ing

V

h, -

h_

3

- 0

.07

fo

ot.

0.0

2345

DIS

CH

AR

GE

(Q

), I

N T

HO

US

AN

DS

OF

CU

BIC

FE

ET

PER

SE

CO

ND

Fig

ure

7. - C

om

pariso

n o

f cu

rre

nt-

me

ter

dis

charg

e m

easure

ments

of

Septe

mber

12

-13

, 2

8,

1983

, to

ra

tin

g c

urv

es

for

tain

ter

gate

s a

t M

issi

ssip

pi

Riv

er

Lock

an

d D

am

14.

Page 30: By Albert J. Heinitz - USGS

ROLLER GATE FLOW

The roller gates at Dams 11 and 14 are the same type of structure and have

the same hydraulic-model rating relationship. The development of discharge

ratings at both dams are being done concurrently, therefore, enabling use of

data from both dams in developing discharge ratings for the gates at each of

the dams.

Gate Opening

The gate opening indicator marks for the roller gates are on an integral

part of the operating machinery of the gate. These indicators presumably give

a fairly accurate reading of the gate opening. A method for measuring the

actual gate openings was not developed.i

Submerged Orifice Flow Coefficient

Discharge coefficients for submerged orifice flow for Dams 11 and 14 were

used to define the relation with the orifice submergence ratio, h_/h . The

coefficients were computed by solving equation (2) in table 1 for C usinggs

the results of the discharge measurements (table 2) that were made under

submerged orifice flow conditions.

The relation of the submerged orifice flow coefficient, C , to thegs

orifice submergence ratio, h^/h , for the rolljer gates on Dams 11 and 14 are3' g

shown in figure 8. (Discharge coefficients for

at Lock and Dam 13 are also shown in figure 8)

occurs at a point when the gate is open 7 feet

measurements subsequently made

, The break in the relationship

or greater and the submergence

ratio is less than 2.4 for the Dam 11 roller gates and less than 1.9 for the

Dam 14 roller gates. The break in the relationship apparently occurs when

22

Page 31: By Albert J. Heinitz - USGS

SUBM

ERG

ED O

RIF

ICE

FLO

W C

OEF

FIC

IEN

T, C

,< c

O

oo-i

.

3 i

<o 5

Z

**,

2V

I <

g

00.

ii Ul *

!2.o

Ul

*-

^ 0

*0

O §£

.

3< U

o PI

CO c CD £

m 50 o O m

CM IT

<O

Page 32: By Albert J. Heinitz - USGS

control of flow of the roller gate transfers from the lower apron (appendage

to the drum) on the roller to the drum of the gate structure. The control

positions of the roller gate are illustrated

gate opening increases significantly when control transfers from the apron to

the drum when the gate is opened more than 7

where the control changes has not been defined

.0 feet. The exact gate opening

The resulting equation, relating the discharge coefficient, C , to the8s

in figure 9 and show that the

gate submergence ratio, h /h , for the rollei

less than 7 feet is defined by the equation:

gates when the gates are open

C = 0.67 (h./h ) gs 3' g'

-1.00(11)

As noted by Collins (1977) and described by King and Brater (1954), many

structures calibrated by the procedures outlined above are found to be

independent or nearly independent of submergence. If the coefficient is

independent of the submergence, the slope of the straight line relation will

be -1.00 as found in equation 11. When substituted for the coefficient in the

submerged orifice flow equation (2), the equation reduces to the free-orifice

equation (1). The average of the coefficients computed for the roller gates

at dams 11 and 14 using the free orifice; equation (1) was 0.67. This

coefficient is in total agreement with those in King and Brater (1954, table

26) for rectangular orifices with partially suppressed contraction.

For conditions when the gates are opeki 7 feet or greater and the

submergence ratio is less than 1.9, the discharge coefficient, C , for thegs

Dam 14 roller gates is defined by the equation:

Cgs =4.20 (h3 /hg ) -3.79 (12)

24

Page 33: By Albert J. Heinitz - USGS

NORMAL POOL NORMAL POOL NORMAL POOL

'. >".' ' ':"»''' -. * . ;* ' ':&!.'

GATE CREST 12 FT. GATE CREST 14 FT. GATE CREST 16 FT.

NORMAL POOL NORMAL POOL NORMAL POOL

GATE CREST 18 FT. GATE CREST 20 FT. GATE OPEN 3 FT.

NORMAL POOL NORMAL POOL NORMAL POOL

GATE OPEN 5 FT. GATE OPEN 7 FT. GATE OPEN 10 FT.

_\_ \/ NORMAL POOL NORMAL POOL

GATE OPEN 14 FT. GATE OPEN 18 FT.

Figure 9 Positions of roller gates for selected openings(Modified from USCE, 1940, Figure 35).

25

Page 34: By Albert J. Heinitz - USGS

The computed coefficients and the results of the measurements made in the

roller gates at Dam 14 are listed in table 2.

Submerged Orifice Discharge Equation

An equation for computing discharge for

roller gates are open less than 7.0 feet was d

equation (2) and substituting equation 11 for

The resulting equation relating the discharge

the static headwater (h. - 1O is:

submerged orifice flow when the

eveloped using the orifice flow

the discharge coefficient, C

(Q) to the gate opening (h ) andO

Q = 537 hg

- h3 )0.5

(13)

where h.. - h_ is the difference between the pool and tailwater gage readings.

This equation is also applicable to submerged orifice flow in the roller gates

at Lock and Dam 11 with the gates open less th£in 7.0 feet.

less

An equation for computing discharge for orifice flow when the roller gates

than 1.9 feet was developed

using the orifice flow equation (2) and substituting equation (12) for the

, relating the discharge

are open 7.0 feet or greater and tu/h is ^ 8

discharge coefficient, C . The resultingSs

(Q) to the tailwater (h ), submergence ratio

(h l - h ) is:

equation,

(h_/h ) and the static headwater

Q = 3,370 (h3/hg)" 3 ' 79 (h] 0.5 (14)

26

Page 35: By Albert J. Heinitz - USGS

where h is the tailwater gage reading plus 5.08 feet, h is the gage reading

and h - h is the difference between the pool and tailwater gage readings. If

the Dam 14 roller gates are operated within the range of allowable safe gate

openings (USCE,1980, plate 31), the discharges defined by equation 14 would

not become effective (table 5). The allowable safe gate openings for the Dam

14 roller gates are established at a much lower discharge than those for Dam

11.

Free Weir Flow Coefficient

Discharge coefficients for free weir flow for the roller gates in a

submerged position were computed by solving equation (5) in table 1 for C

using the results of the discharge measurements (table 2) that were made with

the gates in a submerged position. A graph showing the relationship of C to

the headwater (h... ) over the gate crest is shown in figure 10. Discharge

coefficient-headwater relations were originally developed in corroboration

with the Lock and Dam 11 coefficients. However, the coefficient-headwater

relation for Lock and Dam 14 is published separately in this report and is

modified slightly from that shown in the Lock and Dam 11 report. The

discharges computed by either development are the same, however, the relation

shown in figure 10 of this report defines the coefficients more accurately for

the Lock and Dam 14 roller gates.

27

Page 36: By Albert J. Heinitz - USGS

The resulting equation, relating the dischargB coefficient to the headwater

(hls ) is:

C = 9.6 (h, ) sw Is

-0.50

where h.. = Gage reading + 0.17 + (pool stage - 14.92)

The correction to the gage readings was derived from the observed gage reading

at the point of zero flow.

100

en O

2LJ

O

LJO

3te LJ

LJ LJ

10

(15)

Note

C

h 1s

'SW =

= Go

9.e

"" -T"l

ge reading +

> 0"Ms

>- 0.

x

5C

*-

):

,.

0.17 f (pool stage

O

s^

X__

^N^

HEADWATER (h ls )

TQ^^^

- 14.92)

^NT ^9t

, IN FEET

Figure 10. - Free weir flow coefficient-headwater relation for roller gates in submerged position for Mississippi River Lock and Dam 14.

28

Page 37: By Albert J. Heinitz - USGS

Free Weir Discharge Equation

An equation for computing discharge for free weir flow for the roller

gates in a submerged position was developed using the free weir flow equation

(5) and substituting the above equation (15) for the discharge coefficient,

C . The resulting equation, graphically illustrated in figure 11, relating

the discharge (Q ) to the headwater (h ) over the gate crest is:o J_ o

Q = 960 h, s Is(16)

where h.. is as defined for equation 15 above. The discharge measurements

made at Locks and Dams 11, 12 and 13 are also shown in figure 11.

10

Note:

(

[h

[

I

^

hj s = Gage reading

MEASUREMENTS) Lock and Dam 14

I] Lock and Dam 11

3 Lock and Dam 12

$ Lock and Dam 13

S

V^

vfsL- mr^-^

+ 0.

^

17 -H

DxX

(Dam 14 pool stage - 14.

^tB'

\

^

-Qs

f

^^

= 96 Oh ls

92)

1^x^

o acLJ2CD

oX

UJu.

I'o

1234567DISCHARGE (Q), IN THOUSANDS OF CUBIC FEET PER SECOND

Figure 11. - Discharge-headwater relation for free weir flow for roller gates in submerged position, Mississippi River Lock and Dam 14.

29

Page 38: By Albert J. Heinitz - USGS

DISCHARGE EQUATIONS AND RATINGS

The discharge equations applicable to the control gates when Dam 14 is in

operation have been compiled and listed in tab^.e 3.

Rating tables for both the tainter and roll.er gates were developed for the

predominant flow regime of submerged-orifice flow when the Dam is in

operation. These ratings, tables 4 and 5, list

at 1 foot increments and gate openings at

applicable only with the upstream pool stage at 14.92 feet (h- = 20.00 feet).

Discharges for any other headwater, tailwater a

discharges for tailwater stages

0.5 foot increments and are

and gate opening relationships

encountered can easily be computed using the japplicable equations in table 3

with a small programable computer.

Discharge rating curves for submerged Orifice flow at selected gate

openings (h ) for the tainter and roller gatesO

, prepared from laboratory tests

on hydraulic models of gates are shown in figures 12 and 13. Corresponding

discharge rating curves defined by the methcds outlined in this report are

shown for comparison. Discharges defined by the 2 methods for the tainter

gates are within about 20 percent. Discharges defined by the 2 methods for

the roller gates are generally within about ij) percent for gate openings of 6

feet or less. Large deviations occur between the ratings as the gates are

opened greater than 7.0 feet.

The equations in table 3 were used to compute

settings indicated in the operation schedule,

is in use for operation of Dam 14. Discharges

Plan A until the roller gate openings exceeded

discharges increased to 16 percent greater thcin

the discharges for the gate

Plan A, shown in table 6 which

generally were close to those in

7 feet at which time the

those in Plan A.

30

Page 39: By Albert J. Heinitz - USGS

Tabl

e 3.

Summary

of d

ischarge e

quations f

or control

gates

at M

ississippi R

iver

Lock

and Da

m 14.

Equation

number

Flow r

egim

eEquation o

f discharge

For

tainter

gate

flow:

(10)

Submerged

orifice

Q =

400

h3 (h3/hg

°-93

For

roll

er g

ate

flow

:

(13)

(14)

(16)

Submerged orifice

hg < 7.0

or ^ 7.0

when lyhg > 2.4

Submerged

orifice

h ^7.0 a

nd

h3/h

g < 2.4

Free wei

r*

Q =

537

- h)0.

5

Q =

3,37

0 h.

(h

o/hn

)o

j y

-3.7

9

Qs =

960 h

ls

- h)0.

5

Note

: The

approach v

elocity

head i

s in

clud

ed i

n (h

^ -

h3).

Q = Discharge, in

cubic f

eet

per

seco

nd

h-^ =

Pool s

tage

+ 5

.08

feet

h3 =

Tailwater s

tage +5.

08 f

eet

h for

tainter

gage

s = gage reading

+ gage i

ndicator correction,

e (f

ig.

5).

y (a

vera

ge e

for

all

the t

aint

er g

ates

= -

0.07 foot)

hq f

or ro

ller

gat

es =

gag

e reading

*y F

or free weir

flow o

ver

roller g

ate

cres

t: hl

g = gage reading

+ 0.

17 +

(pool

stag

e-

14.92)

Page 40: By Albert J. Heinitz - USGS

Table 4. Discharge rating table for submerg tainter gate at Mississippi River Lock and

stage of 14.92 fe

ed-orifice flow for a singleDam 14 with upstream pool

bt.

GAGE READING (feet)

.51.01.52.02.53.03.54.04.55.05.56.06.57.07.58.08.59.09.5

4.0

70414402150284035204190485055106160680074408080871093409960

1060011200

**

Tainter

5.0

67613802070273033804020466052905910653071407750836089609560

10200108001130011900

gate discharge, in stage, in feet, i 6.0 7.0 8.0

645132019702610323038404450505056406230682074007980856091309700

103001080011400

6111250187024703060364042204790535059106460702075608110865091909730

1030010800

57511801760232028803420396045005030

ftVs, for ndicated.

9.0

53410901630216026703180369041804670

5550 51606080 56506600 61307110 66107620 70908130864091509650

10200

75608030850089709440

tailwater

10.0 11.0

489100015001980245029203380383042804730517056206060649069307360779082208650

439899

13401770220026103030344038404240464050405430582062106600698073707750

12.0

380779

11601540190022702620298033303680402043604710505053805720605063906720

* Free-orifice flow conditions exist at indicated tailwater stage and gage readings.

Note: Discharges greater than those underlined may exceed those allowable for safe gate operation (USCp, 1980).

Discharges for table 4 were computed ubing equation:

(10) Q = 400 h3 (h3/hg )~°' 93 (h 1 - h 3)M

where h = gage reading + (average e = -0.07)h| = 20.00 feet (14.92 + 5.08)h = tailwater stage + 5.08 feet

32

Page 41: By Albert J. Heinitz - USGS

Table 5. Discharge rating table for submerged-orifice flow for a single roller gate at Mississippi River Lock and Dam 14 with upstream

pool stage of 14.92 feet.

GAGE READING (feet)

.51.01.52.02.53.03.54.04.55.05.56.06.57.07.58.08.59.09.5

4.0

8871770266035504440532062107100799088709760

1060011500

Roller

5.0

8461690254033804230507059206770761084609300

1010011000

gate discharge, in ftVs, for tailwater stage, in feet, indicated. 6.0 7.0 8.0 9.0 10.0 11.0

80216002410321040104810561064207220802088209620

10400

756151022703020378045305290605068007560831090709820

*14500

706141021202830353042404940565063607060777084809180

*10800*14100

6531310196026103270392045705230588065307190784084909150

*10600*13500

59611901790238029803570417047605360596065507150774083408930

*10200*12800

532106015902130266031903720425047805320585063806910744079708500

*9580*11900

12.0

459918

138018402290275032103670413045905050551059606420688073407800

*8670*10600

Note: Discharges greater than those underlined may exceed those allowable for safe gate operation (USCE, 1980, plate 32).

* Discharges computed using equation 14.

Discharges for table 5 were computed using equations:

(13) Q = 537 h (h,- h.) y -^0.5

-3.79(14) Q = 3,370 h3 (h3/hg )~°- /:'(h1 - h 3 ) 0.5

where h = gage readinghj = 20.00 feet (14.92 + 5.08) h3 = tailwater stage + 5.08 feet

33

Page 42: By Albert J. Heinitz - USGS

20

XL

O

18 16 14

\\ t \ \v -N \\

\ p

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odel

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(U

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ings

bas

ed o

n eq

uaH

on 1

0, t

ab

vher

e h,

= 2

0.00

fee

t (1

4.92

+

h3

= ta

ilwat

er s

tage

+ 5

.08

gate

ope

ning

, hg

MO

)le

3

5.08

)fe

et

e: T

he c

urv

es

ext

en

din

g b

elo

w t

his

lin

e a

re

ve

rifie

d a

nd

are

be

yon

d t

he

allo

wable

ga

openin

g f

or

safe

gate

opera

tion,

but

are

sh

ow

n f

or

com

pa

riso

n o

f th

e t

wo m

eth

oc

not

te Is.

12 10

6 8

10

12

14D

ISC

HA

RG

E,

IN T

HO

US

AN

DS

OF

CU

BIC

FEE

T PE

R S

EC

ON

D16

1820

Fig

ure

12. -

Dis

char

ge r

atin

gs

for

sub

me

rge

d o

rific

e f

low

fo

r a

sing

le t

ain

ter

gate

at

Mis

siss

ippi

Riv

erLo

ck a

nd D

am 1

4 co

mp

are

d t

o hyd

raulic

-model

ratin

gs.

Page 43: By Albert J. Heinitz - USGS

LJ

LJ

Lu.

Z JC.

o LJ X a:

Hyd

rau

lic-m

od

el

ratin

gs

(US

CE

, 19

40)

Rat

ings

base

d o

n equatio

ns

13 a

nd 1

4,

tabl

e 3

whe

re h

, =

20

.00

fe

et

(14.

92 +

5.0

8)

h3

= t

ailw

ate

r st

age +

5.0

8 f

eet

6 ga

te o

penin

g,

h

6 8

10

12

14

DIS

CH

AR

GE

, IN

TH

OU

SA

ND

S O

F C

UB

IC F

EET

PER

SE

CO

ND

Fig

ure

13

- D

isch

arg

e r

atin

gs f

or

su

bm

erg

ed

orifice f

low

fo

r a

single

ro

ller

ga

te a

t M

issi

ssip

pi

Riv

er

Lo

ck a

nd

Dam

14

co

mp

are

d t

o h

ydra

ulic

-model

ratings.

Page 44: By Albert J. Heinitz - USGS

MISSISSIPPI

RIVER

LOCK AND

DAM

14

GATE O

PERATION SCHEDULE P

LAN A FOR CO

NTRO

LLED

TAI

LWAT

ER ST

AGES

(A)

Disc

harg

e

ft»/

s

Tail-

stage

(fee

t)

Head

in

feet

Gate

Tainter

1 2

3 4

5

open

ing.

Roller

6 7

in feet,

for

89

10

gate indicated

Tainter

11

12

13

14

1516

17

ON

14,1

0023,300

28,0

0032

,500

37,200

40,7

0045

,000

49,300

54,3

0057

,200

61,8

0065,300

69,100

72,4

0076

,500

80,1

0083

,800

87,8

0091

,800

97,8

00

101,

000

104,

000

108,

000

111,

000

119,

000

130,

000

132,

000

151,000

161,000

161,

000

12,5

0022,000

27,500

32,000

37,000

41,0

0045

,500

50,0

0054

,400

57,8

00

62,300

66,300

70,0

0073,800

78.0

00

81,8

0085

,500

90,0

0094

,000

100,

500

103,

800

107,

500

111,

000

115,

000

119,

000

122,

500

126,

000

130,

000

139,

000

142,

000

4.0

4.2

4.4

4.6

4.8

5.0

5.2

5.4

5.6

5.8

6.0

6.2

6.4

6.6

6.8

7.0

7.2

7.4

7.6

7.8

8.0

8.2

8.4

8.6

8.8

9.0

9.2

9.4

9.6

9.8

10.9

10.7

10.5

10.3

10.1 9.9

9.7

9.5

9.3

9.1

8.9

8.7

8.5

8.3

8.1

7.9

7.7

7.5

7.3

7.1

6.9

6.7

6.5

6.3

6.1

5.9

5.7

5.5

5.3

5.1

0.5

0.5

0.5

0.5

0.5

0.5

0.5

0.5

1.0

1.0

1.5

1.5

1.5

1.5

1.5

1.5

2.0

2.0

2.0

2.5

2.5

2.5

2.5

2.5

3.0

3.0

3.0

3.0

3.0

4.0

0.5

1.0

1.0

1.0

1.0

1.0

1.0

1.5

2.0

2.0

2.5

2.5

3.0

3.0

3.5

3.5

4.0

4.0

4.5

4.5

5.0

5.0

5.5

5.5

6.0

6.0

7.0

7.0

8.0

8.0

0.5

1.0

1.0

1.0

1.5

1.5

1.5

2.0

2.0

2.5

2.5

2.5

3.0

3.0

3.5

3.5

4.0

4.0

4.5

4.5

5.0

5.0

5.5

6.0

6.0

6.0

7.0

7.0

8.0

9.0

0.5

1.0

1.0

1.0

1.5

1.5

2.0

2.0

2.5

2.5

2.5

3.0

3.0

3.0

3.5

3.5

4.0

4.0

4.5

5.0

5.0

5.5

5.5

6.0

6.0

6.5

7.0

7.0

8.0

9.0

0.5

1.0

1.5

1.5

2.0

2.0

2.5

3.0

3.0

3.0

3.5

3.5

4.0

4.0

4.5

4.5

5.0

5.0

5.5

6.0

6.0

6.5

6.5

7.0

7.0

8.0

8.0

9.0

9.0

9.0

0.5

1.0

1.5

2.0

2.0

2.5

3.0

3.0

3.0

3.5

3.5

4.0

4.0

4.5

4.5

5.0

5.0

5.5

5.5

6.0

6.0

6.5

6.5

7.0

8.0

8.0

8.0

9.0

9.0

9.0

0.5

1.0

1.5

2.0

2.0

2.5

3.0

3.0

3.5

3.5

3.5

4.0

4.0

4.5

4.5

5.0

5.0

5.5

5.5

6.0

6.0

6.5

6.5

7.0

7.0

8.0

8.0

9.0

9.0

9.0

0.5

1.0

1.5

2.0

2.0

2.5

3.0

3.0

3.0

3.5

3.5

4.0

4.0

4.5

4.5

5.0

5.0

5.5

5.5

6.0

6.0

6.5

6.5

7.0

7.0

8.0

8.0

8.0

9.0

9.0

0.5

1.0

1.0

1.5

1.5

1.5

2.0

2.0

2.0

2.5

2.5

2.5

3.0

3.0

3.5

3.5

4.0

4.0

4.5

5 .IF

5.0

5.5

5.5

6.0

7.0

7.0

7.0

7.0

8.0

9.0

0.5

1.0

1.0

1.5

1.5

1.5

1.5

2.0

2.0

2.5

2.5

2.5

3.0

3.0

3.5

3.5

4.0

4.0

4.5

*.5

5.0

5.0

5.5

6.0

6.0

6.0

7.0

7.0

8.0

8.0

0.5

1.0

1.0

1.0

1.5

1.5

1.5

2.0

2.0

2.0

2.5

2.5

3.0

3.0

3.5

3.5

3.5

4.0

4.5

4.5

5.0

5.0

5.5

6.0

6.0

6.0

7.0

7.0

8.0

8.0

0.5

1.0

1.0

1.0

1.5

1.5

1.5

2.0

2.0

2.0

2.5

2.5

3.0

3.0

3.0

3.5

3.5

4.0

4.0

4.5

5.0

5.0

5.5

5.5

6.0

6.0

7.0

7.0

8.0

8.0

0.5

1.0

1.0

1.0

1.5

1.5

1.5

2.0

2.0

2.0

2.5

2.5

2.5

3.0

3.0

3.5

3.5

4.0

4.0

4.5

5.0

5.0

5.5

5.5

6.0

6.0

6.5

7.0

8.0

8.0

0.5

0.5

1.0

1.0

1.5

1.5

1.5

1.5

2.0

2.0

2.5

2.5

2.5

3.0

3.0

3.5

3.5

4.0

4.0

4.5

5.0

5.0

5.5

5.5

6.0

6.0

6.0

7.0

8.0

8.0

0.5

0.5

1.0

1.0

1.0

1.5

1.5

1.5

2.0

2.0

2.0

2.5

2.5

3.0

3.0

3.5

3.5

3.5

4.0

4.5

5.0

5.0

5.5

5.5

6.0

6.0

6.0

7.0

7.5

8.0

0.5

0.5

0.5

1.0

1.0

1.5

1.5

1.5

2.0

2.0

2.0

2.5

2.5

2.5

3.0

3.0

3.5

3.5

4.0

*.5

5.0

5.0

5.5

5.5

6.0

6.0

6.0

6.5

7.0

8.0

0.5

0.5

0.5

0.5

0.5

0.5

0.5

0.5

1.0

1.0

1.5

1.5

1.5

1.5

1.5

1.5

1.5

2.0

2.0

2.0

2.0

2.5

3.0

3.0

3.0

3.0

3.0

3.0

3.0

4.0

(A)

Discharge, in

cu

bic

feet

pe

r second,

computed using

equations

in table

3.

Table

6.

Comp

aris

on of

ra

ting

discharges to

fl

ow of Lock and

Dam

14 Ga

te Op

erat

ion

Sche

dule

Pl

an A.

[Mod

ifie

d fr

om USCE,

1980

, plate

29]

Page 45: By Albert J. Heinitz - USGS

CONCLUSIONS

Current-meter discharge measurements made in the forebays of the tainter

and roller gates of Lock and Dam 14 were used to develop discharge

coefficients and equations of discharge for submerged-orifice flow for all the

gates and free-weir flow for the roller gates in a submerged position.

Methodology has been described to compute the actual gate openings of the

tainter gates. The staff-gage indicator gages for the tainter gates could be

accurately set to the true gate opening (h ) using the techniques described inO

case the gages were accidently knocked out of alignment or if the bottom seals

on the gates were changed. The deviation of the discharge from the rating

discharge for the individual gates could be minimized by adjusting the gate

indicator gages to more nearly reflect the computed gate opening, h .o

Discharge rating tables were developed for discrete combinations of

downstream pool elevations and gate openings for submerged-orifice flow which

is the predominant flow regime when the dam is in operation.

37

Page 46: By Albert J. Heinitz - USGS

SELECTED REFERENCES

ASCE, 1962, Nomenclature for Hydraulics: American Society of Civil Engineers, Manuals and Reports No. 43, 74 p.

Collins, D.L., 1977, Computation of records of streamflow atcontrol structure: U.S. Geological Survey Water-Resources Investigations 77-8, 57 p.

Creager, W.P., and Justin, J.D., 1950, Hydro-electric Handbook: New York, John Wiley.

Davis, C.V., and Sorensen, K.E., 1952, Handbook of Applied Hydraulics: McGraw-Hill Book Company.

Heinitz, A.J., Discharge Ratings For Control Gates at Missis­ sippi River Lock and Dam 11, Dubuque, Iowa: U.S. Geolo­ gical Survey Water-Resources Investigations Report 85-4105, 43 p.

King, H.W., and Brater, E.F., 1963, Handbook of hydraulics (5th ed.): New York, Mcgraw-Hill Book Company.

Rantz, S.E. and others, 1982, Measurement; and Computation ofStreamflow: Volume 1. Measurement of U.S. Geological Survey Water-Supply

House, Hunter, 1949, Engineering Hydrauli

Stage and Discharge: Paper 2175, 284 p.

cs, Iowa Institute ofHydraulic Research, State University of Iowa: New York, John Wiley.

U.S. Army Corps of Engineers,1939, Mississippi River Lock and Dam No. 14, Lock pier position data: U.S. Army Engineer District, Rock Island Corps of Engineers, Rock) Island, Illinois, 1 p.

_, 1939, Laboratory tests on hydrau stilling basins: U.S. Army Engineer Corps of Engineers, Rock Island, 111

lie models of roller gate District, Rock Island inois, 279 p.

_, 1940, Laboratory tests on hydraulic model to determine roller gate coefficients for Upper Mississippi River navigation dams: U.S. Army Engineer District, Rock Island Corps of Engineers, Rock Island, Illinois, 72 p.

_, 1940, Laboratory tests on Hydraulic model of Lock and DamNo. 11, Mississippi River, Dubuque, Iowa: U.S. ArmyEngineer District, Rock Island Corps of Engineers, Rock Island, Illinois, 111 p.

_, 1980, Upper Mississippi River ba|sin, Mississippi River-nine foot channel, Appendix 14, Master reservior regulation manual, Lock and Dam No. 14: U.S. Army Engineer District, Rock Island Corps of Engineers, Rock Island, Illinois, 79 p.

38