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Scholars' Mine Scholars' Mine
Masters Theses Student Theses and Dissertations
1965
Discharge characteristics of side weirs Discharge characteristics of side weirs
Edgar Snowden
Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses
Part of the Civil Engineering Commons
Department: Department:
Recommended Citation Recommended Citation Snowden, Edgar, "Discharge characteristics of side weirs" (1965). Masters Theses. 5334. https://scholarsmine.mst.edu/masters_theses/5334
This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected].
DISCK4RGE CHARACTERIS::rrcs OJ.11 SIDE ";,JEIRS
EDGA:2 SNO\')])EN IV
submitted to the Faculty of the
T.J?-:~_:\TERSITY ,JF MISSOT.JRI AT ROLLA
DEGR~E OF
NAS'.:2ER OF SCIEl'JCE IN CIVIL E>:GL\JEERINCx
Rolla~ JYlissour·:L
1965
APFRO"VED BY
u~ (advisor-) --~"~'":j _J_,, _Q~~
f2L£~ ~_Jti_~
ii
ABSTRACT ,
The purpose of this study is to investigate the division
of flow of Hater in a flume of rectangular cross -section l'lhen
the flume is prc,•ided with a side weir. An equation has be~:~n
derived so that the quantity of water flowing over the side
weir compared to the quantity of water flowing in the main
c:-.. annel can oe predicted. This ratio is acceptable only
"
within the ranges of heads) velocities, and weir lengths im-
posed by the geometry of the system tested.
i:..i
A CKNOvlLEDGEMENT
The a~.~--~::-lor wishes to express his deepest appreciation to
Professor V.A.C. Gevecker for his consideration, encourage
ment, interest, and helpful criticisms throughout the research
and writing phases of this study. His guidance has made this
thesis possible.
iv
TABLE OF CONTENTS
Page
ABSTRACT .......... . ii
ACKNOWLEDGEMENT ........ . iii
LIST OF ILLUSTRATIONS ... v
CHAPTER I
Introduction .. ...................................... l
CHAPTER II
Review of Literature ......... . ..... ' .. ,. ....... . 3
CHAPTER III
General Discussion of the Problem................. 11
CHAPTER IV
Test Apparatus . . . . . . . . . . ' ............ . CHAPTER V
Test Procedure.
CHAPTER VI
Test Results .... . . . . . .• . •
CHAPTER VII
Conclusions.
CHAPTER VIII
Recommendations ..... . ...................... " .... APPENDIX ..... · ..... . . . . . . . . . .......... , .. BIBLIOGRAPHY. . .............. . VITA ........................................ .
20
39
L..., •..!..
7?
78
Figure
l
2
3
4
5
6
7
8
9
10
LIST OF ILLUSTRATIONS
Test Apparatus ................................. .
\<Jare Suppressor ................................ .
Head-Measuring Gace ............................ .
Calibration Curve - 12 -inch Su.p:oressed \IJeir ..... -
Discharge -Head Curves f'or S i.dc \·J2ir-s ........... .
Flow-Length- Head Ratio Curves for Side Weirs ..
Depth-Energy-Discharge Curves .................. .
Comparison of Flows- Oblique View ............. .
Comparison of Flows- Side View ................ .
Comparison of Flows - End View· ................. .
v
Page
15
18
19
22
25
28
35
37
38
vi
Gertrude Stein lay dying. About her gathered her rriends~
the great authors and artists or her· day·. 11 ~\l:.at_. 11 she asked,
nwhat is the answer?'' After a spell of r.onc'.erous silence,
she sparkled. 11 Well ~ gentlemen~ ir no o·,1e knows the answer~
what then is the question? 11 And died.
CHAPTER I
INTRODUCTION
1
A study o:f the characteristics of :flow over side weirs
was suggested by a report on the research conference o~ the
Irrigation and =~ainage Division of the American Society of
Civil Engineers held at Logan: Utah, during March, 1964.
This is not a new subject. It is a problem dealing primarily
vli th division of flow about which little is known.
Side weirs have many applications. The research con-
ference was specifically interested in the relief of excess
flows in irrigation channels by means of side weirs when the
channels are subjected to inflow from adjacent watersheds.
Problems solved by side weirs have ranged :from the regu-
lation of :flow in diversion :flumes in Tasman~a, to· the sup-
pression o:f waves in canals in Italy, to tt-.;.:-· ;-rotection of
Hoover Dam against ovc-:etop.~:J:..ng. At t:i:1e pre.:>S.t<~:- ti:ne, the
U.S. Department c:·· ,:.gf."'j_-:;n.lture and the U. 3. ::.;,;;;::x.::<~rl'l.ent oi~
the Interior a:.~ ... c :ln\>):C.s~,·i:;ed in the feasibilj. ti •:::'' discharg-
ing excess f'lo~,r in ir·rigation channels ir.to J:";r: .... c ·; rsvines
in order to prevent the flooding of developed :2.
The research :for this paper comprised ;:; ,, -;~udy ·')f the
phenomena associated with the division of flow of water in
an open channel. The flow was divided into ti'I!C parts, that
which continued ~n the op~~ channel and that which flowed
ov~r --~ s.1d~;,. weil:',it,;,(.:tz'h~~,.:~*D~'~:t+sa't;:1on _.·a,tudied the effects ot: ~·<· .. ,) . . ,: .. :~«~,·:"'' , ... ' ·., ' , . . ·'~~:;·, ~:,~. ':·· ..
', . .<, i"(,<> ; ¢;•'.f ~. ·_,.,
2
geometry on the quantity of flow over the side weir .
•
wri~incs and experiments
·; . ... _ .. clc...-:..:-::.) .L~r·
also clouded by their varied and unwaverin~ conc:us~ons. On
one point some asree: t~e installation and location cf ~
weir give it various characteristics which require t~~t an
the Fruehling formula for flow over a sid2 weir
where
Q ·i -'""1 !.. ~ _-: '-·· .._.·
H
enC c: t~e sill.
They notice~, contrary to t~eir observatis~~.
stated that the failure of "co
~orm as desired was due to their low efficiency and that the
len;:>;ths given to tllese v.J:::::.
velocity of flow.
sur~ace had flattened out a~ ~his increase~ aep~n.
die~ r.ot occur. In explanation, tt1cy could on~y s~~~c~~
Co le::nan and S:;<:
_ .~sr ~edified to include the . ; "" ' - .. ~
the weir length req~~~ea ~o
ma~n flow to a given level~
~he ncad on tha upstream end of the weir,
the head. on the downstream end of the weir, and V is the
average ·/clocity in the main channel. By assigning values of'
··' )
!;j = 10 1 J v -- l1 1 <~2 - "-T J and.
they illustrated the inefZicie~cy of the systc~:
velocity of three feet per secondJ a weir lsngt~ oZ 86 fe~~
was required to reduce the head 3.94 feet; a velocity of
i"'i VG fer.:;t per second required a length of 114 foe"~.
equation is more striking when efficiencies are disresarded
and the original tnov.ght pursued. At what len6tl'"l of sid~o:
•qeir j_s the flow reduced to sj_ll level? :B'or t:r~e dov;nstrearn
head (yl) to be zeroJ the length of side wei~ ~~st ~e
infinite!
posed the formula
where H is the head on the downstreax end of ~~c side weir.
cr.ar ... nel.
t , l . - " . l 928 4 His repor was puc lsnea ~n -. .
of momentum and conservation of' ene::r."gy to tr1e :flow of l'lat<-'~r
over the sides of trapezoidal channel3.
ment with I-Unds 1 theory by allm>V~i..::.1.g i1i:::- c:. ·-:: ;_;i:c-1al trapezoidc..l
channel to .s.pp:c_:_;d.ch one of rectanguj_ar c:o:,:->s -=~ection. Hence,
6
the water while it is p~s~lng over ~h~ weir.
C(.;;.ssion to r:is ovm
fied Bernouilli equation,
Q Ch'H"\; 2g
v-Jhere
c 0.6
H = head on a-t upstream end. of.·
weir
decrease in velocity.
Tyler~ Carollo_,
tc
-formulas pr·e s eo_~~ t ly in use. ::::J
the c.::::.e of the Coleman-SmJ.tL rormula.
and Smi t:r~ froni further consideration~ suggesting that the
7
similitude in ad~~ting the results of their expcri~e~~~ ~o
p::c·actical use. n6
Tyler and associates lJlo-'cte:d ti1\Jil~ o~~:1: da.. t::~ aca::_~~3 t
did not agree. A larger. v~r:~~lc cocf~icient was i~dicatcd.
For a weir length of one and one-half feet, t~GY ~ou~d t~c
be expressed as a f'unctj_:::w ._,.,_
:investigated t1-:e establ·i~~-.::·.:-:.:::. , _ _._L
.f'or;;,ula for weirs with eno. con·crac 'v:Lons Lo predict t£-1e per-
formance of side we:'"-rs ~
wr1ere
b = 0.1
L = actual length of weir crest
N numce:c of end contractions
bette~ suited for siae weirs, althou~~ in extreme c~scs
Ernest .··. Schoder and Kenneth B. 'l'Ur::-J<;;:· :::.c.:.::<:tioncd t.:·:.s
c as~Lc weir formulas, and after twenty-fi ·.r~:: '".;,nc~::c-ed. t;ests
found the: .. the immediate problem was not or.e oi· side weirs
rather of weirs in t:,eneral. cor: i't;.. s i ::;; ll ,,. :C~1
.Ce::oence to the m. a·,--,ly ,_-,....,...!..-' :-d- -~ rl,'·:.·"·. 0-, r.;,;-v-,r:>r· {· "1Y>Y" <·',--.·ow-·- ; C• C' • 7 .1. .. 1 J..J v.r_ ,._,. ._._._.._ ~ c .. !....·--.!.>~'-- ~ vu ...... ~I -L \._)...._ .. :,LA.....L.:...::..~...).
B head on weir rneasured at t1-:e beginn:J..ns:; oi' tLe o.::.."'s.\·I-
down curve
Va the mean velocity of approach above the weir crest
measured in the cross-sec~icn as H
measured in the same cross-section u~ H.
To this paper, R. L. P(-},l~s~:.a~l..l ~ceplit:.:d t:-~a t l1i s exr)e:ci-
once with water led hirn to doubt 11 :::...::-- there :'t.s any suc!'~ thints
as precise weir n8 meat:.urenc;;t::~. Clemens Herschel~
8
President of the A • S . C • E . , added two quotes to the disc:us:::ion
of the paper:
and
Dani2l 3ernouilli of~en said to rr:e ~o 2~c~e~ a 11 cor:~·:·:·~~ -~-- ~; 2.:- ~-J c:d. r-. o r·:rLLll ~ls : i1e l~e ~- i e '1~n 8 tl1.s.. .. c ~~::e ·.::- ~ ga~n.iza ti . ..JD ;::; ~~- Natu:::-e is tc;,o s :Lmple to lea.d to tl:ceiT:; and should sne :ind such, ~he explanation is tha~ one 1 s computax:J..Dns were based upon f'alse hypotheses. :19
11 Tt~,::;se things are beyond all use~ ar1d I G.o fC:'C..J:' 'Gi"r~ .. :. nlO
T·::::::: .. .:.s R. Camp f'ollowed Hinds 1 energy-momentum r.1ethod.,
establishing Hind~ 1 equatjon in differential for~.
c~annels to obtain the surface profile of the water in the
"' -; d.- " C '~ r n"'" e -.l ll ......., __._ ...:... l.t. C).. ..... .1. •
Edwa::c·d I-I. Taylor used an altogether nevJ approaci~. He
prov_ -~ a graphical solution to the division of water a~
.~unc ~..;ions. He reasoned that the momentum equations are
complicated in cases of flow division by the inclusicn o:
three depths~ and that to assume a relation among t~em was
to assume a solution to the problem. Ee remained ~i~~ i~
h~2 belief that a rational analysis of division o~ flow
pi·oblerns is r1ot --, r
practicc.l _ _~_e::
Harold Tults studied water surface p~ofiles associated
with side weirs and found
ity distribution in the cross-section, snd ~~ the locatio~ o:
"che spilJ.··ay in the canal. nJ 3 For a s:c. ~- r -.~. s id2 '::c ::..:c·
located in the middle of a long canal~ ~e
by the maximum permissj_ble conveyan> ::3.e~".,
head in the upstream fl.::Y;-: is :Ligher than C.owr:2. the
,,-- ,. -.-.,-"Y by "',"-. ..-.J.· c +-_-l_on 1114 the e:,.cces~·. , ~ -~~--·--_ .... _ c~ \ -- ~ ~..~_ ~ ·
. l r
J:'C::CE:Dt tex~.-? Two of these pro-
files ,~~- exist only when critical or supercrjti~al flow
2.0
exi;c;ts .. HJ:"lich restricts tl'h,; s::...lrf'ace shape in the :-::.o:r-·c us:.;.::Ll
cases of flow to one of only three possibilities.
~~e effects of the location or inlets and ou~lots o~ a
system was throughly studied by the Bureau of Reclamation in
a model study 6f the Boulder Creek supply C <">"(1<=l..l~ 16 \,...(,.-_c.;.. •
had been designed to include two drainage inle~s and two over-
flow sections. It was found that the cap&city and location
of the overflow sections were not entirely satisfac~ory.
Specifically.. ti1e study indica ted "that a snort sid·3 v-:c: ir· was
more efficient than a long one_, a side weir was more efficient
when located upstream rather than dovmst:c·eam from an :.:._nlet_,
and that the flow depth imrnediately upstr·eam cf thG •:;eir· v:as
alvmys less than that depth irnrnediately dcwnstreaii1.
This lengthy review of literature is by no means a com-
I . d plete resume of all the works en side weirs published urins
this century. It is a su.m:rnary of severaJ. of the r::ore impor-
tant papers availeJ:.'le t;o t:ne a.u.thc:r·.
CHAPTER III
GENERAL DISCUSSION OF 'I':HE PROBLEM
-. i ..I....L.
Little is known about the behavior of floH of vJatc::r ove:::·
weirs and less is known about the division of flow.
the necessity of research in the field of side weirs ~s in-
dico.. ted~ the research mic;ht be directed tcn·Iard any or:2 of
many problems.
ri&lize and each study demands further investigation. A
fundamental and hopefully useful characteristic~ whicn warran~s
study~ is that of the ratio of flows. In conductins this
ing the study to just that.
relat~ the quantity of flow over a side weir to t~e ~uanci~y
remaining in the main channel of a rectangular flume.
numerous equations are available to determine these rel~tive
flows~ mode 1 studies have ctQ;ain and agD.in proved the tl-:.eo::::-·e-
tical predictions to be of dubious value. Is there ~hen any
relationship ~o be found?
What are t!-.c L·dc::;pe~cdcnt variables? ·.:·r::.e lengt::·1 of the
weir) the es o: discharge~ and the ~--' l. '
easily ~· ~~ureo q0antities.
used ~ ~ measure of the flow over the si~c ?he c.;.p-
s trea:-:·. ::..:Kl downstream angles of discharge ('::-: cons icwred
impor".. .. t because they are dictated by the -._,:::-:loe:::..ty of' t:.:1e
flow in the ma~n channel and the head on t~e ~2~r.
l •:)
Division o~ flow should vary with the heads ~nvolved.
Where should the heads be measured? Since previous studies
included the immediate upstream and downs~ream heads, a
r·elation with only one head i"las sought. A knovm head, imwed-
iately downstream, does not mean that an equal and constant
head exists for the rerna~nder of the channel, beca~.;.se the
level of the i-Jater continues to rise do·,mstream from the side:
weir. The head considered ~-:ere, then, is t~>-::e head consid,::r-
ably upstream o~ the side I:Wir. Tl.:Lr.:> hea'-.1. was allov-.red to
vary and the ef~ects on t··le di vis}.on of fl.ovv- were measur·ed
in this study. To reduce "cl1e D."i..l.i-:lber of variables, a constant
height o~ weir crest and n constant bottom slope of zero
were used.
The problem was restricted further by the decision to
place the side weir midway in the length of the flume, makin££
this study one pertaining more to irrigation channels than
to dam spillways. Such a decision influenced the surface
profile that was obtained.
Quantity, head, velocity, weir length, and angles of
discharge were the variables, and the constants were the
geometry and ro:..~ghr.ess of the flume, the pos 1 tion and con-
struction of i::i.-:.e ·:;;.::::lr, c.r.c. the physical pror ... c~:eties o:f:' 1:vater.
'• Tt.is test .... :. :·.:odel study without a 1-c::..cv.;r. 9rototype.
Although data o·c·cu.::..:.:l.::d using the smaller wei r·s v~er:: used to
predict the characteristics of the longer we~rs, i~ was un
fortunate that the results of this laboratory test could not
13
be compared with those of ah existing canal. Geometry of the
cons true ted :flume limit the application of t.he re'sul ts to
flumes of similar ph~sical dimensions and not to flumes in
general.
CHAPTER IV
TEST APPAHATUS
11..:-
The tests conducted in this investigation were performed
in a square wooden flume (Figure 1) designed and cor~structed
by the author. Because laboratory space was critical> this
wooden flume was constructed inside a much larger plexiglas
flume which immediately established the limits of the dj_;·nen
sions of the wooden flume. The plexiglas flume measured 36
feet in length~ and 2 feet in both height and width. The
plexiglas flume was set to a zero per cent slope with a
Dumpy level. A maximum delivery of water only half filled
this horizontal plexiglas flume. The maintenance of steady
flow was difficult.
To simplify measuremc::nts and computations~ the dimensions
of the main channeJ. of' t:·.·_, wooden f'lume were chosen to be one
foot in width a~~ one ~oot in height. T~c :ength of the main
channel of th"::. .~;;c.\;~er flume was chosen tc -~:c_:.~:,~~ ·::;:r:c- 36 foot
length of p:;.~__ . <~ _:;; flt:..n:;e. Placement of t.r~c, ~-,..':..de ·::.,: ~: 2 m:2.dway
in chanr.e:i. a.~·- .-.:Y.\1 C~d. 18 feet for stilli~J.g before the ·A'·=J.ter
reached _ ___ ,10~ '-lei::- and another 18 feet for fur·:_;>_·J:t> still-
. ing be:f"c:.: ; ' ... ~ •.. ~e~ ~eached the end weir .
:L'Lc: wate:..·· ::~c~SSlng over the side weir vva3 car2::...ed in a
secondary flume parallel to the main channel. The dimensions
of this secondary flume were 8-1/4 in-:::hes wide and 12 inches
high. •
:.6
The flume was constructed of exterior-grade plywood
treated for water resistance with PENTA~ a sealing compound.
This procedure rendered t:'ne plywood useful throughout the
testing phase or the investigation. The side panels were
1/4-inch thick~ which proved to be unsatisfactory since they
were still subject to bowing even after horizontal and verti
cal braces had been placed every two feet. The bottom \v-as a
satisfactory :i./2-inch thick. All joints were made watertight
with a water-resistant~ powdered glue and with coatings of a
polyester varnish. There were no leakage problems.
The suppressed weir at the end of the main chanr:Gl was
1/~6-inch galvanized sheet metal~ which had been file~ to a
sharp edge. The weir was placed with its edge 2 inc~es above
the channel floor.
The rectangular side v,eirs were cut ·':rc:r. 26-gc...ge ga..J..
vanized sheet metal to lengths of l-1/2~ 3, 6: 9o :2. 24; '36,
and 42 inches. Each side weir was placed with its edge 4
inches above the main channel floor.
To facil~tate placing and removing the side weirE, 2.
rur1ner, providing . a watertight seat, was fitted into the f>ide
and bottom of the channel. The runner caused a smali amount
of distortion in the flGw of water, but the amount waa less
'chan vii:1at rr;ight have been experienced had v1ood screws been
used to fasten each weir to the side of the flume ..
Various thicknesses o~ honeycomb baffling were used at
17
tr"'e up~3tream end of the main channel :::.n order to reduce tur
bulence. A ch~et one inch thick was found to be ·the most
effective. \IJ"ave formations were reduced by floating a mat
of wooden slats on the surface of the water for the first
10 f-2-et of channel length (Figure 2).
Heads were measured with calibrated dials and rods
placed 6 feet upstream from each weir (Figure 3). Heads
could be measured to a thousandth of a foot.
The water supply was obtained from a 5 inch pipe con
nected directly to a 12 inch feeder line. A gate valve in
the line was used to control the rate of flow. The water
passing over the side weir emptied in"Co a weighing tank
which was mounted on a sca1e -~vi th a capacity of one thousand
pounds.
Time was measured with a stopwatch reading to ·:·.,;e near
est tenth of a second.
Figure 2
Wave Suppressor
J.8
19
Figure 3
- .Head - Measuring Gage
20
CHAP'I'ER V
TEST PROCEDURE
The scales :for weighing the water flowing ove:::-> the weirs
were calibrated by the use of standard weights. The weighing
tank on the seaL:::> had a capacity of' five hundred pounds of
water. In the range from zero to five hundred pounds the
scales indicated no appreciable diff'erence from the standa~d . weights. No adjustments or corrections were theref'orc ncces-
sary.
The stopwatch used for the experiment was assumed to be
accurate~ but since the same watch was used in all t~a test
any inaccuracy would affect each test similarly but not sig-
nif'icantly.
sarr;e readings - \_. ... -the channel
:floor and the ·~(_)_) or· an iron bl·.:>Ck placed c_,r: ·:.!·l.: :'L,.J..nnc:l
:floor.
The suppressed weir located at the end of tne ~na~n
channel was calibrated by 48 test runs during whic~ the side
weir was barricaded. Heads r,vere measured six :feet upstream
of the suppressed weir. The scales were placed beneat~ the
discharge :from the suppressed weir and the scale ar·m was
weighted lightly. When the weigl:.t of' water in the weighing
tank was suffic~ent to raise the scale arm~ the stopwatch
was activated. A heavier known weight was placed on the arm~
21
and when the weight o~ the water raised the scale arm again
the time was recorded. The quantity o~ flow in cubic feet
per second v;as computed to three signi~icant ~igures" since
head and time each contained three significant figures.
Qu.antity (Q) was plotted against head (H) on logarithmic
paper (Figure 4). To obtain the equation of the line best
~1 tting these points, the method o~ least squares vms applied
using both the desk calculator and the digit'al computer. The
quantity-head relationship given by both methods a~reed:
This is in reasonable agreement with the familiar Francis
~ormula:
Both equations give quantity per foot of crest. The di~~er
ence between the two equat:Lo:~s was cnO'tlg:~. t,.: :"eject tne use
o~ Horton 1 s tables based on the Francis ~o~:-.:1:.J.a_, and instead
a_ graph was drawn accord:.ng to the experimer,t;;1.: eq_uation.
Quantities could be read from this graph to three 3~~nificant
~igures. The pe:d'o:rmance of t:;his suppressed we:i..r :::_::;_}_owed
the reading of q~antity of flow from measured heads ~ithout
having to m8.<:, i."<::::'...·ghings o~ main channel flow.
The barrier across the side channel was removed. The
side weirs were tested in order of increasing lengths. Heads,
measured six feet upstream ~rom both the side and suppressed
end weirs, were allowed to vary. The water ~rom the side
weir was caught and weighed in a manner similar to that used
22
i .. i.
0 z 0 0 w (j)
0:: w Q_ t_i
1-w w LL
0 m :::> u z
a w (:J 0::: .q I () (f)
0
,02 .03 .04 .05 .06 .08 0.1
HEAD ( H) IN FEET
DISCHARGE ( Q) VERSUS HEAD ( H >
CALIBRATION CURVE FOR 12-INCH SUPPRESSED WEIR
FIGURE 4
23
in calibrating the suppressed weir. Measurements were taken
of the upst:..""'eam and dov.r.n::.;-'c.ream o.nglec of discharge of water
over the side weir. Side weir discharge was measured for at
least twelve different heads for each size of weir. Suffic-
ient check runs were made to insure accuracy of measured
quantities. Five minutes were allowed to elapse between the
opening or closing of a valve and the measurement of a head.
There was a definite trend to the data collected~ but
when this trend deviated at longer weir lengths the following
check on the data was made. The barrier was placed across
the side weir and the flume was allowed to flow nearly full.
After thirty minutes the flow was measured and was proved to
be constant. The side weirs were then successively placed
in this channel of constant flow. The heaJs on both weirs
were measured. The flow from the side wei:.· v:s.:.:.. l:Jeighed and
added to the flow over the suppressed weir. Ti':e s:J.:o:r. of the
flows equalled the total constant flo'.'/, After- ea.:::! side WE:."ir
checked, the barricade was again inserte~~ and ~h~ quantity
of flow in the main channel was reduced. .--·· . ' '.;:.c-12 exper:unc:;nt con-
tinued similarly after another thirty mirwte wait for co~stant
flow to be assured.
The digital computer was used to calculate the quantity
head relationship for each side weir by the method of least
squares.
CHAPTER VI
TEST RESULTS
24
The :first test was per:formed to correlate· the discharge
o:f and the head on the suppressed weir at the end of the main
channel. The relationship was :found in equation form
Q = 3.78Hl.5l
per foot of weir crest. The difference between this equation
and the Francis formula was not significant. A comparison of
exponents indicated acceptable test procedures. The var· ·::.nee
in coefficients allowing discharges ten per cent in excess
of the Francis formula was attributed to the inherer:c prover
tiee. of' the constructed flume and vleir and to the relatively
small heads to ~hich the equipment was restricted.
Each side weir was analyzed "':;C> dete::·;·;_: .. --.. 2 if' an elementary·
equation for discharge could be found. W~~~ ;:otted on log
arithmic paper~ the data showed that fo1 . ., <;. g:i.v-.;.~n side weir an
equation of the form
Q == cnN does exist. To determine the equations for the lines best
fitting these sets of points~ the method of least squares was
used. 'l.'he results are shown in Figure 5. On this gra:ph~ the
points represent the obser\red data~ and the lines are drawn
according to the calculated equations.
If the equation for the 12-inch weir· had been known, the
0 z 0 0 w (f)
0:::: w Q_
1-w LJ..l LL..
0
a: ::=> 0
z
w (!)
0:::: <( I 0 J)
0
0 0
.01
DISCHARGE
WEIRS OF
25
(';'? • .J <- .0.::> .04 ,05,06 .08 c.: 0_2 0.3 ,...., -~
v;-r o.::-: o.s
HEAD ( 1-n IN FEET
( Q) VERSUS HEAD (H) FOR SIDE
VARYING LENGTHS ( L)
FIGURE 5
equation ror the smaller weirs could have been predicted by
reducing the coerficient in proportion to the change in we~r
length. The equation for a weir longer than twelve inches
could not have been predicted within reason. It is inter-
esting to note that the.predictable weirs were subjected to
greater ranges or head, velocity, and r1ow. It app~ars that
the practice of using a suppressed weir formula to predict
diacharge over a side weir is justifiable within a range or
r-elat1vely small main stream -Jelocities, heads or.. side weirs,
and weir lengths.
Attempts were made to inspect visually the flow of water.
It was found that streamline flow did not exi3t, confirming
the work of Coleman and Smith. The two methods used to
visualize flow "~Jere c:rude. T:h.e dye injection method indicated
that a strcanl~:.;.::; ·;;as ::'..iable to c.hange its direction at any
moment regard:sss or time or head. Turbulence prevented the
dye rrom defining any prolonged strea:;-:~.~-::J.e. An air bubble
method only -~'c.: .• ~,~::::d greater disturbance::_;_, ·~he: f'low. The
bubbles wer-0.~ c:J.~· •. f·_,~icul t to detect when mad·e st.n3..ll enough to
keep the a:no~Jr:t of disturbance at a minirr.um. r.r·~e bubbles
also r·ost.=.: -:o the surface too quickly to g:l. ve an a de qua te
indication c. streamline motion.
Fro~de numbers were computed and were less ~han oneJ
indicating that the·velocity.~as always subcritical. Reynol~s
numbers indicated turbulent flow throughout the entire exper:: -·
ment.
_,_ .....
27
The rat~o of the d~scharge of flow over the side weir to
the discharge over the su:::;~:,ressed \·:eir, Q2/Q1 , was exaE1ined
next. Th~s ratio, a dimensionless quantity, was plotted
against the ratio of length of side weir to the head on the
side weir, L/H, another dimensionless quantity. The head
was measured six feet upstream from the upstream end of the
weir. The ratios when plotted formed a·family of slightly
curved lines. Although the lower end of each curve approached
a straight line, the upper portion was definitely curved.
These upper portions were in the region of the largest heads
and highest discharges. It was found that plotting L/H versus
Q2 /QT , where QT equals the total flow, gave a straig~t lir.e
relationship on logarithmic paper, with some scatter.
11he computer was again called upon tc gj.ve the equation
oZ the line best fitting these points. ~ne lines and the
equations are shown in Figure 6. By a lcr::s ~_, tr:::-'::;ch of the
imagination it appeared there might be ~;.. re-~3.t:i.o2:snip betwe&:n
the coefficients and the weir lengthr To fin~ su~~ a relation
sh~p would g~ve a general eq~ation for the ratio o~ discharGe.
Dimens~onal analys~s allowed such a study.
There are many pert~nent values that may be used in Qe
veloping prediction equations for open channels with constant
bottom slope and cross-section. Because roughness was the
same in all cases and because the variation in temperature
was small throughout the. experiment, :t."'o·:l.ghness and the propeF
ties of water were disregarded in this e.r:alysis. The
' -N
0 - -1-0:: 0 -w -~
~ w 0 0 _J -
(f) lL
0: _J w <! > I-0 0
r-3 0 _J I.L
~r-·· i -_ .; , -:I'-: :--.--~--~· ·-=-'""' .... _,_ ..... _;r.r.~-, ·-~·7"""--l~~G~~---~~=-~~-i"-~ ---t·~~~-~r~-~-;~-~-
(]···- -- . -.•. i_-- - •_~_:.:~:-~!..:-[·. ~---:------:-- --_-·_--,_-_ :·- ___ ; \ i·r L~_36~'Q2/QT=6.50(L/Hr·B6 ~1 _ _:___ : 1 1 I :C i l J : . l : J •1 1 : . . : : i c r -1 i IT: Tr ~ : . : : I L~ 24:' Q2/i.H;3,38( L/H) -. 9D : ! Li= 42"
·-1- --~---~ \ .• j.l II ' ' . ' t N I __ ! ' I •
1 -~~-~ !~~J:·:t---: . ~: 12,. Q2/ QT: 0. B~L/H)-:·.7 7 _· _: ________ : ____ ~-:-. __ .L.:·J. -_f.'·_·,_.-
c C(''
0 . t .l ;;,.'I 5' II tel ';;.1- • ' ,-
r 1!,-c ~~
c r• (~
··!·' l
! . . 1"'
r ,. i . I i
\ :~ ;-:i~ i,i: ~- -- !-- _1 -,- '--: : _·· ' __ : : ••• : _: ... '!-'.~
\ _l __ 'L~9, Q~/QT,=0.49{LiH.x· B? 1; · · ! • i - ·, c·:·:: ' . I : ' . ' I ...
II ' i ' I l= 6_, Q2/:QT= 0.24{L/Id)~.,82: -I. ! I ·:·-+------!:--:. -+ '- :.:.:·~~-- f'- ; .•. :·
,- -1·- -1 ~l -1-1 I l I • ' -'
i : . i 'j I l-: 1 I+ -
Q12/ cir=io~;o~s(1Li;H)-·' 82 :r-_·-·~:·--r·1---K-: ~--·----- -
! • '
--~.
. '-~
~I ... ' i : '· . L i i I i ' f
i· . \
.. ·'·· l : ~~~ -)11 I·:~--·~·,, I . . i I. ' I I ' ·, . I. I .I. . ! ! .
-i I :. : . ' I • • -- •• • .. - ·:. --1 ·]- ' .• -· I - - : j I'. : . ,-- ; .: I ' i ' j ' : I ' 'I l j • I I . I ' . ·. '. I j • ' ' I ' • ' • I . . I . ' . ,· l . I__ I
1 l 1 , I \ , I I I ! 1 -t j
-l- r 1. ·I, -:·I . ; . • - • : ! I I I j · ' , 1 • • t 1 • j 1 --1 · I 1 1 ! ; ' •'t· 'j I I I I ' I I I I I ' : ~-· I 1 '' '-; ' ' I l • j I . • I • • I • I [ ' . ' ' . I I I • I ·l ' I I · ·r-r· · I .. , . , ' . -~ t - ' o ,. '·-t· .). . I •- f'. ·1---·- -~· T'. .. .. r· " ' • J
I ' I I . . ' ' I • I . j I I I . I I I -r ·;-~·--. -, ,... . : . _. ·- -- --~· .--1- t I __ .. --- - ,- ·---~-- ---- ,. - . - l·r :-: Jy :-: : ,_:I! I.--., :r·-··. J. -'~- -~ :+--t-·-- -~--:_ .... ...: . .r. ·r·:--~-~---j~---~-_1_-~--~~-. ; '" I . ' . ·I I I I ! I I . I I I I I I ' .. , _, I .. j I I '
.. ----_ --·.--' _, __ -~-rl_ .... .:. ' ... --j---- . - .. ·--.- ,·,- 4- _, ___ 1_ I- ------1--- ___ ../ .... '- -~--- • --! -,- -- l -L-t -·. -1- ----,·- --· , - ·~-· ·--- - ; ----1- .. -~-...: I I . :I. I . r • r I I I I ' ' I I I I I I '
·_ . . . I t • I , .... -. . I I. . I I ' .. ' . ,,. I I . . I . I ' I I . : . I .. ; I I I I I I I I I I ......... ' I ' I .,.....,.~_..~,_..., ... ,-.~"-"'-----~ ... , __;z;:,,_-_ .. ,co,-..-.... '"' .• ·•--·~· ...:i-.. -.....-alit' . ....-· -~.~·•.o-a.a....,:t.'W.:...,.__~-.. ·~~...._~~--.':':QIJI.,. '~~~ra ->--~~~>Cit&! '""- *"-~•t'L>wo ....... -~~~~
c; 0,1 0.{ r~;::_ ):i 0;-::; O_l' 1.0 2 0 :-~.0 :j_') 6.0 b!J IU 20 30 .:JO 60 c~',) 100
LENGTH
Q21Cl-r
OF SIDE WEIR
VERSUS L/H
FIGURE 6
( L) I
FOR
HEAD (H)
Sl DE Vv E IRS
..
f\) CX>
29
quantities that would contribute were considered to be:
Q2 flow over side weir
QT total :flow
V ve locj_ ty of' wa tE~r 1..n C'lu:!·;c .-~_1-:'t.·:·r pas sing ;:.; ide weir
L length o~ weir
vl f'lume width
H head on si.de weir measured some distance upstrean,
of' weir.
Six quanti ties· involving three basic d:'Lrr.ensior.:s requJ r(; t.Lpee
pi terms by the Buckinghan Pi Theorem. One possible selec-
tion of' pi terms is
Because these pi terms plot as pa~allel lines~ it is evident
they combine by multiplication. Hence
where
TI 3 - L/W
Glenn Murphy expl~esses nl in his Si:nili tude :::..n Enginee::c-i:r-'<::;17
as f'ollows
TI 1 F(n:2,n: \
- 3'
an equation which required a brief' explanation. It says.
that an empirical equation :for a dimensionls3s quantity can
be :found in terms or a function of two other dimensionless
30
functions, by plotting tl1.e original quantity against one o.f
the other runct1ons keeping the remaining quantity a constant.
The bar across a term ind1cates the quantity being held con-
stant. Then the original function is plotted against the
term that was previously held constant while the variable in
the first plot is now held constant. The equations for t}-:ese
two lines are multiplied together. The multiple is divided
by the value of the original quantity at the point where the
tv-ro other quanti ties v-rere held constant, and the quotient
gives the empirical equation for the _original dimensionless
quantity.
In Figure 6 there ar·e seven eq_u2.t::to:~1s f"or Q2 /QT versus
L/H with L/W be1ng held constant, seven forms of F (rc 2 , n 3 ).
Because the L/H ratio W&3 ·..:~.ncontrolled by -sre ey_t!ipment used
to conduct the tes·L;::..) the data had to be sear·e;_-,e\'l to find val-·
ues or constant L/H r.s.tios. There v..-ere -r:ew ::::·..:~~1-: va.~.ues, but
a value of 6.5 ror L/H was found in the ca;:,e --·;· -.=-· ~c ·-. ,,, o.--· 9 ..... ·- . ~"-· ~ ' and
12 inch weirs. At this constant L/H, a plot v:as mc..:ci.::: of
Q2 /QT versus L/W. The equation of this line is
F (:;:;:-- TI ) ·-· Q ., 77TI l • 7 '"2' 3 - ,..L 3 . ( l)
Multiplying this value first by the equation f'or the nine
inch weir and dividing by the value of' Q2/Gl}", at L/W = 9 11 /12''=
0.75, and L/H = 6.5, gives the equation
~ _ 78k~.82n 1.7 '"1 - . J c 3 .
For the six-inch weir the equation is
3l
TI 1 = . 77511 2 - • 77n ~1. 7 .J .
Although equat1on (1) was based upon a line passing through
only four points, the resulting equations justify a generali-
zation of the form
- rrQ.,. . .... 8 'i'' l. 7 7t 1 - . u" ~:? .. , 3 .
Substituting for these values, the following is obtained:
Simplifying,
which 1n the case of a one-foot wide channel becomes
(2)
'3~ \. I
These emp1r1cally derived equations cannot be orrered
for general use because the effect of the channel w1dth could
not be measured due to the geometry of the system. vrnen com-
pared to the measured ratios of flow, the calculated results
g1ve totally unacceptable percentages of e~~or i~ isolated
cases throughout all the tests. For the ~·n~1lest and largest
weirs, the calcu~ated results ave~aged ~in~ per cent in ex-
cess of and les~ than the measured results ~espectively.
the weir lenc~ths ranging .from three inches to two f'eet the
average error was seven per cent. Though such errors are not
t · , · · · · sl· ern the fact that the error is accep ao~e ln englneerlng ae a ,
no ~reater shows a tendency for the water to divide in accord-
ance with the geometry of' the system and its velocity. The
greatest errors occurred at the lowest heads, where surface
tension apparently has an ~f:fect.
32
A plot or the ratios o~ ~low to the Froude numbers also
gave a ramily or curves which were approximately straight,
parallel lines. This confirms the before-mentioned state
ment that the division o~ ~low depends on the geomet.ry and the
·velocity. A similar plot using Reynolds number gave a ~amily
ofparallel lines. In the Reynolds number relationship the
properties of water began to show their e~fect.
If the division of ~low is dependent on velocities and
head, the upstream angle of discharge shoulq·likewise be so
dependent. Graphing angles versus flow ratios, angles versus
heads, and angles versus velocities proved to be inconclusive.
A scattering of points was the only result of.such plottings.
The data and the plots showed that for each weir there was a
maximum angle of discharge. The maximum angle of discharge
was smaller for a longer weir. The data indicated also that
the velocity increased with head. These observations can
explain the existence of the maximum angle. At low heads,
the angle increases with head. As the head increases, the
angle continues to increase while the increasing velocity
tends to drive the exiting water back toward the flume. At
large heads, the angle decreases with increasing velopity
and is ~ndependent of head.
As the weir length is increased, the upstream water
level is drawn down and the resulting heads are lower. Since
it is the head that acts to increase the angle, the lower
heads mean lower maximum angles · o'f discharge.- Also,· the data
33
indicate that ~or a given head~ the velocity in the channel
containing a longer weir is greater than the velocity in the
channol containing the shorter weir. The angles indicate an
increased ratio or rlow with increasing head and a decreased
ratio o~ ~low with increasing velo.ci ties. Although no con
clusions can be drawn rrom the angles'themselves~ their be
havior adds ~urther justification ror raising the head
(always less than one root in these tests) by a decimal ex
ponent in the derived equation.
An attempt was made to:de:termine what length of weir
would be required to reduce the down stream head on the side
weir to zero. According to Coleman and Smith~· the length is
in~inite. The test was conducted on the longer weirs and
the heads were continually reduced so that a nappe was main
tained at the upstream end of the weir. The down stream
head was always considerably higher than the upstream head.
Even with the longest side weir in place~ the downstream head
remained greater than the upstream head. Only when the nappe
was allowed to disappear did the downstream head begin to
decline. FinallY~ when no water passed over the downstream
crest or the weir, the head was so small upstream that the
water just skimmed over the upstream edge of the weir and
down the outside o~ the weir. Within the geometric limita
tions of this experiment, it could not be determined at what
length o~ weir, ir any, the downstream head could be made
zerp while the upstream portion continues to act as a weir.
A constant harassment during the testing was the com
parison of the two measured heads. As far downstream as
34
twelve feet, the head was often higher than the head measur
ed upstream from the side weir. This had been noted by
other experimenters, but the difference in heads and ·the
lengths between gages were not recorded. Witp the upstream
gage 12 feet from the flume entrance and the downstream gage
30 feet from the entrance, the difference in heads was a
great as .05 feet. There were noticeable rises in the water
surface, particularly by a standing wave beginning at the
downstream end of the weir and' extending into the main channel
at an angle of 45 degrees; but none of these ~ises could be .
con~3idered a hydraulic jump in the spectacu.lar sense of that
term.
Tults states, "Fundamentally, the flow along the crest
of a lateral spillway may be treated as a flow division where
the divided water lost over the crest of the spillway, does
h . d 1118 A 1 . . t +-not affect the energy ea . pp y~ng a plc ure Lrom
Vennard19 (Figure 7), it is seen that since the flow is
always subcritical, a hydraulic jump, a jump from super
critical to subcritical velocity, does not occur. This
figure (Fig~re 7b) shows a rise in the water surface for a
decrease in quantity of flow at a constant energy. Hence,
the illogical variations in head can be explained by the
characteristics of flow.
CONSTANT DISCHARGE
ENERGY )
CONSTANT ENERGY
I SUBCRITICAL
:c 1-a... w 0
01 SCHARG E
B
DEPTH- ENERGY- Dl $CHARGE CURVES
Fl G U RE 7
35
)
36
3 Inch Weir
36 Inch Weir
37
3 Inch Weir
Figure 9
Comparison or Flows -- Side View
3 Inch We~r
36 Inch We~r
Figure 10
38
End View
C:-IAPTER VII
CONCLUSIONS
39
The results o~ this study produced in~ormation appli
ca-:)le to the use o~ side channel weirs in irrig.ation and
drainage projects. Several conclusions are drawn as a
dir·ect result- o~ the 1\'0rk perf'ormed in this study within
the small range of' heads and velocities encountered. They
are as f'ollows:
l. The f'low of' water over a side weir can be computed
by an equation of' the f'orm
Q. = CHN.
2. The ratio of the f'low over the side weir to the
total flow can be expressed in terms of' length~ head~ and
chaYJ.nel width.
For the system teG~ed
n -·- 0.9
m = 0.8
p = 1.7
3. The ratio of' t·. ' f'lows can be expressed in terms
of' Froude numbers and Reynolds numbers.
4. The downstream head may be larger than the upstream
head~ and .this higher head might continue .f'or some distance
downstream.
40
-·. A side weir three and one-halr channel widths in
lc::-;'"'··:~h cannot reduce the downstream head to zero and still
--~~ion as a wei~ with a nappe.
4l
CHAPTER VIII
RECOMME:N"""DATIONS
A study is never concluded. Wl'"len time demands that a
s~op be made~ more ques~ions have arisen than have been an-
sv.Jercd. The cons true tion of the apparatus asks~ 11 Is there a
cc"..:.tcr way? ll The data ask,. l!Is there such a thing as a
~:::rccise weir ;;.2asurement?" The results beg, 11 Why? 11 The
~:,·o:::::-'d~.> of' t'n.e critic still sparkle_, TlWhat is the question? 11
It ls hereby recommended that:
l. Side weir investi.gations be made varying the channel
~~d~h and the heights of the weirs concerned in order to in-
crca22 the head on the side weir.
A study be made on a side weir in a flume with steep
bottom slope so that the velocities of flow might reach the
[::>upe:..'"'criti.cal ;:;tage.
3. A study be made where the length of the side weir is
increased to a great extent in order to determine the effect
o~ lenGth on the downstream head.
4. A study be made to determine the surface profile of
the water as it approaches, passes, and continues past the
~>ide weir.
5. A study be made to determine the discharge characte~
j_~_.-t~ics of side weirs whose crests are not parallel with the'
c:hannel botto~n.
6. A study be made with an end weir of adjustable
~e~3~t to allow a constant head to be kept on the side weir
~or different rates of flow in the main channel.
43
APPENDIX·····
DATA FOR CORRELATION OF THE END
SUPPRESSED 12-INCH WEIR
44
45
, .. .. _:__=:::BRATION OF SuPPRESSED END vJEIR
.. ·. ~:_ .--) l ~~ 0 1..,. Ti::::e ~' ~) . ~~eight. Q Hc::s.d ·. -- .-·~ --~ (~· :." "v'Ja te r r .., .- n \ ( \ (1bs./cu . .ft.) ( cf' s) \ J_ '.J>"j ) (SeC) ( ~""~ ) - v.
------ "" -------·--------200 25.6 62.30 0.101 0.125
2CO .... 9.8 62.30 0.123 0.163
300 20.0 62.30 0.161 0.241
300 17.1 62.30 0.177 0.281
300 l r- ~ .-.O.J 62.30 0.185 0.293
-::; r,r, ·v'..: l4 0 -'- •__./ 62.30 0.195 0.324
300 ::._2.2 62.30 0.220 0.395
3CQ 24.6 62.29 0.143 0.196
300 20.4 62.29 0.157 0.236
300 19.9 62.29 0.161 0.242
300 18.6 62.29 0.169 0.259
300 "'7 9 j_ I • 62.29 0.176 0.269
JtJQ 17.3 62.29 0.178 0.279
300 16.7 62.29 0.182 0.282
300 1[..~ Li --" . ' 62.29 0.189 0.313
300 15.1 62.29 0.198 0.319
?.C·O 11.5 62.29 0.229 0.417
300 ~-'-·6 62.29 0.230 0.414
300 11.7 62.29 0.238 0.410
30C - '1 9 .l..L. 62.29 0.232 0.405
300 11.! .. 7 62.29 0.200 0.328
300 16.0 62.29 0.190 0.302
300 19.8 62.29 0.168 0.243
46
C.t -~ --~~-F~J~ ~IOl\f OF SUPPRESSED E:N""D \'ll'EIR ( col-:tinucd)
I· . . of ,_-_; :l. n:: e Sp . 1~.Jc ight \) ~ :0 Q :read ' . . ~:~· ;._:-..._ -l:.- ___ ; J:~ VJater i -i ·, ' ) \- '-~-· ~ ( ,_. 2C) ( 1 b"' /c,l f'·'-) ....... u. \.-V (cfs) r .c._,_ ) ', -'- v •
---.-.---.·-·--·----3CO 20.3 62.29 0.160 0.237 r,,,......r, LVU 18.6 62.29 0.130 0.179
200 19.1 62.29 0.127 0.168
200 2::...2 62.29 0.117 0.151
200 26.5 62.29 0.102 0.121
200 26.3 62.29 0.102 0.122
2GO 18.7 62.29 0.132 0.171
,·:.Jr11'"' .::_\___,V 16.3 62.29 0.139 0.-91
;~oo 16.2 62.29 0.144 0.198
2CO 13.9 62.29 0.160 0.231
2VG 13.2 62.29 0.167 0 2L-:: . ' ...)
r-..., _,....,_ r\ .-.:..uv J..2.2 62.29 0.169 0.263
200 12.0 62.29 0 '7ll • .L ' 0.266
200 11.4 62.29 0.178 0.281
200 11.1 62.29 0.182 0.289
200 i0.6 62.29 0.187 0.303
300 1~ r .:J.G 62.29 0.190 0.308
300 14.1 62.29 0. 206 0.340
300 12.7 62.29 0 ?ill • L_ ....... • 0.379
300 11.8 62.29 0.228 0 . ..-08
300 11.6 62.29 0.229 0 1:.., r .4-J...?
300 10.6 62.29 0.242 0 1J.;:::::2 . ' _,
300 9.5 62.29 0.281 0.559
300 7.6 62.29 0.294 0.633
"S!-\.TA :s'GR 1~-INCH WEIR TEST
~ ...
(\ ~ :.:_: . )
·~~ ,_ u. ~ .. i -'c i t~ y .'3 i Ci. o l;J e i r
viEIR TEST
Suppressed
(ft. )
Quantity Suppressed Weir
C::l..,
( c f~)
Velocity
(ft/sec)
~-8
S::otal FlovJ
Q.--;-, (ci"'s)
-·-··-··-·- -~-- --~~---· ----------·----~-----------------
r~ . , .-'" -.._,,.',.__)~
I ' .. ....... \,_.. . --
j_ s
. -·· ~
. ... ; --"' '· )
,.-....r-/f"\ • '-..- I ' . ...J
.070
.0057
.0071
. OlO~-
.0117
0155
.0
0268
.0528
.0023
0 ,.,...- /') r-)
• Qc...:::_
. oL:.o6
.0153
0 ()·~-
• vO_j
.0290
. 01'"( '-,·
.0057
.258
.260
. 2'T8
.286
.308
.382
.461
.495
~a' .:J 0
.213
. 9~-5
.520
• )_~68
1.1?~1 • ' .__ I
.368
.. 305
-=· s· "' ·...) 0
.322
.250
.480
4 ()~
. 0)
.550
.570
• 6LJ-O
.670
7·:-o • I 0
.900
1.18
1.30
1.33
.365
l • 52
1. l~O
1.22
1.05
.850
625
.500
.891
.672
.464
1.13
1 llL • _L '
1.23
1.26
' 32.J. _L • '
1.39
1. L~8
"' 6LL ..l.. • '
1.88
1.97
1.98
.96
2.14
1.92
1.77
1.59
1.32
1.16
1.61
1.3'7
1.11
.486
l.i02 . . ,;/ 5 c·"'· . ov
.582
.655
.686
.781
.929
1.225
1.353
1.393
.367
1. 594
1.462
1.270
1.091
.878
.640
.506
.920
.690
.470
Head on Side Weir
H _(I_~_j __ ._, .. ,, .. ·
.077
.083
.102
.110
.130
.lL~ 3
.173
.?10
• 211-1-+
. 3.10 ,,
)jl)
0~,.,
• _)1.
. ~3J~)
. :j~~-)
Q2/QT L/H Froude Froude Reynolds Angle of Discharge Deviation of Nu:·:;ber V2 /gL
I·Tumber' V2 /gH
N11mber pvr/u
Q2 /Q.T Upstream Do\'TnS tream fro-;n computed
values x 1000 (degrees)(degrees) (%)
-""-=-----...------·.- ,..;.~,.,,_..~·~_...._ .... J/11.,#.,.,_.,~ •. -._.M~ ,,_.,..'1..,'!'~.·-~·~-........ ~---·..,.,""'~""- .• ,... •. ,.__ ... _"'-4-00..:<.1'...-..--7, ·:-r < ~ ··---~·"'· .·-~~-...... ,u-........ """"'-..,_.., '>,&/V'"I:• , • .,:I~UI"'""'·•-_,.-.._..,,,.,.. ..,....,.,._,,.,-~"''ll!•,.,.r ..• ·•· :•.~·-..,,._, .• ·.:·~-~-... ~-~' -~.-..~~_,._..,.,.,.,.,,.
.011'7
• 01)+l.i-
.0186
,0201
.0222
.0226
.0262
0 ~) 10 . .)-·
(' . ..,,·s • \j •'\r)(
•-'
OJ· oo . . ./
! )•1 ~~- ~··r ' \..,/· .. -
rn(' t \- .I',.._)_)
~~-~ ; ~ (~ ~~
'I, "'', t 1,,:;.,· ... J
1.623
1.506
1.225
1.136
.962
. 8'7L~
,'(23
.595
.512
. ~~o·:.; • ' J
;·2
i.L,O]?
. :bl.
')'J. . ...-
. 31'7
. 322
.375
.394
1111~'" • L-fLtO
LL3o . '
:;lLIJ • _.I I. (
r/·8 .00
n.-78 .o '-'
(l(h • ..)•)i
(--..,.r-•11 • ;: { ,~_r
. 2~~9
!. . '1. ':J
~ I j 'I. ·- t ... _ _,)
.093
.094
.105
.109
1- ·r • J.' I
.124
1 -·~ . 5J
.152
l .... (r:: ·~ :J
'1 'i·) . ___ (.),_
.18·
. ()"() l(i()
• l. .:.· _)
·-~
24.8
25.2
27.8
28.7
31.2
'-!-2.8
45.9
lW.6
1.n.1
' ') 0 ... '- • .J
r- •') r :::> _) • \)
1 o n -~ .. ./ t ._)
! : c I Ji . ../ __ ,. , r
' ~, . ' ·"" j J
lj.Q
48
52
55
60
60 r• .--· ,,, /
56
:3'7
52
5-~~
", 1 _..,~--
')
,- .. \_... :,_)
~-8
55
47
l.f6
43
rr2
39
36
24
10
10
~-))
.. •')
~:} ~-)
''2'/ .. 1:
-J-2L~. 5%
+12.5%
+ 3.6%
+ 2.0%
-t. C.. lof.. • J, ;o
-'-·l 0 7ot'O I -·· ' I
+11. 2Jb
J.l '1 0°1 1 ..... , ;o
' 5 ?.·r./ T • . ;o
-'· ·\ 7 rvl ' -- ! r \_,•,.J
1·1 '! • '1:-/;
, -~ .-, ~r·c/ "i '.:. .) • ;J
' -~ l -, --< . ..-/,"'
') ( J ., ' _,.,
49
continued
Head on Side \·Jeir
0.2/QT L/H Ii'roude 'T , 1, ·u·r·'l''<"' -.... - li u-' J..
V2 /gL
Froude Number V2 /gH
Reynolds Number pvr/u
X 1000
Angle of Discharge
Upstream Downstream
(degrees)(degrees)
Dev:tat:ton of Q2/QT
from ccrnpu ted values
( 7&) H (ft.)
-~--·~·""""""""'"""""""'......._..,..,._,~,.._. • ..,..._._ ... ._~.,_~;. --"'·--·--~-""~--->: .. ; ·,·-.~o,.r..:~_; .·..&.o~~,...._..-.,~-:.'ro.;.,·•~-·-•-~--....-.-rt-..:'11. . ...-..-.;;-. .....,...-.-~---·;·"'"""'..,. . .:~..--.... -....._ ...... J..~'•-''"''· ... _..,.-,..,,,.;:.,..-..·..,..""""'··-.·•...,......--.. --,.,.,.r"-."'""• ·..--· ... -.=--~·-. ,. __ ... ,..... .... ........., ............ ,~ .. ....,..,.," --
.279 .0393 • [~L~8 .915 .180 50.7 58 32 + 9.0%
.241 .0372 .519 .778 . J.6l~ 45.5 60 35 + 3.1%
.185 .0317 .676 .628 .11.~7 J.l~ .1 56 33 - 1.6%
.·131 .0239 o:=.4 .. ;_~ 33 .115 30.8 54 35 - l. 75'~ o/J
.O'TO . 0121.~ 1.786 . 331-l- .097 r.r " l.l1 41.~ +13.3% C::J,C..
,200 .0315 .625 .6J!.Jj. . J.L~6 .~a [ 60 l.J.O -~- LL 8% _)_;;.0 & I • I
.145 . \)252 .862 Llf6 .119 hl.9 55 )f f~ -! J gcrl .. - - -- • jJ
.070 .0121 ] '{oc .]06 ',- J?. 23.7 J.~o 60 !- J 5 lL% -' U()
I - • I I
50
5l
DATA FOR 3-INCH WEIR TEST
...... -, ·-~ -~ .t
-" \._.·,_;
.-'·: I ~-j. _:_··o
,-·-. -"",1) c_ _:;;,.:...
--, ~:· ::) .1. \....J ·~J
-- ·--_.,_ ... _; ._.1
--: -.' ) ___ _, .. _
l •'/ . -'- ' '·-
,..., ·-· .-• V~)L..)
. --~- 0 ~3
057
Q ~J. :-:i(~ t ~L ~ :.l S ::_ c~~(_; ~~I c i r
0933
O'"l )_• • :; -~~ r
0325
( ... ) -. rr ~ . '-'- ./
.0120
. 0835
0 -;;;,)_; 8 . ..) '
0200
.0102
.0930
.0531
.0231
.0323
nl '. '") L:. • \..../ ' ,C.,. I
0(~17 • ..._.-- l
.0322
C-'"'.U'..)
3-INC~-I SID:t: h'EtiR TEST
Hes.d on Su.ppr-essed v!ei L'
Quantity Suppressed l~! c-:i l~
Q.l
Velocity Total Flovl
( c f" <,-,_~ \1 ( ·r'"' _._ I c -==> .... \ - i.J; '-''--\J I
-------·----~~----~-------------------
.1.~65
.416
.360
3 -, l1 • ..L-r
0'"'5 • .::.d
.252
;: ;,6 • .t,....!..l _ _._
. iJ.Ol
. 3l.i-4
.320
.296
.255
.441
.2-1-18
.375
.305
.320
. 386-
. 380
. 321
.247
1.20
.980
.650
.570
.480
i l ~-= ..L • _, __ ___
.950
.750
.670
.660
.l~-70
1.10
1.00
.850
.603
.660
.720
.900
.868
rr-8 .0::::>
• l.J-60
1.89
1.68
~ 5? .L. ~
1.35
1.26
1.14
1.88
1.67
l )17 ..... -;-
1.37
1.29
1.11
... 8-..L. '.l
l. 71
1.57 .., .....,3 ..L._J
1.35
1.42
- 6....., .L. :;,
1.61
1.38
1.11
1.293
i or:::4 -· _.1
.851
.683
.588
.492
1.01LJ.
.78:5
. 705
620
J, gr-• '-I- v
1.193
1. 07lt
.903
.658 ,--,...2
.0':::}
.762
~---2 .;:;o
.920
.690
.470
. 0721
.0704
0603
• OLi-7 5
.0297
~'"'? '· --• v_LJ-:;.
.0630
.0578
0 ;,9..-, . ..... :;,
.0322
0212
.0779
.0690
0587
.0426
.0556
.0641
0 ~·--s . :JO
OL6,• : 0 .
.0223
Head on Side Heir
H (rt)
.266
.232
.188
.133
.093
.058
2llr • - ' :J
.232
.171
l'"'r.: ' jlJ
. 092
. o~G ; ... ,- 1! .<\} r
·)•)'"") . ,·_ ~-)
i (~ :~ / __ )
I /l'J" 1~1-, . ; r1 ~ _] 1 J.'j_C)!_._t,l_e
,. 0 • ::;'-!
1.078
1.330
1.880
~?. 688
il ) l 0 .. , . .) ··-
1.020
l C713 J. • ) I (
J ,1' :2 "1 ·' ()
. • _j()
') ... , ' .
•-. I J (
' 1 .... - •
:'. ~ I : :. (_) / !-
, ~)-\:.· (
' ' -~ : ~ {_)
·. (;. -~ t I __ ~-_....:
1'-f~)_~rt~::: r ·'"2 /:.'T \j 1 o··.J
• Ljlj)~
.350
.287
~?h . ·- ._____ ~-'
l 07 • -1.-_../
.161
!, ·-o • 'i j..)
J'' r '··O . '-
')<g • c.t_.;(
f)"""'·~-..
. (_ jj
. ~~ (=~!s
'-'-J)
' ' I '"'
P:coude iTu.rn be :c V2 /gH
.175
.150
l ·)r • .)0
1- ··r , j_
.109
Oc.r . _)()
• lr(9
.1 1""2 '_) ..
.131
. J;~o
. i 1 j_
I " [~
/ _ _,·
FeynoJ.ds T\r U. L~ l; (~ rJ pvr·/u
X 1000
26.9
42.9
3'7. LJ.
31.5
28.2
2h .~-~
lJ8. 5
1.~2. 6
., r· c
.):J.U
·)'3 ( ) • 0
..-,(""1 n / __ -:1.). 1,)
'·::; '( I - • _.1
I,' • .. I
' I •
) f )
.~-,,c··lr=> o·'·, Dic·c}<"'r'·'' l)·"'Vl''•ltio· o·"' "'_, . C) L -~ r ... o .o. _ ~~ e _ '~ . . c _ n .L
G2/Qrr Ups trca.m Do1·ms treo.m fJ:om cornptJ. ted
values ... ·-·-~·-~ .. -.... ..," __ . ..,.
57 LJ-2
52 37
LJ-6 ~-0
50 ho
l'" rC: 42
36 55
5'( Lj.L~
51 !.J.]
51 li-5
!' l :J '- ~~ ) !-
)I fl } . i'T
Tl ·-~ ') J·
; :.r'! ;_ :~ ; . _/ ' /
.' '.: "i
( !Jb) .. ~~ ._, .• ,~p~='"'"'""'-~ ;><\}_, __ _ _..,. .... ~,_..,._ -- = .~___.. .. .._._._-,.. .. ~"'"''.,..,..
+ 7.0%
+ 1.0%
-· 5. 8%
6. 370
+11. 670
7.0%
, r:- od T 0 • 7/0
+ 9. LtJb
- r~ ad ...-·'JfO
n r;r:f () I ~);J
J
1 --~ ' ()/~ ; -I. . "
'\ _j I
() • ' 'i
53
continued
Head on L/H Froude Froude Reynolds Angle of Discharge Deviation of
Side Weir Numter Number Number Upstream Dov.rnstresm Q2/Qrr
H V2 /gL v2 /gH pvr/u from computed (ft) . values
--·-·--.. ,~~-·---· . ~~--~,~=-·--··-~~~-. .J:..Q.OO~-----~~-~------· ~------------.. --.-·J%2__ ___ . ___ .... ----~-·
.120 2.083 .219 .116 30.2 50 45 - 3.2%
.115 2.174 ,200 .108 29.1 50 ~2 .. 1.5%
.131 1.908 .226 .116 31.5 53 1~-5 - )~. 7%
.153 1.634 .250 .124 33.8 5'7 1.~8 -11.8%
.203 1.232 .330 .149 1+0.6 60 50 Of_ - . 2 .l7o
.182 1. 37l~ .322 .1L~7 . 39.2 60 48 + 1.7%
.132 1.894 .236 .121 31.8 !.~5 50 - 1.5%
.057 l~. 386 .153 .092 22.5 30 60 + o. s;~
\ 'l.
54
55
I
DATA FOR 6-INCH WEIR TEST
56
6 -INC-I SIDE HEIR TEST
I:i( _ Qua~-~ci ty Head Quantity Velocity Total Q2/Q.~ . ...., . ..
Wei:.:-- Sup- Su:opressed ,_, .... L ~la.e on Flow s~~:..c: pressed We:_;_:c ~_-_:\_: ~L :--.. ~~reir
-~- i. 12 Q.': Qrr : :• _,_ ) I r ·.c. ) (ft) c c :rs) (:rt/sec) (crs) \ -- '-' \ v ___ .. ..;
-- .... ~~----~--"'""-·---....... ,... .... ~.-~--,.,---r
.u_:;,o .0193 .278 .550 1.24 .569 .0339
. o.:_;-1 .0151 .279 .550 1.26 .565 .0267
Q7C • i :l . 03Ll-9 . 305 . 630 1.32 .665 .0524
.097 .0458 .309 .640 1.34 .686 .0667
•.. ·- J .0569 .312 .. 650 1.36 .707 .0804
.l35 .0692 .336 .720 1.43 .789 .0876
.2.53 Q708 ?l.llJ. .760 1.49 • 81..~0 .0950 • l ../ . ..) ' .
.l'[d . ogol_J. . 375 .860 1.59 .950 .0951
. ~·-93 .0995 .388 .900 1.62 .999 .0995
0l r:.~ .1278 .424 1.05 1.78 1.178 .1085 . ~- -"-...-'
. J .. 8~5 .1010 . 386 .900 1.63 1.001 .1008
. 15E, 0'78"'1 • I - .349 .780 1.51 .858 .0910
.ll2 0400. • ::J '--' . :::_;:'.8 .640 1.34 .689 .0721
.cso • (;~_L.! 3 .263 .500 1.16 .514 .0278
.060 . c~ ,~.:.S .271 .530 1.21 -551 .0372
.075 .0299 9:' •- Li• .590 1.28 .619 .0482
. 092 o-.:-- . • .J'·- ·, -=<0 C'; . ...... '-' .640 1.35 .678 .0566
.180 .0960 .361 .820 1.53 .920 .1043
.130 . o6oL~ .311 .630 1.32 .690 .0875
or;l .0172 .246 .450 1.09 .470 .0365 . ..---
He:::..d on Side '.·Je1r·
H (ft)
L/H ll~ .L --~) '). c! .. e :\I')·-:~::·,=: l~
v2 /;;L
Froude ~·T unJ; (:; :c V2 I t)-i
-.< . '-, ,- -,, !) 1 '1 .~ -~--v .... -- --~-o , T ' i'': , __ :_ c·~ c c~ r~ vo;r/u
X 1000 --~----- .. -- ... ---..--~ ...... .,..-.--·-------~-~ ... --... ~ ... -- _,_ .... _, ......... -..,:,_, .. ~-·----- _._ ..... ___ ........ ~A>-•.t...,-··- .... -· .,.... •. :~· -- - --·-· .... '""""
.056
.041
.079
• Q9r{
.123
.13~
.153
.1'78
'l '93 ... . 21/)
I 1~ ;
l . ,)
1 -- ) •... .L c._
!"))0
(·;': ()
() ,-,09 u.';;c
qr-].2,1__.)
6.330
).15:5
1! .• 065
-:{ '((-.}I .J. j -j-
.--, r '"8 _).20
;::l,809
2.591
·) -~~ "(: --· • ,J :: .)
") r:o·~ 1",. I! ,_}
j,:L()
;! _,--}, . -- ...
1 {' '1 ___ ·)(:()
,, . :r)j
(\C)·-:-• J:;J
.099
.108
.111
115
. 12'7
1 •')8 • -- _j(
] r--·y . . )
.163 .i • , I J._/l
'1 ~:-•. Ll__.,)
• :1.-:~2
.1L1
j -~-~ ~-~ '"' ' ~
_:~j 1_
o lOr(
.113
. J.1lt
.117
.120
.126
l -~r:; • --- ... /'J
.145
.14'{
.166
1 11 0 I,_.'·!'" ....I
l ·~r( --·. ~)
I i_ :_·
.-:l:, ( • ·~ ./ I
"1
27.0
26.8
29.5
]0.6
31.9
33.9
35.9
39.3
1!0.5
• 11 r- ? ,-:_)' .)
1:o.s .-,( (
_}] I t)
" ~ :·_I ~:t I ~
.~--.~~~.C)
1\i1L;lc · (• f).i.bCf1Ci.l~;:;i2
fJr'·-•tC·JC . .--,1-'J r~~-)-,",~c·l·r·, ,.,-.,1 ·. )...)1:. .1.. ~-u.. 1 _....)._ dJ.-•,:) .~ ....... c.11
3}~
23
36
lj.2
L~8
1~8
~~ 8
51
h.ls j
r- , ..
:u
)5
jO
I. f ,, . r
;·~ _: ~
.. ··-~ .... -.-.- _...,,_, __ r..r·,..,u ...,,....,. ,._,_
60
6r(
53
}_~9
L~ 7
L~o
L~·r
'I
50
l!8
Ji ( ·-rO
'.·g ~ ~ ...
1:' 'i I
. -.-r ( ')
.~ -. ~ ~ ' .....
D'.; Ii_e. i::i.o1l of
0,2/QT r'L'Cm conpu.ted
vo.lucs ( cl)
·.· , .. __ j:~ ... - ~ .. -~ ... ··- ..
+18. 99b
1 ') '7 oaf .-... 1o
+ 5.1%
-· 3 }lot • Tj0
-· 2 qot • ;.;o
- L~. 37b
2 ]d - . . ;a
.!. 9 5;;1 l • ;0
l '] () ']t-.-f -.-.. • _)/J
I "Ll jd .. - - . ·/')
-~- R }! c01. t \j • T;
+ ') s>:;)t "' '·--,
l -, -1 .• --, J
1 . f .... :~' ~: .- ..
. ·- i;J
}I·
57
Herld on r1 • 1 01.c e Vcir
H (ft)
.075
.092
.180
.130
.051
T '· .uj 1{ F:c·Jude 1J t..t r;: ;J~_:: r V2 /c·L
I ......_.-
,, :.ca.::•-Y~_..,.._.;d:"_,:.•·· ~--.•... ,_ '- ....
6.666 .102
•:. !I ':lL\ _.) • 1., • .) • , , 3
• _1__1.
2.TT7 -1 1! l-. -- -,-)
'1 OJt C .) • <)'-.-1) .108
o :;oJ..t. ..I • ' • . err J.~
li'r(Ju.c1c .i'Jun:ber V2 /gH
.110
.119
.138
.113
'IP9 'V,J
-~~n··:1o.lcl·' .l -"--J _ . .,_v
l\}11n1br;r ovr/u ~ ' '
X 1000
i\;Htl C; of' Di SC 11')'o(,'O D·::;via{·j ,..-.,"1 of i l. -~ .. , {..:J- \...... ~ ~ -·-) 1 :..~.1 l_; \_, . ~..... ~ v .. 'v 1 .
Q,) /nrn JL~-~J •
Up~:> t:ceam Dovms tr:0am f:_r_•om cornpu ted values
(7&) , .. ~, ~,...._,, ">oS•,_.. '·"-'o"'J'«, J.~"><j. ........ , •• _-~ -·•'•>•'··-'"""'Jti·-·"'~• .,, .•• _. .... , ... L ..
~- ___ ,_ . .,.,. · .... ·'"•' • . •. , ··t.-~ • ~--'
28.5 1}0 57 + 8.'-l-%
30.6 ~-2 42 + 8.7%
36.7 l!-5 50 1 ro' + . O;b
30.0 50 LJ.5 -- 6 1% • -1
13.1 35 50 + 6.2%
58
59
DATA FOR 9-INCH WEIR TEST
60
9-INCH SIDE WEIR TEST
Head Quantity_ Head Quant:Lty Velocity Total Q2/QT on Side Weir on Sup- Suppressed Flow
Side pressed Weir W<~ir Weir
H Q2 Ql QT (f't) ( CfYs) (ft) ( cf;s) (ft/sec) ( c:r·s)
.053 .0283 .268 .500 1.15 ~ ~: t .528 .0535
.067 • 0~ ~~ .287 .580 1.28 .620 .. 0646
.079 .0508 .292 .595 1.29 .641 .0792
.096 .0673 .308 .630 1.33 .697 .0965
.110 .0795 .312 .640 1.31 .720 .1104
.054 .0322 .257 .480 1.13 .512 .0628
.086 .0572 .288 .570 1.25 .627 .0911
.102 .0734 .304 .620 1. 31 .693 .1058
.123 .0927 -3~5 .690 1.41 .783 .1184
.141 .115·' .344 .760 1.48 .875 .1314
.163 .130·. . 360 .800 1.52 .930 .1397
.183 .164 .404 .960 1.68 1.125 .1462
.227 .217' .. 423 1.05 1.78 1.267 .:).:712
. 199 .187·· .. .404 .960 1.68 1.147 .1630
.175 . .. 157;· .387 .. 860 1.55 1.017 .1543
.150 .-121·. . 349 .760 1.51 .881 .1373
.162 .136' .360 .780 1.54 .920 .1478
.118 . 0870 .304 .610 1.34 .690 .1260
.052 .0258 .242 .440 1.08 .470 .0548
Hcci.d on L/H Froudcc Frou.d~~ T.l --- r }ric· nn~lP 0~ Di~cb~rnn De:\ ~at:Lon of' ,~_cyD.J. '--·'::> .-.L- ::) __ ..._. l .... ~_... .. 1..,.~. l/._...
Slde \~eir Number Nu.m1.· :e :Jrn-oer Q2/Q~r H V2 /gL v2;o·:· I
(ft) o.tl. pvr;u Upstream Downstream from computed
Vel lues X 1.000 (c::\
_.._.....__ ... __ .,,_a-~·-=--~-~,--....._, •- -~.r~r-..,·-· ",,--_.,.,._., '- _ ~-- . ..r.~..,.,-~"7--.-,-......, ••• - .. _ ..... --~--~-·---~------ -~-----·-·-----~ .. ----------·-'"-- -.I--·-·-·"--·---
.053 1LL 151 .055 .oglt 10 7 ~-)5 55 .L 5.1% . l. I
.067 11.194 .068 .112 27.9' 32 58 - 2.0%
.079 9. 49l{. .069 .124 28.6 37 49 - 0.9% I
.096 . 7.813 .073 .116 30.1 42 53 6.0% -
.110 6.818 .071 .109 30.1 43 50; - 8.8%
.054 13.889 .053 .093 19.3 26 58 - 10.5%
.086 8.721 .065 .107 25.4 36 43 - 9.7%
.102 7 I 353 .071 .113 29.8 42 46 - 11.4%
,123 6.098 .082 .125 32.3 4L~ 45 - 5.3%
.. 141 5.319 .091 .133 35.1 46 46 - 6.0%
.163 LL60l .096 .136 36.8 Lt7 44 - 0.5%
.183 lt. 098 .1rr .153 41.3 47 40 + 3. 9/b
.227 3. 301+ .131 .167 1+5. 5 44 45 + 5.9%
.199 3.769 .117 .153 L~l. 9 45 48 + 0. 35~
1!.286 37.8 43 45 6. 77b 0'
.175 .099 .135 - 1-'
63
D . .:.·..:·..-\ FOR 12-INCH WEIR TEST
64
12-INCH SIDE "WEIR TEST
l:..:c:.~d Quantity Head Quantity Velocity Total Q2/QT or. Side Weir on Sup- Suppressed Flow
S .. -... d.e pressed Weir ~ ... : _; ir vJeir
H Q2 ,·. Q] . Q,.,. ( .-. .._ \ (c:rs) (f't) (cts) (f't/sec) ( cfs) \ l.. 'v I
. os.L~ .0417 .247 .45G 1.0$ .492 .0848
.060 . 0519 .257 .480 . 1.13 .532 .0975 .·.
0~,~~~ • j •• .0628 .268 .510. 1.17 .573 .1096
.088 .0897 .290 .580 1.27 .670 .1339
- .llLJ- .307 .640 1.35 .754 .1511 ,..LUO
.126 .136 -335 .720 1.43 .856 .1588
'31:::: • J... . -' 1c:::;c • ~7 .346 .760 1.48 .919 .1730
.1:53 .181 .371 .850 1 .. 58 1.031 .1765
.:::...30 .141· .332 .720 1.41 .861 .1637
. ogL:. . 099· .302 .620 1.32 .719 .1376
l 1.L., .169 .352. .780 1.50 .920 .1836 ·-·.l.. .100 .106 .301 .620 1.33 .690 .1536
Road on ........ . - ..... 1/H Proude ::)ide Weir Number
H V2 /gL (ft)
................ ,._......_,..~""~....-
.054 18.519 .036
.060 16.667 .039
.078 12.821 . 04 3
.088 11.364 .050
.108 9.259 . 057
.126 7.937 .064
.. 135 7. L~07 .068
.153 6 5 ~,c, • J .) .078
.130 7.692 .062
.094 10.638 .054 .
.141 7.092 .069
.100 10.000 .055
Froude Number V2 /gH
---.-..-.087
.093
.098
.109
.120 .
.126
.133
.144
.121
.115
.134
.117
Reyno :1 d;:~ Angle of Discharge J}::vJ_a~=ion of' N'J.mber Q2/',ll pvr/u Upstream Downstr2am from ·c 11l1pU. tcc1
values X 1000 (?s)
-~----''""-""'-'-'~--~ ~.:~ ---~--""""'- ·.·-.--,c .. .,"'C'--..,..,.--.....,_----~-
23.1 23 60 -- 12.1%
24.5 30 48 - 6.1%
25.8 32 4L~ - 8 .d__ '. '/0
28 .4 35 43 - 19.0%
30.8 41 45 - 1L~. 5%
34.3 40 40 - 6.6%
34.8 43 40 - 9.8%
37.8 42 43 - 1.4%
32.9 37 47 - r(. Oojo
29.5 . 37 L~7 -.17.6%
34.9 43 45 - 12.3%
29.7 40 45 - 21+.4%
0> V1.
DATA FOR 24-INCH WEIR TEST
- .
67
24-INCH SIDE "WEIR TEST
Head Quantity Head Quantity Velocity Total Q2/QT OD. Side Weir on Sup- Suppressed Flow
Side pressed Weir VJe:l.r Weir
H Q2 Ql QT (rt) ( cf''s) (f't) ( cf''s) (:rt/sec) (cf's)
.045 .0536 .233 .420 1.05 .473 .1131
.056 .0767 .247 .455 1.10 .531 .1442
.063 .0918 .257 .480 1.13 .571 .1605
.072 .110 .269 .510 1.17 .621 .1787
.081 .128 .281 .560 1..25 .688 .1860
.089 .165 .296 .600 1.30 .765 .2156
.100 .198 .312 .650 1.36 .848 .2334
.112 .235 . 337 .720 1.43 .955 .2460
.126 .270 . 358 .780 1.48 1.050 .2571
.104 .211 . 318 .660 1. 36 .871 .2422
.084 .150 .288 .570 1.25 .720 .2083
.043 .0477 . 230- . 410 1.03 . 457' . .1077
.120 .256 .331 ;660 1.40 .920 .2782
.089 .160 .294 .530 1.30 .690 .2318
.044 .0511 .236 .420 1.08 .470 .1087
DATA FOR 36-INCH WEIR TEST
70
36-INCH SIDE 'ltv"'EIR TEST
I~c0 .. \..~ Quantity Head Quantity Velocity T.otal Q2/QT on Side Weir on Sup- Suppressed Flow Side pressed Weir Weir Weir
H Q . . Ql "i
QT , ~ct) . ( cf'~) (f't) (crs) (ft/seo) (cfs)
.086 .274 .319 .67 1.38 .920 .2978
.076 .197 .277 .50 1.24 .690 .2855
.034 .0594 .231 .42 1.05 .470 .1263
.113 .340 .352 .77 1.48 1.070 .3177
.098 .313 .339 .73 1.44 1.013 . 3089
\ . 087 .264 .316 .66 1.36 .894 .2953
.070 .209 -.286 .57 1.25 .749 .2790
.057 .142 .262 .50 1.16 .602 .2358
.045 .101 .249 .46 1.11 .531 .1902
.028 03°7 • ;;I I .241 .37 . 97 . 384': .1031
.056 .149 .267 .51 1.17 .659 .2261
. 073 .226 .293 .58 1.26 .806 .2803
.100 .344 . 330 .70 1.41 1.044 .3295
.llO .404 .345 .75 1.46 1.154 .3500 '
HE"a:d c:-l lj r~ ~-... _-_,. ·": ... ;_ -, I;.:··.,_~}-. -·~-. r ,-.. -.-, -~ l .--:., !\ ~~l. -~~!- <· ci ~· f):~ :- e ~ -~- .. j )~ \ ~~- ~'- ·t· ~~(I }'1 (,If' ...J. -· .. • ~ • - • ' •
S J. cJ. :~ 1~} ~--~ ~:- ~~ -. l:. ': : '.--. -~. ~ ; :. ·,' ; I·" j_' J: :, H v;) / . ·2; " U fJ ;:; -~-; ~ ~- Z:~i :-: J}~J L~l-1 ,:::_ t }.-· ~-- El ~ ;; V L-!- ncv- ~· ,) t (:: c1 (ft)
vc:Llu:.;;=:; X 1000 ( ('
-.....-....-.. ,--= ;"0,..· -~.--. -'"""-=-··-. 7-)) ' """"- ..... _,. - .......... ' -~- ' ~-- • J• •• , ~ • ,__., .... --- •••• < ~ ' ' ·- - , •• , ... ..._ ~- ·- .. ' -- ---· .... -----~- -- ·- .____ - ~,_._,..., ..... '--· ... -
.086 ----,'; or .020 .122 30.6 15 L!-O 2 () l)rf :J~, • ..Ju -- ::; . c.p
.0'(( 3r- ,-0 .016 .107 26. ~- 25 }r r.: - 7. ?!5 \_J ..----. .)oj ,- :J
. 034 88.25 .011 .086 21.8 5 60 1----, od -- .) • ;o
.113 26.55 .023 .131 33.9 23 26 +10.6%
.098 30.61 .021 .127 32.4 20 28 + 5.5%
.087 34. L~8 .019 .119 30. L~ 24 31 + 0.7%
.070 1.12.06 .016 .107 27.5 26 30 -11.5%
.057 52.63 . 01L~ . 09'( 24.9 22 36 -10.3%
.045 66. 6'{ .013 .092 23 .L~ 20 l!-O - 8.0%
.028 107. ]_lj. .009 .OTT 19.9 no nappe +llt.J.%
.056 h----, 7 r·-:J.). :J .01h .098 2l!-. 9 2h 50 61 - 7 • JO
.073 L~1. 09 .016 .107 27.5 27 1~ 0 9 lJ cl - ' .-p
.100 30.00 .021 .124 31.7 22 32 O%
.110 27.27 .022 .129 33.1 15 32 + 2 . 57b "'.J I-'
72
DATA FOR 42-INCH SIDE WEIR TEST
73
42-INCH SIDE WEIR TEST
H8ad Quantity Head Quantity Velocity Total Q2/Qr on Side \1-Jeir on Sup- Suppressed Flow
Side pressed Weir ''J c :ir \-Jeir
"'-t Q2 Ql (~s) 1.
r c:> "- 2 ( cf s) (ft) ( cr·s) (ft/sec) ~ .1.. ~-
.075 .309 .315 .66 1.37 .969 .3188
.061 .242 .294 .60 1.30 .842 .2874
. Ol+6 .175 .270 .52 1.19 .695 .2517
.076 .312 .313 .61 1.37 .920 .3391
.052 .204 .. 273 .so 1.20 .690 .2956
,-.-,5 . '~·..) .070 .228 .41 1.03 .470 .1489
Head o: s 1 de vr~ J :c
H ( rt)
~~ .. ,-,.-,'"'1!-~~···~ .• I-~· . ..,-.· •• -: ..C; -,
'075
.061
• Ol.J-6
.076
.052
.035
-- I J '/ _,_,_
L' C Cc( i 0. (.)
r::r( JCl :J • .)U
j6.09
Li-6. 05
67.31
100.00
J/ ~e0 -~-·- r"-,
1\]i __ l}";':-:, :,_.]-j
\: ;:~;·,i-, • (_'_; 1_,·
. OJ'(
.ens
.0}3
.orr
.013
.009
}? r· ~) -t)_ c ·; -~-·
J\ - ~' .1- J (; _t I ~ r
1Tl_~_ri11J 2 t) l-J~.~ ::Ut~:~~-· CC>/ -v·r · L~ 11 p::·•v/ll.
·-·~ --·-/ ,_ ··-· _ _ X J()()Q - .; .. ~...-.,.~-c. ~' ·'-' . --- -' .
._ '! l • _I r J. 30.0
.J.J.l.i 27.9
.100 .1
.121 29.7
.102 25.2
,083 21.1-~
J\. ~i - l_ c 0 ,..., ) -i ~-~; c.} J j
1J-;J ~~ t,c:r~~J [!.~)·:-,~:-~~ ~~--- t c·
2li
21
20
15
10
5
) I r::. i_)
Li:S
~0
l15
50
60
]) -: _· \ ~ _I ,:·) f; ("\ j_
I •--
"{.'_,
_f }~'();, C \) ~~~ C; t~ t r~' (1~
\l e~ 1 ~~:. c:, ;3
( c:!) -')
....... -- • . . j· ...
+ ~~ oc~ _..I • /')
+10. 1!}.;
-1·17 .ElJb
+10.3% /
21 I ' rJ ~- ·-t-. \.>;J
-10. 17;
'.] , .. ~-
'-·"·- ..
:: c) •
1
--, " l""o.. •
FOOTNOTES
21.
r l C?Q) S. r:l • 1'"' ~. \-~-u l~e spl ~Kays ror regulating sion canals. Transactions, A.S.C.E., Paper 1694, p. 1561-1588.
75
dive-:'-vol.
C_P;_l\OLLO, J A and N. /\. srr::.~\..LTSK-AL- r -, ~2o \ -:\ · _ • ", - _.__ \__:_::J :)) vlS-
cnarge over side weirs with and wit~ou~ baffles. Journal Boston Society of Civil Engineers, vol. 16, no. 1, p. 118.
_ J .• ~--:;~~:1\~ =~·'-'I., a::"d ::.::.B. TtJRN"ER (1929) Precise weir· measure-ments. Transactions, A.S.C.E., val. 93, Paper 1711, p.999-ll90.
1176. Herschel quotes from WOLF, R. (1860) Biographies relating to the history of civilization in Switzerland. Vol. III,
"1 r-7 /" p. ~tO·
p. ll'76. Herschel quotes from SEAI(ESPEARE_, Julius Caesar, Act II_, scene 2.
(1940) Lateral spillway channels. Transactions 2 (\..- ,- r ,.-..,
A.S.C.E., vol. 105, P er uo9, p. b0o-oL7.
'~:\\Y:::-'JH, E. (19Ltl..~) Flovv characteristics at rectang1..<lar open channel junctions. Transactions, A.S.C.E.; vol. 109, Paper 2223, p. 893-912.
iS_, E. ~ 1956) Flood protection of canals· py lateral spillways. Transactions, A.S.C E., vol 82, hY 1 5, Paper 1077_, p. 1077
, . . Ibid., p. 1077-5.
. CHOvJ_, V.T. ( 1959) Open-channel hydraulics .. NeH York, McGraw Hill, p. 340. ::
16. U.S. Department o~ the Interior~ Bureau of Reclamation,
76
Division o~ Engineering Laqoratories (1956) Hydraulic model studies of Eoulder Creek canal drainage inlet and overflow weir sections. Report no. Ryd. 407, p. 1-14.
l'{. WJRP~-IY, GLEKJ" ( 1950) Similitude in engineering, New York, Ronald Press. p. 41-42.
TULTS, H. r-)56) Flood protection of canals by lateral spillway. Journal or the Hydraulics Div
. ision, A.S.C.E., vol. 82_, HY 1-6_, Paper l077J p. 1077-1
19. VE~~ARDJ JO}lli K. (1962) Elementary fluig me~hanics. 4th ed., New York, Wiley_, p. ~§~.
7?
Bil3LICGRAPEY
8:\.:-~2 r~•. H. (:sAo) Ls. tex•al spillway channels. Transactions~ A.S.C.E ~ vol. 105, Paper 2069.
C~-~0'.'.'_. V.r;}. (:::;_959) Open-channel cydraulics. New York~ McGraw Hill.
" n ·:""'\"!\ffjr.1..,.T ( "1 02-,) lfflli"""\ .,-! ""I ....-.. """"'• ,.,..., .. -, • ,.: __ ...
~'":0. JJ. ul'LL.lli .J.>' 5 l~,e Q-'-SCn=r0lDG-Cc.po.Cl vy
(1916)
(1950)
of s=..de:: W<:~irs. n Institute of Civil Er~gineers (london)) Selected Engineering Papers, no. 6.
Side channel spillways. Transactions, A.S.C.E.; vol. 89, Paper 1587.
Similitude in engineering. New York, Ronald Press.
N"II'II"c\10, H.H.R. (1928) Side spillways :for regulating dive:::·sion canals. Transactions, A.S.C.E., vol. 92, Paper 169~- .
•; - ', -0 'r 0 • ._,...._ -, ••,~
o_) .~ _; ~ \; ~~ :.._L.J:
. C. B. TURJ\lER ( 1929) Precise weir meas1J.rements. Transactions, A.S.C.E., vol. 93, Pc.per 1711.
(1956) Characteristics o:f side flow weirs.
I_..,..
. '
Tl-:.esis. University of Southern California..
:·o~~) R~o~· ~h~r~c~erl·s~~cs ~t recta~~u-~~r \. ....:..../ • • ..r... _._ vv \...i-.~o..~.c;;... C\.. v v.....~- ~ .... b ..J.,.c;,.
open channel junctions. Transactions, A.S.C.E., vol. 109, Paper 2223.
Cr'\.EC.~IIJ ~ :; . A. , and N. A. STEYSKAL ( 1929) Discha~~c over side woirs wit~ and wi~hout b~ffies. Journal Boston Society of Civ~l
~ - r =~cince~s, vo~. ~o, no. ~.
·: \ .. :-· __,..,' \.. j
.. .,.,__ .J •• '·' J ,\..,• J.- -~ v
(1962) Elementary :fluid mechanics. New York, Hiley.
4thed.,
78
VITA
Ed[';ar SnovTden IV was born :May 15, 1934, in 1r·Jashington,
D. C. He graduated ~rom t~e Episcopal High School in
J:.J..,;.xandria, Virginia _ _, in 1952 and :from the University o~
Virsinia with the degree -of Bachelor o:f Arts in Mathematics
• - 9' r J..Yl J. ::;o.
Be was commissioned into the Regular Army as an officer
in the Corp·- of Engineers. He had engineer:ing assignments at
Port Campbell, Kentucky, Ui Jong Bu, Korea, and Fort Belvoir,
Virginia. During his Fort Belvoir tour of duty he was enroll-
0d in the School of Engineering, George Washington UniversityJ
~:;.nC. had "v. _.:; privilege to serve as White House Social Aid to
:eros:l.d8nt John F. Kennedy.
In 1963 he ·was assigned to· the University of Missouri
c:~·~ Ho:ila, enr·olled as an undergraduate student, and completed
·~1s requirements ror the degree of Bachelor of Science in
c·:L vil E:'1gineering in January-' 1965. He continued in the
~n J~rmary, 1965, he became a registered professional
cnzincer in the state of Missouri.
He 'i:Jas married to Miss Patricia May Spokes of' Rolla
in June of' tnat year.