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8/2/2019 Climax Flow Rate Jan 2012
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EV301EngineeringHydrology
ClimaxFlowRate
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ClimaxFlowRateAnalysis Rational
Method,
,
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The rational method is used around the world for peak
flow estimation of small rural drainage basins and is
the most widely used method for urban drainage.
Q=kCiA Q
peak
flow
(cfs or
m3/s).
k conversionfactore ualto1.008 SI or.00278(metric).
C
dimensionless
runoff
coefficient.
i rainfallintensity(in/hr,mm/hr).
A catchmentarea(acres,ha).
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=
Where:
R=Runoffinmillionm3
= 2
C=Constant
=
verage
annua
prec p a on
n
me res.
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beanapproximatemodelforcomputingthe
oo pea resu t ng romag venra n a ,w t t e
runoffcoefficient
accounting
for
all
differences
betweentherainfallintensityandthefloodpeak.
Suchdifferencesresultfrominfiltration
temporarystorage,
and
other
losses.
AmericanSocietyofCivilEngineersandWater
o u o n on ro e era on s oun n a e . .
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RunoffCoefficient Coefficient
that
represents
thefractionofrunoffto
Characterofsoil
Previous
moisture
conditions
Slopeofwatershed
Amount
of
impervious
soil
Landuse
Duration
intensity Table
7.1
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perthetypementionedabove.Therunofffromeach
added
together
to
arrive
at
the
total
runoff.
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different
C. Use weig te average:
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Intensit
Averageintensityforaselectedfrequencyand
urat onover ra nagearea or urat ono storm.
Basedon
design
event
(i.e.
50
year
storm)
Overdesigniscostly
Underdesign maybeinadequate
Durationis
important
Tc =timeofconcentration
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TimeofConcentration Tc
Timeforwatertoflowfromhydraulicallymost
distantpointonthewatershedtothepointof
interest. Rationalmethodassumespeakrunoffrateoccurs
whenrainfallintensity(I)lasts>=Tc
Usedas
storm
duration
minutes.
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TimeofConcentration Tc
Dependson:
Sizeandshapeofdrainagearea
Slopeofdrainagearea
Rainfallintensity
Whetherflowisentirel overlandorwhethersomeis
channelized
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simplified analysis of runoff using isochrones, or
between them as illustrated in the figure below.
the basin, so the ratio between the peak runoff
ratio of the volumes of runoffand rainfall.
time t=0 and has a duration of the time of,
will reach an instantaneous peak at Ci.
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time after rainfall excess begins to when all
por ons o e wa ers e are con r u ng o
the peak flow at the outlet. If the duration is longer than Tc, the
reaching a value of Ci for a time period equal
o e erence o e ra n a ura on an
Tc. In either case the time of rise and time ofrecession are equal to Tc.
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of rainfall and basin size areaccounted for explicitly, while mostother physical characteristics of the
watershed are accounted for
concentration and runoff coefficient.
critical nature ofTc.
,area is not contributing.
no increase in contributing area, andtherefore no increase in peak flow.
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Exam le1: Theclassificationofacatchmentcoveringanarea
2
1.Rocky,impermeable=10%
.3.Forest=30%
Usingtherationalformulaandthecoefficient,
thecatchmentwhentheaverageannual
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R=CAP
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Exam le2:
Theclassificationofacatchmentcoveringanarea
of150km2 isasfollows:
1.Covered
with
vegetation
=30%
2.Cultivated=40%
3.Heav Forest=20%
4.Sandy
Soil
=10%
byRichard,findtheannualrunofffromthecatchment
whentheavera eannual reci itationis650mm.
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WhatistheModifiedRationalMethod
(MRM)
ser eso rapezo a s ape y rograp sarecrea e fordifferentStormDurations.
TheI
in
the
Rational
e uation
is
based
u on
the
duration
andnottheTimeofConcentration,
HoweverthehydrographsinitiallypeakattheoriginalTime.
Therunoff
volume
from
the
pre
development
hydrograph
issubtractedfromeachoftherunoffvolumes(areasundertheTrapezoid),foreachstormduration.
Thegreatestdifferenceinvolumebetweenthepreandrespectivecriticalstormduration.
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Desi nEventRecurrenceInterval
2yearinterval Designofintakesandspreadofwa eronpavemen orpr mary g waysan c y
streets. 10yearinterva Designo inta esan sprea o
wateronpavementforfreewaysandinterstate
g ways. 50 year Designofsubways(underpasses)and
sagverticalcurveswherestormsewerpipeisthe
only
outlet. 100 yearinterval Majorstormcheckonall
projects.
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