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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