Introduction to Irrigation Design.ppt

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    Introduction to Irrigation Design

    Sprinklers uniform application over entire

    area lawns

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    Micro sprays Water uniformly over small

    areas

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    Drip Trickle specific area shrubs

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    Plants need water for

    Cooling evaporation and

    transpiration use energy results ins

    cooling plants Nutrient transport

    Dispersion of plant expelled waste

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    Site Information needed

    Soil texture, profile and infiltration rate

    ater source !uantity and pressure,

    !uality, cost "ayout of site areas to #e irrigated,

    elevations

    Plants to #e irrigated $ainfall and %& rates

    'udget

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    ater Conservation

    Pota#le to effluent

    Irrigation sc(eduling

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    Steps to develop plan)* +#taining site information

    * Determining t(e irrigation re!uirement

    -* Determining water and power supply

    .* Selecting sprinklers and ot(er e!uipment

    /* "ateral layout 0or 1circuiting2 sprinklers3,locating valves and main lines

    4* Si5ing pipe and valves and calculating total

    system pressure loss6* "ocating controllers and si5ing wire

    7* Preparing t(e final irrigation plan

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    Site plan "ocate all #uildings, walkways, driveways,

    parking areas, lig(t or utility poles, retainingwalls

    Indicate w(ere t(ere are slopes and in w(ic(

    direction and (ow steeply t(e ground slopes* "ocate all trees and s(ru# areas and pinpoint

    t(e plant material on t(e drawing*

    soil type

    "ocation of any new planting areas and t(e

    types of vegetation t(at t(ese areas will contain*

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    Available Soil Water

    Soil a#sor#s and (olds water in muc( t(e sameway as a sponge*

    8 given texture and volume of soil will (old a

    given amount of moisture* &(e intake rate of t(e soil will influence t(e rate

    at w(ic( water can #e applied*

    &(e a#ility of soil to (old moisture, and amountof moisture it can (old, will greatly affect t(e

    irrigation operational sc(edule

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    Soil moisture

    Hygroscopic water is moisture t(at is(eld too tig(tly in t(e soil to #e used #yplants*

    apillary water is moisture t(at is (eld int(e pore spaces of t(e soil and can #eused #y plants*

    !ravitational water drains rapidly fromt(e soil and is not readily availa#le to #eused #y plants*

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    Source: ;S

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    Source: ;S

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    Source: ;S

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    Source: ;S

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    Source: ;S

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    Soil moisture &(e permanent wilting point represents t(e

    #oundary #etween capillary water and (ygroscopicwater*

    'ecause (ygroscopic water is not usa#le #y plants,

    continuous soil moisture levels #elow t(epermanent wilting point will result in t(e damage or

    deat( of t(e plants*

    "ield capacity represents t(e #oundary #etween

    gravitational water and capillary water* It is t(eupper limit for soil moisture t(at is usa#le #y plants*

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    Available Water

    Soil Te#ture $ange Average

    in%&in% in%&in%

    'ery coarse(te#tured sands and

    fine sands )%)*()%)+ )%),

    oarse(te#tured loamy sands

    and loamy fine sands )%),()%-) )%)+

    Moderately coarse(te#tured

    sandy loams and fine sandy loams )%-)()%-. )%-/

    Medium te#tured very fine sandy loams0

    loam and silt loams )%-/()%-1 )%-,

    Moderately fine(te#tured sandy clay loams0

    clay loams0 and silty clay loams )%-.()%2- )%-+

    "ine(te#tured sandy clays0 silty clays0

    and clay )%-/()%2- )%-3

    $eference4 5SDA0 6$S0 Engineering Field Manual

    Available for each soil group by soil hori7on from

    6$S Soil Surveys

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    Source: N$CS

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    ater needs

    Soil 8 0inc(es9foot or inc(es9inc(3 ? @ield

    Capacity 0@C3 ilting Point 0P3

    @or specific plant 8 0in3 ? 0soil 83 A

    $ooting Dept(

    $eadily availa#le water ? plant 8 A 8llowa#le

    Depletion 0use /B if not provided3

    Irrigation interval ? 8 A 8D9 usage per day %fficiency ? net water to root 5one9gross water

    applied to system

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    $eference 8vapotranspiration

    8To or potential evapotanspiration represents a

    well watered, fully developed plant suc( as

    grass

    $eference evapotranspiration is multiplied #y acrop coefficient to o#tain t(e %& rate for a

    specific crop

    &(e crop coefficient varies t(roug(out t(e

    growing season

    @or %xample Corn at B ? B*46 at /B?)

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    %stimates of %&

    ax and min temperatures

    $elative (umidly

    ind Net radiation

    odified Penman to estimate 8To

    ; of isconsin we# site (ttp:99www*soils*wisc*edu9wimnext9et9miet*(tml

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    Precipitation $ates

    P ? !98

    ;nits M5ST #e consistent* @or:

    P ? precipitation rate 0in9(r3

    ! ?flow onto area 0gal9min3

    8 ? area 0ftE3P ? F4*- !98

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    Precipitation $ate Importance

    Do not want to apply water faster t(an

    t(e soil can a#sor# it

    e need to know t(e time re!uired toapply t(e correct amount of water

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    Sprinkler Irrigation

    ;niform application #y overlapping

    non=uniform wetting paterns

    Sprinkler spray (eads no movingparts = small area pop up

    icrosprays over(ead small area

    $otary Sprinklers Impact or geardriven

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    $otary Sprinklers uniform application

    over entire area lawns

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    Micro sprays Water

    uniformly over small areas

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    Drip Trickle specific area shrubs

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    &ec(nical Information No55le = remova#le

    controls velocity and flow +perating Pressure inc

    pressure inc water flowand c(ange wetting

    pattern $adius of &(row furt(est point

    ater Distri#utionPatterns

    &raGectory angle

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    Spray >eads

    &ec(nical Information operating

    pressure, flow, radius of t(row, and

    no55le options @ixed (ead

    $otary otor=driven

    $otary Impact

    'u##les