ce-341 evapotranspiration & rwh

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    EVAPOTRANSPIRATION

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    Measurement of Evapotranspiration

    1. Lysimeters

    2. Field Plots

    (invoking water budget equation)

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    a) PENMN!" E#$%&'N

    based on energybalane and mass tran*er

    PET = daily potential evaporation in mm/day

    A = saturation vapour pressure gradient with temperature at mean air temp

    mm of Hg/oC

    Hn = net radiation in mm of water/day

    Ea = f(wind velocity & vapour pressure deficit

    = pshychrometric constant = !"#$ mm of Hg/o

    C

    Estimation of Evapotranspiration

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    Saturation vapour pressure of water and pressure gradient

    Estimation o*

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    ( ) ( )

    +

    +=

    N

    neT

    N

    nbarHH aaan 90.010.0092.056.01 4

    Estimation o* +n

    Ha = incident solar radiation in mm of water/day f( latitude% period of year

    a = !"$ cos(latitude in degree

    ' = !"

    ) = ma*imum possi'le hours of 'right sunshine

    f(latitutde

    n = actual hour of sunshine

    r = reflection coefficient (al'edo

    f(water/land surface

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    Estimation o* Ea

    + = wind velocity at m a'ove the ground in ,m/day

    es = saturation vapour pressure at water temp" in mm of Hg

    ea = actual vapour pressure at air temp" in mm of Hg

    ( )asa eeV

    E

    +=160

    135.0 2

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    Mean monthly solar radiation at top of atmosphere, Hain mm of

    water/day

    Estimation o* +a

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    Mean mont,ly values o* -ossible suns,ine ,ours N

    Estimation o* N

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    b) /LNE0&33LE E#$%&'N

    Empirical e-uation 'ased of data from arid western .

    Evapotranspiration in crop season in cm

    100/

    54.2

    =

    =

    fh

    T

    TPF

    KFE

    ET = PET in a crop season in cm

    0 = f (crop type

    Ph = monthly percent of annual day1time hours2 f (latitutde

    = mean monthly temp" in o3fT

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    4alues o* 5 *or seleted ro-s

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    Monthly daytime hours percentage Pafor use in Blaney-Criddle

    Euation

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    !"#$%"&E! H"!'ES$(!"#$%"&E! H"!'ES$(

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    %hat is !ainwater harvesting)

    onsious olletion and storage o* rainwater to

    ater to demands o* water *or drinking

    domesti -ur-ose 6 irrigation is termed as

    ainwater +arvesting7

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    %hy harvest rainwater )

    &here are many reasons *ut following are some of the important

    ones+

    4&o arrest ground water decline and augment ground water ta*le

    4&o improve water uality in auifers

    4&o conserve surface water runoff during monsoon

    4&o reduce soil erosion

    4&o inculcate a culture of water conservation

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    How to harvest rainwater

    Broadly there are two ways of harvesting rainwater

    i. Surface runoff harvesting

    ii. !oof top rainwater harvesting

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    Components of the roof top rainwater

    harvesting system

    Components of the roof top rainwater harvesting system

    Catchment

    &ransportation

    irst flush

    ilter

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    Sand (ravel ilter

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    Charcoal ilter

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    P'C- Pipe filter+

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    ME&H01S 0 !00 &0P !"#$%"&E! H"!'ES$(

    Storage of 1irect use

    !echarging ground water auifers

    a. !echarging of *ore wells*. !echarging of dug wells+

    c. !echarge pits

    d. !echarge &renches

    e. Soa2 ways or !echarge Shafts

    f. Percolation &an2s

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    !echarging of *ore wells

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    !echarge Pits

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    Soa2 away or !echarge Shafts

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    !echarging of dug wells

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    !echarge &renches