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    UNIT -1

    INTRODUCTION

    Importance of Irrigation

    Definition Irrigation is the controlled application of water to croplands. Its

    primary objective is to create an optimal soil moisture regime

    for maximizing crop production and quality while at the same

    time minimizing the environmental degradation inherent in

    irrigation of agricultural lands

    Estimates of magnitude world-wide: 544 million acres

    (17% of land 1/3 of food production)Purpose

    Raise a crop where nothing would grow otherwise (e.g., desert areas) Grow a more profitable crop (e.g., alfalfa vs. wheat) Increase the yield and/or quality of a given crop (e.g., fruit) Increase the aesthetic value of a landscape (e.g., turf, ornamentals) Providing insurance against short duration droughts Reducing the hazard of frost (increase the temperature of the plant) Reducing the temperature during hot spells Washing or diluting salts in the soil Softening tillage pans and clods

    Delaying bud formation by evaporative cooling Promoting the function of some micro organisms

    Reasons for yield/quality increase

    Reduced water stress Better germination and stands Higher plant populations More efficient use of fertilizer Improved varieties

    Other Benefits of Irrigation

    Increase in Crop Yield Protection from femine

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    Cultivation of superior crops Elimination of mixed cropping: Economic development Hydro power generation Domestic and industrial water supply

    Methods of Irrigation

    Under gravity irrigation, water is distributed by means of open canals and

    conducts with out pressure. Gravity irrigation methods are less expensive,

    but requires more skill and experience to achieve rescannable efficiency.

    This method also requires that the land to be irrigated should have a flatter

    slope, other wise the cost of land leveling and preparation at times be come

    very high. Gravity irrigation method. Includes furrow, boarder, basin, wild-

    flooding and corrugation.

    1. Furrow irrigation

    In this method of surface irrigation, water is applied to the field by furrow

    which are small canales having a continuous our nearly uniform slope in the

    direction of irrigation. Water flowing in the furrow into the soil spreads

    laterally to

    irrigate the area between furrows.

    The rate of lateral spread of water in the soil depends on soil type.i.e. For a

    given time, water will infiltrate more vertically and less laterally in relatively

    sandy soils than in clay soil.

    Where the land grade is less than 1% in the direction of furrow, striate

    graded furrows may be adapted. The grade can be as much as 2 to 3%

    depending on the soil type and the rainfall intensity, which affects erosion.

    When field sloped is too steep to align the furrows down the slope, control

    furrows which run along curved routed may be used. Spacing of furrowsdepends on the crop type and the type of machinery used for cultivation and

    planting.

    Length of furrows depends largely on permeability of the soil, the available

    labor and skill, and experiences of the irrigation.

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    Flow rates are related to the infiltration to the rate of the soil.

    Longitudinal slope of furrow depends up on the soil type, especially its

    errodiability and the velocity of flow.

    slope may be related to discharge as follows.

    2. Boarder - strip Irrigation

    The farms are divided into number of strips of 5 to 20 meters wide and 100

    to 400 meters long. Parallel earth bunds or levees are provided in order to

    guide the advancing sheet of water.

    Recommended safe limits of longitudinal slope also depends on the soil

    texture:

    Sandy loam to sandy soils 0.25 - 0.6%

    Medium loam soils 0.2 - 0.4%

    Clay to clay loam soils 0.05 - 0.2%

    3. Basin irrigation

    Large stream of water is applied to almost level and smaller unit of fields

    which are surrounded by levees or bunds. The applied water is retained in

    the basin until it filtrates.

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    Soil type, stream size and irrigation depth are the important factors

    indeterming the basin area.

    Method of irrigation Type of Crop suited

    Border strip method Wheat, Leafy vegetables, Fodders

    Furrow method Cotton, Sugarcane, Potatoes

    Basin method Orchard trees

    4. Wild flooding

    Water is applied all over the field especially, before plowing for soil that

    can't be plowed when dry.

    Under closed conduit- there are two types of irrigation

    1. Sprinkler2. Drip irrigation

    1. Sprinkler irrigation:

    It is mostly used for young growth, to humid the atmosphere, for soil

    compaction( specially for sandy loam soils before planting, for land having

    up and down slope and used to wash out plant leaves especially in dustyarea.

    Sprinkler irrigation offers a means of irrigating areas which are so irregular

    that they prevent use of any surface irrigation methods. By using a low

    supply rate, deep percolation or surface runoff and erosion can be

    minimized. Offsetting these advantages is the relatively high cost of the

    sprinkling equipment and the permanent installations necessary to supply

    water to the sprinkler lines.

    Very low delivery rates may also result in fairly high evaporation from the

    spray and the wetted vegetation. It is impossible to get completely uniform

    distribution of water around a sprinkler head and spacing of the heads must

    be planned to overlap spray areas so that distribution is essentially uniform

    Advantages

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    Economical to labour & uniform distribution.2. Drip irrigation

    This is used especially where there is shortage of water and salt problem.

    The drip method of irrigation, also called trickle irrigation. The method isone of the most recent developments in irrigation. It involves slow and

    frequent application of water to the plant root zone and enables the

    application of water and fertilizer at optimum rates to the root system.

    It minimizes the loss of water by deep percolation below the root zone or by

    evaporation from the soil surface. Drip irrigation is not only economical in

    water use but also gives higher yields with poor quality water.

    Advantages

    No loss. of water because all water drops at root zone. No water logging and rise of water table at result salinity

    problems caused by this irrigation type is almost nil.

    Uniform distribution of water. Good water management. Economical use of lobour.

    CONSUMPTIVE USE OF WATER

    The amount of irrigation water that is needed depends not only on the

    amount of water already available from rain fail, but also on the total

    amount of water needed by the various crops.

    IRRIGATION WATER NEED = Crop water need available rain fall

    The first thing you need to consider when planning your garden is what

    growing zone you live in.

    This is based on both the temperature range of your climate and the amountof precipitation. Take a close look at the area in which you are going to

    plant your garden. If the ground tends to be very moist, choose plants that

    can tolerate constantly wet soil, and even standing water.

    If you live in an area that suffers from frequent droughts, however, select

    plants that can tolerate going long periods without water, especially in light

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    of the frequent watering restrictions imposed on such areas.

    If you are lucky enough to live in an area that has a balanced climate, you

    have a wider range of choices for your plants.

    Low Water Requirement Plants

    Plants that require low levels of

    water are often called drought

    tolerant. Drought-tolerant plants

    can thrive in hot, dry conditions

    with very little water. They

    include both perennials and

    annuals. Most drought-tolerant

    plants only have to be hand-

    watered when they are plantedand while they are establishing

    themselves. After that, they can be left to the natural cycle of the elements.

    Popular drought tolerant trees include the red cedar. live oak, crape myrtle,

    and the windmill and saw palmetto palm trees. All citrus trees are also

    drought tolerant. Many homeowners in areas prone to drought, such as parts

    of the southern United States, use shrubs and ground covering vines as part

    of their landscaping. These include Texas sage, orange jasmine and Chinese

    fountain grass. There are not many perennial drought-tolerant plants, but

    amaryllis is one that is very popular, along with the African iris. Populardrought-olerant annuals include marigold, cosmos and the Dahlberg daisy.

    Mid-Level Water Requirement Crops

    Most plants land in this range when it comes to water requirements. These

    plants do not need to be watered every day, but they need to be watered

    when the soil has been dry for over a week or two. Sometimes these plants

    are classified as plants lying in the "occasional water zone". These include

    popular plants such as geraniums, most roses, wisteria, clematis and other

    vine plants, sunflowers, spring flowering bulbs, and most floweringperennial shrubs. Note that flowering annuals planted in containers will need

    watering at least once or twice a week, while annuals planted in the ground

    will need watering less often.

    High Water Requirement Plants

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    Some plants require large amounts of water. These plants typically grow in

    marshy areas or bogs, or along the banks of rivers, streams and lakes. The

    soil for these plants should always be kept moist. Standing water is not a

    concern for these plants, so you don't have to worry about root rot.

    Perennials are especially good for wet areas because they don't have to bereplanted year after year, which can be difficult in marshy areas. Popular

    perennials for wet soil include iris plants, cannas, bee balms, ferns, and bog

    salvia. Aquatic mint is a pleasant ground cover that likes wet soil. The red

    osier dogwood does very well in wet conditions. Most annual flowering

    plants also do well in constantly moist soil.

    Water Requirement of Different Crops

    Amount of water required by a crop in its whole production period is called

    water requiremrnt. The amont of water taken by crops vary considerably.

    What crops use more water and which ones less.......

    Crop

    Water

    Requirement

    (mm)

    Rice 900-2500

    Wheat 450-650

    Sorghum 450-650

    Maize 500-800

    Sugarcane 1500-2500

    Groundnut 500-700

    Cotton 700-1300

    Soybean 450-700

    Tobacco 400-600

    Tomato 600-800

    Potato 500-700

    Onion 350-550

    Chillies 500

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    Sunflower 350-500

    Castor 500

    Bean 300-500

    Cabbage 380-500

    Pea 350-500

    Banana 1200-2200

    Citrus 900-1200

    Pineapple 700-1000

    Gingelly 350-400

    Ragi 400-450

    Grape 500-1200

    Irrigation water requirement

    This case study shows how to calculate the total water requirement for a

    command area (irrigation blocks) under various crops, soil textures and

    conveyance loss conditions. In order to evaluate the required irrigation gift

    for the entire command area a simple water balance has to be set-up. Thetotal water demand for each irrigation block and the crops in each block are

    calculated by summing the following components:

    infiltration (percolation loss) through the soil (I)

    seepage (conveyance loss) through the channel (S)

    maximum evapotranspiration of the crop (ETm)

    In this exercise, the irrigation water requirement is calculated for a 10-day

    period during the harvest stage.

    Evaluation of Percolation loss (I)

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    The command area is divided in irrigation blocks. First, these irrigation

    blocks are crossedwith the soil texture map to determine the area of each

    soil texture class in each block.

    Percolation losses differ per soil texture class so a table with the following

    percolation data is created:

    TexturePercolation loss

    (mm/day)

    Clay 4

    Loam 12

    Sandy clay 14

    Clay loam 7

    The percolation table isjoinedwith the cross table to get the percolation foreach soil texture class in each block. The amount of water loss for each soil

    texture class per block is calculated with a tabcalc statement. In order to get

    the total percolation loss per block the results of the previous operation are

    aggregated.

    Evaluation of Conveyance loss (S)

    Conveyance losses are calculated in about the same way as the percolation

    losses. First, the map with the irrigation blocks is crossedwith the channel

    distribution map. The conveyance loss per meter channel length differs per

    channel type and is 0.2 m per day for clay channels and 0.01 m per day for

    concrete channels. A new table indicating water loss per channel type is

    created andjoinedto the cross table. The amount of water loss for each type

    of channel per block is calculated with a simple tabcalc formula. Finally the

    results are aggregatedto evaluate the total conveyance loss per irrigation

    block.

    Evaluation of maximum evapotranspiration (ETm)

    Crop water requirements are normally expressed by the rate of

    evapotranspiration (ET). The evaporative demand can be expressed as the

    reference crop evapotranspiration (ETo) which predicts the effect of climate

    on the level of crop evapotranspiration. In this case study the ETo is 8

    mm/day. Empirically-determined crop coefficients (kc) can be used to relate

    ETo to maximum crop evapotranspiration (ETm) when water supply fully

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    meets the water requirement of the crop. The value of kc varies with crop

    and development stage. The kc values for each crop and development stage

    are available in a table.

    For a given climate, crop and crop development stage, the maximum

    evapotranspiration (ETm) in mm/day of the period considered is:

    ETm = kc * ETo

    Maximum evapotranspiration refers to conditions when water is adequate for

    unrestricted growth and development under optimum agronomic and

    irrigation management. Maximum evapotranspiration is calculated in this

    case study by crossing the irrigation block map with the map that shows the

    different crop types in the command area,joining the cross table with the kc

    table and by applying the maximum evapotranspiration formula with atabcalc statement.

    Water balance calculation (S+I+ETm)

    The required irrigation gift for the entire command area is equal to the sum

    of water losses due to infiltration through the soil (I), seepage through the

    channel (S) and maximum evapotranspiration (ETm) for each block. The

    total amount of water requirement in harvest period for each block is

    reclassifiedin irrigation classes using the following table:

    Upper

    boundary

    Irrigation

    class

    4000 1

    6000 2

    8000 3

    10000 4

    12000 5

    14000 6

    Finally, you will create a script to automate the calculation procedure. With

    the script, you can easily calculate the water requirements for other growing

    stages.

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    Factors Influencing Crop Water Requirements for Irrigation

    i. Influence of climate

    A certain crop grown in a sunny and hot climate needs more water per day

    than the same crop grown in a cloudy and cooler climate. There are,

    however, apart from sunshine and temperature, other climatic factors which

    influence the crop water need. These factors are humidity and wind speed.

    When it is dry, the crop water needs are higher than when it is humid. In

    windy climates, the crops will use more water than in calm climates.

    The highest crop water needs are thus found in areas which are hot, dry,

    windy and sunny. The lowest values are found when it is cool, humid and

    cloudy with little or no wind.

    From the above, it is clear that the crop grown in different climatic zones

    will have different water needs. For example, a certain maize variety grown

    in a cool climate will need less water per day than the same maize variety

    grown in a hotter climate.

    Effect of major Climatic Factors on Crop Water Needs

    Climatic factor Crop water need

    High Low

    Sunshine sunny (no clouds) cloudy (no sun)

    Temperature hot cool

    Humidity low (dry) high (humid)

    Wind speed windy little wind

    Table - AVERAGE DAILY WATER NEED OF STANDARD GRASS

    DURING IRRIGATION SEASON (mm)

    Climatic zone Mean daily temperature

    low (< 15C) medium (15-25C) high (> 25C)

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    Desert/arid 4-6 7-8 9-10

    Semi-arid 4-5 6-7 8-9

    For the various field crops it is possible to determine how much water they

    need compared to the standard grass. A number of crops need less waterthan grass, a number of crops need more water than grass and other crops

    need more or less the same amount of water as grass. Understanding of this

    relationship is extremely important for the selection of crops to be grown in

    a water harvesting scheme (see Chapter 6, Crop Husbandry).

    Table - CROP WATER NEEDS IN PEAK PERIOD OF VARIOUS

    CROPS COMPARED TO THE STANDARD GRASS CROP

    -30% -10% Same as Standard Grass +10% +20%Citrus

    Olives

    Squash Crucifers

    Groundnuts

    Melons

    Onions

    Peppers

    Grass

    Clean cultivated nuts & fruit

    trees

    Barley

    Beans

    Maize

    Cotton

    Lentils

    Millet

    Safflower

    Sorghum

    Soybeans

    Sunflower

    Wheat

    Nuts & fruit trees with

    cover crop

    ii. Influence of crop type on crop water needs

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    As different crops require different amount of water for maturity, duties are

    also required. The duty would vary inversely as the water requirement of

    crop.

    The influence of the crop type on the crop water need is important in two

    ways.

    a. The crop type has an influence on the daily water needs of a fully grown

    crop; i.e. the peak daily water needs of a fully developed maize crop will

    need more water per day than a fully developed crop of onions.

    b. The crop type has an influence on the duration of the total growing season

    of the crop. There are short duration crops, e.g. peas, with a duration of the

    total growing season of 90-100 days and longer duration crops, e.g. melons,

    with a duration of the total growing season of 120-160 days. There are, ofcourse, also perennial crops that are in the field for many years, such as fruit

    trees.

    While, for example, the daily water need of melons may be less than the

    daily water need of beans, the seasonal water need of melons will be higher

    than that of beans because the duration of the total growing season of melons

    is much longer.

    Data on the duration of the total growing season of the various crops grown

    in an area can best be obtained locally. These data may be obtained from, forexample, the seed supplier, the Extension Service, the Irrigation Department

    or Ministry of Agriculture.

    Table gives some indicative values or approximate values for the duration of

    the total growing season for the various field crops. It should, however, be

    noted that the values are only rough approximations and it is much better to

    obtain the values locally.

    There are three broad classes of irrigation systems:

    Pressurized distribution

    Gravity flow distribution

    Drainage flow distribution.

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    1. Pressurized Distribution

    The pressurized systems include sprinkler, trickle, and the array of similar

    systems in which water is conveyed to and distributed over the farmland

    through pressurized pipe networks. There are many individual system

    configurations identified by unique features (centre-pivot sprinkler

    systems).

    2. Gravity Flow Irrigation System

    Gravity flow systems convey and distribute water at the field level by a free

    surface, overland flow regime. These surface irrigation methods are also

    subdivided according to configuration and operational characteristics.

    3. Control of drainage flow irrigation System

    Irrigation by control of the drainage system, subirrigation, is not common

    but is interesting conceptually. Relatively large volumes of applied irrigation

    water percolate through the root zone and become a drainage or groundwater

    flow. By controlling the flow at critical points, it is possible to raise the level

    of the groundwater to within reach of the crop roots. These individualirrigation systems have a variety of advantages and particular applications.

    Irrigation systems are often designedto maximize efficiencies and minimize

    labour and capital requirements. The most effective management practices

    are dependent on the type of irrigation system and its design. For example,

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    management can be influenced by the use of automation, the control of or

    the capture and reuse of runoff, field soil and topographical variations and

    the existence and location of flow measurement and water control structures.

    Questions that are common to all irrigation systems are when to irrigate,

    how much to apply, and can the efficiency be improved. A large number of

    considerations must be taken into account in the selection of an irrigation

    system. These will vary from location to location, crop to crop, year to year,

    and farmer to farmer.

    Compatibility of the irrigation systems:

    The irrigation system for a field or a farm must be compatible with the other

    existing farm operations, such as land preparation, cultivation, and harvest.

    Level of Mechanization

    Size of Fields

    Cultivation

    Pest Control

    Topographic Limitations.

    Restrictions on irrigation system selection due to topography include:

    groundwater levels

    the location and relative elevation of the water source,

    field boundaries,

    acreage in each field,

    the location of roads

    power and water lines and other obstructions,

    the shape and slope of the field

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    UNIT-2&4

    IRRIGATION METHOD

    CANAL IRRIGATION

    Cheap labour and availability of cement reduces the cost of canal

    construction

    Huge quantities of water from Monsoon rainfall & melting of snow can be

    stored in reservoirs during summer season.

    Irregular supply of water in the rivers is then regulated by construction of

    dams & barrages. Canal system irrigates a vast area. Even the deserts have

    been made productive.

    TANK IRRIGATIONIndia, an irrigation tank or tank is an artificialreservoirof any size. (The word sagar

    refers to a large lake, usually man-made).[1]

    It can also have a natural or man-madespring included as part of a structure. Tanks are part of an ancient tradition of harvesting

    and preserving the local rainfall and water from streams and rivers for later use,primarily for agriculture and drinking water, but also for sacred bathing and ritual. Often

    a tank was constructed across a slope so to collect and store water by taking advantageof local mounds and depressions.

    [2]Tank use is especially critical in parts ofSouth India

    withoutperennialrainfall where water supply replenishment is dependent on a cycle ofdry seasons alternating with monsoon seasons.

    Causes:

    Abundance of silt eroded from the Karakoram, Hindu Kush and Himalayan

    mountains.

    Deforestation - ruthless cutting of trees for fuel and timber. Rivers form

    narrow and deep valleys in the mountainous areas. Most of the eroded

    material is washed down into the plains and piles up in reservoirs of the

    dams.

    Effects:

    Blockage of canals because silt accumulates. Weakens the foundation of dams. Reduced capacity of reservoir and less flow of water affects the

    generation of hydro-electric power. It also results in availability of

    less water for irrigation purposes.

    http://en.wikipedia.org/wiki/Indiahttp://en.wikipedia.org/wiki/Indiahttp://en.wikipedia.org/wiki/Reservoirhttp://en.wikipedia.org/wiki/Reservoirhttp://en.wikipedia.org/wiki/Reservoirhttp://en.wikipedia.org/wiki/Irrigation_tank#cite_note-glossary-0#cite_note-glossary-0http://en.wikipedia.org/wiki/Irrigation_tank#cite_note-glossary-0#cite_note-glossary-0http://en.wikipedia.org/wiki/Irrigation_tank#cite_note-glossary-0#cite_note-glossary-0http://en.wikipedia.org/wiki/Irrigation_tank#cite_note-Tank_management-1#cite_note-Tank_management-1http://en.wikipedia.org/wiki/Irrigation_tank#cite_note-Tank_management-1#cite_note-Tank_management-1http://en.wikipedia.org/wiki/Irrigation_tank#cite_note-Tank_management-1#cite_note-Tank_management-1http://en.wikipedia.org/wiki/South_Indiahttp://en.wikipedia.org/wiki/South_Indiahttp://en.wikipedia.org/wiki/South_Indiahttp://en.wikipedia.org/wiki/Perennial_planthttp://en.wikipedia.org/wiki/Perennial_planthttp://en.wikipedia.org/wiki/Perennial_planthttp://en.wikipedia.org/wiki/Perennial_planthttp://en.wikipedia.org/wiki/South_Indiahttp://en.wikipedia.org/wiki/Irrigation_tank#cite_note-Tank_management-1#cite_note-Tank_management-1http://en.wikipedia.org/wiki/Irrigation_tank#cite_note-glossary-0#cite_note-glossary-0http://en.wikipedia.org/wiki/Reservoirhttp://en.wikipedia.org/wiki/India
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    Flow of floodwater is hampered which may cause heavy damage tothe dam because of mounds of silt which block the flow of water.

    Large-scale afforestation especially on the foothills of Himalayas. Cemented embankment of canals. .

    Installation of silt trap before the water flows to the dams. Structural measures such as operating the reservoir at lower level

    during flood and allowing free flow during low flow season for

    sluicing sediments from the reservoir.

    Uses of CANAL Irrigation:

    1. Soft soil and level land of the Indus Plain makes digging of canalseasier than in the rugged lands of Balochistan.

    2. By canal irrigation millions of gallons of water are utilized that wouldflow into the Arabian Sea.

    3. Cheap labour and availability of cement reduces the cost of canalconstruction

    4. Canal system irrigates a vast area. Even the deserts have been madeproductive.

    5. Irregular supply of water in the rivers is then regulated byconstruction of dams & barrages.

    6. Huge quantities of water from Monsoon rainfall & melting of snowcan be stored in reservoirs during summer season.

    7. Southward slope of the rivers makes construction of canals easier,because water flows southwards naturally.

    Lining of Irrigation CanalsMost of the irrigation channels in Iraq are earthen channels. The

    major advantage of an earth channel is its low initial cost, these suffer

    from certain disadvantages, like the following:-

    1- Maximum velocity limited to prevent erosion.

    2- Seepage of water into the ground.

    3- Possibility of vegetation growth in banks, leading to increased friction.4-Possibility of bank failure, due to erosion.

    5-More maintenance requirement.Types of Canal LiningTypes of lining are generally classified according to the materials

    used for their construction. Concrete, rock masonry, brick masonry,

    bentonite-earth mixtures, natural clays of low permeability, and different

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    mixtures of rubble, plastic, and asphaltic materials are the commonly

    used materials for canal lining. The suitability of the lining material is

    decided by:

    A- Economy.

    B- Structural stability.

    C- Resistance to erosion.

    E- Durability.

    F- Hydraulic efficiency.

    [A] Concrete Lining[B] Precast concrete lining[C] Shotcrete Lining[D] Bricks, Tiles and Stone lining[E] Asphaltic Lining[F] Earth Linings1- Stabilized Earth LiningsSub-grade is stabilized using either clay for granular subgrade or by

    adding chemicals that compact the soil.

    2- Loose Earth Blankets

    Fine grained soil is laid on the sub grade and evenly spread. However,

    this type of lining is subject to erosion, and requires a flatter side slopes

    of canal.

    3- Compacted Earth Linings

    The graded soil containing about 15 percent clay is spread over thesubgrade and compacted.

    4- Buried Bentonite Membranes

    Bentonite is a special type of clay soil, found naturally, which swell

    considerably when wetted.

    5- Soil-cement Linings:These linings are constructed using cement (15 to 20 per cent by

    volume) and sandy soil (not containing more than about 35 per cent of silt

    and clay particles). Cement and sandy soil can be mixed in place and

    compacted at the optimum moisture content. This method of construction

    is termed the dry-mixed soil-cement method.

    3- Failure of Canal LiningThe main causes of failure of lining are the water pressure that

    developed behind the lining material due to high water table, saturation

    of the embankment by canal water, sudden lowering of water levels in the

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    channel, and saturation of the embankment sustained by continuous

    rainfall. When the water level in canal was raised and lowered the banks

    suffering from instability due to erosion and seepage through the banks

    may be occurs. In order to minimize the seepage, a secondary berms were

    constructed along the length of bank at various locations.Diversion head works: Weirs and Barrages, Layout of diversion head works andcomponents, failure of hydraulic structures on previous foundations, Blighs Creep

    theory, Lanes weighted theory and Khoslas theory, concept of low net, u/s and d/scutoffs and protection measures, design of vertical drop weir.

    Canal Structures: Types of falls and their location, design principles and Trapezoidalnotch fall, siphon well drop, straight glacis fall. Canal regulation works, alignment of off

    taking canal. Distributary head regulators and cross regulation and their design. Canalescapes, types of metering flumes, types of canal modules and proportionality,

    sensitivity, flexibility.

    Cross Drainage Works: Definition, classification, design principles of aqueducts,siphon aqueducts, canal siphons, super passages and inlet and outlets, selection of crossdrainage works.

    Bridges and Culverts: Discharge, Waterway and sour depth computations, Depth of

    Bridge foundation, spans and vertical clearance, efflux computations, pipe culverts andbox culverts.

    Water Power: Classification of Hydropower plants, definitions pf terms, load, head,power, efficiency, load factor, installed capacity, utilization factor, capacity factor, use of

    mass curve and flow duration curve. Components of power plant-intakes, fore/bay,

    penstocks, functions and types of sewage tanks, General arrangement of power house,sub-structure and super-structure.

    .

    Design of HydraulicStructures

    Design of HydraulicStructuresCOURSE Contents

    1. Introduction

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    2. Gravity Dams Site selection,

    Forces,

    Stability analysis.3. Diversion Works Weirs and

    Barrages

    4. Canals Design and Canal Falls.

    5. Cross Drainage Works

    6. Head Regulators and Crossregulators

    IS CodesIS Code 6512: Criteria for Design of Solid Gravity

    Dams

    IS Code 1893: Criteria for Earthquake ResistantDesign of Structures

    IS Code 7784-Cross-Drainage Works: Part 1 -

    General

    IS Code 7784- Cross-Drainage Works: Part 2 -

    Aqueduct

    IS Code 7784- Cross-Drainage Works: Part 2

    Syphon AqueductIS Code 7784- Cross-Drainage Works: Part 2

    Canal Syphon

    IS Code 7784- Cross-Drainage Works: Part 2

    Superpassage

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    IS Code 7784- Cross-Drainage Works: Part 2

    Level Crossing

    UNIT-3 DIVERSION AND IMPOUNDING STRUCTURES

    Why study Hydraulic Structures?

    INTRODUCTIONDevelopment of water resources of

    a region

    Requires

    Conception

    Planning

    Design

    Construction

    Operation

    of various facilities to utilise andcontrol water, and

    to maintain water quality.

    Utilize/Need water

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    Domestic & Industrial uses

    Irrigation

    Power generationNavigation

    Other purposes

    Water Resources Engineering

    Utilisation of water

    Control of waterWater quality management

    Water is controlled and regulated

    Flood control

    Land drainage

    Sewerage

    Bridges

    Not cause damage to property,

    inconvenience to the

    public, or loss of lifeWater-quality management

    Required quality of water for

    different uses

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    Preserve Ecological balance

    Contamination of

    Groundwater/Surface waterWater Resources development

    projects are planned

    to serve various purposes

    Main Purposes

    Domestic & Industrial uses,Irrigation

    Power generation, Navigation,

    Flood control

    Secondary Purposes

    Recreational, Fish and wild life,

    Drainage control,

    Watershed management, Sediment

    control,

    Salinity control, Pollutionabatement

    Miscellaneous Purposes

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    Employment, Accelerate

    development etc

    Single-purpose andMulti-purposeWater Resources projects Two

    Main Steps

    First step How much water is

    available?

    Knowledge of HydrologyPrecipitation average

    Abstraction Losses

    Runoff, Yield of basin

    Flood Peak runoff

    Reservoir sizing Mass curve

    Second step How to utilise and

    control water?

    Require various structure

    Hydraulic StructuresTypes of Hydraulic Structures

    Storage

    Diversion

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    Transportation

    Regulation

    ControlMain source of water is

    Precipitation

    Precipitation is not uniform over

    space and time

    Monsoon, North East, Himalaya,W. Ghat

    Store water at surplus location

    during surplus

    period Storage structures

    Reservoirs

    Dam and Reservoir coexist

    Dam solid barrier across river

    Reservoir artificial lake u/s of

    damReservoirDam

    Reservoir

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    Dam Spillway

    RESERVOIRS RESERVOIRSTypes of Reservoirs Single-purposeand Multi-purpose

    Storage (or conservation) reservoirs

    Flood control reservoirs

    Multipurpose reservoirDistribution reservoirs

    Balancing reservoirs

    Flood Control runoff exceeding

    safe capacity of

    river is stored in the reservoir.

    Stored water is

    released in controlled manner

    Detention Reservoirs regulated byGATES

    Adv: More flexibility of operation andbetter control of

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    outflow; Discharge from various

    reservoirs can be adjusted

    Disadv: More expensive; Possibility ofhuman error

    Retarding Reservoirs UNGATES

    Adv: Less expensive; Outflow is

    automatic so possibility ofhuman error

    Disadv: No flexibility of operation;Discharge from various

    reservoirs may coincide heavy flood

    Multipurpose ReservoirsServe two or more purposes. In India,

    most of the reservoirs

    are designed as multipurpose reservoirs

    to store water for

    irrigation and hydropower, and also toeffect flood control

    Distribution Reservoirs

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    Serve two or more purposes. In India,

    most of the reservoirs

    are designed as multipurpose reservoirsto store water for

    irrigation and hydropower, and also to

    effect flood control

    Distribution ReservoirsSmall storage reservoirs to tide over the

    peak demand ofwater. The distribution reservoir is

    helpful in permitting

    the pumps to work at a uniform rate. It

    stores water

    during the period of lean demand andsupplies the same

    during the period of high demand. As the

    storage is

    limited, it merely helps in distribution of

    water as per

    demand for a day or so and not forstoring it for a long

    period. Distribution reservoirs are mainly

    used for

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    municipal water supply but rarely used

    for the supply of

    water for irrigation.RESERVOIRS RESERVOIRSBalancing ReservoirsA balancing reservoir is a small reservoir

    constructed d/s of

    the main reservoir for holding waterreleased from the

    main reservoir.

    RESERVOIRS RESERVOIRSStorage Capacity of ReservoirsStorage capacity of a reservoir depends

    upon the topography of

    the site and the height of dam.

    Engineering surveys

    The storage capacity and the water

    spread area at different

    elevations can be determined from thecontour map.

    In addition to finding out the capacity of

    a reservoir, the

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    contour map of the reservoir can also be

    used to determine

    the land and property which would besubmerged when the

    reservoir is filled upto various elevations.

    To estimate the compensation to be paid

    to the owners of the

    submerged property and land. The time

    schedule,according to which the areas should be

    evacuated, as the

    reservoir is gradually filled, can also be

    drawn..

    UNIT-5

    IRRIGATION WATER MANAGEMENT

    Both the elevation-area curve and the

    elevation- storage curve on

    the same paper. Abscissa - areas and

    volumes - opposite

    di ti

    Area-Elevation Curve

    from contour map An

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    elevation-area curve is

    then drawn between

    the surface area asabscissa and the

    elevation as ordinate.

    Elevation-Capacity

    Curve: is determined

    from elevation-area

    curve using diffformulae.

    Storage Capacity calculation

    formulae

    1. Trapezoidal formula2. Cone formula

    3. Prismoidal formula

    4. Storage Volume from cross-sectional

    areas

    Basic Terms and Definitions1. Full reservoir level (FRL): is the

    highest water level to which

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    the water surface will rise during normal

    operating

    conditions. Also called the full tank level(FTL) or the

    normal pool level (NPL).

    2. Maximum water level (MWL): is the

    maximum level to which

    the water surface will rise when the

    design flood passes overthe spillway. Also called the maximum

    pool level (MPL) or

    maximum flood level (MFL).

    3. Minimum pool level: is the lowest level

    up to which the water

    is withdrawn from the reservoir under

    ordinary conditions.

    It corresponds to the elevation of the

    lowest outlet (or

    sluiceway) of the dam. However, in the

    case of a reservoir forhydroelectric power; the minimum pool

    level is fixed after

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    considering the minimum working head

    required for the

    efficient working of turbines.

    Basic Terms and Definitions4. Useful storage: volume of water stored

    between the full

    reservoir level and the minimum pool

    level. Also known as

    the live storage.

    5. Surcharge storage: is the volume of

    water stored above the

    full reservoir level upto the maximum

    water level. Thesurcharge storage is an uncontrolled

    storage which exists

    only when the river is in flood and the

    flood water is passing

    over the spillway. This storage is available

    only for the

    absorption of flood and it cannot be used

    for other purposes.

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    6. Dead storage: volume of water held

    below the minimum pool

    level. The dead storage is not useful, as itcannot be used for

    any purpose under ordinary operating

    conditions.

    7. Bank storage: If the banks of the

    reservoir are porous, some

    water is temporarily stored by them whenthe reservoir is

    full.

    8. Valley storage: The volume of water

    held by the natural river

    channel in its valley upto the top of its

    banks before the

    construction of a reservoir is called the

    valley storage. May

    be important in flood control reservoirs.

    9. Yield from a reservoir: Yield is the

    volume of water whichcan be withdrawn from a reservoir in a

    specified period of

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    time. The yield is determined from the

    storage capacity of

    the reservoir and the mass inflow curve.10 Safe yield (Firm yield): is the

    maximum quantity of water

    which can be supplied from a reservoir in

    a specified period

    of time during a critical dry year. Lowest

    recorded naturalflow of the river for a number of years is

    taken as the

    critical dry period for determining the

    safe yield

    11. Secondary yield: is the quantity of

    water which is available

    during the period of high flow in the

    rivers when the yield is

    more than the safe yield. It is supplied on

    as and when basisat the lower rates. The hydropower

    developed from

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    secondary yield is sold to industries at

    cheaper rates.

    12. Average yield: is the arithmeticaverage of the firm yield

    and the secondary yield over a long

    period of time.

    13. Design yield: is the yield adopted in

    the design of a reservoir.

    Fixed after considering the urgency of thewater needs and

    the amount of risk involved. The design

    yield should be such

    that the demands of the consumers are

    reasonably met with,

    and at the same time, the storage required

    is not unduly

    large.