1 Part B3: Irrigation B3.1 Fundamentals of Irrigation.
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Transcript of 1 Part B3: Irrigation B3.1 Fundamentals of Irrigation.
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Part B3: Irrigation
B3.1 Fundamentals of Irrigation
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B3.1 Fundamentals of irrigationTopics
• Why irrigate?
• Water needs– Plants and water– Soil and water– The Irrigation cycle
• Available water– Mass curves, flow-duration curves
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B3.1.1 Fundamentals of irrigation Why irrigation is good
• May be the only means to permit agriculture (mainly in arid regions)
• Increase in annual yields (double cropping)
• May enable higher value crops to be grown
• Crops can be harvested at chosen times – not when the rain falls
• Yields can be controlled
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B3.1.1 Fundamentals of irrigation Why irrigation is bad
• Badly applied water can permanently damage soil– Erosion– Salination– Leaching
• Standing water can spread disease
• Social control is needed– State control – dependence, loss of control– Private control – marginalisation, loss of
control
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B3.1.1 Fundamentals of irrigation Why irrigation is bad (cont’d)
• Farmers may become vulnerable to outside forces beyond their control– Fuel for pumping– Pump competition– Competition for water sources
• Reservoirs (dams)
• Potential for failure – ruin – unrest
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B3.1.1 Fundamentals of irrigation Considerations
• Biologically optimum water may not match commercial optimum water– Water efficiency of crop
• Irrigation must exceed water deficit– Non-uniform application– Unintended losses– Irrigation water is impure (salination)
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B3.1.1 Fundamentals of irrigation Considerations
• Good management essential– Too little water – dead or stunted crop– Too much water – dead or stunted crop– Water needs met in an untimely way –
dead or stunted crop
– If water supply does not meet demand there will be conflict
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B3.1.1 Fundamentals of irrigation Considerations: Planning
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B3.1.1 Fundamentals of irrigation Considerations: Planning
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B3.1.1 Fundamentals of irrigation Considerations: Some criteria
• Energy requirement
• Capital intensity
• Labour intensity– In building– In running/maintaining
• Efficiency– Losses– Excess runoff– Excess wash through (percolation)
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B3.1.1 Fundamentals of irrigation Considerations: Water sources
Source Energy needs
Rivers either coming from a wetter zone or maintained by aquifers during dry season
low
Reservoirs or lakes filled during rains and drawn down during irrigation season
0
Naturally sustained aquifers (water stored in the ground) accessed via wells
med-high
Fossil (unsustained aquifers) until they deplete high
Artificially sustained aquifers replenished by controlled percolation or injection
med-high
Waste water from a household or a city med
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B3.1.1 Fundamentals of irrigation Considerations: Methods of application
Application method Labour Capital ‘Energy’ Efficiency
Recession irrigation low 0 0 n.a.
Gravity-fed surface methods – basin, border, furrow
low-med
low 0 0.3 – 0.6
Sub-surface pipes low high low n.k.
Pitcher/drip (continuous slow release) med high med 0.7 – 0.9
Spraying med-high
high high 0.6 – 0.8
Bucket (very small scale agriculture) v high v low 0 ~0.7
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B3.1.1 Fundamentals of irrigation Is it worth it?
• Value of crop– will it repay the investment? Is it worth
employing sophisticated methods?
• Climate – Is the land marginal? Will some temporal
readjustment be beneficial (more or better crops)?
• Topography – how will the system be laid out? Will
pumping be needed?
• Water– How much water do you need? Is it
available?
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B3.1.2 Fundamentals of irrigation Crops and water: Transpiration
convection
evaporation
Solar radiation
Reflection
long wave radiation
Measured in mm/day
Negligible thermal mass
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ETcr = Crop evapotranspiration (mm/day)
Kc = Crop coefficient
ETo = Reference crop evapotranspiration (mm/day)
B3.1.2 Fundamentals of irrigation Crops and water: Crop coefficient
cr c oET K ET
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B3.1.2 Fundamentals of irrigation Crops and water: Crop coefficient
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B3.1.2 Fundamentals of irrigation Crops and water: Crop coefficient
Relative humidity >70% (humid) <20% (dry) Growing period (days)Mid
seasonFinal
growthMid
seasonFinal
growth
Barley 1.1 0.25 1.2 0.2 120-165
Green beans 0.95 0.85 1.0 0.9 75-90
Maize 1.1 0.55 1.2 0.6 80-110
Millet 1.05 0.3 1.15 0.25 105-140
Sorghum 1.05 0.5 1.15 0.55 120-130
Cotton 1.1 0.65 1.2 0.65 180-195
Tomatoes 1.1 0.6 1.2 0.65 135-180
Cabbage/Cauliflower 1.0 0.85 1.2 0.95 80-95
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B3.1.2 Fundamentals of irrigation Crops and water: Pan coefficient
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ETcr = Reference crop evapotranspiration
Kp = Pan coefficient
Eoan =Pan evaporation
B3.1.2 Fundamentals of irrigation Crops and water: Pan coefficient
o p panET K E
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B3.1.2 Fundamentals of irrigation Crops and water: Pan coefficient
Cropped area Dry Fallow area
Humidity <40% 40-70% >70% <40% 40-70% >70%
Light wind 0.65 0.75 0.85 0.60 0.70 0.80
Moderate wind 0.60 0.70 0.75 0.55 0.65 0.70
Strong wind 0.55 0.60 0.70 0.50 0.55 0.65
Very strong wind 0.5 0.65 0.60 0.40 0.5 0.55
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B3.1.3 Fundamentals of irrigation Soil and water: The soil reservoir
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B3.1.3 Fundamentals of irrigation Soil and water: Water content of the soil
• Gravity water: Water that drains through the soil into the water table – not usually considered available to plants
• Capillary water: water held in interstices in the soil – available to plants
• Hydroscopic water: water chemically bonded to the soil - not usually considered available to plants
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B3.1.3 Fundamentals of irrigation Soil and water: Water content of the soil
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B3.1.3 Fundamentals of irrigation Soil and water: Available water
% mm/m
Fine sand 2-3% 30-50
Sandy loam 3-6% 40-100
Silt loam 6-8% 60-120
Clay loam 8-14% 90-210
Clay 13-20% 190-300
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B3.1.3 Fundamentals of irrigation Soil and water: The root zone
Used 80% of total
60%
40%
20%
Average 50%
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B3.1.3 Fundamentals of irrigation Soil and water: Available water
Root depth (full grown)
Shallow
Beans 0.6-0.7 m
Grass 0.4-0.6 m
Rice 0.5-0.7 m
Medium
Barley 1.0-1.5m
Grains (small) 0.9-1.5 m
Sweet potatoes 1.0-1.5 m
Tomatoes 0.7-1.5 m
Deep
Alfalfa 1.0-2.0 m
Orchards 1.0-2.0 m
Maize 1.0-2.0 m
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B3.1.3 Fundamentals of irrigation Soil and water: The root zone: Wilting point
Plant sucks water from interstices in soil
Less water in the soil need greater suction
At some point (the wilting point) the plant is losing more water than it is gaining
Finally, the plant uses more if its internal water than it can recover and wilts permanently
(permanent wilting point)
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Wp = Water used by plant (mm)
f = factor (~0.5)
Wa = Available water (mm/m)
Wpwp = Permanent wilting point (mm/m)
dr = Root depth (m)
B3.1.3 Fundamentals of irrigation Soil and water: Useful water
p a pwp rW f W W d
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B3.1.3 Fundamentals of irrigation Soil and water: Soil water balance
Precipitation (P)
Drainage (D) & deep percolation
Surface inflow and Irrigation (F) Runoff (R)
Evapotranspiration (E)
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S = Water stored in soil (mm)
F = Surface inflow and irrigation (mm)
P = Precipitation (mm)
E = Evapotranspiration (mm)
D = Drainage (mm)
R = Runoff (mm)
B3.1.3 Fundamentals of irrigation Soil and water: Soil water balance
S F P E D R
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B3.1.4 Fundamentals of irrigation The irrigation cycle
• When the wilting point is reached, the plant needs replenishment– Application of irrigation is needed
• Water should rise above the field capacity– Saturation, ponding, salination
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Wa = Water applied (mm)
f = factor (~0.5)
Wfc = Field capacity (mm/m)
Wpwp = Permanent wilting point (mm/m)
dr = Root depth (m)
B3.1.4 Fundamentals of irrigation The irrigation cycle: How much?
• If application is at permanent wilting point:
a fc pwp rW f W W d
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T = Time between irrigations (days)
Wa = Water applied (mm)
ETcr = Crop evapotranspiration (mm/day)
P = Precipitation (mm/day)
B3.1.4 Fundamentals of irrigation The irrigation cycle: When?
a
cr
WT
ET P
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Ta = Application time (hr)
Wa = Water applied (mm)
I = Infiltration rate (mm/hr)
B3.1.4 Fundamentals of irrigation The irrigation cycle: For how long?
aa
WT
I
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B3.1.4 Fundamentals of irrigation The irrigation cycle: For how long?: Infiltration
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B3.1.4 Fundamentals of irrigation The irrigation cycle: For how long?: Infiltration
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B3.1.4 Fundamentals of irrigation The irrigation cycle: For how long?: infiltration
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B3.1.4 Fundamentals of irrigation The irrigation cycle: For how long?: infiltration
mm/hr
Sand 30
Sandy loam 20-30
Silt loam 10-20
Clay loam 5-10
Clay 1-5
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B3.1.4 Fundamentals of irrigation The irrigation cycle: Notes
• So far we have made no account of irrigation efficiency (~0.3-0.8) so we will have to increase volume and time of application
• Water may not be available for the needed rate of application – action will need to be taken
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B3.1.5 Fundamentals of irrigation Water supply: Mass curve
0
500
1,000
1,500
2,000
2,500
3,000
1996 1997
Cu
mm
ula
tiv
e r
ain
fall
(mm
)
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Next: Irrigation techniques