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Louisiana Yards and Neighborhoods

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Gravity causes 'free' water to drain down below root zone. ... Systems Drip/Micro Irrigation ... Filtration is essential for drip or micro systems. ... – PowerPoint PPT presentation

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Title: Louisiana Yards and Neighborhoods


1
Louisiana Yards and Neighborhoods
  • Water Efficiently!

2
Water efficiently!
  • Plants
  • Soils
  • Systems
  • Mechanics

3
Plants
  • Plant water needs
  • Water movement
  • Evaporation and transpiration
  • Evapotranspiration
  • ET-LAIS (EvapoTransporation values from Louisiana
    Agriclimatic Information System)
  • Temperature vs. relative humidity

4
Plant Water Needs
  • Germination
  • Vegetative phase
  • Reproductive phase
  • Transpiration cools plant, provides suction to
    pull water and nutrients from the soil into roots
  • Plants have differing water needs

5
Water Movement
6
Evaporation and Transpiration
  • Evaporation dominates vegetative phase of growth
    and increases with increased frequency of
    irrigation.
  • Transpiration dominates reproductive phase of
    growth and is affected by plant density,
    mono-culture/mixed bed, exposure to sun, wind and
    built environment.

7
Evapotranspiration
8
ET-LAIS
  • To find ET values at LAIS weather stations
  • http//www.lsuagcenter.com/weather/Etotabledata.a
    sp
  • A description of ET use http//www.lsuagcenter.co
    m/weather/potentialUseOfETOData.asp

9
Temperature vs. Relative Humidity
10
Soil (or Media)
  • Porosity
  • Permeability
  • Field capacity
  • Wilting point
  • Available water holding capacity
  • Soil texture
  • Water intake rate and depth
  • Compaction

11
Soil Porosity
  • Volume of pore space within a given volume of
    soil ().
  • Pore spaces are available for air and/or water
    and/or roots.
  • When soil is saturated with water, there is no
    room for air.
  • Roots (of most plants) will not grow into water.

12
Soil Permeability
  • How fast can water move into/through soil
    (inches/hour)?
  • Higher in dry soil, lower in wet soil
  • Higher in soils with larger pore spaces (sands,
    loams)
  • Lower in soils with smaller pore spaces (silts,
    clays)

13
Soil Field Capacity
  • Moisture content of soil 24-48 hours after
    saturation.
  • Gravity causes free water to drain down below
    root zone.
  • Air moves into pore spaces as water drains.
  • Water is readily available to plant.
  • Moisture content at field capacity may be sand
    10, silt loam 20, clay 50.

14
Soil - Wilting Point
  • Moisture content of soil after plant has removed
    all the water it can.
  • Moisture content at wilting point may be
  • Sand 1
  • Silt loam 5
  • Clay 25

15
Soil Available Water-holding Capacity
  • Available water holding capacity (AWHC) field
    capacity minus wilting point.
  • AWHC for sand may be 10-1 9, or .09 x 12
    inches/foot 1.08 inches/foot.
  • AWHC for silt loam may be 20-5 15, or .15 x
    12 inches/foot 1.8 inches/foot.
  • AWHC for clay may be 50- 35 15, or .15 x 12
    inches/foot 1.8 inches/foot

16
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17
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18
Soil Compaction
  • Compaction reduces both porosity and
    permeability.
  • Compaction can be increased by traffic, tillage
    and chemical changes such as adding sodium or
    calcium.
  • Soil compacts easily when wet.

19
Systems
  • Garden furrow irrigation
  • Lawn sprinkler irrigation
  • Drip or micro irrigation

20
Systems Garden Furrow Irrigation
  • High losses of water to evaporation and
    percolation below root zone
  • Low distribution uniformity as water travels down
    the row
  • Short-term saturation of soil pore spaces
  • Wet furrows after irrigation

21
Systems Lawn Sprinkler Irrigation
  • If properly designed, installed, maintained and
    operated, sprinklers provide most efficient means
    for uniform irrigation of lawns.
  • Higher pressure requirements 30-60 pounds per
    square inch (psi) than furrow or drip irrigation.
  • Easily automated.

22
Systems Drip/Micro Irrigation
  • Facilitates daily or more frequent irrigation to
    reduce plant moisture stress
  • Low pressure requirements 10-15 pounds per
    square inch (psi)
  • Low flow rates gallons per hour (gph) instead of
    gallons per minute (gpm)
  • Easily modified as needed

23
Mechanics
  • Basics
  • Flow restrictions
  • Schedule 40 PVC pipe flow rates
  • Drainage

24
Mechanics Basics
  • Flow rate gallons/minute (gpm) or inches/day.
  • Pressure pounds/square inch (psi).
  • Pressure is lost from pipe friction and other
    restrictions to flow.
  • Freeze protection exposed PVC is at risk below
    20 degrees.
  • Backflow protection is essential.

25
Mechanics Basics(continued)
  • Electronic controllers available to automate
    system.
  • Filtration is essential for drip or micro
    systems.
  • Water quality check pH, salts, sodium, iron,
    manganese, calcium.
  • Chemigation is possible.
  • Maintenance is essential.

26
Mechanics Flow Restrictions
  • Water flowing through a pipe creates friction,
    which reduces pressure.
  • Changing water flow direction reduces pressure.
  • The labor to install a 1-inch pipe is the same as
    for a ¾-inch pipe, but friction losses are
    greatly reduced.

27
Mechanics Schedule 40 PVC Pipe Flow Rates
28
Mechanics Drainage
  • Design landscape to drain.
  • Surface drainage is the only practical solution.
  • Subsurface drainage is absolutely the last
    resort.
  • Divert drainage coming onto landscape from your
    roof, driveway or your neighbors yard.

29
Louisiana Yards and Neighborhoods
  • Water Efficiently!
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