Plant and Soil Water Potential Presentation

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Plant and Soil
Water Potential
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Research Background
• Hawkesbury Forest Experiment
• University of Western Sydney,
Richmond, NSW
• Whole Tree Chambers
• CO2 x Drought Experiment
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Research Background
• Ambient CO2: 380ppm
• Elevated CO2: Am + 300ppm
• Irrigated: 10mm every 3 days
• Drought: no water
• Control treatment
• My Job: The Drought
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Quantifying Drought
• Rainfall
• Soil Water Content
– Volumetric
– Gravimetric
• Soil Water Availability
– Dependent on Soil Texture
– Soil Water Potential
Image: Craig Barton
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Definition
• Water Potential:
– Free energy associated with water
– Free energy is the potential to do work
– Water moves from higher to lower potentials
– Water moves from mountains to ocean
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Definition
• Water Potential Units of Measurement:
J/kg
MPa
Bars
RH
-1
-0.001
-0.01
0.999993
-10
-0.01
-0.1
0.999926
-33
-0.033
-0.33
0.999756
-100
-0.1
-1
0.999261
-1000
-1
-10
0.992638
-1500
-1.5
-15
0.988977
-10000
-10
-100
0.928772
Air Dry
-100000
-100
-1000
0.477632
Oven Dry
-1000000
-1000
-10000
0.000618
High Potential
Field Capacity
Wilting Point
Low Potential
Source: Decagon Inc.
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Soil-Plant-Atmosphere
Continuum
Low Potential
Atmosphere = -100 Bar
Leaf air = -7.0 Bar
Leaf cell = -1.0 Bar
Trunk = -0.8 Bar
Soil = -0.33 Bar
High Potential
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Quantifying Drought - Atmosphere
• Weather Station:
– Vapour Pressure Deficit
• Armidale in Summer approx. 3 kPa
• Sydney in Summer approx. 6 kPa
• Alice Springs in Summer approx. 10 kPa
– Potential Evaportranspiration
• Penman-Montieth Equation
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Quantifying Drought - Soils
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Source: Decagon Inc.
Quantifying Drought - Soils
•
Thermocouple inside ceramic
•
Heat pulse sent through sensor
•
Temperature rise measured
•
Dry soil = large increase
•
Wet soil = small increase
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Quantifying Drought - Soils
• Thermal Matric Potential
Sensor:
– Advantages:
• Highly accurate
• Large measurement range
• Logging capability
– Disadvantages:
• Calibration required
• Careful installation
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Quantifying Drought - Soils
• Moisture Release Curves:
– Quantifying soil moisture content
Against soil water potential for
Varying Soil Textures
– Standard practice to measure
Between Field Capacity and
Graph Source:
Remko Duursma, UWS
Plant Wilting Point: -0.33 to -15 Bar
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Graph Source:
Remko Duursma, UWS
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• Moisture Release Curves:
– Advantages:
• Relatively cheap
• Established methodology
– Disadvantages:
• Time consuming (months)
• Soils highly variable
• Many curves needed
• Reliance on extrapolation
Image: Craig Barton
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Quantifying Drought - Soils
• Moisture Release Curves:
– Advantages:
• Cheap (per sample)
• Fast response time (one day)
• Many curves can be constructed
• Larger portion of curve (-1000MPa)
– Disadvantages:
• Poor resolution at wet end of curve
• (Pressure plate can resolve wet end)
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Soil-Plant-Atmosphere
Continuum
Low Potential
Atmosphere = -100 Bar
Leaf air = -7.0 Bar
?
Leaf cell = -1.0 Bar
Trunk = -0.8 Bar
Soil = -0.33 Bar
High Potential
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Quantifying Drought - Plants
• Leaf Water Potential with WP4-T:
– Advantages:
• True leaf water potential
– Disadvantages:
• Tricky methodology
• Slow response time (30 minutes)
• Rarely done
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Quantifying Drought - Plants
• Leaf Water Potential with Pressure Bomb:
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Quantifying Drought - Plants
• Leaf Water Potential with Pressure Bomb:
– Advantages:
• Proven, accurate technique
• Widely used, easy to do
• Data is potentially powerful
– Disadvantages:
• Spot measurement, destructive
• Slow sampling (for large sample size)
• Xylem water potential
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Predawn Leaf Water Potential
Ambient CO2 Results Only:
Pre-Dawn Leaf Water Potential
(MPa)
0
-0.2
-0.4
-0.6
-0.8
Irrigated
Drought
Graph Source:
David Ellsworth, UWS
-1
June
October
Nov
Dec
Jan
late Jan
Month
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Midday Leaf Water Potential
Graph Source:
David Ellsworth, UWS
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Unexpected Results
Ambient
Drought
Elevated
Drought
Graph Source:
Remko Duursma, UWS
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Combining Instruments
Leaf Water Potential + Neutron Probe Soil Moisture
Graph Source:
Remko Duursma, UWS
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Combining Instruments
Leaf Water Potential + Neutron Probe Soil Moisture
+ Soil Water Potential =
COMPLETE STORY
Elevated
Drought
Ambient
Drought
Graph Source:
Remko Duursma, UWS
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Diurnal Leaf Water Potential
Time of Day
Hydraulic Architecture?
Leaf Water Potential (MPa)
8p
m
7p
m
5p
m
3p
m
1p
m
11
am
9a
m
7a
m
What regulates Plant Water
Status?
Stomatal Closure?
5a
m
0
-0.5
-1
-1.5
-2
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Ambient
Graph Source:
Michael Forster, UWS; Derek Eamus, UTS
Elevated
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-2.5
Combining Instruments
Leaf Water Potential + Sap Flow (Tree Water Use)
Graph Source:
Michael Forster, UWS; Derek Eamus, UTS
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Combining Instruments
Time of Day
Leaf Water Potential (MPa)
8p
m
7p
m
5p
m
3p
m
1p
m
11
am
9a
m
7a
m
5a
m
0
-0.5
Graph Source:
Michael Forster, UWS; Derek Eamus, UTS
-1
-1.5
-2
Ambient
Elevated
-2.5
Slope of lines is similar
No difference in soil to leaf
hydraulic pathway
Plant water status under
control of stomata
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Combining Instruments
Leaf Water Potential + Stomatal Conductance (Porometer)
Graph Source:
David Ellsworth, UWS;
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Pressure Bomb Data
Time of Day
0
Leaf Water Potential (MPa)
m
5a
m
7a
m
9a
am
1
1
m
1p
m
3p
m
5p
m
7p
m
8p
-0.5
-1
-1.5
-2
Ambient
Elevated
-2.5
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Stem Psychrometer Data
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Graph Source:
Alec Downey, ICT International
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PSY-1 New Instrument
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Psychrometer/Hygrometer
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Psychrometer/Hygrometer
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Definition
• Water Potential Units of Measurement:
J/kg
MPa
Bars
RH
-1
-0.001
-0.01
0.999993
-10
-0.01
-0.1
0.999926
-33
-0.033
-0.33
0.999756
-100
-0.1
-1
0.999261
-1000
-1
-10
0.992638
-1500
-1.5
-15
0.988977
-10000
-10
-100
0.928772
Air Dry
-100000
-100
-1000
0.477632
Oven Dry
-1000000
-1000
-10000
0.000618
High Potential
Field Capacity
Wilting Point
Low Potential
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A New Generation
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A New Generation - Psychrometer
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The Ideal System
Atmosphere
Weather Station
WP4-C
Porometer
Leaves
Pressure Bomb
Psychrometer
Sap Flow
Thermal Matric Potential Sensor
WP4-C
Soil Moisture Sensors
Stem / Trunk
Roots
Soil
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Continuous Logging Options
Atmosphere
Weather Station
Leaves
Psychrometer
Sap Flow
Thermal Matric Potential Sensor
Soil Moisture Sensors
Stem / Trunk
Roots
Soil
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Acknowledgements
Thank you to David Ellsworth, David Tissue, Craig Barton,
Derek Eamus and Remko Duursma for kind permission to use data.
The Hawkesbury Forest Experiment involved researchers from:
University of Western Sydney, University of Technology, Sydney,
University of New South Wales, Macquarie University,
Industry & Investment, NSW, and Swedish University of Agricultural Sciences
All researchers involved with the HFE acknowledge the provision
of funding by the Australian Government's Department of Climate Change
and the Department of Agriculture, Fisheries and Forestry
for the Hawkesbury Forest Experiment.
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ICT International Pty Ltd
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sales@international.com.au
Phone: 61 2 6772 6770
Fax:
61 2 6772 7616
PO Box 503, Armidale, NSW, Australia, 2350
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