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5 REASONS YOU’RE GETTING
LESS ACCURATE
SOIL MOISTURE RELEASE CURVES
Leo Rivera
METER Group, Inc.
INTRODUCTION
ABOUT ME
Background in Soil Physics & Pedology
14 years of experience measuring and
interpreting soil hydraulic properties
and soil moisture release curves
WHAT IS A SOIL MOISTURE
RELEASE CURVE?
SOIL FINGERPRINT
SOIL MOISTURE RELEASE CURVES
Two variables necessary to describe
state of matter or energy in
environment
• Extensive variable – describes the extent
or amount of matter or energy
• Intensive variable – describes the
intensity or quality of matter or energy
EXTENSIVE
INTENSIVE
WHY IS A SOIL MOISTURE
RELEASE CURVE IMPORTANT?
IMPORTANCE
HOW DO MOISTURE RELEASE CURVES
HELP US?
Soil moisture release curves unlock our
understanding of:
• How water is stored in soil
• Available water for primary productivity
• Water and solute movement in soils
This is key for:
• Optimizing water use for crops
• Modeling soil hydrology
7
MAKING DECISIONS
IRRIGATION
How can we use Soil Moisture Release
Curves to make irrigation decisions?
We need to understand both water
potential and water content
• VWC – How much irrigation to apply
• Water potential – availability of water to crops
SOIL MOISTURE RELEASE CURVE
WHAT ELSE CAN IT TELL ME?
• Shrink-swell capacity
• Cation exchange capacity
• Soil specific surface area
HOW ARE THEY MEASURED?
HOW ARE THEY MEASURED?
The earliest tools for measuring
SMRCs arose in the 1920s
They have continued to evolve
• (1920) Filter paper technique
• (1930) Pressure plate method
• (1950) Vapor method
• (1960) Evaporation method
HOW HAS TECHNOLOGY
ADVANCED OUR CAPABILITIES?
• The search for the perfect water
potential measurement
• Advancements have been slow and
dependent on evolving technology
• Searching to cover the full range
TOOLS FOR MEASURING
WATER POTENTIAL
WHAT FACTORS IMPACT
ACCURACY?
WHAT FACTORS IMPACT
ACCURACY?
MEASUREMENT METHODS
Understand the limits of different
methods
• Equilibration issues
• Getting enough measurement points
No method covers the entire range
Spatial variability (sample size)
WHAT FACTORS IMPACT
ACCURACY?
PHYSICAL & CHEMICAL TRAITS
Hysteresis
Osmotic and Matric Potential
• yT = ym + yg + yo + yp
• yT – Total water potential
• ym – matric potential - adsorption to surfaces
• yg – gravitational potential - position
• yo – osmotic potential - solutes
• yp – pressure potential - hydrostatic or pneumatic
WHAT FACTORS IMPACT
ACCURACY?
GETTING THE FULL PICTURE?
0
10
20
30
40
50
60
70
80
0.01 0.1 1 10 100
Water
Content,
%
Water Potential, -kPa
0
10
20
30
40
50
60
70
80
0.01 0.1 1 10 100 1000 10000 100000 1000000
Water
Content,
%
Water Potential, -kPa
BEST PRACTICES FOR GETTING
ACCURATE MEASUREMENTS
BEST PRACTICES
WHICH PROPERTIES ARE CRITICAL
What range of water potential is critical?
What range is the water being held?
• Coarse vs. fine textured soils
• Soilless media vs. mineral soils
0
10
20
30
40
50
60
0.1 1 10 100 1000 10000 100000 1000000
VWC,
𝝷
MATRIC POTENTIAL, -KPA
LFS (HYPROP) LFS (WP4C) LFS (Fitted Curve)
SiL (HYPROP) SiL (WP4C) SiL (Fitted Curve)
BEST PRACTICES
ACCOUNTING FOR HYSTERESIS
Accounting for hysteresis
• Wetting vs. drying curves
Evaporation method (drying curve)
Vapor pressure methods (wetting & drying)
BEST PRACTICES
CORRECTING FOR OSMOTIC POTENTIAL
Matric (ψm) vs. Osmotic potential (ψo)
• Tensiometer methods measure ψm
• Vapor pressure methods measure ψm+ ψo
Correct for ψo with saturated extract EC
BEST PRACTICES
CHOOSING THE RIGHT MODEL
Models have evolved too
How do we choose a model?
• Does the curve show bimodal characteristics?
• Is θr still relevant?
• How complex of a model is ok?
0
10
20
30
40
50
60
70
80
0.01 0.1 1 10 100 1000 10000 100000 1000000
Water
Content,
%
Water Potential, -kPa
SUMMARY
REAL-WORLD EXPERIENCE
Example:
• Plant breeding research group
• Soil type - Clay Loam
• Typical ETo - 6 to 7 mm/day
Year 1 vs. Year 2
What they implemented:
• Irrigation scheme 0.5 L/hr (30
min/30 off) @ 2-3 cycles
What was the issue?
SOILS MOISTURE RELEASE
CURVES
OTHER RESOURCES
Soil Moisture 201 Soil Moisture 202
https://www.metergroup.com/environment/master-class/
QUESTIONS
Leo Rivera
leo.rivera@metergroup.com
www.linkedin.com/in/leonardo-rivera-71422143
@countsracing

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5 Reasons You’re Getting Less Accurate Soil Moisture Release Curves

  • 1.
  • 2. 5 REASONS YOU’RE GETTING LESS ACCURATE SOIL MOISTURE RELEASE CURVES Leo Rivera METER Group, Inc.
  • 3. INTRODUCTION ABOUT ME Background in Soil Physics & Pedology 14 years of experience measuring and interpreting soil hydraulic properties and soil moisture release curves
  • 4. WHAT IS A SOIL MOISTURE RELEASE CURVE?
  • 5. SOIL FINGERPRINT SOIL MOISTURE RELEASE CURVES Two variables necessary to describe state of matter or energy in environment • Extensive variable – describes the extent or amount of matter or energy • Intensive variable – describes the intensity or quality of matter or energy EXTENSIVE INTENSIVE
  • 6. WHY IS A SOIL MOISTURE RELEASE CURVE IMPORTANT?
  • 7. IMPORTANCE HOW DO MOISTURE RELEASE CURVES HELP US? Soil moisture release curves unlock our understanding of: • How water is stored in soil • Available water for primary productivity • Water and solute movement in soils This is key for: • Optimizing water use for crops • Modeling soil hydrology 7
  • 8. MAKING DECISIONS IRRIGATION How can we use Soil Moisture Release Curves to make irrigation decisions? We need to understand both water potential and water content • VWC – How much irrigation to apply • Water potential – availability of water to crops
  • 9. SOIL MOISTURE RELEASE CURVE WHAT ELSE CAN IT TELL ME? • Shrink-swell capacity • Cation exchange capacity • Soil specific surface area
  • 10. HOW ARE THEY MEASURED?
  • 11. HOW ARE THEY MEASURED? The earliest tools for measuring SMRCs arose in the 1920s They have continued to evolve • (1920) Filter paper technique • (1930) Pressure plate method • (1950) Vapor method • (1960) Evaporation method
  • 12. HOW HAS TECHNOLOGY ADVANCED OUR CAPABILITIES? • The search for the perfect water potential measurement • Advancements have been slow and dependent on evolving technology • Searching to cover the full range
  • 15. WHAT FACTORS IMPACT ACCURACY? MEASUREMENT METHODS Understand the limits of different methods • Equilibration issues • Getting enough measurement points No method covers the entire range Spatial variability (sample size)
  • 16. WHAT FACTORS IMPACT ACCURACY? PHYSICAL & CHEMICAL TRAITS Hysteresis Osmotic and Matric Potential • yT = ym + yg + yo + yp • yT – Total water potential • ym – matric potential - adsorption to surfaces • yg – gravitational potential - position • yo – osmotic potential - solutes • yp – pressure potential - hydrostatic or pneumatic
  • 17. WHAT FACTORS IMPACT ACCURACY? GETTING THE FULL PICTURE? 0 10 20 30 40 50 60 70 80 0.01 0.1 1 10 100 Water Content, % Water Potential, -kPa 0 10 20 30 40 50 60 70 80 0.01 0.1 1 10 100 1000 10000 100000 1000000 Water Content, % Water Potential, -kPa
  • 18. BEST PRACTICES FOR GETTING ACCURATE MEASUREMENTS
  • 19. BEST PRACTICES WHICH PROPERTIES ARE CRITICAL What range of water potential is critical? What range is the water being held? • Coarse vs. fine textured soils • Soilless media vs. mineral soils 0 10 20 30 40 50 60 0.1 1 10 100 1000 10000 100000 1000000 VWC, 𝝷 MATRIC POTENTIAL, -KPA LFS (HYPROP) LFS (WP4C) LFS (Fitted Curve) SiL (HYPROP) SiL (WP4C) SiL (Fitted Curve)
  • 20. BEST PRACTICES ACCOUNTING FOR HYSTERESIS Accounting for hysteresis • Wetting vs. drying curves Evaporation method (drying curve) Vapor pressure methods (wetting & drying)
  • 21. BEST PRACTICES CORRECTING FOR OSMOTIC POTENTIAL Matric (ψm) vs. Osmotic potential (ψo) • Tensiometer methods measure ψm • Vapor pressure methods measure ψm+ ψo Correct for ψo with saturated extract EC
  • 22. BEST PRACTICES CHOOSING THE RIGHT MODEL Models have evolved too How do we choose a model? • Does the curve show bimodal characteristics? • Is θr still relevant? • How complex of a model is ok? 0 10 20 30 40 50 60 70 80 0.01 0.1 1 10 100 1000 10000 100000 1000000 Water Content, % Water Potential, -kPa
  • 23. SUMMARY REAL-WORLD EXPERIENCE Example: • Plant breeding research group • Soil type - Clay Loam • Typical ETo - 6 to 7 mm/day Year 1 vs. Year 2 What they implemented: • Irrigation scheme 0.5 L/hr (30 min/30 off) @ 2-3 cycles What was the issue?
  • 24. SOILS MOISTURE RELEASE CURVES OTHER RESOURCES Soil Moisture 201 Soil Moisture 202 https://www.metergroup.com/environment/master-class/