Skip to the content Skip to the navigation Accessibility information
Decagon Devices
Login|Register| Contact us
US: 1.800.755.2751
International: +1.509.332.2756
  • Home
  • Products
    • Water Activity
    • Environmental Instruments
    • Sensors
    • Data Loggers and Collectors
    • Environmental Monitoring Systems
    • Lysimeters and Infiltrometers
  • Services
    • Thermal Properties Testing
    • Soil Moisture Release Curve Construction
    • Campbell Scientific Data Logger Programming
    • Soil Moisture Sensor Custom Calibration
  • Support
  • News & Events
  • Where to Buy
  • About Us
    • About Us
    • Contact Us
    • Sister Companies
    • Employment
    • GA Harris Fellowship
    • People
  • Education
  • Forums
    • Soil Moisture
    • Data Loggers and Data Management
    • Canopy Measurements
    • Soil Water Potential
    • Lysimetry and Hydrology
    • Clarke Topp Twenty Questions
    • Best Practices of Soil Moisture Measurements Virtual Seminar Questions
    • Methods of Sampling and Analyzing Soil Pore Solution Virtual Seminar Questions
    • Basic Principles of Radiation Measurement to Predict ET, Climate Change, Photosynthesis and Crop Yield
    • Lysimetry Basics: Peering in to the Black Box Virtual Seminar Questions
Education
Subscribe to
newsletter
Tips, tricks, and Scholarships
Email to
a Friend
Send this page link to a friend
See Virtual
Seminars
Current and archived topics

Water Potential Theory

  • Measurements:
    • Water Potential
  • Applications:
    • Characterizing Soil Expansion,
    • Irrigation Scheduling,
    • Moisture Release Curves,
    • Plant Ecology,
    • Watershed Characterization
  • Products:
    • Water Potential Instruments,
    • HYPROP,
    • MPS-1 Dielectric water potential sensor,
    • Water Potential Sensors,
    • MPS-2 Dielectric Water Potential,
    • WP4 Dewpoint Potentiameter,
    • WP4C Dewpoint Potentiameter

Water potential is a measure of the difference in potential energy between the water in a sample and the water in a reference pool of pure, free water. Free water has a potential of zero by definition.  Since soil water generally has an energy state lower than that of pure free water, its potential usually has a negative value. The energy of soil water can be changed by changing the pressure of the water (pressure potential), changing the concentration of solutes in the water (osmotic potential), or by the adhesive and cohesive forces that bind water to solid surfaces and in capillaries of a matrix (matric potential). The energy of soil water also depends on the position of the water in a gravitational field (gravitational potential).

Water Potential Theory

Differences in water potential drive water movement from the soil to the atmosphere

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Learn about instruments that measure water potential

Read about the history of water potential

 

 

 

Visit the Soil Water Potential Forum

 

 

Sign up for News & Updates

2365 NE Hopkins Court
Pullman, WA 99163 - USA
1-800-755-2751 / Int'l: 509-332-2756
© 2013 Decagon Devices, Inc. - All Rights Reserved