Water Potential Formula:
From: | To: |
Water potential (Ψ) is a measure of the potential energy of water per unit volume relative to pure water in reference conditions. It is the sum of four components: solute potential (Ψs), pressure potential (Ψp), gravity potential (Ψg), and matric potential (Ψm).
The calculator uses the water potential equation:
Where:
Explanation: The equation sums all potential components that affect water movement in plants and soils.
Details: Water potential determines the direction and rate of water movement in biological systems, crucial for understanding plant water relations, soil-plant-atmosphere continuum, and cellular water balance.
Tips: Enter all potential components in MPa (megapascals). The calculator sums them to give total water potential. Negative values indicate water potential lower than pure water.
Q1: What are typical values for water potential components?
A: Ψs is typically negative (-0.5 to -3 MPa), Ψp positive (0.3-2 MPa in turgid cells), Ψg depends on height (0.01 MPa/m), Ψm negative in dry soils.
Q2: How does water potential affect plant cells?
A: Water moves from high to low potential. When Ψ outside < Ψ inside, water enters (turgor); when Ψ outside > Ψ inside, water leaves (plasmolysis).
Q3: What's the relationship to water potential gradient?
A: The difference in Ψ between two points determines the driving force for water movement.
Q4: How is water potential measured experimentally?
A: Using pressure chambers, psychrometers, or osmometers for different components.
Q5: Why is water potential more useful than water content?
A: It directly indicates water's energy state and movement potential, regardless of system.