Calculate total water potential from pressure and solute values.
Calculate the potential energy of water using pressure potential and solute potential. This shows how water flows in a system from higher to lower water potential. This tool is widely used in AP Biology, plant physiology, and experiments with osmosis.
You can calculate how solute concentration in a solution affects how water moves, the pressure inside cells, and how cells behave. You can also predict the direction of water movement and estimate the water potential. This Easy free calculator will help you understand how water gets in and out of cells.
The term "water potential" refers to the energy responsible for the flow of water between different regions. The water potential in pure water is higher, while adding solutes lowers the free energy of water and makes it more negative.
Where:
Where:
Water potential gradient from soil to atmosphere showing passive water movement through root hair, xylem, and leaf cells.
A plant cell has:
Calculation:
Ψ = 0.7 + (−1.2)
Ψ = −0.5 bars
Water moves toward this cell from regions with a higher water potential.
|
Component |
Symbol |
Possible Range |
Biological Meaning |
|
Total Water Potential |
Ψ |
Negative to 0 |
Predicts water movement direction |
|
Pressure Potential |
Ψp |
Positive, 0, or negative |
Turgor in turgid cells; tension in xylem |
|
Solute Potential |
Ψs |
Always ≤ 0 |
Effect of dissolved solutes on free energy |
|
Osmotic Potential |
Ψo |
Always ≤ 0 |
Synonym for solute potential |
Water movement can be explained by comparing the relative water potential of the cell. This helps determine the direction of water movement in plant cells and exam-based scenarios.
|
Cell State |
Ψp (bars) |
Ψs (bars) |
What Happens/ Exam tip |
|
Fully Turgid |
+0.5 to +1.0 |
-0.8 to -1.5 |
The cell wall exerts maximum pressure; Ψ is often close to 0. |
|
Flaccid |
0 |
< -1.5 |
No turgor, wilting, water tends to enter from the soil |
|
Plasmolyzed |
Negative |
< -2.0 |
Membrane pulls away from the wall; severe water stress; reversible if timely rehydrated |
The transport of water is passive, moving from the soil to the roots, then to the xylem, and finally into the leaves, as each section has less water potential than the last. Soil at field capacity typically has a water potential of about −0.03 MPa, while dry atmospheric air can contain a water potential of −100 MPa.
Conversion: 1 bar = 0.1 MPa = 100 kPa. AP Biology uses bars or MPa, while GCSE and A Level Biology use kPa.
|
Biological Context |
Bars |
MPa |
kPa |
|
Pure water (reference) |
0 |
0 |
0 |
|
Field capacity(soil after drainage) |
-0.3 |
-0.03 |
-30 |
|
Typical root cell water potential |
-5 |
-0.5 |
-500 |
|
Permanent wilting point of most crops |
-15 |
-1.5 |
-1500 |
|
Solute |
i Value |
Ions Produced |
Common use in Biology Labs |
|
Sucrose (C₁₂H₂₂O₁₁) |
1 |
Does not ionize |
AP Biology osmosis labs (potato, dialysis tubing) |
|
Sodium Chloride (NaCl) |
2 |
Na⁺ + Cl⁻ |
Soil salinity studies, marine plant physiology |
Dissolved solutes lower the water energy, making Ψs negative.
Yes. High pressure potential in turgid cells can make the total water potential positive.
Osmotic potential is another name for solute potential (Ψs).
Yes. Temperature changes the value of Ψs in the Van’t Hoff equation. Higher temperatures slightly reduce the magnitude of Ψs.
AP Biology uses Ψs = −iMRT in osmosis labs to calculate tissue water potential from sucrose solutions.
This calculator uses bars. AP Biology uses bars or MPa, while GCSE and A-Level Biology use kPa.