Water Potential () is a measure of the tendency of water molecules to move from one area to another; it is measured in units of pressure, such as kilopascals (kPa).
Pure water has the highest possible water potential, defined as kPa at standard atmospheric pressure.
The addition of solutes lowers the water potential, making the value negative; therefore, the more concentrated a solution, the more negative its water potential becomes.
The total water potential of a system is the sum of solute potential () and pressure potential (), expressed as .
| Feature | Animal Cell | Plant Cell |
|---|---|---|
| Hypotonic Effect | Swells and bursts (Cytolysis) | Becomes Turgid (Normal/Supportive) |
| Hypertonic Effect | Shrivels (Crenation) | Plasmolysed (Protoplast shrinks) |
| Structural Limit | Cell membrane only | Rigid Cell Wall |
| Ideal State | Isotonic | Hypotonic (Turgid) |
Unlike diffusion, which refers to the movement of any particle, osmosis refers specifically to the movement of water molecules.
While active transport moves substances against a gradient using energy, osmosis is always a passive movement down a water potential gradient.
Check the Signs: Always remember that water potential values are negative. A value of kPa is lower than kPa. Water always moves toward the more negative number.
Terminology Precision: Use the term 'partially permeable' rather than 'semi-permeable' to be more scientifically accurate in an exam context.
Net vs. Gross: Emphasize that water molecules move in both directions, but osmosis refers to the net (overall) movement.
Identify the Solution: Before answering, classify the external solution as hypotonic, hypertonic, or isotonic relative to the cell's cytoplasm.