Resources | Subject Notes | Biology
Objective: Explain the importance of water potential and osmosis in the uptake and loss of water by organisms.
Water potential (Ψ) is a measure of the tendency of water to move from one area to another. It is defined as the difference in water potential between a pure solvent (usually water) and a solution.
Water potential is typically expressed in units of Pascals (Pa) or kilopascals (kPa). Pure water has a water potential of zero (Ψ = 0). Solutions with solutes have a negative water potential.
Several factors can influence water potential:
Osmosis is the net movement of water across a semi-permeable membrane from a region of high water potential to a region of low water potential.
Semi-permeable membranes allow the passage of water molecules but restrict the passage of larger solute molecules. Cell membranes are examples of semi-permeable membranes.
Water moves down the water potential gradient – from areas of higher water potential (less negative) to areas of lower water potential (more negative).
Osmotic pressure is the pressure required to prevent the flow of water across a semi-permeable membrane. It is directly related to water potential.
Plants require water for photosynthesis, turgor pressure (which provides structural support), and nutrient transport. Osmosis plays a crucial role in the uptake and loss of water in plants.
Water is absorbed by the roots from the soil via osmosis. The soil typically has a higher water potential than the root cells (due to dissolved minerals). This causes water to move into the root cells.
The pressure exerted by the cell contents against the cell wall. Turgor pressure is maintained by the influx of water through osmosis. When turgor pressure is high, the plant cells are firm and the plant is rigid.
Water is lost from the plant primarily through transpiration, which is the evaporation of water from the leaves. This creates a water potential gradient between the leaves (high water potential) and the atmosphere (low water potential), driving water movement out of the leaves.
Several factors influence the rate of transpiration:
Osmosis is essential for maintaining the water balance in animal cells.
An isotonic solution has the same water potential as the cell. There is no net movement of water across the cell membrane.
A hypotonic solution has a higher water potential than the cell. Water moves into the cell, causing it to swell and potentially burst (lysis).
A hypertonic solution has a lower water potential than the cell. Water moves out of the cell, causing it to shrink (plasmolysis).
Concept | Description |
---|---|
Water Potential (Ψ) | Measure of water tendency to move. Zero in pure water, negative in solutions. |
Osmosis | Net movement of water across a semi-permeable membrane from high to low water potential. |
Turgor Pressure | Pressure of cell contents against the cell wall, maintained by osmosis. |
Transpiration | Water loss from plants through evaporation from leaves. |
Isotonic Solution | Same water potential as the cell; no net water movement. |
Hypotonic Solution | Higher water potential than the cell; water moves into the cell. |
Hypertonic Solution | Lower water potential than the cell; water moves out of the cell. |
Suggested diagram: A diagram showing a plant cell in an isotonic, hypotonic, and hypertonic solution, illustrating plasmolysis and turgor pressure.