Lecture Outline: Diffusion & Osmosis
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- Three Major Categories of Transport Processes
- Active Transport.
- Passive Transport.
- Vesicular Transport
- Named because it uses vesicles.
- Will be discussed in a separate lecture, but is noted as one of the three mechanisms.
- Distinctions Between Active and Passive Transport
- Energy Requirement Distinction
- Both require energy for movement.
- Passive transport: Energy is built into the system (no additional energy required).
- Active transport: Requires additional energy to occur.
- The Concept of a Gradient
- Definition: A difference in measurements at two places.
- Examples: Pressure gradient, voltage (gradient of electrical potential energy).
- Concentration Gradient: Relevant type for the experiment; involves differences in solute/solvent concentration inside and outside the cell.
- Passive Transport and Diffusion
- Passive Transport Mechanism and Energy
- Driven by the gradient itself, which is a form of potential energy.
- Based on random movement in all directions (Brownian motion).
- Net effect is directional: Movement from high concentration to low concentration (down the gradient).
- Ceases when the gradient is zero (equilibrium).
- Simple Diffusion (Without a Membrane)
- Example: Sugar cube dissolving in water.
- Solutes and solvents diffuse independently down their respective gradients simultaneously.
- Diffusion Through a Selectively Permeable Membrane (SPM)
- Definition of SPM: A membrane that allows certain things through but not others.
- Requirements for Diffusion through SPM
- A gradient must be in place (the tendency).
- The particle must have a way to pass through the membrane.
- Multiple solutes diffuse independently down their own gradients.
- Osmosis: The Diffusion of Solvent (Water)
- Osmosis is a Special Case of Diffusion.
- Two Requirements for Osmosis
- The moving particle must be the solvent (water in biological systems).
- Movement must occur through a selectively permeable membrane.
- Direction of Water Movement
- Water moves from high water concentration to low water concentration (down the water gradient).
- This is equivalent to movement from low solute concentration to high solute concentration.
- Total Solute Concentration
- Only the water concentration gradient matters for osmosis.
- Total solute concentration is an indirect measure of water concentration.
- Achieving Equilibrium in Osmosis
- Equilibrium occurs when the water gradient is zero.
- In the U-tube setup, equilibrium occurs when the force of gravity equals the osmotic pressure (no net osmosis).
- Tonicity and the Cell Environment
- Definition: Tonicity refers to the tendency for osmosis to occur through a cell membrane.
- Usage Rule: Tonicity terms must only describe the cell's surroundings or environment, never the cell itself.
- Hypotonic Environment (Hypo = Below/More Watery)
- Characteristics: Lower solute concentration/more watery than the cell.
- Osmosis: Water moves into the cell.
- Effects on Cells
- Animal cells: Swells, bursts (Lysis).
- Plant cells: Swells, pressurized (Turgid); ideal condition for the plant.
- Hypertonic Environment (Hyper = Above/Less Watery)
- Characteristics: Higher solute concentration/less watery than the cell.
- Osmosis: Water moves out of the cell.
- Effects on Cells
- Animal cells: Shrivels (Crenation).
- Plant cells: Plasma membrane collapses away from the cell wall (Plasmolysis/Plasmolyzed); fatal.
- Isotonic Environment (Iso = Same/Equal Wateriness)
- Characteristics: Wateriness is the same inside and outside the cell.
- Osmosis: Water moves in both directions at the same rate (no net volume change).
- Effects on Cells
- Animal cells: This is the ideal condition.
- Plant cells: Limp state (Flaccid); survivable but not ideal.