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Cell membranes control the movement of substances into and out of cells. The fluid mosaic model describes the plasma membrane as a dynamic structure composed of a phospholipid bilayer with embedded and peripheral proteins, cholesterol, and glycoproteins. Understanding membrane structure, the mechanisms of transport, the factors that affect membrane permeability, and the basics of cell signalling is essential for A-Level Biology.
Key Definition: The fluid mosaic model (proposed by Singer and Nicolson, 1972) describes the cell membrane as a phospholipid bilayer with a mosaic of proteins that can move laterally within it.
| Component | Role |
|---|---|
| Phospholipid bilayer | Forms the basic barrier; hydrophobic interior prevents passage of water-soluble molecules and ions |
| Channel proteins | Provide hydrophilic pores for specific ions/polar molecules to pass through by facilitated diffusion |
| Carrier proteins | Change shape to transport specific molecules across the membrane (facilitated diffusion or active transport) |
| Cholesterol | Regulates membrane fluidity; prevents it becoming too rigid at low temperatures or too fluid at high temperatures; reduces permeability to small water-soluble molecules |
| Glycoproteins | Cell signalling, cell recognition, immune response (antigens on cell surface); act as receptors for hormones and neurotransmitters |
| Glycolipids | Cell-cell recognition, stability of membrane, and tissue compatibility |
| Peripheral proteins | Attached to the inner or outer surface of the membrane; involved in cell signalling and maintaining cell shape |
The membrane is described as fluid because phospholipids and proteins can move laterally within the bilayer, and mosaic because of the varied, irregular pattern of proteins scattered throughout.
A diagram of the fluid mosaic model would show two rows of phospholipids with their hydrophilic heads (circles) facing outward towards the aqueous environment and their hydrophobic tails (two lines) facing inward. Embedded within the bilayer are large integral proteins spanning the whole membrane (transmembrane proteins), channel proteins with a central pore, and smaller peripheral proteins on the surface. Cholesterol molecules would be shown wedged between the phospholipid tails. Glycoproteins and glycolipids project from the outer surface with branching carbohydrate chains.
Exam Tip: When describing the fluid mosaic model, always mention both aspects: "fluid" (lateral movement of components) and "mosaic" (variety of proteins). Simply drawing a diagram without explaining these terms will lose marks on a "describe" question.
The permeability of cell membranes can be affected by several factors. A common practical investigation uses beetroot cells (which contain a red pigment, betacyanin, in their vacuoles) to study these effects.
Exam Tip: In the beetroot practical, the dependent variable is the intensity of red colour in the surrounding solution (measured using a colorimeter). The more permeable the membrane, the more betacyanin is released and the greater the absorbance reading. Control variables include beetroot disc size, volume of solution, and time of exposure.
Passive transport requires no metabolic energy (no ATP) and moves substances down their concentration gradient.
Key Definition: Diffusion is the net movement of molecules or ions from a region of higher concentration to a region of lower concentration, down a concentration gradient.
Rate of diffusion ∝ (surface area × concentration difference) ÷ thickness of exchange surface
Worked Example 1 — Fick's Law:
Two exchange surfaces are compared:
Which surface has the greater rate of diffusion?
Solution: Using Fick's law (proportional relationship):
Surface A: Rate ∝ (50 × 0.4) ÷ 0.2 = 20 ÷ 0.2 = 100 arbitrary units
Surface B: Rate ∝ (100 × 0.2) ÷ 0.1 = 20 ÷ 0.1 = 200 arbitrary units
Surface B has the greater rate of diffusion, despite having a lower concentration difference, because it has double the surface area and half the thickness.
Key Definition: Osmosis is the net movement of water molecules from a region of higher water potential (Ψ) to a region of lower (more negative) water potential, across a partially permeable membrane.
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