Cell Membrane & Transport
The big idea
Concentration gradients are like hills
Picture concentration as elevation. Where molecules are packed together in high numbers, they are sitting at the top of a hill. Left alone, they tumble downhill — from high concentration to low — for free, just like water flows downhill. That is passive transport. Moving molecules uphill, against their natural tendency, requires a push. That push is powered by ATP. That is active transport.
Downhill — passive transport
High → Low concentration. No energy needed — the gradient itself does the work, just like releasing a ball at the top of a hill. The cell simply opens a path and molecules flow on their own.
- Simple diffusion — small molecules slip straight through the lipid core
- Facilitated diffusion — channel proteins open a hydrophilic gate
- Osmosis — water moves down its own concentration gradient
Uphill — active transport
Low → High concentration. Molecules must be pushed against their natural tendency — like rolling a boulder uphill. Protein pumps use the energy from splitting ATP to force this movement.
- Na⁺/K⁺ pump — maintains the voltage across nerve and muscle cells
- H⁺ pump — concentrates acid in the stomach
- Calcium pumps — allow muscles to relax after each contraction
Click a tab to explore each transport type
Phospholipid Structure
The cell membrane is a phospholipid bilayer — two sheets of phospholipid molecules arranged tail-to-tail. The hydrophilic (water-loving) phosphate heads face outward toward aqueous environments, while the hydrophobic (water-fearing) fatty-acid tails face inward, forming an oily core that blocks most polar molecules.
- Each phospholipid has a polar, charged head and two non-polar fatty-acid tails
- The bilayer is ~7 nm thick and fluid at body temperature
- Membrane proteins float in the bilayer — the fluid mosaic model (Singer & Nicolson, 1972)
- Cholesterol is embedded between phospholipids, regulating membrane fluidity
Transport types at a glance
| Type | Protein? | ATP? |
|---|---|---|
| Simple diffusion | No | No |
| Facilitated diffusion | Yes | No |
| Active transport | Yes | Yes |
| Osmosis | Aquaporin | No |
Key concepts
Selectively permeable
The membrane is not a wall — it is a selective filter. Small, non-polar molecules cross freely; large or charged molecules need protein help or active pumping.
Downhill is free
Moving from high to low concentration (down the gradient) requires zero energy — it happens spontaneously, like water flowing downhill. Both forms of diffusion exploit this.
Uphill costs ATP
Pushing molecules from low to high concentration — against their gradient — is like rolling a boulder uphill. Protein pumps use ATP hydrolysis to supply that force.
When transport fails
Quick recap
- 1
Phospholipid bilayer — Two leaflets of phospholipids, hydrophilic heads outward, hydrophobic tails inward. ~7 nm thick.
- 2
Fluid mosaic model — Membrane proteins float freely within the bilayer, giving it a mosaic appearance.
- 3
Simple diffusion — Small non-polar molecules (O₂, CO₂) dissolve into and cross the lipid core. No protein, no ATP.
- 4
Facilitated diffusion — Polar molecules and ions use channel or carrier proteins. Still down the gradient — no ATP.
- 5
Active transport — Pumps (e.g. Na⁺/K⁺ ATPase) use ATP to move ions against their gradient — essential for membrane potential.