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Biology · Cells, Membranes & Organisation

Diffusion, osmosis, active transport and vesicles

A hypothetical membrane bag contains a dissolved substance that cannot cross its membrane, while water can cross. Place it in a different surrounding solution. Before predicting a change, ask what is permeable, what concentrations differ, and whether a pressure difference also matters. The word osmosis is not a substitute for those conditions.

The earlier biology chapters introduce living systems, evidence, water, ions and biological molecules. Here, polar means a molecule has unevenly distributed electrical charge, and an ion is an electrically charged atom or group of atoms. Concentration means amount of a substance per volume. No microscope or home experiment is required; the examples use explicitly constructed observations.

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By the end, you can

Predict transport under stated conditions and distinguish passive movement, energy coupling and vesicle traffic.

01

Distinguish movement from net movement

Thermal molecular motion continues in both directions. For a neutral dissolved substance in a simple, comparable medium, a concentration difference can produce net diffusion from higher to lower concentration. Net means the difference between the opposing transfers. At equilibrium, molecular motion continues even though there is no sustained net transfer.

A membrane crossing also requires an available route. Simple diffusion uses the lipid phase; facilitated diffusion uses a channel or carrier. Both are passive when movement proceeds down the relevant gradient without energy being coupled to drive it uphill. The presence of a protein does not by itself make transport active.

For ions, concentration and electrical potential both matter. Their combined influence is described by an electrochemical gradient. A higher concentration inside cannot, by itself, predict the direction of a positively charged ion through an open channel: an electrical difference may reinforce or oppose that concentration effect.

02

Water movement changes the conditions that drive it

Osmosis is water movement across a selectively permeable membrane. With equal starting pressure and other conditions matched, a higher concentration of nonpenetrating solute on one side can favour net water movement toward that side. Solute and pressure both contribute to water potential, a way to express the tendency of water to move. Water moves from higher to lower water potential when a route is available.

As water enters a bounded space, concentrations and pressure may change. A plant cell's wall can resist expansion, allowing internal pressure, or turgor, to rise and oppose further net water entry. An animal cell lacks that wall and may swell or shrink as its surroundings change. A cell's response depends on permeability and the relevant timescale as well as the solution outside.

Tonicity describes a solution's effect on cell volume through the behaviour of effectively nonpenetrating solutes. Hypertonic surroundings tend to draw water out, hypotonic surroundings favour entry, and isotonic surroundings do not cause sustained net volume change under the stated conditions. Equal total solute concentration alone does not prove equal tonicity if solutes cross differently.

In the diagram's idealised initial comparison, water passes and the illustrated neutral solute does not; pressure initially matches. Before reading the arrow, predict which way net water movement begins. The dots express only a relative starting concentration, not measured particle counts, osmotic pressure values or a prediction of the final volume.

Predict the initial water movement from stated conditions

Predict the initial water movement from stated conditionsTwo starting solutions are separated by a membrane that passes water but not the illustrated neutral solute. The left solution has lower solute concentration and the right has higher solute concentration; initial pressure and temperature match. A net-water arrow points right while smaller arrows show water movement in both directions. Dot numbers are qualitative symbols, not measured concentrations or a final-state model.Lower nonpenetrating-soluteconcentrationHigher nonpenetrating-soluteconcentrationInitial net water movementWater molecules move both waysWater passes; this solute does notStarting pressure and temperature match
Idealised initial comparison only. Changing pressure, concentrations and permeability affect what happens next.
Read the diagram in words

Two starting solutions are separated by a membrane that passes water but not the illustrated neutral solute. The left solution has lower solute concentration and the right has higher solute concentration; initial pressure and temperature match. A net-water arrow points right while smaller arrows show water movement in both directions. Dot numbers are qualitative symbols, not measured concentrations or a final-state model.

Predict the initial water movement from stated conditions
Illustrated solutionQualitative solute-dot count
Lower nonpenetrating-solute concentration4
Higher nonpenetrating-solute concentration8
Initial net water movement
Lower nonpenetrating-solute concentration → Higher nonpenetrating-solute concentration
Water molecules move both ways
Lower nonpenetrating-solute concentration ↔ Higher nonpenetrating-solute concentration
Starting pressure and temperature match
ConditionMeaning in this model
Illustrated soluteneutral and nonpenetrating
Membrane passes waterYes
Equal starting pressureYes
Equal starting temperatureYes
Illustrated solute crosses the membraneNo
Final volume predictedNo
Diagram key
  • Lower nonpenetrating-solute concentration
  • Higher nonpenetrating-solute concentration
  • Water passes; this solute does not
  • Initial net water movement
  • Water molecules move both ways
  • Starting pressure and temperature match
03

Move against a gradient by coupling processes

Active transport couples movement against a substance's relevant gradient to an energy-releasing process. A primary active transporter can use ATP directly. A secondary active transporter couples one substance's downhill movement to another's uphill movement; it depends on energy stored in the driving gradient. If metabolism previously built that gradient, the absence of ATP use at this transporter does not make the overall transport passive.

Endocytosis and exocytosis use membrane rearrangement and vesicles rather than passage through a small-molecule channel. Endocytosis encloses extracellular material in a membrane compartment. Exocytosis fuses a compartment with the plasma membrane to release its contents. Entry into a vesicle is not the same as direct entry into the cytosol. These processes require cellular machinery and energy but should not be explained simply as diffusion against a concentration gradient.

Worked example

Keep the permeability assumption in the prediction

An idealised bag starts with a higher concentration of a neutral, nonpenetrating solute than the surrounding water solution. Temperature and starting pressure match, and the membrane passes water. Predict initial net water entry. If the bag can expand, dilution changes its internal concentration; if its boundary strongly resists expansion, rising pressure also matters. The initial arrow does not establish endless entry or a final equal concentration.

Now change the assumption: the solute can rapidly cross too. The original reasoning about a persistent nonpenetrating-solute difference no longer applies. We would need its crossing rate and the changing concentrations to predict volume over time. Naming the changed assumption is more informative than saying that osmosis failed.

Check your understanding

  1. Does zero net diffusion mean molecules have stopped moving?

    Show reasoning

    No. Opposing transfers can balance while molecular motion continues.

  2. Can a transporter be active without directly consuming ATP?

    Show reasoning

    Yes. Secondary active transport couples uphill movement to downhill movement of another substance. Maintaining the driving gradient requires an energy source.

  3. Why is 'water always moves toward more solute' incomplete?

    Show reasoning

    The prediction requires membrane permeability, pressure and other relevant conditions. Pressure can oppose osmotic entry, and penetrating solutes may not maintain the same volume effect.

What to carry forward

A transport prediction needs a route, a relevant gradient, energy coupling where required, and a timescale.

References

Resources supporting this lesson’s explanations and examples.

  1. Mary Ann Clark, Matthew Douglas and Jung Choi · OpenStax4 sources
    1. Biology 2e — Passive Transport (2018)Mary Ann Clark, Matthew Douglas and Jung Choi · OpenStaxOpen textbook sectionopenstax.orgRead source
    2. Biology 2e — Active Transport (2018)Mary Ann Clark, Matthew Douglas and Jung Choi · OpenStaxOpen textbook sectionopenstax.orgRead source
    3. Biology 2e — Transport of Water and Solutes in Plants (2018)Mary Ann Clark, Matthew Douglas and Jung Choi · OpenStaxOpen textbook sectionopenstax.orgRead source
    4. Biology 2e — Bulk Transport (2018)Mary Ann Clark, Matthew Douglas and Jung Choi · OpenStaxOpen textbook sectionopenstax.orgRead source
  2. Learning (by) osmosis: an approach to teaching osmolarity and tonicity (Advances in Physiology Education 42:626–635, 2018)Predrag Vujovic, Michael Chirillo and Dee U. Silverthorn · Universities of Belgrade and Texas at AustinPhysiology education researchjournals.physiology.orgRead source