B3.1 Gas exchangeIB Biology SL: Revision notes
Section 1
Why gas exchange gets harder with size
All organisms must exchange oxygen and carbon dioxide with their environment. As an organism gets larger, its surface area-to-volume ratio falls (a cube of side x has SA:V = 6/x), and the distance from its centre to the surface increases. Diffusion alone becomes too slow and the surface too small, so large organisms need specialised gas-exchange surfaces and transport systems.
A larger organism has a larger surface area but a smaller surface area-to-volume ratio. Always say 'ratio'.
Section 2
Properties of gas-exchange surfaces and concentration gradients
Gas-exchange surfaces are permeable to O₂ and CO₂, made of a thin tissue layer (short diffusion distance), moist (gases dissolve before diffusing) and have a large surface area.
In animals, steep concentration gradients are maintained by a dense network of blood vessels, continuous blood flow that removes O₂ and brings CO₂, and ventilation — with air in lungs, and with water pumped over the gills in fish.
Section 3
Adaptations of mammalian lungs
- Branched network of bronchioles carries air to millions of alveoli.
- Many alveoli give a high surface area.
- Alveolus walls are one layer of thin cells.
- Extensive capillary beds surround each alveolus.
- Surfactant reduces surface tension in the moist lining, stopping the alveoli sticking together and collapsing when air is exhaled.
Section 4
Ventilation and lung volumes
Inhalation: external intercostal muscles contract, moving the ribs up and out; the diaphragm contracts and flattens. Thorax volume rises, pressure falls below atmospheric, air flows in.
Exhalation: at rest, these muscles relax and elastic recoil reduces volume. In forced exhalation, the internal intercostals pull the ribs down and in and the abdominal muscles push the diaphragm up.
Tidal volume = volume in or out per resting breath. Inspiratory reserve = extra volume that can be inhaled after a normal breath in. Expiratory reserve = extra that can be forced out after a normal breath out. Vital capacity = tidal volume + inspiratory reserve + expiratory reserve.
Pressure changes follow volume changes: bigger thorax, lower pressure, air in.
Section 5
Gas exchange in leaves and tissue distribution
In a transverse section of a dicotyledonous leaf, from top to bottom: waxy cuticle, upper epidermis, palisade mesophyll, spongy mesophyll with large air spaces, lower epidermis with stomata controlled by guard cells, and a vein (xylem above phloem) in the midrib. The cuticle reduces water loss; stomata let CO₂ in and O₂ out; air spaces give a large, moist internal surface; veins supply water and remove sugars.
Section 6
Transpiration and stomatal density
Transpiration is the loss of water vapour from leaves. It is a consequence of gas exchange: stomata must open for CO₂ uptake, so water vapour diffuses out. Rate increases with higher temperature, higher light intensity (stomata open), lower humidity and more air movement.
Stomatal density = number of stomata ÷ area of field of view (πr²). Count several fields, because biological material is variable: repeating measurements increases reliability.
Use the radius, not the diameter, when calculating the area of a circular field of view.
That's the notes covered.
Carry on to the next subtopic.