All organisms absorb and release gases from the environment.
Plants absorb CO₂ for photosynthesis and release O₂.
Humans absorb O₂ for respiration and release CO₂.
Small organisms have a large surface area to volume ratio, allowing for direct gas exchange.
Larger organisms require specialized structures for gas exchange (e.g., lungs, gills, or leaf structures).
Permeable – Allows free diffusion of gases.
Large Surface Area – Maximizes gas exchange.
Moist – Helps gases dissolve for efficient diffusion.
Thin – Short diffusion distance ensures rapid gas exchange.
Gases diffuse down concentration gradients.
Oxygen moves into organisms where O₂ levels are lower.
CO₂ diffuses out as cellular respiration increases its concentration.
Ventilation helps maintain concentration gradients.
Mammals use lungs for gas exchange.
Airways include bronchi, bronchioles, and alveoli.
Airways – Ensure ventilation.
Large Surface Area – 300 million alveoli in human lungs.
Extensive Capillary Beds – Blood supply maximizes diffusion.
Short Diffusion Distance – Thin alveolar and capillary walls.
Moist Surface with Surfactant – Keeps alveoli open and allows gases to dissolve.
Image: Human lung tissue
Inhalation:
External intercostal muscles contract, expanding the ribcage.
Diaphragm contracts and moves down.
Lung volume increases, reducing pressure, drawing air in.
Exhalation:
Internal intercostal muscles contract, pulling ribs inward.
Diaphragm relaxes and moves up.
Lung volume decreases, increasing pressure, pushing air out.
Image: Lung ventilation mechanism
Ventilation rate – Number of breaths per minute.
Tidal volume – Volume of air inhaled/exhaled per breath.
Vital capacity – Maximum air exhaled after deep inhalation.
Inspiratory reserve volume – Additional air inhaled after tidal breath.
Expiratory reserve volume – Additional air exhaled beyond tidal breath.
Image: Spirometry graph of lung volumes
Leaves have large, moist surfaces for efficient gas exchange.
Key Adaptations:
Waxy cuticle – Reduces water loss.
Guard cells – Control stomatal openings.
Air spaces – Facilitate diffusion.
Spongy mesophyll – Provides a large moist surface.
Veins – Transport water for evaporation.
Image: Structure of a leaf showing gas exchange adaptations
Plan diagrams illustrate leaf tissues:
Upper epidermis – Protective outer layer.
Palisade mesophyll – Site of photosynthesis.
Spongy mesophyll – Facilitates gas diffusion.
Lower epidermis – Contains stomata.
Xylem and phloem – Transport water and nutrients.
Image: Lower epidermis of a leaf with stomata
Loss of water vapor from leaves through stomata.
Factors affecting transpiration:
Temperature – Increases evaporation.
Humidity – Decreases transpiration.
Wind – Prevents saturation near stomata, increasing transpiration.
Image: Transpiration process
Methods:
Peel-off epidermis and examine under a microscope.
Apply clear nail varnish, peel off, and examine.
Take a photograph and count stomata.
Formula:
Stomatal density=mean number of stomataarea of field of view (mm²)\text{Stomatal density} = \frac{\text{mean number of stomata}}{\text{area of field of view (mm²)}}
Image: Stomatal density measurement
Effect of CO₂ on Hemoglobin’s Oxygen Affinity:
Increased CO₂ lowers blood pH, reducing hemoglobin’s oxygen affinity.
CO₂ binds to hemoglobin, forming carbaminohemoglobin with lower oxygen affinity.
Bohr Shift:
At high CO₂ levels, hemoglobin releases more oxygen.
In the lungs (low CO₂, high pH), hemoglobin rebinds oxygen efficiently.
Image: Oxygen dissociation curve showing the Bohr shift