Parts of the respiratory system
Air enters through the nose or mouth, where it is warmed, moistened and filtered. It travels down thetrachea (windpipe), which is held open by C-shaped rings of cartilage, then into twobronchi, one for each lung. The bronchi branch again and again into narrowerbronchioles, about 23 generations of branching in total, ending in clusters ofalveoli. The lungs sit inside the rib cage, above the dome-shaped diaphragm.
How breathing works
The lungs have no muscles of their own. Breathing in (inspiration) happens when thediaphragm contracts and flattens, and the external intercostal muscles pull the ribs up and out. The chest gets bigger, the lungs expand with it, and the pressure inside them falls slightly below the air pressure outside. Air flows in until the pressures are equal.
Quiet breathing out (expiration) is mostly passive: the diaphragm relaxes and domes upwards, the stretchy lungs recoil, the pressure inside rises slightly above atmospheric, and air flows out. During exercise, internal intercostal and abdominal muscles help push air out faster. The simulator shows the pressure inside the lungs: just one or two centimetres of water below or above atmospheric is enough to move half a litre of air.
Gas exchange in the alveoli
The two lungs contain roughly 480 million alveoli with a total surface area of about 70 m², the size of a small apartment. Each alveolus is wrapped in capillaries, and the barrier between air and blood is less than a thousandth of a millimetre thick. Gases move by diffusion, from high to low concentration (more precisely, partial pressure). Oxygen diffuses from the alveolar air into the blood and binds to haemoglobin in red blood cells; carbon dioxide diffuses from the blood into the alveoli to be breathed out.
Breathing by the numbers
- Tidal volume: air moved in a normal breath, about 500 mL at rest.
- Breathing rate: about 12–20 breaths per minute in a resting adult.
- Minute ventilation: rate × tidal volume, about 6–8 L per minute at rest and over 100 L per minute in hard exercise.
- Dead space: about 150 mL of each breath stays in the airways and never reaches the alveoli.
- Oxygen saturation: usually 95–100 % in healthy people at sea level.
Exercise, altitude and asthma
Exercise: working muscles produce much more carbon dioxide, so breathing becomes faster and deeper to remove it and to supply extra oxygen. High altitude: air is still 21 % oxygen, but the air pressure is lower, so there is less oxygen in each breath; saturation falls even though breathing speeds up, and over weeks the body adapts by making more red blood cells. Asthma: the airways become inflamed and the muscles around them tighten, raising resistance to airflow. Breathing out is hardest, so air becomes trapped and the lungs stay over-inflated.
What controls breathing
Breathing is controlled automatically by the medulla in the brainstem. Chemoreceptors constantly monitor carbon dioxide (and the acidity it causes) in the blood. A rise in carbon dioxide is the main stimulus to breathe harder, which is why you cannot hold your breath for very long.
Key terms
- Ventilation
- Moving air in and out of the lungs.
- Alveoli
- Microscopic air sacs where gas exchange happens.
- Partial pressure
- The share of the total gas pressure due to one gas, such as oxygen.
- Haemoglobin
- The iron-containing protein in red blood cells that carries oxygen.
Common misconceptions
- “The lungs pull air in.” The diaphragm and rib muscles enlarge the chest; the lungs follow.
- “We breathe out only carbon dioxide.” Exhaled air is still about 16 % oxygen and mostly nitrogen.
- “Breathing and respiration are the same thing.” Breathing is ventilation; respiration is the chemical process in cells that releases energy.
Educational model only. The values in this simulator are simplified textbook estimates. It cannot assess breathing problems, asthma or oxygen levels in a real person and is not medical advice. If you or someone else has difficulty breathing, seek medical help immediately. See our educational and medical disclaimer.
Key takeaways
- Breathing in: diaphragm contracts and ribs lift, the chest gets bigger, pressure falls, air flows in.
- Gas exchange happens by diffusion across the thin walls of the alveoli.
- Ventilation = breathing rate × tidal volume.
- Lower air pressure (altitude) or narrowed airways (asthma) reduce how well oxygen reaches the blood.
Model note: lung mechanics use a single resistance and compliance; gas values use the alveolar gas equation and a standard oxygen–haemoglobin curve. Real lungs vary from region to region.