Breathing and Exchange of Gases
Every quiet minute of your life, roughly twelve to sixteen times, your ribcage lifts, your diaphragm drops, and air rushes into two spongy bags in your chest — and you never have to think about it. This chapter takes that automatic act apart and shows it is really five separate events chained together: breathing, or pulmonary ventilation, diffusion of gases at the alveoli, transport of those gases by blood, diffusion of gases again between blood and tissues, and finally cellular respiration inside mitochondria, which actually consumes the oxygen and makes the carbon dioxide — a process this chapter deliberately hands off to Chapter 12. Only the first four of these five steps belong here; the fifth is chemistry you already know. You will meet the architecture of the human respiratory system, from external nostrils through the pharynx, larynx, trachea and branching bronchi down to millions of thin-walled alveoli — the exchange surface. You will learn why breathing is nothing more than manipulating pressure inside an airtight thoracic chamber, and how spirometry turns that mechanical act into clinically useful numbers such as tidal volume and vital capacity. You will see why oxygen and carbon dioxide move in the directions they do — driven purely by partial-pressure gradients across a diffusion membrane under a millimetre thick — and how nearly all of the oxygen and most of the carbon dioxide travel chemically bound rather than simply dissolved: oxygen as oxyhaemoglobin, carbon dioxide mostly as bicarbonate manufactured on the spot by carbonic anhydrase. Finally, you will meet the neural circuitry in the medulla and pons that adjusts breathing rate without conscious effort, and the disorders — asthma, emphysema, occupational lung disease — that arise when this finely tuned system breaks down. Master this chapter and the next one, Body Fluids and Circulation, will make immediate sense: it is the delivery van for exactly the gases this chapter loads and unloads.
- Respiratory mechanisms vary with organisation and habitat: sponges, coelenterates and flatworms diffuse gases over the body surface; earthworms use a moist cuticle; insects use tracheal tubes; most aquatic arthropods and molluscs use gills; terrestrial vertebrates use lungs; frogs add cutaneous respiration.
- The human tract runs nostrils to nasal chamber to pharynx to larynx (guarded by the epiglottis while swallowing) to trachea to primary, secondary and tertiary bronchi to bronchioles to alveoli, cartilage-supported down to the initial bronchioles.
- Respiration has five steps: breathing, diffusion at the alveolar membrane, transport by blood, diffusion between blood and tissues, and cellular utilisation of O2.
- Breathing is pressure-driven: diaphragm and external intercostal contraction enlarges the thoracic cavity, dropping intra-pulmonary pressure below atmospheric for inspiration; relaxation raises it above atmospheric for passive expiration.
- Volumes (tidal ~500 mL, IRV 2500 to 3000 mL, ERV 1000 to 1100 mL, RV 1100 to 1200 mL) combine into capacities — IC, EC, FRC, VC, TLC — measured with a spirometer.
- Gas exchange is diffusion down partial-pressure gradients, helped by CO2's solubility being 20 to 25 times that of O2, across a diffusion membrane of squamous epithelium, capillary endothelium and a shared basement substance.
- Oxygen travels 97 per cent as oxyhaemoglobin, 3 per cent dissolved; the sigmoid oxygen dissociation curve shows how pO2, pCO2, H+ and temperature control loading in lungs and unloading at tissues.
- Carbon dioxide travels mainly as bicarbonate (about 70 per cent, via carbonic anhydrase), then as carbaminohaemoglobin (20 to 25 per cent), with only about 7 per cent dissolved in plasma.
- The medullary rhythm centre sets basic rhythm, the pons pneumotaxic centre fine-tunes it, and a chemosensitive area plus aortic/carotid receptors respond mainly to CO2 and H+ — oxygen's role in regulation is minor.
- Key idea: breathing pumps air along a pressure gradient created by the diaphragm and intercostal muscles, and once inside the body oxygen and carbon dioxide move entirely by diffusion down their own partial-pressure gradients — oxygen carried mainly as oxyhaemoglobin and carbon dioxide mainly as bicarbonate generated by carbonic anhydrase — with the whole rhythm regulated by a medullary centre that responds chiefly to rising CO2 and H+, not falling O2.
Breathing pumps air by a pressure gradient built with the diaphragm and intercostal muscles, and once air is inside the body every gas — oxygen into blood and tissues, carbon dioxide back out — moves purely by diffusion down its own partial-pressure gradient, carried chemically as oxyhaemoglobin and as bicarbonate, and the entire rhythm is set by a brainstem centre tuned mainly to carbon dioxide and hydrogen ion levels rather than to oxygen.
What this chapter covers
This article follows NCERT's own map through the chapter:
- Respiratory organs across the animal kingdom, then the human respiratory system, nostrils to alveoli, and its conducting versus exchange parts.
- The mechanism of breathing — how the diaphragm and intercostal muscles change thoracic volume and intra-pulmonary pressure to drive inspiration and expiration.
- Respiratory volumes and capacities — tidal volume, the reserve volumes, residual volume, and the five capacities built from them.
- Exchange of gases — how partial pressures of O2 and CO2 differ across the pathway and drive diffusion.
- Transport of gases — O2 as oxyhaemoglobin, CO2 as bicarbonate, carbaminohaemoglobin and dissolved gas, and the oxygen dissociation curve.
- Regulation of respiration — the medullary rhythm centre, the pneumotaxic centre, and chemosensitive receptors.
- Disorders of the respiratory system — asthma, emphysema and occupational respiratory disorders.
The core ideas
Respiratory organs across the animal kingdom
Mechanisms of breathing vary among animal groups mainly with their level of organisation and habitat. Lower invertebrates such as sponges, coelenterates and flatworms have no dedicated respiratory organ — they exchange O2 and CO2 by simple diffusion over the entire body surface, since every cell lies close to the surface. Earthworms use their moist cuticle. Insects use a network of tracheal tubes that carries atmospheric air directly to tissues, bypassing the blood for gas transport altogether. Vascularised gills (branchial respiration) serve most aquatic arthropods and molluscs, while vascularised lungs (pulmonary respiration) serve terrestrial forms. Among vertebrates, fishes use gills while amphibians, reptiles, birds and mammals use lungs; frogs additionally respire through their moist skin (cutaneous respiration). The common thread is the same physical requirement: a large, thin, moist, richly vascularised surface for diffusion.
The human respiratory system: from nostrils to alveoli
Humans have a pair of external nostrils opening above the upper lip, leading through the nasal passage into a nasal chamber, which opens into the pharynx — part of which is the common passage for food and air. The pharynx opens through the larynx into the trachea. The larynx is a cartilaginous box that also helps in sound production (the sound box); during swallowing its opening (the glottis) is covered by a thin elastic cartilaginous flap, the epiglottis, keeping food out of the larynx. The trachea is a straight tube running to the mid-thoracic cavity, dividing at the level of the 5th thoracic vertebra into a right and a left primary bronchus. Each primary bronchus divides repeatedly into secondary and tertiary bronchi and then bronchioles, ending in very thin terminal bronchioles. The trachea, the bronchi and the initial bronchioles are supported by incomplete cartilaginous rings that keep the airway from collapsing while still letting it flex. Each terminal bronchiole gives rise to many thin, irregular-walled, richly vascularised sac-like alveoli; the branching network of bronchi, bronchioles and alveoli makes up the lungs. Each of the two lungs is covered by a double-layered pleura, with pleural fluid between the layers reducing friction as the lung surface moves. The lungs sit inside the thoracic chamber, an airtight compartment bounded dorsally by the vertebral column, ventrally by the sternum, laterally by the ribs, and below by the dome-shaped diaphragm. Because the pleura couples the lung surface tightly to the thoracic wall, any change in thoracic volume is transmitted to pulmonary volume — essential, since we cannot directly alter pulmonary volume ourselves. It is useful to split the tract into two functional zones. Nostrils to terminal bronchioles form the conducting part, which transports air to the alveoli while clearing it of foreign particles, humidifying it, and warming it to body temperature. The alveoli and their ducts form the respiratory (exchange) part — where O2 and CO2 actually diffuse between blood and air.
The mechanics of breathing: pressure gradients do the work
Breathing has two stages: inspiration, during which atmospheric air is drawn in, and expiration, during which CO2-rich alveolar air is released. Air moves purely because a pressure gradient is created between the lungs and the atmosphere — the lungs have no muscle in their walls to actively pump air. Inspiration occurs only when intra-pulmonary pressure drops below atmospheric pressure; expiration occurs when it rises above atmospheric pressure. The diaphragm and the external and internal intercostal muscles generate these gradients. Inspiration begins with contraction of the diaphragm, increasing thoracic volume along the antero-posterior axis as the dome flattens; simultaneously, contraction of the external intercostals lifts the ribs and sternum, increasing thoracic volume along the dorso-ventral axis. This combined increase is transmitted through the pleura to an equal increase in pulmonary volume, lowering intra-pulmonary pressure below atmospheric and forcing air in. Relaxation of these muscles reduces thoracic and pulmonary volume, raising intra-pulmonary pressure slightly above atmospheric and expelling air — expiration, essentially passive elastic recoil under quiet breathing; additional abdominal muscles can force both phases when needed. A healthy human breathes 12 to 16 times per minute, and a spirometer measures the volumes moved for clinical assessment of lung function.
Respiratory volumes and capacities
Spirometry resolves the air moved during breathing into a small set of standard volumes, which are then added together in different combinations to give clinically meaningful capacities.
Tidal volume (TV) is the volume of air inspired or expired during one normal, quiet breath — approximately 500 mL, so a healthy adult moves roughly 6000 to 8000 mL of air per minute at rest. Inspiratory reserve volume (IRV) is the extra air that can be forcibly inspired beyond a normal tidal inspiration, averaging 2500 to 3000 mL. Expiratory reserve volume (ERV) is the extra air that can be forcibly expired beyond a normal tidal expiration, averaging 1000 to 1100 mL. Residual volume (RV) is the air that remains in the lungs even after the most forcible expiration, averaging 1100 to 1200 mL — never exhaled, and it keeps the alveoli from collapsing. Adding volumes together gives the capacities used in clinical diagnosis:
| Capacity | Made of | Meaning |
|---|---|---|
| Inspiratory capacity (IC) | TV + IRV | total air a person can inspire after a normal expiration |
| Expiratory capacity (EC) | TV + ERV | total air a person can expire after a normal inspiration |
| Functional residual capacity (FRC) | ERV + RV | air left in the lungs after a normal expiration |
| Vital capacity (VC) | ERV + TV + IRV | maximum air breathed out after the deepest possible inspiration (or in after the deepest possible expiration) |
| Total lung capacity (TLC) | RV + ERV + TV + IRV (or VC + RV) | total air the lungs hold at the end of a forced inspiration |
Because residual volume can never be exhaled, RV, FRC and TLC cannot be read directly off a simple spirometer trace — only combinations that exclude RV (TV, IRV, ERV, IC, EC, VC) are directly measurable this way. This is a favourite Board and NEET distinction, and it is developed further in the derivation and worked examples below.
Exchange of gases: partial pressures and the diffusion membrane
The alveoli are the primary site of gas exchange; exchange also occurs between blood and tissues. In both places, O2 and CO2 move by simple diffusion, driven mainly by a pressure or concentration gradient; gas solubility and membrane thickness also affect the rate. The pressure contributed by one gas within a mixture of gases is its partial pressure — written for oxygen and for carbon dioxide. NCERT's Table 14.1 gives these values (in mm Hg) at each site along the pathway:
| Site | (mm Hg) | (mm Hg) |
|---|---|---|
| Atmospheric air | 159 | 0.3 |
| Alveolar air | 104 | 40 |
| Deoxygenated blood | 40 | 45 |
| Oxygenated blood | 95 | 40 |
| Tissues | 40 | 45 |
These numbers show a clear gradient for oxygen from alveoli to blood and blood to tissues, and an equal and opposite gradient for carbon dioxide from tissues to blood and blood to alveoli. Because CO2 is 20 to 25 times more soluble than O2, the amount diffusing per unit of partial-pressure difference is much larger for CO2, compensating for its comparatively small gradient (about 5 mm Hg, against oxygen's 55 to 64 mm Hg). The diffusion membrane has three layers: the thin squamous epithelium of the alveolus, the endothelium of the alveolar capillary, and a shared basement substance sandwiched between them. Even with three layers, total thickness is much less than a millimetre — so every relevant factor favours diffusion of O2 from alveoli toward tissues, and of CO2 from tissues toward alveoli.
Transport of oxygen: haemoglobin and the oxygen dissociation curve
Blood carries both O2 and CO2. About 97 per cent of O2 is transported by red blood cells (RBCs); the remaining 3 per cent stays dissolved in plasma. Haemoglobin (Hb), the red, iron-containing pigment inside RBCs, binds O2 reversibly to form oxyhaemoglobin; each haemoglobin molecule carries up to four molecules of O2. Binding of O2 to haemoglobin depends primarily on , but , H+ concentration and temperature also interfere. Plotting percentage saturation of haemoglobin against gives an S-shaped, or sigmoid, curve — the oxygen dissociation curve. In the alveoli, high , low , low H+ and lower temperature all favour formation of oxyhaemoglobin; in the tissues, low , high , high H+ and higher temperature all favour dissociation instead. So oxygen binds at the lung surface and is released at the tissues — exactly where needed. Under normal conditions, every 100 mL of oxygenated blood delivers around 5 mL of O2 to the tissues. This rightward shift of the curve under high , high H+ and high temperature — conditions of actively metabolising tissue — is widely called the Bohr effect: haemoglobin releases more oxygen exactly where tissues are working hardest.
Transport of carbon dioxide: bicarbonate, carbamino compounds, and dissolved gas
CO2 is transported by blood through three parallel routes. About 20 to 25 per cent is carried by haemoglobin as carbaminohaemoglobin, a binding related to (pO2 is a major factor too). When is high and is low, as in the tissues, more CO2 binds haemoglobin; when is low and is high, as in the alveoli, CO2 dissociates and is released. The great majority, nearly 70 per cent, is carried as bicarbonate (HCO3-). RBCs contain a very high concentration of the enzyme carbonic anhydrase (a smaller amount is in plasma too), which catalyses the reaction in both directions:
At the tissues, high drives CO2 into blood and pushes this reaction forward, producing HCO3- and H+. At the alveoli, low reverses it, regenerating CO2 and H2O so CO2 diffuses out into alveolar air — CO2 trapped as bicarbonate at the tissue level is thus carried to the lungs and released as gas. The remaining roughly 7 per cent stays dissolved in plasma. Every 100 mL of deoxygenated blood delivers approximately 4 mL of CO2 to the alveoli.
Regulation of respiration: the neural control loop
The body maintains and adjusts respiratory rhythm neurally, without conscious effort. A specialised respiratory rhythm centre in the medulla is primarily responsible. A second centre, the pneumotaxic centre, sits in the pons and moderates the rhythm centre's output; its signal can reduce the duration of inspiration and thereby alter respiratory rate. A chemosensitive area next to the rhythm centre is highly sensitive to CO2 and hydrogen ions; a rise in either activates it, signalling the rhythm centre to adjust breathing until the excess is eliminated. Receptors in the aortic arch and carotid artery also sense CO2 and H+ changes and signal the rhythm centre. Oxygen's own role in regulating respiratory rhythm under normal conditions is quite insignificant — the system is tuned to CO2 and H+, not O2, which is why breathing stays comfortable until oxygen is severely depleted, as at very high altitude.
Disorders of the respiratory system
Asthma is difficulty in breathing with wheezing, from inflammation of the bronchi and bronchioles. Emphysema is a chronic disorder in which alveolar walls are damaged, reducing the exchange surface; cigarette smoking is a major cause. Occupational respiratory disorders arise in industries such as grinding or stone-breaking, where dust overwhelms the body's defences; long exposure causes inflammation leading to fibrosis and serious lung damage, so workers should wear protective masks.
The goal here is to trace, step by step, how muscular contraction in the chest translates into the pressure gradient that physically pulls air into the lungs and pushes it back out, using only the fact that gas moves from higher pressure to lower pressure. Because the pleura tightly couples the lung surface to the thoracic wall, any change in thoracic volume becomes an equal change in pulmonary volume — the hinge on which the whole mechanism turns.
Step 1. The diaphragm, a dome-shaped sheet of muscle forming the floor of the thoracic chamber, contracts and flattens, increasing thoracic volume along the antero-posterior axis.
Step 2. Simultaneously the external intercostal muscles contract, lifting the ribs and sternum outward, increasing thoracic volume along the dorso-ventral axis and adding to Step 1's gain.
Step 3. Because the lung surface is bound to the thoracic wall by the pleura, this overall increase in thoracic volume produces an equal increase in pulmonary volume — the lungs stretch along with the expanding chest wall.
Step 4. Since pressure and volume of a fixed amount of gas vary inversely, this increase in pulmonary volume drops intra-pulmonary pressure below atmospheric pressure, and air flows down the gradient into the lungs — inspiration.
Step 5. Relaxation of the diaphragm and external intercostals lets both return to resting position, reducing thoracic and pulmonary volume and raising intra-pulmonary pressure slightly above atmospheric, so air flows back out — expiration, passive under quiet breathing. Abdominal and internal intercostal muscles can force both phases when needed.
Go deeper · Derivation B · 1 minThe Partial-Pressure Cascade That Drives Diffusion of Oxygen and Carbon Dioxide
The goal is to follow the partial pressures of O2 and CO2 across every site in the pathway — atmosphere, alveoli, deoxygenated blood, oxygenated blood, and tissues — and show that at each junction the gradient points exactly the way the gas actually moves, using only NCERT's Table 14.1 values.
Step 1. Atmospheric air carries mm Hg and mm Hg. After mixing with residual air, humidifying and warming, alveolar air settles at mm Hg and mm Hg.
Step 2. Deoxygenated blood arriving at the alveolar capillaries carries mm Hg and mm Hg — a 64 mm Hg gradient favouring O2 into blood, and a 5 mm Hg gradient favouring CO2 into the alveolus.
Step 3. The 5 mm Hg CO2 gradient looks small beside the 64 mm Hg O2 gradient, but CO2's solubility is 20 to 25 times higher, so a comparable volume still diffuses per unit time — solubility compensates for the smaller pressure difference.
Step 4. Oxygenated blood leaving the lungs carries mm Hg and mm Hg, and travels to the tissues.
Step 5. At the tissues, cellular respiration keeps local at 40 mm Hg and at 45 mm Hg — a 55 mm Hg gradient favouring O2 into tissue and a 5 mm Hg (solubility-compensated) gradient favouring CO2 into blood, after which the deoxygenated blood returns to the lungs and the cascade repeats.
Go deeper · Derivation C · 1 minThe Carbonic Anhydrase Reaction and Carbon Dioxide Transport as Bicarbonate
The goal is to show how the single reversible reaction catalysed by carbonic anhydrase traps CO2 as bicarbonate at the tissues and releases it as CO2 gas at the alveoli, so that one enzyme, run in opposite directions at two sites, accounts for roughly 70 per cent of all CO2 transport.
Step 1. At the tissues, active catabolism keeps local high (45 mm Hg), so CO2 diffuses from tissue fluid into blood — into both plasma and RBCs.
Step 2. Inside the RBC, carbonic anhydrase catalyses , which immediately dissociates into and — the forward direction, favoured wherever is high.
Step 3. In parallel, some CO2 binds directly to haemoglobin, forming carbaminohaemoglobin — together with bicarbonate and dissolved CO2 this accounts for the full 100 per cent of transported CO2 (about 20 to 25 per cent carbaminohaemoglobin, about 7 per cent dissolved).
Step 4. The bicarbonate formed in Step 2 diffuses into plasma and is carried by flowing blood to the pulmonary capillaries, hiding CO2 in a form that does not raise gas pressure the way dissolved CO2 would.
Step 5. At the alveoli, is low (40 mm Hg against blood's 45 mm Hg), so the reaction reverses: , regenerating free CO2. Carbaminohaemoglobin simultaneously releases its bound CO2. The regenerated CO2 diffuses out into alveolar air and is expired, completing the cycle; every 100 mL of deoxygenated blood delivers roughly 4 mL of CO2 to the alveoli this way.
Worked examples
Board level - Respiratory volumes and capacities from spirometer data
A healthy adult's spirometer trace gives tidal volume (TV) = 500 mL, inspiratory reserve volume (IRV) = 3000 mL, expiratory reserve volume (ERV) = 1100 mL, and residual volume (RV) = 1200 mL. Find the inspiratory capacity, expiratory capacity, functional residual capacity, vital capacity and total lung capacity.
Step 1. Inspiratory capacity: mL.
Step 2. Expiratory capacity: mL.
Step 3. Functional residual capacity: mL.
Step 4. Vital capacity: mL.
Step 5. Total lung capacity: mL. Answer: IC = 3500 mL, EC = 1600 mL, FRC = 2300 mL, VC = 4600 mL, TLC = 5800 mL.
Competitive level (NEET) - Oxygen delivery to resting and exercising tissues
Using NCERT's figure that every 100 mL of oxygenated blood delivers about 5 mL of O2 to the tissues, find the rate of oxygen delivery (in mL per minute) when cardiac output is 5000 mL/min at rest, and again when cardiac output rises to 20,000 mL/min during vigorous exercise, assuming the same 5 mL per 100 mL extraction in both cases.
Step 1. At rest, the blood delivered per minute is 5000 mL, so the number of 100 mL units is .
Step 2. Oxygen delivered at rest mL O2 per minute.
Step 3. During exercise, cardiac output is 20,000 mL/min, so the number of 100 mL units is .
Step 4. Oxygen delivered during exercise mL O2 per minute. Answer: 250 mL O2/min at rest, rising to 1000 mL O2/min during exercise — a fourfold increase driven entirely by the fourfold rise in cardiac output, since extraction per 100 mL is held constant. Timing note: well under a minute — divide cardiac output by 100 and multiply by 5 mL. The trap is forgetting that real exercising muscle also widens its extraction beyond 5 mL per 100 mL; this question's constant-extraction assumption is a simplification, so do not invent extraction changes unless the question supplies a new figure.
Competitive level (NEET) - Partitioning carbon dioxide transport in the blood
Tissues load 200 mL of CO2 into the blood every minute. Using NCERT's transport percentages (about 70 per cent as bicarbonate, about 20 to 25 per cent as carbaminohaemoglobin, and about 7 per cent dissolved in plasma), estimate how many mL of CO2 travel by each route. Take the carbaminohaemoglobin share as 23 per cent for this calculation.
Step 1. Check the percentages sum to 100: , so the three routes are exhaustive and there is no leftover CO2 unaccounted for.
Step 2. CO2 as bicarbonate: mL, generated via the carbonic-anhydrase reaction inside the RBC and carried mostly in plasma.
Step 3. CO2 as carbaminohaemoglobin: mL, bound directly to haemoglobin.
Step 4. CO2 dissolved in plasma: mL. Answer: 140 mL as bicarbonate, 46 mL as carbaminohaemoglobin, 14 mL dissolved in plasma — summing back to the full 200 mL. Timing note: about 30 seconds — convert each percentage to a decimal and multiply once, and always check the fractions sum to 100 per cent first, since NEET distractors sometimes quietly supply percentages that sum to 95 or 105.
Common traps
Treating "breathing" and "respiration" as identical. NCERT calls gas exchange with the atmosphere "breathing, commonly known as respiration," but breathing (pulmonary ventilation) is only step (i) of a five-step process; cellular respiration, the oxidation of glucose inside mitochondria, is a separate topic in Chapter 12.
Confusing which volumes a simple spirometer can measure. TV, IRV, ERV and capacities built only from those three (IC, EC, VC) can be read directly off a spirometer trace. RV, and anything containing RV (FRC, TLC), cannot be, because residual air is never expired.
Assuming O2 drives breathing rate the way CO2 does. The chemosensitive area and aortic/carotid receptors are tuned mainly to CO2 and H+; O2's own role in normal regulation is quite insignificant, so rate does not rise sharply until oxygen is severely depleted.
Mixing up the diffusion membrane's layers. It is three layers — alveolar squamous epithelium, a shared basement substance, and capillary endothelium — not one, though combined thickness is still under a millimetre.
You should be able to…
- List the respiratory organs of sponges, earthworms, insects, aquatic arthropods and molluscs, fishes, and terrestrial vertebrates, and explain why each suits its habitat.
- Trace the human respiratory pathway from external nostrils to alveoli, naming every structure along the way.
- Distinguish the conducting part of the respiratory tract from the respiratory (exchange) part.
- Explain, in terms of thoracic volume and intra-pulmonary pressure, how the diaphragm and intercostal muscles cause inspiration and expiration.
- Define TV, IRV, ERV and RV, and correctly build IC, EC, FRC, VC and TLC from them.
- State the partial pressures of O2 and CO2 at each site along the pathway and explain the resulting diffusion gradients.
- Describe O2 transport (97% oxyhaemoglobin, 3% dissolved) and the shape and meaning of the oxygen dissociation curve.
- Describe CO2 transport (about 70% bicarbonate via carbonic anhydrase, 20 to 25% carbaminohaemoglobin, about 7% dissolved) and write the carbonic anhydrase reaction both ways.
- Explain the roles of the medullary rhythm centre, the pneumotaxic centre and the chemosensitive area (plus aortic/carotid receptors) in regulating breathing.
- Describe asthma, emphysema and occupational respiratory disorders, including their causes.
Ask the tutor: want to work through a few more spirometer or oxygen-dissociation-curve NEET problems together, or trace how this chapter's oxygenated blood becomes the subject of the next chapter, Body Fluids and Circulation?
Why does the oxygen dissociation curve have an S shape instead of a straight line?
Each haemoglobin molecule carries up to four O2 molecules, and binding the first makes it easier for the next ones to bind — a cooperative effect that shifts the molecule's shape and raises its affinity. At very low pO2 (tissues) the curve rises slowly; through the middle range it rises steeply, so a small pO2 change unloads or loads a lot of oxygen; near full saturation (alveoli) it flattens, since almost every haemoglobin already carries its full four. That steep middle section is exactly the pO2 range the body operates in — why the sigmoid shape is so physiologically useful.
Is breathing the same thing as respiration, and is that the same as cellular respiration?
Not quite. Breathing (pulmonary ventilation) is purely mechanical: moving air in and out of the lungs. Respiration, strictly, includes breathing plus diffusion of gases at the alveoli, transport by blood, and diffusion at the tissues — four of this chapter's five steps. Cellular respiration is different again: the biochemical process inside mitochondria that consumes the delivered O2 to oxidise glucose, releasing energy and CO2 — that chemistry belongs to Chapter 12, not this one.
Why is expiration usually passive but inspiration always needs muscular effort?
Inspiration must actively enlarge the thoracic cavity against the elastic recoil of the lungs and chest wall, so it always needs contraction of the diaphragm and external intercostals, using energy. Quiet expiration simply lets that same elastic recoil pull the diaphragm and rib cage back once the inspiratory muscles relax — no extra contraction needed, so it is passive. Only forced expiration, like a hard cough, recruits extra muscles (internal intercostals and abdominals) to push out more air than passive recoil alone would manage.
What actually happens to breathing at high altitude, given that oxygen barely matters to regulation?
At high altitude, atmospheric pO2 is much lower, so less oxygen loads onto haemoglobin even though breathing mechanics are unchanged — this shortage is called hypoxia. Near sea level, the body's regulatory system barely uses pO2 as a signal; it is tuned to CO2 and H+, the more sensitive moment-to-moment indicators of metabolic demand. Only when pO2 falls to quite low levels, as at altitude, does oxygen deprivation itself start to matter for breathing control and for symptoms like breathlessness and fatigue, and the body compensates over days by making more red blood cells.
Why does the chapter emphasise that residual volume can never be exhaled?
Because it keeps the alveoli from collapsing completely between breaths. If every last bit of air could be forced out, the delicate, thin-walled alveoli would flatten together, and the surface tension of their fluid lining would make re-inflating them enormously difficult — like separating two wet sheets of plastic. The permanently retained residual volume keeps alveoli gently inflated at all times, which is also exactly why RV (and anything built from it, like FRC and TLC) cannot be read off an ordinary spirometer trace — the instrument only measures air that actually leaves the body.