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Spec Mapping — OCR H420 Module 3.1.1 — Exchange surfaces, content statements covering the use of a spirometer to measure tidal volume, vital capacity, ventilation rate and oxygen uptake; the interpretation of spirometer traces; and the precautions required for safe operation (refer to the official OCR H420 specification document for exact wording). This is one of OCR's classic practical+calculation topics — the spirometer is both an instrument students may use under PAG conditions and the source of routine 6-mark data-interpretation questions.
Measuring how much air moves in and out of the lungs gives insight into the health of the respiratory system and allows scientists to quantify ventilation. The instrument traditionally used to make these measurements is the spirometer. This lesson introduces the standard lung volumes — tidal volume, vital capacity, residual volume, and inspiratory/expiratory reserve volumes — and explains how to interpret a spirometer trace. It also explores the derived quantities of ventilation rate (pulmonary ventilation) and FEV₁, and the precautions needed for safe use.
The spirometer was invented by John Hutchinson in 1846, a British surgeon working on life-insurance actuarial science: he found that vital capacity was the single best predictor of longevity in his cohort of 2,130 male patients. Modern spirometry remains a routine test, used to diagnose asthma, chronic obstructive pulmonary disease (COPD), pulmonary fibrosis and occupational lung diseases such as silicosis and asbestosis. The instrument is the cornerstone of respiratory medicine.
Key Definitions:
- Tidal volume (TV) — the volume of air moved into or out of the lungs in a single normal breath at rest, typically about 500 cm³ (0.5 dm³).
- Vital capacity (VC) — the maximum volume of air that can be forcibly expelled after the deepest possible inhalation; typically 4.5–5 dm³ in an adult.
- Residual volume (RV) — the volume of air remaining in the lungs after the most forceful possible exhalation; approximately 1.0–1.5 dm³. It cannot be measured directly with a spirometer.
- Inspiratory reserve volume (IRV) — the extra air that can be drawn in above a normal tidal inhalation.
- Expiratory reserve volume (ERV) — the extra air that can be forced out after a normal tidal exhalation.
- Total lung capacity (TLC) — VC + RV; the total volume the lungs can hold.
| Volume | Adult value (dm³) | Definition |
|---|---|---|
| Tidal volume (TV) | 0.5 | Normal resting breath |
| Inspiratory reserve (IRV) | 3.0 | Extra in beyond TV |
| Expiratory reserve (ERV) | 1.1 | Extra out beyond TV |
| Vital capacity (VC = TV + IRV + ERV) | 4.6 | Max out after max in |
| Residual volume (RV) | 1.2 | Left after max out |
| Total lung capacity (TLC = VC + RV) | 5.8 | Total lung volume |
These values vary with age, sex, size and fitness. Endurance athletes typically have larger vital capacities, and healthy values fall gradually with age.
A classical spirometer consists of a chamber of air or oxygen floating on water. A tube leads from the chamber to a mouthpiece through which the subject breathes. As the subject inhales, the chamber falls; as they exhale, it rises. A pen attached to the chamber traces a graph on a rotating drum (kymograph), producing a characteristic trace of volume against time.
flowchart LR
A[Subject] -->|Inhale| B[Chamber falls]
B --> C[Pen moves up on trace]
A -->|Exhale| D[Chamber rises]
D --> E[Pen moves down on trace]
Because CO₂ is absorbed by the soda lime, the total volume in the chamber gradually falls over time as the subject consumes oxygen. The gradient of this baseline fall gives the rate of oxygen uptake, which can be used to calculate metabolic rate.
A typical spirometer trace shows a regular waveform over time. Between calm breaths the peaks and troughs are separated by the tidal volume. The frequency gives the breathing (ventilation) rate in breaths per minute. A deep forced breath gives a sudden excursion equal to the vital capacity, from which IRV and ERV can be read off.
Pulmonary ventilation rate (also called minute ventilation) is defined as:
Ventilation rate=Tidal volume×Breathing rate
For example, a person at rest breathing at 12 breaths per minute with a tidal volume of 0.5 dm³ has a ventilation rate of 0.5 × 12 = 6 dm³ min⁻¹. During strenuous exercise, both TV and breathing rate can rise considerably, so ventilation might reach 100 dm³ min⁻¹ or more.
The FEV₁ / FVC ratio is a clinically important measure of lung function:
Exam Tip: OCR questions often provide spirometer traces for healthy and diseased subjects and ask you to compare them. Look for: (1) smaller tidal volume, (2) smaller vital capacity, (3) slower FEV₁ (shallower initial slope), and (4) increased breathing rate as a compensation.
Because CO₂ is removed by soda lime, the only net volume change in the spirometer chamber arises from oxygen being absorbed by the subject. The gradient of the baseline on the trace therefore gives the rate of oxygen consumption:
Rate of O2 uptake=TimeVolume decrease
For example, if the baseline falls by 1.2 dm³ over 2 minutes, then oxygen consumption is 0.6 dm³ min⁻¹. This figure can be converted into an estimate of metabolic rate.
A student breathes quietly into a spirometer and produces the following values:
Ventilation rate = 0.45 × 16 = 7.2 dm³ min⁻¹ Rate of O₂ uptake = 0.9 / 3 = 0.3 dm³ min⁻¹
Lung volumes scale predictably with several factors:
A 17-year-old swimmer enters the school PAG laboratory. Her trace shows:
Calculations:
The unusually high VC and ratio are consistent with the cumulative effect of regular endurance training on the elastic and mechanical properties of the lung and chest wall.
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