HLT-RESP80-02 · Lesson 6 · 40 clock hours · theory
Pulmonary Gas Exchange: Diffusion, Partial Pressures, and the Alveolar Gas Equation
Objective. Students will apply Dalton's law and Henry's law to calculate partial pressures of oxygen and carbon dioxide in alveolar gas and arterial blood, and use the alveolar gas equation to identify causes of hypoxemia.
⚠ Pending professional review
This lesson, its worked examples and its practice questions has not yet been verified by a licensed clinician in the field or by a certification or approval body. It is a study draft and may contain errors. Do not use it to make decisions about any patient or medication. Always follow your instructor, your supervising professional, and current official references and regulations.
VoTechWorks program approval and accreditation are still in progress. Credentials are issued only by the certifying bodies named in each program, after their own exams.
Pulmonary Gas Exchange: Diffusion, Partial Pressures, and the Alveolar Gas Equation
Why This Matters
Every clinical decision you make as a respiratory therapist — adjusting FiO₂, setting ventilator parameters, interpreting arterial blood gases — rests on understanding how oxygen moves from room air into the bloodstream and how carbon dioxide travels in the opposite direction. Errors in this reasoning can lead to inadequate oxygenation or unnecessary interventions, both of which harm patients. Master these principles before you touch any patient.
Dalton's Law of Partial Pressures
The air we breathe is a mixture of gases. Dalton's Law states that the total pressure of a gas mixture equals the sum of the pressures each gas would exert if it occupied the space alone. Each individual pressure is called a partial pressure.
At sea level, barometric pressure (PB) is approximately 760 mmHg. Dry air is about 21% oxygen (FiO₂ = 0.21). The partial pressure of oxygen in dry air is therefore:
PO₂ = FiO₂ × PB = 0.21 × 760 = 159.6 mmHg
However, air entering the airways is immediately humidified and warmed to body temperature (37 °C). Water vapor at 37 °C exerts a pressure of 47 mmHg (PH₂O). This water vapor dilutes every other gas, so it must be subtracted before calculating partial pressures of inhaled gases:
Inspired PO₂ = FiO₂ × (PB − PH₂O) = 0.21 × (760 − 47) = 0.21 × 713 ≈ 150 mmHg
The Alveolar Gas Equation
Once humidified air reaches the alveoli, oxygen is consumed and carbon dioxide is added. The alveolar gas equation accounts for this and gives us the partial pressure of oxygen in the alveoli (PAO₂):
PAO₂ = FiO₂ × (PB − PH₂O) − PaCO₂ / RQ
- FiO₂: fraction of inspired oxygen (decimal form, e.g., 0.21 for room air)
- PB: barometric pressure (mmHg)
- PH₂O: water vapor pressure at body temperature = 47 mmHg
- PaCO₂: arterial partial pressure of carbon dioxide (a reliable approximation of alveolar CO₂)
- RQ: respiratory quotient — the ratio of CO₂ produced to O₂ consumed; assumed to be 0.8 unless otherwise stated
At sea level on room air with a normal PaCO₂ of 40 mmHg:
PAO₂ = 0.21 × (760 − 47) − 40 / 0.8 = 149.7 − 50 = 99.7 mmHg ≈ 100 mmHg
Henry's Law and Gas Solubility
Henry's Law states that the amount of a gas dissolved in a liquid is proportional to its partial pressure above that liquid (at constant temperature). This explains why oxygen dissolved in plasma is directly tied to PAO₂ — higher alveolar O₂ partial pressure drives more O₂ into the blood. It also explains why CO₂, being about 20 times more soluble than O₂ in blood, diffuses across the alveolar-capillary membrane with relative ease.
Normal Gas Values: Alveolar and Arterial
| Location | PO₂ (mmHg) | PCO₂ (mmHg) |
|---|---|---|
| Alveolar (PAO₂ / PACO₂) | ~100 | ~40 |
| Arterial (PaO₂ / PaCO₂) | 80–100 | 35–45 |
| Mixed venous | ~40 | ~45 |
Note that arterial PaO₂ is slightly lower than PAO₂. This normal difference reflects small amounts of physiologic shunting and ventilation-perfusion (V/Q) mismatch. The difference is quantified as the alveolar-arterial (A-a) oxygen gradient:
A-a gradient = PAO₂ − PaO₂
A normal A-a gradient on room air in a young adult is roughly 5–15 mmHg; it increases with age and with supplemental oxygen. An elevated A-a gradient indicates a problem with gas exchange at the lung level.
Four Causes of Hypoxemia
Hypoxemia is a below-normal PaO₂. Understanding its cause directs your intervention:
1. Hypoventilation: Reduced alveolar ventilation raises PaCO₂, which displaces O₂ in the alveolus. PAO₂ falls even though the lungs themselves are normal. A-a gradient is normal. Treatment: support ventilation.
2. V/Q mismatch: Some lung units are ventilated but poorly perfused, or perfused but poorly ventilated. Most common cause of hypoxemia in clinical practice (pneumonia, COPD, pulmonary embolism). A-a gradient is elevated. Treatment: improve V/Q matching; supplemental O₂ often helps.
3. Diffusion impairment: Thickened alveolar-capillary membrane (pulmonary fibrosis, pulmonary edema) slows gas transfer. A-a gradient is elevated. O₂ usually responds to supplemental oxygen; CO₂ is rarely a problem due to its high solubility.
4. Shunt: Blood bypasses ventilated alveoli (intracardiac shunt, consolidated lung). A-a gradient is elevated. Hypoxemia is refractory to supplemental oxygen — this is an important clinical red flag.
High altitude reduces PB, which lowers PAO₂ even with normal lung function; A-a gradient remains normal.
Safety and Scope of Practice
- Never adjust FiO₂ or ventilator settings without verifying your calculations and confirming with current blood gas data and physician orders.
- Recognize that a normal SpO₂ does not rule out hypercapnia — you must check PaCO₂ separately.
- When you identify a cause of hypoxemia, communicate findings clearly using correct terminology; the physician orders treatment, but accurate assessment is your professional responsibility.
- Errors in applying the alveolar gas equation (wrong units, wrong RQ, forgetting to subtract PH₂O) will produce incorrect PAO₂ values and could contribute to clinical misjudgment. Check your arithmetic.
Key terms10
Partial pressureThe pressure exerted by a single gas in a mixture, calculated as the fraction of that gas multiplied by the total pressure of the mixture.
Dalton's LawThe total pressure of a gas mixture equals the sum of the partial pressures of all component gases.
Henry's LawThe amount of a gas dissolved in a liquid is proportional to its partial pressure above the liquid at a given temperature.
Alveolar gas equationPAO₂ = FiO₂ × (PB − PH₂O) − PaCO₂/RQ; calculates the partial pressure of oxygen in the alveoli.
Respiratory quotient (RQ)The ratio of carbon dioxide produced to oxygen consumed by the body; assumed to be 0.8 under typical conditions.
A-a gradient (alveolar-arterial oxygen gradient)The difference between alveolar PAO₂ and arterial PaO₂; an elevated value indicates impaired gas exchange at the lung level.
HypoxemiaAn abnormally low partial pressure of oxygen in arterial blood (PaO₂).
ShuntBlood that passes from the right side of the heart to the left without participating in gas exchange; produces hypoxemia that does not respond to supplemental oxygen.
Diffusion impairmentSlowed transfer of gas across the alveolar-capillary membrane, typically due to membrane thickening, resulting in an elevated A-a gradient.
V/Q mismatchAn imbalance between ventilation and perfusion in lung units; the most common cause of hypoxemia in clinical practice.
Worked examples4
1. A patient breathes room air (FiO₂ = 0.21) at sea level (PB = 760 mmHg). Their PaCO₂ is 40 mmHg. Calculate PAO₂ using the alveolar gas equation.
- Identify values: FiO₂ = 0.21, PB = 760 mmHg, PH₂O = 47 mmHg, PaCO₂ = 40 mmHg, RQ = 0.8.
- Calculate the inspired oxygen term: FiO₂ × (PB − PH₂O) = 0.21 × (760 − 47) = 0.21 × 713 = 149.73 mmHg.
- Calculate the CO₂ correction term: PaCO₂ / RQ = 40 / 0.8 = 50 mmHg.
- Subtract: PAO₂ = 149.73 − 50 = 99.73 mmHg, rounded to approximately 100 mmHg.
Answer: PAO₂ ≈ 100 mmHg
2. A patient is receiving 40% oxygen (FiO₂ = 0.40) via Venturi mask at sea level. Their PaCO₂ is 50 mmHg (hypoventilation). Calculate PAO₂ and determine the A-a gradient if PaO₂ from the ABG is 65 mmHg.
- Identify values: FiO₂ = 0.40, PB = 760 mmHg, PH₂O = 47 mmHg, PaCO₂ = 50 mmHg, RQ = 0.8.
- Calculate inspired oxygen term: 0.40 × (760 − 47) = 0.40 × 713 = 285.2 mmHg.
- Calculate CO₂ correction: 50 / 0.8 = 62.5 mmHg.
- PAO₂ = 285.2 − 62.5 = 222.7 mmHg, approximately 223 mmHg.
- Calculate A-a gradient: PAO₂ − PaO₂ = 223 − 65 = 158 mmHg. This is markedly elevated, indicating significant gas-exchange impairment beyond simple hypoventilation.
Answer: PAO₂ ≈ 223 mmHg; A-a gradient ≈ 158 mmHg (markedly elevated)
3. A healthy hiker ascends to an altitude where barometric pressure is 523 mmHg. They breathe room air (FiO₂ = 0.21) and their PaCO₂ is 35 mmHg (mild hyperventilation from altitude). Calculate PAO₂.
- Identify values: FiO₂ = 0.21, PB = 523 mmHg, PH₂O = 47 mmHg, PaCO₂ = 35 mmHg, RQ = 0.8.
- Calculate inspired oxygen term: 0.21 × (523 − 47) = 0.21 × 476 = 99.96 mmHg.
- Calculate CO₂ correction: 35 / 0.8 = 43.75 mmHg.
- PAO₂ = 99.96 − 43.75 = 56.21 mmHg, approximately 56 mmHg.
- Note: The low PAO₂ is caused entirely by reduced PB; the lung itself is normal, so the A-a gradient would remain normal.
Answer: PAO₂ ≈ 56 mmHg (hypoxemia due to altitude, not lung disease)
4. A patient on room air has a PaO₂ of 58 mmHg and a PaCO₂ of 40 mmHg at sea level. Calculate PAO₂ and A-a gradient, and state what this elevated gradient suggests.
- Identify values: FiO₂ = 0.21, PB = 760 mmHg, PH₂O = 47 mmHg, PaCO₂ = 40 mmHg, RQ = 0.8.
- Calculate PAO₂: 0.21 × (760 − 47) − 40/0.8 = 0.21 × 713 − 50 = 149.73 − 50 = 99.73 mmHg ≈ 100 mmHg.
- Calculate A-a gradient: PAO₂ − PaO₂ = 100 − 58 = 42 mmHg.
- Interpret: A-a gradient of 42 mmHg is elevated above the normal range (~5–15 mmHg in a young adult on room air). This indicates the cause of hypoxemia is within the lung — V/Q mismatch, diffusion impairment, or shunt — not simple hypoventilation alone.
Answer: PAO₂ ≈ 100 mmHg; A-a gradient = 42 mmHg (elevated, indicating intrapulmonary cause of hypoxemia)
The math in this lesson2
Learners evaluate the alveolar gas equation from FiO₂, barometric pressure, water vapor and PaCO₂.
A-SSE.1N-Q.1
In class: Lecture and worked examples: instructor walks through Dalton's law, the alveolar gas equation (PAO2 = FiO2 × [PB − PH2O] − PaCO2/RQ), and normal alveolar and arterial gas values; students solve five calculation problems with increasing complexity. · Paired problem-solving: students receive a set of clinical scenarios (high altitude, hypoventilation, diffusion impairment) and calculate expected PAO2 and A-a gradient for each, then rank scenarios by severity of gas-exchange impairment. · Group debrief: pairs present one scenario each; class discusses how each cause of hypoxemia would be addressed differently by the respiratory therapist, linking physiology to intervention.
Materials: Egan's Fundamentals of Respiratory Care; calculation worksheet; scientific calculators; whiteboard; NBRC content outline (Therapist Multiple Choice exam blueprint, current version).
Check: Five-problem calculation quiz; students must correctly solve at least four of five problems including correct use of the alveolar gas equation to pass.
Practice check8
Answer each question, then check it. Nothing is recorded; this is your own practice.
Record this lesson on my transcript. Sign in with your key and enrollment email to record lessons (enroll free if you have no key). This page stays open to read and practise.