Alveolar Gas Equation:
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The alveolar gas equation calculates the partial pressure of oxygen in the alveoli (PAO2). It's fundamental for understanding pulmonary gas exchange and assessing respiratory function.
The calculator uses the alveolar gas equation:
Where:
Explanation: The equation accounts for oxygen dilution by water vapor and the effect of CO2 on alveolar oxygen concentration.
Details: PAO2 is essential for calculating the alveolar-arterial (A-a) gradient, which helps differentiate causes of hypoxemia and assess lung function.
Tips: Enter all required values. Defaults are provided for sea-level conditions (PB=760, PH2O=47, FiO2=0.21, PaCO2=40, R=0.8). Adjust for altitude or different clinical scenarios.
Q1: What is a normal PAO2 value?
A: At sea level breathing room air, normal is about 100 mmHg. It decreases with altitude and increases with supplemental oxygen.
Q2: Why is water vapor pressure important?
A: Water vapor dilutes inspired gases in the alveoli. At body temperature (37°C), water vapor pressure is 47 mmHg.
Q3: What is the respiratory quotient (R)?
A: R is the ratio of CO2 produced to O2 consumed. It's typically 0.8 for normal diets but varies with metabolism.
Q4: How does altitude affect PAO2?
A: Lower barometric pressure at altitude reduces PAO2. For example, at 5000 ft, PB ≈ 632 mmHg.
Q5: What's the difference between PAO2 and PaO2?
A: PAO2 is alveolar oxygen, while PaO2 is arterial oxygen. The difference (A-a gradient) indicates gas exchange efficiency.