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Multiple Choice

Which factors are involved in calculating PAO2 using the alveolar gas equation?

The alveolar gas equation shows PAO2 depends on the oxygen you breathe and how the gas is conditioned in the lungs, balanced by CO2 removal. The factors involved are FiO2, barometric pressure, water vapor pressure, PaCO2, and the respiratory quotient. FiO2 and barometric pressure determine the pressure of oxygen entering the alveoli after humidification (Pb minus the water vapor pressure, PH2O, multiplied by FiO2). The term PaCO2 divided by the respiratory quotient (R) accounts for the amount of O2 used relative to CO2 produced during metabolism. In equation form, PAO2 is approximately FiO2*(Pb - PH2O) - (PaCO2 / R). For example, at sea level (Pb ≈ 760 mmHg, PH2O ≈ 47 mmHg) with FiO2 ≈ 0.21 and PaCO2 ≈ 40 mmHg, and R ≈ 0.8, PAO2 comes out around 100 mmHg. This framework explains why changing any of those factors shifts PAO2. Hb saturation does not set PAO2 directly, and using only FiO2 and PaCO2 omits essential influences like humidification and barometric pressure, so they aren’t sufficient on their own.

The alveolar gas equation shows PAO2 depends on the oxygen you breathe and how the gas is conditioned in the lungs, balanced by CO2 removal. The factors involved are FiO2, barometric pressure, water vapor pressure, PaCO2, and the respiratory quotient. FiO2 and barometric pressure determine the pressure of oxygen entering the alveoli after humidification (Pb minus the water vapor pressure, PH2O, multiplied by FiO2). The term PaCO2 divided by the respiratory quotient (R) accounts for the amount of O2 used relative to CO2 produced during metabolism. In equation form, PAO2 is approximately FiO2*(Pb - PH2O) - (PaCO2 / R). For example, at sea level (Pb ≈ 760 mmHg, PH2O ≈ 47 mmHg) with FiO2 ≈ 0.21 and PaCO2 ≈ 40 mmHg, and R ≈ 0.8, PAO2 comes out around 100 mmHg. This framework explains why changing any of those factors shifts PAO2. Hb saturation does not set PAO2 directly, and using only FiO2 and PaCO2 omits essential influences like humidification and barometric pressure, so they aren’t sufficient on their own.