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Alveolar gas equation

 
Wikipedia: Alveolar gas equation

The alveolar partial pressure of oxygen (pO2) is required to calculate both the alveolar-arterial gradient of oxygen and the amount of right-to-left shunt, which are both clinically useful quantities. However it is not practicable to take a sample of gas from the alveoli in order to directly measure the partial pressure of oxygen. The alveolar gas equation allows the calculation of the alveolar partial pressure of oxygen from data that is practically measurable. It was first characterized in 1946.[1]

Contents

Assumptions

The equation relies on the following assumptions:

  • Inspired gas contains no carbon dioxide (CO2) or water
  • Nitrogen (and any other gases except oxygen) in the inspired gas are in equilibrium with their dissolved states in the blood
  • Inspired and alveolar gases obey the ideal gas law
  • Carbon dioxide (CO2) in the alveolar gas is in equilibrium with the arterial blood i.e. that the alveolar and arterial partial pressures are equal
  • The alveolar gas is saturated with water

Equation

p_AO_2=F_IO_2(P_{ATM}-pH_2O)-\frac{p_aCO_2(1-F_IO_2[1-RQ])}{RQ}

If FIO2 is small then
F_IO_2[1-RQ]\approx0
In which case the equation can be simplified to:
p_AO_2 \approx F_IO_2(P_{ATM}-pH_2O)-\frac{p_aCO_2}{RQ} where:

Quantity Description Sample value
pAO2 The alveolar partial pressure of oxygen (pO2) 107 mmHg
FIO2 The fraction of inspired gas that is oxygen (expressed as a decimal). 0.21
PATM The prevailing atmospheric pressure 760 mmHg
pH2O The saturated vapour pressure of water at body temperature and the prevailing atmospheric pressure 47 mmHg
paCO2 The arterial partial pressure of carbon dioxide (pCO2) 36 mmHg
RQ The respiratory quotient 0.8

Sample Values given for air at sea level at 37°C.

See also

References

External links



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