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Alveolar gas equation

From Wikipedia, the free encyclopedia
Formula for the partial pressure of alveolar oxygen

Thealveolar gas equation is the method for calculatingpartial pressure ofalveolar oxygen (pAO2). The equation is used in assessing if thelungs are properly transferringoxygen into theblood. The alveolar air equation is not widely used in clinical medicine, probably because of the complicated appearance of its classic forms.The partial pressure of oxygen (pO2) in thepulmonary alveoli is required to calculate both thealveolar-arterial gradient of oxygen and the amount of right-to-leftcardiac shunt, which are both clinically useful quantities. However, it is not practical 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]

Assumptions

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The equation relies on the following assumptions:

  • Inspired gas contains no carbon dioxide (CO2)
  • 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 theideal 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

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pAO2=FIO2(PATMpH2O)paCO2(1FIO2(1RER))RER{\displaystyle p_{A}{\ce {O2}}=F_{I}{\ce {O2}}(P_{{\ce {ATM}}}-p{\ce {H2O}})-{\frac {p_{a}{\ce {CO2}}(1-F_{I}{\ce {O2}}(1-{\ce {RER}}))}{{\ce {RER}}}}}

IfFiO2 is small, or more specifically ifFIO2(1RER)1{\displaystyle F_{I}{\ce {O2}}(1-{\ce {RER}})\ll 1} then the equation can be simplified to:

pAO2FIO2(PATMpH2O)paCO2RER{\displaystyle p_{A}{\ce {O2}}\approx F_{I}{\ce {O2}}(P_{{\ce {ATM}}}-p{\ce {H2O}})-{\frac {p_{a}{\ce {CO2}}}{{\ce {RER}}}}}

where:

QuantityDescriptionSample value
pAO2{\displaystyle p_{A}{\ce {O2}}}The alveolar partial pressure of oxygen (pO2{\displaystyle p{\ce {O2}}})107 mmHg (14.2 kPa)
FIO2{\displaystyle F_{I}{\ce {O2}}}The fraction of inspired gas that is oxygen (expressed as a decimal).0.21
PATM{\displaystyle P_{ATM}}The prevailing atmospheric pressure760 mmHg (101 kPa)
pH2O{\displaystyle p{\ce {H2O}}}The saturated vapour pressure of water at body temperature and the prevailing atmospheric pressure47 mmHg (6.25 kPa)
paCO2{\displaystyle p_{a}{\ce {CO2}}}The arterial partial pressure of carbon dioxide (pCO2{\displaystyle p{\ce {CO2}}} )40 mmHg (5.33 kPa)
RER{\displaystyle {\text{RER}}}Therespiratory exchange ratio0.8

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

DoublingFiO2 will doublepiO2.

Other possible equations exist to calculate the alveolar air.[2][3][4][5][6][7][8]

pAO2=FIO2(PBpH2O)pACO2(FIO2+1FIO2R)=pIO2pACO2(FIO2+1FIO2R)=pIO2VTVTVD(pIO2pEO2)=pEO2pIO2(VDVT)1VDVT{\displaystyle {\begin{aligned}p_{A}{\ce {O2}}&=F_{I}{\ce {O2}}\left(PB-p{\ce {H2O}}\right)-p_{A}{\ce {CO2}}\left(F_{I}{\ce {O2}}+{\frac {1-F_{I}{\ce {O2}}}{R}}\right)\\[4pt]&=p_{I}{\ce {O2}}-p_{A}{\ce {CO2}}\left(F_{I}{\ce {O2}}+{\frac {1-F_{I}{\ce {O2}}}{R}}\right)\\[4pt]&=p_{I}{\ce {O2}}-{\frac {V_{T}}{V_{T}-V_{D}}}\left(p_{I}{\ce {O2}}-p_{E}{\ce {O2}}\right)\\[4pt]&={\frac {p_{E}{\ce {O2}}-p_{I}{\ce {O2}}\left({\frac {V_{D}}{V_{T}}}\right)}{1-{\frac {V_{D}}{V_{T}}}}}\end{aligned}}}

Abbreviated alveolar air equation

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pAO2=pEO2piO2VDVT1VDVT{\displaystyle p_{A}{\ce {O2}}={\frac {p_{E}{\ce {O2}}-p_{i}{\ce {O2}}{\frac {V_{D}}{V_{T}}}}{1-{\frac {V_{D}}{V_{T}}}}}}pAO2,pEO2, andpiO2 are the partial pressures of oxygen in alveolar, expired, and inspired gas, respectively, and VD/VT is the ratio of physiologic dead space over tidal volume.[9]

Respiratory quotient (R)

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R=pECO2(1FIO2)piO2pEO2(pECO2FiO2){\displaystyle R={\frac {p_{E}{\ce {CO2}}(1-F_{I}{\ce {O2}})}{p_{i}{\ce {O2}}-p_{E}{\ce {O2}}-(p_{E}{\ce {CO2}}*F_{i}{\ce {O2}})}}}

Physiologic dead space over tidal volume (VD/VT)

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VDVT=pACO2pECO2pACO2{\displaystyle {\frac {V_{D}}{V_{T}}}={\frac {p_{A}{\ce {CO2}}-p_{E}{\ce {CO2}}}{p_{A}{\ce {CO2}}}}}

Intuitive Explanation

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As it is not practical 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.

Firstly, the partial pressure of inhaled oxygen is simply the fraction of inhaled oxygen multiplied by the atmospheric pressureFIO2PATM{\displaystyle F_{I}{\ce {O2}}*P_{{\ce {ATM}}}}. Once oxygen enters the airways, we must account for the partial pressure of water vapor which is assumed to reach 100% saturation, henceFIO2(PATMpH2O){\displaystyle F_{I}{\ce {O2}}(P_{{\ce {ATM}}}-p{\ce {H2O}})}. Once the humidified atmospheric air reaches the alveoli, gas exchange takes place so we need to consider the amount ofO2{\displaystyle {\ce {O2}}} that enters the blood andCO2{\displaystyle {\ce {CO2}}} that leaves the blood. Conveniently, the arterial bloodpaCO2{\displaystyle p_{a}{\ce {CO2}}} equals the alveolar bloodpACO2{\displaystyle p_{A}{\ce {CO2}}} and so this is a value we know. It would also be convenient if the same number ofCO2{\displaystyle {\ce {CO2}}} andO2{\displaystyle {\ce {O2}}} molecules were exchanged, in which case the alveolar gas equation would simply bepAO2FIO2(PATMpH2O)paCO2{\displaystyle p_{A}{\ce {O2}}\approx F_{I}{\ce {O2}}(P_{{\ce {ATM}}}-p{\ce {H2O}})-p_{a}{\ce {CO2}}}. However in reality the number ofCO2{\displaystyle {\ce {CO2}}} molecules exchanged differs slightly from the number ofO2{\displaystyle {\ce {O2}}} molecules, according to therespiratory exchange ratio. Hence the alveolar gas equation becomes:

pAO2FIO2(PATMpH2O)paCO2RER{\displaystyle p_{A}{\ce {O2}}\approx F_{I}{\ce {O2}}(P_{{\ce {ATM}}}-p{\ce {H2O}})-{\frac {p_{a}{\ce {CO2}}}{{\ce {RER}}}}}

See also

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References

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  1. ^Curran-Everett D (June 2006). "A classic learning opportunity from Fenn, Rahn, and Otis (1946): the alveolar gas equation".Adv Physiol Educ.30 (2):58–62.doi:10.1152/advan.00076.2005.PMID 16709734.S2CID 42010762.
  2. ^Raymond L, Dolan W, Dutton R, et al: Pulmonary function and gas exchange during altitude hypoxia (abstract).Clin Res 19:147, 1971
  3. ^Spaur WH, Raymond LW, Knott MM, et al: Dyspnea in divers at 49.5 ATA: Mechanical not chemical in origin.Undersea Biomed Res 4:183-198, 1977
  4. ^Rossier P-H, Blickenstorfer E: Espace mort et hyperventilation.Helv Med Acta 13:328-332, 1946
  5. ^Riley RL, Lilienthal JL Jr, Proemmel DD, et al: On thedetermination of the physiologically effective pressures of oxygen and carbon dioxide in alveolar air.Am J Physiol 147:191-198, 1946
  6. ^McNicol MW, Campbell EJM: Severity of respiratory failure: arterial blood gases in untreated patients.Lancet 1:336-338, 1965
  7. ^Begin R, Renzetti AD Jr: Alveolar-arterial oxygen pressure gradient: I. Comparison between an assumed and actual respiratory quotient in stable chronic pulmonary disease; Relationship to aging and closing volume in normal subjects.Respir Care 22:491-500, 1977
  8. ^Suwa K, Geffin B, Pontoppidan H, et al: A nomogram fordeadspace requirement during prolonged artificial ventilation.Anesthesiology 29:1206-1210, 1968
  9. ^Fenn WO, Rahn H, Otis AB: A theoretical study of the composition of alveolar air at altitude.Am J Physiol 146:637-653, 1946

External links

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Respiration
Control
Lung volumes
Circulation
Interactions
Insufficiency
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