Alveolar Gas Composition
When the inspired gas reaches the alveolus, O2 is transported across the alveolar membrane, and CO2 moves from the capillary bed into the alveolus. The process by which this occurs is described in Chapter 23. At the end of inspiration and with the glottis open, the total pressure in the alveolus is atmospheric; thus, the partial pressures of the gases in the alveolus must equal the total pressure, which in this case is atmospheric. The composition of the gas mixture, however, is changed and can be described as
where PIO2 is the inspired partial pressure of O2, which is equal to the fraction (F) of inspired O2 (FIO2) times barometric pressure (Pb) minus water vapor pressure (PH2O). PACO2 is the CO2 tension of alveolar gas, and R is the respiratory exchange ratio or respiratory quotient. The respiratory quotient is the ratio of CO2 excreted (CO2) to the O2 taken up (O2) by the lungs. This quotient is the amount of CO2 produced relative to the amount of O2 consumed by metabolism and is dependent on caloric intake. The respiratory quotient varies between 0.7 and 1.0 and is 0.7 in states of exclusive fatty acid metabolism and 1.0 in states of exclusive carbohydrate metabolism. Under normal dietary conditions, the respiratory quotient is assumed to be 0.8. Thus, the quantity of O2 taken up exceeds the quantity of CO2 that is released in the alveoli.
The partial pressures of O2, CO2, and N2 from ambient air to the alveolus are shown in Table 22-1.
Table 22-1 Total and Partial Pressures of Respiratory Gases in Ideal Alveolar Gas and Blood at Sea Level (760 mmHg)
where CO2 is the rate of CO2 production by the body, A is alveolar ventilation, and FACO2 is the fraction of CO2 in dry alveolar gas. This relationship demonstrates that the rate of elimination of CO2 from the alveolus is related to alveolar ventilation and to the fraction of CO2 in the alveolus. Alveolar PACO2 is defined by the following:
Hence, we can substitute in the previous equation and demonstrate the following relationship: