We recently found [at approximately 90% maximal O2 consumption (VO2max)] that as inspiratory PO2 (PIO2) was reduced, VO2 and mixed venous PO2 (PVO2) fell together along a straight line through the origin, suggesting tissue diffusion limitation of VO2max. To extend these observations to VO2max and directly examine effluent venous blood from muscle, six normal men cycled at VO2max while breathing air, 15% O2 and 12% O2 in random order on a single day. From femoral venous, mixed venous, and radial arterial samples, we measured PO2, PCO2, pH, and lactate and computed mean muscle capillary PO2 by Bohr integration between arterial (PaO2) and femoral venous PO2 (PfvO2). VO2 and CO2 production (VCO2) were measured by expired gas analysis, VO2max averaged 61.5 +/- 6.2 (air), 48.6 +/- 4.8 (15% O2), and 38.1 +/- 4.1 (12% O2) ml.kg-1.min-1. Corresponding values were 16.8 +/- 5.6, 14.4 +/- 5.0, and 12.0 +/- 5.0 Torr for PfVO2; 23.6 +/- 3.2, 19.1 +/- 4.2, and 16.2 +/- 3.5 Torr for PVO2; and 38.5 +/- 5.4, 30.3 +/- 4.1, and 24.5 +/- 3.6 Torr for muscle capillary PO2 (PmCO2). Each of the PO2 variables was linearly related to VO2max (r = 0.99 each), with an intercept not different from the origin. Similar results were obtained when the subjects were pushed to a work load 30 W higher to ensure that VO2max had been achieved. By extending our prior observations 1) to maximum VO2 and 2) by direct sampling of femoral venous blood, we conclude that tissue diffusion limitation of VO2max may be present in normal humans. In addition, since PVO2, PfVO2, and PmCO2 all linearly relate to VO2max, we suggest that whichever of these is most readily obtained is acceptable for further evaluation of the hypothesis.

No abstract

Pulmonary gas exchange was studied in eight normal subjects both before and after 2 wk of altitude acclimatization at 3,800 m (12,470 ft, barometric pressure = 484 Torr). Respiratory and multiple inert gas tensions, ventilation, cardiac output (Q), and hemoglobin concentration were measured at rest and during three levels of constant-load cycle exercise during both normoxia [inspired PO2 (PIO2) = 148 Torr] and normobaric hypoxia (PIO2 = 91 Torr). After acclimatization, the measured alveolar-arterial PO2 difference (A-aPO2) for any given work rate decreased (P less than 0.02). The largest reductions were observed during the highest work rates and were 24.8 +/- 1.4 to 19.7 +/- 0.8 Torr (normoxia) and 22.0 +/- 1.1 to 19.4 +/- 0.7 Torr (hypoxia). This could not be explained by changes in ventilation-perfusion inequality or estimated O2 diffusing capacity, which were unaffected by acclimatization. However, Q for any given work rate was significantly decreased (P less than 0.001) after acclimatization. We suggest that the reduction in A-aPO2 after acclimatization is a result of more nearly complete alveolar/end-capillary diffusion equilibration on the basis of a longer pulmonary capillary transit time.

The venous admixture to the pulmonary circulation in the anesthetized dog was calculated from the O2. tension of the alveolar gas and arterial blood and the O2 content of the arterial and mixed venous blood when breathing 43 or 99% oxygen-nitrogen mixtures. The average shunt flow varies from 1–10% and averages about 5% of the total flow. When positive pressure breathing is applied the shunt flow is reduced in every animal and averages 1.0%. Indirect evidence suggests that the major part of this shunt reduction with pressure breathing is due to the opening of lung areas which had spontaneously collapsed during the barbital anesthesia. Submitted on November 30, 1959