ABSTRACT
Negative arterial to end-tidal pco2 differences ((a-ET)pco2) have been reported in normoxia. To determine the influence of blood temperature on (a-ET)pco2, 11 volunteers (21 ± 2 years) performed incremental exercise to exhaustion in normoxia (Nx, Pio2: 143 mmHg) and hypoxia (Hyp, Pio2: 73 mmHg), while arterial blood gases and temperature (ABT) were simultaneously measured together with end-tidal pco2 (PE tco2). After accounting for blood temperature, the (a-ET) pco2 was reduced (in absolute values) from -4.2 ± 1.6 to -1.1 ± 1.5 mmHg in normoxia and from -1.7 ± 1.6 to 0.9 ± 0.9 mmHg in hypoxia (both P < 0.05). The temperature corrected (a-ET)pco2 was linearly related with absolute and relative exercise intensity, VO2, VCO2, and respiratory rate (RR) in normoxia and hypoxia (R(2): 0.52-0.59). Exercise CO2 production and PE tco2 values were lower in hypoxia than normoxia, likely explaining the greater (less negative) (a-ET)pco2 difference in hypoxia than normoxia (P < 0.05). At near-maximal exercise intensity the (a-ET)pco2 lies close to 0 mmHg, that is, the mean Paco2 and the mean PE tco2 are similar. The mean exercise (a-ET)pco2 difference is closely related to the mean A-aDO2 difference (r = 0.90, P < 0.001), as would be expected if similar mechanisms perturb the gas exchange of O2 and CO2 during exercise. In summary, most of the negative (a-ET)pco2 values observed in previous studies are due to lack of correction of Paco2 for blood temperature. The absolute magnitude of the (a-ET)pco2 difference is lower during exercise in hypoxia than normoxia.
