Effect of reduced hemoglobin concentration on leg oxygen uptake during maximal exercise in humans

Abstract

Maximum oxygen uptake (VO2max) is affected by hemoglobin concentration ([Hb]). Whether this is simply due to altered convection of O2 into the muscle microcirculation or also to [Hb]-dependent diffusive transport of O2 out of the muscle capillary is unknown in humans. To examine this, seven healthy volunteers performed four maximal cycle exercise bouts at sea level immediately after 8 wk at altitude (3,801 m, barometric pressure 485 Torr), a sojourn designed to increase [Hb]. The first two bouts were at ambient [Hb] of 15.9 +/- 0.7 g/100 ml breathing 21 or 12% O2 in random order. [Hb] was then decreased to a prealtitude level of 13.8 +/- 0.6 g/100 ml by venesection and isovolemic replacement with 5% albumin in 0.9% saline, and the exercise bouts were repeated. At whole body VO2max, PO2, PCO2, pH, and O2 saturation were measured in radial arterial and femoral venous blood. Femoral venous thermodilution blood flow was determined for calculation of leg VO2. Mean muscle capillary PO2 and muscle diffusing capacity (DO2) were computed by Bohr integration between measured arterial and femoral venous PO2. Averaged over both fractional concentrations of inspired O2, leg VO2 at maximum decreased by 17.7 +/- 4.3% as [Hb] was lowered while leg O2 delivery decreased by 17.5 +/- 2.6% and DO2 decreased by 10.7 +/- 2.7% (all P < 0.05). The relative contributions of decreases in leg O2 delivery and DO2 to the decrease in VO2max were computed to be 64 and 36%, respectively. These findings suggest that [Hb] is an important determinant of O2 diffusion rates into working muscle in humans. Possible mechanisms include 1) dependence of DO2 on intracapillary red blood cell spacing, 2) changes in the total rate of dissociation of O2 from [Hb], and 3) increased red blood cell flow heterogeneity as [Hb] is reduced.