P. Robach et al., Operation Everest III: role of plasma volume expansion on Vo(2max) during prolonged high-altitude exposure, J APP PHYSL, 89(1), 2000, pp. 29-37
We hypothesize that plasma volume decrease (Delta PV) induced by high-altit
ude (HA) exposure and intense exercise is involved in the limitation of max
imal O-2 uptake ((V)over dot O-2max) at HA. Eight male subjects were decomp
ressed for 31 days in a hypobaric chamber to the barometric equivalent of M
t. Everest (8,848 m). Maximal exercise was performed with and without plasm
a volume expansion (PVX, 219-292 mi) during exercise, at rea level (SL), at
HA (370 mmHg, equivalent to 6,000 m after 10-12 days) and after return to
SL (RSL, 1-3 days). Plasma volume (PTS) was determined at rest at SL, HA, a
nd RSL by Evans blue dilution. PV was decreased by 26% (P < 0.01) at HA and
was 10% higher at RSL than at SL. Exercise-induced Delta PV was reduced bo
th by PVX and HA (P < 0.05). Compar ed with SL, (V)over dot O-2max was decr
eased by 58 and 11% at HA and RSL, respectively. (V)over dot (2max) was enh
anced by PVX at HA (+9%, P < 0.05) but not at SL or RSL. The more PV was de
creased at HA, the more (V) over dot O-2 was improved by PVX (P < 0.05). At
exhaustion, plasma renin and aldosterone were riot modified at HA compared
with SL but were higher at RSL, whereas plasma atrial natriuretic factor w
as lower at HA. The present results suggest that PV contributes to the limi
tation of (V) over dot O-2 during acclimatization to HA. RSL-induced PVX, w
hich may be due to increased activity of the renin-aldosterone system, coul
d also influence the recovery of (V) over dot O-2.