Wolfel E E, Groves B M, Brooks G A, Butterfield G E, Mazzeo R S, Moore L G, Sutton J R, Bender P R, Dahms T E, McCullough R E
Cardiovascular Pulmonary Research Laboratory, University of Colorado Health Sciences Center, Denver 80262.
J Appl Physiol (1985). 1991 Mar;70(3):1129-36. doi: 10.1152/jappl.1991.70.3.1129.
Arterial O2 delivery during short-term submaximal exercise falls on arrival at high altitude but thereafter remains constant. As arterial O2 content increases with acclimatization, blood flow falls. We evaluated several factors that could influence O2 delivery during more prolonged submaximal exercise after acclimatization at 4,300 m. Seven men (23 +/- 2 yr) performed 45 min of steady-state submaximal exercise at sea level (barometric pressure 751 Torr), on acute ascent to 4,300 m (barometric pressure 463 Torr), and after 21 days of residence at altitude. The O2 uptake (VO2) was constant during exercise, 51 +/- 1% of maximal VO2 at sea level, and 65 +/- 2% VO2 at 4,300 m. After acclimatization, exercise cardiac output decreased 25 +/- 3% compared with arrival and leg blood flow decreased 18 +/- 3% (P less than 0.05), with no change in the percentage of cardiac output to the leg. Hemoglobin concentration and arterial O2 saturation increased, but total body and leg O2 delivery remained unchanged. After acclimatization, a reduction in plasma volume was offset by an increase in erythrocyte volume, and total blood volume did not change. Mean systemic arterial pressure, systemic vascular resistance, and leg vascular resistance were all greater after acclimatization (P less than 0.05). Mean plasma norepinephrine levels also increased during exercise in a parallel fashion with increased vascular resistance. Thus we conclude that both total body and leg O2 delivery decrease after arrival at 4,300 m and remain unchanged with acclimatization as a result of a parallel fall in both cardiac output and leg blood flow and an increase in arterial O2 content.(ABSTRACT TRUNCATED AT 250 WORDS)
在短期次最大强度运动期间,到达高海拔时动脉血氧输送量会下降,但此后保持恒定。随着动脉血氧含量随适应过程增加,血流量会下降。我们评估了几个可能影响在4300米适应环境后进行更长时间次最大强度运动期间血氧输送的因素。七名男性(23±2岁)在海平面(气压751托)、急性上升到4300米(气压463托)以及在海拔居住21天后进行了45分钟的稳态次最大强度运动。运动期间摄氧量(VO₂)恒定,在海平面为最大VO₂的51±1%,在4300米为VO₂的65±2%。适应环境后,运动心输出量比到达时下降了25±3%,腿部血流量下降了18±3%(P<0.05),心输出量分配到腿部的百分比没有变化。血红蛋白浓度和动脉血氧饱和度增加,但全身和腿部的血氧输送量保持不变。适应环境后,血浆量的减少被红细胞量的增加所抵消,总血量没有变化。适应环境后,平均体循环动脉压、体循环血管阻力和腿部血管阻力均升高(P<0.05)。运动期间平均血浆去甲肾上腺素水平也与血管阻力增加呈平行升高。因此,我们得出结论,到达4300米后全身和腿部的血氧输送量均下降,适应环境后保持不变,这是由于心输出量和腿部血流量同时下降以及动脉血氧含量增加所致。(摘要截短至250字)