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PubMed2003

Effects of high altitude and water deprivation on arginine vasopressin release in men.

High-altitude exposure changes the distribution of body water and electrolytes. Arginine vasopressin (AVP) may influence these alterations. The purpose of this study was to examine the effect of a 24-h water deprivation trial (WDT) on AVP release after differing altitude exposures. Seven healthy males (age 22 +/- 1 yr, height 176 +/- 2 cm, mass 75.3 +/- 1.8 kg) completed three WDTs: at sea level (SL), after acute altitude exposure (2 days) to 4,300 m (AA), and after prolonged altitude exposure (20 days) to 4,300 m (PA). Body mass, standing and supine blood pressures, plasma osmolality (Posm), and plasma AVP (PAVP) were measured at 0, 12, 16, and 24 h of each WDT. Urine volume was measured at each void throughout testing. Baseline Posm increased from SL to altitude (SL 291.7 +/- 0.8 mosmol/kgH2O, AA 299.6 +/- 2.2 mosmol/kgH2O, PA 302.3 +/- 1.5 mosmol/kgH2O, P < 0.05); however, baseline PAVP measurements were similar. Despite similar Posm values, the maximal PAVP response during the WDT (at 16 h) was greater at altitude than at SL (SL 1.7 +/- 0.5 pg/ml, AA 6.4 +/- 0.7 pg/ml, PA 8.7 +/- 0.9 pg/ml, P < 0.05). In conclusion, hypoxia appeared to alter AVP regulation by raising the osmotic threshold and increasing AVP responsiveness above that threshold.

Adult↗
PubMed2005

Endocrine responses to acute and chronic high-altitude exposure (4,300 meters): modulating effects of caloric restriction.

High-altitude anorexia leads to a hormonal response pattern modulated by both hypoxia and caloric restriction (CR). The purpose of this study was to compare altitude-induced neuroendocrine changes with or without energy imbalance and to explore how energy sufficiency alters the endocrine acclimatization process. Twenty-six normal-weight, young men were studied for 3 wk. One group [hypocaloric group (HYPO), n = 9] stayed at sea level and consumed 40% fewer calories than required to maintain body weight. Two other groups were deployed to 4,300 meters (Pikes Peak, CO), where one group (ADQ, n = 7) was adequately fed to maintain body weight and the other [deficient group (DEF), n = 10] had calories restricted as above. HYPO experienced a typical CR-induced reduction in many hormones such as insulin, testosterone, and leptin. At altitude, fasting glucose, insulin, and epinephrine exhibited a muted rise in DEF compared with ADQ. Free thyroxine, thyroid-stimulating hormone, and norepinephrine showed similar patterns between the two altitude groups. Morning cortisol initially rose higher in DEF than ADQ at 4,300 meters, but the difference disappeared by day 5. Testosterone increased in both altitude groups acutely but declined over time in DEF only. Adiponectin and leptin did not change significantly from sea level baseline values in either altitude group regardless of energy intake. These data suggest that hypoxia tends to increase blood hormone concentrations, but anorexia suppresses elements of the endocrine response. Such suppression results in the preservation of energy stores but may sacrifice the facilitation of oxygen delivery and the use of oxygen-efficient fuels.

Adaptation, Physiological↗
PubMed1991

Arterial catecholamine responses during exercise with acute and chronic high-altitude exposure.

Exercise at high altitude is a stress that activates the sympathoadrenal systems, which could affect responses to acute altitude exposure and promote adaptations during chronic altitude exposure. However, catecholamine levels are not clearly described over time at high altitude. In seven male volunteers (23 yr, 72 kg), resting arterial norepinephrine concentrations (ng/ml) on arrival at Pikes Peak (0.338 +/- 0.041) decreased compared with sea-level values (0.525 +/- 0.034) but increased to above sea-level values after 21 days at 4,300 m (0.798 +/- 0.052). Furthermore, during 45 min of constant submaximal exercise, values were similar at sea level (1.670 +/- 0.221) and on acute exposure to 4,300 m (2.123 +/- 0.086) but increased after 21 days of chronic exposure (2.693 +/- 0.216). By contrast, resting arterial epinephrine values (ng/ml) during acute and chronic exposure (0.708 +/- 0.033 vs. 0.448 +/- 0.026) both exceeded those of sea level (0.356 +/- 0.020). During exercise values on arrival were greater than at sea level (0.921 +/- 0.024 vs. 0.397 +/- 0.035) but fell to 0.612 +/- 0.025 ng/ml after 21 days. Exercise norepinephrine levels were related to systemic vascular resistance measurements (r = 0.93), whereas epinephrine levels were related to circulating lactate (r = 0.95). We conclude that during exercise at altitude there is a dissociation between norepinephrine, an indicator of sympathetic neural activity, and epinephrine, an indicator of adrenal medullary response. These actions may account for different metabolic and physiological responses to acute vs. chronic altitude exposure.

Adult↗
PubMed2004

Plasma volume expansion does not increase maximal cardiac output or VO2 max in lowlanders acclimatized to altitude.

With altitude acclimatization, blood hemoglobin concentration increases while plasma volume (PV) and maximal cardiac output (Qmax) decrease. This investigation aimed to determine whether reduction of Qmax at altitude is due to low circulating blood volume (BV). Eight Danish lowlanders (3 females, 5 males: age 24.0 +/- 0.6 yr; mean +/- SE) performed submaximal and maximal exercise on a cycle ergometer after 9 wk at 5,260 m altitude (Mt. Chacaltaya, Bolivia). This was done first with BV resulting from acclimatization (BV = 5.40 +/- 0.39 liters) and again 2-4 days later, 1 h after PV expansion with 1 liter of 6% dextran 70 (BV = 6.32 +/- 0.34 liters). PV expansion had no effect on Qmax, maximal O2 consumption (VO2), and exercise capacity. Despite maximal systemic O2 transport being reduced 19% due to hemodilution after PV expansion, whole body VO2 was maintained by greater systemic O2 extraction (P < 0.05). Leg blood flow was elevated (P < 0.05) in hypervolemic conditions, which compensated for hemodilution resulting in similar leg O2 delivery and leg VO2 during exercise regardless of PV. Pulmonary ventilation, gas exchange, and acid-base balance were essentially unaffected by PV expansion. Sea level Qmax and exercise capacity were restored with hyperoxia at altitude independently of BV. Low BV is not a primary cause for reduction of Qmax at altitude when acclimatized. Furthermore, hemodilution caused by PV expansion at altitude is compensated for by increased systemic O2 extraction with similar peak muscular O2 delivery, such that maximal exercise capacity is unaffected.

Acclimatization↗
PubMed1995

Acclimatization to high altitude increase muscle sympathetic activity both at rest and during exercise.

This investigation examined the relationship between alterations in plasma norepinephrine associated with 21 days of high-altitude exposure and muscle sympathetic activity both at rest and during exercise. Healthy sea level residents, divided into a control group (n = 5) receiving a placebo or a drug group (n = 6) receiving 240 mg/day of propranolol, were studied while at sea level, upon arrival (acute), and after 21 days of residence (chronic) at 4,300 m. Arterial norepinephrine levels and net leg uptake and release of norepinephrine were determine both at rest and during 45 min of submaximal exercise via samples collected from femoral arterial and venous catheters. Arterial norepinephrine levels increased significantly after chronic altitude exposure both at rest (84%) and during exercise (174%) compared with sea level and acute values. A net uptake of norepinephrine was found in resting legs at sea level (0.28 +/- 0.05 nmol/min) and with acute exposure (0.07 +/- 0.06 nmol/min); however, a significant switch to net leg norepinephrine release was observed with chronic altitude exposure (0.51 +/- 0.11 nmol/min). With exercise, a net release of norepinephrine by the leg occurred across all conditions with chronic exposure, again eliciting the greatest values (5.3 +/- 0.6, 8.0 +/- 1.7, and 14.4 +/- 3.1 nmol/min for sea level, acute, and chronic exposure, respectively). It was concluded that muscle sympathetic activity is significantly elevated both at rest and during submaximal exercise as a result of chronic high-altitude exposure, and muscle is a major contributor to the increase in plasma norepinephrine levels associated with prolonged altitude exposure. The presence of dense beta-blockade did not alter this adaptation to altitude.

Acclimatization↗
PubMed1999

Effects on regional brain metabolism of high-altitude hypoxia: a study of six US marines.

Previous studies of brain glucose metabolism in people indigenous to high-altitude environments uncovered two response patterns: Quechuas native to the high Andes of South America sustained modest hypometabolism in most brain regions interrogated, whereas Sherpas, native to the Himalayas and considered by many biologists to be most effectively high-altitude adapted of all humans, showed brain metabolic patterns similar to lowlanders, with no acclimation effects noted. In the present study, the database was expanded to include hypoxia acclimation effects in lowlanders. Positron emission tomography (PET) and [(18)F]-2-deoxy-2-fluro-D-glucose (FDG) imaging techniques were used to assess regional cerebral glucose metabolic rates (rCMR(glc)) in six US marines (Caucasian lineage) before and after a 63-day training program for operations at high altitudes ranging from 10,500 to 20,320 ft. Significant changes in rCMR(glc) were found for 7 of 25 brain regions examined. Significant decreases in absolute cerebral glucose metabolism after high-altitude exposure were found in five regions: three frontal, the left occipital lobe, and the right thalamus. In contrast, for the right and left cerebellum significant increases in metabolism were found. The magnitudes of these differences, in terms of absolute metabolism, were large, ranging from 10 to 18%. Although the results may not be solely the result of lower oxygen levels at high altitude, these findings suggest that the brain of healthy human lowlanders responds to chronic hypoxia exposure with precise, region-specific fine tuning of rCMR(glc). The observed short-term hypoxia acclimation responses in these lowlanders clearly differ from the long-term hypoxia adaptations found in brain metabolism of people indigenous to high-altitude environments.

Adult↗
PubMed1975

Effect of altitude relocations upon AaDo2 at rest and during exercise.

The supine pulmonary venous admixture (shunt) has been measured at Cerro de Pasco, 4,350 m altitude in eight subjects native to high altitude (HAN) under resting condition. Alveolar-arterial O2 tension difference (AaDO2) was also determined at rest and during exercise. The same subjects were studied again after 10 days' sojourn at sea level in Lima at 150 m altitude. They were compared with four subjects from sea level (SLN) who were studied first at Lima and after 2 and 10 days at Cerro de Pasco. At altitude, AaDO2 was smaller in HAN than SLN both at rest and during exercise. Shunt was the same in both groups. It is concluded that HAN show more even ventilation/perfusion relationship (VA/Q) at altitude, probably due to their high pulmonary artery pressure. On the contrary, SLN show less even VA/Q on altitude exposure, since their shunt decreased 37%. At sea level, HAN increased their AaDO2 due partially to an increase of 110% in their shunt, and in part due to less even VA/Q as shown by augmented VD/VT ratios. Each group tended to have a more effective gas exchange in its own environment.

Adult↗
PubMed1976

Alkaline shift in lumbar and intracranial CSF in man after 5 days at high altitude.

In six healthy male volunteers at sea level (PB 747-759 Torr), we measured pH and PCO2 in cerebrospinal fluid (CSF), and in arterial and jugular bulb blood; from these data we estimated PCO2 (12) and pH for the intracranial portion of CSF. The measurements were repeated after 5 days in a hypobaric chamber (PB 447 Torr). Both lumbar and intracranial CSF were significantly more alkaline at simulated altitude than at sea level. Decrease in [HCO3-] IN lumbar CSF at altitude was similar to that in blood plasma. Both at sea level and at high altitude, PCO2 measured in the lumbar CSF was higher than that estimated for the intracranial CSF. At altitude, hyperoxia, in comparison with breathing room air, resulted in an increase in intracranial PCO2, and a decrease in the estimated pH in intracranial CSF. With hyperoxia at altitude, alveolar ventilation was significantly higher than during sea-level hyperoxia or normoxia, confirming that a degree of acclimatization had occurred. Changes in cerebral arteriovenous differences in CO2, measured in three subjects, suggest that cerebral blood flow may have been elevated after 5 days at altitude.

Acid-Base Equilibrium↗
PubMed1979

Evidence for increased intrathoracic fluid volume in man at high altitude.

To determine if subclinical pulmonary edema occurs commonly at high altitude, 25 soldiers participated in two consecutive 72-h field exercises, the first at low altitude (200-875 m) and the second at high altitude (3,000-4,300 m). Various aspects of ventilatory function and pulmonary mechanics were measured at 0, 36, and 72 h of each exercise. Based on physical examination and chest radiographs there was no evidence of pulmonary edema at high altitude. There was, however, an immediate and sustained decrease in vital capacity and transthoracic electrical impedance as well as a clockwise rotation of the transpulmonary pressure-volume curve. In contrast, closing capacity and residual volume did not change immediately upon arrival at high altitude but did increase later during the exposure. These observations are consistent with an abrupt increase in thoracic intravascular fluid volume upon arrival at high altitude followed by a more gradual increase in extravascular fluid volume in the peribronchial spaces of dependent lung regions.

Adolescent↗
PubMed1980

Control of breathing in Sherpas at low and high altitude.

Sherpas are well known for their physical performance at extreme altitudes, yet they are reported to have blunted ventilatory responses to acute hypoxia and relative hypoventilation in chronic hypoxia. To examine this paradox, we studied ventilatory control in Sherpas in comparison to that in Westerners at both low and high altitude. At low altitude, 25 Sherpas had higher minute ventilation, higher respiratory frequency, and lower end-tidal carbon dioxide tension than 25 Westerners. The hypoxic ventilatory response of Sherpas was found to be similar to that in Westerners, even though long altitude exposure had blunted the responses of some Sherpas. At high altitude, Sherpas again had higher minute ventilation and a tendency toward higher arterial oxygen saturation than Westerners. Oxygen administration increased ventilation further in Sherpas but decreased ventilation in Westerners. We conclude that Sherpas differ from other high-altitude natives; their hypoxic ventilatory response is not blunted, and they exhibit relative hyperventilation.

Adaptation, Physiological↗
PubMed1981

Collateral ventilation may protect against high-altitude pulmonary hypertension.

We propose that the pulmonary hypertension developed by cattle and swine at high altitude is associated with their lack of collateral ventilation. We reason that if collateral ventilation helps keep interregional oxygen tensions homogeneous, then in its absence, local ventilation-perfusion balance must rely on arterial constriction; the additional work causes arterial walls to be more muscular at low altitude, a characteristic of cattle and swine that appears prerequisite for the development of pulmonary hypertension at high altitude. In contrast, species with collateral ventilation, e.g., dogs, have thin-walled pulmonary arteries and therefore can not sustain pulmonary vasoconstriction at altitude. Sheep, however, challenge the hypothesis, because their thick lobular septae should block collateral ventilation, yet they have thin pulmonary arteries and resist high-altitude hypertension. We measured collateral ventilation by determining how long it takes air injected into isolated segments to escape. Cattle and swine had no collateral ventilation (time constants greater than 30 s), whereas dogs and sheep had collateral ventilation (time constants less than 0.8 s). These data support the hypothesis that only species without collateral ventilation develop pulmonary hypertension at high altitude.

Altitude↗
PubMed1985

Ventilation-perfusion inequality in normal humans during exercise at sea level and simulated altitude.

To investigate the effects of both exercise and acute exposure to high altitude on ventilation-perfusion (VA/Q) relationships in the lungs, nine young men were studied at rest and at up to three different levels of exercise on a bicycle ergometer. Altitude was simulated in a hypobaric chamber with measurements made at sea level (mean barometric pressure = 755 Torr) and at simulated altitudes of 5,000 (632 Torr), 10,000 (523 Torr), and 15,000 ft (429 Torr). VA/Q distributions were estimated using the multiple inert gas elimination technique. Dispersion of the distributions of blood flow and ventilation were evaluated by both loge standard deviations (derived from the VA/Q 50-compartment lung model) and three new indices of dispersion that are derived directly from inert gas data. Both methods indicated a broadening of the distributions of blood flow and ventilation with increasing exercise at sea level, but the trend was of borderline statistical significance. There was no change in the resting distributions with altitude. However, with exercise at high altitude (10,000 and 15,000 ft) there was a significant increase in dispersion of blood flow (P less than 0.05) which implies an increase in intraregional inhomogeneity that more than counteracts the more uniform topographical distribution that occurs. Since breathing 100% O2 at 15,000 ft abolished the increased dispersion, the greater VA/Q mismatching seen during exercise at altitude may be related to pulmonary hypertension.

Acclimatization↗
PubMed1986

Propranolol does not impair exercise oxygen uptake in normal men at high altitude.

Decreased maximal O2 uptake (VO2max) and stimulation of the sympathetic nervous system have been previously shown to occur at high altitude. We hypothesized that tachycardia mediated by beta-adrenergic stimulation acted to defend VO2max at high altitude. Propranolol treatment beginning before high-altitude (4,300 m) ascent reduced heart rate during maximal and submaximal exercise in six healthy men treated with propranolol (80 mg three times daily) compared with five healthy subjects receiving placebo (lactose). Compared with sea-level values, the VO2max fell on day 2 at high altitude, but the magnitude of fall was similar in the placebo and propranolol treatment groups (26 +/- 6 vs. 32 +/- 5%, P = NS) and VO2max remained similar at high altitude in both groups once treatment was discontinued. During 30 min of submaximal (80% of VO2max) exercise, propranolol-treated subjects maintained O2 uptake levels that were as large as those in placebo subjects. The maintenance of maximal or submaximal levels of O2 uptake in propranolol-treated subjects at 4,300 m could not be attributed to increased minute ventilation, arterial O2 saturation, or hemoglobin concentration. Rather, it appeared that propranolol-treated subjects maintained O2 uptake by transporting a greater proportion of the O2 uptake with each heartbeat. Thus, contrary to our hypothesis, beta-adrenergic blockade did not impair maximal or submaximal O2 uptake at high altitude due perhaps to compensatory mechanisms acting to maintain stroke volume and cardiac output.

Adult↗
PubMed1987

Internal carotid and vertebral arterial flow velocity in men at high altitude.

Cerebral blood flow increases at high altitude, but the mechanism of the increase and its role in adaptation to high altitude are unclear. We hypothesized that the hypoxemia at high altitude would increase cerebral blood flow, which would in turn defend O2 delivery to the brain. Noninvasive Doppler ultrasound was used to measure the flow velocities in the internal carotid and the vertebral arteries in six healthy male subjects. Within 2-4 h of arrival on Pikes Peak (4,300 m), velocities in both arteries were slightly and not significantly increased above sea-level values. By 18-44 h a peak increase of 20% was observed (combined P less than 0.025). Subsequently (days 4-12) velocities declined to values similar to those at sea level. At altitude the lowest arterial O2 saturation (SaO2) and the highest end-tidal PCO2 was observed on arrival. By day 4 and thereafter, when the flow velocities had returned toward sea-level values, hemoglobin concentration and SaO2 were increased over initial high-altitude values such that calculated O2 transport values were even higher than those at sea level. Although the cause of the failure for cerebral flow velocity to increase on arrival is not understood, the subsequent increase may act to defend brain O2 transport. With further increase in hemoglobin and SaO2 over time at high altitude, flow velocity returned to sea-level values.

Adult↗
PubMed1988

Operation Everest II: oxygen transport during exercise at extreme simulated altitude.

A decrease in maximal O2 uptake has been demonstrated with increasing altitude. However, direct measurements of individual links in the O2 transport chain at extreme altitude have not been obtained previously. In this study we examined eight healthy males, aged 21-31 yr, at rest and during steady-state exercise at sea level and the following inspired O2 pressures (PIO2): 80, 63, 49, and 43 Torr, during a 40-day simulated ascent of Mt. Everest. The subjects exercised on a cycle ergometer, and heart rate was recorded by an electrocardiograph; ventilation, O2 uptake, and CO2 output were measured by open circuit. Arterial and mixed venous blood samples were collected from indwelling radial or brachial and pulmonary arterial catheters for analysis of blood gases, O2 saturation and content, and lactate. As PIO2 decreased, maximal O2 uptake decreased from 3.98 +/- 0.20 l/min at sea level to 1.17 +/- 0.08 l/min at PIO2 43 Torr. This was associated with profound hypoxemia and hypocapnia; at 60 W of exercise at PIO2 43 Torr, arterial PO2 = 28 +/- 1 Torr and PCO2 = 11 +/- 1 Torr, with a marked reduction in mixed venous PO2 [14.8 +/- 1 (SE) Torr]. Considering the major factors responsible for transfer of O2 from the atmosphere to the tissues, the most important adaptations occurred in ventilation where a fourfold increase in alveolar ventilation was observed. Diffusion from alveolus to end-capillary blood was unchanged with altitude. The mass circulatory transport of O2 to the tissue capillaries was also unaffected by altitude except at PIO2 43 Torr where cardiac output was increased for a given O2 uptake. Diffusion from the capillary to the tissue mitochondria, reflected by mixed venous PO2, was also increased with altitude. With increasing altitude, blood lactate was progressively reduced at maximal exercise, whereas at any absolute and relative submaximal work load, blood lactate was higher. These findings suggest that although glycogenolysis may be accentuated at low work loads, it may not be maximally activated at exhaustion.

2,3-Diphosphoglycerate↗
PubMed1989

Effect of beta-adrenoceptor blockade on renin-aldosterone and alpha-ANF during exercise at altitude.

The renin-aldosterone system may be depressed in subjects exercising at high altitude, thereby preventing excessive angiotensin I (ANG I) and aldosterone levels, which could favor the onset of acute mountain sickness. The role of beta-adrenoceptors in hormonal responses to hypoxia was investigated in 12 subjects treated with a nonselective beta-blocker, pindolol. The subjects performed a standardized maximal bicycle ergometer exercise with (P) and without (C) acute pindolol treatment (15 mg/day) at sea level, as well as during a 5-day period at high altitude (4,350 m, barometric pressure 450 mmHg). During sea-level exercise, pindolol caused a reduction in plasma renin activity (PRA, 2.83 +/- 0.35 vs. 5.13 +/- 0.7 ng ANG I.ml-1.h-1, P less than 0.01), an increase in plasma alpha-atrial natriuretic factor (alpha-ANF) level (23.1 +/- 2.9 (P) vs. 10.4 +/- 1.5 (C) pmol/1, P less than 0.01), and no change in plasma aldosterone concentration [0.50 +/- 0.04 (P) vs. 0.53 +/- 0.03 (C) nmol/1]. Compared with sea-level values, PRA (3.45 +/- 0.7 ng ANG I.ml-1.h-1) and PA (0.39 +/- 0.03 nmol/1) were significantly lower (P less than 0.05) during exercise at high altitude. alpha-ANF was not affected by hypoxia. When beta-blockade was achieved at high altitude, exercise-induced elevation in PRA was completely abolished, but no additional decline in PA occurred. Plasma norepinephrine and epinephrine concentrations tended to be lower during maximal exercise at altitude; however, these differences were not statistically significant. Our results provide further evidence that hypoxia has a suppressive effect on the renin-aldosterone system. However, beta-adrenergic mechanisms do not appear to be responsible for inhibition of renin secretion at high altitude.

Adult↗
PubMed1994

Albuminuria and overall capillary permeability of albumin in acute altitude hypoxia.

The mechanism of proteinuria at high altitude is unclear. Renal function and urinary excretion rate of albumin (Ualb) at rest and during submaximal exercise and transcapillary escape rate of 125I-labeled albumin (TERalb) were investigated in 12 normal volunteers at sea level and after rapid and passive ascent to 4,350 m. The calcium antagonist isradipine (5 mg/day; n = 6) or placebo (n = 6) was administered to abolish hypoxia-induced rises in blood pressure. Lithium clearance and urinary excretion of beta 2-microglobulin were used to evaluate renal tubular function. High altitude increased Ualb from 2.8 to > 5.0 micrograms/min in both groups (P < 0.05). In the placebo group, high altitude significantly increased filtration fraction (P < 0.05), but this response was abolished by isradipine. Lithium clearance and urinary excretion of beta 2-microglobulin remained unchanged by hypoxia in both groups. Exercise did not reveal any further renal dysfunction. In both groups, high altitude increased TERalb from 4.8 to > 6.7%/h (P < 0.05). In conclusion, acute altitude hypoxia increases Ualb despite unchanged tubular function and independent of effects of isradipine on filtration fraction. The elevated TERalb suggests an overall increase in capillary permeability, including the glomerular endothelium, as the critical factor in high-altitude induced albuminuria.

Adult↗
PubMed1996

Altitude and beta-blockade augment glucose utilization during submaximal exercise.

To test the hypothesis that altitude exposure increases glucose utilization and that this increment is mediated by a beta-adrenergic mechanism, the effects of hypobaric hypoxia and beta-blockade on glucose rates of appearance (Ra), disappearance (Rd), oxidation (Rox), and leg uptake [G = 2(arteriovenous glucose difference)(1 - leg blood flow)] were measured during rest and a given submaximal exercise task. We studied six healthy beta-blocked (beta) men [26.7 +/- 1.2 (SE) yr, 74.0 +/- 6.6 kg] and five matched controls (C; 26 +/- 1.2 yr, 69.3 +/- 2.6 kg) in energy and nitrogen balance during rest and leg cycle-ergometer exercise at sea level, on acute altitude exposure to 4,300 m (barometric pressure = 463 Torr), and after 3 wk of habituation. Subjects received a primed continuous infusion of [6,6-2H]- and [1-13C]glucose, rested for > or = 90 min, and then immediately exercised for 45 min at 89 W, which elicited 49% of sea-level peak O2 consumption (VO2peak; 65% of altitude VO2peak). At sea level, resting Ra was 1.47 +/- 0.19 and 1.66 +/- 0.16 mg x kg-1 x min-1 for C and beta, respectively, and increased to 3.04 +/- 0.25 and 3.56 +/- 0.27 mg x kg-1 x min-1, respectively, during exercise. Thus glucose Ra was significantly increased by beta-blockade during rest and exercise at sea level. At sea level, beta-blockade increased leg G, which accounted for 49 and 69% of glucose disposal during exercise in C and beta, respectively. On acute altitude exposure, glucose Ra rose significantly during rest and exercise relative to sea level, whereas blockade continued to augment this increment. During exercise on acute exposure, G increased more than at sea level and accounted for a greater percentage (80 and 97%, respectively) of Rd in C and beta during exercise. Similarly, Rox values, particularly during exercise, were increased significantly at altitude relative to sea level, and beta-blockade potentiated this effect. During a given submaximal exercise task after acclimatization, glucose Ra, Rox, and G were increased relative to sea level, but these increments were less than those in response to exercise measured on acute exposure. We conclude that altitude exposure increases glucose use during rest and a given submaximal exercise bout and beta-blockade exaggerates the response.

Adrenergic beta-Antagonists↗