Effects of acute exposure to high altitude on ventilatory drive and respiratory pattern

To assess changes in ventilatory regulation in terms of central drive and timing, on exposure to high altitude, and the effects of induced hyperoxia at high altitude, six healthy normal lowland subjects (mean age 19.5 +/- 1.64 yr) were studied at low altitude (518 m) and on the first 4 days at high altitude (3,940 m). The progressive increase in resting expired minute ventilation (VE; control mean 9.94 +/- 1.78 to 14.25 +/- 2.67 l/min on day 3, P less than 0.005) on exposure to high altitude was primarily due to a significant increase in respiratory frequency (f; control mean 15.6 +/- 3.5 breaths/min to 23.8 +/- 6.2 breaths/min on day 3, P less than 0.01) with no significant change in tidal volume (VT). The increase in f was due to significant decreases in both inspiratory (TI) and expiratory (TE) time per breath; the ratio of TI to TE increased significantly (control mean 0.40 +/- 0.08 to 0.57 +/- 0.14, P less than 0.025). Mouth occlusion pressure did not change significantly, nor did the ratio of VE to mouth occlusion pressure. The acute induction of hyperoxia for 10 min at high altitude did not significantly alter VE or the ventilatory pattern. These results indicate that acute exposure to high altitude in normal lowlanders causes an increase in VE primarily by an alteration in central breath timing, with no change in respiratory drive. The acute relief of high altitude hypoxia for 10 min has no effect on the increased VE or ventilatory pattern.     

Ventilation and hypoxic ventilatory response of Tibetan and Aymara high altitude natives

Newcomers acclimatizing to high altitude and adult male Tibetan high altitude natives have increased ventilation relative to sea level natives at sea level. However, Andean and Rocky Mountain high altitude natives have an intermediate level of ventilation lower than that of newcomers and Tibetan high altitude natives although generally higher than that of sea level natives at sea level. Because the reason for the relative hypoventilation of some high altitude native populations was unknown, a study was designed to describe ventilation from adolescence through old age in samples of Tibetan and Andean high altitude natives and to estimate the relative genetic and environmental influences. This paper compares resting ventilation and hypoxic ventilatory response (HVR) of 320 Tibetans 9–82 years of age and 542 Bolivian Aymara 13–94 years of age, native residents at 3,800–4,065 m. Tibetan resting ventilation was roughly 1.5 times higher and Tibetan HVR was roughly double that of Aymara. Greater duration of hypoxia (older age) was not an important source of variation in resting ventilation or HVR in either sample. That is, contrary to previous studies, neither sample acquired hypoventilation in the age ranges under study. Within populations, greater severity of hypoxia (lower percent of oxygen saturation of arterial hemoglobin) was associated with slightly higher resting ventilation among Tibetans and lower resting ventilation and HVR among Aymara women, although the associations accounted for just 2–7% of the variation. Between populations, the Tibetan sample was more hypoxic and had higher resting ventilation and HVR. Other systematic environmental contrasts did not appear to elevate Tibetan or depress Aymara ventilation. There was more intrapopulation genetic variation in these traits in the Tibetan than the Aymara sample. Thirty-five percent of the Tibetan, but none of the Aymara, resting ventilation variance was due to genetic differences among individuals. Thirty-one percent of the Tibetan HVR, but just 21% of the Aymara, HVR variance was due to genetic differences among individuals. Thus there is greater potential for evolutionary change in these traits in the Tibetans. Presently, there are two different ventilation phenotypes among high altitude natives as compared with sea level populations at sea level: lifelong sustained high resting ventilation and a moderate HVR among Tibetans in contrast with a slightly elevated resting ventilation and a low HVR among Aymara. Am J Phys Anthropol 104:427–447, 1997. © 1997 Wiley-Liss, Inc.     

Low acute hypoxic ventilatory response and hypoxic depression in acute altitude sickness

Persons with acute altitude sickness hypoventilate at high altitude compared with persons without symptoms. We hypothesized that their hypoventilation was due to low initial hypoxic ventilatory responsiveness, combined with subsequent blunting of ventilation by hypocapnia and/or prolonged hypoxia. To test this hypothesis, we compared eight subjects with histories of acute altitude sickness with four subjects who had been asymptomatic during prior altitude exposure. At a simulated altitude of 4,800 m, the eight susceptible subjects developed symptoms of altitude sickness and had lower minute ventilations and higher end-tidal PCO2's than the four asymptomatic subjects. In measurements made prior to altitude exposure, ventilatory responsiveness to acute hypoxia was reduced in symptomatic compared to asymptomatic subjects, both when measured under isocapnic and poikolocapnic (no added CO2) conditions. Diminution of the poikilocapnic relative to the isocapnic hypoxic response was similar in the two groups. Ventilation fell, and end-tidal PCO2 rose in both groups during 30 min of steady-state hypoxia relative to values observed acutely. After 4.5 h at 4,800 m, ventilation was lower than values observed acutely at the same arterial O2 saturation. The reduction in ventilation in relation to the hypoxemia present was greater in symptomatic than in asymptomatic persons. Thus the hypoventilation in symptomatic compared to asymptomatic subjects was attributable both to a lower acute hypoxic response and a subsequent greater blunting of ventilation at high altitude.     

Blunted hypoxic ventilatory drive in subjects susceptible to high-altitude pulmonary edema

It has been proposed that subjects susceptible to high-altitude pulmonary edema (HAPE) show exaggerated hypoxemia with relative hypoventilation during the early period of high-altitude exposure. Some previous studies suggest the relationship between the blunted hypoxic ventilatory response (HVR) and HAPE. To examine whether all the HAPE-susceptible subjects consistently show blunted HVR at low altitude, we evaluated the conventional pulmonary function test, hypoxic ventilatory response (HVR), and hypercapnic ventilatory response (HCVR) in ten lowlanders who had a previous history of HAPE and compared these results with those of eight control lowlanders who had no history of HAPE. HVR was measured by the progressive isocapnic hypoxic method and was evaluated by the slope relating minute ventilation to arterial O2 saturation (delta VE/delta SaO2). HCVR was measured by the rebreathing method of Read. All measurements were done at Matsumoto, Japan (610 m). All the HAPE-susceptible subjects showed normal values in the pulmonary function test. In HCVR, HAPE-susceptible subjects showed relatively lower S value, but there was no significant difference between the two groups (1.74 +/- 1.16 vs. 2.19 +/- 0.4, P = NS). On the other hand, HAPE-susceptible subjects showed significantly lower HVR than control subjects (-0.42 +/- 0.23 vs. -0.87 +/- 0.29, P less than 0.01). These results suggest that HAPE-susceptible subjects more frequently show low HVR at low altitude. However, values for HVR were within the normal range in 2 of 10 HAPE-susceptible subjects. It would seem therefore that low HVR alone need not be a critical factor for HAPE. This could be one of several contributing factors.     

Augmented hypoxic ventilatory response in men at altitude.

To test the hypothesis that the hypoxic ventilatory response (HVR) of an individual is a constant unaffected by acclimatization, isocapnic 5-min step HVR, as delta VI/delta SaO2 (l.min-1.%-1, where VI is inspired ventilation and SaO2 is arterial O2 saturation), was tested in six normal males at sea level (SL), after 1-5 days at 3,810-m altitude (AL1-3), and three times over 1 wk after altitude exposure (PAL1-3). Equal medullary central ventilatory drive was sought at both altitudes by testing HVR after greater than 15 min of hyperoxia to eliminate possible ambient hypoxic ventilatory depression (HVD), choosing for isocapnia a P'CO2 (end tidal) elevated sufficiently to drive hyperoxic VI to 140 ml.kg-1.min-1. Mean P'CO2 was 45.4 +/- 1.7 Torr at SL and 33.3 +/- 1.8 Torr on AL3, compared with the respective resting control end-tidal PCO2 of 42.3 +/- 2.0 and 30.8 +/- 2.6 Torr. SL HVR of 0.91 +/- 0.38 was unchanged on AL1 (30 +/- 18 h) at 1.04 +/- 0.37 but rose (P less than 0.05) to 1.27 +/- 0.57 on AL2 (3.2 +/- 0.8 days) and 1.46 +/- 0.59 on AL3 (4.8 +/- 0.4 days) and remained high on PAL1 at 1.44 +/- 0.54 and PAL2 at 1.37 +/- 0.78 but not on PAL3 (days 4-7). HVR was independent of test SaO2 (range 60-90%). Hyperoxic HCVR (CO2 response) was increased on AL3 and PAL1. Arterial pH at congruent to 65% SaO2 was 7.378 +/- 0.019 at SL, 7.44 +/- 0.018 on AL2, and 7.412 +/- 0.023 on AL3.(ABSTRACT TRUNCATED AT 250 WORDS)     

Brain tissue pH and ventilatory acclimatization to high altitude.

31P nuclear magnetic resonance spectroscopy (31P-NMRS) was performed on brain cross sections of four human subjects before and after 7 days in a hypobaric chamber at 447 Torr to test the hypothesis that brain intracellular acidosis develops during acclimatization to high altitude and accounts for the progressively increasing ventilation that develops (ventilatory acclimatization). Arterial blood gas measurements confirmed increased ventilation. At the end of 1 wk of hypobaria, brain intracellular pH was 7.023 +/- 0.046 (SD), unchanged from preexposure pH of 6.998 +/- 0.029. After return to sea level, however, it decreased to 6.918 +/- 0.032 at 15 min (P less than 0.01) and 6.920 +/- 0.046 at 12 h (P less than 0.01). The ventilatory response to hypoxia increased [from 0.35 +/- 0.11 (l/min)/(-%O2 saturation) before exposure to 0.69 +/- 0.19 after, P = 0.06]. Brain intracellular acidosis is probably not a supplemental stimulus to ventilatory acclimatization to high altitude. However, brain intracellular acidosis develops on return to normoxia from chronic hypoxia, suggesting that brain pH may follow changes in blood and cerebrospinal fluid pH as they are altered by changes in ventilation.     

Low P50 in deer mice native to high altitude

Whereas it is widely believed that animals native to high altitude show lower O2 partial pressures at 50% hemoglobin saturation (P50) than do related animals native to low altitude, that "fact" has not been well documented. Consequently, P50 at pH 7.4, PCO2(7.4), the CO2 Bohr effect, and the buffer slope (delta log PCO2/delta pH) were determined via the mixing technique in Peromyscus maniculatus native to a range of altitudes but acclimated to 340 or 3,800 m. PCO2(7.4) and buffer slope were substantially lower at high altitude. The change in P50(7.4) between acclimation altitudes was minimal (0.8% increase at 3,800 m), because of counterbalancing changes in PCO2, 2,3-diphospho-D-glycerate concentration, and perhaps other factors. At both acclimation altitudes there was a highly significant negative correlation between P50(7.4) and native altitude. Since pH in vivo probably increases slightly at high altitude, the data on P50 corrected to pH 7.4 are probably underestimates of the difference in in vivo P50 at low vs. high altitude. Hence these results corroborate theoretical predictions that low P50 is advantageous under severe hypoxic stress.     

Activity and oxygen consumption during hypoxic exposure in high altitude and lowland sceloporine lizards

Summary Resting rates of O₂ consumption against , exercise endurance times and during recovery from vigorous exercise were measured inSceloporus occidentalis captured near sea level and inS. graciosus captured above 2850 m. Oxygen consumption against was also measured inS. occidentalis captured above 2850 m. When was recorded continuously, as ambient was slowly reduced from 155 Torr, it became directly dependent upon ambient between 110 and 120 Torr. The critical for the high altitude lizards was lower than that for the lowland lizards, which enabled the former to maintain relatively higher 's when ambient was reduced below 120 Torr. The high altitude lizards also had significantly greater endurance when stimulated to exercise at 1600 m ( 130 Torr). Both the higher under hypoxia and the greater endurance roughly parallel a significantly greater maximum in the high altitude lizards. At a simulated altitude of 3600 m ( 100 Torr), maximum and rate of recovery of the O₂ debt calculated from post active were significantly reduced in the lowland but not the high altitude lizards. The effects of simulated altitude conditions on the lowland but not the mountaine animals indicate adaptations to altitude in these sceloporine lizards. We did not find any consistent relationship between organ/body weight ratios or hematocrit and our measures of endurance or the altitude at which the lizards were captured.     

Role of adenosine in hypoxic ventilatory depression

The role of adenosine in the ventilatory depression induced by hypoxia was studied in 82 spontaneously breathing urethan-anesthetized 4-day-old rabbit pups. Respiration was monitored with a pneumotachograph. The animals were exposed to hypoxia (6% O2 in N2) for 30 min or until the occurrence of terminal apnea. In all animals hypoxia produced an initial increase in ventilation followed by a decrease. In the control group 52% of the animals became apneic after 7 min of hypoxic exposure. By contrast, pretreatment with dipyridamole (10 or 20 mg/kg), an adenosine uptake blocker, significantly shortened the time needed to reach apnea. Thus at 7 min of hypoxia 93% of the animals that received dipyridamole became apneic. On the other hand, administration of adenosine antagonists 8-p-sulfophenyltheophylline (5 or 8 mg/kg) and aminophylline (10 or 25 mg/kg) significantly prolonged the time required to produce apnea. Only 20% of the animals that received these antagonists became apneic at 7 min of hypoxia. These results suggest that adenosine is potentially involved in the ventilatory depression produced by hypoxia in neonatal rabbit pups.