• Y Matsuzawa and T Kobayashi.
• First Department of Internal Medicine, Shinshu University School of Medicine, Matsumoto, Japan.
• Nihon Kyobu Shikkan Gakkai Zasshi. 1992 Dec 1; 30 Suppl: 139-46.

AbstractTo investigate the role of hypoxic ventilatory response (HVR) in the pathogenesis of acute mountain sickness (AMS) and high-altitude pulmonary edema (HAPE), we performed two studies. In the first study, nine healthy male lowlanders were exposed to a simulated altitude of 3,700 m (485 Torr) for 24 h in a hypobaric chamber. Subjects (n = 4) with lower alveolar ventilation on arrival at 3,700 m subsequently developed more severe AMS 24 h after the exposure. The relative hypoventilation was related to the lower HVR measured at low altitude, suggesting a possible role of low HVR in AMS. In the second study nine lowlanders with a previous history of HAPE (HAPE-S) and six control subjects were exposed to a simulated altitude of 3,200 m (515 Torr). At low altitude, HVR (delta VE/delta SaO2) in HAPE-S was significantly lower than that of controls (-0.40 +/- 0.20 vs. -0.85 +/- 0.21 L/min/%, p < 0.01). At high altitude HAPE-S showed lower PaO2, higher PaCO2 and lower PAO2, compared with controls, i.e., relative hypoventilation. In one of the HAPE-S, who showed the lowest PaO2 at the simulated altitude, oxygen breathing resulted in a paradoxical increase in ventilation, suggesting hypoxic ventilatory depression. These two studies suggest that low HVR may a contributing rather than a critical factor in the pathogenesis of AMS and HAPE.

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