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University Laboratory of Physiology, University of Oxford, Oxford, United Kingdom
Submitted 10 September 2004 ; accepted in final form 8 December 2004
Ventilatory acclimatization to hypoxia (VAH) consists of a progressive increase in ventilation and decrease in end-tidal PCO2 (PETCO2). Underlying VAH, there are also increases in the acute ventilatory sensitivities to hypoxia and hypercapnia. To investigate whether these changes could be induced with very mild alterations in end-tidal PO2 (PETO2), two 5-day exposures were compared: 1) mild hypoxia, with PETO2 held at 10 Torr below the subject's normal value; and 2) mild hyperoxia, with PETO2 held at 10 Torr above the subject's normal value. During both exposures, PETCO2 was uncontrolled. For each exposure, the entire protocol required measurements on 13 consecutive mornings: 3 mornings before the hypoxic or hyperoxic exposure, 5 mornings during the exposure, and 5 mornings postexposure. After the subjects breathed room air for at least 30 min, measurements were made of PETCO2, PETO2, and the acute ventilatory sensitivities to hypoxia and hypercapnia. Ten subjects completed both protocols. There was a significant increase in the acute ventilatory sensitivity to hypoxia (Gp) after exposure to mild hypoxia, and a significant decrease in Gp after exposure to mild hyperoxia (P < 0.05, repeated-measures ANOVA). No other variables were affected by mild hypoxia or hyperoxia. The results, when combined with those from other studies, suggest that Gp varies linearly with PETO2, with a sensitivity of 3.5%/Torr (SE 1.0). This sensitivity is sufficient to suggest that Gp is continuously varying in response to normal physiological fluctuations in PETO2. We conclude that at least some of the mechanisms underlying VAH may have a physiological role at sea level.
acclimatization to hypoxia; respiratory control; chemoreflexes; acute ventilatory response to hypoxia
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