1983
DOI: 10.1152/jappl.1983.55.3.678
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Pulmonary gas exchange on the summit of Mount Everest

Abstract: Pulmonary gas exchange was studied on members of the American Medical Research Expedition to Everest at altitudes of 8,050 m (barometric pressure 284 Torr), 8,400 m (267 Torr) and 8,848 m (summit of Mt. Everest, 253 Torr). Thirty-four valid alveolar gas samples were taken using a special automatic sampler including 4 samples on the summit. Venous blood was collected from two subjects at an altitude of 8,050 m on the morning after their successful summit climb. Alveolar CO2 partial pressure (PCO2) fell approxim… Show more

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Cited by 183 publications
(72 citation statements)
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“…Results were reproducible and agreed with those of a previous field study (AMREE) [4]. In particular, we also found that PA,O 2 did not decline further from Camp 3 at 7,467 m to the South Col at 8,000 m.…”
Section: Discussionsupporting
confidence: 91%
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“…Results were reproducible and agreed with those of a previous field study (AMREE) [4]. In particular, we also found that PA,O 2 did not decline further from Camp 3 at 7,467 m to the South Col at 8,000 m.…”
Section: Discussionsupporting
confidence: 91%
“…Mean data are presented in figure 4. Once again, Operation Everest II data [5] are presented alongside, as well as available data from the AMREE [4]. Mean (±SEM) values for PA,O 2 declined from 8.5±0.2 kPa (64±1.6 mmHg) on Lamjura Pass to 5.1±0.08 kPa (38±0.6 mmHg) at 7,467 m at Camp 3, but there was no further decline at 8,000 m (PA,O 2 5.1±0.2 kPa (38±1.2 mmHg)).…”
Section: Alveolar (End-expiratory) Partial Pressure Of Oxygenmentioning
confidence: 99%
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“…Barometric pressure at sea level is ;760 mmHg (containing 20.9% oxygen) corresponding to a PiO 2 of 160 mmHg (2). At 8,848 m, the altitude at the summit of Mount Everest, the barometric pressure is ;253 mmHg and the PiO 2 is ;42 mmHg, which results in almost immediate unconsciousness in unacclimatized subjects (3).…”
Section: Altitudementioning
confidence: 99%
“…The low PA,O 2 limits the alveolar-arterial driving gradient for oxygen uptake and, in combination with a lower mixed venous oxygen tension, also delays alveolar-capillary equilibration [13]. These issues are of greater concern during exercise when the smaller pressure differential across the alveolar-capillary barrier, in conjunction with the increased cardiac output, shortened capillary transit time and greater venous oxygen desaturation, create an effective diffusion limitation for oxygen that leads to further arterial desaturation [9,10,14].…”
Section: Gas Exchange and Oxygen Deliverymentioning
confidence: 99%