Pulmonary gas exchange, diffusing capacity in natives and newcomers at high altitude.
At high altitude, in resting conditions, no differences have been observed between High Altitude Natives (HAN) and acclimatized Sea Level Natives (SLN) in AaDO2, aADCO2 or venous admixture. In acclimatized SLN, AaDO2 is smaller than at sea level because of: (1) The minor effect on arterial oxygenation of the probably constant venous admixture. (2) The reduction of VA/Q inequality as shown by a smaller aADCO2. In HAN, DLCO is greater than in SLN; the contribution of DM or VC in this difference remains unsettled, mainly because of the difficulties of measurement of DM and VC in HAN suddenly exposed to acute hyperoxia. In SLN, in acute hypoxia, DLCO increased transitorily. Asynchronous mechanisms of adaptation to high altitude are evoked.
D000064:Acclimatization; D000328:Adult; D000531:Altitude; D002245:Carbon Dioxide / Q000097:blood; D002248:Carbon Monoxide / Q000097:blood*; D006801:Humans; D006863:Hydrogen-Ion Concentration; D008433:Mathematics; D010100:Oxygen / Q000097:blood*; D011650:Pulmonary Alveoli / Q000502:physiology; D011653:Pulmonary Diffusing Capacity; D012119:Respiration
D002245:Carbon Dioxide; D002248:Carbon Monoxide; D010100:Oxygen