| Autor: |
Petrassi FA; Department of Kinesiology, Recreation, and Sport, Indiana State University, Terre Haute, Indiana., Davis JT; Department of Kinesiology, Recreation, and Sport, Indiana State University, Terre Haute, Indiana., Beasley KM; Department of Kinesiology, Recreation, and Sport, Indiana State University, Terre Haute, Indiana., Evero O; Altitude Research Center, Division of Pulmonary and Critical Care Medicine, Department of Medicine, University of Colorado Anschutz Medical Campus , Denver, Colorado., Elliott JE; Department of Kinesiology, Recreation, and Sport, Indiana State University, Terre Haute, Indiana., Goodman RD; Oregon Heart and Vascular Institute, Echocardiography, Springfield, Oregon., Futral JE; Oregon Heart and Vascular Institute, Echocardiography, Springfield, Oregon., Subudhi A; Altitude Research Center, Division of Pulmonary and Critical Care Medicine, Department of Medicine, University of Colorado Anschutz Medical Campus , Denver, Colorado., Solano-Altamirano JM; Faculty of Chemical Sciences, Meritorious Autonomous University of Puebla , Puebla, Mexico., Goldman S; Department of Chemistry, University of Guelph , Guelph, Ontario , Canada., Roach RC; Altitude Research Center, Division of Pulmonary and Critical Care Medicine, Department of Medicine, University of Colorado Anschutz Medical Campus , Denver, Colorado., Lovering AT; Department of Kinesiology, Recreation, and Sport, Indiana State University, Terre Haute, Indiana. |
| Abstrakt: |
Blood flow through intrapulmonary arteriovenous anastomoses (Q IPAVA ) occurs in healthy humans at rest and during exercise when breathing hypoxic gas mixtures at sea level and may be a source of right-to-left shunt. However, at high altitudes, Q IPAVA is reduced compared with sea level, as detected using transthoracic saline contrast echocardiography (TTSCE). It remains unknown whether the reduction in Q IPAVA (i.e., lower bubble scores) at high altitude is due to a reduction in bubble stability resulting from the lower barometric pressure (P B ) or represents an actual reduction in Q IPAVA . To this end, Q IPAVA , pulmonary artery systolic pressure (PASP), cardiac output (Q T ), and the alveolar-to-arterial oxygen difference (AaDO 2 ) were assessed at rest and during exercise (70-190 W) in the field (5,260 m) and in the laboratory (1,668 m) during four conditions: normobaric normoxia (NN; [Formula: see text] = 121 mmHg, P B = 625 mmHg; n = 8), normobaric hypoxia (NH; [Formula: see text] = 76 mmHg, P B = 625 mmHg; n = 7), hypobaric normoxia (HN; [Formula: see text] = 121 mmHg, P B = 410 mmHg; n = 8), and hypobaric hypoxia (HH; [Formula: see text] = 75 mmHg, P B = 410 mmHg; n = 7). We hypothesized Q IPAVA would be reduced during exercise in isooxic hypobaria compared with normobaria and that the AaDO 2 would be reduced in isooxic hypobaria compared with normobaria. Bubble scores were greater in normobaric conditions, but the AaDO 2 was similar in both isooxic hypobaria and normobaria. Total pulmonary resistance (PASP/Q T ) was elevated in HN and HH. Using mathematical modeling, we found no effect of hypobaria on bubble dissolution time within the pulmonary transit times under consideration (<5 s). Consequently, our data suggest an effect of hypobaria alone on pulmonary blood flow. NEW & NOTEWORTHY Blood flow through intrapulmonary arteriovenous anastomoses, detected by transthoracic saline contrast echocardiography, was reduced during exercise in acute hypobaria compared with normobaria, independent of oxygen tension, whereas pulmonary gas exchange efficiency was unaffected. Modeling the effect(s) of reduced air density on contrast bubble lifetime did not result in a significantly reduced contrast stability. Interestingly, total pulmonary resistance was increased by hypobaria, independent of oxygen tension, suggesting that pulmonary blood flow may be changed by hypobaria. |
