| Literature DB >> 30756526 |
Takeshi Ogawa1, Naoto Fujii2, Yasuhiro Kurimoto2, Takeshi Nishiyasu2.
Abstract
During exposure to high altitude, hypoxia develops because of reductions in barometric pressure and partial pressure of O2 . Although several studies have examined the effects of hypoxia on exercise performance and physiological responses, such as maximal minute ventilation ( V · Emax ) and maximal oxygen uptake ( V · O2max ), how barometric pressure reduction (hypobaria) modulates them remains largely unknown. In this study, 11 young men performed incremental treadmill running tests to exhaustion under three conditions chosen at random: normobaric normoxia (NN; 763 ± 5 mmHg of barometric pressure, equivalent to sea level), hypobaric hypoxia (HH; 492 ± 1 mmHg of barometric pressure, equivalent to 3500 m above sea level (m a.s.l.)), and hypobaric normoxia (HN; 492 ± 1 mmHg of barometric pressure while breathing 32.2 ± 0.1% O2 to match the inspiratory O2 content under NN). V · Emax was higher in HN than in NN (160.9 ± 10.7 vs. 150.7 ± 10.0 L min-1 , P < 0.05). However, no differences in V · O2max and arterial oxyhemoglobin saturation were observed between NN and HN (all P > 0.05). Time to exhaustion was longer in HN than in NN (932 ± 83 vs. 910 ± 79 s, P < 0.05). These results suggest that reduced air density during exposure to an altitude of 3500 m a.s.l. increases maximal ventilation and extends time to exhaustion without affecting oxygen consumption or arterial oxygen saturation.Entities:
Keywords:
zzm321990
Year: 2019 PMID: 30756526 PMCID: PMC6372535 DOI: 10.14814/phy2.14002
Source DB: PubMed Journal: Physiol Rep ISSN: 2051-817X
Variables measured at O2max
| NN | HH | HN | |
|---|---|---|---|
|
| 3974 ± 338 | 2860 ± 241 | 4011 ± 327 |
|
| 63.0 ± 4.7 | 46.0 ± 5.6 | 63.6 ± 5.6 |
|
| 4580 ± 282 | 3506 ± 215 | 4531 ± 327 |
|
| 150.7 ± 10.0 | 154.2 ± 11.8 | 160.9 ± 10.6 |
|
| 68 ± 10 | 70 ± 10 | 73 ± 10 |
| VT [L] | 2.2 ± 1.03 | 2.25 ± 0.36 | 2.25 ± 0.3 |
|
| 38.1 ± 3.6 | 54.3 ± 6.6 | 40.4 ± 4.9 |
|
| 33.0 ± 3.1 | 44.0 ± 3.1 | 35.6 ± 3.5 |
|
| 101.8 ± 6.6 | 95.3 ± 10.0 | 106.8 ± 8.6 |
| PETCO2 [mmHg] | 39.2 ± 3.3 | 31.6 ± 3.9 | 36.8 ± 3.5 |
| PAO2 [mmHg] | 128.5 ± 10.6 | 76.9 ± 3.5 | 126.2 ± 4.2 |
| SaO2 [%] | 91 ± 3 | 69 ± 4 | 90 ± 5 |
| HRmax [beats min−1] | 195 ± 3 | 181 ± 8 | 192 ± 8 |
| Time to exhaustion [s] | 910 ± 79 | 614 ± 73 | 932 ± 83 |
Values are mean ± standard deviation (n = 11).
NN: normobaric normoxia; HH: hypobaric hypoxia; HN: hypobaric normoxia; O2max: maximal oxygen uptake; CO2max: maximal carbon dioxide output; f R: respiratory frequency; VT: tidal volume; VA: alveolar ventilation; PETCO2: end tidal CO2 pressure; PAO2: partial pressure of alveolar O2; SaO2: arterial oxyhemoglobin saturation; HRmax: maximal heart rate.
P < 0.05 versus NN.
P < 0.05 versus HH.
Variables analyzed during the last 30 s of voluntary hyperventilation at rest
| NN | HN | % change | |
|---|---|---|---|
|
| 147.9 ± 11.9 | 158.1 ± 12.7 | 6.9 |
|
| 68 ± 10 | 73 ± 11 | 7.4 |
| VT [L] | 2.23 ± 0.28 | 2.24 ± 0.3 | −0.2 |
|
| 12.19 ± 2.11 | 10.15 ± 1.66 | −15.5 |
|
| 4.46 ± 0.84 | 4.48 ± 1.02 | 1.11 |
|
| 7.73 ± 2.04 | 5.67 ± 1.80 | −23.1 |
| % | 12.4 ± 3.6 | 9.1 ± 3.4 | −23.4 |
| SaO2 [%] | 100 ± 0 | 100 ± 0 | 0 |
| PImax [cmH2O] | 8.98 ± 2.80 | 6.20 ± 2.00 | −27.6 |
| PEmax [cmH2O] | −9.15 ± 2.11 | −6.87 ± 1.59 | −23.2 |
Values are mean ± standard deviation (n = 10).
NN: normobaric normoxia; HN: hypobaric normoxia; E: minute ventilation; f R: respiratory frequency; VT: tidal volume; O2mimc: oxygen uptake during mimic ventilation; O2rest: oxygen uptake at rest; O2vent: calculated O2 at respiratory muscles; %O2max: percentage occupation of O2vent to O2max; PI max: peak inspiratory mouth pressure; PE max: peak expiratory mouth pressure.
P < 0.05 versus NN.
Figure 1Estimated oxygen consumption at O2max. Grey area shows O2 at rest, the black area shows the O2 of the respiratory muscles, and the white area shows other tissues. NN, normobaric normoxia; HN, hypobaric normoxia. *P < 0.05 versus NN.