Pulmonary gas exchange in humans during exercise at sea level

1986 ◽  
Vol 60 (5) ◽  
pp. 1590-1598 ◽  
Author(s):  
M. D. Hammond ◽  
G. E. Gale ◽  
K. S. Kapitan ◽  
A. Ries ◽  
P. D. Wagner
Keyword(s):  
Gas Exchange ◽  
Sea Level ◽  
Minute Ventilation ◽  
Normal Subjects ◽  
Inert Gas ◽  
Diffusion Limitation ◽  
O2 Uptake ◽  
Heavy Exercise ◽  
Blood Temperature ◽  
O2 Diffusion

Previous studies have shown both worsening ventilation-perfusion (VA/Q) relationships and the development of diffusion limitation during exercise at simulated altitude and suggested that similar changes could occur even at sea level. We used the multiple-inert gas-elimination technique to further study gas exchange during exercise in healthy subjects at sea level. Mixed expired and arterial respiratory and inert gas tensions, cardiac output, heart rate, minute ventilation, respiratory rate, and blood temperature were recorded at rest and during steady-state exercise in the following order: rest, minimal exercise (75 W), heavy exercise (300 W), heavy exercise breathing 100% O2, repeat rest, moderate exercise (225 W), and light exercise (150 W). Alveolar-to-arterial O2 tension difference increased linearly with O2 uptake (VO2) (6.1 Torr X min-1 X 1(-1) VO2). This could be fully explained by measured VA/Q inequality at mean VO2 less than 2.5 l X min-1. At higher VO2, the increase in alveolar-to-arterial O2 tension difference could not be explained by VA/Q inequality alone, suggesting the development of diffusion limitation. VA/Q inequality increased significantly during exercise (mean log SD of perfusion increased from 0.28 +/- 0.13 at rest to 0.58 +/- 0.30 at VO2 = 4.0 l X min-1, P less than 0.01). This increase was not reversed by 100% O2 breathing and appeared to persist at least transiently following exercise. These results confirm and extend the earlier suggestions (8, 21) of increasing VA/Q inequality and O2 diffusion limitation during heavy exercise at sea level in normal subjects and demonstrate that these changes are independent of the order of performance of exercise.

Pulmonary gas exchange in humans during normobaric hypoxic exercise

1986 ◽  
Vol 61 (5) ◽  
pp. 1749-1757 ◽  
Author(s):  
M. D. Hammond ◽  
G. E. Gale ◽  
K. S. Kapitan ◽  
A. Ries ◽  
P. D. Wagner
Keyword(s):  
Gas Exchange ◽  
Minute Ventilation ◽  
Barometric Pressure ◽  
Normal Subjects ◽  
Inert Gas ◽  
Diffusion Limitation ◽  
Heavy Exercise ◽  
Blood Temperature ◽  
O2 Partial Pressure ◽  
Hypoxic Exercise

Previous studies (J. Appl. Physiol. 58: 978–988 and 989–995, 1985) have shown both worsening ventilation-perfusion (VA/Q) relationships and the development of diffusion limitation during heavy exercise at sea level and during hypobaric hypoxia in a chamber [fractional inspired O2 concentration (FIO2) = 0.21, minimum barometric pressure (PB) = 429 Torr, inspired O2 partial pressure (PIO2) = 80 Torr]. We used the multiple inert gas elimination technique to compare gas exchange during exercise under normobaric hypoxia (FIO2 = 0.11, PB = 760 Torr, PIO2 = 80 Torr) with earlier hypobaric measurements. Mixed expired and arterial respiratory and inert gas tensions, cardiac output, heart rate (HR), minute ventilation, respiratory rate (RR), and blood temperature were recorded at rest and during steady-state exercise in 10 normal subjects in the following order: rest, air; rest, 11% O2; light exercise (75 W), 11% O2; intermediate exercise (150 W), 11% O2; heavy exercise (greater than 200 W), 11% O2; heavy exercise, 100% O2 and then air; and rest 20 minutes postexercise, air. VA/Q inequality increased significantly during hypoxic exercise [mean log standard deviation of perfusion (logSDQ) = 0.42 +/- 0.03 (rest) and 0.67 +/- 0.09 (at 2.3 l/min O2 consumption), P less than 0.01]. VA/Q inequality was improved by relief of hypoxia (logSDQ = 0.51 +/- 0.04 and 0.48 +/- 0.02 for 100% O2 and air breathing, respectively). Diffusion limitation for O2 was evident at all exercise levels while breathing 11% O2.(ABSTRACT TRUNCATED AT 250 WORDS)

Mechanism of exercise-induced hypoxemia in horses

1989 ◽  
Vol 66 (3) ◽  
pp. 1227-1233 ◽  
Author(s):  
P. D. Wagner ◽  
J. R. Gillespie ◽  
G. L. Landgren ◽  
M. R. Fedde ◽  
B. W. Jones ◽  
...  
Keyword(s):  
Cardiac Output ◽  
Treadmill Exercise ◽  
Inert Gas ◽  
Diffusion Limitation ◽  
O2 Uptake ◽  
Heavy Exercise ◽  
Physiological Basis ◽  
Blood Temperature ◽  
Exercise Induced ◽  
Arterial Po2

Arterial hypoxemia has been reported in horses during heavy exercise, but its mechanism has not been determined. With the use of the multiple inert gas elimination technique, we studied five horses, each on two separate occasions, to determine the physiological basis of the hypoxemia that developed during horizontal treadmill exercise at speeds of 4, 10, 12, and 13–14 m/s. Mean, blood temperature-corrected, arterial PO2 fell from 89.4 Torr at rest to 80.7 and 72.1 Torr at 12 and 13–14 m/s, respectively, whereas corresponding PaCO2 values were 40.3, 40.3, and 39.2 Torr. Alveolar-arterial PO2 differences (AaDO2) thus increased from 11.4 Torr at rest to 24.9 and 30.7 Torr at 12 and 13–14 m/s. In 8 of the 10 studies there was no change in ventilation-perfusion (VA/Q) relationships with exercise (despite bronchoscopic evidence of airway bleeding in 3) and total shunt was always less than 1% of the cardiac output. Below 10 m/s, the AaDO2 was due only to VA/Q mismatch, but at higher speeds, diffusion limitation of O2 uptake was increasingly evident, accounting for 76% of the AaDO2 at 13–14 m/s. Most of the exercise-induced hypoxemia is thus the result of diffusion limitation with a smaller contribution from VA/Q inequality and essentially none from shunting.

Pulmonary gas exchange in humans exercising at sea level and simulated altitude

1986 ◽  
Vol 61 (1) ◽  
pp. 260-270 ◽  
Author(s):  
P. D. Wagner ◽  
G. E. Gale ◽  
R. E. Moon ◽  
J. R. Torre-Bueno ◽  
B. W. Stolp ◽  
...  
Keyword(s):  
Gas Exchange ◽  
Arterial Pressure ◽  
Sea Level ◽  
Pulmonary Arterial Pressure ◽  
Minute Ventilation ◽  
Statistical Significance ◽  
Random Order ◽  
Normal Subjects ◽  
Simulated Altitude ◽  
Pulmonary Arterial

In a previous study of normal subjects exercising at sea level and simulated altitude, ventilation-perfusion (VA/Q) inequality and alveolar-end-capillary O2 diffusion limitation (DIFF) were found to increase on exercise at altitude, but at sea level the changes did not reach statistical significance. This paper reports additional measurements of VA/Q inequality and DIFF (at sea level and altitude) and also of pulmonary arterial pressure. This was to examine the hypothesis that VA/Q inequality is related to increased pulmonary arterial pressure. In a hypobaric chamber, eight normal subjects were exposed to barometric pressures of 752, 523, and 429 Torr (sea level, 10,000 ft, and 15,000 ft) in random order. At each altitude, inert and respiratory gas exchange and hemodynamic variables were studied at rest and during several levels of steady-state bicycle exercise. Multiple inert gas data from the previous and current studies were combined (after demonstrating no statistical difference between them) and showed increasing VA/Q inequality with sea level exercise (P = 0.02). Breathing 100% O2 did not reverse this increase. When O2 consumption exceeded about 2.7 1/min, evidence for DIFF at sea level was present (P = 0.01). VA/Q inequality and DIFF increased with exercise at altitude as found previously and was reversed by 100% O2 breathing. Indexes of VA/Q dispersion correlated well with mean pulmonary arterial pressure and also with minute ventilation. This study confirms the development of both VA/Q mismatch and DIFF in normal subjects during heavy exercise at sea level. However, the mechanism of increased VA/Q mismatch on exercise remains unclear due to the correlation with both ventilatory and circulatory variables and will require further study.

Diffusion limitation in normal humans during exercise at sea level and simulated altitude

1985 ◽  
Vol 58 (3) ◽  
pp. 989-995 ◽  
Author(s):  
J. R. Torre-Bueno ◽  
P. D. Wagner ◽  
H. A. Saltzman ◽  
G. E. Gale ◽  
R. E. Moon
Keyword(s):  
Sea Level ◽  
Minute Ventilation ◽  
Inert Gas ◽  
Diffusion Resistance ◽  
Diffusion Limitation ◽  
O2 Concentration ◽  
Normal Humans ◽  
Respiratory Gases ◽  
Arterial Po2 ◽  
Alveolar Capillary

The relative roles of ventilation-perfusion (VA/Q) inequality, alveolar-capillary diffusion resistance, postpulmonary shunt, and gas phase diffusion limitation in determining arterial PO2 (PaO2) were assessed in nine normal unacclimatized men at rest and during bicycle exercise at sea level and three simulated altitudes (5,000, 10,000, and 15,000 ft; barometric pressures = 632, 523, and 429 Torr). We measured mixed expired and arterial inert and respiratory gases, minute ventilation, and cardiac output. Using the multiple inert gas elimination technique, PaO2 and the arterial O2 concentration expected from VA/Q inequality alone were compared with actual values, lower measured PaO2 indicating alveolar-capillary diffusion disequilibrium for O2. At sea level, alveolar-arterial PO2 differences were approximately 10 Torr at rest, increasing to approximately 20 Torr at a metabolic consumption of O2 (VO2) of 3 l/min. There was no evidence for diffusion disequilibrium, similar results being obtained at 5,000 ft. At 10 and 15,000 ft, resting alveolar-arterial PO2 difference was less than at sea level with no diffusion disequilibrium. During exercise, alveolar-arterial PO2 difference increased considerably more than expected from VA/Q mismatch alone. For example, at VO2 of 2.5 l/min at 10,000 ft, total alveolar-arterial PO2 difference was 30 Torr and that due to VA/Q mismatch alone was 15 Torr. At 15,000 ft and VO2 of 1.5 l/min, these values were 25 and 10 Torr, respectively. Expected and actual PaO2 agreed during 100% O2 breathing at 15,000 ft, excluding postpulmonary shunt as a cause of the larger alveolar-arterial O2 difference than accountable by inert gas exchange.

Gas exchange in nonperfused dog lungs

1981 ◽  
Vol 51 (5) ◽  
pp. 1261-1267 ◽  
Author(s):  
J. W. Shepard ◽  
V. D. Minh ◽  
G. F. Dolan
Keyword(s):  
Gas Exchange ◽  
Minute Ventilation ◽  
Left Lung ◽  
Co2 Concentration ◽  
Gas Transfer ◽  
O2 Uptake ◽  
Tissue Metabolism ◽  
End Tidal

Gas exchange was studied under conditions of zero perfusion both in situ and in vitro. Six dogs, anesthetized with pentobarbital sodium, underwent surgical interruption of both pulmonary and bronchial circulations to the left lung. Despite the absence of perfusion, O2 uptake for the left lung ranged from 0.76 to 0.98 ml/min, whereas CO2 elimination greatly exceeded O2 uptake ranging from 1.68 to 4.34 ml/min. In addition, CO2 output was observed to vary directly with the level of minute ventilation (VE) and inversely with end-tidal CO2 concentration. To investigate the mechanisms responsible for these findings we studied 20 excised, ventilated, but nonperfused dog lungs to evaluate the relative roles of tissue metabolism and transpleural diffusion to gas exchange. The results obtained with these excised lungs under conditions of varying VE and extrapleural gas concentrations indicate that the high respiratory exchange ratios observed in situ can be explained by the greater rate with which CO2 diffuses through the pleura, and that reduced ventilation decreases total gas transfer by decreasing the transpleural partial pressure driving gradient. Our data further document that the concentration of CO2 in alveolar gas may differ significantly from that present in inspired gas under conditions of ventilation-perfusion ratio equal to infinity, and that tissue metabolism as well as transpleural diffusion contribute to gas exchange in nonperfused lung.

Operation Everest II: pulmonary gas exchange during a simulated ascent of Mt. Everest

1987 ◽  
Vol 63 (6) ◽  
pp. 2348-2359 ◽  
Author(s):  
P. D. Wagner ◽  
J. R. Sutton ◽  
J. T. Reeves ◽  
A. Cymerman ◽  
B. M. Groves ◽  
...  
Keyword(s):  
Arterial Pressure ◽  
Sea Level ◽  
Pulmonary Arterial Pressure ◽  
Flow Distribution ◽  
Barometric Pressure ◽  
Normal Subjects ◽  
O2 Uptake ◽  
Mean Pulmonary Arterial Pressure ◽  
Pulmonary Arterial

Eight normal subjects were decompressed to barometric pressure (PB) = 240 Torr over 40 days. The ventilation-perfusion (VA/Q) distribution was estimated at rest and during exercise [up to 80–90% maximal O2 uptake (VO2 max)] by the multiple inert gas elimination technique at sea level and PB = 428, 347, 282, and 240 Torr. The dispersion of the blood flow distribution increased by 64% from rest to 281 W, at both sea level and at PB = 428 Torr (heaviest exercise 215 W). At PB = 347 Torr, the increase was 79% (rest to 159 W); at PB = 282 Torr, the increase was 112% (108 W); and at PB = 240 Torr, the increase was 9% (60 W). There was no significant correlation between the dispersion and cardiac output, ventilation, or pulmonary arterial wedge pressure, but there was a correlation between the dispersion and mean pulmonary arterial pressure (r = 0.49, P = 0.02). When abnormal, the VA/Q pattern generally had perfusion in lung units of zero or near zero VA/Q combined with units of normal VA/Q. Alveolar-end-capillary diffusion limitation of O2 uptake (VO2) was observed at VO2 greater than 3 l/min at sea level, greater than 1–2 l/min VO2 at PB = 428 and 347 Torr, and at higher altitudes, at VO2 less than or equal to 1 l/min. These results show variable but increasing VA/Q mismatch with long-term exposure to both altitude and exercise. The VA/Q pattern and relationship to pulmonary arterial pressure are both compatible with alveolar interstitial edema as the primary cause of inequality.

Pulmonary gas exchange during exercise in athletes. I. Ventilation-perfusion mismatch and diffusion limitation

1994 ◽  
Vol 77 (2) ◽  
pp. 912-917 ◽  
Author(s):  
S. R. Hopkins ◽  
D. C. McKenzie ◽  
R. B. Schoene ◽  
R. W. Glenny ◽  
H. T. Robertson
Keyword(s):  
Gas Exchange ◽  
Aerobic Capacity ◽  
Maximal Exercise ◽  
Cycle Ergometer ◽  
Pulmonary Gas Exchange ◽  
Inert Gases ◽  
Inert Gas ◽  
Diffusion Limitation ◽  
Maximal Aerobic Capacity ◽  
Arterial Blood

To investigate pulmonary gas exchange during exercise in athletes, 10 high aerobic capacity athletes (maximal aerobic capacity = 5.15 +/- 0.52 l/min) underwent testing on a cycle ergometer at rest, 150 W, 300 W, and maximal exercise (372 +/- 22 W) while trace amounts of six inert gases were infused intravenously. Arterial blood samples, mixed expired gas samples, and metabolic data were obtained. Indexes of ventilation-perfusion (VA/Q) mismatch were calculated by the multiple inert gas elimination technique. The alveolar-arterial difference for O2 (AaDO2) was predicted from the inert gas model on the basis of the calculated VA/Q mismatch. VA/Q heterogeneity increased significantly with exercise and was predicted to increase the AaDO2 by > 17 Torr during heavy and maximal exercise. The observed AaDO2 increased significantly more than that predicted by the inert gas technique during maximal exercise (10 +/- 10 Torr). These data suggest that this population develops diffusion limitation during maximal exercise, but VA/Q mismatch is the most important contributor (> 60%) to the wide AaDO2 observed.

Effect of residence at altitude on the perception of breathlessness on return to sea level in normal subjects

1993 ◽  
Vol 84 (2) ◽  
pp. 159-167 ◽  
Author(s):  
Rachel C. Wilson ◽  
W. L. G. Oldfield ◽  
P. W. Jones
Keyword(s):  
Oxygen Consumption ◽  
Tidal Volume ◽  
Sea Level ◽  
Minute Ventilation ◽  
Normal Subjects ◽  
Cycle Ergometer ◽  
Respiratory Frequency ◽  
Borg Scale ◽  
Oxygen Pulse ◽  
Ventilatory Equivalent

1. The effect of residence at altitude on the perception of breathlessness after return to sea level was examined in normal subjects. Breathlessness (Borg scale), minute ventilation, respiratory frequency, tidal volume, ‘oxygen pulse’ (oxygen consumption/heart rate) and the ventilatory equivalent for oxygen (minute ventilation/oxygen consumption) were measured at exercise (cycle-ergometer) during 5 months of training before 4 weeks at 4000 m and during the 6 month period after return to sea level. 2. There was no change in the subjects' pattern of breathing (respiratory frequency and tidal volume) or ‘oxygen pulse’ after the period at altitude (P = 0.0001). The ventilatory equivalent for oxygen was increased at all work rates after the period at altitude (P = 0.02). This ratio was slightly lower after 6 weeks and had returned to normal by 6 months (P = 0.4). 3. During training there was no change in breathlessness score (P = 0.6). On return to sea level, breathlessness score relative to ventilation was reduced (P = 0.0001). This was maintained for at least 6 weeks, but not as long as 6 months. 4. This study has demonstrated that, in normal subjects, the otherwise stable and reproducible relationship between breathlessness and ventilation may be disrupted for several weeks by factors other than lung disease. 5. The mechanism responsible for this is not clear, but the observations are consistent with the hypothesis that prior experience of breathlessness may condition subsequent estimates of breathlessness.

Effects of beta-adrenergic blockade on ventilation and gas exchange during exercise in humans

1983 ◽  
Vol 54 (5) ◽  
pp. 1306-1313 ◽  
Author(s):  
E. S. Petersen ◽  
B. J. Whipp ◽  
J. A. Davis ◽  
D. J. Huntsman ◽  
H. V. Brown ◽  
...  
Keyword(s):  
Heart Rate ◽  
Gas Exchange ◽  
Time Constant ◽  
Minute Ventilation ◽  
Work Rate ◽  
Beta Blockade ◽  
Adrenergic Blockade ◽  
O2 Uptake ◽  
Beta Adrenergic ◽  
Co2 Partial Pressure

The effects of beta-adrenergic blockade induced by intravenous propranolol hydrochloride (0.2 mg/kg) on ventilatory and gas exchange responses to exercise were studied during tests in which the work rate was either increased progressively or maintained at a constant load in six healthy young male subjects. Heart rate during exercise decreased by about 20% and cardiac output, as estimated by a modification of the method of Kim et al. (J. Appl. Physiol. 21: 1338–1344, 1966), by about 15%. The relation between work rate and O2 uptake (VO2) was unaffected by propranolol, whereas maximal O2 uptake (VO2max) decreased by 5% and the anaerobic threshold, estimated noninvasively, was lowered by 23%. The relations between CO2 output (VCO2) and end-tidal CO2 partial pressure (PCO2) and between VCO2 and minute ventilation (VE) were both unaffected. The time constants for changes of VO2, VCO2, and VE during on-transients from unloaded pedaling to either a moderate (ca. 50% VO2max) or a heavy (ca. 67% VO2max) work rate in the control studies were in agreement with previously reported values, i.e., 42, 60, and 69 s, respectively. beta-Blockade was associated with a significantly increased time constant for VO2 of 61 s but with less consistent and insignificant changes for VCO2 and VE. There was a small but significant increase of the time constant for heart rate from 40 to 45 s. It is concluded that propranolol exerts its primary influence during exercise on the cardiovascular system without any discernible effect on ventilatory control.

Susceptibility of different gases to ventilation-perfusion inequality

1979 ◽  
Vol 46 (2) ◽  
pp. 372-386 ◽  
Author(s):  
P. D. Wagner
Keyword(s):  
Gas Exchange ◽  
Partition Coefficient ◽  
Geometric Mean ◽  
Differential Susceptibility ◽  
Inert Gas ◽  
O2 Uptake ◽  
Compartment Models ◽  
Algebraic Analysis ◽  
Co2 Output ◽  
Different Gases

Calculations of O2 and CO2 transfer in lung models of both series and parallel ventilation-perfusion (VA/Q) inequality have been performed by several investigators. In some cases, O2 uptake was found to be depressed more than CO2 output but in other examples CO2 elimination was interfered with to a greater extent. To understand the fundamental basis of differential susceptibility of various gases to VA/Q inequality, an algebraic analysis of inert gas exchange in two-compartment models of both series and parallel inequality is presented. For both types of inequality, the result is remarkably simple, in that the gas most affected is one whose partition coefficient is the geometric mean of the ventilation-to-perfusion ratios of the two compartments. Transfer of O2 and CO2 in these models was predicted well by the inert gas results not only qualitatively but even quantitatively. Similarly good quantitative predictions were obtained in more complicated multicompartment VA/Q distributions. The results therefore explain and reconcile the findings of various reported studies and in particular account for the observation that CO2 transfer is compromised in many examples of series inequality.

Sign in / Sign up

Export Citation Format

Share Document